Nephtys cirrosa and Bathyporeia spp. in infralittoral sand

Summary

UK and Ireland classification

Description

Well-sorted medium and fine sands characterized by Nephtys cirrosa and Bathyporeia spp. (and sometimes Pontocrates spp.) which occur in the shallow sublittoral to at least 30 m depth. This biotope occurs in sediments subject to physical disturbance, as a result of wave action (and occasionally strong tidal streams in outer estuarine variants of the biotope). The magelonid polychaete Magelona mirabilis may be frequent in this biotope in more sheltered, less tideswept areas whilst in coarser sediments the opportunistic polychaete Chaetozone setosa may be commonly found. The faunal diversity of this biotope is considerably reduced compared to less disturbed biotopes (such as SS.SSa.IMuSa.FfabMag) and for the most part consists of the more actively-swimming amphipods. Sand eels Ammodytes sp. may occasionally be observed in association with this biotope (and others) and spionid polychaetes such as Spio filicornis and S. martinensis may also be present. Occasional Lanice conchilega may be visible at the sediment surface. Variants of the biotope in coarser sediment may have more variable fauna, with the absence of Nephtys, and presence of bryozoans, such as Crisia, however retain examples of Bathyporeia spp. and Magelona spp. Stochastic recruitment events in the Nephtys cirrosa populations may be very important to the population size of other polychaetes present and may therefore create a degree of variation in community composition (Bamber, 1994).

Depth range

0-5 m, 5-10 m

Additional information

No text entered.

Listed By

Habitat review

Ecology

Ecological and functional relationships

  • Communities in wave exposed sand habitats and, by extension, any sediments subject to hydrodynamic disturbance have been assumed to be primarily controlled by specific species responses to the hydrodynamic climate and sediment characteristics which are intimately linked, a scenario where biological interactions do not appear to play a critical role (McLachlan, 1983). Consequently mean macrobenthic diversity and species richness of clean mobile sands is generally lower than that of the surrounding seabed, reflecting greater stresses inherent in such environments (Elliott et al., 1998).
  • Intertidal and subtidal sandy biotopes comprise an unusual ecosystem in that the customary food chain of plants-herbivores-carnivores is not clearly discernible (Eltringham, 1971), the physical environment being too harsh for vegetation to become established. The absence of macroalgae means that herbivorous macrofauna either feed on the biogenic film, on and in the deposit (e.g. Bathyporeia pelagica which is an epistrate feeder) or on phytoplankton from the overlying seawater.
  • The meiofauna are likely to be important consumers of the microphytobenthic productivity. The dominant components of sandbank meiofauna are nematodes and harpacticoid copepods with several other taxa of variable importance (McLachlan, 1983). There is a well established relationship between the relative proportions of nematodes, harpaticoids and grain size. Nematodes tend to dominate in finer sediments, harpaticoids in coarser sediments and in sediments with a median grain size of 0.3-0.35 mm they are both equally important (Gray, 1971; McLachlan et al., 1981).
  • Polychaete worms are dominant infaunal predators, they are opportunistic and actively pursue prey, so that their numbers may be closely related to that of their prey which includes other polychaetes and small crustaceans (Meire et al., 1994). Bamber (1993) found a significant linear correlation between declining densities of Scoloplos armiger and increasing densities of Nephtys cirrosa in a psammophilous polychaete community from the Solent Coast, Hampshire. Nephtys species also scavenge, as does the isopod, Eurydice pulchra, which also actively preys upon the amphipod Bathyporeia pelagica.
  • Conspicuous epibenthic species that may be encountered within the biotope include shrimps (Crangon crangon), crabs (Carcinus maenas, Cancer pagurus and Pagurus bernhardus), starfish (Asterias rubens). Sand eels, Ammodytes sp., may be locally abundant, whilst juvenile gadoids (Gadus morhua & Pollachius virens), adult and juvenile flatfish (Pleuronectes platessa, Limanda limanda & Platichthys flesus) frequent the biotope to feed upon the epi- and infauna.

Seasonal and longer term change

  • A seasonal pattern of abundance is demonstrated by many species, and is characterized by annual recruitment of species increasing their density typically in late summer/autumn. For instance, common cumaceans recorded within the biotope, Pseudocuma longicornis and Cumopsis goodsiri, are almost entirely restricted in their presence to late summer-autumn months (Bamber, 1993). Two reproductive peaks for Bathyporeia pelagica occur in spring and autumn suggesting that an overwintering population matures slowly and reproduces in the spring, and their progeny mature rapidly over five months to reproduce in the autumn of the same year (Watkin, 1939b).
  • Warmer summers may cause temporary declines in the abundance of some species as a result of recruitment failure (juveniles being potentially more sensitive). For instance in a sandy shore community following the warm summer of 1989, Bamber (1993) recorded a significant decrease in the Bathyporeia sarsi population, a species which shows its southern limit of distribution in the English Channel.
  • Mortality of some of the infaunal and epifaunal population may be expected as a result of any winter storms that cause suspension of the substratum.
  • Seasonal changes been documented for the meiofauna of sandy shores in temperate regions, with the meiofauna occurring in lower abundance and moving deeper into the sediment in winter (citations in McLachlan, 1983). Vertical migrations other than seasonal have been reported in response to heavy rain, wave disturbance, tidal factors and changes in moisture and oxygen over the tidal cycle.
  • Vertical migrations from the substratum into the overlying sea water are made by the dominant crustaceans e.g. Eurydice pulchra and Bathyporeia pelagica on nearly every night of the year. Such behaviour is endogenously controlled and has a circatidal rhythm that is coupled to a circasemilunar pattern of emergence (Alheit & Naylor, 1976; Jones & Naylor, 1970; Preece, 1971; Fincham, 1970a & 1970b; Watkin, 1939b).

Habitat structure and complexity

Superficially the habitat may appear to be rather homogenous, but within the sand a variety of niches are probably available for colonization. For instance, sandbanks may show a gradient from finer sediments to coarser sediments resulting from the prevailing current pattern. The upper sand layers may be characterized by sand waves and ripples occurring on a variety scales, which are continually destroyed and rebuilt by currents, a process visible at the waters surface by the appearance of patches of suspended sediment. In other instances the distribution of different grades of sandy sediment may be very patchy and at the bottom of depressions finer sediments, more stable deposits, enriched with some mud might be found (Vanosmael et al., 1982).

Productivity

The macrobenthic infauna of the biotope consists of animals which feed largely on particulate matter in or on the sand, and which are themselves preyed upon by populations of juvenile flatfish (McIntyre & Eleftheriou, 1968). Owing to the lack of stable substrata, benthic microalgae constitute the main primary producers of the biotope and the quality of light (as critical depth for primary production) reaching sandbanks in the sublittoral will determine the type of microalgae colonizing the sediment. Owing to turbulence created by tidal flow and wave action, overlying water may be particularly turbid, limiting primary production further. Steele & Baird (1968) estimated microphytobenthic production to be 4-9 g C/m²/yr a figure they considered to be inadequate for the macrofauna and rich meiofauna (assuming an ecological efficiency of 10%, the infaunal biota of this biotope would probably have an annual requirement in the region of 25 g C/m²). To support the infauna the biotope must be subsidised to a high degree by organic matter produced in the water column and other environments and transported to the biotope, consequently productivity of this biotope is mostly secondary (McLachlan, 1980). Primary production in the water column was estimated to be in the region of 95 g C/m² annually (Steele & Baird, 1968) and some of this is directly available or may reach the benthos indirectly after intervening trophic levels. Baird & Steele (1968) demonstrated that only 3-5% of the organic matter in the sand was unattached, so that a continuous supply of material and rapid filtering of water through the sand are essential if the requirements of the benthos are to be met.

Recruitment processes

Characterizing macrofauna of the biotope are iteroparous, meaning that they breed several times per lifetime. Some species have a brooding and benthic mode of reproduction whilst others are broadcast spawners with a planktonic phase of development.
  • Important meiofaunal nematodes and harpacticoid copepods of the sandy shore are reported to have year-round reproduction with generation times ranging from 1-3 months (McIntyre, 1969).
  • Bathyporeia pelagica may breed throughout the year, but the greatest reproductive activity occurs during spring and late summer/autumn. Males and females pair whilst swimming and mate on the night-time ebb tides following each new and full moon. Development of an egg to the stage when it is released as a juvenile takes just 15 days to complete. The overwintering population of Bathyporeia pelagica consists largely of juvenile animals. These mature in spring to form the majority of the next breeding population and eventually die in June and July, after a lifespan of about one year (Fish & Preece, 1970).
  • Eurydice pulchra breeds between April and August once sea temperatures rise above 10°C, and the highest number of juveniles occur around the periods of maximum summer temperatures. Although the first juveniles may reach sexual maturity before the onset of winter, they begin breeding in the following spring and die during their second autumn after a total lifespan of approximately 15 months. Mid-summer juveniles also mature to breed the following summer and only reached 12 months of age before dying. In contrast, the last broods appearing as late as October, do not mature until late the following summer. They breed in their second October and then overwinter for a second time, producing a second brood in the spring before dying of at 18-20 months old (Hayward, 1994; Jones, 1970; Fish, 1970).
  • Polychaete worms such as Nephtys spp. and spionid worms release their eggs and sperm into the water where, after fertilization and a relatively prolonged planktonic phase of development, they metamorphose and commence a benthic habit. Recruitment of Nephtys species seems related to environmental conditions in central parts of the species range, marginal populations exhibit occasional reproductive failures, e.g. Nephtys cirrosa, which is a temperate species and reaches the northern limit of its range in the north of the British Isles. Populations of Nephtys cirrosa on the east and west coasts of northern Britain exhibit different reproductive patterns. In south-west Scotland gravid adults breed every year in early autumn, whilst those on the east coast experience periods (e.g. over three years) of reproductive failure (Olive & Morgan, 1991).

Time for community to reach maturity

As a consequence of the dynamic nature of the habitat the faunal component of the biotope is very sparse and low in species richness. Therefore, the community might be considered 'mature' (in terms of representative species present) only a few days or weeks after the last disturbance, as displaced polychaetes and crustaceans re-enter the substratum.

Additional information

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Preferences & Distribution

Habitat preferences

Depth Range 0-5 m, 5-10 m
Water clarity preferencesNo information
Limiting Nutrients No information
Salinity preferences Full (30-40 psu)
Physiographic preferences Enclosed coast or Embayment, Estuary, Open coast
Biological zone preferences Infralittoral
Substratum/habitat preferences Fine clean sand, Medium clean sand
Tidal strength preferences Very weak (negligible), Weak < 1 knot (<0.5 m/sec.)
Wave exposure preferences Exposed, Moderately exposed
Other preferences

Additional Information

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Species composition

Species found especially in this biotope

Rare or scarce species associated with this biotope

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Additional information

The occurrence of rare species and very high diversity is unusual in mobile sandbanks. However, important species of interstitial polychaete may be recorded within the biotope, for instance, Polygordius appendiculatus, which has a preference for coarse and medium sands. In mobile subtidal sandbanks in the North Sea, Vanosmael et al., (1982) found exceptional numbers of Epilonematidae and Draconematoidea (Nematoda) and three important species of interstitial polychaetes, Polygordius appendiculatus, Protodriloides chaetifer and a species of the genus Protodrilus. Such species are adapted to the extreme instability of the substratum of the sandbanks and are confined to such biotopes (Elliott et al., 1998).

