The System of Environmental Economic Accounting - Ecosystem Accounting (SEEA-EA) is a spatially-based, integrated statistical framework for organizing biophysical information about ecosystems, measuring ecosystem services, tracking changes in ecosystem extent and condition, valuing ecosystem services and assets and linking this information to measures of economic and human activity. It is an integrated statistical framework adopted by the United Nations Statistical Commission.
The SEEA-EA outlines five sets of ecosystem accounts:
As part of a recent amendment to Regulation (EU) No 691/2011 on environmental economic accounts, it will be mandatory to report ecosystem extent, condition and services (physical flow) accounts in line with SEEA-EA, although for Marine Ecosystems only the extent at level 1 of the EU Ecosystem Typology is mandatory. The monetary flow of ecosystem services and the monetary value of ecosystem assets will not need to be accounted for under the new regulation. Mandatory reporting by member states will commence in 2026.
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The ecosystem extent accounts reported in this release were produced using a compiled ecosystem extent map for the reference year 2024. This map was created using a wide range of EU and national level geospatial data (Table 4.1).
| Source dataset name | Dataset type | Reference year | Update frequency |
|---|---|---|---|
| EMODnet seagrass | vector; area | 2025 | irregular |
| EMODnet macroalgae | vector; area | 2025 | irregular |
| EMODnet biogenic substrate | vector; area | 2025 | irregular |
| INFOMAR | vector; area | 2025 | irregular |
| Licensed aquaculture sites | vector; area | 2021 | irregular |
| EPA_TransitionalWaterbodies_Cycle3 | vector; area | 2021 | 6 years |
| EUSeaMap 2023 Broad-Scale Predictive Habitat Map for Europe | vector; area | 2023 | biennial |
| Harris et al. (2014) - Slope geomorphic feature layer | vector; area | 2014 | static |
| Harris et al. (2014) - Canyon geomorphic feature layer | vector; area | 2014 | static |
| Harris et al. (2014) - Escarpment geomorphic feature layer | vector; area | 2014 | static |
| Harris et al. (2014) - Fan geomorphic feature layer | vector; area | 2014 | static |
| Harris et al. (2014) - Plateau geomorphic feature layer | vector; area | 2014 | static |
| Harris et al. (2014) - Seamount geomorphic feature layer | vector; area | 2014 | static |
| Irish Shelf Seabed Geomorphological Map v2023 - Fluid Flow | vector; area | 2023 | irregular |
| OSPAR Habitats in the North-East Atlantic Ocean - 2025 Polygon Records | vector; area | 2025 | annual review |
| NPWS Site Specific Conservation Objectives - Marine Community Types | vector; area | 2025 | irregular |
| Macroalgal canopy cover in Europe (2025) | vector; area | 2025 | irregular |
| Seagrass cover (Essential Ocean Variable) in European waters (2025) | vector; area | 2025 | irregular |
| Live hard coral cover (Essential Ocean Variable) in European waters (2025) | vector; area | 2025 | irregular |
| EPA Water Framework Directive Coastal Water Bodies - Cycle 3 | vector; area | 2021 | 6 years |
| EPA Dumping at Sea Sites - DumpBoundaries | vector; area | 2026 snapshot; filtered to 2024 | annual |
| Licensed Aquaculture Sites | vector; area | 2022 | irregular |
| IE GSI MI Shipwrecks Irish Waters WGS84 LAT | vector; point | 2007 dataset; metadata revised 2026 | as needed |
| EMODnet Human Activities - Wind Farms | vector; area | 2026 | annual |
| EMODnet Human Activities - Oil and Gas Offshore Installations | vector; point | 2024 | annual |
| EMODnet Digital Bathymetry (DTM 2024) | raster; area | 2024 | 2 years |
A number of pre-processing steps were necessary in order to compile and merge the wide range of different source data used to produce the final ecosystem extent map. Firstly, EUSeaMap – the base map onto which all other data were layered – was clipped to the EAA and reprojected to the European LAEA projection/ EPSG:3035. Then, all other source data were formatted and re-projected to EPSG:3035 to ensure compatibility with EUSeaMap.
