<?xml version="1.0" encoding="UTF-8"?><WMS_Capabilities version="1.3.0" updateSequence="53365" xmlns="http://www.opengis.net/wms" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.opengis.net/wms https://ows.emodnet-seabedhabitats.eu/geoserver/schemas/wms/1.3.0/capabilities_1_3_0.xsd">
  <Service>
    <Name>WMS</Name>
    <Title>EMODnet Seabed Habitats  Map Library WMS Service</Title>
    <Abstract>WMS end-point for individual habitat maps and models held by EMODnet Seabed Habitats.&#13;
&#13;
Includes all data with access limitations as "View and Download" or "View only"</Abstract>
    <KeywordList>
      <Keyword>WMS</Keyword>
      <Keyword>Geoserver</Keyword>
      <Keyword>EMODnet</Keyword>
    </KeywordList>
    <OnlineResource xlink:type="simple" xlink:href="http://www.emodnet-seabedhabitats.eu"/>
    <ContactInformation>
      <ContactPersonPrimary>
        <ContactPerson>JNCC EMODnet Seabed Habitats Team</ContactPerson>
        <ContactOrganization>Joint Nature Conservation Committee</ContactOrganization>
      </ContactPersonPrimary>
      <ContactPosition/>
      <ContactAddress>
        <AddressType>Office</AddressType>
        <Address>Joint Nature Conservation Committee</Address>
        <City>Peterborough</City>
        <StateOrProvince>Cambridgeshire</StateOrProvince>
        <PostCode>PE1 1JY</PostCode>
        <Country>UK</Country>
      </ContactAddress>
      <ContactVoiceTelephone/>
      <ContactFacsimileTelephone/>
      <ContactElectronicMailAddress>euseamap@jncc.gov.uk</ContactElectronicMailAddress>
    </ContactInformation>
    <Fees>None</Fees>
    <AccessConstraints>None</AccessConstraints>
  </Service>
  <Capability>
    <Request>
      <GetCapabilities>
        <Format>text/xml</Format>
        <DCPType>
          <HTTP>
            <Get>
              <OnlineResource xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?SERVICE=WMS&amp;"/>
            </Get>
            <Post>
              <OnlineResource xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?SERVICE=WMS&amp;"/>
            </Post>
          </HTTP>
        </DCPType>
      </GetCapabilities>
      <GetMap>
        <Format>image/png</Format>
        <Format>application/atom+xml</Format>
        <Format>application/json;type=utfgrid</Format>
        <Format>application/pdf</Format>
        <Format>application/rss+xml</Format>
        <Format>application/vnd.google-earth.kml+xml</Format>
        <Format>application/vnd.google-earth.kml+xml;mode=networklink</Format>
        <Format>application/vnd.google-earth.kmz</Format>
        <Format>image/geotiff</Format>
        <Format>image/geotiff8</Format>
        <Format>image/gif</Format>
        <Format>image/jpeg</Format>
        <Format>image/png; mode=8bit</Format>
        <Format>image/svg+xml</Format>
        <Format>image/tiff</Format>
        <Format>image/tiff8</Format>
        <Format>image/vnd.jpeg-png</Format>
        <Format>image/vnd.jpeg-png8</Format>
        <Format>text/html; subtype=openlayers</Format>
        <Format>text/html; subtype=openlayers2</Format>
        <Format>text/html; subtype=openlayers3</Format>
        <DCPType>
          <HTTP>
            <Get>
              <OnlineResource xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?SERVICE=WMS&amp;"/>
            </Get>
          </HTTP>
        </DCPType>
      </GetMap>
      <GetFeatureInfo>
        <Format>text/plain</Format>
        <Format>application/vnd.ogc.gml</Format>
        <Format>text/xml</Format>
        <Format>application/vnd.ogc.gml/3.1.1</Format>
        <Format>text/xml; subtype=gml/3.1.1</Format>
        <Format>text/html</Format>
        <Format>application/json</Format>
        <DCPType>
          <HTTP>
            <Get>
              <OnlineResource xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?SERVICE=WMS&amp;"/>
            </Get>
          </HTTP>
        </DCPType>
      </GetFeatureInfo>
    </Request>
    <Exception>
      <Format>XML</Format>
      <Format>INIMAGE</Format>
      <Format>BLANK</Format>
      <Format>JSON</Format>
    </Exception>
    <Layer>
      <Title>EMODnet Seabed Habitats  Map Library WMS Service</Title>
      <Abstract>WMS end-point for individual habitat maps and models held by EMODnet Seabed Habitats.&#13;
&#13;
Includes all data with access limitations as "View and Download" or "View only"</Abstract>
      <!--All supported Coordinate Reference Systems:-->
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      <CRS>EPSG:2013</CRS>
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        <Title>Hierarchical benthic habitat classification in the Atlantic Ocean (Mission Atlantic)</Title>
        <Abstract>Group for the Hierarchical benthic habitat classification in the Atlantic Ocean layers.  Classification of the Atlantic Ocean seabed into broad-scale benthic habitats employing a hierarchical top-down clustering approach aimed at informing Marine Spatial Planning. This work was performed at the University of Plymouth in 2021 with data provided by a wide group of partners representing the nations surrounding the Atlantic Ocean. It classifies continuous environmental data into discrete classes that can be compared to observed biogeographical patterns at various scales. It has 3 levels of classification. For ease of use, a layer is provided for each level. Level 1 has 4 classes. Level 2 has 15 classes nested within level 1. Layers indices are 2 digits (1[level1 class index]1[level 2 class index]). Level 3 has 157 classes nested within level 2 and class names have 4 digits (1digit[level1 class index]1[level 2 class index]2[level 3 class index]). Note that the classification was performed for the whole world and thus it has more classes than in the presented layer.</Abstract>
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          <Title>Hierarchical_classifications_group style</Title>
          <Abstract>Default style for Hierarchical_classifications_group layer</Abstract>
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          <Abstract>Seabed habitat map (Habitat Directive classification system) performed by Stareso, Evemar and Sintinelle within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
Digital data sources: sonar (2010-2011), orthos (2010-2011), historical data (Pasqualini, 1997)
Ground truth data sources (2002-2012): diving, sea-viewer, direct human observations
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          <Abstract>Seabed habitat map (Habitat Directive classification system) performed by Stareso, Evemar and Sintinelle within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
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          <Abstract>Seabed habitat map (Habitat Directive classification system) performed by Stareso, Evemar and Sintinelle within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
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          <Title>[GB001232] ANNEX I habitat for Stanton Banks SCI</Title>
          <Abstract>Stanton Banks was designated as a Special Area of Conservation (SAC) through the Offshore Marine Conservation (Natural Habitats) Regulations 2007 and has now been accepted as a Site of Community Importance (SCI).  The Joint Nature Conservation Committee (JNCC) in partnership with Cefas and supported by British Geological Survey (BGS) staff conducted a field survey to investigate the presence and extent of Annex I habitat features within the Stanton Banks SCI in order to facilitate discussions on possible fisheries management options.  The survey was designed to acquire 
sufficient data to provide a robust characterisation of the Annex I rocky reef habitats, targeting areas of particular interest to fishers, and to contribute to the development of a robust baseline for future monitoring within the proposed SAC.  In addition, the survey involved the characterisation and mapping of the sedimentary habitats surrounding the reef feature within the site boundary, in order to provide information on the wider environmental context.</Abstract>
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          <Title>[GB001260] Map describing potential MDAC coverage within pockmarks at Braemar Pockmarks SAC</Title>
          <Abstract>A composite Habitats Directive Annex I feature extent map of Submarine structures made by leaking gases for the Braemar Pockmarks SAC was created by British Geological Survey for JNCC to provide the most up-to-date knowledge of Methane-Derived Authigenic Carbonate (MDAC) coverage within the site.

Existing polygon data from the 2012 JNCC/CEFAS survey (CEND19x/12 )  was combined  groundtruthing  information (PB and BGS datasets), to build  a composite understanding of “High” and “Potential” Annex I feature within the site.</Abstract>
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          <Title>[GB001261] Map describing potential MDAC coverage within pockmarks at Scanner Pockmarks SAC</Title>
          <Abstract>A composite Habitats Directive Annex I feature extent map of Submarine structures made by leaking gases for the Scanner Pockmarks SAC was created by British Geological Survey for JNCC to provide the most up-to-date knowledge of Methane-Derived Authigenic Carbonate (MDAC) coverage within the site.

Existing polygon data from the 2012 JNCC/CEFAS survey (CEND19x/12 )  was combined with information extracted from previous surveys. Backscatter data and side scan sonar data was used to characterise the nature of the seafloor, in particular the presence of methane-derived authigenic carbonate (MDAC), to build  a composite understanding of “High” and “Potential” Annex I feature within the site.</Abstract>
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          <Title>[GB001327] ANNEX I habitat for Bassurelle Sandbank Site of Community Importance (SCI)</Title>
          <Abstract>An ArcGIS polygon shapefile of the potential extent of Annex I sandbank habitat identified at Bassurelle Sandbank SCI was created using the data collected and processed as described below.

EUNIS class assignments from the particle size data were used in conjunction with the interpreted still images to inform the semi-automated process of map production using object-based image analysis (OBIA), implemented in the software package eCognition v8.8.1. The OBIA was used to map habitats. It was not possible to use this technique for the mapping of Annex I habitats (specifically the sandbank feature at Bassurelle Sandbank SCI). Instead, an expert driven process of slope analysis in ArcGIS 9.3.1 and 3D visual interpretation using the Fledermaus v7 software package was used to identify the potential extent of the bank feature.</Abstract>
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          <Title>[GB001552] Composite map describing MDAC coverage at Croker Carbonate Slabs SAC</Title>
          <Abstract>A composite Habitats Directive Annex I feature extent map of Submarine structures made by leaking gases for the Croker Carbonate Slabs cSAC/SCI was created by JNCC staff to provide the most up-to-date knowledge of MDAC coverage within the site.

Existing polygon data from three previous surveys (CEND1108, CEND0513 and CEND2315) and habitat maps were combined with groundtruthing point information, to build  a composite understanding of “High” and “Potential” Annex I feature within the site.</Abstract>
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          <Title>[GB003026] ANNEX I habitat for Anton Dohrn Seamount</Title>
          <Abstract>The cruise took place between the 1st and 29th of July 2009 and surveyed two Areas of Search (AoS) for offshore Special Areas of Conservation (SACs): Anton Dohrn Seamount located 155km west of the St Kilda archipelago, and East Rockall Bank located 260km west of the St Kilda archipelago. The main aims of the survey were to acquire acoustic and photographic ?ground-truthing? data to enable geological, geomorphological and biological characterisation of the Anton Dohrn Seamount and East Rockall Bank AoS. Specifically, the data acquired will lead to the production of broadscale habitat maps, the identification and description of Annex I reef habitats with particular attention to the occurrence of bedrock, stony and biogenic reef, to identify and record any anthropogenic impacts in the areas of search and finally to evaluate data acquisition methods, techniques and equipment.</Abstract>
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          <Abstract>The purpose of this section of the project is to utilise the provided multibeam bathymetry and backscatter mosaic, processed sidescan sonar data layers and seabed substrate layers for integration and interpretation with other datasets to ultimately deliver seabed habitat data layers. 
JNCC required Fugro EMU to map the Annex 1 Reef habitat  where possible and, where sufficient data exist, Annex 1 Reef subtypes. JNCC also require that a seabed habitat map is created to as detailed a hierarchical level as possible within EUNIS, where data are sufficient to enable this.

The project report (14/J/3/02/2570/1626) details the methods used in analysing the data providedwith a specified level of confidence. The following deliverables were produced with the report: 
• Derived data layers from MBES (hillshade, slope and rugosity)
• Seabed substrate data layer
• Seabed habitat data layers (including Annex 1 reef and reef subtypes and EUNIS)
• MEDIN metadata (xls/xml)

All data have been referenced to the WGS84 datum.</Abstract>
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          <Abstract>It is widely recognised that M. modiolus reefs represent biodiversity ‘hotspots’ (e.g. Rees et al., 2008). In the Craigbrain and Burial Island Modiolus reefs, diversity indices from samples containing more than 9 live Modiolus per m2 showed numbers of taxa per sample ranging from 31 to 161, Shannon-Weiner diversity indices of between 2.0 and 4.3, and Pielou’s evenness index ranging from 0.52 to 0.95, which are all comparable to figures from similar open coast Modiolus reefs such as those of North Llyn and sites in Loch Alsh (see Fariñas-Franco et al., 2014). The diversity indices did not differ markedly from the surrounding area which is characterised by muddy sandy gravels with high shell content (mostly dead Modiolus shell), however the infaunal communities were significantly different between “Modiolus reef” and “surrounding sediments” (as determined through multivariate community analysis, including cluster analysis and ANOSIM routines). Due to inconsistencies in recording of epifaunal species from the grab samples, the epifaunal communities could not be statistically examined; however it was clear that there is a marked increase in the number of epifaunal species over the reef areas. Density of living Modiolus ranged from zero to 530 per m2 . These numbers are similar to those in other open coast reefs, such as the North Llyn beds (Fariñas-Franco et al., 2014), and the variation in numbers per m2 is indicative of the patchy nature of the reefs. The Craigbrain site appears to show the highest numbers of living Modiolus per m2 , however due to the limited number of samples and small areal coverage of grab samples it cannot be concluded that this reef site is markedly different from the Burial Island reef site, and the infaunal community analysis does not show statistically significant differences between the Craigbrain and Burial Island reef sites.</Abstract>
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          <Abstract>Map of MDAC extent created from a side scan survey of Holden Reef boundary region 2017. This Annex I habitat 'Submarine structures made by leaking gases' is within the Pen Llyn a'r Sarnau/Lleyn Peninsula and the Sarnau SAC.</Abstract>
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          <Abstract>The description and mapping of marine habitat types according to Annex I of Directive 92/43/EOK (EEC, 1992) and / or the European Nature Information System (EUNIS) in 66 of approximately 300 Greek NATURA 2000 network sites, were the subject of Research Work for the Ministry of Environment Planning and Public Works of Greece. This research project, under the name: Identification and description of habitat types at sites of interest for conservation, lasted from 1999 to 2002 and was carried out by the National Centre for Marine Research (NCMR, renamed as Hellenic Centre for Marine Research - HCMR since 2003) in association with the Institute of Marine Biology of Crete (IBCM, joined to HCMR since 2003), the Aristotle University of Thessaloniki and the Fisheries Research Institute (FRI). The recognition and imprinting of marine habitat types was based on the combined use of aerial photos of scale 1:5000 acquired during the second half of 1999 for the needs of the project, data from the scientific echo sounder Sea-Bed discrimination system RoxAnn, phytobenthos samples and in situ observations by scuba diving and underwater cameras. Regarding the sampling, hard bottom samplings were carried out using SCUBA diving. The samples were collected on hard substrates mainly in the upper infralittoral zone (30 to 50 cm below the lowest sea level). For the study of the soft bottom habitats, oceanographic cruses were carried out with the IMBC R/V Filia, using a Smith McIntyre sediment sampler.</Abstract>
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          <Title>[FR004025] Seabed Habitat (Habitat Directive) - FR5300033  'Iles Houat Hoedic'  - FR004025</Title>
          <Abstract>Seabed habitat map performed by SARL - TBM Chauvaud and HOCER within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB). Map confidence (rated by Ifremer, January 2021) : 70%</Abstract>
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          <Title>[GR789365] Habitat maps of the Protected Area of northern Karpathos and Saria (GR4210003) (December 2020)</Title>
          <Abstract>The targeted area in Greece is the Protected Area of northern Karpathos and Saria (GR4210003). According to the standard form of the SCI, its marine part has an area of 5181.74 ha, i.e. about 45% of its total area, which includes habitat 1110, habitat 1120, habitat 1170 and habitat A5.531.Bottom substrates were surveyed with a DeepVision (DE3468D) portable side scan sonar trawled on the “Saria” vessel with a high precision GPS system. The survey vessel performed a number of transects in the study sub-areas, in most cases parallel to the shoreline and with an overlap of the scanned area of the bottom between two adjacent transect lines. All data were continuously recorded onboard the survey vessel on a computer with the appropriate software systems installed . Additionally, the BlueRobotics, BLUE ROV2 (ver. heavy duty) underwater drone was used for ground truthing of the different habitat types. The sonograms of the scanned area were later used for the creation of substrate type maps of the area. Data analysis was performed with the software products DeepView Pro for the side scan sonar data, and QGIS3.12 for the creation of substrate and overview maps. Data exported in KML format by DeepView and transformed in shape files in QGIS. Polygons of the same habitat were merged so each feature within the shapefile is assigned to each habitat. To ensure that the data will display properly the shapefiles were cleaned by removing any geometry or topology errors. The shape length and area was calculated and all habitats visualized via Geoserver on MedOBIS viewer (https://portal.lifewatchgreece.eu/) in WGS84 coordinate system (EPSG:4326). An OGC standard for geospatial styling (Styled Layer Descriptor (SLD)) was used through Geoserver to create styles for each layer. The Open Street Map was used as a basemap, as it is an updated open source map.</Abstract>
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          <Title>[GB100244] 2012 Natural England (NE) Solent Maritime SAC - Intertidal Survey</Title>
          <Abstract>Centre for Marine and Coastal Studies (CMACS) Ltd were contracted by Natural England to carry out feature condition monitoring on intertidal features within the Solent Maritime Special Area of Conservation (SAC) which encompassed Chichester Harbour, Langstone Harbour, Southampton Water, West Solent and the northern coast of the Isle of Wight. 
      
     Surveys were based around transects with a 400m wide corridor (i.e. 200m either side of the transect) and with locations for target notes placed at 50m intervals within the survey corridor.  Surveys were carried out on foot where the intertidal area was small and/or firm underfoot and from a hovercraft where soft sediments were present. 
      
     Target notes and photographs of visible flora and fauna were supplemented with 0.01m2 core samples consisting of five faunal replicates and a further one for particle size analysis (PSA), as well as 1m2 quadrats dug out to 20cm to aid biotope classification.  Samples were sieved at 0.5mm and all invertebrates enumerated and biomass estimated by wet weight by species. 
      
     Chichester Harbour was characterised by mud habitats in the upper reaches with sand shores to the south of Thorney Island and near to the harbour mouth.  Algal mats were recorded in the upper reaches of the harbour, notably Bosham Channel, where seagrass was also present but extensive beds were only discovered recorded from the southwestern corner of the harbour.  Fauna in the muddy areas was dominated by oligochaetes and cirratulid polychaetes especially Tubificoides benedii and Tharyx killariensis as well as the small gastropod Hydrobia ulvae.  In sandy areas, the fauna was characterised by the lugworm Arenicola marina, the orbiniid polychaete Scoloplos armiger and tanaid crustaceans. 
      
     Langstone Harbour was also characterised by mud habitats almost throughout the entire area but with some areas of coarse mixed sediment on the upper shore which supported a wide variety of macroalgae but which also showed signs of bait digging.  Algal mats were much more prevalent in Langstone Harbour than in Chichester Harbour but seagrass was also much more extensive.  The fauna of the samples from Langstone Harbour was very similar to that of Chichester Harbour with a numerical dominance of cirratulids, oligochaetes and Hydrobia ulvae. 
      
     In Southampton Water, there was a greater mix of habitats from tide-swept coarse sediment to fine silt and clay.  The tide-swept gravels and pebble at the mouth of the Hamble Estuary supported a diverse assemblage of macroalgae and epifauna which included ascidians, barnacles, bivalves and sponges.  Within the Hamble Estuary itself, there were very soft fine sediments which supported cockles but there were also thick algal mats which supported large numbers of Hydrobia ulvae but caused anoxia at the mud surface.  Soft, fine sediments were also encountered on the western side of Southampton Water from Calshot to Hythe with a fauna dominated by Tharyx killariensis but with large numbers of cockles and Hydrobia ulvae near Calshot itself. 
      
     On the seaward side of Calshot, to western side of the Beaulieu Estuary, there were coarse mixed sediments which supported ephemeral algae, small actiniarians, and a rich fauna of polychaetes, amphipods and molluscs.  There was also a large seagrass bed on the lower shore at Calshot and evidence of bait digging in these areas, particularly at Lepe Beach.  Within the Beaulieu and Lymington Estuaries the habitats were fine, soft sediments with a similar fauna to the mud areas of Chichester and Langstone Harbours but with a greater prevalence of ragworm and tellins. 
      