Sensitivity review

Sensitivity characteristics of the habitat and relevant characteristic species

The biotope description and characterizing species are taken from JNCC (2022). This biotope is characterized by mobile clean sand sediments in shallow water. The mobility of the sediment leads to a species-poor community, with polychaetes (Nephtys cirrosa), and burrowing amphipods (Bathyporeia spp.) characterizing the biotope. The sediments and wave exposure are key factors maintaining the biotope and are considered in the sensitivity assessments where the pressure may alter these.  

Resilience and recovery rates of habitat

The species inhabiting this biotope are characteristic of mobile sediments and are adapted to the high levels of disturbance.  The species present in the biotope must either be able to withstand mobile sediments through physical robustness, mobility and ability to re-position within sediments such as Nephtys cirrosa and the mobile amphipods and/or to recover rapidly to sustain population losses following severe erosion. Characterizing species typically have opportunistic life history strategies, with short life histories (typically two years or less, see below), rapid maturation and extended reproductive periods. Typically they produce juveniles that are either brooded (amphipods and isopds) and are therefore present to repopulate the disturbed habitat directly, or have pelagic larvae (Nephtys cirrosa) capable of dispersal within the water column. Adults may also be transported in the water column.

The amphipods characterizing this biotope are found in sediments subject to physical disturbance, as a result of wave action or in wave sheltered biotopes, strong tidal streams. This group is, therefore, tolerant of disturbed environments and can recover quickly. Bathyporeia spp. are short lived, reaching sexual maturity within 6 months with 6-15 eggs per brood, depending on species.  Reproduction may be continuous (Speybroeck et al., 2008) with one set of embryos developing in the brood pouch whilst the next set of eggs is developing in the ovaries. However, specific reproductive periods vary between  species and between locations (Mettam, 1989) and bivoltine patterns (twice yearly peaks in reproduction) have been observed (Mettam, 1989; Speybroeck et al., 2008). Adult amphipods are highly mobile in the water column and recolonization by the adults is likely to be a significant recovery pathway.  The life history traits of rapid sexual maturation and production of multiple broods annually support rapid local recolonization of disturbed sediments where some of the adult population remains.

Nephtys cirrosa is a relatively long-lived polychaete with a lifespan of 6 to possibly as much as 9 years. It matures at 1 year and the females release over 10,000 (and up to 80,000 depending on species) eggs of 0.11-0.12mm from April through to March. These are fertilized externally and develop into an early lecithotrophic larva & a later planktotrophic larva which spends as much as 12 months in the water column before settling from July-September. The genus has a relatively high reproductive capacity and widespread dispersion during the lengthy larval phase. It is likely to have a high recoverability following disturbance (MES, 2010). Adults are mobile and capable of swimming and adults are therefor qable to migrate in and out of this biotope.

Resilience assessment. As a consequence of the dynamic nature of the habitat the faunal component of the biotope is very sparse and low in species richness. Therefore, the community might be considered 'mature' only a few days or weeks after the last storm event, as the mobile species displaced from the biotope and those from adjacent area colonize the substratum via the surf plankton. Even following severe disturbances recovery would be expected to occur within a year; biotope resilience is therefore assessed as ‘High’ for any level of impact (e.g. where resistance is ‘None’, ‘Low’ or ‘Medium’).

NB: The resilience and the ability to recover from human induced pressures is a combination of the environmental conditions of the site, the frequency (repeated disturbances versus a one-off event) and the intensity of the disturbance. Recovery of impacted populations will always be mediated by stochastic events and processes acting over different scales including, but not limited to, local habitat conditions, further impacts and processes such as larval-supply and recruitment between populations. Full recovery is defined as the return to the state of the habitat that existed prior to impact.  This does not necessarily mean that every component species has returned to its prior condition, abundance or extent but that the relevant functional components are present and the habitat is structurally and functionally recognizable as the initial habitat of interest. It should be noted that the recovery rates are only indicative of the recovery potential.

Climate Change Pressures

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ResistanceResilienceSensitivity
Global warming (extreme) [Show more]

Global warming (extreme)

Extreme emission scenario (by the end of this century 2081-2100) benchmark of:

  • A 5°C rise in SST and NBT (coastal to the shelf seas),

  • A 6°C rise in surface air temperature (in eulittoral and supralittoral habitats).

  • A 1°C rise in Deep-sea habitats (>200 m) off the continental shelf, and

  • A 5°C rise in surface air temperature in intertidal habitats exclusive to Scotland. Further detail.

Evidence

Under the middle emission, high emission and extreme scenarios, sea surface temperatures are expected to increase by 3, 4 and 5°C respectively, leading to temperatures increasing to between 22-24°C by the end of this century in the south of the UK, although northern UK temperatures will be up to 5°C lower. Species from the genus Bathyporeia spp. have high upper lethal temperature limits (the temperature at which 50% of individuals died after 24 hours exposure) of 37.5°C for Bathyporeia pilosa and 33.4°C for Bathyporeia pelagica (Preece, 1971). The ability to withstand these high temperatures may be because they can be found in the intertidal, where temperatures fluctuate much more than the subtidal, where conditions are more stable. While they can withstand a short-term, sharp temperature increase, their ability to withstand long-term changes in temperature is more difficult to discern. Most species of Bathyporeia (Bathyporeia pelagica, Bathyporeia elegans, Bathyporeia sarsi) have a limited distribution, being primarily found around the UK, and from the coast of Norway down to the French coast of the Bay of Biscay, and are abundant in the North Sea (Künitzer et al., 1992).

Nephtys cirrosa has a less limited, and more southern distribution than amphipods from the genus Bathyporeia spp. and is therefore more likely to exhibit greater temperature tolerance. It is common in the NE Atlantic, including the English Channel and the North Sea and down the coast of Spain and Portugal, and can also be found in the Mediterranean and the Black Sea down to a depth of 45 m (Rainer, 1991).

Sensitivity assessment. With sea surface temperatures around the UK currently falling between 6-19°C (Huthnance, 2010), populations of Nephtys cirrosa and Bathyporeia spp. are likely to be able to adapt to cope with a gradual rise in ocean temperatures of 3°C (middle emission scenario), leading to mean summer high temperatures of 22°C by the end of this century, as these species currently experience summer temperatures of 22°C in the Bay of Biscay (Koutsikopoulos et al., 1998). Therefore, for the middle emission scenario, resistance is assessed as ‘High’, and resilience as ‘High’, and sensitivity is assessed as ‘Not sensitive’

Under the high emission and extreme scenarios, whereby summer sea surface temperatures are expected to increase 4-5°C to 23-24°C in southern England, there is likely to be some impact on Bathyporeia spp. although Nephtys cirrosa is expected to be able to withstand this temperature rise, as its distribution includes the Mediterranean, where these temperatures are exceeded. Whilst Bathyporeia spp. have been known to withstand short-term extreme temperature fluctuations (Preece, 1971), species from the genus Bathyporeia are known to have a more limited geographical distribution, and occur north of the Bay of Biscay where summer temperatures reach 22°C (Koutsikopoulos et al., 1998), which suggests that this may be a cut off point for proliferation of this species. An increase of 4-5°C is likely to cause some mortality and loss to populations in southern England (an increase in temperature of 4-5°C in Scotland, Northern England, Wales or Ireland would lead to temperatures of 22°C), resistance is assessed as ‘Medium’, and resilience is assessed as ‘Very Low’ as any population declines in southern England will not recover due to the long-term nature of global warming. Therefore, this biotope is assessed as ‘Medium’ sensitivity to both the high emission and extreme scenarios.

Medium
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Very Low
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Medium
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Global warming (high) [Show more]

Global warming (high)

High emission scenario (by the end of this century 2081-2100) benchmark of:

  • A 4°C rise in SST, NBT (coastal to the shelf seas) and surface air temperature (in eulittoral and supralittoral habitats).

  • A 1°C rise in Deep-sea habitats (>200 m) off the continental shelf, and

  • A 3°C rise in surface air temperature in intertidal habitats exclusive to Scotland. Further detail.

Evidence

Under the middle emission, high emission and extreme scenarios, sea surface temperatures are expected to increase by 3, 4 and 5°C respectively, leading to temperatures increasing to between 22-24°C by the end of this century in the south of the UK, although northern UK temperatures will be up to 5°C lower. Species from the genus Bathyporeia spp. have high upper lethal temperature limits (the temperature at which 50% of individuals died after 24 hours exposure) of 37.5°C for Bathyporeia pilosa and 33.4°C for Bathyporeia pelagica (Preece, 1971). The ability to withstand these high temperatures may be because they can be found in the intertidal, where temperatures fluctuate much more than the subtidal, where conditions are more stable. While they can withstand a short-term, sharp temperature increase, their ability to withstand long-term changes in temperature is more difficult to discern. Most species of Bathyporeia (Bathyporeia pelagica, Bathyporeia elegans, Bathyporeia sarsi) have a limited distribution, being primarily found around the UK, and from the coast of Norway down to the French coast of the Bay of Biscay, and are abundant in the North Sea (Künitzer et al., 1992).

Nephtys cirrosa has a less limited, and more southern distribution than amphipods from the genus Bathyporeia spp. and is therefore more likely to exhibit greater temperature tolerance. It is common in the NE Atlantic, including the English Channel and the North Sea and down the coast of Spain and Portugal, and can also be found in the Mediterranean and the Black Sea down to a depth of 45 m (Rainer, 1991).

Sensitivity assessment. With sea surface temperatures around the UK currently falling between 6-19°C (Huthnance, 2010), populations of Nephtys cirrosa and Bathyporeia spp. are likely to be able to adapt to cope with a gradual rise in ocean temperatures of 3°C (middle emission scenario), leading to mean summer high temperatures of 22°C by the end of this century, as these species currently experience summer temperatures of 22°C in the Bay of Biscay (Koutsikopoulos et al., 1998). Therefore, for the middle emission scenario, resistance is assessed as ‘High’, and resilience as ‘High’, and sensitivity is assessed as ‘Not sensitive’

Under the high emission and extreme scenarios, whereby summer sea surface temperatures are expected to increase 4-5°C to 23-24°C in southern England, there is likely to be some impact on Bathyporeia spp. although Nephtys cirrosa is expected to be able to withstand this temperature rise, as its distribution includes the Mediterranean, where these temperatures are exceeded. Whilst Bathyporeia spp. have been known to withstand short-term extreme temperature fluctuations (Preece, 1971), species from the genus Bathyporeia are known to have a more limited geographical distribution, and occur north of the Bay of Biscay where summer temperatures reach 22°C (Koutsikopoulos et al., 1998), which suggests that this may be a cut off point for proliferation of this species. An increase of 4-5°C is likely to cause some mortality and loss to populations in southern England (an increase in temperature of 4-5°C in Scotland, Northern England, Wales or Ireland would lead to temperatures of 22°C), resistance is assessed as ‘Medium’, and resilience is assessed as ‘Very Low’ as any population declines in southern England will not recover due to the long-term nature of global warming. Therefore, this biotope is assessed as ‘Medium’ sensitivity to both the high emission and extreme scenarios.

Medium
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Very Low
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High
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Medium
Medium
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Low
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Global warming (middle) [Show more]

Global warming (middle)

Middle emission scenario (by the end of this century 2081-2100) benchmark of:

  • A 3°C rise in SST, NBT (coastal to the shelf seas) and surface air temperature (in eulittoral and supralittoral habitats).