Merging of different data sources involves successive ‘layering’ of each dataset on top of the next to produce a map that uses the most accurate and up-to-date data. This can also be thought of as ‘gap-filling’, whereby the first map is added to a blank canvas after which the next is used to update and/or fill gaps in the previous. The priority assigned to each dataset depends on three main attributes of the source data, including the year for which the data refers (i.e. data age), the degree of correspondence between the source data and the ecosystem type definition, and accuracy (i.e. expected level of error in the source data).
The EU Ecosystem Typology (EUET) was developed by Eurostat as a common classification to harmonize the reporting on ecosystem accounts in the EU. It uses three levels of increasing ecological detail to classify European ecosystems, see Table 4.2 and 4.3.
At level 1, the EU ecosystem typology is an updated MAES ecosystem typology, and is defined in Annex IX of Regulation (EU) 691/2011 on the European environmental-economic accounts and has been adopted as mandatory reporting on ecosystem extent to Eurostat.
At level 2, the main ecosystem types are further differentiated into sub-types in a manner that is relevant to ecosystem service and condition modelling and reporting. The breakdown at level 2 can be submitted to Eurostat as part of the reporting under the Regulation, on a voluntary basis.
Level 3 presents an additional, more detailed layer to support ecosystem service and condition modelling and national uses.
The marine ecosystem types are mapped according to an agreed step-wise classification workflow:
Some areas within the marine EEA could not be classified any further, so are mapped as 12. Marine Ecosystems. Similarly, some areas could be mapped only to level 2 of the typology, and are mapped as e.g. Sublittoral Sediments n.f.d. - not further defined.
The result of classifying all ecosystem types based on the different source data was a compiled raster map. To maintain coherence with the terrestrial and transitional map, it was aggregated to a resolution of 100 × 100m (1 hectare).
| Ecosystem | Descriptor |
|---|---|
| Marine Macrophyte Communities (12.1) | Communities dominated by macroscopic forms of marine vegetation (e.g. seagrasses or macroalgae) located below the low-tide mark, forming communities resembling underwater forests or grasslands (as opposed to macrophytes forming carbonate structures, see 12.2.4) regardless of the type of substrate they colonise. For accounting purposes (ecosystem extent accounts), a threshold of >25% of macrophyte cover (per grid cell) is proposed as a minimum for including the area in this class. |
| Biogenic Reefs & Animal Forests (12.2) | Communities dominated by macroscopic forms of organisms forming hard structures or other types of complex structures on the seabed, i.e. actively modifying the physical environment of the seabed. They mostly represent sessile (i.e. attached to the surface) marine animals (but see 12.2.4, which are photosynthetic organisms forming non-attached carbonate structures), located below the low-tide mark, regardless of the type of substrate they colonise. For accounting purposes (ecosystem extent accounts), a threshold of >25% of area cover (per grid cell) of target biota is proposed as a minimum for including the respective area in this class. |
| Sublittoral Sediments (12.3) | Seabed dominated by sediments of any size class (clay, silt, sand, gravel, cobble) or mixed sediments in the sublittoral zone, extending from the low-tide mark to the upper edge of the continental (or island) slope. Includes seeps and vents in sublittoral sediments (bubbling reef). Excludes: • Sediments with installed anthropogenic structures, sites with mined or dumped sediments (see 12.8) • Sediments with >25% cover by macrophytes (see 12.1) or biogenic reefs and/or animal forest (see 12.2) measured at a grid cell level |
| Sublittoral Rocky Substrates (12.4) | Hard, solid seabed extending from the low-tide mark to the upper edge of the continental (or island) slope. Includes seeps (and vents) in sublittoral rocky substrates. Excludes: • Rocky substrates with anthropogenic structures (see 12.8) • Rocky substrates with >25% cover by macrophytes (see 12.1) or biogenic reefs and/or animal forest (see 12.2) measured at a grid cell level. |
| Continental & Island Slope (12.5) | A steep decline from the edge of a continental shelf (or around an island) to the deep ocean floor. |
| Deep-Sea Ecosystems (12.6) | Marine ecosystems located beyond the outer level of the continental/island slope. |