     The north coast of the Isle of Wight was characterised by protrusions of clay and outcrops of bedrock which supported piddocks and a rich crustacean fauna as well as a variety of macroalgae predominantly fucoids.  In addition, the habitats of Thorness Bay included mixed coarse sediment supporting barnacles and littorinids and sand supporting sand mason worms and small patches of seagrass beds.  The very sheltered areas of Newtown Harbour and the Medina Estuary where typically mud habitats with cockles and thick algal mat but also with some mixed sediments mid estuary which supported cockle, sponges and littorinids.</Abstract>
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          <Title>[GB100249] 2012 Natural England (NE) The Wash and North Norfolk Coast SAC - Baseline Monitoring Survey of Large Shallow Inlet and Bay</Title>
          <Abstract>This report describes the results from an interdisciplinary field survey aimed at identifying the  location, extent and condition of Annex I habitat features in the Large Shallow Inlet and Bay of The  Wash and North Norfolk Coast SAC.  The habitat features of interest are (i) subtidal boulder and  cobble communities, and (ii) Sabellaria spinulosa reefs.  Information presented is intended to serve  as a baseline for future monitoring of the identified features.  Acoustic sidescan data were acquired from selected areas within the broader SAC area, together  with grountruthing samples representative of distinct acoustic signatures.  Groundtruthing  techniques included the acquisition of video and still images of the seabed and of sediment and  faunal sample. 
     Of particular interest was an  area to the north of the eastern Well survey area between 10 and 47 m deep which exhibited a high  density of hard and rugged features, confirmed as boulder and cobble reef on chalk bedrock by the  photographic record.  This area also harboured a high number of epifaunal taxa not observed in the  surrounding sediments.  The area has been delimited and covers approximately 470 ha.  The acoustic record did not reveal the occurrence of areas of Sabellaria spinulosa reef.  Infaunal  samples did collect representatives of this species but in densities too small to be considered as reef.   At most sites where S. spinulosa was observed, the abundance and diversity of the whole infaunal  assemblage was higher than in areas where S. spinulosa was absent.   Analysis of both infaunal and epifaunal assemblages revealed several distinct communities throughout the survey area.</Abstract>
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          <Title>Biotope Mapping of the Intertidal Reef Feature at Flamborough Head Special Area of Conservation</Title>
          <Abstract>The data gathered from the surveys was used to compare to the original biotopes recorded in 2001, and provide an assessment of the Reef Feature using advice from Regulation 33. The main notable differences were the loss off Mytilus biotopes from transects 2 and 4, and a expansion in Mytilus biotopes in transect 9. The first target set by Regulation 33, of no decrease in extent and diversity of rocky shore biotopes has been met, with Flamborough Head still notable for its range of rocky shore biotopes. The second target set is to ensure that the distribution of characteristic chalk cliff biotopes, does not significantly decrease from the original baseline survey but this could not be assessed.</Abstract>
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          <Title>[GB100362] 2015 Natural England (NE) Shell Flat and Lune Deep Site of Community Importance (SCI) - Drop-Down Video Survey</Title>
          <Abstract>In order to help inform site condition monitoring, Seastar Survey Ltd. were contracted by Natural England to undertake a drop-down video (DDV) survey of the Lune Deep reefs feature with the aim of defining the distribution and extent of any subtidal boulder and/or bedrock reef communities and establishing a baseline for the site against which future condition of these reef sub-features can be assessed.  The survey plan was designed to assess the extent and distribution of reef features using a high definition Freshwater Lens Camera System (FLCS).  Camera stations were selected using existing acoustic data supplied to Seastar Survey by Natural England.  Thirty-nine transects were successfully surveyed.</Abstract>
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            <Keyword>habitat</Keyword>
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          <Abstract>Mapping of the Natura 2000 site FR5300017 "Abers - Côte des légendes"  was jointly performed in the framework of three different actions: (i) the Natura 2000 convention for Brittany, and (iii) CARTHAM Project.
It is based on the interpretation of various types of data from a number of surveys carried out between 2005-2012 both in the intertidal and subtidal zones. Additionally the seabed « Carte G » from the French hydrographic survey (SHOM) was used in the interpretation process.
In the tidal zone the identification was made by interpreting coastal ortho-photographs from BD Ortho (2005 et 2009) and digitising them on scale 1 : 2000ème with further qualification of the polygons based on ground truth data.
The compilation comprises the following various data sources.
Lamarche S., Bajjouk T., 2013. Cartographie des habitats benthiques intertidaux du site Natura 2000 FR 5300017 - Abers - Côtes des légendes - Parties estuariennes. Réf. RST - DYNECO/AG/13-05/TB.
Rollet C., Bonnot-Courtois Ch., Hamon N. et Loarer R., 2010. Carte des habitats benthiques intertidaux du secteur des Abers - Zone intertidale (multisource Rebent,) - Echelle : 1/10 000
ErHold et al., (2012, unpublished). Cartographie de natures des fonds subtidaux du secteur des Abers - Côtes des légendes.
TBM, 2012. Inventaire cartographique des habitats marins du site Natura 2000 Abers Côtes des Légendes FR5300017. Rapport CRTHAM, 104 p.</Abstract>
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          <Abstract>Mapping of the Natura 2000 site « Roches de Penmarc'h » was jointly performed in the framework of two different actions: (i) the Natura 2000 convention for Brittany and (ii) the Interreg Area MeshAtlantic Project. 
It is based on the interpretation of various types of data from a number of surveys carried out between 2011-2012 both in the intertidal and subtidal zones. Additionally the seabed « Carte G » from the French hydrographic survey (SHOM) was used in the interpretation process.  
In the tidal zone the identification was made by interpreting coastal ortho-photographs from BD Ortho (2005 et 2009) and digitising them on scale 1 : 2000ème with further qualification of the polygons based on ground truth data.
For the subtidal zone, several data sources from 2011 were available: bathymetric lidar (with sounding density about 1pt*3m-2), single beam sounder on sonar and video transects, side scan sonar (resolution of about 0.2m), underwater video, grab sediment and fauna samples. In the outer rocky circalittoral zone, side scan sonar corridors were surveyed with a coverage of 30-50% depending on places. In the offshore circalittoral zone (known as La Grande vasière) where soft sediment is predominant, side scan sonar coverage was reduced to about 5-10%. In these latter two circalittoral zones, interpolation between sonar corridors was supported by SHOM « Carte G » (approx. scale 1 : 100 000) along with a 100m resolution depth DTM. On rocky seabed, exposure at the seabed was described using kinetic energy from a combination of wave and current hydrodynamic models according to the methods described in: http://doi.org/10.13155/49975
Rocky substrate in intertidal and infralittoral zones was derived from the combined interpretation of both the topographic and bathymetric Lidar DTMs and aerial photographs, where permitted by water transparency. Various representations of the DTMs (slope, hillshade) helped delineate rocky outcrops with good reliability. 
Biological qualification of the substrate polygons was made through taxonomic analysis of benthos samples collected by MNHN in the framework of the project « Ecological assessment of Natura 2000 site « Roches de Penmarc’h ».</Abstract>
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&#13;
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&#13;
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or the emodnet_open_maplibrary WCS service endpoint for vector maps https://ows.emodnet-seabedhabitats.eu/emodnet_open_maplibrary/wcs?&#13;
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More information on Technical report: Science, Technology, and Society Initiative to Minimize Unwanted Catches in European Fisheries WP1. Ecological, socioeconomic and technical characteristics of discarding fisheries Deliverable 1.2 GIS maps (juveniles) Responsible beneficiary: 1 -CSIC Contractual due date: month 24 Dissemination level: PUBLIC Report Status: FINAL Actual submission</Abstract>
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More information on Technical report: Science, Technology, and Society Initiative to Minimize Unwanted Catches in European Fisheries WP1. Ecological, socioeconomic and technical characteristics of discarding fisheries Deliverable 1.2 GIS maps (juveniles) Responsible beneficiary: 1 -CSIC Contractual due date: month 24 Dissemination level: PUBLIC Report Status: FINAL Actual submission</Abstract>
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More information on Technical report: Science, Technology, and Society Initiative to Minimize Unwanted Catches in European Fisheries WP1. Ecological, socioeconomic and technical characteristics of discarding fisheries Deliverable 1.2 GIS maps (juveniles) Responsible beneficiary: 1 -CSIC Contractual due date: month 24 Dissemination level: PUBLIC Report Status: FINAL Actual submission</Abstract>
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More information on Technical report: Science, Technology, and Society Initiative to Minimize Unwanted Catches in European Fisheries WP1. Ecological, socioeconomic and technical characteristics of discarding fisheries Deliverable 1.2 GIS maps (juveniles) Responsible beneficiary: 1 -CSIC Contractual due date: month 24 Dissemination level: PUBLIC Report Status: FINAL Actual submission</Abstract>
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&#13;
Cod (Gadus morhua) is represented by three stocks in the Baltic Sea; Eastern Baltic, Western Baltic and Kattegat cod, which is reflected in the map. “Potential spawning areas” were initially delimitated based on Hüssy (2011). In addition, the Gdansk deep as delineated by Bagge et al. (1994) was included as it sometimes contributes to reproduction of Eastern Baltic cod (Hinrichsen et al. 2016). The Gotland basin has ceased to contribute to the reproduction of cod (Hinrichsen et al. 2016). These definitions were applied in the HOLAS II project (HELCOM 2018a) based on approval by all HELCOM Contracting Parties in a review process (there referred to as ‘occasional successful spawning’ and ‘successful spawning’). Following HELCOM (2018b) additional potential spawning areas were identified by environmental thresholds for egg development and survival based on salinity and oxygen conditions (Hinrichsen et al. 2016) during 2011-2016. Separate thresholds were used for Eastern Baltic, Western Baltic and Kattegat cod. Areas denoted “high probability spawning areas” correspond to where the initial delineations (Hüssy 2011, Bagge et al. 1994) achieve the environmental threshold values.&#13;
&#13;
Stocks: Kattegat cod: ICES subdivision 21, Western Baltic cod: ICES subdivisions 22-24 Eastern Baltic cod: ICES subdivisions 24 + 25-32&#13;
&#13;
EFH type: Potential spawning areas&#13;
&#13;
Approach: Literature review combined with identification of environmental window for spawning based on: salinity and oxygen for Eastern Baltic cod, and on: salinity and depth for Western Baltic Cod and Kattegat cod&#13;
&#13;
Variables and thresholds: Eastern Baltic cod: Salinity &gt; 11, Oxygen &gt; 1.5 ml/L (annual average)&#13;
Western Baltic cod and Kattegat cod: Salinity &gt; 18, Depth &gt;20 m&#13;
&#13;
Quality: The Arkona deep is functional for spawning of both the Eastern and the Western Baltic cod and in effect, the definition of the Arcona Basin as a high probability areas in the Arkona basin reflect the result for Eastern Baltic cod.&#13;
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It is difficult to collect egg samples to verify cod spawning, as cod eggs may drift in deep areas, and instead the level of ichthyoplankton is a main source for estimation of good environmental conditions for cod spawning. Modelling based on ichthyoplankton should be validated by comparison with distribution of running adults, to resolve the potential influence of prevailing current speed. The proposed delineations are also influenced by research on the maturity of adults and histology of gonads.&#13;
The adult and juvenile cod are distributed far outside of the spawning areas depicted in the map.&#13;
&#13;
Attribute information: Raster value representing no spawning (0), potential spawning area (0.5) and high probability spawning area (1).&#13;
&#13;
References&#13;
- Bagge, O, F Thurow, E Steffensen, and J Bay (1994) The Baltic cod. Dana 10:1-28&#13;
- HELCOM (2018a) State of the Baltic Sea - Second HELCOM holistic assessment 2011-2016. Baltic Sea Environment Proceedings 155&#13;
- HELCOM (2018b) Outcome of the regional expert workshop on essential fish habitats, organized by Pan Baltic Scope project and HELCOM (HELCOM Pan Baltic Scope EFH WS 1-2018)&#13;
- Hüssy, K (2011) Review of western Baltic cod (Gadus morhua) recruitment dynamics. ICES Journal of Marine Science 68:1459-1471&#13;
- Hüssy, K, HH Hinrichsen, and B Huwer (2012) Hydrographic influence on the spawning habitat suitability of western Baltic cod (Gadus morhua). ICES Journal of Marine Science, doi:10.1093/icesjms/fss136&#13;
- Hinrichsen, HH, A Lehmann, C Petereit, A Nissling, D Ustups, U Bergström, and K. Hüssy (2016) Spawning areas of eastern Baltic cod revisited. Using hydrodynamic modelling to reveal spawning habitat suitability, egg survival probability, and connectivity patterns. Progress in Oceanography 143:13-25&#13;
SwAM (2019). Swedish Agency for Marine and Water Management. Symphony Metadata March 2019.whttps://www.havochvatten.se/download/18.67e0eb431695d86393371d86/1552566811384/bilaga-1-symphony-metadata.zip</Abstract>
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          <Title>[FI004002] Potential spawning areas for Baltic flounder (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential spawning areas for Baltic flounder was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
Baltic flounder (Platichthys solemdali) is a key species in many coastal areas of the Baltic Sea. It is the only endemic fish species of the Baltic Sea. Baltic flounder spawns in shallow coastal areas and on offshore banks, with eggs developing on the sea floor. Successful spawning may be expected at salinities down to around 5-7 (Nissling et al. 2002). ‘‘Potential spawning areas’ were initially delineated by a species distribution model (Orio et al. 2017) developed based on years 1993-1997 to consider a period with relatively better oxygen conditions, but applied with more recent data (2011-2014). The area was further delineated to encompass only areas shallower than 30 m in order to represent the demersal spawning habitat. ‘High probability spawning areas’ were identified as the sub-section encompassing salinity &gt; 6. It should be noted that flounders in the Baltic Sea were recently separated into two species, and that spawning areas of the European flounder (Platichthys flesus) are described separately. The two data layers do not overlap and can be combined to obtain a map on spawning areas for both flounder species taken together.&#13;
&#13;
Stocks: ICES identifies two stocks of Baltic flounder: ICES subdivisions 26, 28 (East of Gotland and Gulf of Gdansk), and 27, 29-32 (Northern Central Baltic Sea and Northern Baltic Sea).&#13;
&#13;
EFH Type: Spawning areas&#13;
&#13;
Approach: Species distribution modelling combined with identification of environmental salinity window and depth conditions for spawning, supplemented with additional information from monitoring in Estonian waters.&#13;
&#13;
Variables and thresholds: Depth &lt; 30 m, Salinity &gt; 6&#13;
&#13;
Quality: The data layer is based on species distribution modelling focusing on mature flounder at the spawning stage and should be considered a rough estimation.&#13;
The data layers on environmental variables are based on modelling. Other variables than those tested in the model may also be influential.&#13;
The studies from which the thresholds values for environmental variables have been obtained are based on publications conducted before the separation of Baltic flounder from European flounder but have taken the specific characteristics of the separate spawning ecotypes into account.&#13;
&#13;
Attribute information: Raster value representing no spawning (0), potential spawning area (0.5) and high probability spawning area (1).&#13;
&#13;
References:&#13;
- Momigliano, P, GP Denys, H Jokinen, and J Merilä (2018) Platichthys solemdali sp. nov. (Actinopterygii, Pleuronectiformes): a new flounder species from the Baltic Sea. Frontiers in Marine Science 5:225&#13;
- Nissling, A, L Westin, and O Hjerne (2002) Reproductive success in relation to salinity for three flatfish species, dab (Limanda limanda), plaice (Pleuronectes platessa), and flounder (Pleuronectes flesus), in the brackish water Baltic Sea. ICES Journal of Marine Science 59:93-108&#13;
- Orio, A, U Bergström, M Casini, M Erlandsson, R Eschbaum, K Hüssy, A Lehmann, L Ložys, D Ustups, and A-B Florin (2017a) Characterizing and predicting the distribution of Baltic Sea flounder (Platichthys flesus) during the spawning season. Journal of Sea Research 126:46-55&#13;
- Seifert, T, F Tauber, and B Kayser (2001) A high resolution spherical grid topography of the Baltic Sea -2nd edition. Baltic sea Science Congress, Stockholm 25-29 November 2001, Poster #147</Abstract>
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          <Title>[FI004003] Potential spawning areas for European flounder (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential spawning areas for European flounder was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
European flounder (Platichthys flesus) is a key species in many coastal areas of the Baltic Sea, mainly in the central and southern sub-basins. Adults feed in shallow, coastal areas during summer and move out to deeper areas in winter, where the spawning takes place in spring. European flounder spawns above the sea floor in deep water, in areas with sufficiently high salinity for fertilization and pelagic egg development. ‘Potential spawning areas’ were initially delineated by a species distribution model (Orio et al. 2017) developed based on years 1993-1997 to consider a period with relatively better oxygen conditions, but applied with more recent data (2011-2014). The area was further delineated to encompass only areas deeper than 30 m in order to represent pelagic spawning habitat. ‘High probability spawning areas’ were identified as the sub-section encompassing salinity &gt; 10. It should be noted that flounders in the Baltic Sea were recently separated into two species, and that spawning areas of the Baltic flounder (Platichthys solemdali) are described separately. The two data layers do not overlap and can be combined to obtain a map on spawning areas for both flounder species taken together.&#13;
&#13;
Stock: ICES identifies two stocks of European flounder in the Baltic Sea: ICES subdivisions 22-23 (Belt Sea and the Sound), and 24-25 (West of Bornholm and Southern Central Baltic Sea).&#13;
&#13;
EFH type: Spawning areas&#13;
&#13;
Approach: Species distribution modelling combined with identification of environmental salinity window and depth conditions for spawning.&#13;
&#13;
Variables and thresholds: Depth &gt; 30 m, Salinity &gt; 10&#13;
&#13;
Quality: The data layer is based on species distribution modelling focusing on mature flounder at the spawning stage and should be considered a rough estimation.&#13;
The data layers on environmental variables are based on modelling. Other variables than those tested in the model may also be influential.&#13;
The studies from which the thresholds values for environmental variables have been obtained are based on publications conducted before the separation of Baltic flounder from European flounder but have taken the specific characteristics of the separate spawning ecotypes into account.&#13;
Note: the map on European flounder spawning areas is currently missing information for the western Baltic Sea including the Kattegat.&#13;
&#13;
Attribute information: Raster value representing no spawning (0), potential spawning area (0.5) and high probability spawning area (1).&#13;
&#13;
References:&#13;
- Momigliano, P, GP Denys, H Jokinen, and J Merilä (2018) Platichthys solemdali sp. nov. (Actinopterygii, Pleuronectiformes): a new flounder species from the Baltic Sea. Frontiers in Marine Science 5:225&#13;
- Nissling, A, L Westin, and O Hjerne (2002) Reproductive success in relation to salinity for three flatfish species, dab (Limanda limanda), plaice (Pleuronectes platessa), and flounder (Pleuronectes flesus), in the brackish water Baltic Sea. ICES Journal of Marine Science 59:93-108&#13;
- Orio, A, U Bergström, M Casini, M Erlandsson, R Eschbaum, K Hüssy, A Lehmann, L Ložys, D Ustups, and A-B Florin (2017a) Characterizing and predicting the distribution of Baltic Sea flounder (Platichthys flesus) during the spawning season. Journal of Sea Research 126:46-55&#13;
- Seifert, T, F Tauber, and B Kayser (2001) A high resolution spherical grid topography of the Baltic Sea -2nd edition. Baltic sea Science Congress, Stockholm 25-29 November 2001, Poster #147</Abstract>
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          <Title>[FI004004] Potential nursery areas for flounder (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential nursery areas for flounders was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
The two flounder species in the Baltic Sea (Platichthys flesus and P. solemdali) have different reproductive strategies, spawning in the pelagic and in shallow waters, respectively. However, they utilize the same type nursery habitat. For both species, young of the year are found on shallow bottoms from June to September, primarily on sandy substrates. Flounder nursery areas were predicted by a generalized additive model with flounder abundance as response variable and seven map-based predictor variables. The model was based on data from available surveys of juvenile flounder in the Baltic Sea, compiled within the Pan Baltic Scope project (see HELCOM 2018a). To represent the nursery season and the current situation, only results from surveys performed in June-September during 2004-2018 were used, resulting in totally 2,114 samples. All abundance estimates were harmonized to numbers of juvenile flounder per square meter. Values for the predictor variables were extracted for each sampling point in GIS. The following environmental variables were used: salinity, wave exposure, water depth, slope of the bottom, surface temperature, bottom currents, and distance to high probability spawning area for European flounder.&#13;
&#13;
Stock: Baltic flounder: ICES subdivisions 26, 28 (East of Gotland and Gulf of Gdansk), and 27, 29-32 (Northern Central Baltic Sea and Northern Baltic Sea). European flounder: ICES subdivisions 22-23 (Belt Sea and the Sound), and 24-25 (West of Bornholm and Southern Central Baltic Sea).).&#13;
&#13;
EFH type: Nursery areas&#13;
&#13;
Approach: Species distribution modelling&#13;