  • A 1°C rise in Deep-sea habitats (>200 m) off the continental shelf.

  • A 2°C rise in surface air temperature in intertidal habitats exclusive to Scotland. Further detail.

Evidence

Under the middle emission, high emission and extreme scenarios, sea surface temperatures are expected to increase by 3, 4 and 5°C respectively, leading to temperatures increasing to between 22-24°C by the end of this century in the south of the UK, although northern UK temperatures will be up to 5°C lower. Species from the genus Bathyporeia spp. have high upper lethal temperature limits (the temperature at which 50% of individuals died after 24 hours exposure) of 37.5°C for Bathyporeia pilosa and 33.4°C for Bathyporeia pelagica (Preece, 1971). The ability to withstand these high temperatures may be because they can be found in the intertidal, where temperatures fluctuate much more than the subtidal, where conditions are more stable. While they can withstand a short-term, sharp temperature increase, their ability to withstand long-term changes in temperature is more difficult to discern. Most species of Bathyporeia (Bathyporeia pelagica, Bathyporeia elegans, Bathyporeia sarsi) have a limited distribution, being primarily found around the UK, and from the coast of Norway down to the French coast of the Bay of Biscay, and are abundant in the North Sea (Künitzer et al., 1992).

Nephtys cirrosa has a less limited, and more southern distribution than amphipods from the genus Bathyporeia spp. and is therefore more likely to exhibit greater temperature tolerance. It is common in the NE Atlantic, including the English Channel and the North Sea and down the coast of Spain and Portugal, and can also be found in the Mediterranean and the Black Sea down to a depth of 45 m (Rainer, 1991).

Sensitivity assessment. With sea surface temperatures around the UK currently falling between 6-19°C (Huthnance, 2010), populations of Nephtys cirrosa and Bathyporeia spp. are likely to be able to adapt to cope with a gradual rise in ocean temperatures of 3°C (middle emission scenario), leading to mean summer high temperatures of 22°C by the end of this century, as these species currently experience summer temperatures of 22°C in the Bay of Biscay (Koutsikopoulos et al., 1998). Therefore, for the middle emission scenario, resistance is assessed as ‘High’, and resilience as ‘High’, and sensitivity is assessed as ‘Not sensitive’

Under the high emission and extreme scenarios, whereby summer sea surface temperatures are expected to increase 4-5°C to 23-24°C in southern England, there is likely to be some impact on Bathyporeia spp. although Nephtys cirrosa is expected to be able to withstand this temperature rise, as its distribution includes the Mediterranean, where these temperatures are exceeded. Whilst Bathyporeia spp. have been known to withstand short-term extreme temperature fluctuations (Preece, 1971), species from the genus Bathyporeia are known to have a more limited geographical distribution, and occur north of the Bay of Biscay where summer temperatures reach 22°C (Koutsikopoulos et al., 1998), which suggests that this may be a cut off point for proliferation of this species. An increase of 4-5°C is likely to cause some mortality and loss to populations in southern England (an increase in temperature of 4-5°C in Scotland, Northern England, Wales or Ireland would lead to temperatures of 22°C), resistance is assessed as ‘Medium’, and resilience is assessed as ‘Very Low’ as any population declines in southern England will not recover due to the long-term nature of global warming. Therefore, this biotope is assessed as ‘Medium’ sensitivity to both the high emission and extreme scenarios.

High
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High
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Not sensitive
Medium
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Marine heatwaves (high) [Show more]

Marine heatwaves (high)

High emission scenario benchmark: A marine heatwave occurring every two years, with a mean duration of 120 days, and a maximum intensity of 3.5°C. Further detail.

Evidence

Marine heatwaves due to increased air-sea heat flux are predicted to occur more frequently, last for longer and at increased intensity by the end of this century under both middle and high emission scenarios (Frölicher et al., 2018). Both Bathyporeia pilosa and Bathyporeia pelagica are known to be able to withstand short-term high temperatures, with upper lethal temperatures after 24 hrs for both species exceeding 33°C, and no mortality observed at 29°C (Preece, 1971).

In Kiel Fjord in the Baltic Sea, where temperatures generally range from 0-20°C, simulated marine heatwaves on natural communities (summer temperature increased to 25°C), led to increased biomass in two out of four species of polychaetes, whilst a decrease in both biomass and abundance was seen for a tube-dwelling polychaete (Pansch et al., 2018). In the same study, the biomass of two of the four amphipod species significantly increased, whereas no significant negative impacts were seen on either biomass or abundance of the other species. The southern limit of Gammarus salinus is the Bay of Biscay, and this species has a similar distribution to species from the genus Bathyporeia. Gammarus salinus appeared to have a slight positive response in abundance and biomass to a simulated heatwave of 25°C, although this was not significant (Pansch et al., 2018).

Sensitivity assessment. Under the middle emission scenario, if heatwaves occurred every three years, with a maximum intensity of 2°C for a period of 80 days by the end of this century, this could lead to summer sea temperatures reaching up to 24°C in southern England. It is likely that both Nephtys cirrosa and Bathyporeia spp. will be able to withstand a heatwave of this intensity and duration, as Nephtys cirrosa can withstand Mediterranean temperatures and Gammarus salinus, which has a similar geographical range as Bathyporeia spp. can withstand heatwaves of this magnitude. Therefore, resistance is assessed as ‘High’, resilience as ‘High’, and the biotope is assessed as ‘Not sensitive’. Under the high emission scenario, if heatwaves occur every two years by the end of this century, reaching a maximum intensity of 3.5°C for 120 days, this could lead to the heatwave lasting the entire summer with temperatures reaching up to 26.5°C. Nephtys cirrosa will likely be able to withstand this temperature. Although species from the genus Bathyporeia are known to be able to withstand high temperatures for short periods (Preece, 1971), they do not occur south of the Bay of Biscay and some mortality is likely during a prolongued three-month heatwave event. As such, under the high emission scenario, resistance has been assessed as ‘Medium’. As recovery of Bathyporeia spp. populations is rapid, resilience is assessed as ‘High’.  Therefore, this biotope is assessed as having ‘Low’ sensitivity to marine heatwaves under the high emission scenario. 

Medium
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High
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Low
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Marine heatwaves (middle) [Show more]

Marine heatwaves (middle)

Middle emission scenario benchmark:  A marine heatwave occurring every three years, with a mean duration of 80 days, with a maximum intensity of 2°C. Further detail.

Evidence

Marine heatwaves due to increased air-sea heat flux are predicted to occur more frequently, last for longer and at increased intensity by the end of this century under both middle and high emission scenarios (Frölicher et al., 2018). Both Bathyporeia pilosa and Bathyporeia pelagica are known to be able to withstand short-term high temperatures, with upper lethal temperatures after 24 hrs for both species exceeding 33°C, and no mortality observed at 29°C (Preece, 1971).

In Kiel Fjord in the Baltic Sea, where temperatures generally range from 0-20°C, simulated marine heatwaves on natural communities (summer temperature increased to 25°C), led to increased biomass in two out of four species of polychaetes, whilst a decrease in both biomass and abundance was seen for a tube-dwelling polychaete (Pansch et al., 2018). In the same study, the biomass of two of the four amphipod species significantly increased, whereas no significant negative impacts were seen on either biomass or abundance of the other species. The southern limit of Gammarus salinus is the Bay of Biscay, and this species has a similar distribution to species from the genus Bathyporeia. Gammarus salinus appeared to have a slight positive response in abundance and biomass to a simulated heatwave of 25°C, although this was not significant (Pansch et al., 2018).

Sensitivity assessment. Under the middle emission scenario, if heatwaves occurred every three years, with a maximum intensity of 2°C for a period of 80 days by the end of this century, this could lead to summer sea temperatures reaching up to 24°C in southern England. It is likely that both Nephtys cirrosa and Bathyporeia spp. will be able to withstand a heatwave of this intensity and duration, as Nephtys cirrosa can withstand Mediterranean temperatures and Gammarus salinus, which has a similar geographical range as Bathyporeia spp. can withstand heatwaves of this magnitude. Therefore, resistance is assessed as ‘High’, resilience as ‘High’, and the biotope is assessed as ‘Not sensitive’. Under the high emission scenario, if heatwaves occur every two years by the end of this century, reaching a maximum intensity of 3.5°C for 120 days, this could lead to the heatwave lasting the entire summer with temperatures reaching up to 26.5°C. Nephtys cirrosa will likely be able to withstand this temperature. Although species from the genus Bathyporeia are known to be able to withstand high temperatures for short periods (Preece, 1971), they do not occur south of the Bay of Biscay and some mortality is likely during a prolongued three-month heatwave event. As such, under the high emission scenario, resistance has been assessed as ‘Medium’. As recovery of Bathyporeia spp. populations is rapid, resilience is assessed as ‘High’.  Therefore, this biotope is assessed as having ‘Low’ sensitivity to marine heatwaves under the high emission scenario. 

High
Medium
Medium
Low
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High
High
High
High
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Not sensitive
Medium
Medium
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Ocean acidification (high) [Show more]

Ocean acidification (high)

High emission scenario benchmark: a further decrease in pH of 0.35 (annual mean) and corresponding 120% increase in H+ ions , seasonal aragonite saturation of 20% of UK coastal waters and North Sea bottom waters, and the aragonite saturation horizon in the NE Atlantic, off the continental shelf, occurring at a depth of 400 m by the end of this century 2081-2100. Further detail 

Evidence

Increasing levels of CO2 in the atmosphere have led to the average pH of sea surface waters dropping from 8.25 in the 1700s to 8.14 in the 1990s (Jacobson, 2005). There is no direct evidence of the impact of ocean acidification on either Nephtys cirrosa or amphipods from the genus Bathyporeia, which characterize this habitat. Amphipods are generally thought to be less sensitive to ocean acidification than some other taxa and are actually found in greater numbers at naturally CO2 enriched vents (Kroeker et al., 2011, Garrard et al., 2014, Vizzini et al., 2017). This increase in abundance is not directly related to CO2 enrichment, but rather due to indirect effects such as reduced predation or increased food supply.  A laboratory study found that under CO2 enrichment, the population size of the amphipod Gammarus locusta increased 20 fold and the proportion of gravid females doubled, suggesting that ocean acidification may confer an advantage to amphipods by relaxing environmental constraints on reproduction (Heldt et al., 2016). Further laboratory experiments show little effect of ocean acidification at levels expected for the high emission scenario at the end of this century (pH 7.8) (Hauton et al., 2009, Hale et al., 2011, Lim & Harley, 2018).

Non-calcifying polychaetes are also thought to be less sensitive than many other taxa.  When non-calcifying polychaetes were transplanted from control to low pH areas, they showed evidence of either adaptation or acclimation to their conditions (Calosi et al., 2013). There is some evidence that sperm may be affected by ocean acidification at levels expected in the high emission scenario, with percentage sperm motility (Schlegel et al., 2014) and sperm velocity (Campbell et al., 2014) decreasing in the polychaetes Galeolaria caespitosa and Arenicola marina, leading to a decrease in sperm fertility success (Campbell et al., 2014). Reduced sperm fertility and hence recruitment, may lead to some population-level effects. However, at natural CO2 vents, the abundance of polychaetes either remained the same (Kroeker et al., 2011) or increased (Garrard et al., 2014, Vizzini et al., 2017). Most species of polychaetes generally exhibit high fecundity and are free spawning (Ramirez-Llodra, 2002), which may help them maintain population levels, even with a decrease in fertilization success. For example, Nephtys cirrosa is a reasonably fecund species that releases between 10,000 – 80,000 eggs into the water column during a spawning cycle (MES, 2010).

