Mixed turf of hydroids and large ascidians with Swiftia pallida and Caryophyllia (Caryophyllia) smithii on weakly tide-swept circalittoral rock

Summary

UK and Ireland classification

Description

This biotope typically occurs from exposed through to sheltered circalittoral bedrock or boulders subject to moderately strong to weak tidal streams. It is found in water depths ranging from 4 m to 37 m. This biotope is distinguished by frequently occurring Swiftia pallida and Caryophyllia smithii and a diverse range of ascidians including Clavelina lepadiformis, Ascidia mentula, Polycarpa pomaria, Diazona violacea and Corella parallelogramma. A sparse, yet diverse hydroid turf is often apparent, with species such as Aglaophenia tubulifera, Nemertesia antennina, Polyplumaria frutescens, Halecium halecinum, Abietinaria abietina, Nemertesia ramosa and Halopteris catharina often recorded. Spaces amongst the turf are usually colonised by the polychaete Spirobranchus triqueter and encrusting red algae. Crinoids such as Antedon petasus, Antedon bifida and Leptometra celtica may be seen filter feeding on the tops of outcrops and boulders, along with the soft coral Alcyonium digitatum. Other echinoderms such as Echinus esculentus, Crossaster papposus and Asterias rubens may also be recorded. There may also be a bryozoan component to the sparse faunal turf. Species such as Securiflustra securifrons and Eucratea loricata as well as the crustose Parasmittina trispinosa are all usually present. There may be a few isolated growths of sponge, such as Iophonopsis nigricans, Axinella infundibuliformis and Haliclona urceolus. Other species that may be present include the brachiopod Terebratulina retusa and the top shell Calliostoma zizyphinum. The crustacean Munida rugosa may be visible in crevices. Kelp forests and parks are typically found above this biotope, in the infralittoral, with Saccharina latissima and Laminaria hyperborea. This biotope is found in Scottish sealochs and, in the most sheltered situations, may graduate into NeoPro at greater depths. All records are from the west coast of Scotland (east coast of Lewis /Outer Hebrides). (Information from Connor et al., 2004; JNCC, 2015). 

Depth range

10-20 m, 20-30 m, 30-50 m

Additional information

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Sensitivity reviewHow is sensitivity assessed?

Sensitivity characteristics of the habitat and relevant characteristic species

CR.HCR.XFa.SwiLgAs is similar to the CR.MCR.EcCr.CarSwi biotope complex as they are characterized by dense aggregations of the cup coral Caryophyllia smithii and the northern sea fan Swiftia pallida on rock or boulders with a thin layer of silt.  This assessment focuses on the characterizing Caryophyllia smithii and Swiftia pallida.  The faunal turf of CR.HCR.XFa.SwiLgAs is typical of circalittoral environments and composed of typically opportunistic species but is considered where appropriate. Given the lack of information on Swiftia pallida, evidence for other sea fans, including Eunicella verrucosa is presented where applicable.  Other species present are considered opportunistic colonizers, ephemeral or not important characterizing within the biotopes.

Resilience and recovery rates of habitat

Caryophyllia smithii is a small (max 3 cm across) solitary coral, common within tide swept sites of the UK (Wood, 2005), and distributed from Greece (Koukouras, 2010) to the Shetland Islands and Orkney (NBN, 2015; Wilson, 1975). It was suggested by Fowler & Laffoley (1993) that Caryophyllia smithii was a slow growing species (0.5-1 mm in horizontal dimension of the corallum per year), which in turn suggested that inter-specific spatial competition with colonial faunal or algae species were important factors in determining local abundance of Caryophyllia smithii (Bell & Turner, 2000). Caryophyllia smithii reproduces between January and March and spawning occurs from March to June (Tranter et al., 1982). The pelagic stage of the larvae may last up to 10 weeks, which provides this species with a good dispersal capability (Tranter et al., 1982) Asexual reproduction and division is also commonly observed (Hiscock & Howlett, 1976).  Bell (2002) reported that juvenile Caryophyllia smithii have variable morphology which gives them an advantage in colonizing a wide range of habitats.

Sea fans are sessile colonial cnidarians that grow erect from the substratum, with each colony formed of many small polyps, each with tentacles that may be either extended or retracted. Swiftia pallida is a small sea fan that forms slender colonies with infrequent branching, up to 20 cm tall but usually 7- 10 cm. Branches are irregularly orientated and twig-like (Manuel, 1988; Hiscock, 2007).  Populations of Swiftia pallida are thought to be self-sustaining, with short-lived larvae and limited potential for larval dispersal. It is thought that the colonization of the Shetland Islands has been prevented by geographical barriers (Hiscock et al., 2001). Reproduction is likely to be annual and may be triggered by either summer high or winter low temperatures (Hiscock et al., 2001).  Although Swiftia pallida has not been specifically studied, the average number of eggs per polyp in other gorgonians increases with increasing colony size. The number of eggs released from larger colonies can be orders of magnitude higher than for smaller colonies (Beiring & Lasker, 2000). It has been suggested that when a large colony size is attained, more energy is available for reproduction because relative colony growth decreases (Beiring & Lasker, 2000). Swiftia pallida abundance may be up to three colonies per metre (Minchin, 1987c). Growth rates for this species are unknown, however, the pink sea fan Eunicella verrucosa has highly variable growth. A population of Eunicella verrucosa at Lundy Island had growth rates of approximately 1 cm/year, which may be similar to Swiftia pallida.  The lifespan of Swiftia pallida is estimated to be between 10 and 20 years (Hiscock et al. 2001; Wilding & Wilson, 2009).  Very little information was found on the recovery potential of this species.  The ability to recolonize an area following mass mortality is likely to be restricted (Hiscock et al., 2001).