&#13;
Variables and thresholds: High probability nursery areas represent areas with a predicted abundance &gt; 0.03 juvenile flounder/m² based on the applied data sets and model. Potential nursery areas represent predicted abundance levels between 0,0001 and 0,03 juvenile flounder/m². Areas with a predicted abundance &lt; 0.0001 juvenile flounders/m² are defined as not being flounder nursery areas.&#13;
&#13;
Quality: Data on juvenile flounder abundances to support the spatial model is missing from Denmark, Germany, Poland and Russia. Predictions are uncertain in these areas, and especially along the south coast of the Baltic Sea.&#13;
The mix of data from different years, months and gear types may have contributed to increasing the variability in the dataset, even though a relatively high deviance explained by the model (41%) shows that it has predictive power.&#13;
The spatial resolution of the predictor variables varies between 200 m and 2 km, which gives coarse predictions locally even though values are representative at an overall regional scale.&#13;
The prediction is limited by a lack of accurate spatial information on surface sediments. Sandy substrates are well known as important flounder nursery habitats. Unfortunately, the only available sediment map on a Baltic Sea wide scale was too inaccurate for shallow waters where juvenile flounder occurs and was therefore excluded from the model.&#13;
The map on flounder nursery areas does not make assumptions on species identity in any area.&#13;
&#13;
Attribute information: Raster value representing no nursery area (0), potential nursery area (0.5) and high probability nursery area (1). -999 indicates No data.&#13;
&#13;
References&#13;
HELCOM (2018a) Outcome of the regional expert workshop on essential fish habitats, organized by Pan Baltic Scope project and HELCOM (HELCOM Pan Baltic Scope EFH WS 1-2018)&#13;
HELCOM (2018b) HELCOM Map and Data service. Layers: mean slope and bottom currents. https://maps.helcom.fi/website/mapservice/. Accessed March 2019&#13;
HELCOM (2020) Essential fish habitats in the Baltic Sea – identification of potential spawning, recruitment and nursery areas.&#13;
Lehmann, A, W Krauß, and HH Hinrichsen (2002) Effects of remote and local atmospheric forcing on circulation and upwelling in the Baltic Sea. Tellus A 54:299-316</Abstract>
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          <Title>[FI004005] Potential spawning areas for herring (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential spawning areas for herring was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
Herring (Clupea harengus) is widely distributed in the Baltic Sea and is common in all sub-basins. Herring feeds in the pelagic, mainly on zooplankton, and is an important prey for cod, other fish, and marine mammals. In fisheries management, herring in the Baltic Sea is sub-divided into several stocks. Herring spawns in coastal areas or offshore shallows. It has demersal eggs, which are attached to the substrate. Spawning may occur both in spring and autumn, depending on population, but spring spawning dominates today. Spawning areas of herring were identified by main habitat associations, based on existing observations of herring spawning grounds in the Baltic Sea. ‘Potential spawning areas’ were delineated based on the distribution of any of the following: modelled photic zone, photic hard bottom, charophytes, Fucus spp, Furcellaria lumbricalis, and Zostera marina, several data layers were combined due to uncertainty in the coverage of some of them, ‘High probability’ spawning areas were identified as areas where the modelled photic zone overlaps with any of the other layers. The habitat variables were identified by other existing HELCOM data layers.&#13;
&#13;
Stock: Herring in ICES subdivisions 22-24 (spring spawning), subdivisions 25-27, 28.2, 29 and 32, subdivision 28.1 (Gulf of Riga), subdivisions 30-31.&#13;
&#13;
EFH type: Spawning areas&#13;
&#13;
Approach: Habitat associations combined with manual corrections to eastern Gulf of Finland (Neva inlet), Curonian lagoon, Szczechin lagoon, Vistula lagoon and German waters&#13;
&#13;
Variables and thresholds: Distribution of Photic zone, Photic hard bottom, Charophytes, Fucus spp., Furcellaria lumbricalis, Zostera marina. The resulting data layer was corrected by removing recruitment areas in eastern Gulf of Finland (Neva inlet), Curonian lagoon, Szczechin lagoon and enhancing that of the Vistula lagoon.&#13;
&#13;
Quality: The data layer is mainly developed based on main habitat associations as identified from scientific literature, not actual data on herring spawning.&#13;
The delineations are based on other data layers (benthic and habitat-related ecosystem components) for which mapping is not exhaustive and sampling density may vary between countries. Underlying data layers on vegetation (Fucus, Furcellaria, charophytes, Zostera) are based on inventory data and species distribution models. Information on the distribution of Furcellaria is lacking from Russia.&#13;
Herring preferably spawns in shallow areas. However, the layer does not include depth as a variable, as some known spawning areas offshore would not be included if the depth restriction is used. Due to constraints in the resolution of the underlying data layer, the map also identifies areas shallower than one meter as potential spawning areas of Baltic herring. However, spawning of Baltic herring does not usually occur in such shallow depth.&#13;
The map represents potential spawning areas. In addition, behavioral components and hydrographic factors influence on the actual chose of spawning site at a certain occasion. Due to these constraints, the data layer on Baltic herring spawning habitats should be considered as a rough estimation.&#13;
&#13;
Attribute information: Raster value representing no spawning (0), potential spawning area (0.5) and high probability spawning area (1).&#13;
&#13;
References&#13;
- Fey, DP (2001) Differences in temperature conditions and somatic growth rate of larval and early juvenile spring spawned herring from the Vistula Lagoon, Baltic Sea manifested in the otolith size to fish size relationship. Journal of Fish Biology 58: 1257–1273&#13;
- Fey, DP, AM Lejk, P Margonski, L Szymanek, I Psuty, T Nermer, F Lempe, HV Strehlow, P Polte, D Moll, N Stybel, A Hiller, and M van Laak (2014a) Herring. An analysis of spawning ground management, ecological conditions and human impacts in Greifswald Bay, Vistula Lagoon and Hanö Bight. NMFRI, Gdynia, 177 pp.&#13;
- Fey, D, A. Szkudlarek-Pawelczyk, and A. Wozniczka (2014b) Abundance and distribution of larval herring, Clupea harengus (Actinopterygii: Clupeiformes: Clupeidae) in the Pomeranian Bay, Baltic Sea as an indicator of spawning sites. Acta Ichthyologica et Piscatoria 44: 309–317&#13;
- HELCOM (2018a) HELCOM Map and Data service. Layers: mean slope and bottom currents. https://maps.helcom.fi/website/mapservice/. Accessed March 2019&#13;
- HELCOM (2018b) HELCOM Map and Data service. Layers: Seabed sediment polygon (BALANCE), Fucus distribution, Furcellaria lumbricalis distribution. https://maps.helcom.fi/website/mapservice/ Accessed 29 October 2018&#13;
- Kanstinger P, J Beher, G Grenzdörffer, C Hammer, KB Huebert, D Stepputtis, and M Peck (2018) What is left? Macrophyte meadows and Atlantic herring (Clupea harengus) spawning sites in the Greifswalder Bodden, Baltic Sea. Estuar Coast Shelf Sci 201:72-81)&#13;
- Krasovskaya, N (2002) Spawning of Baltic herring in the Vistula Lagoon: Effects of environmental conditions and stock parameters. Bulletin of Sea Fish. Inst. No. 1 (155), Gdynia: 3–25&#13;
- Popiel, J (1984) On the biology of the Baltic herring. Reports of the Sea Fisheries Institute, Gdynia, vol. 19, 8-16.</Abstract>
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          <Title>[FI004006] Potential spawning areas for sprat (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential spawning areas for sprat was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
Sprat (Sprattus sprattus) occurs in the entire Baltic Sea, and mainly in open sea areas. It is assessed as a single stock in the Baltic Sea within fisheries management. Sprat eggs are pelagic, and sprat spawning is well known from the deep basins in the central Baltic, where it typically occurs from February to August. Further north, spawning starts later in the year, and is less certain. Recent fisheries surveys indicate that sprat spawning does no longer occur in the Gulf of Finland. Sprat spawning areas were delineated using environmental variables due to lack of coherent field data across the Baltic Sea countries. “Potential sprat spawning areas” were delineated as areas with salinity &gt; 6 and water depth &gt; 30 m, but for the Arcona basin depth &gt; 20 m was used (Grauman, 1980, Bauman et al. 2006, Voss et al. 2012). “High probability spawning areas” were delineated for areas deeper than 70 m.&#13;
&#13;
Stock: Sprat in subdivisions 22-32 (ICES)&#13;
&#13;
EFH type: Potential spawning areas&#13;
&#13;
Approach: Environmental envelope, corrected for areas 20-40 m south of Bornholm.&#13;
&#13;
Variables and thresholds: Potential spawning area: Depth &gt; 30 m, Salinity &gt; 6 (annual average)&#13;
High probability spawning area: Depth &gt;70 m, Salinity &gt; 6 (annual average)&#13;
&#13;
Quality: The map is based on literature and environmental variables, not actual data on sprat spawning. The map might overestimate the spawning area west and north of Gotland. The data layers on environmental variables are based on modelling.&#13;
&#13;
Attribute information: Raster value representing no spawning (0), potential spawning area (0.5) and high probability spawning area (1).&#13;
&#13;
References:&#13;
- Baumann, H, H Hinrichsen, C Mollmann, F Koster, A Malzahn, and A Temming (2006) Recruitment variability in Baltic Sea sprat (Sprattus sprattus) in tightly coupled to temperature and transport patterns affecting the larval and early juvenile stages. Canadian Journal of Fisheries and Aquatic Science 63:2191-2201&#13;
- Grauman GB (1980) Long term changes in the abundance data of eggs and larvae of sprat in the Baltic Sea. Fisheries research in the Baltic Sea, Riga. 15:138-150 (in Russian)&#13;
- HELCOM (2018) Outcome of the regional expert workshop on essential fish habitats, organized by Pan Baltic Scope project and HELCOM (HELCOM Pan Baltic Scope EFH WS 1-2018)&#13;
- Voss R, MA Peck, HH Hinrichsen, C Clemmesen, H Baumann, D Stepputis, M Bernreuther, JO Schmidt, A Temming, and FW Köster (2012) Recruitment processes in Baltic sprat - A re-evaluation of GLOBEC Germany hypotheses. Progress in Oceanography 107:61-79</Abstract>
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          <Title>[FI004007] Potential recruitment areas for perch (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential recruitment areas for perch was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
Perch (Perca fluviatilis) is a key species in many Baltic coastal areas. It is of freshwater origin and spawns predominantly in freshwater tributaries, close to the coastline, or in enclosed bays. Species distribution modelling have shown the importance of suitable environmental conditions for perch reproduction. Young perch has limited dispersal from its spawning area, and tagging studies have shown that most (50-95 % of the recaptures of perch are made up to 20 km from tagging site (Johnsson 1978, Böhling and Lehtonen 1985, Veneranta et al. 2011, Saks et al. 2020). Due to lack of coherent data on perch spawning and nursery areas across the Baltic Sea countries, environmental variables were used in delineating potential recruitment areas for perch. The map was originally developed within the HOLAS II project (HELCOM 2018) when it was approved by all HELCOM Contracting Parties in a dedicated review process. Potential perch recruitment areas were delineated as areas with suitable condition of depth, wave exposure and salinity. Thresholds were obtained from literature, and selected to rather overestimate than underestimate the recruitment area. For the Finnish coastline, a national model was used. The map was subsequently considered by the Pan Baltic Scope project, who proposed adjustments to thresholds for some areas in Russian waters, and corrections to Estonian and German waters.&#13;
&#13;
Stock: Several, undefined&#13;
&#13;
EFH type: Recruitment areas&#13;
&#13;
Approach: Environmental window, national modelling approach in Finnish waters, supplemented with corrections to Estonian, German and Russian waters based on national validation with monitoring data.&#13;
&#13;
Variables and thresholds: Depth &lt; 4 m (for Danish waters &lt; 3 m), Logged exposure &lt; 5 (For Koporo Bay and Narva Bay in Russian waters &lt; 5.23), Salinity &lt; 10. Based on the model for the Finnish coastline, perch recruitment areas were defined as: Unsuitable for reproduction: P(catch larvae) &lt; 0.5, Suitable for reproduction: P(catch larvae) &gt; 0.5, Important for reproduction: the smallest area where the expected cumulative larval abundance is 80% of the total expected abundance over study area.&#13;
&#13;
Quality: Recruitment area here refers to essential habitats for young-of-the-year perch (based on inventory data from spawning until the end of the first summer). The map is based on literature and environmental variables, derived from inventory data. The species distribution modelling studies, where the thresholds values for environmental variables have been obtained, are from the northern Baltic Sea. Here, the same thresholds have been applied in the southern Baltic. Also, the data layers on environmental variables are based on modelling. Due to these constraints, the data layer should be considered as a rough estimation.&#13;
&#13;
Attribute information: Raster value representing the potential occurrence of perch recruitment area (either 0 or 1).&#13;
&#13;
References&#13;
- Bergström, U, G Sundblad, A-L Downie, M Snickars, C Boström, and M Lindegarth (2013) Evaluating eutrophication management scenarios in the Baltic Sea using species distribution modelling. Journal of Applied Ecology 50:680-690&#13;
- Böhling, P, and H Lehtonen (1985) Effect of environmental factors on migrations of perch (Perca fluviatilis) tagged in the coastal waters of Finland. Finnish Fisheries Research 5: 31-40&#13;
- HELCOM (2018) State of the Baltic Sea - Second HELCOM holistic assessment 2011-2016. Baltic Sea Environment Proceedings 155&#13;
- HELCOM (2020) Essential fish habitats in the Baltic Sea – identification of potential spawning, recruitment and nursery areas&#13;
- Isæus, M (2004) Factors structuring Fucus communities at open and complex coastlines in the Baltic Sea. PhD thesis, Stockholm University&#13;
- Johnsson, T (1978) Dispersal area of perch, Perca fluviatilis, tagged in a stream flowing into the Bothnian Sea. Aquilo, Series Zoologica 18: 62-64&#13;
- Kallasvuo, M, J Vanhatalo, and L Veneranta (2017) Modeling the spatial distribution of larval fish abundance provides essential information for management. Canadian Journal of Fisheries and Aquatic Sciences 74:636-649&#13;
- Saks, L, R Eschbaum, K Jürgens, and I Taal (2020) Ahvena ränded Liivi lahel ja Väinameres. Eesti Mereinstituut, Tartu. https://www.kalateave.ee/images/pdf¬/Uuringud/¬Ahvena_r%¬C3%A4nded_Liivi_lahel_-ja_V%C3%A4inameres.pdf&#13;
- Seifert, T, F Tauber, and B Kayser (2001) A high resolution spherical grid topography of the Baltic Sea -2nd edition. Baltic sea Science Congress, Stockholm 25-29 November 2001, Poster #147&#13;
- Skovrind, M, EAF Christensen, L Jacobs, and PR Moller (2013) Marine spawning sites of Perca fluviatilis revealed by oviduct-inserted acoustic transmitters. Aquatic Biology 19:201-206&#13;
- Snickars, M, G Sundblad, A Sandström, L Ljunggren, U Bergström, G Johansson, and J Mattila (2010) Habitat selectivity of substrate spawning fish - modelling requirements of the Eurasian perch, Perca fluviatilis. Marine Ecology Progress Series 398:235-243&#13;
- Sundblad, G, Bergström, U, Sandström, A, and P Eklöv (2014) Nursery habitat availability limits adult stock sizes of predatory coastal fish. ICES Journal of Marine Science 71:672-680&#13;
- Veneranta, L, L Urho, A Lappalainen, and M Kallasvuo (2011) Turbidity characterizes reproduction areas of pikeperch (Sander lucioperca (L.)) in the northern Baltic Sea. Estuarine, Coastal and Shelf Science 95:199-206</Abstract>
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          <Title>[FI004008] Potential recruitment areas for pikeperch (PBS EFH)</Title>
          <Abstract>Essential fish habitat (EFH) map on Potential recruitment areas for pikeperch was prepared in PanBalticScope project (co-founded by the European Maritime and Fisheries Fund of the European Union) http://www.panbalticscope.eu/&#13;
&#13;
Pikeperch (Sander lucioperca) is a species of freshwater origin, which spawns predominantly in freshwater tributaries and has a relatively limited dispersal away from its recruitment area. Species distribution modelling studies have shown the importance of suitable environmental conditions for pikeperch recruitment. Due to lack of coherent data on pikeperch spawning and nursery areas across the Baltic Sea countries, the distribution of pikeperch recruitment areas was delineated based on areas with suitable conditions of depth, wave exposure, salinity, water transparency (Secchi depth) and distance to deeper (10 m) waters. The threshold values were obtained from literature. Temperature, although important for pikeperch, was left out due to high variation in timing of suitable spawning temperatures across the Baltic Sea. The map on pikeperch recruitment areas was originally developed within the HOLAS II project (HELCOM 2018) when it was approved by all HELCOM Contracting Parties in a dedicated review process after correction to Swedish waters. The map was subsequently considered by the Pan Baltic Scope project, who proposed adjustments to Estonian, German, Lithuanian and Polish waters.&#13;
&#13;
Stock: Several, undefined&#13;
&#13;
EFH type: Recruitment areas&#13;
&#13;
Approach: Environmental window with national approach for Finnish waters, selected data points corrected for Estonian, German, Lithuanian, Polish, and Swedish waters.&#13;
&#13;
Variables and thresholds: Depth &lt; 5 m, Logged exposure &lt; 5, Salinity &lt; 7, Secchi depth &lt; 2, Distance to deep (10m) water &lt; 4km. Based on the model for the Finnish coastline, pikeperch recruitment areas were defined as: Unsuitable for reproduction: P(catch larvae) &lt; 0.5, Suitable for reproduction: P(catch larvae) &gt; 0.5, Important for reproduction: the smallest area where the expected cumulative larval abundance is 80% of the total expected abundance over study area.&#13;
&#13;
Quality: Recruitment area here refers to essential habitats for young-of-the-year pikeperch (based on inventory data from spawning until the end of the first summer). The map is based on literature and environmental variables, derived from inventory data. The species distribution modelling studies, where the thresholds values for environmental variables have been obtained, are from the northern Baltic Sea. Also, the data layers on environmental variables are based on modelling. Here, same thresholds have been applied in the southern Baltic. Due to these constraints, the data layer should be considered as a rough estimation. In addition, temperature is important for pikeperch recruitment but was not included as a delineating variable due to high variation in timing. The data layer may underestimate pikeperch in Finnish waters with respect to habitats for young-of-the-year pikeperch, as it focused on newly-hatched larvae when the dispersal is more limited compared to later in the season.&#13;
&#13;
Attribute information: Raster value representing the potential occurrence of pikeperch reproduction area (either 0 or 1).&#13;
&#13;
References:&#13;
- Alikas, K, and Kratzer, S (2017) Improved retrieval of Secchi depth for optically-complex waters using remote sensing data. Ecological Indicators 77: 218-227&#13;
- Bergström, U, G Sundblad, A-L Downie, M Snickars, C Boström, and M Lindegarth (2013) Evaluating eutrophication management scenarios in the Baltic Sea using species distribution modelling. Journal of Applied Ecology 50:680-690&#13;
- HELCOM (2018) State of the Baltic Sea - Second HELCOM holistic assessment 2011-2016. Baltic Sea Environment Proceedings 155&#13;
- HELCOM (2020) Essential fish habitats in the Baltic Sea – identification of potential spawning, recruitment and nursery areas&#13;
- Gunnartz, U, M Lif, P Lindberg, L Ljunggren, A Sandström, and G Sundblad (2011) Kartläggning av lekområden för kommersiella fiskarter längs den svenska ostkusten - en intervjustudie (In Swedish with summary in English). Finfo 2011:3:1-42 https://www.havochvatten.se/download/18.64f5b3211343cffddb2800018015/1348912838028/finfo2011_3.pdf&#13;
- Isæus, M (2004) Factors structuring Fucus communities at open and complex coastlines in the Baltic Sea. PhD thesis, Stockholm University&#13;
- Kallasvuo, M, J Vanhatalo, and L Veneranta (2017) Modeling the spatial distribution of larval fish abundance provides essential information for management. Canadian Journal of Fisheries and Aquatic Sciences 74:636-649&#13;
- Seifert, T, F Tauber, and B Kayser (2001) A high resolution spherical grid topography of the Baltic Sea -2nd edition. Baltic sea Science Congress, Stockholm 25-29 November 2001, Poster #147&#13;
- Sundblad, G, Bergström, U, Sandström, A, and P Eklöv (2013) Nursery habitat availability limits adult stock sizes of predatory coastal fish. ICES Journal of Marine Science 71:672-680&#13;
- Veneranta, L, L Urho, A Lappalainen, and M Kallasvuo (2011) Turbidity characterizes reproduction areas of pikeperch (Sander lucioperca (L.)) in the northern Baltic Sea. Estuarine, Coastal and Shelf Science 95:199-206</Abstract>
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          <Abstract>This dataset contains the habitats map from the SCI (Site of Community Importance) “Sistema de Cañones Submarinos Occidentales del Golfo de León”. The marine area “South-West Gulf of Lions canyons system” is located in the northeastern part of the Iberian Peninsula. The coastline belongs to the Catalan province of Girona, featuring a large number of rocky outcrops with many coves, small beaches, vertical cliffs and islets. Cape Creus is the most notorious element of the landscape, which corresponds to the easternmost part of the Pyrenees Mountains. This small peninsula is characterized by its wildness, and despite its low relief it penetrates into the Mediterranean Sea for more than 10 kilometers.This study was supported by the INDEMARES-LIFE+ Project, EC contract INDEMARES-LIFE+ (07/NAT/E/000732): Inventory and Designation of the Natura 2000 network in marine areas of the Spanish State (www.indemares.es/en). This work was coordinated by the Biodiversity Foundation (www.fundacion-biodiversidad.es). Habitats are classified according to EUNIS nomenclature and the List of Marine Habitats in Spain (LPRE, that it’s classified hierarchically and was completed and published in March 2013). Habitats classification are been simplified owing to the requirements of the EMODnet (European Marine Observation and Data Network) portal for Seabed Habitats.</Abstract>
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          <Title>[FR000003] Peuplements benthiques en Manche occidentale (zone prélittorale) (1968) au 1/180000</Title>
          <Abstract>Cette cartographie a été réalisée en 2010 d’après la carte générale de la Manche occidentale de la thèse de Louis Cabioch (Station biologique de Roscoff) "Contribution à la connaissance des peuplements benthiques de la Manche occidentale" publiée en 1968, et complétée pour la partie "Secteur Goëlo" par des données originales fournies par le même auteur.