Sensitivity Assessment. Direct evidence of the impact of ocean acidification on Nephtys cirrosa and Bathyporeia spp. is lacking. However, in general, non-calcifying polychaetes and amphipods appear to be tolerant. Therefore, it is likely that the characterizing species of this biotope will show a ‘High’ resistance to a decrease in pH, even though ocean acidification has been shown to lead to negative impacts on polychaete fertilization success under experimental conditions (Campbell et al., 2014, Schlegel et al., 2014). As such, based on the evidence available, under both the middle and high emission scenarios the biotope is assessed as ‘High’ resistance to ocean acidification, and ‘High’ resilience, leading to an assessment of ‘Not sensitive’ at the benchmark level

High
Medium
Medium
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High
High
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Not sensitive
Medium
Medium
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Ocean acidification (middle) [Show more]

Ocean acidification (middle)

Middle emission scenario benchmark: a further decrease in pH of 0.15 (annual mean) and corresponding 35% increase in H+ ions with no coastal aragonite undersaturation and the aragonite saturation horizon in the NE Atlantic, off the continental shelf, at a depth of 800 m by the end of this century 2081-2100. Further detail.

Evidence

Increasing levels of CO2 in the atmosphere have led to the average pH of sea surface waters dropping from 8.25 in the 1700s to 8.14 in the 1990s (Jacobson, 2005). There is no direct evidence of the impact of ocean acidification on either Nephtys cirrosa or amphipods from the genus Bathyporeia, which characterize this habitat. Amphipods are generally thought to be less sensitive to ocean acidification than some other taxa and are actually found in greater numbers at naturally CO2 enriched vents (Kroeker et al., 2011, Garrard et al., 2014, Vizzini et al., 2017). This increase in abundance is not directly related to CO2 enrichment, but rather due to indirect effects such as reduced predation or increased food supply.  A laboratory study found that under CO2 enrichment, the population size of the amphipod Gammarus locusta increased 20 fold and the proportion of gravid females doubled, suggesting that ocean acidification may confer an advantage to amphipods by relaxing environmental constraints on reproduction (Heldt et al., 2016). Further laboratory experiments show little effect of ocean acidification at levels expected for the high emission scenario at the end of this century (pH 7.8) (Hauton et al., 2009, Hale et al., 2011, Lim & Harley, 2018).

Non-calcifying polychaetes are also thought to be less sensitive than many other taxa.  When non-calcifying polychaetes were transplanted from control to low pH areas, they showed evidence of either adaptation or acclimation to their conditions (Calosi et al., 2013). There is some evidence that sperm may be affected by ocean acidification at levels expected in the high emission scenario, with percentage sperm motility (Schlegel et al., 2014) and sperm velocity (Campbell et al., 2014) decreasing in the polychaetes Galeolaria caespitosa and Arenicola marina, leading to a decrease in sperm fertility success (Campbell et al., 2014). Reduced sperm fertility and hence recruitment, may lead to some population-level effects. However, at natural CO2 vents, the abundance of polychaetes either remained the same (Kroeker et al., 2011) or increased (Garrard et al., 2014, Vizzini et al., 2017). Most species of polychaetes generally exhibit high fecundity and are free spawning (Ramirez-Llodra, 2002), which may help them maintain population levels, even with a decrease in fertilization success. For example, Nephtys cirrosa is a reasonably fecund species that releases between 10,000 – 80,000 eggs into the water column during a spawning cycle (MES, 2010).

Sensitivity Assessment. Direct evidence of the impact of ocean acidification on Nephtys cirrosa and Bathyporeia spp. is lacking. However, in general, non-calcifying polychaetes and amphipods appear to be tolerant. Therefore, it is likely that the characterizing species of this biotope will show a ‘High’ resistance to a decrease in pH, even though ocean acidification has been shown to lead to negative impacts on polychaete fertilization success under experimental conditions (Campbell et al., 2014, Schlegel et al., 2014). As such, based on the evidence available, under both the middle and high emission scenarios the biotope is assessed as ‘High’ resistance to ocean acidification, and ‘High’ resilience, leading to an assessment of ‘Not sensitive’ at the benchmark level

High
Medium
Medium
High
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High
High
High
High
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Not sensitive
Medium
Medium
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Sea level rise (extreme) [Show more]

Sea level rise (extreme)

Extreme scenario benchmark: a 107 cm rise in average UK by the end of this century (2018-2100). Further detail.

Evidence

Sea-level rise is occurring through a combination of thermal expansion and ice melt.  Sea levels have risen 1-3 mm/yr in the last century (Cazenave & Nerem, 2004, Church et al., 2004, Church & White, 2006). The most recent projections on sea-level rise suggest a rise of 50 cm under the middle emission scenario, 70 cm under the high emission scenario, and 107 cm under the extreme scenario. Species from the genus Bathyporeia and Nephtys cirrosa are abundant at on the Dogger Bank, which has a depth range of 15- 36 m (Wieking & Kröncke, 2003), suggesting that, as long as the habitat remains the same (sand), these species will be tolerant of future sea-level rise for all three scenarios. Nephtys cirrosa occurs on clean sand, down to a depth of 45 m (Rainer, 1991), whilst species of Bathyporeia are often abundant at depths <30 m (Künitzer et al., 1992)

Any potential increase in wave exposure in relation to sea-level rise (e.g. Fujii & Raffaelli, 2008) is not expected to impact this biotope, as these species occur on medium to very fine sand in moderately exposed to exposed areas (JNCC, 2019), therefore an increase in exposure is unlikely to change habitat classification.  However, as wave action is reduced with depth, an increase in depth may stabilize the sediment allowing the habitat to transition into IMuSaFfabMag, resulting in loss of the deeper portions of the biotope. However, over time the biotope may extend inshore, depending on location. Sensitivity assessment. There is likely to be considerable variation between sites, and the depth range occupied by the biotope.  Hence, it is difficult to assess the effect of the different sea-level rise scenarios.  As the biotope can occur from 0-10 m in depth, it is assumed that a sea-level rise of 50 cm, or 70 cm (middle to high emission scenarios) would have limited effect but that a 107 cm rise (the extreme scenario) might result in loss of part of the deeper extent of the biotope in some sites.  Therefore, resistance is assessed as ‘High’ under the middle and high emission scenarios so that resilience is ‘High’ and sensitivity assessed as ‘Not sensitive’.  But resistance is possibly ‘Medium’ under the extreme scenario, so that resilience is ‘Very low’ and sensitivity assessed as ‘Medium’, albeit with ‘Low’ confidence.

Medium
Low
NR
NR
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Very Low
High
High
High
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Medium
Low
Low
Low
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Sea level rise (high) [Show more]

Sea level rise (high)

High emission scenario benchmark: a 70 cm rise in average UK by the end of this century (2018-2100). Further detail.

Evidence

Sea-level rise is occurring through a combination of thermal expansion and ice melt.  Sea levels have risen 1-3 mm/yr in the last century (Cazenave & Nerem, 2004, Church et al., 2004, Church & White, 2006). The most recent projections on sea-level rise suggest a rise of 50 cm under the middle emission scenario, 70 cm under the high emission scenario, and 107 cm under the extreme scenario. Species from the genus Bathyporeia and Nephtys cirrosa are abundant at on the Dogger Bank, which has a depth range of 15- 36 m (Wieking & Kröncke, 2003), suggesting that, as long as the habitat remains the same (sand), these species will be tolerant of future sea-level rise for all three scenarios. Nephtys cirrosa occurs on clean sand, down to a depth of 45 m (Rainer, 1991), whilst species of Bathyporeia are often abundant at depths <30 m (Künitzer et al., 1992)

Any potential increase in wave exposure in relation to sea-level rise (e.g. Fujii & Raffaelli, 2008) is not expected to impact this biotope, as these species occur on medium to very fine sand in moderately exposed to exposed areas (JNCC, 2019), therefore an increase in exposure is unlikely to change habitat classification.  However, as wave action is reduced with depth, an increase in depth may stabilize the sediment allowing the habitat to transition into IMuSaFfabMag, resulting in loss of the deeper portions of the biotope. However, over time the biotope may extend inshore, depending on location. Sensitivity assessment. There is likely to be considerable variation between sites, and the depth range occupied by the biotope.  Hence, it is difficult to assess the effect of the different sea-level rise scenarios.  As the biotope can occur from 0-10 m in depth, it is assumed that a sea-level rise of 50 cm, or 70 cm (middle to high emission scenarios) would have limited effect but that a 107 cm rise (the extreme scenario) might result in loss of part of the deeper extent of the biotope in some sites.  Therefore, resistance is assessed as ‘High’ under the middle and high emission scenarios so that resilience is ‘High’ and sensitivity assessed as ‘Not sensitive’.  But resistance is possibly ‘Medium’ under the extreme scenario, so that resilience is ‘Very low’ and sensitivity assessed as ‘Medium’, albeit with ‘Low’ confidence.

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
Low
Low
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Sea level rise (middle) [Show more]

Sea level rise (middle)

Middle emission scenario benchmark: a 50 cm rise in average UK sea-level rise by the end of this century (2081-2100). Further detail.

Evidence

Sea-level rise is occurring through a combination of thermal expansion and ice melt.  Sea levels have risen 1-3 mm/yr in the last century (Cazenave & Nerem, 2004, Church et al., 2004, Church & White, 2006). The most recent projections on sea-level rise suggest a rise of 50 cm under the middle emission scenario, 70 cm under the high emission scenario, and 107 cm under the extreme scenario. Species from the genus Bathyporeia and Nephtys cirrosa are abundant at on the Dogger Bank, which has a depth range of 15- 36 m (Wieking & Kröncke, 2003), suggesting that, as long as the habitat remains the same (sand), these species will be tolerant of future sea-level rise for all three scenarios. Nephtys cirrosa occurs on clean sand, down to a depth of 45 m (Rainer, 1991), whilst species of Bathyporeia are often abundant at depths <30 m (Künitzer et al., 1992)

Any potential increase in wave exposure in relation to sea-level rise (e.g. Fujii & Raffaelli, 2008) is not expected to impact this biotope, as these species occur on medium to very fine sand in moderately exposed to exposed areas (JNCC, 2019), therefore an increase in exposure is unlikely to change habitat classification.  However, as wave action is reduced with depth, an increase in depth may stabilize the sediment allowing the habitat to transition into IMuSaFfabMag, resulting in loss of the deeper portions of the biotope. However, over time the biotope may extend inshore, depending on location. Sensitivity assessment. There is likely to be considerable variation between sites, and the depth range occupied by the biotope.  Hence, it is difficult to assess the effect of the different sea-level rise scenarios.  As the biotope can occur from 0-10 m in depth, it is assumed that a sea-level rise of 50 cm, or 70 cm (middle to high emission scenarios) would have limited effect but that a 107 cm rise (the extreme scenario) might result in loss of part of the deeper extent of the biotope in some sites.  Therefore, resistance is assessed as ‘High’ under the middle and high emission scenarios so that resilience is ‘High’ and sensitivity assessed as ‘Not sensitive’.  But resistance is possibly ‘Medium’ under the extreme scenario, so that resilience is ‘Very low’ and sensitivity assessed as ‘Medium’, albeit with ‘Low’ confidence.