Alcyonium digitatum colonies are likely to have a lifespan that exceeds 20 years as colonies have been followed for 28 years in marked plots (Lundälv, pers. comm., in Hartnoll, 1998). Colonies that were 10-15 cm in height were aged at between 5 and 10 years old (Hartnoll, unpublished). Sexual maturity is predicted to occur, at its earliest, when the colony reaches its second year of growth. However, the majority of colonies are not predicted to reach maturity until their third year (Hartnoll, 1975).  Alcyonium digitatum spawns from December and January. Gametes are released into the water where fertilization occurs. The embryos are neutrally buoyant and float freely for seven days when they give rise to actively swimming lecithotrophic planulae which may have an extended pelagic life before they eventually settle (usually within 1 or 2 further days) and metamorphose to polyps (Matthews, 1917; Hartnoll, 1975; Budd, 2008). Larvae have been reported to survive for up to 35 weeks as non-feeding planulae and may favour the dispersal and eventual discovery of a site suitable for settlement (Hartnoll, 1975).  Alcyonium digitatum can recruit onto bare surfaces within two years but may take up to five years to fully recover following significant mortality (Whomersley & Picken, 2003; Hiscock et al., 2010).

The life cycle of hydroids typically alternates between an attached solitary or colonial polyp generation and a free-swimming medusa generation.  Planulae larvae produced by hydroids typically metamorphose within 24 hours and crawl only a short distance away from the parent plant (Sommer, 1992).  Gametes liberated from the medusae (or vestigial sessile medusae) produce gametes that fuse to form zygotes that develop into free-swimming planula larvae (Hayward & Ryland, 1994) that are present in the water column between 2-20 days (Sommer, 1992).  It has also been suggested that rafting on floating debris as dormant stages or reproductive adults (or on ships hulls or in ship ballast water), together with their potentially long lifespan, may have allowed hydroids to disperse over a wide area in the long-term and explain the near cosmopolitan distributions of many hydroid species (Cornelius, 1992; Boero & Bouillon 1993). Hydroids are therefore classed as potential fouling organisms, rapidly colonising a range of substrata placed in marine environments and are often the first organisms to colonize available space in settlement experiments (Gili & Hughes, 1995).  For example, hydroids were reported to colonize an experimental artificial reef within less than 6 months, becoming abundant in the following year (Jensen et al., 1994).  In similar studies, Obelia species recruited to the bases of reef slabs within three months and the slab surfaces within six months of the slabs being placed in the marine environment (Hatcher, 1998).  Bradshaw et al., (2002) observed that reproduction in Nemertesia antennina occurred regularly, with three generations per year. It was also observed that the presence of adults stimulates larval settlement, therefore if any adults remain, reproduction is likely to result in local recruitment. 

The recolonization of epifauna on vertical rock walls was investigated by Sebens (1985, 1986).  He reported that rapid colonizers such as encrusting corallines, encrusting bryozoans, amphipods and tubeworms recolonized within 1-4 months.  Ascidians such as Dendrodoa carnea, Molgula manhattensis and Aplidium spp. achieved significant cover in less than a year, and, together with Halichondria panicea, reached pre-clearance levels of cover after two years.  A few individuals of Alcyonium digitatum and Metridium senile colonized within four years (Sebens, 1986) and would probably take longer to reach pre-clearance levels.

Resilience assessment: The hydroids that characterize this biotope are likely to recover from damage very quickly. Based on the available evidence, resilience for the hydroid species assessed is ‘High’ (recovery within two years) for any level of perturbation (where resistance is ‘None’, ‘Low’, ‘Medium’ or ‘High’). Depending on the season of the impact and level of recovery, recovery could occur within six months. Caryophyllia smithii colonized the wreck of the Scylla within a year, however, this may be due to the time of the vessel sinking and if removed recovery may take longer.   Alcyonium digitatum is likely to recruit fairly rapidly, however full recovery following a significant decline may take longer.  Swiftia pallida is likely to be the slowest to recover and if a population was completely removed from the habitat (resistance of ‘None’) resilience has been assessed as ‘Low’ (recovery in 10-25 years) because of the low larvae dispersal, probable importance of self-sustaining communities and slow growth rate of Swiftia pallida (Hiscock et al., 2001). For resistance assessments of ‘Low’ or ‘Medium’, resilience has been assessed as ‘Medium’ (recovery in 2-10 years).

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

Mitchell et al. (1983) suggested that the Scottish and Irish populations of Swiftia pallida were at the southern limit of the species range.  It should be noted that there are reports of Swiftia pallida in deep waters (518-766 m depth) in the Mediterranean (Mastrototaro et al., 2010), however, distribution in the British Isles appears to be limited to the Atlantic coasts of Scotland and Ireland (NBN, 2015).  Hiscock et al. (2001) predicted the loss of all populations occurring in the Inner Hebrides and mainland western Scotland with a 2°C increase in summer surface temperatures over a 20 year period. 

Caryophyllia smithii is found across the British Isles (NBN, 2015) and has been recorded in Greece (Koukouras, 2010).  It is, therefore, unlikely to be significantly affected by an increase at the benchmark level. However, Tranter et al. (1982) suggested Caryophyllia smithii reproduction was cued by seasonal increases in seawater temperature. Therefore, unseasonal increases in temperature may disrupt natural reproductive processes and negatively influence recruitment patterns. Holt (pers. comm.) also suggested that long-term increases in temperature due to climate change may allow the parasitic barnacle Adna anglica to extend its range northwards and overlap the range of this biotope. Adna anglica is a southern species limited to the southwest of Britain where it parasitizes Caryophillia and has probably contributed to the decrease in abundance of Leptopsammia (Holt pers. comm.). It may impact the abundance of Caryophyllia if climate change allowed it to extend its range northwards (Holt pers. comm.). Other species present in the biotope are widespread across the British Isles or are not important to the classification of this biotope.

Sensitivity assessment.  The CR.HCR.XFa.SwiLgAs biotope has a northern distribution within the British Isles, with the characterizing Swiftia pallida being intolerant of warmer conditions.  Resistance is likely to be ‘Low’ so that resilience is assessed as ‘Medium’ and sensitivity as ‘Medium’.

Low
Medium
Medium
Medium
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Medium
Low
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Medium
Low
Low
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

Caryophyllia smithii is a southern species (Fish & Fish, 1992) with a northern range limit in the Shetland Isles (NBN, 2015).  It is likely to be close to its northerly range limit and, therefore, likely to be negatively affected by a decrease in temperature at the benchmark level. Swiftia pallida is classed as a northerly species and is recorded in Scotland, south-west Ireland (e.g. Kenmare Bay) on the west coasts of Norway and Sweden and in deep water from the Bay of Biscay and the Mediterranean (Wilding & Wilson, 2009).