La carte au 1 / 180 000 de la thèse a été numérisée en 2003 et les données du secteur Goëlo en 2007, dans le cadre du Réseau de surveillance de la flore et de la faune benthique marine Rebent. L’harmonisation avec la typologie EUNIS a été effectuée avec l’expertise de Frank Gentil.</Abstract>
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          <Abstract>This map of the benthic communities of the Western Channel off the north coasts of Brittany, in the region of Roscoff , is picked up from the thesis of Louis Cabioch (1968, Roscoff Biological Station) : "Contribution à la connaissance des peuplements benthiques de la Manche occidentale", published in 1968 in the "Cahiers de biologie marine, tome IX, cahier 5 supll.".

Two maps representing the distribution of the benthic communities and the tiers were in particular produced in the document cited above : a map (scale = 1:180000) entitled "Répartition générale des peuplements benthiques prélittoraux" and a map (scale = 1:50 000) (figure 45) entitled "Répartition des peuplements benthiques dans la région de Roscoff" which is that described here.

This map was digitized in 2003, as part of the REBENT programme, i.e. the surveying network for the benthic fauna and flora.

The harmonization with the EUNIS typology was made in 2006, as part of the REBENT and Interreg-MESH programmes.</Abstract>
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          <Abstract>This map of the benthic communities of the normano-breton Gulf is picked up from the thesis of Christian Rétière, entitled "Contribution à la connaissance des peuplements benthiques du golfe normanno-breton", published in 1979.

This map was digitized in 2003, as part of the REBENT programme, i.e. the surveying network for the benthic fauna and flora. The original legend is transferred to the "ORIG_HAB" attribute data fied.

The harmonization with the EUNIS typology was made in 2006, as part of the REBENT and Interreg-MESH programmes.</Abstract>
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          <Title>[FR000025] Cartographie des habitats benthiques du secteur des Glénan (REBENT, 2006)</Title>
          <Abstract>This comprehensive map of the benthic communities of Les Glénan is realized as part of the REBENT programme, i.e. the surveying network for the benthic fauna and flora. It is the result of the treatment, the analysis and the data aggregation from authors and multiple specialized agencies :
- ORTHOLITTORALE 2000,
- IFREMER, Lidar altimetry in 2005,
- M. Le Hir, S. Chauvaud, G. Robert, from the engineering firm " Télédétection et Biologie Marine " (TBM) in 2005,
- N. Alloncle, student at the Brest University in 2005,
- CEVA in 2004 and 2005,
- Bathymetric data from SHOM,
- Rebent intertidal and subtidal field studies data collected between 2003 and 2006.

For these studies, various methods were used : coastal orthophotography, altimetric data from LIDAR, acoustic techniques, benthic sampling techniques, intertidal surveys.

The habitat typology held for the cartography is the EUNIS classification, the European reference (October, 2004 version).

In the rocky sectors, groupings of EUNIS classes were realized when the EUNIS typology was difficult to apply. It allows describing more easily the various environments.

The original legend is transferred to the "ORIG_HAB" attribute data field.

The harmonization with the EUNIS typology was made in 2006, as part of the REBENT and Interreg-MESH programmes.</Abstract>
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          <Title>[FR000035] Carte des peuplements benthiques du secteur Vilaine (source : Ehrhold A., Blanchet A., Hamon D., 2008) - Echelle : 1/ 2000 à 1/10000</Title>
          <Abstract>Cette carte des peuplements benthiques de la zone subtidale du secteur Vilaine est le résultat du traitement, de l'analyse et de l'agrégation de données de :
- A. Ehrhold, A. Blanchet, D. Hamon de l'Ifremer (2004 à 2008).
- Données bathymétriques du SHOM.

Deux sources croisées d'acquisition des données ont été employées :
un système acoustique embarqué (sonar à balayage latéral), permettant de définir des premières classes de signatures acoustiques, correspondant à des unités morpho-sédimentaires, complétées par des campagnes de prélèvements à la benne (échantillons sédimentaires biologiques).

La typologie des habitats a été élaborée par les auteurs suivants : D. Hamon, A. Blanchet, A. Ehrhold.</Abstract>
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          <Title>[FR000036] Carte des peuplements benthiques subtidaux de la baie de Douarnenez (Source Blanchet A., Hamon D. et al., 2005) - Echelle 1/25000</Title>
          <Abstract>La carte numérique des peuplements benthiques de la zone subtidale du secteur Douarnenez a été publiée en 2005 dans l'Atlas thématique de l'environnement marin de la baie de Douarnenez (Partenariat Ifremer et ville de Douarnenez, Ed. Ifremer, Coordination Augris C.).

Différentes méthodes ont été employées : méthodes acoustiques (sonar à balayage latéral, sondeur multifaisceaux), prélèvements d'échantillons (benne Hamon), observations sous-marines (vidéo). La typologie des habitats a été élaborée par les auteurs suivants : D. Hamon, A. Blanchet, C. Chevalier (Ifremer/Dyneco/Benthos).</Abstract>
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            <Keyword>FR000036</Keyword>
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          <Title>[FR000037] Carte des peuplements benthiques du secteur de Concarneau (Source A. Ehrhold, A. Blanchet, D. Hamon, 2007) - Echelle : 1/2 000 à 1/10 000</Title>
          <Abstract>Cette carte des habitats benthiques de la zone subtidale du secteur de Concarneau est le résultat du traitement, de l'analyse et de l'agrégation de données de :
- A. Ehrhold, A. Blanchet, D. Hamon de l'Ifremer en 2003, 2005 et 2006,
- données bathymétriques du SHOM.

Différentes techniques d'imageries ont été employées : systèmes acoustiques embarqués et vidéo sous-marine. Les données ont été complétées par des campagnes de prélèvements à la benne. La typologie des habitats a été élaborée par les auteurs suivants : D. Hamon, A. Blanchet, A. Ehrhold.</Abstract>
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          <Title>[FR000040] Carte des peuplements benthiques de la côte landaise au large d'Arcachon (Source Monbet Y., 1972) - Echelle : 1 / 300 000</Title>
          <Abstract>Cette carte des peuplements benthiques du secteur d'Arcachon a été réalisée d’après la thèse d'Yves Monbet, intitulée " Etude bionomique du plateau continental au large d'Arcachon (application de l'analyse factorielle) ", publiée en 1972.
Cette étude sur les fonds chalutables de la côte landaise et girondine au large d’Arcachon a permis d’identifier 5 aires sédimentaires disposées parallèlement à la côte.
Les peuplements benthiques sont répartis en 2 grands ensembles, l’ensemble côtier composé de 3 peuplements et l’ensemble subcôtier de 4 peuplements.
La carte a été numérisée en 2005 et une harmonisation avec la typologie EUNIS a été effectuée en 2007 (projet REBENT).</Abstract>
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          <Title>[FR000041] Carte des peuplements de la partie française de la Mer du Nord (Source Davoult D., Dewarumez J.-M., Prygiel J., Richard A., 1988) au 1/149000</Title>
          <Abstract>Cette carte numérique est reproduite d'après la carte papier au 1/149000, réalisée par Davoult D., Dewarumez J.M., Prygiel J. et Richard A. et publiée en 1988 par la Station Marine de Wimereux, avec le concours de l'Ifremer et de la Région Nord-Pas de Calais.
Cette carte a fait l'objet en 2006 d'une numérisation dans le cadre du réseau de surveillance de la flore et de la faune benthique marine REBENT.</Abstract>
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          <Title>[FR000043] Carte biosédimentaire des fonds meubles des Pertuis charentais (Source Hily C., 1976) - Echelle 1 / 100 000</Title>
          <Abstract>Cette carte est la synthèse de cartes extraites de la thèse de Christian Hily sur les "Pertuis Charentais" publiée en 1976 et de la carte de Claude Chassé intitulée "Pertuis et îles Charentais - Carte bio-sédimentaire (Prévision)" de 1974, (avec pour la partie ouest, l'intégration des travaux géomorphologiques de J.P. Barusseau, D. Dorel et M. Tesson et des travaux de biologie de F. Lagardère (vasière de Gironde)).
Une harmonisation avec la typologie EUNIS a été réalisée en 2008, avec l’expertise de l’auteur (projets Rebent et Interreg-MESH).</Abstract>
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          <Abstract>Cette carte est la synthèse des cartes de l'atlas de Claude Chassé et Michel Glémarec de l'Université de Bretagne Occidentale, "Atlas du littoral français, atlas des fonds meubles du plateau continental du Golfe de Gascogne, cartes biosédimentaires", publié en 1976 avec le concours du CNEXO. Cet atlas comprend deux types de cartes : cinq cartes biosédimentaires côtières au 1/100000 et une carte plus générale au 1/500000.

Ces cartes ont fait l'objet en 2003 d'une numérisation dans le cadre du Réseau de surveillance de la flore et de la faune benthique marine REBENT. Sous forme numérique, ces cartes ont été regroupées en un seul lot de données.</Abstract>
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          <Title>[FR000048] Carte des peuplements macrobenthiques en Manche orientale (Source Cabioch L., Gentil F., Glaçon R., Retière C., 1978) - Echelle 1 / 100 000 à 1 / 200 000</Title>
          <Abstract>Cette carte des peuplements macrobenthiques en Manche orientale est reproduite d'après la carte, réalisée par Louis Cabioch, Franck Gentil, René Glaçon et Christian Rétière de l'Observatoire Océanologique de Roscoff, communiquée lors du colloque de l'UOF, les 26 et 27 janvier 1978 à Brest. La carte originale n'a jamais été publiée. C'est une communication directe des auteurs.

Pour cette étude, des échantillonnages ont été réalisés entre 1971 et 1975.

Cette carte a fait l'objet en 2006 d'une numérisation dans le cadre du Réseau de surveillance de la flore et de la faune benthique marine REBENT. 

Une harmonisation avec la typologie EUNIS a été réalisée en 2007, dans le cadre des projets REBENT et Interreg-MESH.</Abstract>
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          <Abstract>Cette cartographie numérique des peuplements benthiques des substrats meubles de la baie de Saint-Brieuc a été réalisée en 2010, d'après la carte au 1/50000 établie par Gérard Thouzeau de l'Université de Bretagne Occidentale et Dominique Hamon d'Ifremer centre de Brest et publiée en 1992.
Une harmonisation avec la typologie EUNIS a été réalisée en 2011 par Dominique Hamon.
Les documents à l'origine de ce jeu de données sont le résultat de travaux de recherche issus des programmes EUPHORBE et PNDR Coquille Saint-Jacques.</Abstract>
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          <Abstract>Cette carte des peuplements benthiques du secteur Quiberon est le résultat du traitement, de l'analyse et de l'agrégation de données de :
- campagnes REBENT 1 et 2 (2003) ;
- campagne IMPACT 8 (2002).

Deux sources croisées d'acquisition des données ont été employées : un système acoustique embarqué (sondeur multifaisceaux) et remorqué (sonar à balayage latéral), permettant de définir des premières classes de signatures acoustiques, correspondant à des unités morpho-sédimentaires, complétées par des campagnes de prélèvements à la benne (échantillons sédimentaires biologiques), des profils vidéo et des plongées.</Abstract>
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          <Abstract>Cette carte des peuplements benthiques de la Mer d’Iroise est reproduite d'après la carte réalisée par Raffin C. en 2003 pour sa thèse "Bases biologiques et écologiques de la conservation du milieu marin en mer d'Iroise".
Cette carte a fait l'objet en 2007 d'une numérisation dans le cadre du réseau de surveillance de la flore et de la faune benthique marine REBENT. La légende d'origine est reportée dans le champ attributaire LEG_ORIG. Une harmonisation avec la typologie EUNIS a été réalisée en 2011. La méthode utilisée inclut une re-détermination individuelle des polygones, avec intervention d'experts scientifiques. Christian Hily (IUEM/LEMAR) a validé cette harmonisation en mai 2011.</Abstract>
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          <Abstract>Cette carte des peuplements benthiques subtidaux du secteur Morlaix est le résultat du traitement, de l'analyse et de l'agrégation des données de campagnes REBENT entre 2008 et 2010.
Deux sources croisées d'acquisition des données ont été employées : un système acoustique embarqué (sondeur multifaisceaux) et remorqué (sonar à balayage latéral), permettant de définir des premières classes de signatures acoustiques, correspondant à des unités morpho-sédimentaires, complétées par des campagnes de prélèvements à la benne (échantillons sédimentaires biologiques) et des profils vidéo.</Abstract>
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          <Abstract>Cette carte des peuplements benthiques subtidaux du secteur Trégor-Goëlo est le résultat du traitement, de l'analyse et de l'agrégation des données des campagnes REBENT 10 et 11 (2006), HALIOTREGOR (2008) et IFR-NEOMYSIS (2011).
Deux sources croisées d'acquisition des données ont été employées : un système acoustique embarqué (sondeur multifaisceaux) et remorqué (sonar à balayage latéral), permettant de définir des premières classes de signatures acoustiques, correspondant à des unités morpho-sédimentaires, complétées par des campagnes de prélèvements à la benne (échantillons sédimentaires biologiques) et des profils vidéo.</Abstract>
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          <Abstract>La carte de nature des fonds du site Natura 2000 en mer des Roches de Penmarc'h a été réalisée dans le cadre du programme Interreg MeshAtlantic et constitue la première étape de l'élaboration de la carte des habitats subtidaux du site. Ce jeu de données provient de l'interprétation et l'interpolation des acquisitions intertidales et subtidales ayant eu lieu sur le site de Penmarc'h entre 2011 et 2012. Ont participé à l'élaboration de ce produit :
- Stevenn Lamarche (coord.), (Ifremer - Applications Géomatiques)
- Jacques Populus (Ifremer - Applications Géomatiques)
- Anthony Doré (MNHN SPN - Station de Biologie Marine de Concarneau)
- Fabrice Pluquet (HOCER)
- Anouar Hamdi (Géomaticien)
- Eliot Besson (Stagiaire)</Abstract>
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          <Abstract>FR7200775 - DOMAINE D'ABBADIA ET CORNICHE BASQUE
Produit issu du programme MESH ATLANTIC. 
Réalisé par l'IMA. 
Habitats : intertidaux. 
EUNIS 2007 
Numérisation des habitats d'après les données existantes et une prospection terrain sur l'estran.</Abstract>
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          <Abstract>FR7200776 - FALAISE DE SAINT-JEAN-DE-LUZ A BIARRITZ.
Produit issu du programme MESH ATLANTIC. 
Réalisé par l'IMA. 
Habitats : intertidaux.
EUNIS 2007
Numérisation des habitats d'après les données existantes et une prospection terrain sur l'estran.</Abstract>
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          <Abstract>FR7200813 - COTE BASQUE ROCHEUSE ET SON EXTENSION AU LARGE.
Produit issu du programme MESH ATLANTIC. 
Réalisé par l'IMA. 
Habitats : intertidal, infralittoral, circalittoral.
EUNIS 2007
Numérisation des habitats d'après les données existantes, données Vecteurs, polygones des habitats.
Synthèse bibliographique, prospection terrain (multibeam)</Abstract>
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Digital data sources : Side scan sonar (2011), bathymetric datas (2009), orthophotos (2007) 
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          <Abstract>The result of a multidisciplinary field survey of the Haig Fras SAC which was initiated in January and completed during March/April 2011. The current study was initiated to investigate the extent of Annex I reef habitat at Haig Fras. Cefas and JNCC collected full-coverage multibeam bathymetric and backscatter data and associated ground-truthing data. This data has been analysed to update the extent of the Annex I reef and produce a broadscale habitat map. Seven biotopes were identified from drop camera transects with the predominant biotope characterised by Devonshire cup corals, sponges and crustose communities on wave-exposed circalittoral rock. The broadscale habitat map indicates the presence of four main biotopes; high energy circalittoral rock, moderate energy circalittoral rock, deep circalittoral coarse sediment and deep circalittoral sand.</Abstract>
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          <Abstract>In May 2008 (18-27 May), a survey commissioned by JNCC undertook seabed habitat investigations of two Areas of Search (AoS) for offshore SACs. The objectives of this survey, within the Submarine structures in the mid-Irish Sea AoS and the Solan Bank AoS, were to acquire high quality acoustic data capable of identifying and delineating habitats listed under Annex I of the 1992 EC Habitats Directive; primarily the Annex I habitat Submarine structures made by leaking gases in the former AoS and Annex I Reef habitat in the latter AoS. Surveys consisted of both broad-scale and fine-scale acoustic techniques, utilising sidescan sonar and multibeam swathe bathymetry, along with a variety of ground-truthing techniques including towed and drop down video/stills and Hamon grab sampling. A Rock dredge was also used at a few stations in order to gather samples of epibiota from hard substrata to assist with the taxonomic identification of the video and still images. The range of sampling techniques employed ensured that any Annex I habitats could be adequately described and  characterised. For both AoSs survey planning and interpretation of survey data utilised extensive pre-existing data sets.</Abstract>
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          <Abstract>Updated broadscale habitat map for East of Celtic Deep recommended Marine Conservation Zone (rMCZ), resulting from an analysis of the dedicated survey data. The broadscale habitat ‘A5.2 Subtidal sand’ was the most widespread habitat, occupying roughly two-thirds of the rMCZ site. The sand is shaped into subaqueous dunes in the east and the northwest of the site, but occurs as flat seabed in the central area. ‘A5.4 Subtidal mixed sediments’ are found in the east, in the troughs between dunes and on flat areas of seabed. ‘A5.3 Subtidal mud’ is limited to water depths &gt;90 m in the west of the site.

Classification system details: EUNIS habitats and a separate FOCI layer. Survey technique details: Multibeam: Kongsberg EM2040; 0.1m2 mini Hamon grab; Camera sledge.</Abstract>
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          <Title>[GB001120] Beachy Head East rMCZ EUNIS habitat map</Title>
          <Abstract>Updated habitat map resulting from an integrated analysis of the 2012 dedicated survey data for Beachy Head East recommended Marine Conservation Zone (rMCZ).</Abstract>
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          <Title>[GB001122] Broadscale habitat (EUNIS level 3) for Farnes East recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>A broadscale habitat feature class was created to illustrate predicted extent of broadscale habitats present at Farnes East rMCZ. These broadscale habitats include 'Moderate energy circalittoral rock', 'Subtidal coarse sediment', 'Subtidal sand', 'Subtidal mud' and 'Subtidal mixed sediments' as determined from particle size analysis of sediment samples and descriptive analysis of still images from underwater camera data. The assigned classes at each ground-truth stationwere used to inform the semi-automated process of map production using object-based image analysis (OBIA)in combination with regression kriging. Groundtruthing data collected during 2012 on the RV Cefas Endeavour (surveyID CEND0412).

Classification system details: EUNIS habitats and a separate FOCI layer. Survey technique details: 0.1m2 mini Hamon grab; Camera sledge; multibeam data colected by EGS under contract in 2012.</Abstract>
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          <Abstract>Updated habitat map resulting from integrated analysis of the CHP acoustic data and the 2012 dedicated ground truth survey data for North East of Farnes Deep (formerly known as Rock Unique) rMCZ.

Classification system details: EUNIS habitats and a separate FOCI layer. Survey technique details: 0.1m2 mini Hamon grab; Camera sledge; Existing multibeam data used. Associated datasets: GB001127</Abstract>
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          <Title>[GB001128] Broadscale habitat (EUNIS level 3) for East of Haig Fras recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>Updated habitat map resulting from an integrated analysis of the 2012 (CEND 3/12a) and 2013 (CEND 5/13) dedicated survey data for East of Haig Fras recommended Marine Conservation Zone (rMCZ). It shows the seabed at the site to be a heterogenous fine scale mosaic of sand, coarse and mixed sediments, with mud habitat in deeper areas. The two broadscale habitats ‘A5.1 Subtidal coarse sediment’ and ‘A5.4 Mixed sediments’ are presented as a complex ‘A5.1/A5.4 Subtidal coarse/mixed sediments’. They show no differentiation in their acoustic or topographical properties that would allow them to be mapped separately. The ‘A4 Circalittoral rock’ habitat is present in scattered small patches.