| Coastal Inlets (12.7) | Bodies of water partially, to a various degree, enclosed by land, having an outlet to the sea or ocean. For accounting purposes, only the extent of bays meeting the definition of class 12 marine ecosystems (i.e. above the high-tide mark) are to be recorded in this class. Excluded are: the intertidal and supratidal areas of bays; these are to be classified in their respective classes, e.g. 10.2 Intertidal macrophyte communities and biogenic reefs, 10.3 Intertidal areas, and 10.4 Other transitional waters, Coastal dunes and fine sediment shores, 11.2 Rocky, boulder and coarse sediment shores, 11.3 Coastal halophytic wetlands, and 11.4 Artificial shorelines |
| Anthropogenic Structures & Modified Ecosystems (12.8) | Man-made structures in the marine environment with an intended installation on a longer-term to permanent basis (i.e. at least a couple of accounting periods), including transport, aquaculture and energy infrastructure and areas where human activities have permanently or in a long term modified the physical aspects of the sea bed, such as dumping and mining areas. Excluded: bottom trawling, dredging (except for port areas, i.e. dredged ports are included in 12.8.1), navigable waterways. |
| Ecosystem type (Level 2) | Ecosystem type (Level 3) | Description |
|---|---|---|
| Marine Macrophyte Communities (12.1) |
Kelp Forests (12.1.1) | Ecosystems formed by dense groups of large brown seaweed known as kelp, in cool, nutrient-rich coastal waters, formed primarily (but not exclusively) by species from the order Laminariales. Understory of other types of marine vegetation may be present. |
| Seagrass Meadows & Beds (12.1.2) | Ecosystems dominated by seagrasses in the sublittoral zone | |
| Fucoids & Other Sublittoral Macrophyte Beds n.e.c. (12.1.3) | Ecosystems formed by fucoids (order Fucales), and/or other macrophytes not elsewhere classified, except for macrophytes forming hard (calcium carbonate) structures (see 12.2.4), in the sublittoral zone. | |
| Biogenic Reefs & Animal Forests (12.2) |
Coral Reefs (12.2.1) | Biogenic structures formed by reef-building (i.e. hard) corals. |
| Shellfish Beds & Reefs (12.2.2) | Biogenic structures formed by accumulations of shellfish (molluscs and crustaceans). They may form a 3-dimensional structure (reef) or form an aggregation on the seabed without an important vertical dimension. | |
| Worm Reefs (12.2.3) | Biogenic structures formed by colonies of tube-dwelling marine worms. | |
| Rhodolith/Maerl Beds (12.2.4) | Biogenic structures formed by the accumulation of rhodoliths (i.e. red algae from the order Corallinales). | |
| Sponge Aggregations (12.2.5) | Biogenic structures formed by the accumulation of sponges. | |
| Other Biogenic Reefs & Animal Forests n.e.c. (12.2.6) | Other biogenic reefs and animal forests not elsewhere classified. | |
| Sublittoral Sediments (12.3) | Sublittoral Mud (Clay & Silt) Plains (12.3.1) | Seabed in the sublittoral zone dominated by cohesive mud, sandy mud and muddy sand, where organism can bury and therefore infauna can be present, extending from the lower limit of the intertidal zone to the shelf break, predominantly in areas where the reduced influence of waves and/or tidal currents allow fine sediments to settle. Excludes: seabed of sublittoral sediment with macrophytes and/or other habitat-forming species covering >25%) of the seabed (see 12.1 and 12.2). |
| Sublittoral Sand Plains (12.3.2) | Medium and fine sands or non-cohesive muddy sands from the lower limit of the intertidal zone to the shelf break, where organisms can bury and therefore infauna can be present, often subject to a degree of wave action or tidal currents which restrict the silt and clay content to 25%) of the seabed (see 12.1 and 12.2). | |
| Sublittoral Mixed Sediment Beds (12.3.3) | Seabed in the sublittoral zone dominated by mixed sediment (i.e. > 50 % of the grid cell area represents sediment) of several size classes neither of which covers >50% of the area of the sediment within the grid cell, where organisms can bury and therefore infauna can be present. | |
| Sublittoral Coarse Sediment Beds (12.3.4) | Coarse sediments including coarse sand, gravel, pebbles, shingle and cobbles which are often unstable due to tides and/or wave action. Typically lack a significant seaweed component and infauna. | |
| Seeps & Vents in Sublittoral Sediments (Incl. Bubbling Reef) (12.3.5) | Features in sublittoral sediments created by leaks of gas (e.g. methane), brine or groundwater from the sediment, or hydrothermal vents (associated with tectonic or volcanic activity). Their activity may be continuous or episodic. | |