Sensitivity assessment. Caryophyllia smithii is already close to its northern range limit and a decrease would likely significantly affect the northern populations of the species and hence the biotope.  Resistance is assessed as ‘Low’, resilience as ‘Medium’ and sensitivity as ‘Medium’.

Low
Low
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Medium
Medium
Medium
Medium
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Medium
Low
Low
Low
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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

CR.HCR.XFa.SwiLgAs is a circalittoral biotope complex and an increase at the benchmark would result in a change from full to hyper salinity.  No records of the characterizing Caryophyllia smithii or Swiftia pallida in hypersaline conditions was found. 

No evidence (NEv)
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Not relevant (NR)
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No evidence (NEv)
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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

This biotope occurs in full salinity.  Caryophyllia smithii has been recorded in biotopes from Full to Low salinity (Connor et al., 2004) and would probably tolerate a change at the benchmark level. Swiftia pallida has only been recorded in full salinity biotopes (Connor et al., 2004) and is likely to be intolerant of a decrease in salinity. Resistance has been assessed as ‘Low’, resilience as ‘Medium’ and sensitivity has been assessed as ‘Medium’.

Low
Low
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Medium
Low
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Medium
Low
Low
Low
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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

Swiftia pallida, Alcyonium digitatum, Caryophyllia smithii, Spirobranchus triqueter and sponges are suspension feeders, relying on water currents to supply food (Hiscock, 1983). These taxa, therefore, thrive in conditions of vigorous water flow e.g. around Orkney and St Abbs, Scotland, where Alcyonium digitatum dominated biotopes may experience tidal currents of 3 and 4 knots (approximately 1.5 m/sec) during spring tides (De Kluijver, 1993). Caryophyllia smithii, in particular, is described as favouring sites with a high tidal flow (Bell & Turner, 2000; Wood, 2005).

This biotope consists mainly of species firmly attached to the substratum, which would be unlikely to be displaced by an increase in the strength of tidal streams at the benchmark level.

Sea fans are found in strong tidal streams but probably retract their polyps when current velocity gets too high for the polyps to retain food. Tidal streams exert a steady pull on the colonies and are therefore likely to detach only very weakly attached colonies. Colonies rely on high water flow rates to bring food and to remove silt (Hiscock, 2007). Caryophyllia smithii has been recorded in biotopes from negligible to strong water flow (0-6 knots) (Connor et al., 2004).  No evidence for Swiftia pallida was found, however, Bunker (1986) reported that the sea fan Eunicella verrucosa was present in areas subject to at least moderate tidal stream, but was most abundant in strong tidal streams.  There is a tendency for Eunicella verrucosa to grow aligned across the direction of the prevailing current (Bunker, 1986).

Sensitivity assessment. The CR.HCR.XFa.SwiLgAs biotope is found from weak to moderately strong water flow (1-3 knots) but can be found from extremely exposed to sheltered wave exposure.  It is likely that the biotope exists in high energy habitats, with either water flow or wave action prevailing.  Change in water flow is, therefore, probably only relevant to wave sheltered examples.  The characterizing species (including gorgonians, soft corals and Caryophyllia smithii) are generally associated with moderate to high energy environments. However, a change at the benchmark level is unlikely to be significant. Resistance is, therefore, assessed as ‘High’, resilience as ‘High’ and the biotope is assessed as ‘Not Sensitive’ at the benchmark level.

High
Medium
Medium
Medium
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High
High
High
High
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Not sensitive
Medium
Medium
Medium
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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

Changes in emergence are Not Relevant to this biotope as it is restricted to fully subtidal/circalittoral conditions - the pressure benchmark is relevant only to littoral and shallow sublittoral fringe biotopes.

Not relevant (NR)
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Not relevant (NR)
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Not relevant (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

Dead sea fans have been recorded washed up along Chesil Beach (UK) following winter storms (Hatcher & Trewhella, 2006). However, Bunker (1986) reported that Eunicella verrucosa was most abundant in moderately exposed locations. Caryophyllia smithii has been recorded in very sheltered to extremely exposed biotopes (Connor et al., 2004).  Bell (2002) reported that Caryophyllia smithii near Lough Hyne (Ireland) exposed to strong wave action on open coasts were relatively small, possibly down to juvenile morphological variability, as Caryophyllia smithii found deeper and in sediment were thinner and taller.

Sensitivity assessment. The CR.HCR.XFa.SwiLgAs biotope occurs in wave exposed to sheltered conditions but can be found from weak to moderately strong water flow (1-3 knots).  It is likely that the biotope exists in high energy habitats, with either water flow or wave action prevailing.  Change in wave exposure is, therefore, probably only relevant to habitats that experience weak water flow.  The characterizing species (including gorgonians and Caryophyllia smithii) are generally associated with moderate to high energy environments. However, a change at the benchmark level is unlikely to be significant. Resistance is, therefore, assessed as ‘High’, resilience as ‘High’ and the biotope is assessed as ‘Not Sensitive’ at the benchmark level.

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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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

Chan et al. (2012) studied the response of the gorgonian Subergorgia suberosa to heavy metal-contaminated seawater from a former coastal mining site in Taiwan. Cu, Zn, and Cd each showed characteristic bioaccumulation. Metallic Zn accumulated but rapidly dissipated. In contrast, Cu easily accumulated but was slow to dissipate, and Cd was only slowly absorbed and dissipated. Associated polyp necrosis, mucus secretion, tissue expansion, and increased mortality were reported in Subergorgia suberosa exposed to water polluted with heavy metals.

However, this pressure is Not assessed but the evidence is presented where available.

Not Assessed (NA)
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Not assessed (NA)
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Not assessed (NA)
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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.

CR.HCR.XFa.SwiLgAs is a sub-tidal biotope (Connor et al., 2004). Oil pollution is mainly a surface phenomenon and its impact upon circalittoral turf communities is likely to be limited. However, as in the case of the Prestige oil spill off the coast of France, high swell and winds can cause oil pollutants to mix with the seawater and could potentially negatively affect sub-littoral habitats (Castège et al., 2014).