Created with Object Based Image Analysis (OBIA) on acoustic data and groundtruthed samples. Acoustic data gathered by Gardline under tender, groundtruthing gathered by Cefas on cruises CEND 3/12a and CEND 5/13.</Abstract>
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          <Abstract>Annex I habitat map created from data collected on the CEND 11/08 survey to Solan Bank - subsequently translated to EUNIS. Sublittoral sediments defined using acoustic and groundtruth data.&#13;
&#13;
Survey Techniques: Kongsberg EM3000D multi beam echosounder; Benthos SIS 1624 towed sidescan sonar; 0.1m2 Hamon grab; Rock dredge; Camera sledge; Drop frame video camera.&#13;
&#13;
See JNCC report 430, 2010 for more information.&#13;
&#13;
Orthorectified aerial photography used was flown to a scale of 1:5000. Photography was flown at low tide on a spring tide between the months of April and September to ensure maximum vegetation coverage.  As a result of this and due to adverse weather conditions over some of the key tidal windows the whole project area was not captured in one block, but flown in stages between 2006 and 2009. Although ground-truthing was undertaken to support and validate the habitat map, not all areas were ground-truthed.</Abstract>
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          <Abstract>The aim of the survey was to map the seabed environment around North Rona. The survey will form the baseline for future management of the area to determine the scope and nature of any appropriate assessment. The survey area encompasses the seabed all around North Rona.&#13;
&#13;
In order to record and characterise the habitats around North Rona, Seastar Survey Ltd. undertook an acoustic and a ground-truthing survey (video/still photography survey) in 2009. The aim of the acoustic element of the survey was to identify different backscatter returns and describe as well as delineate the extent of the various seabed habitat types occurring around North Rona.  &#13;
&#13;
A digital sidescan sonar mosaic, in conjunction with single beam echo sounder derived bathymetry, provided the initial broadview to map the substrata present throughout the survey area as well as allowing the identification of any features of interest.  &#13;
&#13;
The aim of the ground-truthing element of the survey was to provide a description of the richness and diversity of the habitats on both rocky reef and the softer sediments. The biotope distribution and species composition was developed through interpretation of drop-down video footage and digital still photography, taken after evaluation of the sidescan mosaic.  &#13;
&#13;
The results of all elements of the survey were used to create a Geographical Information System (GIS) which enabled a high level of processing, interpretation and display of the sidescan sonar mosaic, bathymetry, substrata types, biotopes and the digital photography.</Abstract>
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          <Abstract>Data collected aboard the MV Franklin in July 2009: Acoustics (Multibeam echosounder), Drop camera/towed video (10 sites).&#13;
The original survey plan (Stewart 2009) for the Anton Dohrn Seamount AoS involved a combination of radial transects on the top of Anton Dohrn and a suite of transects parallel to the flanks of the seamount both at the top of the flank and a level near the base the flank tohighlight the lower level of possible rock or hard substrate. &#13;
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Survey work carried out in Caernarfon Bay showed this area was very diverse in terms of both its seabed features and benthic communities. 

The location of a well-documented horse mussel (Modiolus modiolus) reef was clearly identified from multibeam bathymetry and backscatter data, and was sampled using video, SPI and grab samples. 

The area was rich in both infauna and epifauna, with a variety of different biotopes being recorded. Other features of the Caernarfon Bay survey area included an area of cobble and boulder ridges in the southwest with associated tide-swept epifaunal communities, and an area of muddy sediments in shallower waters to the east, with patches of stable cobbles that upported a rich seaweed and epifaunal community.</Abstract>
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The reef has high biodiversity and is vulnerable to anthropogenic activities, such as benthic fishing. The mussel reef forms an undulating surface that is significantly different to the surrounding seabed and therefore acoustic monitoring methods can be used to monitor changes in extent and identity areas of potential damage. Work is carried out on the north Llyn horse mussel reef in Pen Llyn a'r Sarnau jointly by CCW and University of Wales Bangor.
Project is carried out in conjunction with the Across Wales drop-down video project.</Abstract>
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          <Abstract>Updated habitat map resulting from an integrated analysis of the dedicated 2012 survey (CEND8/12a) data for Markham's Triangle rMCZ.

Map created via unsupervised classification and expert interpretation.

A new habitat map for the site was produced by analysing and interpreting the available acoustic data and the groundtruth data collected by the dedicated survey of this site. The process is a combination of two approaches, auto-classification (image analysis) and expert interpretation, as described below. The routine for auto-classification is flexible and dependent on site-specific data, allowing for application of a bespoke routine to maximise the acoustic data available.

ArcGIS was used to perform an initial unsupervised classification on the supplied backscatter image. The single band backscatter mosaic was filtered and smoothed prior to the application of an Iso cluster/maximum likelihood classification routine.
For further information, refer to: Green, S. &amp; Cooper, R. (2013), Markhamâ€™s Triangle rMCZ Post-survey Site Report.</Abstract>
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          <Title>[GB001224] Broadscale habitat (EUNIS level 3) for South East of Falmouth recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>Updated habitat map resulting from an integrated analysis of the dedicated 2012 survey data (CEND3/12b) for South East of Falmouth rMCZ.

A new habitat map for the site was produced by analysing and interpreting the available acoustic data and the groundtruth data collected by the dedicated survey of this site. The process is a combination of two approaches, auto-classification (image analysis) and expert interpretation, as described below. The routine for auto-classification is flexible and dependent on site-specific data, allowing for application of a bespoke routine to maximise the acoustic data available.
ArcGIS was used to perform an initial unsupervised classification on the supplied backscatter image. The single band backscatter mosaic was filtered and smoothed prior to the application of an Iso cluster/maximum likelihood classification routine.
For further information, refer to the South-East Falmouth rMCZ Post-survey Site Report vs. 8 (Green, S. &amp; Cooper, R., 2015).</Abstract>
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          <Abstract>The objective of this project was to generate seabed habitat maps for locations with full coverage acoustic datasets to as detailed a hierarchical level as possible within the Marine Habitat Classification for Britain and Ireland (version 04.05), also known as MNCR classification, (Connor et al. 2004). The acoustic data were at various stages of processing and interpretation, therefore the mapping of habitats and biotopes in some areas have required a greater amount of work to reach the same level compared to other areas.
     The constituent polygons within the habitat/biotope maps are labelled to an appropriate level of the Habitat Classification and translated to the corresponding EUNIS code.
     In order to generate seabed habitat maps for the areas the data associated with each area were required to undergo some preliminary preparation and processing in order to ensure suitability and compatibly with the mapping methodologies employed. 
A top-down approach was adopted based on the methods developed by MESH and UKSeaMap and used by EUSeaMap, which utilised the updated seabed substrate information provided by BGS. 
     Three maps for each MPA proposal have been produced (the level of habitat detail which could be mapped was restricted to level 3 or 4 of the EUNIS classification and level 2 or 3 of the  MNCR classification) with associated metadata and peripheral supplementary data to aid in future analysis and interpretation. A confidence assessment using the MESH confidence assessment method has been undertaken for each habitat map produced and certainty of classification maps accompany each habitat map also.</Abstract>
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          <Title>[GB001316] Broadscale habitat (EUNIS level 3) for North West of Jones Bank recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>A broadscale habitat layer was produced by analysising and interpreting the acoustic and ground truth data collected by Gardline onboard the MV Tridens onboard 29th February and 31st March 2012and RV Cefas Endeavour between 11th and 12th July 2012 . PSA data were used to assign each sample a EUNIS class which then informed theexpert visual interpretation process of map production.

Updated version of earlier broadscale habitat feature class NWJB_20140912_BSH_DRAFT, with all polygons less than 200 sqm in area merged to neigbouring polygon with the longest shared border.

Bathymetry and backscatter data collected by Gardline onboard the MV Tridens onboard 29th February and 31st March 2012 were used in conjunction with ground thruth samples to produce a Broadscale habitat map of North West of Jones Bank.
Ground thruth samples were collected on both Gardline and Cefas survey cruises from 50 stations. Benthic grabs were taken at 44 stations. An underwater camera system was deployed at 17 stations to collect video and still information. Sediment samples were collected with a grab system consisting of a 0.1 m2 mini Hamon grab and Day Grab.  On recovery, the grab was emptied into a large plastic bin and a representative subsample of sediment (approx. 0.5 litres) taken for particle size analysis (PSA).  The remaining sample was photographed, then sieved over a 1 mm mesh to collect the benthic macrofauna. 
Camera deployments lasted a minimum of 10 minutes, with the vessel using its dynamic positioning capability to move along the planned transect at c. 0.5 knots (c. 0.25 ms-1) across a 100 m ‘bullring’ centred on the sampling station.  Still photographic images were captured at one minute intervals and opportunistically if features of interest were observed. Video and photographic still images were processed by Envision Mapping Ltd in accordance with the guidance documents developed by Cefas and the JNCC for the acquisition and processing of video and still data (Coggan and Howell, 2005).
Particle size analysis (PSA) was carried out by Cefas following standard laboratory practice, and results were checked by Cefas specialist staff following the recommendations of the National Marine Biological Analytical Quality Control (NMBAQC) scheme (Mason, 2011). Setup and operation followed the MESH ‘Recommended Operating Guidelines (ROG) for underwater video and photographic imaging techniques’ (Cogganet al., 2007).</Abstract>
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          <Title>[GB001333] Padstow Bay and Surrounds BSH</Title>
          <Abstract>Feature class depicting broadscale habitat features at The Padstow Bay and Surrounds MCZ. The map is a result of an integrated analysis of existing MBES full coverage of bathymetry and partial coverage of backscatter data from the Civil Hydrography Programme (CHP) and dedicated ground-truthing survey data, collected in 2013. Habitat classes observed at each ground-truthing station were used to inform a semi-automated process of map production using object-based image analysis (OBIA). The map shows the seabed at the site to be characterised largely by outcropping bedrock (‘A3.2 Moderate energy infralittoral rock’ and ‘A4.2 Moderate energy circalittoral rock’), with deposits of ‘A5.1 Subtidal coarse sediment’ in valleys and crevasses in the rock and flat areas of ‘A5.2 Subtidal sand ‘, mainly closer to shore.</Abstract>
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          <Title>[GB001336] Broadscale habitat (EUNIS level 3) for South West Deeps (West) recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>Updated habitat map resulting from an integrated analysis of the 2013 dedicated survey data (collected on cruise CEND0613) for South West Deeps (West) recommended Marine Conservation Zone (rMCZ).

A new habitat map for the site was produced by analysing and interpreting the available acoustic data and the ground-truth data collected by the dedicated surveys of South West Deeps West rMCZ.  The process is a combination of two approaches, auto-classification (image analysis) and expert interpretation. The routine for auto-classification is flexible and dependent on site-specific data, allowing for application of a bespoke routine to maximise the acoustic data available. ArcGIS was used to perform an initial unsupervised classification on the supplied backscatter image. The single band backscatter mosaic was filtered and smoothed prior to the application of an Iso cluster/maximum likelihood classification routine. For further information, refer to the South-West Deeps (West) rMCZ Post-survey Site Report.</Abstract>
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          <Title>[GB001494] Hartland Point to Tintagel recommended Marine Conservation Zone (rMCZ) BSH</Title>
          <Abstract>An updated Broadscale habitat (BSH)map was created based on a WGS84 datum. The new BSH map for the site was produced by analysing and interpreting acousticdata(both existing data aquired as part of the Civil Hydrography Programme (CHP)and data newly acquired during a targeted survey), and ground truth data collected by twodedicated surveysof this site(EA survey- SNGN 03/13 and Cefas survey - CEND01/13Y). Four main BSHs were identified, “A4.1Highenergy circalittoral rock”,“A4.2 Moderate energy circalittoral rock”, "A5.1 Subtidal coarse sediment"and “A5.2 Subtidal sand”.The circalittoral rock BSH are mapped as a complex, as it was not possible to delineate the energy regime based on available GIS data layers.</Abstract>
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          <Abstract>This it the updated broadscale habitat (BSH) map for the Whitsand and Looe Bay MCZ. Several BSH were identified as part of this map creation including: Infralittoral rock, moderate energy circalittoral rock, subtidal sand, subtidal mixed sediments, subtidal coarse sediment</Abstract>
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          <Abstract>Feature class depicting broadscale habitat features at the Mid St George’s Channel rMCZ. The map is a result of an integrated analysis of newly acquired and previously available acoustic data together with ground-truthing data collected by a dedicated survey of the sitein 2013. Habitat classes observed at each ground-truthing station were used to inform a semi-automated process of map production using object-based image analysis (OBIA). The map shows the seabed at the site to be characterised largely by ‘A5.1 Subtidal coarse sediment’ and ‘A5.4 Subtidal mixed sediments’, which are mapped together as a complex due to difficulty in separating the two from the underlying acoustic data. Smaller patches of ‘A5.2 Subtidal sand’ and ‘A4.2 Moderate energy circalittoral rock’ are also found within the site.

A new habitat map for the Mid St Georges Channel Marine recommended Marine Conservation Zone (rMCZ) was produced by analysing and interpreting newly acquired and previously available acoustic data together with ground-truthing data collected by a dedicated survey of the site.  

Full coverage multibeam echosounder (MBES) data covering 70% of the Mid St George’s Channel rMCZ was collected in 2012 by Osiris Projects.  An additional block of full coverage MBES data was collected by RV Cefas Endeavour on CEND05/13, adding a further 5% area coverage of the site. The remaining 25% of the rMCZ has partial coverage (31%) MBES data collected under the Mid Irish Sea Project.  More detail on the acoustic data used, and references to the aquisitieon reports can be found in the Mid St Georges Channel Marine rMCZ Post-Survey Site Report (Defra Contract Reference: MB0129; Report Number 29)

Ground-truth sampling for the site was planned using a standard MCZ ground-truthing sampling grid, applied to different habitat types identified from the processed bathymetry and backscatter layers. Station positions were then modified to target features of interest, in particular suspected reef features. The survey was carried out between 1-6th May 2013 on the RV CEFAS Endeavour cruise CEND0513. Ground truth samples were collected from 130 stations. Benthic grab samples were recovered at 115 stations, video transects at 71stations and short (2 minute) deployments of the drop camera were carried out at a further 49 grab stations. Station metadata are presented in Appendix 1 of the Mid St George’s Channel rMCZ Post-Survey Site Report (Defra Contract Reference: MB0129; Report Number 29) and further detail on ground-truth sample collection can be found in the Site Report and the Mid St George’s Channel rMCZ Survey Report.

The new habitat map was produced via a combination of object-based image analysis (OBIA) of the acoustic data, implemented in the software package eCognition® v8.7.2, and expert judgement aided by statistical analysis, linking the ground truth observations to the acoustic and topographic properties. Full methodology for production of the broadscale habitat layer, with appropriate references for methods used, can be found in the Mid St George’s Channel rMCZ Post-Survey Site Report.</Abstract>
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          <Abstract>A broadscale habitat map was produced by analysising and interpreting the acoustic and ground truth data collected at South Rigg rMCZ. Acoustic data was used to identify areas of Rock and sediment and groundtruthing data was used to divide the sediment areas into one of the four sediment classes, namely coarse sediment, sand, mud and mixed sediment. These areas were then divided into littoral and subtidal zones and different energy areas (Low, Moderate or High). These classes could then be classified using EUNIS.</Abstract>
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          <Title>[GB001509] Broadscale habitat (EUNIS level3) for the Offshore Brighton recommended Marine Conservation Zone (rMCZ)</Title>
          <Abstract>Broadscale habitat (EUNIS level 3) for Offshore Brighton recommended Marine Conservation Zone (rMCZ). Seabed texture polygons mapped using expert interpretation of acoustic data (MBES bathymetry and backscatter) and groundtruthing data from PSA analysis and image (stills and video) classification. Using data collected during cruise CEND0812 on the RV Cefas Endeavour (29/04/12 to 14/06/12) and previous surveys.

A new habitat map for the site was produced by analysing and interpreting the available acoustic data and the ground truth data collected by the dedicated survey of the Offshore Brighton rMCZ, in addition to existing modelled bathymetry (Astrium,2011). The process involves geological review and expert judgement to interpret the sediment textures present.

To map substrata type across the rMCZ, we assessemed the sea bed and generated line work based on MBES, backscatter and derivatives (rugosity, slope) in conjunction with ground truth information (PSA, video and stills) in order to assign BSH classsifications.

For further information, refer to the Offshore Brighton rMCZ Post-survey Site Report (Dove and Green, 2015).</Abstract>
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. Using data collected during cruise CEND0812 on the RV Cefas Endeavour (29/04/12 to 14/06/12) and previous surveys.</Abstract>
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          <Abstract>Broadscale habitat (EUNIS level 3) for Greater Haig Fras recommended Marine Conservation Zone (rMCZ).

A broadscale habitat feature class was created to illustrate predicted extent of broadscale habitats present at Greater Haig Fras rMCZ. These broadscale habitats include 'High energy circalittoral rock', 'Moderate energy circalittoral rock', 'Subtidal coarse/mixedsediment', 'Subtidal sand' and 'Subtidal mud' as determined from particle size analysis of sediment samples and descriptive analysis of still images from underwater camera data. The assigned classes at each ground-truth stationwere used to inform the semi-automated process of map production using object-based image analysis (OBIA).</Abstract>
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Updated habitat map resulting from an intergrated analysis of the acoustic and ground-truth survey data from 2013 (onboard the Coastal Survey Vessel (CSV) Water Guardian on cruise wgdn0112). Sediment types at each groundtruthing station were used to inform a semi-automated process of map production using object-based image analysis (OBIA).</Abstract>
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          <Abstract>Updated habitat map resulting from an intergrated analysis of the acoustic and ground truth survey data in 2014 (onboard the RV Cefas Endeavour). Broadscale habitats at each ground truth station were used to inform a semi-automated mapping process using object-based image analysis (OBIA). The majority of the seabed was classified as the BSH 'A4.1 High energy circalittoral rock/A4.2 Moderate energy circalittoral rock', with a with a large sediment bank in the north of the rMCZ made up of the BSHs 'A5.1 Subtidal coarse sediment' and 'A5.2 Subtidal sand'.</Abstract>
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Phase I Biotope mapping was carried out across the rMCZ for broad scale habitats. Phase II infaunal sediment sampling was carried out to provide information on the benthic infaunal assemblages and particle size distribution of the study sites by means of core sampling. Sediment surface scrapes were obtained for heavy metals and organic contaminants analysis. Phase II quantitative survey of intertidal rocky reefs comprised of a quadrat survey with percentage cover of species present within each quadrat being recorded. 
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Aerial imagery and OS mapping was digitised to produce baseline maps of biotope boundaries. The maps were annotated in the field to identify biotopes and boundaries as well as significant features. In addition, intertidal sediment cores were taken at 16 stations (0.01m2 cores 3 replicates at each station) distributed throughout the Cumbria Coast rMCZ at the low, mid and high shore, in order to assess the benthic species present, along with an additional sample for Particle Size Analysis. Samples were sieved over a 0.5mm sieve. Sediment scrape samples were also taken at 4 stations at the midshore for Tributyl tin, heavy metal and organic contaminant analysis. The Phase II quantitative survey of intertidal rocky reefs comprised of 9 quadrat sites per transect with 3 replicate quadrats at each low, mid and upper shore zone or the main biotope present. Percentage cover of species present within each 0.25m2  quadrat was recorded. The methods used for data collection and processing followed protocols and standards for biotope mapping and sampling.  MEDIN Data Guideline for sediment sampling by grab or core for benthos.</Abstract>
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          <Abstract>A Natural England commissoined verification survey of intertidal sediments within the Beachy Head West rMCZ. 
Phase I Biotope mapping was carried out across the rMCZ for broad scale habitats where intertidal coarse sediment occurred. Phase II Infaunal sampling was carried out to provide information on the benthic infaunal assemblages and particle size distribution of the study sites by means of core sampling. Sediment surface scrapes were obtained for heavy metals and organic contaminants analysis. 
The data was used to produce a EUNIS Level 3 boradscale habitat map of the Beachy Head West rMCZ.
Aerial imagery and OS mapping was digitised to produce baseline maps of biotope boundaries. The maps were annotated in the field to identify biotopes and boundaries as well as significant features. In addition, intertidal sediment cores were taken at 6 stations (0.01m2 cores 3 replicates at each station) distributed throughout the Beachy Head West rMCZ, in order to assess the benthic species present, along with an additional sample for Particle Size Analysis. Samples were sieved over a 0.5mm sieve. Sediment scrape samples were also taken at 3 stations for Tributyl tin, heavy metal and organic contaminant analysis. The methods used for data collection and processing followed protocols and standards for biotope mapping and sampling.  MEDIN Data Guideline for sediment sampling by grab or core for benthos.</Abstract>
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          <Abstract>A Natural England commissoined verification survey of intertidal sediments within the Thanet Coast rMCZ.
Phase I Biotope mapping was carried out across the rMCZ for broad scale habitats.
The data was used to produce a EUNIS Level 3 boradscale habitat map of the Thanet Coast rMCZ.</Abstract>
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          <Title>[GB003006] 2013 Natural England Verification Survey of Intertidal Sediments within the Stour &amp; Orwell Estuaries rMCZ</Title>
          <Abstract>Aerial imagery and OS mapping was digitised to produce baseline maps of biotope boundaries. The maps were annotated in the field to identify biotopes and boundaries as well as significant features. In addition, intertidal sediment cores were taken at 16 stations (0.01m2 cores 3 replicates at each station) distributed throughout the Cumbria Coast rMCZ at the low, mid and high shore, in order to assess the benthic species present, along with an additional sample for Particle Size Analysis. Samples were sieved over a 0.5mm sieve. Sediment scrape samples were also taken at 4 stations at the midshore for Tributyl tin, heavy metal and organic contaminant analysis. The Phase II quantitative survey of intertidal rocky reefs comprised of 9 quadrat sites per transect with 3 replicate quadrats at each low, mid and upper shore zone or the main biotope present. Percentage cover of species present within each 0.25m2  quadrat was recorded. The methods used for data collection and processing followed protocols and standards for biotope mapping and sampling.  MEDIN Data Guideline for sediment sampling by grab or core for benthos.</Abstract>
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          <Abstract>EUNIS-translated Indicative biotopes for the Gwynt y Mor study area determined from the analysis of grab samples from the site between 2002-2004. 