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
Low
Low
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Hydrological Pressures

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ResistanceResilienceSensitivity
Temperature increase (local) [Show more]

Temperature increase (local)

Benchmark. A 5°C increase in temperature for one month, or 2°C for one year. Further detail

Evidence

The amphipods that occur within this habitat are mobile and can avoid unfavourable conditions to some extent. Bathyporeia life cycles vary between locations and this is related to temperature (Mettam, 1989). Preece (1971) tested temperature tolerances of Bathyporeia pelagica and Bathyporeia pilosa in the laboratory.  Individuals acclimated to 15oC for 24 hours were exposed to temperature increases (water temperature raised by 0.2oC/minute). As test  temperature were reached individuals were removed, placed in seawater at 4oC and allowed to recover for 24 hours at which point mortalities were tested. Amphipods were also allowed to bury into sediments and held at test temperatures for 24 hours of 32.5oC, 31.8oC and 29.5oC before being allowed to recover in fresh seawater at 15oC for a further 24 hours, before mortalities were assessed. Upper lethal temperatures (the temperature at which 50% of individuals died for adult males and gravid females of Bathyporeia pilosa were 37.5oC and 39.4oC, respectively. Bathyporeia pelagica exhibited lower tolerances and adult males and gravid females had upper lethal temperature tolerances of 33.4 and 34.2oC respectively. These tests measures short-term exposure only and species had lower tolerance for longer-term (24 hour exposure).  No mortality occurred for Bathyporeia pilosa individuals held at 29.5oC and 30.8oC; however 15% of individuals exposed to water temperatures of 31.8oC and 96% at 32.5oC died. Bathyporeia pelagica exhibited lower tolerances, 11% of individuals died after 24 hr exposure to 29.5oC and 100% mortality occurred at 30.8oC and above (Preece, 1971).

Emery et al. (1957) reported that Nephtys spp. could withstand summer temperatures of 30-35°C so is likely to withstand the benchmark acute temperature increase. An acute increase in temperature at the benchmark level may result in physiological stress endured by the infaunal species but is unlikely to lead to mortality.

Sensitivity assessment. Typical surface water temperatures around the UK coast vary seasonally from 4-19 oC (Huthnance, 2010).  A chronic increase in temperature throughout the year of 2oC may fall within the normal temperature variation and an acute increase in water temperatures from 19 to 24oC for a month may be tolerated by the characterizing species supported by deeper burrowing and/or migration. For Bathyporeia spp. temperature increases above 30oC appear to be critical based on Preece (1971). Biotope resistance is therefore assessed as ‘High’ and resilience as ‘High’ so that the biotope is assessed as ‘Not sensitive’. Increased water and air temperatures and desiccation may lead to greater synergistic effects and the loss of characterizing amphipods and isopods may result in shifts between the variant sub-biotopes. 

High
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Medium
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High
High
High
High
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Not sensitive
High
Medium
Low
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Temperature decrease (local) [Show more]

Temperature decrease (local)

Benchmark. A 5°C decrease in temperature for one month, or 2°C for one year. Further detail

Evidence

Crisp (1964) reported that species of amphipod and isopods seemed to be unharmed by the severe winter of 1962-1963. This may be due to burial in sediments buffering temperature or seasonal migration to deeper waters to avoid freezing. 

Preece (1971) tested the temperature tolerances of Bathyporeia pelagica and Bathyporeia pilosa in the laboratory.  Individuals acclimated to 15oC for 24 hours were placed in a freezer in wet sediment. As test temperatures were reached individuals were removed and allowed to recover for 24 hours at which point mortalities were tested. Amphipods were also allowed to bury into sediments and held at test temperatures of -1oc, -3oC and -5oC for 24 hours before being allowed to recover in fresh seawater at 15oC for a further 24 hours before mortalities were assessed. Lower lethal short-term tolerances of Bathyporeia pilosa and Bathyporeia pelagica were -13.6oC and -6.4oC respectively.  Sensitivity to longer-term exposure is greater, especially for Bathyporeia pelagica. Bathyporeia pilosa individuals could withstand temperatures as low as -1oC for 24 hours, while 42% of Bathyporeia pelagica died. At -3oC 5% of Bathyporeia pilosa died (100% of Bathyporeia pelagica) but this rose to 82% at -5oC.

Nephtys cirrosa reaches its northern limit in Scotland, and German Bight of the North Sea. A decrease in temperature is likely to result in loss of the species from the SS.SSa.SSaVS biotope in Scotland.

Sensitivity assessment. Typical surface water temperatures around the UK coast vary seasonally from 4-19 oC (Huthnance, 2010).  A chronic decrease in temperature throughout the year of 2oC may fall within the normal temperature variation but an acute decrease in water temperatures from 4oC to -1oC at the coldest part of the year may lead to freezing and lethal effects on for a month may be tolerated by the characterizing species supported by deeper burrowing and/or migration to deeper waters. For Bathyporeia spp. seawater temperature decreases below -1oC appear to be critical based on Preece (1971). Biotope resistance is therefore assessed as ‘Medium’ and resilience as ‘High’ so that biotope sensitivity is assessed as 'Low'.

High
High
High
High
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High
High
High
High
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Not sensitive
High
High
High
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Salinity increase (local) [Show more]

Salinity increase (local)

Benchmark. A increase in one MNCR salinity category above the usual range of the biotope or habitat. Further detail

Evidence

This biotope is found in full salinity (30-35 ppt) habitats (JNCC, 2015), a change at the pressure benchmark is therefore assessed as a change to hypersaline conditions. Little evidence was found to assess responses to hypersalinity. However, monitoring at a Spanish desalination facility where discharges close to the outfall reached a salinity of 53, found that amphipods were sensitive to the increased salinity and that species free-living in the sediment were most sensitive. The study area did not host any of the species characterizing this biotope but the results indicate a general sensitivity (De-la-Ossa-Carretero, et al., 2016).

Sensitivity assessment.  Not assessed, ‘No evidence’.

No evidence (NEv)
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No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
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Salinity decrease (local) [Show more]

Salinity decrease (local)

Benchmark. A decrease in one MNCR salinity category above the usual range of the biotope or habitat. Further detail

Evidence

The biotope is found in full salinity habitats (JNCC, 2015). A change at the pressure benchmark refers to a decrease from full to variable (18-35 ppt), or to reduced salinity (18-30 ppt). Bathyporeia pelagica migrates seaward in response to reduced salinities, the effect of which is enhanced by higher temperature (Preece, 1970). Bathyporeia pilosa is, however, more tolerant of low salinities and is capable of reproducing at salinities as low as 2 (Khayrallah, 1977). Populations of Bathyporeia pilosa within the upper reaches of the Severn Estuary experience wide fluctuations in salinity ranging from 1-22 depending on the season and tidal cycle (Mettam, 1989). The physiological stress for this environment affects size and reproduction (Mettam, 1989). Speybroeck et al. (2008) noted that Bathyporeia pilosa tends to occur subtidally in estuarine and brackish conditions. Local populations may be acclimated to the prevailing salinity regime and may exhibit different tolerances to other populations subject to different salinity conditions and, therefore, caution should be used when inferring tolerances from populations in different regions.  

A reduction in salinity at the pressure benchmark could result in the loss of species or changes in abundance and biotope reversion to the biotope SS.SSa.SSaVS.MoSaVS which occurs in typical mobile sand conditions but in reduced salinities and lacks Nepthys cirrosa and Bathyporeia spp. (although these may be washed in from adjacent communities) (JNCC, 2015) or a change to SS.SSa.SSaVS.NcirLim, which occurs in variable salinity and contains the bivalve  Macoma balthica.

Sensitivity assessment. A decrease in salinity is likely to lead to changes in species abundance and richness and may lead to biotope reclassification. Biotope resistance is assessed as ‘None’ and resilience as ‘High’ (following restoration of typical habitat conditions). Sensitivity is therefore assessed as ‘Medium’. 

Medium
High
Medium
High
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High
High
Low
High
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Low
High
Low
High
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Water flow (tidal current) changes (local) [Show more]

Water flow (tidal current) changes (local)

Benchmark. A change in peak mean spring bed flow velocity of between 0.1 m/s to 0.2 m/s for more than one year. Further detail

Evidence

Water movement is a key factor physically structuring this biotope although exposure to wave action may be more significant for many examples than tidal streams. This biotope is recorded where tidal streams are weak (<0.5 m/s)or very weak (negligible) (JNCC, 2015), in areas where flows are lower, wave action may be more important in maintaining the sediment mobility that structures the biotope.  Where similar sand habitats occur in  more sheltered areas the biological structure alters in response to the increased or decreased sediment mobility with Magelona mirabilis found in higher abundances in more sheltered habitats and Chaetozone setosa found in more disturbed habitats (JNCC, 2015). An increase in disturbance may lead to biotope reversion to the similar biotope SS.SSa.IFiSa.IMoSa which occurs in more disturbed areas. A decrease in disturbance may lead to changes to SS.SSa.IMuSa.FfabMag, where finer sediments are deposited.

Sensitivity assessment. The sediments that characterize this biotope and sub-biotopes are mobile sands that range from medium to fine, a change at the pressure benchmark (increase or decrease) may lead to some changes in sediment sorting. Based on the range of water flows experienced, biotopes occurring in habitats at the middle of the range are considered to be 'Not sensitive' to an increase or decrease in flow at the pressure benchmark. Changes in water flow in areas sheltered from wave action could. however, lead to changes in biotope classification due to the increase in sediment stability.

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
Low
Low
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Emergence regime changes [Show more]

Emergence regime changes

Benchmark.  1) A change in the time covered or not covered by the sea for a period of ≥1 year or 2) an increase in relative sea level or decrease in high water level for ≥1 year. Further detail

Evidence

Not relevant to sublittoral biotopes.​

Not relevant (NR)
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Not relevant (NR)
NR
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Not relevant (NR)
NR
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NR
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Wave exposure changes (local) [Show more]

Wave exposure changes (local)

Benchmark. A change in near shore significant wave height of >3% but <5% for more than one year. Further detail

Evidence

Water movement is a key factor physically structuring this biotope, with sediment sorting and mobilisation by tidal streams and wave action modifying the sediments present and the level of disturbance. The assessed biotope is found in habitats that are exposed to sheltered from wave action (JNCC, 2015).

Sensitivity assessment. Wave action is a key factor structuring this biotope through sediment mobility.  As the biotope occurs across two wave exposure categories (JNCC, 2015) this is considered to indicate, by proxy, that a change in wave exposure at the pressure benchmark is less than the natural range of wave heights experienced.  Biotope resistance to this pressure is therefore assessed as ‘High’ and resilience as ‘High (by default) so that the biotope is considered to be ‘Not sensitive’ at the pressure benchmark. 

High
High
Medium
High
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High
High
High
High
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Not sensitive
High
Medium
High
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Chemical Pressures

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ResistanceResilienceSensitivity
Transition elements & organo-metal contamination [Show more]

Transition elements & organo-metal contamination

Benchmark. Exposure of marine species or habitat to one or more relevant contaminants via uncontrolled releases or incidental spills. Further detail

Evidence

This pressure is Not assessed but evidence is presented where available.