Filter feeders are highly sensitive to oil pollution, particularly those inhabiting the tidal zones which experience high exposure and show correspondingly high mortality, as are bottom-dwelling organisms in areas where oil components are deposited by sedimentation (Zahn et al., 1981). White et al. (2012) reported on deepwater gorgonian communities, including Swiftia pallida six months after the Deep Water Horizon oil spill. Stress in the gorgonians was observed including excessive mucous production, retracted polyps and smothering of brown flocculent material (floc) which contained oil from the Macondo well. Hsing et al. (2013) reported that, following smothering by floc associated with the Deepwater Horizon spill, recovery of corals and gorgonians was inversely correlated with floc presence.

Not Assessed (NA)
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Not assessed (NA)
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Not assessed (NA)
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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.

Not Assessed (NA)
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Not assessed (NA)
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Not assessed (NA)
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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)
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Not relevant (NR)
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No evidence (NEv)
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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)
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Not assessed (NA)
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Not assessed (NA)
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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

In general, respiration in most marine invertebrates does not appear to be significantly affected until extremely low concentrations are reached. For many benthic invertebrates this concentration is about 2 ml/l (ca 2.66 mg/l) (Herreid, 1980; Rosenberg et al., 1991; Diaz & Rosenberg, 1995). Cole et al. (1999) suggest possible adverse effects on marine species below 4 mg/l and probable adverse effects below 2 mg/l.

Little information on the effects of oxygenation on bryozoans was found.  No evidence was found concerning the effects of hypoxia for Swiftia pallida. However, as a species that lives in fully oxygenated waters in conditions of flowing waters, it is expected that it would be intolerant to decreased oxygen levels. Bell (2002) reported that an oxycline at Lough Hyne (<5 % surface concentration) limited vertical colonization by Caryophillia smithii.

Sensitivity assessment. Despite limited evidence, Swiftia pallida and Caryophyllia smithii are unlikely to tolerate hypoxic events given their preference for moderate water movement. Resistance is ‘Low’, resilience is ‘Medium’ and sensitivity is ‘Medium’.  It should be noted that, as these biotopes occur in high energy habitats, low oxygen events are likely to be short-lived.

Low
Low
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Medium
Low
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Medium
Low
Low
Low
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Nutrient enrichment [Show more]

Nutrient enrichment

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

Evidence

Echavarri-Erasun et al. (2007) described the effects of deepwater sewage outfall discharges on the relative abundance of rocky reef communities.  Species typical of hard substrata (including Caryophyllia smithii and bryozoans) increased in total richness and abundance near the outfall.

Whilst Swifita pallida could be at risk of competition from algae in shallow waters due to nutrient enrichment, this biotope occurs in the circalittoral below the depth suitable for most macroalgae. If nutrient enrichment resulted in algal blooms, then their subsequent death could result in deposition of dead algae on the sea bed and resultant localised hypoxia (see above).

This biotope is considered to be 'Not sensitive' at the pressure benchmark, that assumes compliance with good status as defined by the WFD.

Not relevant (NR)
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Not relevant (NR)
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Not sensitive
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Organic enrichment [Show more]

Organic enrichment

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

Evidence

Echavarri-Erasun et al. (2007) described the effects of deepwater sewage outfall discharges on the relative abundance of rocky reef communities.  Species typical of hard substrata (including Caryophyllia smithii and bryozoans) increased in total richness and abundance near the outfall.

Sensitivity assessment. Evidence for some of the characterizing species suggests some tolerance, or even increased abundance when exposed to organic enrichment in the circalittoral.  However, ‘No evidence’ for the important characterizing Swiftia pallida could be found.

No evidence (NEv)
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Not relevant (NR)
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No evidence (NEv)
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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

If rock were replaced with sediment, this would represent a fundamental change to the physical character of the biotope and the species would be unlikely to recover. The biotope would be lost.

Sensitivity assessment. Resistance to the pressure is considered ‘None’, and resilience ‘Very low’. Sensitivity has been 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

Not relevant’ to biotopes occurring on bedrock.

Not relevant (NR)
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Not relevant (NR)
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Not relevant (NR)
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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

The species characterizing this biotope are epifauna or epiflora occurring on rock and would be sensitive to the removal of the habitat. However, extraction of rock substratum is considered unlikely and this pressure is considered to be ‘Not relevant’ to hard substratum habitats.

Not relevant (NR)
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Not relevant (NR)
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Not relevant (NR)
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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

Physical disturbance by fishing gear has been shown to adversely affect emergent epifaunal communities with hydroid and bryozoan matrices reported to be greatly reduced in fished areas (Jennings & Kaiser, 1998). Heavy mobile gears could also result in movement of boulders (Bullimore, 1985; Jennings & Kaiser, 1998). Whilst no evidence for Swiftia pallida was found, reviews have considered the sea fan Eunicella verrucosa to be sensitive to abrasion (MacDonald et al., 1996; Hall et al., 2008; Tillin et al., 2010).  Swiftia pallida has been observed tangled in lobster pot netting and detached in the vicinity of lobster pots (Holt, pers comm.).  Other studies suggest that Eunicella verrucosa may be more resistant to abrasion pressures.  Eno et al. (2001) conducted experimental potting on areas containing fragile epifaunal species in Lyme Bay, south-west England. Divers observed that pink sea fan ‘flexed and bent before returning to an upright position under the weight of pots’. Although relatively resistant to a single event it was not clear whether repeated exposure could cause further damage or whether injuries had been inflicted that could lead to deterioration (Eno et al., 2001). Observation of pots suggested that these were dragged along the bottom when wind and tidal streams were strong, however little damage to epifauna was observed.  Eunicella verrucosa were patchily distributed in areas subject to potting damage, but the study could not determine whether this was due to damage from potting (Eno et al., 2001). A further four-year study on potting in the Lundy Marine Protected Area detected no significant differences in Eunicella verrucosa between areas subject to commercial potting and those where this activity was excluded (Sheehan et al., 2013).

However, Tinsley (2006) observed flattened sea fans, that had continued growing, with new growth being aligned perpendicular to the current, so clearly even colonies of Eunicella verrucosa that are damaged can continue to survive. Healthy Eunicella verrucosa are able to recover from minor damage and scratches to the coenenchyme (Tinsley, 2006), and the coenenchyme covering the axial skeleton will regrow over scrapes on one side of the skeleton in about one week (Hiscock, pers. comm.)  Hinz et al. (2011) reported that Eunicella verrucosa did not show a significant negative response with respect to abundance and average body size to the intensity of scallop dredging.