Data originally in Classification system of UK and Ireland, translated to EUNIS at JNCC, 2013.

Original non-eunis data retreived from the Crown Estate http://www.marinedataexchange.co.uk/ItemDetails.aspx?id=10609</Abstract>
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          <Title>[GB003010] Distribution of intertidal Zostera beds around Northern Ireland 2012</Title>
          <Abstract>Surveys undertaken in Lough Foyle (Aug 2009), Carlingford Lough (Aug-Sep 2012), Strangford Lough (Aug-Sep 2012) and Dundrum Bay (Jul 2012). These surveys are done primarily as part of a rolling 6 year programme for the EU Water Framework Directive.

These polygons were mapped and merged to collate inter-tidal seagrass surveys originally assessed as part of the Water Framework Directives suite of Biological Quality Element tools. The data collected can also be used to inform the habitat map as it corresponds to the Eunis code 'A2.611-Mainland Atlantic Zostera noltii or Zostera angustifolia meadows'.

Surveys undertaken by Quercus at Queen's University, Belfast on behalf of the Department of the Environment, Northern Ireland (DOE).

Subsequently translated into EUNIS habitat classification scheme.</Abstract>
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          <Title>[GB003012] East Rockall habitats</Title>
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Data collected in 2009 aboard the MV Franklin in July 2009: Acoustics (Multibeam echosounder), Sidescan Sonar, Drop camera/towed video (17 sites).
For the East Rockall Bank AoS the original survey plan consisted primarily of a series of traverses along the top and base of the eastern flank of Rockall Bank and several traverses at right angles across the top of the bank and down into the Rockall Trough. However to maximise the coverage along the rocky escarpment that runs along the length of the AoS, this initial plan was replaced with a long double swath width of multibeam echosounder data acquired along the escarpment; the upper break in slope, roughly coincident with the 500m bathymetric contour, as imaged previously by the SEA 7 2005 multibeam echosounder datasets. 
From previous studies (including FRS drop camera surveys), this area was selected as being the most likely place to host Annex I reef habitats, in particular as potential sites for Lophelia pertusa. A number of survey lines at right angles to the break in slope were added to the along-escarpment line to better characterise features of interest observed on the 2005 multibeam echosounder dataset downslope of the escarpment.
Additionally several survey lines were located on the top of the bank, across an area of suspected iceberg ploughmarks.</Abstract>
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          <Title>[GB100053] Acoustic mapping of the seabed of the Menai Strait. North East Menai.</Title>
          <Abstract>The section of the Menai Straits that were surveyed were divided into three parts.

The hardness/roughness isopleths were combined using CAMRIS GIS to produce a composite map showing 7 types of group (very hard/very rough; hard/rough; moderately hard/moderately rough; moderately soft/moderately smooth; soft/moderately rough; soft/smooth; very soft/very smooth).
A map for the whole of the survey area was followed by a map showing the biotope types as observed using the remote video, which are as follows (SA = superabundant; A = abundant; C = common; O = occasional)

Sand/shell: Medium fine sand with shell: very silty.
Coarse sand/silt: Coarse sand: very silty.
Gravel: Barren
Silty cobble: Silt accretion (A); Cerianthus (O-C); Urticina (O-C).
Silty cobble/rich: Silt accretion (A); sponges (Haliclona, Halichondria) (C); hydroids (C); Urticina (O-C).
Boulder/cobble sponge: Similar to above, but with sponges C-A.
Cobble/bounder faunal turf: Hydroids (C); Tubularia (O); Alcyonium(O); Flustra(O).
Cobble hydroid turf: Short turf of hydroids (C-A).
Cobble Pomatoceros: Pomatoceros and barnacles (A).
Bedrock/boulder silt sponge: Similar to boulder/cobble sponge above, but on bedrock/boulder.
Boulder Laminaria: Small Laminaria hyperboraea (C); red algal turf (C).
Bedrock sponge/Flustra: Bedrock with encrusting sponges (C-A) and Flustra (O-C).
Bedrock Mytilus. Small Mytilus (A-SA); Asteria(C-SA); encrusting corralines (O).
Bedrock and faunal turf: Hydroids (C); Tubularia(O); Alcyonium(O); encrusting and branching sponges(O-C).


The maps were subsequently transposed into EUNIS in 2006 using expert judgement.</Abstract>
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          <Title>[GB100078] Moray Firth benthic biotope map of Guillam area</Title>
          <Abstract>Envision Mapping Ltd was contracted to undertake a survey of the Moray Firth cSAC within the 30m contour. The purpose was to map the main sediment features and biota using  acoustic remote sensing techniques combined with grab and video sampling. A RoxAnn? acoustic ground discrimination system was used in conjunction with a GeoSwath? interferometric swath bathymetric system. The survey was comprehensive (100% cover with the swath system or a minimum track spacing of 80m) over priority areas but incomplete over areas outside these priority areas. The biotopes were classified using the most recent Marine Habitat Classification (Connor et al. 2004) using a combination of multivariate analysis and video analysis and matching the characterising species to the classification system.</Abstract>
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          <Title>[GB100083] Mapping the distribution of benthic biotopes in Loch Torridon: substrate close to shore</Title>
          <Abstract>This brief report presents the analysis completed to date. Little biological data exists for the majority of the deeper water of the Loch and for this reason the initial classification has been confined to habitat type.</Abstract>
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          <Abstract>The survey of the marine environment around the Isle of Wight has been undertaken as part of the BioMar Project which is funded by the EC through the LIFE Programme. The survey from Bembridge to the Needles took place in June/July 1994. The baseline resource survey was to determine the major habitats present with their distribution.</Abstract>
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          <Title>[GB100088] Acoustic mapping of the seabed of the Menai Strait. South West Menai.</Title>
          <Abstract>The section of the Menai Straits that were surveyed were divided into three parts.

The hardness/roughness isopleths were combined using CAMRIS GIS to produce a composite map showing 7 types of group (very hard/very rough; hard/rough; moderately hard/moderately rough; moderately soft/moderately smooth; soft/moderately rough; soft/smooth; very soft/very smooth).
A map for the whole of the survey area was followed by a map showing the biotope types as observed using the remote video, which are as follows (SA = superabundant; A = abundant; C = common; O = occasional)

Sand/shell: Medium fine sand with shell: very silty.
Coarse sand/silt: Coarse sand: very silty.
Gravel: Barren
Silty cobble: Silt accretion (A); Cerianthus (O-C); Urticina (O-C).
Silty cobble/rich: Silt accretion (A); sponges (Haliclona, Halichondria) (C); hydroids (C); Urticina (O-C).
Boulder/cobble sponge: Similar to above, but with sponges C-A.
Cobble/bounder faunal turf: Hydroids (C); Tubularia (O); Alcyonium(O); Flustra(O).
Cobble hydroid turf: Short turf of hydroids (C-A).
Cobble Pomatoceros: Pomatoceros and barnacles (A).
Bedrock/boulder silt sponge: Similar to boulder/cobble sponge above, but on bedrock/boulder.
Boulder Laminaria: Small Laminaria hyperboraea (C); red algal turf (C).
Bedrock sponge/Flustra: Bedrock with encrusting sponges (C-A) and Flustra (O-C).
Bedrock Mytilus. Small Mytilus (A-SA); Asteria(C-SA); encrusting corralines (O).
Bedrock and faunal turf: Hydroids (C); Tubularia(O); Alcyonium(O); encrusting and branching sponges(O-C).


