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Seagrass beds on Atlantic littoral sand
Code: MA522
Correspondence with other classifications:
General description
This habitat has a widespread distribution and is not limited to a few locations. Intertidal Zostera marina beds may extend into the subtidal zone, where they may develop into a perennial form with broad and long leaf and root systems (rhizomes), which survive in winter.
Mid- and upper-shore wave-sheltered muddy fine sand or sandy mud can have high densities of Z. noltii (formerly known as Z. noltei or Z. nana), Z. marina and/or Ruppia spp. Z. noltii forms stands with a cover of delicate trailing narrow leaves that are up to about 20 cm long. As it survives the winter as rhizomes, the locations remain stable over several years. It may occur as monospecific, or with Z. marina or Ruppia spp. and with occasional plants of lower salt-marsh species, such as annual Salicornia spp. or Spartina anglica, as stands of Z. noltii may pass down shore not only to Z. marina, but also to lower saltmarsh communities, notably the Salicornietum europaeae. The factors that determine the distribution of Z. noltii are not entirely clear. This species is peculiar of situations where the substrate dries out on exposure, and on flats with a gentle bar/hollow topography, where it forms distinctive mosaics with Z. marina. It can also occur in shallow standing water; accordingly, it is often found in small permanently submerged lagoons and pools, and on sediment shores where the muddiness of the sediment retains water and stops the roots from drying out. An anoxic layer is usually present at about 5 cm below the surface of the sediment. Seasonal variation may occur in the area covered by intertidal seagrass beds, as plants die back in winter. Intertidal seagrass beds may also be subject to heavy grazing by geese, which can significantly reduce the extent of the plant cover. The rhizomes of Z. noltii will remain in place within the sediment in both situations, and plants towards the lower limit may remain winter-green.
This habitat has a widespread distribution and is not limited to a few locations. Intertidal Zostera marina beds may extend into the subtidal zone, where they may develop into a perennial form with broad and long leaf and root systems (rhizomes), which survive in winter.
Mid- and upper-shore wave-sheltered muddy fine sand or sandy mud can have high densities of Z. noltii (formerly known as Z. noltei or Z. nana), Z. marina and/or Ruppia spp. Z. noltii forms stands with a cover of delicate trailing narrow leaves that are up to about 20 cm long. As it survives the winter as rhizomes, the locations remain stable over several years. It may occur as monospecific, or with Z. marina or Ruppia spp. and with occasional plants of lower salt-marsh species, such as annual Salicornia spp. or Spartina anglica, as stands of Z. noltii may pass down shore not only to Z. marina, but also to lower saltmarsh communities, notably the Salicornietum europaeae. The factors that determine the distribution of Z. noltii are not entirely clear. This species is peculiar of situations where the substrate dries out on exposure, and on flats with a gentle bar/hollow topography, where it forms distinctive mosaics with Z. marina. It can also occur in shallow standing water; accordingly, it is often found in small permanently submerged lagoons and pools, and on sediment shores where the muddiness of the sediment retains water and stops the roots from drying out. An anoxic layer is usually present at about 5 cm below the surface of the sediment. Seasonal variation may occur in the area covered by intertidal seagrass beds, as plants die back in winter. Intertidal seagrass beds may also be subject to heavy grazing by geese, which can significantly reduce the extent of the plant cover. The rhizomes of Z. noltii will remain in place within the sediment in both situations, and plants towards the lower limit may remain winter-green.
In some areas, Z. marina may also be interspersed with Ruppia beds (Connor et al., 2004).
Expanses of clean or muddy fine sand and sandy mud in shallow water and on the lower shore (typically to about 5 m depth) can have dense stands of Z. marina/angustifolia. The community composition may be dominated by these Zostera species and, therefore, be characterised by the associated biota. Other biota present can be closely related to that of areas of sediment not supporting seagrass beds, for example Saccharina latissima, Chorda filum, and infaunal species, such as Ensis spp. and Echinocardium cordatum.
In southern areas, Cymodocea nodosa can also form patches in well sorted fine sands or on superficial muddy sands in sheltered intertidal zones. Frequently is mixed with other habitat forming phanerogams (Zostera noltii and Zostera marina) at muddy sands rich in organic nutrients. Shallow meadows of Cymodocea and Zostera are usually found in sheltered bays close to harbours, e.g. Cadiz Bay, or in areas subject to human impact.
In the North East Atlantic, C. nodosa is nowadays restricted to scattered locations from southern Portugal and Spain to Senegal, including Canary Island and Madeira. Southern Portugal constitutes the current northern geographic limit of its distribution.