A study by Boulcott & Howell (2011) on the effects of scallop dredging in rocky substrata suggested that associated epifaunal communities, such as bryozoans, hydroids, soft corals and sponges were removed by a passing scallop dredge.  However, on hard, uneven rock damage, damage to more resistant epifauna, whilst in evidence, was restricted.  The study also recorded that the mobile substrata present was likely to be moved and turned by of the passing dredge, leading to further damage to the epifaunal communities. 

Sensitivity assessment. Swiftia pallida is sessile and epifaunal and, based on evidence for Eunicella verrucosa, is likely to be severely damaged by heavy gears, such as scallop dredging (MacDonald et al., 1996).  However, some studies suggest the sea fan Eunicella verrucosa may be more resistant, particularly to low intensity lighter abrasion pressures, such as pots and associated anchor damage (Eno et al. 2001; Sheehan et al., 2013), and this could be the case for Swiftia pallida.  Therefore, a resistance of ‘Low’ is recorded. Resilience is assessed as ‘Medium’ and sensitivity as ‘Medium’.

Low
Low
NR
NR
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Medium
Low
NR
NR
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Medium
Low
Low
Low
Help
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

The species characterizing this biotope group are epifauna or epiflora occurring on rock which is resistant to subsurface penetration.  The assessment for abrasion at the surface only is therefore considered to equally represent sensitivity to this pressure. This pressure is thought ‘Not Relevant’ to hard rock biotopes

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
Help
Not relevant (NR)
NR
NR
NR
Help
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

Bell & Turner (2000) studied populations of Caryophyllia smithii at three sites of differing sedimentation regime in Lough Hyne, Ireland. Calyx size was largest at the site of least sedimentation and smallest at the site of most sedimentation. In contrast, the height of individuals was greatest at the site of most sedimentation and smallest at the site of least sedimentation. The height of individuals correlated with the level of surrounding sediment. High density correlated with high sedimentation and depth (Bell & Turner, 2000). 

While siltation may inhibit feeding, colonies of the sea fan Eunicella verrucosa produce mucus to clear themselves of silt (Hiscock, 2007) and sea fans are probably tolerant of increases in suspended sediment (Hiscock et al., 2004).  Bunker (1986) reported that Eunicella verrucosa were mostly observed on bedrock or boulders, but did occur at sites up to ‘moderately silted’.

Sensitivity assessment. CR.HCR.XFa.SwiLgAs occurs on bedrock in the circalittoral and is unlikely to experience highly turbid conditions.  From the evidence presented above, the characterizing species tolerate some siltation and a change at the benchmark level is unlikely to cause mortality.  Resistance is recorded as ‘High’, resilience as ‘High’ and the biotope is assessed as ‘Not sensitive’ at the benchmark level.

High
Low
NR
NR
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High
High
High
High
Help
Not sensitive
Low
Low
Low
Help
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

Caryophyllia smithii is small (approx. <3 cm height from the seabed) and would therefore likely be inundated in a 'light' sedimentation event. However, Bell & Turner (2000) reported Caryophyllia smithii was abundant at sites of 'moderate' sedimentation (7 mm ± 0.5 mm) in Lough Hyne. It is therefore likely that Caryophyllia smithii would be resistant to periodic sedimentation. If 5 cm of sediment were removed rapidly, via tidal currents, Caryophyllia smithii would likely remain within the biotope.  Burton et al. (2005) partly attributed fluctuations in Caryophyllia smithii abundance at Skomer Island to surface sediment cover.  Bell (2002) reported that juvenile Caryophyllia smithii are morphologically variable and initially undergo rapid growth with tall and thin forms in deeper, sheltered, relatively sedimented conditions near Lough Hyne, Ireland.  It was concluded that this was to escape the thin layer of sediment present.  

Swiftia pallida generally grows to a height of about 7-10 cm (Wilson, 2007).  It is found on rocks covered with a fine layer of silt (Mitchell et al., 1983). While siltation may inhibit feeding, colonies of the sea fan Eunicella verrucosa produce mucus to clear themselves of silt (Hiscock, 2007). It is however thought that smothering causes mortality (Hiscock et al., 2004).  Bunker (1986) reported that Eunicella verrucosa were mostly observed on bedrock or boulders, but did occur at sites up to ‘moderately silted’.

Sensitivity assessment. Smothering by 5 cm would cover the majority of Caryophyllia smithii and the smallest examples of the other characterizing species and could result in limited mortality.  Caryophyllia smithii has been reported as quite tolerant of temporary burial and the biotope occurs in moderate water flow and the sediment would likely be removed rapidly.  Resistance was assessed as ‘High’, resilience as ‘High’ and the biotope is assessed as ‘Not sensitive’ at the benchmark level.

High
Medium
Medium
Medium
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High
High
High
High
Help
Not sensitive
Medium
Medium
Medium
Help
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

Caryophyllia smithii is small (approx. <3 cm height from the seabed) and would therefore likely be inundated in a “light” sedimentation event. However, Bell & Turner (2000) reported Caryophyllia smithii was abundant at sites of “moderate” sedimentation (7 mm ± 0.5 mm) in Lough Hyne. It is therefore likely that Caryophyllia smithii would be resistant to periodic sedimentation. If the sediment was removed rapidly, via tidal currents, Caryophyllia smithii would likely remain within the biotope.  Burton et al. (2005) partly attributed fluctuations in Caryophyllia smithii abundance at Skomer Island to surface sediment cover.  Bell (2002) reported that juvenile Caryophyllia smithii are morphologically variable and initially undergo rapid growth with tall and thin forms in deeper, sheltered, relatively sedimented conditions near Lough Hyne, Ireland.  It was concluded that this was to escape the thin layer of sediment present.  

Swiftia pallida generally grows to a height of about 7-10 cm (Wilson, 2007).  It is found on rocks covered with a fine layer of silt (Mitchell et al., 1983). While siltation may inhibit feeding, colonies of the sea fan Eunicella verrucosa produce mucus to clear themselves of silt (Hiscock, 2007). It is however thought that smothering causes mortality (Hiscock et al., 2004).  Bunker (1986) reported that Eunicella verrucosa were mostly observed on bedrock or boulders, but did occur at sites up to ‘moderately silted’.