The maps were subsequently transposed into EUNIS in 2006 using expert judgement.</Abstract>
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The purpose of the study was to establish a physical and biological baseline dataset to facilitate an assessment of favourable condition status of littoral sediment habitats of the SSSI site, as well as identifying species and biotopes that are representative and/or notable within the Tamar, Tavy &amp; St John's Lake.
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The aim of the survey was to provide a baseline dataset for future management and condition monitoring of the intertidal interest features in the Dee Estuary. Phase I Biotope Mapping including sediment cores for fauna and Particle Size Analysis.</Abstract>
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The survey aimed to standardise fauna, and the information for mud/sand habitats and communities of the Dee Esturay SAC, in order to act as a baseline for future management and condition monitoring. Phase I survey of the intertidal zone, mud/sand and rock habitats resulting in the production of detailed biotope maps.</Abstract>
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A MESH Confidence Score of 86 was assigned to the dataset based on the information given in the reports supporting the GIS.</Abstract>
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          <Title>[GB200015] Video Survey of Proposed Greater Dowsing Windfarm Site</Title>
          <Abstract>Video survey to record seabed type for Greater Dowsing wind farm development area (Offshore Power).</Abstract>
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          <Title>[GB200016] Triton Knoll Offshore Wind Farm Video Study</Title>
          <Abstract>Ecological survey to provide site specific information for three potential, alternative development areas within the Greater Wash (Offshore Power).</Abstract>
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          <Title>[GB200054] 2014 Seabed habitat data layer (EUNIS) for Pobie Bank Reef SCI</Title>
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JNCC undertook a survey with Marine Scotland Science to Pobie Bank Reef cSAC  with the aim of gathering high quality evidence to better ascertain the distribution of bedrock and stony reef for the development of management advice. Multibeam bathymetry and backscatter data and sidescan sonar data were collected, as were benthic infaunal and PSA samples and underwater stills and video imagery. Data were gathered from the FRV Scotia from 23rd August to 6th September 2013.
Data (acoustic and underwater camera tow video and stills) from two SEA surveys undertaken at Pobie Bank Reef cSAC in 2003 and 2006 were made available and utilised in the analysis. Also available is a biological data interpretation report based on these data. The report was prepared by Envision in 2009, and contains the most recent habitat map for Pobie Bank Reef cSAC.</Abstract>
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Multibeam bathymetry data processed with the Caraibes software (v3.9) and a 30m grid created.
The data was acquired in 1995 when multibeam systems were first emerging onto the commercial market. The number of beams per ping was limited and thus the data density low in comparison to more modern data. Data editting was only done on data that was significantly in error. The multibeam backscatter data was also processed in the Caraibes software package and produced 2 mosaics at 50m resolution. The backscatter data did not have higher resolution data. 
Correlation with ground truth data, consisting of sediment samples and photographic imagery samples, predominantly toward the top of slope and seamount summit and flanks,allowed basic interpretation of the bathymetry and backscatter data near the sample locations. 
To aid interpetation, the sediment samples had been divided into FOLK categories and habitat type determinations, as well as faunal communities in some instances, had beeen made for the photographic imagery samples.
Characterisation was spread over the whole area and divided into polygon regions by finding interpretive boundaries on either backscatter imagery (such as texture changes or contrast changes) or on the bathymetric layers of slope, rugosity and relief.</Abstract>
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          <Title>[GB300026] Habitat Mapping for Conservation and Management of the Southern Irish Sea (HABMAP) Extension project - Combined L3 L4 output, primary biotope.</Title>
          <Abstract>The HABMAP project was set up in response to the need for better spatial awareness of habitat distributions in the Southern Irish Sea. This work  produced habitat maps of the seabed using novel predictive modelling techniques. This dataset is related to the predictive modelling only. The HABMAP Extension Project has built on the methods developed during the original project, and has repeated the modelling work using higher resolution / improved input datasets to help increase the accuracy of the predictive map outputs. The modelling work has also been extended to cover all of Welsh waters (previously cut-off at the Interreg funding boundary), notably including the Dee and Severn estuaries.  The purpose of this data capture was to provide seabed habitat maps that could be used for conservation and management. Project outputs might be used in strategic planning, decision making for offshore developments, Marine Protected Area selection, sensitivity mapping and mapping essential fish habitats. However, because of the way the  has been produced, and the fact that some data has been modelled and derived, the maps are not appropriate to act as the sole evidence for any specific planning or regulatory decision or assessment without further supporting studies or evidence.
The project boundaries were as follows: Southern Irish Sea- land-based boundaries include the whole Welsh coast to the English border on the east side of the Dee Estuary in the north, and the whole Severn Estuary and Bristol Channel coastline in the south, extending as far as Morte Point (east of Ifracombe) in England. The southern project boundary then extends offshore (skirting the northern tip of Lundy) across to a point approx 60km west of Waterford on the Irish coast, including the whole SE Ireland coastline and offshore banks as well as parts of the Celtic Sea. The boundary then extends northwards along the Irish coast to a point approximately 40 km north of Dublin.
The outputs of the project included a Combined Level3/Level4 habitat map, presented here after translation to the EUNIS habitat classification system from the Marine Habitat Classification System for Britain and Ireland. Each polygon of the original output contained up to 46 different biotopes, either predicted by the model or recorded as present, and presented in order of likelihood. Only the primary biotope has been taken from the original dataset to produce this EUNIS output, polygons originally containing more than one habitat are flagged in the "VAL_COMM" field. Information on whether the biotope was recorded as present or was a predictive output of the model, and a confidence value present in the original dataset have also been recorded in the "VAL_COMM" field</Abstract>
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          <Abstract>The distribution of the bioconstruction along the Apulian coasts are not well known and, in some areas, totally unknown. This is particularly evident for the Coralligenous assemblages. Furthermore, a regional scale georeferenced cartography is not yet available and the knowledge of the cliffs is really poor. The aim of the Biomap project, started in 2013, is to fill this gap by providing an effective cartography tool for the evaluation of the already instituted Sites of Conservation Interest (SCIs). High resolution acoustic data (MBES multibeam echosounder), seismic profiles (Chirp sonar and sub-bottom profiler) and ROV images were acquired for the habitat mapping within 3 MPAs and 21 SCIs up to 100m depth. Furthermore, data acquired outside the above mentioned protected areas were used in specific deeper zones (up to 700m depth).</Abstract>
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          <Abstract>GIS NATURA is a geographic information system incorporating, under one system, the Italian fauna, flora and fungi checklists, the fauna and flora distribution databases, the existing data on marine biocoenoses, the distribution models of Italian vertebrates (REN), the distribution of priority habitats according to the Habitats Directive, the vegetation series (Corine Land Cover level 4), the phytoclimatic, ecopedological and landscape maps, the administrative cartography, the boundaries of parks and protected areas (including Special Protection Areas and Sites of Community Importance). Project ended in 2005 and the most important product for the marine environment is a multiscale patchwork of different (already available) cartographic datasets for both Posidonia oceanicaand other benthic biocoenoses.</Abstract>
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          <Abstract>The elaboration of this map started in 1999 within a project funded by the Italian Environmental Ministry aimed to identify the distribution of the Posidonia meadows along the Sardinia coasts. During the first phase of the project, different field activities were carried out by using Side Scan Sonar, ROV and scuba diver. In this phase also biological samples were collected. Furthermore, remote sensing surveys were conducted using hyperspectral scanner and aerial photo. Collected data were elaborated for the creation of the Posidonia meadows distribution. Maps show the upper limits and a number of different Posidonia meadows with distinction of different facies (i.e. Posidonia on rock, Posidona on sand, Posidonia on matte etc).</Abstract>
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Aldino S. Campos, Neil C. Mitchell, Condor seamount (Azores, NE Atlantic): A
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          <Abstract>Mapping of the Natura 2000 site FR5300017 "Abers - Côte des légendes"  was jointly performed in the framework of three different actions: (i) the Natura 2000 convention for Brittany, and (iii) CARTHAM Project.
It is based on the interpretation of various types of data from a number of surveys carried out between 2005-2012 both in the intertidal and subtidal zones. Additionally the seabed « Carte G » from the French hydrographic survey (SHOM) was used in the interpretation process.
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A confidence score in the [0-100] scale has been assigned to each polygon (SUM_CONF field)
The compilation comprises the following various data sources.
Lamarche S., Bajjouk T., 2013. Cartographie des habitats benthiques intertidaux du site Natura 2000 FR 5300017 - Abers - Côtes des légendes - Parties estuariennes. Réf. RST - DYNECO/AG/13-05/TB.
Rollet C., Bonnot-Courtois Ch., Hamon N. et Loarer R., 2010. Carte des habitats benthiques intertidaux du secteur des Abers - Zone intertidale (multisource Rebent,) - Echelle : 1/10 000
ErHold et al., (2012, unpublished). Cartographie de natures des fonds subtidaux du secteur des Abers - Côtes des légendes.
TBM, 2012. Inventaire cartographique des habitats marins du site Natura 2000 Abers Côtes des Légendes FR5300017. Rapport CRTHAM, 104 p.</Abstract>
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The North of Celtic Deep rMCZ is located between Welsh territorial waters and Republic of Ireland offshore waters, 12 nm from the Welsh coast. It is the most southerly MCZ in the Irish Sea Conservation Zone. A number of Broad Scale Habitat (BSH) features and Features of Conservation Interest (FOCI) have been proposed by the regional project for designation within the rMCZ, and a number of additional FOCI had been noted as being recorded within the rMCZ, but there was insufficient confidence in the records to warrant including them as features proposed for designation.&#13;
Report Available: X:\OffshoreSurvey\SurveyData\2012_02_RVCefasEndeavour_MCZVerification_CEND_3_12_a\north_celtic_deep_v1\cruise_documentation\NCLD_cend0312\cruise_report</Abstract>
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&#13;
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          <Abstract>Littoral sediments are found across the intertidal zone and range from boulders, through gravel and sand, to silt and clay (mud). The type of sediment is critical to structuring biological community composition. Sand shores usually support a range of oligochaetes, polychaetes and crustaceans, and muddy shores also favour bivalves. The invertebrate communities present in littoral sediments can support large populations of predatory birds. Littoral sediment environments are extremely dynamic and can change markedly over time. &#13;
&#13;
The aim of this project was to undertake a field survey of the intertidal sediments of the SSSIs located at Brading Marshes to St. Helen's Ledges, King's Quay Shore, and the Yar Estuary, Isle of Wight in order to enable a condition assessment of the littoral sediment feature. The survey determined: the extent of the sediment feature; the biological communities present, the sediment character, and the distribution of the biotopes, at each site. &#13;
&#13;
The methods followed the standard guidelines for monitoring intertidal environments (Davies et al., 2001). Background information on the study sites was collated in July-August 2008 and the field survey was conducted 17 August-20 September 2008. Maps and aerial photographs were used to compare the extent of littoral sediment in the field, and the distribution of biotopes was mapped using a walkover Phase 1 survey, including photographs. Each site was then sub-sampled representatively (15-25 cells per site) using relatively rapid techniques to record sediment type and macrofauna. More detailed sampling of sediment character and biotope composition was undertaken at five transects per site, each with a mid and lower shore sampling station, where photographs were taken and sediment cores were collected for particle size analysis and identification of infauna in the laboratory. All field data were spatially referenced and integrated within a GIS. Data analysis consisted of summary statistics and multivariate statistical techniques using PRIMER (Clarke and Warwick 2001). There were few methodological constraints, although access to the western shore at the Yar Estuary was restricted. &#13;
&#13;
The total extent of littoral habitat mapped at Brading Marshes to St. Helen's Ledges was 130ha. The most extensive biotope type was Polychaetes on littoral fine sand (LS.LSa.FiSa.Po), which covered 40% of the site and formed large flats outside Bembridge harbour. Inside the harbour, Polychate/bivalve dominated mid estuarine mud shores (LS.LMu.MEst) dominated. This pattern reflected a marked contrast between the more exposed littoral sediments outside the harbour, where fine/medium sand and gravel were typical, and the poorly sorted silt with clay inside the harbour. Sediment infauna was generally not abundant and showed variable species richness and density, with a high community dissimilarity between samples. Polychaetes such as Lanice conchilega, Hediste diversicolor and Nephtys spp. were most characteristic but the snail Hydrobia ulvae dominated the community within the harbour. A patch of eelgrass (Zostera) was mapped in the intertidal zone. King's Quay Shore comprised almost 50ha of littoral sediment. A variety of sandy biotope types characterised the site, with Barren or amphipod dominated mobile sand shores (LS.LSaMoSa) and Polychates on littoral fine sand (LS.LSa.FiSa.Po) each covering a third of its area. Sediments were dominated by brown, very fine/medium sand of variable thickness, overlying a basal sub-unit of stiff brown/grey clay, often with a veneer of mixed gravel at or near the surface. The sediment supported moderate faunal diversity and numbers, and there was considerable community dissimilarity between samples. The polychaete Heteroclymene robusta was most abundant, supported by polychaetes Lanice conchilega and Arenicola marina, and the periwinkle Littorina littorea. Oysters (Ostrea edulis) and eelgrass (Zostera) were both recorded at the site during the survey. &#13;
&#13;
A total of approximately 42ha of littoral sediment was mapped at the Yar Estuary, with 86% of this comprising the Polychaete/bivalve dominated mid estuarine mud shores (LS.LMu.MEst) biotope type. Throughout the estuary, sediments were dominated by very poorly and poorly sorted grey/dark grey/black silt and clay (mud), which were often highly anoxic at shallow depths. Sediment samples showed that there were few faunal species present but they were in some abundance. The snail Hydrobia ulvae was by far the most numerous, contributing substantially to community similarity across the site, although the vast majority of shells were empty. The bivalve Abra tenuis and the polychaete Arenicola marina were locally quite abundant. There was some evidence of saltmarsh erosion at the site, possibly resulting in increased littoral sediment habitat. Multivariate comparisons of all three sites highlight the dissimilarity between the Yar sediment, which has quite a uniformly small grain size, and the mixed or larger grain sizes that characterise the other two sites. The faunal composition showed high dissimilarity between all sites and a clear distinction between communities from silt substrates and those where sand predominates, suggesting that community composition is influenced both by sediment type and site characteristics. &#13;
&#13;
Brading Marshes to St. Helen's Ledges and King's Quay Shore both contain a good range of biotopes and could be considered to represent diverse sedimentary landscapes. In general, the sediment tended to be rather species-poor, especially at the Yar Estuary, and faunal abundance was limited, except at the Yar where snails were numerous. It is possible, however, that the sampling intensity was insufficient to adequately represent the faunal population. It appears that the condition of the littoral sediment feature is favourable at Brading Marshes to St. Helen's Ledges and King's Quay Shore SSSIs, although at both sites invertebrate numbers seem to be quite low and there is a limited amount of comparable information so monitoring is advisable. At the Yar Estuary, a comparison with previous information indicates that the quality of the sediment infauna may have declined and the extent of littoral sediment increased over the past 30 years, although natural dynamics make establishing a baseline difficult. Thus, the condition of the littoral sediment feature at the Yar Estuary SSSI appears favourable for sediment attributes but may be declining for biotope composition.</Abstract>
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          <Title>[GB100314] Biological Survey of the Intertidal Sediments of the South Shore of the Solway Firth</Title>
          <Abstract>One of the key responsibilities of the statutory nature conservation agencies in the UK is the identification and protection of a series of sites intended to conserve important wildlife and earth science features. Such sites may be designated under national legislation (e.g. Sites of Special Scientific Interest (SSSIs)), or European legislation such as Special Areas of Conservation (SACs) under the Habitats Directive, and Special Protection Areas (SPAs) under the Birds Directive. Regular monitoring of sites is undertaken in order to assess the effectiveness of legislative and policy measures in contributing to biodiversity conservation. The intertidal mudflats and sandflats are a designated interest feature of the Solway Firth estuary, and as such, the survey reported here has aimed to provide data to support the overall monitoring programme of the site. Ultimately, the data will form a part of the ongoing condition assessment for the site.</Abstract>
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          <Title>[GB100364] Berwickshire &amp; North Northumberland Coast Intertidal Mud and Sand Flats Assessment</Title>
          <Abstract>Marine Ecological Surveys Limited (MESL) was commissioned by Natural England to conduct an intertidal monitoring survey of the Berwickshire and North Northumberland (BNNC) Special Area of Conservation (SAC) specifically looking at the intertidal mud and sand flats. The survey was undertaken by MESL between the 29th August and the 7th September, 2015 and involved Phase I mapping and Phase II sampling of the intertidal mud and sand flats found throughout the site. The study focuses on a number of embayments found within the site, which include Embleton Bay, Beadnell Bay, Budle Bay, Fenham Flats, Holy Island Sands, Ross Back Sands, Cheswick Sands and Goswick Sands.</Abstract>
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          <Title>[GB100353] Fal and Helford SAC Subtidal Seagrass Condition Assessment</Title>
          <Abstract>A combination of drop-down/towed video (DD/TV) and diver surveys were carried out on the subtidal seagrass beds within the Fal and Helford Special Area of Conservation (SAC) between June and September 2015. The DD/TV surveys were carried out by Ecospan Environmental Ltd, and the diver surveys by Natural England. The results and conclusions drawn from both survey methods are reported here together. The principal aim of the surveys was to obtain standardised biological information for the seagrass beds within the SAC, and to compare these data with previous studies for the purpose of condition monitoring of the seagrass sub-feature where possible. These surveys were intended to provide an ecological baseline for assessment of specific attributes to inform the condition from which to assess future change where previous data does not exist.</Abstract>
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          <Title>[GB100259] Portsmouth Harbour SPA/SSSI Intertidal Mudflat Condition Assessment 2014</Title>
          <Abstract>At the instruction of Natural England, Marine Ecological Surveys Limited (MESL) conducted the survey of intertidal sediments within the Portsmouth Harbour Special Protected Area (SPA)/Site of Special Scientific Interest (SSSI). MESL undertook the Portsmouth Harbour SPA/SSSI assessment in a single survey conducted between the 20th - 22nd of September 2013. The survey was specifically designed to gather information on the littoral sediment features of Portsmouth Harbour SPA/SSSI, and thus a dataset to inform future condition monitoring of the site.</Abstract>
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          <Title>[GB100317] Morecambe Bay SAC Subtidal Cobble and Boulder Skear Communities Drop-down Video Survey</Title>
          <Abstract>Morecambe Bay is an ecologically diverse area, encompassing the coastal plain estuaries of the rivers Wyre, Lune, Keer, Kent and Leven which form an extensive area of shallow coastal sediments (Sotheran and Walton, 1997). The Morecambe Bay Special Area of Conservation (SAC) was designated under the Natura 2000 programme in 2005 due to the substantial amounts of Annex I habitat present within the Bay which include; ‘estuaries,’ ‘mudflats and sandflats not covered by water at low tide,’ ‘large shallow inlets and bays,’ ‘sandbanks which are slightly covered by sea water all the time’ and ‘reefs.’ In order to inform site condition monitoring, Seastar Survey Ltd. were contracted by Natural England to undertake a drop-down camera survey in the Morecambe Bay SAC in order to define the distribution and extent of any subtidal cobble and boulder skear communities present.</Abstract>
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          <Title>[GB100274] Littoral mud and sandflat condition monitoring and rMCZ verification survey of the Alde, Ore and Butley Estuaries</Title>
          <Abstract>Natural England has commissioned surveys in order to monitor and assess the extent and condition of the mudflats and sandflats not covered by seawater at low tide feature of the Alde, Ore and Butley Estuaries SAC. Natural England in partnership with Environment Agency, Cefas, and Defra have additionally requested that the surveys add to the current information available for the Alde Ore Estuary rMCZ. More specifically, the data collection is proposed to add to knowledge on the presence and extent of the Habitats of Conservation Importance (HOCI) within the rMCZ boundary where more evidence is required.</Abstract>
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          <Title>[GB100373] Dee Estuary Biotopes and Physical Attributes Assessment</Title>
          <Abstract>The Dee Estuary is located on the north-west British coastline between the Wirral Peninsula in England and north-east Wales. It covers an area of 14,000 ha and is one of the largest estuaries in the UK. Coastal processes are dominated by strong tidal streams and large sediment fluxes affecting the intertidal. The primary task of this study was to undertake dedicated survey work in order to derive high quality data on existing biotopes and supporting physical attributes. Additional evidence from surface contaminants samples and anthropogenic pressure information was collected to assist with assessment of change against historical evidence for each sub-feature. A parallel high level evaluation was also conducted on the presence of key benthic prey items for designated bird species.</Abstract>
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Survey Techniques: Kongsberg EM3000D multi beam echosounder; Benthos SIS 1624 towed sidescan sonar; 0.1m2 Hamon grab; Rock dredge; Camera sledge; Drop frame video camera.&#13;
&#13;
See JNCC report 430, 2010 for more information.&#13;
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The original survey plan (Stewart 2009) for the Anton Dohrn Seamount AoS involved a combination of radial transects on the top of Anton Dohrn and a suite of transects parallel to the flanks of the seamount both at the top of the flank and a level near the base the flank tohighlight the lower level of possible rock or hard substrate. &#13;
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Phase I and Phase II surveys of the littoral habitats were undertaken by Ecospan Environmental Ltd during the spring tides on the 5th of December 2013 and the 3rd of March 2014. These surveys were commissioned by Natural England and were designed to provide additional data on the extent and presence of certain features within the MCZ.</Abstract>
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The results will be compared to previous work and interpretation of the resulting information (together with other relevant published work) will inform Natural England on the current status of the rocky shores sub-feature of the site.&#13;
&#13;
This is an updated version of the metadata created by The Marine Biological Association of the United Kingdom in 2015 (https://gis.ices.dk/geonetwork/srv/eng/catalog.search#/metadata/6cdbfde2-b8f2-42a7-98f1-0bd4a076f414). This newer version is INSPIRE compliant as part of the standardisation process for uploading the data to EMODnet Seabed Habitats.</Abstract>
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          <Abstract>Field surveys using combined Common Standards Monitoring (CSM) and National Vegetation Classification (NVC) methodology were conducted in the saltmarsh habitat of The Wash Special Area of Conservation (SAC) during July 2013. The area was surveyed between The River Nene and Gibraltar Point (Skegness). This project is part of the IPENS programme (LIFE11NAT/UK/000384IPENS) which is financially supported by LIFE, a financial instrument of the European Community. LIFE+, is a new strategic approach to managing England's Natura 2000 sites. One of the main aims of this survey was to survey and map the saltmarsh plant communities of The Wash section of The Wash and North Norfolk Coast SAC. This required repeat surveys of all 14 transects surveyed by Posford Haskoning (2003) and additional transect locations, where considered appropriate. The survey was undertaken in a three week period from 10th July to 30th July 2013.</Abstract>
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Region: the county Rogaland&#13;
Number of field observations: 633&#13;
Field sampling year: 1992, 1993, 2012&#13;
Prevalence: 43 and 22 for 50% and 85% calcium carbonate content respectively&#13;
Presence / absences: 275/358 and 142/491 for 50% and 85% calcium carbonate content respectively&#13;
Method: BRT run with the R-package Dismo. The grid is made up by a combination of three BRT models; two simplified models including 12 and 13 predictors for carbonate sand with 50% calcium content) and one BRT model based on 10 predictor variables for carbonate sand with 85% calcium content; all run with tree complexity equal to 5. The grid constitutes the maximum predicted probability values among these three models, which all are “smoothed” by applying a neighborhood analysis (i.e. mean of 3x3 neighbor cells) in advance of combining the models).&#13;
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Prevalence: 12%&#13;
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Region: The counties Aust-Agder and Telemark&#13;
Number of field observations: 1848&#13;
Field sampling years: 1992 and 2008&#13;
Prevalence: 13.6%&#13;
Presence / absences: 252/1596&#13;
Method: BRT run in R with the R-package Dismo. (The model predicts carbonate sand on peaks and in sheltered areas where it is unlikely to find carbonate sand. Such areas have been identified through rules set up in collaboration with geologists at Geological Survey of Norway (NGU; curvature index values &gt;|1|, and the wave exposure index less than 10 000, cf Rinde et al. 2006) and removed from the shape layers for predicted presence of carbonate sand created from the grid layer.&#13;
Number of predictor variables: 10&#13;
Information about the predictor variables: curvature at coarse, medium and detailed resolution with a 1025, 525 and 125 m moving calculating window respectively, based on a 25 m resolution DEM; DEM, slope at two resolutions (12.5 and 25 m); wave exposure, longitude, and an optimal radiation index, all with 25 m resolution; and aspect based on a 12.5 resolution DEM. &#13;
AUC internal: 0.96.</Abstract>
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Model run in UTM zone 33N &#13;
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Data collected 2011-2013 by NGU, NIVA included absences from kelp surveys&#13;
The data were collected in Nordland county, but the models covers also a small part of Troms in the North and Trøndelag in the south. &#13;
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      <Layer queryable="1">
        <Title>MSFD habitat maps</Title>
        <Abstract>Habitat maps collated by EMODnet Seabed Habitats in the MSFD Benthic Broad Habitat Types  classification system.&#13;
&#13;
Ownership of the individual maps is retained by the original owners, for more information please see the individual metadata record tied to the map, which can be seen in the query response.&#13;
&#13;
This service is configured for viewing individual maps. For download access to relevant maps, please use the emodnet_open_maplibrary WFS service endpoint https://ows.emodnet-seabedhabitats.eu/emodnet_open_maplibrary/wfs? &#13;
&#13;
Maps have been standardised to the EMODnet Seabed Habitats Translated Habitat Data Exchange format, for more information see: https://www.emodnet-seabedhabitats.eu/contribute-data/data-exchange-format/</Abstract>
        <KeywordList>
          <Keyword>features</Keyword>
          <Keyword>benthic</Keyword>
          <Keyword>habitat</Keyword>
          <Keyword>biotype</Keyword>
          <Keyword>marine</Keyword>
          <Keyword>ocean</Keyword>
          <Keyword>msfd</Keyword>
        </KeywordList>
        <CRS>EPSG:3857</CRS>
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        <MetadataURL type="ISO19115:2003">
          <Format>text/html</Format>
          <OnlineResource xlink:type="simple" xlink:href="https://gis.ices.dk/geonetwork/emodnet-seabedhabitats/eng/catalog.search#/metadata/061c9d9c-8dc4-449f-8ac6-758840253fc3"/>
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        </MetadataURL>
        <Style>
          <Name>default-style-msfd_group</Name>
          <Title>msfd_group style</Title>
          <Abstract>Default style for msfd_group layer</Abstract>
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            <Format>image/png</Format>