Characteristic species
Zostera noltii, Z. marina, Ruppia maritima and/or R. cirrhosa, Cymodocea nodosa
Associated species
The infaunal community of Zostera-beds is often formed by polychaetes Scoloplos armiger, Pygospio elegans and Arenicola marina, oligochaetes, spire shell Peringia ulvae, and bivalves Cerastoderma edule and Macoma balthica. The green algae Ulva spp. may be present on the sediment surface. Ruppia beds may be populated by fish such as Belone belone, Gasterosteus aculeatus, Syngnathus acus and Spinachia spinachia, which are less common on filamentous algal-dominated sediments. Seaweeds such as Chaetomorpha spp., Ulva spp., Cladophora spp., and Chorda filum are also often present in addition to occasional fucoids. In some cases, the stoneworts Lamprothamnium papulosum and Chara aspera occur. Infaunal and epifaunal species may include mysid crustacea, the polychaete Arenicola marina, the gastropod Peringia ulvae, the amphipod Corophium volutator, and oligochaetes such as Heterochaeta costata.
Human activities and anthropogenic pressures threatening the habitat
OSPAR considers that the widespread loss of seagrass is largely a combination of the direct and indirect impacts of the rapid growth in human activities in the coastal zone. Anthropogenic pressures on this habitat include abrasion, pollution, eutrophication (leading to effects such as smothering by epiphytes and algal blooms), changes in hydrological conditions including wave exposure, change in suspended solids, infilling, but also shellfish fisheries, trampling, coastal development, land reclamation, human intrusion, for example driving across intertidal seagrass beds and bait digging. Moreover, invasive algae species can hamper the growth and distribution of seagrass (e.g. Gracilaria spp. in the Wadden Sea).
Best practices in nature restoration
The protection of this habitat is often included in legislation aimed at conservation of seagrass beds, e.g., local by-laws and regulations and cross-border agreements covering large geographical areas, as in the case of the Wadden Sea. It is also a characteristic feature of several habitat types listed in Annex 1 of the HD. The establishment of protected areas and zoning as part of Integrated Coastal Zone Management plans has also been beneficial for the protection of this habitat. These designations and plans can provide a framework under which specific measures, e.g., restrictions on activities such as bait digging, clam raking, and waste water management, may be introduced.
Measures:
- Active seagrass restoration (transplantation and seed-based methods);
- Fisheries management;
- Improvement of water quality.
Bibliographic sources
- Connor, D.W., Dalkin, M.J., Hill, T.O., Holt, R.H.F. & Sanderson, W.G., 1997a. Marine biotope classification for Britain and Ireland. Vol. 2. Sublittoral biotopes. Joint Nature Conservation Committee, Peterborough, JNCC Report no. 230, Version 97.06.
- EEA, 2022b. EUNIS marine habitats classification 2022 with crosswalks to Annex I in separate rows.
- European Red List of Species and habitats: A2.61 Seagrass beds on Atlantic littoral sediments.
- Finck, P., Heinze, S., Raths, U., Riecken, U. & Ssymank, A., 2017. Rote Liste der gefährdeten Biotoptypen Deutschlands. Dritte fortgeschriebene Fassung 2017.-Natursch. Biol. Vielf. 156, 637 S.
- Gamble, C., Glover, A., Debney, A., Bertelli, C., Green, B., Hendy, I., Lilley, R., Nuuttila, H., Potouroglou, M., Ragazzola, F., Unsworth, R., & Preston, J. (Eds.), 2021. Seagrass Restoration Handbook: UK and Ireland. Zoological Society of London.
- JNCC: Littoral seagrass beds.
- JNCC: Zostera marina/angustifolia beds on lower shore or infralittoral clean or muddy sand.
- JNCC: Zostera noltei beds in littoral muddy sand.
- OSPAR: Cymdocoea meadows.
- OSPAR: Zostera beds.
- Polte, P., Asmus, H., 2006. Intertidal seagrass beds (Zostera noltii) as spawning grounds for transient fishes in the Wadden Sea. Marine Ecology Progress Series 312: 235-243 S.
- The Marine Life Information Network (MarLIN): Ruppia maritima in reduced salinity infralittoral muddy sand.
- The Marine Life Information Network (MarLIN): Zostera (Zostera) marina beds on lower shore or infralittoral clean or muddy sand.
- The Marine Life Information Network (MarLIN): Zostera (Zosterella) noltei beds in littoral muddy sand.
- Unsworth R. K. F., Bertelli C. M., Coals L., Cullen-Unsworth L. C., den Haan S., Jones B. L. H., Rees S. R., Thomsen E., Wookey A., Walter B., 2023. Bottlenecks to seed-based seagrass restoration reveal opportunities for improvement, Global Ecology and Conservation, Volume 48, e02736n. Vincent, A. C., Berglund, A. & Ahnesjö, I., 1995. Reproductive ecology of five pipefish species in one eelgrass meadow. Environmental Biology of Fishes 44: 347-361.