Sensitivity assessment. Smothering by 30 cm of sediment would likely bury the majority of characterizing species, with only those individuals on boulders and vertical surfaces escaping burial.  The biotope occurs in moderate water flow and it is likely that the sediment would probably be removed rapidly.  Resistance is assessed as ‘Medium’, resilience as ‘Medium’ and sensitivity as ‘Medium’.

Medium
Medium
Medium
Medium
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Medium
Low
NR
NR
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Medium
Low
Low
Low
Help
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

Not assessed.

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’ was found

No evidence (NEv)
NR
NR
NR
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Not relevant (NR)
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

Whilst no evidence could be found on the effects of noise or vibrations on the characterizing species, it is unlikely that these species would be adversely affected by noise.  This pressure ‘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

Whilst no evidence could be found for the effect of light on the characterizing species of these biotopes, it is unlikely that these species would be impactedThe biotope is circalittoral, occurs below 10 m and is dependent on secondary rather than primary production. Resistance to this pressure is assessed as 'High' and resilience as 'High'. This biotope is therefore considered to be 'Not sensitive' at the benchmark level.

 

High
Low
NR
NR
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High
High
High
High
Help
Not sensitive
Low
Low
Low
Help
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

Barriers and changes in tidal excursion are ‘Not relevant’ to biotopes restricted to open waters.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
Help
Not relevant (NR)
NR
NR
NR
Help
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
NR
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Not relevant (NR)
NR
NR
NR
Help
Not relevant (NR)
NR
NR
NR
Help
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

‘Not relevant’.

Not relevant (NR)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
Help
Not relevant (NR)
NR
NR
NR
Help

Biological Pressures

Use [show more] / [show less] to open/close text displayed

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

No evidence of translocation or genetic modification of populations of the characterizing species was found. Therefore, there is currently ‘No evidence’ on which to assess this pressure.

No evidence (NEv)
NR
NR
NR
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Not relevant (NR)
NR
NR
NR
Help
No evidence (NEv)
NR
NR
NR
Help
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

This biotope is classed as circalittoral and, therefore, no invasive algal species have been considered.  Solidobalanus fallax barnacles are an invasive southern species only recently recorded in south-west England (Southward et al., 2004) and have been observed fouling (primarily damaged or diseased) gorgonians (Hall-Spencer et al., 2007). Resistance is, therefore, assessed as ‘Medium’, resilience as ‘Medium’ and sensitivity as ‘Medium’.  Due to the constant risk of new invasive species, the literature for this pressure should be revisited.

Medium
Low
NR
NR
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Medium
Low
NR
NR
Help
Medium
Low
Low
Low
Help
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

Whilst no evidence of disease in Swiftia pallida could be found, the first recorded incidence of cold-water coral disease was noted in the sea fan Eunicella verrucosa, in south-west England in 2002 (Hall-Spencer et al., 2007).  Video surveys of 634 separate colonies at 13 sites revealed that disease outbreaks were widespread in south-west England from 2003 to 2006. Coenenchyme became necrotic in diseased specimens, leading to tissue sloughing and exposing skeletal gorgonin to settlement by fouling organisms. Sites, where necrosis was found, had significantly higher incidences of fouling. No fungi were isolated from diseased or healthy tissue, but significantly higher concentrations of bacteria occurred in diseased specimens. Vibrios isolated from Eunicella verrucosa did not induce disease at 15°C, but at 20°C controls remained healthy and test gorgonians became diseased. Bacteria associated with diseased tissue produced proteolytic and cytolytic enzymes that damaged Eunicella verrucosa tissue and may be responsible for the necrosis observed. Monitoring at the site where the disease was first noted showed new gorgonian recruitment from 2003 to 2006; some individuals had died and become completely overgrown, whereas others had continued to grow around a dead central area (Hall-Spencer et al., 2007). No evidence for disease in the characterizing bryozoans could be found.

Sensitivity assessment.  Based on reports of mortality linked to disease in the sea fan Eunicella verrucosa, a disease may result in mortality of Swiftia pallida.  It should be noted that the colder temperatures in which Swiftia pallida occurs may confer some resistance.  Resistance is assessed as ‘Medium’, resilience as ‘Medium’ and sensitivity as ‘Medium’. 

Medium
Low
NR
NR
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Medium
Low
NR
NR
Help
Medium
Low
Low
Low
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

Eunicella verrucosa was collected historically as a curio by divers and was collected until recently in the British Isles (Wells et al., 1983; Bunker, 1986). It is now protected under schedule 5 of the Wildlife and Countryside Act 1981, no evidence of harvesting of the sea fan Swifita pallida or any of the other characterizing species was found. 

As there is historical evidence of harvesting of other sea fans, the sessile, epifaunal Swifita pallida would have no resistance to harvesting by divers.  Therefore, resistance is assessed as ‘None’, resilience as ‘Low’ and sensitivity as ‘High’.

None
Low
NR
NR
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Low
Low
NR
NR
Help
High
Low
Low
Low
Help
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 characteristic species probably compete for space within the biotope, so that loss of one species would probably have little if any effect on the other members of the community. However, removal of the characteristic epifauna due to by-catch is likely to remove a proportion of the biotope and change the biological character of the biotope.  As sessile epifauna, the characterizing species and likely to be severely damaged by heavy gears, such as scallop dredging (MacDonald et al., 1996).  However,  some studies suggest that sea fans may be more resistant, particularly to low intensity, lighter abrasion pressures, such as pots and associated anchor damage (Eno et al. 1996; Sheehan et al., 2013)  Taking all the evidence into account, a resistance of ‘Low’ is recorded, albeit with a low confidence value owing to the lack of consensus in the literature. Resilience is assessed as ‘Medium’ and sensitivity as ‘Medium’.

Low
Low
NR
NR
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Medium
Low
NR
NR
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Medium
Low
Low
Low
Help

Bibliography

  1. Beiring, E.A. & Lasker, H.R., 2000. Egg production by colonies of a gorgonian coral. Marine Ecology Progress Series, 196, 169-177.

  2. Bell, J.J. & Turner, J.R., 2000. Factors influencing the density and morphometrics of the cup coral Caryophyllia smithii in Lough Hyne. Journal of the Marine Biological Association of the United Kingdom, 80, 437-441. DOI https://dx.doi.org/10.1017/S0025315400002137

  3. Bell, J.J., 2002. Morphological responses of a cup coral to environmental gradients. Sarsia, 87, 319-330. DOI https://doi.org/10.1080/00364820260400825

  4. Boulcott, P. & Howell, T.R.W., 2011. The impact of scallop dredging on rocky-reef substrata. Fisheries Research (Amsterdam), 110 (3), 415-420.