Levels of contaminants that exceed the pressure benchmark may cause impacts. For most metals, toxicity to crustaceans increases with decreased salinity and elevated temperature, therefore marine species living within their normal salinity range may be less susceptible to heavy metal pollution than those living in salinities near the lower limit of their salinity tolerance (McLusky et al., 1986). Jones (1973; 1975b) found that mercury (Hg) and copper (Cu) reacted synergistically with changes in salinity and increased temperature (10°C) to become increasingly toxic to species of isopod, including Eurydice pulchra.

Not Assessed (NA)
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Not assessed (NA)
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Not assessed (NA)
NR
NR
NR
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Hydrocarbon & PAH contamination [Show more]

Hydrocarbon & PAH contamination

Benchmark. Exposure of marine species or habitat to one or more relevant contaminants via uncontrolled releases or incidental spills. Further detail

Evidence

This pressure is Not assessed but evidence is presented where available.

Not Assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
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NR
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Synthetic compound contamination [Show more]

Synthetic compound contamination

Benchmark. Exposure of marine species or habitat to one or more relevant contaminants via uncontrolled releases or incidental spills. Further detail

Evidence

This pressure is Not assessed but evidence is presented where available.

In general, crustaceans are widely reported to be intolerant of synthetic chemicals (Cole et al., 1999) and intolerance to some specific chemicals has been observed in amphipods. Powell (1979) inferred from the known susceptibility of Crustacea to synthetic chemicals and other non-lethal effects, that there would probably also be a deleterious effect on isopod fauna as a direct result of chemical application. All were killed at about 10 ppm BP 1002 after 24 hours exposure, whilst at 5 ppm four out of five individuals survived when transferred to clean seawater.

Not Assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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Radionuclide contamination [Show more]

Radionuclide contamination

Benchmark. An increase in 10µGy/h above background levels. Further detail

Evidence

No evidence.

No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
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Introduction of other substances [Show more]

Introduction of other substances

Benchmark. Exposure of marine species or habitat to one or more relevant contaminants via uncontrolled releases or incidental spills. Further detail

Evidence

This pressure is Not assessed.

Not Assessed (NA)
NR
NR
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Not assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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De-oxygenation [Show more]

De-oxygenation

Benchmark. Exposure to dissolved oxygen concentration of less than or equal to 2 mg/l for one week (a change from WFD poor status to bad status). Further detail

Evidence

Information concerning the reduced oxygen tolerance of Nephtys cirrosa was not found but evidence (Alheit, 1978; Arndt & Schiedek, 1997; Fallesen & Jørgensen, 1991) indicated a similar species, Nephtys hombergii, to be very tolerant of episodic oxygen deficiency and at the benchmark duration of one week.

Laboratory studies by Khayrallah (1977) on Bathyporeia pilosa, indicated that it has a relatively poor resistance to conditions of hypoxia in comparison to other interstitial animals. However, Mettam (1989) and Sandberg (1997) suggest that Bathyporeia pilosa can survive short-term hypoxia.

Sensitivity assessment.  This biotope  is characterized by mobile sands in areas that experience strong water flows or are wave exposed. The mixing effect of wave action and water movement will limit the intensity and duration of exposure to deoxygenated waters. The species characterizing the biotope are also mobile and able to migrate vertically or shorewards to escape unsuitable conditions. Biotope resistance is therefore assessed as ‘High’ and resilience as ‘High’ (by default) so that the biotope is considered to be ‘Not sensitive’.

High
High
Medium
High
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High
High
High
High
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Not sensitive
High
Medium
High
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Nutrient enrichment [Show more]

Nutrient enrichment

Benchmark. Compliance with WFD criteria for good status. Further detail

Evidence

In-situ primary production is limited to microphytobenthos within and on sediments and the high levels of sediment mobility may limit the level of primary production as abrasion would be likely to damage diatoms (Delgado et al., 1991). The amphipods feed on epipsammic diatoms attached to the sand grains (Nicolaisen & Kanneworff, 1969). Both these groups may benefit from slight nutrient enrichment if this enhanced primary production. 

Sensitivity assessment.  Nutrient level is not a key factor structuring the biotope at the pressure benchmark. In general, however, primary production is low and this biotope is species poor and characterizing species may be present at low abundances (depending on sediment mobility). Biotope resistance is therefore assessed as ‘High’, resilience as ‘High’ (by default) and the biotope is considered to be ‘Not sensitive’.

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
Low
Low
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Organic enrichment [Show more]

Organic enrichment

Benchmark. A deposit of 100 gC/m2/yr. Further detail

Evidence

The biotope occurs in mobile sand sediments where wave action leads to particle sorting, in-situ primary production is restricted to microphytobenthos although sediment mobility may restrict production levels (Delgado et al., 1991). 

Sensitivity assessment.  At the pressure benchmark organic inputs are unlikely to significantly affect the structure of the biological assemblage or impact the physical habitat, due to remobilisation and transport by wave or currents. Biotope sensitivity is therefore assessed as ‘High’ and resilience as ‘High’ (by default) and the biotope is therefore considered to be ‘Not sensitive’.

High
High
High
High
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High
High
High
High
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Not sensitive
High
High
High
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Physical Pressures

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ResistanceResilienceSensitivity
Physical loss (to land or freshwater habitat) [Show more]

Physical loss (to land or freshwater habitat)

Benchmark. A permanent loss of existing saline habitat within the site. Further detail

Evidence

All marine habitats and benthic species are considered to have a resistance of ‘None’ to this pressure and to be unable to recover from a permanent loss of habitat (resilience is ‘Very Low’).  Sensitivity within the direct spatial footprint of this pressure is therefore ‘High’.  Although no specific evidence is described confidence in this assessment is ‘High’, due to the incontrovertible nature of this pressure.

None
High
High
High
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Very Low
High
High
High
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High
High
High
High
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Physical change (to another seabed type) [Show more]

Physical change (to another seabed type)

Benchmark. Permanent change from sedimentary or soft rock substrata to hard rock or artificial substrata or vice-versa. Further detail

Evidence

The biotope is characterized by the sedimentary habitat (JNCC, 2015), a change to an artificial or rock substratum would alter the character of the biotope leading to reclassification and the loss of the sedimentary community including the characterizing polychaetes and amphipods.

Sensitivity assessment. Based on the loss of the biotope, resistance is assessed as ‘None’, recovery is assessed as ‘Very low’ (as the change at the pressure benchmark is permanent and sensitivity is assessed as ‘High’.

None
High
High
High
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Very Low
High
High
High
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High
High
High
High
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Physical change (to another sediment type) [Show more]

Physical change (to another sediment type)

Benchmark. Permanent change in one Folk class (based on UK SeaMap simplified classification). Further detail

Evidence

The pressure benchmark refers to the simplified Folk classification developed by Long (2006) and the UK Marine Habitat Classification Littoral and Sublittoral Sediment Matrices (Connor et al., 2004). The biotope occurs on mobile sands, a change at the pressure benchmark refers to a change to sandy muds or muddy sands or to coarser gravel sediments. Experiments by Van Tomme et al. (2013) have shown that the optimal sedimentary habitats for some of he species that characterize this biotope vary slightly. Bathyporeia pilosa prefer the finest sediments, although at a subtidal dredge disposal site the change to a finer sediment led to a reduction in the abundance of Bathyporeia pilosa (Witt et al., 2004). Bathyporeia sarsi has a broader preference and also occurred in medium-coarse sediments (Van Tomme et al., 2013). 

Nepthys cirrosa occurs in fine to coarser sands, with greatest abundance in the Belgium part of the North Sea recorded in medium grain sizes (Degraer et al., 2006). A change to gravelly sand is unlikely to impact this species, however, a change to muddy sand may limit the species abundance as the species displays a slight preference for low mud content levels (< 10%) (Degraer et al., 2006).  

Sensitivity assessment. A change to either a finer muddy sediment or a coarser sediment, is likely to lead to changes in the abundance and identity of the characterizing species . Based on the loss of the biotope, resistance is assessed as ‘None’, recovery is assessed as ‘Very low’ (as the change at the pressure benchmark is permanent and sensitivity is assessed as ‘High’.

None
High
High
High
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Very Low
High
High
High
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High
High
High
High
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Habitat structure changes - removal of substratum (extraction) [Show more]

Habitat structure changes - removal of substratum (extraction)

Benchmark. The extraction of substratum to 30 cm (where substratum includes sediments and soft rock but excludes hard bedrock). Further detail

Evidence

Bathyporeia pelagica lives infaunally in the uppermost 3 cm of sandy substrata as does the isopod Eurydice pulchra (Fish, 1970). Extraction of the sediment to 30cm is likely to remove the characterizing polychaetes, amphipods and isopods within the footprint (although if disturbed some may be able to escape). 

Sensitivity assessment. Biotope resistance to extraction of sediment and characterizing species is assessed as ‘None. Resilience is assessed as ‘High’, as sediment recovery will be enhanced by wave action and mobility of sand. The characterizing species are likely to recover through transport of adults in the water column or migration from adjacent patches. Biotope sensitivity is therefore assessed as ‘Medium’.

None
High
High
High
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High
High
High
High
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Medium
High
High
High
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Abrasion / disturbance of the surface of the substratum or seabed [Show more]

Abrasion / disturbance of the surface of the substratum or seabed

Benchmark. Damage to surface features (e.g. species and physical structures within the habitat). Further detail

Evidence

This biotope group is present in mobile sands, the associated species are generally present in low abundances and adapted to frequent disturbance suggesting that resistance to surface abrasion would be high. The amphipod and isopod species present are agile swimmers and are characterized by their ability to withstand sediment disturbance (Elliott et al. 1998). Similarly, the polychaete Nephtys cirrosa is adapted to life in unstable sediments and lives within the sediment. This characteristic is likely to protect this species from surface abrasion.

Comparisons between shores with low and high levels of trampling found that the amphipod Bathyporeia pelagica is sensitive to abrasion and compaction from human trampling, other species including Pontocrates arenarius and the isopod Eurydice affinis also decreased in response to trampling but Bathyporeia pelagica appeared to be the most sensitive  (Reyes-Martínez et al., 2015).  

Sensitivity assessment. Resistance to a single abrasion event is assessed as ‘Low’ based on the evidence for trampling from Reyes-Martínez et al. (2015). Resilience is assessed as ‘High’, based on migration from adjacent populations and in-situ reproduction by surviving amphipods.  Sensitivity is therefore assessed as ‘Low’. This assessment may underestimate sensitivity to high-levels of abrasion (repeated events within a short period). The trampling evidence and the evidence for penetration from mobile gears (see below) differ in the severity (resistance) of impact. This may be due to different levels of intensity (multiple trampling/abrasion events vs single penetration/towed gear impacts) or the nature of the pressure. Abrasion from trampling also involves a level of compaction that could collapse burrows and damage species through compression. Penetration may, however, break sediments open allowing mobile species to escape or species may be pushed forwards from towed gear by a pressure wave where this is deployed subtidally (Gilkinson et al., 1998). Both risk assessments are considered applicable to single events based on the evidence and the sensitivity assessment for both pressures is the same although resistance differs. 