| Sublittoral Sediments n.f.d. | Other Sublittoral Sediments not further defined. | |
| Sublittoral Rocky Substrates (12.4) |
Sublittoral Rocky Substrates (12.4.1) | Hard, solid seabed extending from the low-tide mark to the upper edge of the continental (or island) slope. |
| Seeps & Vents in Sublittoral Rocky Substrates (12.4.2) | Features in sublittoral rocky substrates created by leaks of gas (e.g. methane), brine or groundwater from the sediment, or hydrothermal vents (associated with tectonic or volcanic activity). Their activity may be continuous or episodic. | |
| Continental & Island Slope (12.5) |
Slope Surface without Depressions (12.5.1) | Continental or island slope without a depression. |
| Depressions on the Continental Slope (12.5.2) | A depression on the continental slope. Includes: deep-sea trenches and canyons, channels, slope failures and slumps on the continental slope. | |
| Deep-Sea Ecosystems (12.6) | Abyssal Plains (12.6.1) | A large, flat deep-sea floor region located beyond continental margins. |
| Deep-Sea Morphological Features - Raised (12.6.2) | Includes: seamounts, knolls and banks, oceanic ridges, abyssal hills, carbonate mounds and slumps on the sea floor. | |
| Deep-Sea Morphological Features - Depressed (12.6.3) | Includes: deep-sea trenches, canyons and channels. | |
| Deep-Sea Vents & Seeps (12.6.4) | Features in the deep-sea bed created by leaks of gas (e.g. methane), brine or groundwater from the sediment, or hydrothermal vents (associated with tectonic or volcanic activity). Their activity may be continuous or episodic. | |
| Deep-Sea Ecosystems n.f.d. | Other Deep-Sea Ecosystems not further defined. | |
| Water bodies that are partly enclosed by land yet directly connected to a sea or ocean. They have specific geographic features and often shallow water that distinguishes them from the open sea or ocean. | ||
| Fjords (12.7.2) | A long, narrow, marine inlet formed by glacial erosion into a deep, U-shaped trough that is filled with seawater. Fjords are typically over-deepened i.e., deeper in the fjord basin than at their mouth—where they are often bounded by a distinct threshold (or sill) formed by an end moraine deposited by the retreating glacier. This morphology results in limited bottom-water exchange. Fjords are usually steep-sided, deep, and relatively narrow, often branching inland. | |
| Anthropogenic Structures & Modified Ecosystems (12.8) | Aquaculture Installations (12.8.2) | Permanent aquaculture installations (fish cages, anchoring infrastructure, access bridges etc.) |
| Energy Infrastructure (12.8.3) | Infrastructure for the production of energy from any source (wind, wave, oil extraction etc.). These include physical platforms of any size in coastal waters, shelf or the open sea. | |
| Seabed Mining & Dumping Zones (12.8.4) | Includes designated areas for seabed mining and for the disposal of material (e.g. dredged sediment from ports and navigation channels). Excludes: dredged areas of ports and harbours (see 12.8.1); dredged navigation channels (out of scope). | |
| Other Anthropogenic Structures n.e.c. (12.8.5) | Other anthropogenic structures compliant with the definition of 12.8 not elsewhere classified (e.g. shipwrecks, artificial reefs for restoration purposes, etc.). |
A validation exercise was carried out to test agreement between a modified Folk-9 substrate map derived from EUNIS Level 3 habitats and point data from measured sediment samples compiled from INFOMAR surveys.
Within the sediment-only subset (5,939 points), 69.45 percent of samples matched the mapped Folk-9 class exactly, increasing to 85.72 percent when adjacent sediment classes were considered equivalent. Across the broader overlap subset (6,346 points), where classes were represented in both datasets, exact agreement was 67.59 percent and increased to 86.48 percent under the ±1-class tolerance rule.
This ecosystem extent map combines data from a range of survey types carried out at different scales, over different time periods, and for different purposes. This means that there are some limitations that must be kept in mind when using the data:
Spatial data on marine ecosystems are not regularly updated. Marine ecosystems, therefore, are mapped based on best and most recently available data. This means that future iterations of these accounts may have changes that reflect improved surveying efforts of marine habitats, rather than real changes from one ecosystem to another.
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