  5. Budd, G.C. 2008. Alcyonium digitatum Dead man's fingers. 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. Available from: http://www.marlin.ac.uk/species/detail/1187

  6. Bullimore, B., 1985. An investigation into the effects of scallop dredging within the Skomer Marine Reserve. Report to the Nature Conservancy Council by the Skomer Marine Reserve Subtidal Monitoring Project, S.M.R.S.M.P. Report, no 3., Nature Conservancy Council.

  7. Bunker, F., 1986. Survey of the Broad sea fan Eunicella verrucosa around Skomer Marine Reserve in 1985 and a review of its importance (together with notes on some other species of interest and data concerning previously unsurveyed or poorly documented areas). Volume I. Report to the NCC by the Field Studies Council.

  8. Castège, I., Milon, E. & Pautrizel, F., 2014. Response of benthic macrofauna to an oil pollution: Lessons from the “Prestige” oil spill on the rocky shore of Guéthary (south of the Bay of Biscay, France). Deep Sea Research Part II: Topical Studies in Oceanography, 106, 192-197.

  9. Chamberlain Jr., J.A. & Graus, R.R., 1975. Water Flow and Hydromechanical Adaptations of Branched Reef Corals. Bulletin of Marine Science, 25 (1), 112-125.

  10. Chan, I., Tseng, L. C., Kâ, S., Chang, C. F. & Hwang, J. S., 2012. An experimental study of the response of the gorgonian coral Subergorgia suberosa to polluted seawater from a former coastal mining site in Taiwan. Zoological Studies, 51 (1), 27-37.

  11. Cocito, S., Ferrier-Pagès, C., Cupido, R., Rottier, C., Meier-Augenstein, W., Kemp, H., Reynaud, S. & Peirano, A., 2013. Nutrient acquisition in four Mediterranean gorgonian species. Marine Ecology Progress Series, 473179-188.

  12. Cole, S., Codling, I.D., Parr, W. & Zabel, T., 1999. Guidelines for managing water quality impacts within UK European Marine sites. Natura 2000 report prepared for the UK Marine SACs Project. 441 pp., Swindon: Water Research Council on behalf of EN, SNH, CCW, JNCC, SAMS and EHS. [UK Marine SACs Project.]. Available from: http://ukmpa.marinebiodiversity.org/uk_sacs/pdfs/water_quality.pdf

  13. Connell, S.D., 2003. The monopolization of understorey habitat by subtidal encrusting coralline algae: a test of the combined effects of canopy-mediated light and sedimentation. Marine Biology, 142 (6), 1065-1071.

  14. Connor, D.W., Allen, J.H., Golding, N., Howell, K.L., Lieberknecht, L.M., Northen, K.O. & Reker, J.B., 2004. The Marine Habitat Classification for Britain and Ireland. Version 04.05. ISBN 1 861 07561 8. In JNCC (2015), The Marine Habitat Classification for Britain and Ireland Version 15.03. [2019-07-24]. Joint Nature Conservation Committee, Peterborough. Available from https://mhc.jncc.gov.uk/

  15. De Kluijver, M.J., 1993. Sublittoral hard-substratum communities off Orkney and St Abbs (Scotland). Journal of the Marine Biological Association of the United Kingdom, 73 (4), 733-754.

  16. Diaz, R.J. & Rosenberg, R., 1995. Marine benthic hypoxia: a review of its ecological effects and the behavioural responses of benthic macrofauna. Oceanography and Marine Biology: an Annual Review, 33, 245-303.

  17. Echavarri-Erasun, B., Juanes, J.A., García-Castrillo, G. & Revilla, J.A., 2007. Medium-term responses of rocky bottoms to sewage discharges from a deepwater outfall in the NE Atlantic. Marine Pollution Bulletin, 54 (7), 941-954.

  18. Eno, N.C., MacDonald, D. & Amos, S.C., 1996. A study on the effects of fish (Crustacea/Molluscs) traps on benthic habitats and species. Final report to the European Commission. Study Contract, no. 94/076.

  19. Eno, N.C., MacDonald, D.S., Kinnear, J.A.M., Amos, C.S., Chapman, C.J., Clark, R.A., Bunker, F.S.P.D. & Munro, C., 2001. Effects of crustacean traps on benthic fauna ICES Journal of Marine Science, 58, 11-20. DOI https://doi.org/10.1006/jmsc.2000.0984

  20. Fish, J.D. & Fish, S., 1996. A student's guide to the seashore. Cambridge: Cambridge University Press.

  21. Fowler, S. & Laffoley, D., 1993. Stability in Mediterranean-Atlantic sessile epifaunal communities at the northern limits of their range. Journal of Experimental Marine Biology and Ecology, 172 (1), 109-127. DOI https://doi.org/10.1016/0022-0981(93)90092-3

  22. Gili, J-M. & Hughes, R.G., 1995. The ecology of marine benthic hydroids. Oceanography and Marine Biology: an Annual Review, 33, 351-426.

  23. Hall, K., Paramour, O.A.L., Robinson, L.A., Winrow-Giffin, A., Frid, C.L.J., Eno, N.C., Dernie, K.M., Sharp, R.A.M., Wyn, G.C. & Ramsay, K., 2008. Mapping the sensitivity of benthic habitats to fishing in Welsh waters - development of a protocol. CCW (Policy Research) Report No: 8/12, Countryside Council for Wales (CCW), Bangor, 85 pp. 

  24. Hall-Spencer, J.M., Pike, J. & Munn, C.B., 2007. Diseases affect cold-water corals too: Eunicella verrucosa (Cnidaria: Gorgonacea) necrosis in SW England Diseases of Aquatic Organisms, 76, 87-97.