Low
High
High
High
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High
High
Low
High
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Low
High
Low
High
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Penetration or disturbance of the substratum subsurface [Show more]

Penetration or disturbance of the substratum subsurface

Benchmark. Damage to sub-surface features (e.g. species and physical structures within the habitat). Further detail

Evidence

This biotope group is present in mobile sands, the associated species are generally present in low abundances and adapted to frequent disturbance suggesting that resistance to abrasion and penetration and disturbance of the sediment would be high. The amphipod  species present are agile swimmers and are characterized by their ability to withstand sediment disturbance (Elliott et al., 1998).

Bergman and Santbrink (2000) found that direct mortality of gammarid amphipods, following a single passage of a beam trawl (in silty sediments where penetration is greater) was 28%. Similar results were reported from experiments in shallow, wave disturbed areas, using a toothed, clam dredge. Bathyporeia spp. experienced a reduction of 25% abundance in samples immediately after intense clam dredging, abundance recovered after 1 day (Constantino et al. 2009). Experimental hydraulic dredging for razor clams resulted in  no statistically significant differences in Bathyporeia elegans abundances between treatments after 1 or 40 days (Hall et al., 1990), suggesting that recovery from effects was very rapid. Ferns et al. (2000) examined the effects of a tractor-towed cockle harvester on benthic invertebrates and predators in intertidal plots of muddy and clean sand. Harvesting resulted in the loss of a significant proportion of the most common invertebrates from both areas. In the muddy sand, the population of Bathyporeia pilosa remained significantly depleted for more than 50 days, whilst the population in clean sand recovered more quickly. These results agree with other experimental studies that clean sands tend to recover more quickly that other habitat types with higher proportions of fine sediment (Dernie et al., 2003).

Sensitivity assessment. Based on the evidence above it is considered that Bathyporeia spp. and other characterizing species will have ‘Medium’ resistance (mortality <25%) to abrasion, their small size, infaunal position and mobility enabling a large proportion of the population to escape injury. Recovery is assessed as ‘High’ and sensitivity is therefore categorised as ‘Low’.The trampling evidence (see above) and the evidence for penetration from mobile gears  differ in the severity (resistance) of impact. This may be due to different levels of intensity (multiple trampling/abrasion events vs single penetration/towed gear impacts) or the nature of the pressure. Abrasion from trampling also involves a level of compaction that could collapse burrows and damage species through compression. Penetration may, however, break sediments open allowing mobile species to escape or species may be pushed forwards from towed gear by a pressure wave where this is deployed subtidally (Gilkinson et al., 1998). 

Medium
High
High
High
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High
High
High
High
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Low
High
High
High
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Changes in suspended solids (water clarity) [Show more]

Changes in suspended solids (water clarity)

Benchmark. A change in one rank on the WFD (Water Framework Directive) scale e.g. from clear to intermediate for one year. Further detail

Evidence

The characterizing species live within the sand and are unlikely to be directly affected by an increased concentration of suspended matter in the water column. Within the mobile sands habitat storm events or spring tides may re-suspend or transport large amounts of material and therefore species are considered to be adapted to varying levels of suspended solids.

 Bathyporeia spp. feed on diatoms within the sand grains (Nicolaisen & Kanneworff, 1969), an increase in suspended solids that reduced light penetration could alter food supply. However, diatoms are able to photosynthesise while the tide is out and therefore a reduction in light during tidal inundation may not affect this food source , depending on the timing of the tidal cycle.

Amphipods may be regular swimmers within the surf plankton, where the concentration of suspended particles would be expected to be higher (Fincham, 1970a). Furthermore, during the winter, when Bathyporeia pelagica extends its distribution into the mouths of estuaries the species may encounter concentrations of suspended sediment measurable in grams per litre (benchmark is mg/l) (Cole et al. 1999).  

Sensitivity assessment. Increased inorganic suspended solids may increase abrasion but it is likely that the infaunal species would be unaffected. The biotope is considered to be ‘Not sensitive’ to a decrease in suspended solids that does not affect sediment transport and supply to the biotope. Biotope resistance is assessed as ‘Medium’ as some effects on feeding and diatom productivity may occur from increases in suspended solids, resilience is assessed as ‘High’, following a return to usual conditions and sensitivity is assessed as ‘Low’. This more precautionary assessment is presented in the table.  Indirect effects such as deposition, erosion and associated sediment change that may result from changes in suspended solids in the long-term are assessed separately. 

Medium
Low
NR
NR
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High
High
High
High
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Low
Low
Low
Low
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Smothering and siltation rate changes (light) [Show more]

Smothering and siltation rate changes (light)

Benchmark. ‘Light’ deposition of up to 5 cm of fine material added to the seabed in a single discrete event. Further detail

Evidence

Evidence for the effects of siltation by thick layers of added sediment from beach nourishment is described for the heavy deposition pressure below. The pressure benchmark for light deposition refers to the addition of a relatively thin layer of deposits in a single event.  Species adapted to coarse sediments may not be able to burrow through fine sediments, or experienced reduced burrowing ability. For example, Bijkerk (1988, results cited from Essink, 1999) found that the maximal overburden through which Bathyporeia could migrate was approximately 20 cm in mud and 40 cm in sand.  No further information was available on the rates of survivorship or the time taken to reach the surface.

Sensitivity assessment.  As the biotope is associated with wave exposed habitats or those with strong currents, some sediment removal will occur, mitigating the effect of deposition. The mobile polychaete Nephtys cirrosa and amphipods are likely to be able to burrow through a 5cm layer of fine sediments. Biotope resistance is therefore assessed as ‘High’ and resilience as ‘High’ (by default). The biotope is therefore considered to be ‘Not sensitive’ to this pressure.  Repeated deposits or deposits over a large area or in sheltered systems that were shifted by wave and tidal action may result in sediment change (see physical change pressure).

High
High
Medium
High
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High
High
High
High
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Not sensitive
High
Medium
High
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Smothering and siltation rate changes (heavy) [Show more]

Smothering and siltation rate changes (heavy)

Benchmark. ‘Heavy’ deposition of up to 30 cm of fine material added to the seabed in a single discrete event. Further detail

Evidence

Studies have found that beach ‘replenishment’ or ‘nourishment’ that involves the addition of sediments on beaches can have a number of impacts on the infauna (Peterson et al., 2000, Peterson et al., 2006). Impacts are more severe when the sediment added differs significantly in grain size or organic content (Nelson et al., 1989, Peterson et al., 2000).  For example, Maurer et al. (1981) found that the amphipod Parahaustorius longimerus which occurs intertidally in clean, well-sorted sands and is an active, effective burrower was able to regain the surface after being buried by sand far more easily than when buried under silt/clay mixtures.

A thick layer of sediment has a smothering effect and in most instances buried species will die although some polychaetes can escape up to 90cm of burial In response to nourishment (Speybroek et al., 2007, references therein). Peterson et al. (2000) found that the dominant macrofauna were reduced by 86-99% 5-10 weeks after the addition of sediment that was finer than the original sediments but with a high shell content.

Little empirical information was found for the ability of characterizing species to reach the surface after burial. Bijkerk (1988, results cited from Essink, 1999) found that the maximal overburden through which Bathyporeia could migrate was approximately 20 cm in mud and 40 cm in sand.  No further information was available on the rates of survivorship or the time taken to reach the surface and no information was available for other characterizing species.

Leewis et al. (2012) investigated the recovery of  Bathyporeia sarsi, following beach nourishment by comparing beaches that had been exposed at different times. The lengths of beach nourished varied from 0.5 kn to > 7 km.  Recovery to original abundances appeared to occur within one year for the characterizing species which were in agreement with other studies (Leewis et al., 2012 and references therein).  

Repeated events are not considered at the pressure benchmark but it is noted that annual beach nourishment can alter beach sediments (see physical change pressure) and result in suppression of macroinvertebrate populations (Manning et al., 2014).

Sensitivity assessment. The thickness of sediment applied during beach nourishment is likely to exceed the 30cm pressure benchmark but the results from studies on the activity are informative, particularly with regard to recovery rate. Sediment removal by wave action could mitigate the level of effect but overall smothering by fine sediments is likely to result in mortality of characterizing amphipods and isopods and possibly Nephtys cirrosa. Biotope resistance is therefore assessed as ‘Low’ and resilience as High (based on Leewis et al., 2012), biotope sensitivity is therefore assessed as ‘Low’.

Low
High
Medium
High
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High
High
High
High
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Low
High
Medium
High
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Litter [Show more]

Litter

Benchmark. The introduction of man-made objects able to cause physical harm (surface, water column, seafloor or strandline). Further detail

Evidence

This pressure is not assessed. Amphipods may also consume microplastics although no negative effects have been documented. Ugolini et al. ( 2013) found that Talitrus saltator could consume polyethylene microspheres.  Most microspheres were expelled in 24 h. and were totally expelled in one week. microsphere ingestion on the survival capacity in the laboratory. Analyses carried out on faeces of freshly collected individuals revealed the presence of polyethylene and polypropylene, confirming that microplastic debris could be swallowed by Talitrus saltator in natural conditions. The talitrid Orchestia gammarellus has also been recorded as ingesting microplastics in the size range 20-200µm (Thompson et al., 2004).

Not Assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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Not assessed (NA)
NR
NR
NR
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Electromagnetic changes [Show more]

Electromagnetic changes

Benchmark. A local electric field of 1 V/m or a local magnetic field of 10 µT. Further detail

Evidence

No evidence for the characterizing species was found to assess this pressure. For some amphipods there is evidence for geomagnetic orientation being inhibited or disrupted by the presence of electromagnetic fields or by changing magnetic fields. Arendse & Barendregt (1981) manipulated magnetic fields to alter orientation of the talitrid amphipod Orchestia cavimana

Deep-water amphipods Gondogenia arctica have been shown to be sensitive to even weak electromagnetic fields which cancel magnetic orientation (Tomanova & Vacha, 2016). Loss of orientation was observed at a radiofrequency electromagnetic field of 2 nT (0.002  µT) (Tomanova & Vacha, 2016).

No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
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Underwater noise changes [Show more]

Underwater noise changes

Benchmark. MSFD indicator levels (SEL or peak SPL) exceeded for 20% of days in a calendar year. Further detail

Evidence

Not relevant.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Introduction of light or shading [Show more]

Introduction of light or shading

Benchmark. A change in incident light via anthropogenic means. Further detail

Evidence

As this feature is not characterized by the presence of primary producers it is not considered that shading would alter the character of the habitat. No specific evidence was found to assess the sensitivity of the characterizing species to this pressure. Changes in light level may, however, affect activity rhythms of the invertebrates. Amphipods within the biotope prefer shade and therefore an increase in light may inhibit activity, particularly at night when they emerge from the sediment and are most active (Jelassi et al., 2015; Ayari, 2015). Hartwick (1976) found that artificial lighting interfered with learning or orientation cues by Talitrids.  

Orientation by light has been well studied for intertidal amphipods (particularly Talitrus saltator). Intertidal amphipods orientate themselves by a range of factors that include (but are not limited to) visual cues based on solar or astronomic cues such as the moon and the geomagnetic field (Scapini, 2014). Activity patterns are also linked to internal biological clocks that respond to diel, tidal, lunar and seasonal cycles, so that animals are active during the most suitable time of day or night (Scapini, 2014).  The introduction of light or an increase in shading could, therefore, alter behavioural patterns and navigation.