            <OnlineResource xmlns:xlink="http://www.w3.org/1999/xlink" xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?service=WMS&amp;version=1.3.0&amp;request=GetLegendGraphic&amp;format=image%2Fpng&amp;width=20&amp;height=20&amp;layer=msfd_group"/>
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        </Style>
        <Layer queryable="1" opaque="0">
          <Name>de005001</Name>
          <Title>[DE005001] Habitats and Biotopes in the German Baltic Sea</Title>
          <Abstract>The dataset provides full-coverage maps of the habitats and biotopes in the German Baltic Sea at a resolution of 1 x 1 km for the entire region and at 50 x 50 m resolution in specific areas. We combined geological and biological surveys to map the seabed and collected extensive data to classify different habitats and their associated benthic communities. Using newly established national guidelines and predictive habitat modelling, we produced highly accurate maps. For upload to EMODnet four separate maps were made:&#13;
- Broad Habitat Types according to the Marine Strategy Framework Directive (MSFD).&#13;
- Annex I Habitat types&#13;
- Habitat types classified according to the Baltic Sea-wide HELCOM underwater biotope and habitat classification (HUB)&#13;
-  other habitat types, OHTs for German marine waters include biotope types according to S30 of the German Federal Nature Conservation Act (BNatSchG), according to the European Habitats Directive (92/43/EEC), as well as the Baltic Sea-wide HELCOM Red List types</Abstract>
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            <Keyword>benthic</Keyword>
            <Keyword>eunis</Keyword>
            <Keyword>habitat</Keyword>
            <Keyword>biotope</Keyword>
            <Keyword>marine</Keyword>
            <Keyword vocabulary="emodnet_sbh_admin_repcat">Habitats - seabed habitats (including coastal wetlands) - collection of classified maps</Keyword>
            <Keyword vocabulary="emodnet_sbh_admin_int_ext">External</Keyword>
            <Keyword>DE005001</Keyword>
            <Keyword vocabulary="emodnet_sbh_admin_sizekb">1992</Keyword>
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          <Style>
            <Name>annexi</Name>
            <Title>annexi</Title>
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              <Format>image/png</Format>
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          <Style>
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            <Title>msfd_maplibrary</Title>
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              <Format>image/png</Format>
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            <Title>helcomhub_maplibrary</Title>
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              <Format>image/png</Format>
              <OnlineResource xmlns:xlink="http://www.w3.org/1999/xlink" xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?service=WMS&amp;version=1.3.0&amp;request=GetLegendGraphic&amp;format=image%2Fpng&amp;width=20&amp;height=20&amp;layer=de005001&amp;style=helcomhub_maplibrary"/>
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      <Layer queryable="1">
        <Title>Other habitat maps</Title>
        <Abstract>Habitat maps collated by EMODnet Seabed Habitats in classification systems other than EUNIS and Habitats Directive Annex I.&#13;
&#13;
Ownership of the individual maps is retained by the original owners, for more information please see the individual metadata record tied to the map, which can be seen in the query response.&#13;
&#13;
This service is configured for viewing individual maps. For download access to relevant maps, please use the emodnet_open_maplibrary WFS service endpoint https://ows.emodnet-seabedhabitats.eu/emodnet_open_maplibrary/wfs? &#13;
&#13;
Maps have been standardised to the EMODnet Seabed Habitats Original Habitat Data Exchange format, for more information see: https://www.emodnet-seabedhabitats.eu/contribute-data/data-exchange-format/</Abstract>
        <KeywordList>
          <Keyword>features</Keyword>
          <Keyword>benthic</Keyword>
          <Keyword>eunis</Keyword>
          <Keyword>habitat</Keyword>
          <Keyword>biotope</Keyword>
          <Keyword>marine</Keyword>
          <Keyword>ocean</Keyword>
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        <Style>
          <Name>default-style-other_group</Name>
          <Title>other_group style</Title>
          <Abstract>Default style for other_group layer</Abstract>
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            <Format>image/png</Format>
            <OnlineResource xmlns:xlink="http://www.w3.org/1999/xlink" xlink:type="simple" xlink:href="https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/ows?service=WMS&amp;version=1.3.0&amp;request=GetLegendGraphic&amp;format=image%2Fpng&amp;width=20&amp;height=20&amp;layer=other_group"/>
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        <Layer queryable="1" opaque="0">
          <Name>be000007</Name>
          <Title>[BE000007] Project Habitat BELSPO/AWZ-WWK MN0290; subzone WK; habitat map</Title>
          <Abstract>Area West Coast, potential future marine nature reserve close to the coast; together with other datasets (identical lui), full-coverage habitat maps were obtained; data has been verified; expert data collection</Abstract>
          <KeywordList>
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            <Keyword>benthic</Keyword>
            <Keyword>habitat</Keyword>
            <Keyword>biotope</Keyword>
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            <Keyword>BE000007</Keyword>
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            <Keyword vocabulary="emodnet_sbh_admin_int_ext">External</Keyword>
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          <CRS>EPSG:3857</CRS>
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          <Style>
            <Name>polygon</Name>
            <Title>A boring default style</Title>
            <Abstract>A sample style that just prints out a transparent red interior with a red outline</Abstract>
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              <Format>image/png</Format>
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        <Layer queryable="1" opaque="0">
          <Name>be000017</Name>
          <Title>[BE000017] Project Habitat BELSPO/AWZ-WWK MN0290; subzone WK; habitat map</Title>
          <Abstract>Area West Coast, potential future marine nature reserve close to the coast; together with other datasets (identical lui), full-coverage habitat maps were obtained; data has been verified; expert data collection</Abstract>
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            <Keyword>BE000017</Keyword>
            <Keyword vocabulary="emodnet_sbh_admin_repcat">Habitats - seabed habitats (including coastal wetlands) - collection of classified maps</Keyword>
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            <Title>A boring default style</Title>
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              <Format>image/png</Format>
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          <Name>be000031</Name>
          <Title>[BE000031] Project Habitat BELSPO/AWZ-WWK MN0290; subzone WK; habitat map</Title>
          <Abstract>Area West Coast, potential future marine nature reserve close to the coast; together with other datasets (identical lui), full-coverage habitat maps were obtained; data has been verified; expert data collection</Abstract>
          <KeywordList>
            <Keyword>features</Keyword>
            <Keyword>benthic</Keyword>
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            <Keyword>BE000031</Keyword>
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            <Title>A boring default style</Title>
            <Abstract>A sample style that just prints out a transparent red interior with a red outline</Abstract>
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              <Format>image/png</Format>
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        <Layer queryable="1" opaque="0">
          <Name>be000048</Name>
          <Title>[BE000048] Project Habitat AWZ-WWK; area BB; habitat map</Title>
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          <KeywordList>
            <Keyword>features</Keyword>
            <Keyword>benthic</Keyword>
            <Keyword>habitat</Keyword>
            <Keyword>biotope</Keyword>
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            <Keyword>BE000048</Keyword>
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          <Style>
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            <Title>A boring default style</Title>
            <Abstract>A sample style that just prints out a transparent red interior with a red outline</Abstract>
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          <Abstract>This dataset contains the habitats map from the SCI (Site of Community Importance) “Espacio marino de Illes Columbretes”. The Columbretes Islands, a series of small islands, islets and submerged elevations of volcanic origin, are found in the Western Mediterranean at the northern limit of the Gulf of Valencia, 28 miles from the Gulf of Oropesa and just over 50 kilometers from the coast to the east of Castellón de la Plana. There are 24 islets gathered in 4 groups each named after its largest landmass. This volcanic field covers an area of 90 by 40 kilometers at a depth of 80 to 90 metres. The Illa Grossa and the other islands and islets are formed from basaltic materials or phonolitic rocks. These islands and the associated submerged volcanic field are one of the rare examples of Quaternary volcanism in the Mediterranean. This study was supported by the INDEMARES-LIFE+ Project, EC contract INDEMARES-LIFE+ (07/NAT/E/000732): Inventory and Designation of the Natura 2000 network in marine areas of the Spanish State (www.indemares.es/en). This work was coordinated by the Biodiversity Foundation (www.fundacion-biodiversidad.es). This study was made possible through the collaboration of multiple teams of researchers: Department of Ecology (University of Barcelona - UB), Center for Advanced Studies of Blanes (CEAB - CSIC), Institute of Marine Sciences (ICM - CSIC), Balearic Oceanography Centre (COB) - IEO (Spanish Institute of Oceanography) and Consolidate Research Group Marine Geosciences (GRC-GM) (University of Barcelona - UB). Habitats are classified according to EUNIS nomenclature and the List of Marine Habitats in Spain (LPRE, that it’s classified hierarchically and was completed and published in March 2013). Habitats classification are been simplified owing to the requirements of the EMODnet (European Marine Observation and Data Network) portal for Seabed Habitats.</Abstract>
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          <Title>[FR003014] Seabed Habitat (EUNIS and EUNIS submission) - Lot 06 'Pertuis Charentais et Estuaire de la Gironde' (Cartham) - FR003014</Title>
          <Abstract>Seabed habitat map (current EUNIS classification system and submission) performed by CREOCEAN, LIENSs, EPOC, GEOTRANSFERT, RE NATURE ENVIRONNEMENT &amp; IODDE within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
This map concerns polygons for which at least one habitat IS NOT in the current EUNIS classification (2007-2011). 
Digital data sources: orthos (2000), prefectural decrees
Ground truth data sources (2011-2012): direct human observations
Map confidence rated by Ifremer : 89%</Abstract>
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          <Abstract>Seabed habitat map ('Typologie des biocenoses de Mediterranee' classification system) performed by Asconit Consultants (mandatary), UPVD, LECOB, OCEANIDE &amp; ADENA within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
Digital data sources : historical maps (1986).
Ground truth data sources :Van Veen grab (2010-2011).
Map confidence rated by Ifremer : 64%</Abstract>
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          <Abstract>Seabed habitat map ('Typologie des biocenoses de Mediterranee' classification system) performed by GIS Posidonie within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
Digital data sources :  Side scan sonar (2010), bathymetrics (2008).
Ground truth data sources : Sediment dredge (1 point, 2010)
Map confidence rated by Ifremer : 72% (Habitat : 'vase'; Areas with doubtful outlines).</Abstract>
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            <Keyword vocabulary="emodnet_sbh_admin_sizekb">214</Keyword>
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          <Abstract>Seabed habitat map (Typologie des biocenoses de Mediterranee classification system) performed by Andromede Oceanologie &amp; Stareso within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
Digital data sources: sonar (2010), bathymetry (2007), orthos (2009), historical data (2001, 1997)
Ground truth data sources: direct human observations (06/2011) 
Map confidence rated by Ifremer : 87%</Abstract>
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          <Abstract>Seabed habitat map (Habitat Directive classification system) performed by Stareso within the framework of CARTHAM ("cartographie des habitats marins") project coordinated by the French Biodiversity Agency (Agence française pour la biodiversité, AFB).
Digital data sources: historical data (Guennoc et al., 2001)
Ground truth data sources: none
Map confidence rated by Ifremer : 45%</Abstract>
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                                                                                             &#13;
*Chris Roelfsema, Stuart Phinn, Stacy Jupiter, James Comley, and Simon Albert. 2013. Mapping coral reefs at reef to reef-system scales, 10s-1000s km2, using object-based image analysis. Int. J. Remote Sens. 34, 18 (20 September 2013), 6367-6388. https://doi.org/10.1080/01431161.2013.800660.</Abstract>
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                                                                                             &#13;
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&#13;
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&#13;
Government of the Virgin Islands Department of Planning and Natural Resources (VIDPNR) &#13;
&#13;
Commonwealth of Puerto Rico, Department of Natural and Environmental Resources &#13;
&#13;
Caribbean Fisheries Management Council &#13;
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National Park Service &#13;
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NOAA, National Geophysical Data Center &#13;
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NOAA, Coastal Services Center &#13;
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NOAA, National Geodetic Survey &#13;
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St. Croix Environmental Association &#13;
&#13;
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&#13;
More detailed maps using a reduced minimum mapping unit from one acre to 1,000 square meters (~1/4 acre), &#13;
&#13;
Increased coverage of areas formerly classified as unknown, &#13;
&#13;
More detailed habitat classification, and &#13;
&#13;
Maps of marine areas adjacent to two natural reserves (Bosque Estatal de Guanica and Reserva Natural Finca Belvedere) in coordination with the NOAA Fisheries Caribbean Field Office. &#13;
&#13;
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&#13;
Kendall, M.S., C.R. Kruer, K.R. Buja, J.D. Christensen, M. Finkbeiner, R.A. Warner and M.E. Monaco. 2001. Methods used to map the benthic habitats of Puerto Rico and the U.S. Virgin Islands. NOAA Technical Memorandum NOS NCCOS CCMA 152. Silver Spring, MD. 45 pp</Abstract>
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&#13;
Kendall, M.S., C.R. Kruer, K.R. Buja, J.D. Christensen, M. Finkbeiner, R.A. Warner and M.E. Monaco. 2001. Methods Used to Map the Benthic Habitats of Puerto Rico and the U.S. Virgin Islands. NOAA Technical Memorandum NOS NCCOS CCMA 152. Silver Spring, MD.</Abstract>
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*Chris Roelfsema, Stuart Phinn, Stacy Jupiter, James Comley, and Simon Albert. 2013. Mapping coral reefs at reef to reef-system scales, 10s-1000s km2, using object-based image analysis. Int. J. Remote Sens. 34, 18 (20 September 2013), 6367-6388. https://doi.org/10.1080/01431161.2013.800660.</Abstract>
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          <Abstract>"This dataset provides a map of benthic habitats in the nearshore waters of St. Croix in the U.S. Virgin Islands. The Biogeography Branch of NOAA/NOS/NCCOS acquired aerial photographs of the nearshore waters of Puerto Rico and the U.S. Virgin Islands in 1999. These images, along with field sampling for validation, were used to create geographic information system (GIS) maps of the study area's coral reefs, seagrass beds, mangrove forests, and other important marine habitats. Mapped areas encompass the insular shelf between the shoreline and shelf edge, except where turbidity prevented visualization of the bottom. NOAA's partners included: Government of the Virgin Islands Department of Planning and Natural Resources (VIDPNR) Commonwealth of Puerto Rico, Department of Natural and Environmental Resources Caribbean Fisheries Management Council National Park Service NOAA, National Geophysical Data Center NOAA, Coastal Services Center NOAA, National Geodetic Survey St. Croix Environmental Association NOAA mapped 21 distinct benthic habitat types within eight zones and added these data to a GIS using visual interpretation of orthorectified aerial photographs. NOAA mapped benthic features that covered an area of 490 m2?in the U.S. Virgin Islands, including 300 km2?of coral reef and hard bottom, 161 km2?of submerged vegetation, 24 km2?of unconsolidated sediment, and 2 km2?of mangroves. Since 2002, these maps have been used for a wide range of applications, including: coral reef monitoring, marine protected area design, fisheries assessments, and student projects."</Abstract>
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          <Abstract>This dataset provides a map of benthic habitats in the nearshore waters of St. Thomas and St. John in the U.S. Virgin Islands. The Biogeography Branch of NOAA/NOS/NCCOS acquired aerial photographs of the nearshore waters of Puerto Rico and the U.S. Virgin Islands in 1999. These images, along with field sampling for validation, were used to create geographic information system (GIS) maps of the study area's coral reefs, seagrass beds, mangrove forests, and other important marine habitats. Mapped areas encompass the insular shelf between the shoreline and shelf edge, except where turbidity prevented visualization of the bottom. NOAA's partners included: Government of the Virgin Islands Department of Planning and Natural Resources (VIDPNR) Commonwealth of Puerto Rico, Department of Natural and Environmental Resources Caribbean Fisheries Management Council National Park Service NOAA, National Geophysical Data Center NOAA, Coastal Services Center NOAA, National Geodetic Survey St. Croix Environmental Association NOAA mapped 21 distinct benthic habitat types within eight zones and added these data to a GIS using visual interpretation of orthorectified aerial photographs. NOAA mapped benthic features that covered an area of 490 m2?in the U.S. Virgin Islands, including 300 km2?of coral reef and hard bottom, 161 km2?of submerged vegetation, 24 km2?of unconsolidated sediment, and 2 km2?of mangroves. Since 2002, these maps have been used for a wide range of applications, including: coral reef monitoring, marine protected area design, fisheries assessments, and student projects.</Abstract>
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          <Abstract>Benthic habitats of the moderate-depth marine environment in and around the Virgin Islands Coral Reef National Monument of St. John were mapped using a combination of semi-automated classification and visual interpretation of acoustic imagery. This work replaces previous NOAA maps by Kendall et al. (2001) (1) for the waters around St. John. The objective of this effort, conducted by NOAA's Center for Coastal Monitoring and Assessment - Biogeography Branch in partnership with the U.S. National Park Service (NPS), was to provide spatially-explicit information on the habitat types, biological cover and live coral cover of the moderate-depth area south of St. John. This product provides a fine-scale assessment of the status, abundance, and distribution of moderate-depth marine habitats south of St. John. The NOAA effort provides the U.S. National Park Service with increased technical capacity for ocean exploration, management, and stewardship. Direct implications to management measures include evaluation of management efficacy, a spatial framework for improved monitoring sampling design, improved assessment of human-use impacts, and marine spatial planning to support alternative marine protected area boundary alternatives. Rhodoliths (encrusting marine red algae that resemble coral) and sand were the most common found habitats in the moderate depth region south of St. John. Turf, fleshy, coralline, or filamentous algae were pervasive in both the shallow and moderate depth areas, accounting for 74 percent and 92.8 percent of these mapped areas, respectively. Only four percent of the moderate depth area had live hard and soft coral covers greater than 10 percent. The moderate-depth map begins at the optical limit of the associated shallow-water benthic habitat map (GUI:VI004004), also poduced by NOAA for the region, and continues to the edge of the acoustic imagery. The integration of these two maps is possible, given that the same general habitat classification schemes and minimum mapping units were applied to both the shallow-water and moderate-depth maps. That being said, NOAA emphasizes that the differences between the two maps must be thoroughly understood, in order to recognize the limitations associated with using the maps in an integrated fashion. Integration of the shallow-water and moderate-depth maps will provide a seamless benthic habitat map, extending from the shoreline of St. John southward to the 55 m isobath. Both maps are found at https://coastalscience.noaa.gov/project/benthic-habitat-mapping-st-john-u-s-virgin-islands-national-park-reef-national-monument/.(1) Kendall, M.S., C.R. Kruer, K.R. Buja, J.D. Christensen, M. Finkbeiner, R.A. Warner and M.E. Monaco. 2001. Methods Used to Map the Benthic Habitats of Puerto Rico and the U.S. Virgin Islands. NOAA Technical Memorandum NOS NCCOS CCMA 152. Silver Spring, MD</Abstract>
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          <Abstract>This map shows the benthic marine habitats surrounding countries in the Southeastern Caribbean. This map is originally part of the wider Allen Coral Atlas Global Benthic Habitat Maps dataset found at www.allencoralatlas.org. The Allen Coral Atlas dataset maps the benthic habitat for the world's shallow coral reefs at 5 m pixel resolution. The Allen Coral Atlas brings together partners from Planet, University of Queensland, Arizona State University's Center for Global Discovery and Conservation Science (GDCS), the National Geographic Society and Vulcan Inc. to take high resolution satellite imagery and advanced analytics to map and monitor the world's coral reefs in unprecedented detail. Global Benthic Habitat Maps characterise different coral reef bottom types. These bottom types include communities of living organisms attached to the reef (benthos), as well as sediments and underlying substrate. The six Allen Coral Atlas Global Benthic Habitat Map classes used were developed by Roelfsema et al 2013* with input from other coral reef benthic classifications. This classification maximizes the breadth of information available from Planet Dove remote sensing data to create the best set of classes to support users. *Chris Roelfsema, Stuart Phinn, Stacy Jupiter, James Comley, and Simon Albert. 2013. Mapping coral reefs at reef to reef-system scales, 10s-1000s km2, using object-based image analysis. Int. J. Remote Sens. 34, 18 (20 September 2013), 6367-6388. https://doi.org/10.1080/01431161.2013.800660.</Abstract>
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          <Abstract>The close location of the site complex Mandra_Poda to the industrial zone of Burgas is the main influencing factor. The former Mandernsko lake is turned into a dam lake with a registered flow. The MandraPoda Complex includes Mandra Lake with its adjacent wetlands.Mandra Lake is located at the Black Sea coast and is the southernmost of the Burgas lakes. Its north-eastern part touches on the town of Burgas. This former semi-saline lake has been turned into a freshwater reservoir. A lagoon, covering the areas of Poda and Uzungeren, has been preserved between the reservoir wall and the Black Sea.The following natural coastal and marine habitat types of significance for conservation, according to the Biodiversity Act and to the Habitats Directive have been established: 1140 Mudflats and sandflats not covered by seawater at low tide ;1150 Coastal lagoons; 1160 Large shallow inlets and bays; 1310 Salicornia and other annuals colonizing mud and sand; 1410 Mediterranean salt meadows (Juncetalia maritimi)</Abstract>
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          <Abstract>The Shabla complex includes the Shabla Lake and the Shabla Lagoon. The Shabla Lake is a firth brackish lake near the sea coast. The semi-saline Shabla Lagoon is located1.5 km to the southeast of the lake and is separated from the sea by high dunes.The territory of the Ramsar site is 404 ha, of which 150 ha of open water.The lake falls into the boundaries of the Natura 2000 protected sites “Shablenski ezeren komplex” (code BG0000156, according to theBirds Directive) and protected site “Ezero Shabla - Crapetz” (code BG0000621, according to theHabitats Directives).This location provides suitable habitats to 223 species fromthe Biodiversity Act, which are in need of special protectionmeasures.The following habitats according to Annex I to Directive 92/43EEC have been established: Marine - 1110 Sand Banks, which are slightly covered by sea water all the time; : 1150 Coastal lagoons; ; 2110 Embryonic shifting dunes; 2120 Pannonic dunes along the shoreline with Ammophila arenaria (white dunes)</Abstract>
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          <Abstract>Atanasovsko Lake is a hypersaline lake which resembles a liman to the north and a lagoon to the south. A considerable part of its surface is used for salt production with preserved primitive salt production methods. It is located north of the city of Burgas, near the sea coast. The lake lies at 1 m below sea level. Small freshwater marshes, together with a system of canals overgrown with marsh vegetation, surround the lake. The fresh water from the catchment area of the lake is collected in a canal during November-April and flows into the sea. The eastern part of this canal also supplies the salt-works w ith seawater from Burgas Bay during May-October. Thus the water in the canal is fresh during the first half of the year and saline during the second half.The northern part of the lake has been a maintained reserve since 1999. The lake was declared a wetland of international significance under the Ramsar Convention in 1984, and the Ramsar site was enlarged in 2003. In 2007, this area was included in the Natura 2000 network under the name of Protected site Atanasovsko ezero in accordance with the Birds Directive and the Habitats Directive with a code BG000270 and a territory of 7 208,89 ha.The site is representative as the rarest ecosystem type for Bulgaria (coastal halophytic communities). The priority habitat 1150 * Coastal lagoons covers 20.6 % (1 483,2 ha) of the entire protected area (7 200 ha). This is the largest compact area occupied by this habitat in Bulgaria, highly valuable for its relative area, its representativeness and its importance for nature conservation.The following marine habitats according to Annex I to Directive 92/43EEC have been established: 1150 - Coastal lagoons,1160 - Large shallow inlets and bays, 1310 - Salicornia and other annuals colonizing mud and sand, 1410 - Mediterranean salt meadows (Juncetalia maritimi), 1530 - Pannonic salt steppes and salt marshes, 2110 - Embryonic shifting dunes</Abstract>
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          <Abstract>Burgas Lake is situated on the Black Sea coast, west of the city of Burgas, between the lakes Atanasovsko and Mandra. Vaya is the largest Bulgarian Black Sea coastal lake, an open liman. Burgas Lake is a shallow brackish coastal lake an open firth with a weak connection to the sea. Burgas lake falls into the boundaries of proposal for Natura 2000 Protected site under the Birds Directive and the Habitats Directive. The lake is a Ramsar site with territory of 27.6 km2.Habitat Types listed in Annex I to Habitats Directive and in the Biodiversity Act such as 1310 Salicornia and other annuals colonizing mud and sand, 1410 Mediterranean salt meadows (Juncetalia maritimi) are well represented in the lake and 1510 Mediterranean salt steppes (Limonietalia). Habitat 1310 is proposed to be delisted from the area.</Abstract>
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          <Abstract>A small bay on the Black Sea, near the estuary of the Marinka River. The bottom of the bay upstream of the estuary is covered by salty deposits forming vast 5–10 cm deep shallows (Bulgaria’s only seasidesilt field). The shore represents a sand strip with stony sections in some parts.A Protected site according to the Birds and Habitats Directives(“Zaliv Chengene Skele”Chengene Skele BayBG0000242), with a territory of190.1 ha.The bay is one of the most representative localities of theprotected algae species of Zostera marina. The followinghabitats according to Annex I to Directive 92/43EEC have beenestablished: 1110 Sand Banks, which are slightly covered bysea water all the time; 1140 Mudflats and sand-flats not coveredby seawater at low tide and 1410 Mediterranean salt meadows(Juncetalia maritimi).</Abstract>
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&#13;
Citation: Piechaud, N.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modeled density map of Syringammina fragillissima at a fine scale from the Rockall Bank in North East Atlantic between 1981-2010. https://marineinfo.org/doc/dataset/8141</Abstract>
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Citation: Graves K.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modelled distribution map of Acanella arbuscula assemblage in the North East Atlantic in 2021. https://marineinfo.org/doc/dataset/8227</Abstract>
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&#13;
Citation: Graves K.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modelled distribution map of discrete Lophelia pertusa colonies in the North East Atlantic in 2021. https://marineinfo.org/doc/dataset/8243</Abstract>
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        <Abstract>Modelled density of the seapen Kophobelemnon stelliferum in the North East Atlantic. The Random Forest density model trained on data collected by an ROV was constrained by an ensemble of Maxent and Random Forest presence-absence model trained on a larger dataset also collected by an ROV. This species provides structural complexity in an environment where it is lacking and, thus, promotes higher biodiversity where they settle. They are vulnerable to mechanical disturbance of the sediment by fishing gear and a better understanding of their distribution will lead to better management of their population. This work was performed at the University of Plymouth in 2021.&#13;
&#13;
Citation: Rix J.; Graves K.; Piechaud N.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modeled distribution map of Kophobelemnon stelliferum assemblage in the North East Atlantic in 2021. https://marineinfo.org/doc/dataset/8251</Abstract>
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&#13;
Citation: Bridges, A.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modeled distribution map of Lophelia Reef and Pheronema aggregations in the North East Atlantic in 2022. https://marineinfo.org/doc/dataset/8213</Abstract>
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&#13;
Citation: Graves K.; Howell, K.; University of Plymouth (UoP), United Kingdom; (2023): Modeled distribution map of mixed cold-water coral community in the Northeast Atlantic in 2021. https://marineinfo.org/doc/dataset/8254</Abstract>
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&#13;
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