Changes in light and level of shade may indirectly affect the characterizing Bathyporeia spp. through changes in  behaviour and food supply via photosynthesis of diatoms within sediments. Benthic microalgae play a significant role in system productivity and trophic dynamics, as well as habitat characteristics such as sediment stability (Tait & Dipper, 1998). Shading could prevent photosynthesis leading to death or migration of sediment diatoms altering sediment cohesion and food supply to the grazing amphipods.

Sensitivity assessment. Changes in light are not considered to directly affect the biotope however, some changes in behaviour or food supply for Bathyporeia spp could result. Sensitivity is assessed as ‘Medium’ and resilience is assessed as ’High’. Biotope sensitivity is, therefore, assessed as ‘Low’.

Medium
High
Low
Low
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High
High
Low
High
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Low
High
Low
Low
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Barrier to species movement [Show more]

Barrier to species movement

Benchmark. A permanent or temporary barrier to species movement over ≥50% of water body width or a 10% change in tidal excursion. Further detail

Evidence

As the amphipods and isopods that characterize this biotope have benthic dispersal strategies (via brooding), water transport is not a key method of dispersal over wide distances, as it is for some marine invertebrates that produce pelagic larvae such as the characterizing Nephtys cirrosa.  Barriers that limit tidal excursion and flushing may reduce connectivity or help to retain larvae.

Sensitivity assessment. The biotope (based on the biological assemblage) is considered to have ‘High’ resistance to the presence of barriers that lead to a reduction in tidal excursion, resilience is assessed as ‘High’ (by default) and the biotope is considered to be ‘Not sensitive’.

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
Low
Low
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Death or injury by collision [Show more]

Death or injury by collision

Benchmark. Injury or mortality from collisions of biota with both static or moving structures due to 0.1% of tidal volume on an average tide, passing through an artificial structure. Further detail

Evidence

Not relevant’ to seabed habitats.  NB. Collision by grounding vessels is addressed under ‘surface abrasion.

Not relevant (NR)
NR
NR
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Not relevant (NR)
NR
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Not relevant (NR)
NR
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Visual disturbance [Show more]

Visual disturbance

Benchmark. The daily duration of transient visual cues exceeds 10% of the period of site occupancy by the feature. Further detail

Evidence

The characterizing species are likely to be able to detect light and some movement but are unlikely to have any visual acuity and are considered to not be sensitive to this factor. The amphipods emerge from the sediments at night and are unlikely to be disturbed although like many species they may flee from movements.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Biological Pressures

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ResistanceResilienceSensitivity
Genetic modification & translocation of indigenous species [Show more]

Genetic modification & translocation of indigenous species

Benchmark. Translocation of indigenous species or the introduction of genetically modified or genetically different populations of indigenous species that may result in changes in the genetic structure of local populations, hybridization, or change in community structure. Further detail

Evidence

Key characterizing species within this biotope are not cultivated or translocated. This pressure is therefore considered ‘Not relevant’ to this biotope group.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Introduction or spread of invasive non-indigenous species [Show more]

Introduction or spread of invasive non-indigenous species

Benchmark. The introduction of one or more invasive non-indigenous species (INIS). Further detail

Evidence

The American slipper limpet Crepidula fornicata was introduced to the UK and Europe in the 1870s from the Atlantic coasts of North America with imports of the eastern oyster Crassostrea virginica. It was recorded in Liverpool in 1870 and the Essex coast in 1887-1890. It has spread through expansion and introductions along the full extent of the English Channel and into the European mainland (Blanchard, 1997, 2009; Bohn et al., 2012, 2013a, 2013b, 2015; De Montaudouin et al., 2018; Helmer et al., 2019; Hinz et al., 2011; McNeill et al., 2010; Powell-Jennings & Calloway, 2018; Preston et al., 2020; Stiger-Pouvreau & Thouzeau, 2015).

Crepidula fornicata is recorded from shallow, sheltered bays, lagoons and estuaries or the sheltered sides of islands, in variable salinity (18 to 40) although it prefers ca 30 (Tillin et al., 2020). Larvae require hard substrata for settlement. It prefers muddy gravelly, shell-rich, substrata that include gravel, or shells of other Crepidula, or other species e.g., oysters, and mussels. It is highly gregarious and seeks out adult shells for settlement, forming characteristic ‘stacks’ of adults. But it also recorded in a wide variety of habitats including clean sands, artificial substrata, Sabellaria alveolata reefs and areas subject to moderately strong tidal streams (Blanchard, 1997, 2009; Bohn et al., 2012, 2013a, 2013b, 2015; De Montaudouin et al., 2018; Hinz et al., 2011; Powell-Jennings & Calloway, 2018; Preston et al., 2020; Stiger-Pouvreau & Thouzeau, 2015; Tillin et al., 2020).

The availability of hard substrata (e.g., gravel) may only restrict initial colonization as higher densities of Crepidula function as substrata for subsequent colonization (Thieltges et al., 2004; Blanchard, 2009). However, Bohn et al. (2015) noted that Crepidula occurred at low density or was absent in areas of homogenous fine sediment and areas dominated by boulders. Bohn et al. (2015) suggested that wave action (exposure) probably prevented the establishment of large numbers of Crepidula in high-energy areas. Blanchard (2009) noted that sandy areas in the Bay of Saint-Mont Michel were not colonized by Crepidula because of surface sand mobility. Thieltges et al. (2003) also noted that storm events removed some clumps of mussels and presumably Crepidula onto tidal flats where they disappeared, which caused their abundance to fluctuate. Similarly, Crepidula was absent from sandy substrata in Swansea Bay but was most abundant in the shelter of the breakwater at the Swansea east site (Powell-Jennings & Calloway, 2018). Powell-Jennings & Calloway (2018) noted that Crepidula is killed by sudden burial and possibly burial due to deposition, which could mitigate Crepidula density.

The North American amphipod Gammarus tigrinus was detected in the north-eastern Baltic Sea in 2003 and has rapidly expanded into European waters since (Jänes et al., 2015).  Native gammarids, such as Gammarus salinus have almost disappeared from some habitats of the northeastern Baltic Sea and the competition for space between the invasive Gammarus tigrinus the native Gammarus salinus has been a contributing factor in certain habitats (Kotta et al., 2011). Competition for space alone did not explain the mass disappearance of Gammarus salinus as Gammarus tigrinus did not out-compete Gammarus salinus in all Baltic Sea habitats, limiting confidence in the evidence. However, Gammarus tigrinus has been identified in many UK estuaries and coasts and appears likely to influence species composition in the biotope (NBN Gateway 2016). This species prefers lower salinities and is typical of brackish waters (Kotta et al., 2013) and is therefore not considered a threat to this biotope where salinities are unaltered from the usual full salinity conditions.

Sensitivity assessment. The sediments characterizing this biotope are mobile and frequent disturbance limits the establishment of marine and coastal invasive non-indigenous species. The habitat conditions are unsuitable for most species, including Crepidula fornicata, which is unlikely to become established due to the mobility of the sediment. The unsuitable habitat conditions are exemplified by the low species richness characterizing this biotope. Therefore, this biotope is considered to have 'High' resistance to this pressure and 'High' resilience (by default) and is assessed as 'Not sensitive' to this pressure. 

High
Low
NR
NR
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High
High
High
High
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Not sensitive
Low
NR
NR
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Introduction of microbial pathogens [Show more]

Introduction of microbial pathogens

Benchmark. The introduction of relevant microbial pathogens or metazoan disease vectors to an area where they are currently not present (e.g. Martelia refringens and Bonamia, Avian influenza virus, viral Haemorrhagic Septicaemia virus). Further detail

Evidence

 Amphipods may also be infected by a number of parasites or pathogens that alter population numbers through changes in host condition, growth, behaviour and reproduction (Green Extabe & Ford, 2014). Infection by acanthocephalan larvae, for example, may alter behaviour and responses of gammarid amphipods (Bethel & Holmes, 1977). 

No evidence was found for pathogen/parasite outbreaks that may result in mass-mortalities in the characterizing species and this pressure is not assessed.

No evidence (NEv)
NR
NR
NR
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No evidence (NEv)
NR
NR
NR
Help
No evidence (NEv)
NR
NR
NR
Help
Removal of target species [Show more]

Removal of target species

Benchmark. Removal of species targeted by fishery, shellfishery or harvesting at a commercial or recreational scale. Further detail

Evidence

Intertidal populations of Nepthys cirrosa may be targeted by bait diggers.  There is limited information on the effect of digging directly on Nephtys cirrosa populations, however there is evidence on effects on another Nephtys species: Nephtys hombergii. Nephtys hombergii is directly removed through commercial bait digging and by recreational anglers and abundance significantly decreased in areas of the Solent, UK, where bait digging (primarily for Nereis virens) had occurred (Watson et al. 2007). Recovery of Nephtys hombergii has been assessed to be very high as re-population would occur initially relatively rapidly via adult migration and later by larval recruitment. Dittman et al. (1999) observed that Nephtys hombergii was amongst the macrofauna that colonized experimentally disturbed tidal flats within two weeks of the disturbance that caused defaunation of the sediment. However, if sediment is damaged recovery is likely to be slower, for instance Nephtys hombergii abundance was reduced by 50% in areas where tractor towed cockle harvesting was undertaken on experimental plots in Burry inlet, south Wales, and had not recovered after 86 days (Ferns et al., 2000).

Sensitivity assessment. Although Nephtys cirrosa may be targeted by bait differs where this species occurs intertidally, subtidal populations are not considered to be impacted unless there was a change in emergence regime. This pressure is, therefore considered to be 'Not relevant' to the assessed biotope.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
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Removal of non-target species [Show more]

Removal of non-target species

Benchmark. Removal of features or incidental non-targeted catch (by-catch) through targeted fishery, shellfishery or harvesting at a commercial or recreational scale. Further detail

Evidence

The loss of the key characterizing species through unintentional removal would alter the character of the biotope. The ecosystem services such as secondary production and food for higher trophic levels would be lost. The polychaete Nephtys cirrosa and the amphipods are predated on by flat fish and other invertebrate predators during tidal inundation (Speybroeck et al., 2007; Van Tomme et al., 2014).

Sensitivity assessment. Biotope resistance to loss of the characterizing species is assessed as ‘Low’ as the burrowing lifestyle and mobility of species mean that a proportion of the population may escape incidental removal. Resilience is assessed as ‘High’ based on in-situ recovery and migration from adjacent populations and sensitivity is therefore assessed as ‘Low’. Despite the loss of a high proportion of the characterizing species  the biotope would still be classified as belonging to the LS.LSa.MoSa group as some examples, particularly those that are very exposed to wave action, contain few species at low abundance (JNCC, 2015).

Low
Low
NR
NR
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High
High
High
High
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Low
Low
Low
Low
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Citation

This review can be cited as:

Tillin, H.M., Garrard, S.L.,, Lloyd, K.A., & Watson, A., 2023. Nephtys cirrosa and Bathyporeia spp. in infralittoral sand. In Tyler-Walters H. and Hiscock K. (eds) Marine Life Information Network: Biology and Sensitivity Key Information Reviews, [on-line]. Plymouth: Marine Biological Association of the United Kingdom. [cited 08-10-2024]. Available from: https://marlin.ac.uk/habitat/detail/154

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Last Updated: 08/11/2023