  25. Hartnoll, R.G., 1975. The annual cycle of Alcyonium digitatum. Estuarine and Coastal Marine Science, 3, 71-78.

  26. Hartnoll, R.G., 1998. Circalittoral faunal turf biotopes: an overview of dynamics and sensitivity characteristics for conservation management of marine SACs, Volume VIII. Scottish Association of Marine Sciences, Oban, Scotland, 109 pp. [UK Marine SAC Project. Natura 2000 reports.] Available from: http://ukmpa.marinebiodiversity.org/uk_sacs/pdfs/circfaun.pdf

  27. Hayward, P.J. & Ryland, J.S. 1998. Cheilostomatous Bryozoa. Part 1. Aeteoidea - Cribrilinoidea. Shrewsbury: Field Studies Council. [Synopses of the British Fauna, no. 10. (2nd edition)]

  28. Hayward, P.J. & Ryland, J.S. (ed.), 1995. The marine fauna of the British Isles and north-west Europe. Volume 2. Molluscs to Chordates. Oxford Science Publications. Oxford: Clarendon Press.

  29. Herreid, C.F., 1980. Hypoxia in invertebrates. Comparative Biochemistry and Physiology Part A: Physiology, 67 (3), 311-320. DOI https://doi.org/10.1016/S0300-9629(80)80002-8

  30. Hinz, H., Tarrant, D., Ridgeway, A., Kaiser, M.J. & Hiddink, J.G., 2011. Effects of scallop dredging on temperate reef fauna. Marine Ecology Progress Series, 432, 91-102.

  31. Hiscock, K. 2007. Eunicella verrucosa Pink sea fan. 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. Available from: http://www.marlin.ac.uk/species/detail/1121

  32. Hiscock, K. & Howlett, R. 1976. The ecology of Caryophyllia smithii Stokes & Broderip on south-western coasts of the British Isles. In Underwater Research (ed. E.A. Drew, J.N. Lythgoe & J.D. Woods), pp. 319-344. London: Academic Press.

  33. Hiscock, K., 1983. Water movement. In Sublittoral ecology. The ecology of shallow sublittoral benthos (ed. R. Earll & D.G. Erwin), pp. 58-96. Oxford: Clarendon Press.

  34. Hiscock, K., Sharrock, S., Highfield, J. & Snelling, D., 2010. Colonization of an artificial reef in south-west England—ex-HMS ‘Scylla’. Journal of the Marine Biological Association of the United Kingdom, 90 (1), 69-94. DOI https://doi.org/10.1017/S0025315409991457

  35. Hiscock, K., Southward, A., Tittley, I. & Hawkins, S., 2004. Effects of changing temperature on benthic marine life in Britain and Ireland. Aquatic Conservation: Marine and Freshwater Ecosystems, 14 (4), 333-362.

  36. Hiscock, K., Southward, A., Tittley, I., Jory, A. & Hawkins, S., 2001. The impact of climate change on subtidal and intertidal benthic species in Scotland. Scottish National Heritage Research, Survey and Monitoring Report , no. 182., Edinburgh: Scottish National Heritage

  37. Jennings, S. & Kaiser, M.J., 1998. The effects of fishing on marine ecosystems. Advances in Marine Biology, 34, 201-352.

  38. Jensen, A.C., Collins, K.J., Lockwood, A.P.M., Mallinson, J.J. & Turnpenny, W.H., 1994. Colonization and fishery potential of a coal-ash artificial reef, Poole Bay, United Kingdom. Bulletin of Marine Science, 55, 1263-1276.

  39. JNCC (Joint Nature Conservation Committee), 2022.  The Marine Habitat Classification for Britain and Ireland Version 22.04. [Date accessed]. Available from: https://mhc.jncc.gov.uk/

  40. JNCC (Joint Nature Conservation Committee), 2022.  The Marine Habitat Classification for Britain and Ireland Version 22.04. [Date accessed]. Available from: https://mhc.jncc.gov.uk/

  41. Koukouras, A., 2010. Check-list of marine species from Greece. Aristotle University of Thessaloniki. Assembled in the framework of the EU FP7 PESI project

  42. MacDonald, D.S., Little, M., Eno, N.C. & Hiscock, K., 1996. Disturbance of benthic species by fishing activities: a sensitivity index. Aquatic Conservation: Marine and Freshwater Ecosystems, 6 (4), 257-268.

  43. Manuel, R.L., 1988. British Anthozoa. Synopses of the British Fauna (New Series) (ed. D.M. Kermack & R.S.K. Barnes). The Linnean Society of London [Synopses of the British Fauna No. 18.]. DOI https://doi.org/10.1002/iroh.19810660505

  44. Mastrototaro, F., d’Onghia, G., Corriero, G., Matarrese, A., Maiorano, P., Panetta, P., Gherardi, M., Longo, C., Rosso, A. & Sciuto, F., 2010. Biodiversity of the white coral bank off Cape Santa Maria di Leuca (Mediterranean Sea): An update. Deep Sea Research Part II: Topical Studies in Oceanography, 57 (5), 412-430.

  45. Matthews, A., 1917. The development of Alcyonium digitatum with some notes on early colony formation. Quarterly Journal of Microscopial Science, 62, 43-94.

  46. Miller M.W. & Hay, M.E. 1998. Effects of fish predation and seaweed competition on the survival and growth of corals. Oecologia, 113 (2), 231-238.

  47. Minchin, D., 1987. Swiftia pallida Madsen (Coelenterata: Gorgonacea) in Irish waters, with a note on Pseudanthessiusthorelli (Brady) (Crustacea: Copepoda) new to Ireland Irish Naturalists' Journal, 22(5), 183-185

  48. Mitchell, R., Earll, R.C. & Dipper, F.A., 1983. Shallow sublittoral ecosystems in the Inner Hebrides. Proceedings of the Royal Society of Edinburgh Section B 83 161-184

  49. NBN, 2015. National Biodiversity Network 2015(20/05/2015). https://data.nbn.org.uk/

  50. Picton, B.E. & Morrow C.C., 2005. Encyclopedia of Marine Life of Britain and Ireland http://www.habitas.org.uk/marinelife/species.asp?item=D10920, 2008-01-08

  51. Rosenberg, R., Hellman, B. & Johansson, B., 1991. Hypoxic tolerance of marine benthic fauna. Marine Ecology Progress Series, 79, 127-131. DOI https://dx.doi.org/10.3354/meps079127

  52. Ryland, J.S., 1970. Bryozoans. London: Hutchinson University Library.

  53. Ryland, J.S., 1976. Physiology and ecology of marine bryozoans. Advances in Marine Biology, 14, 285-443.

  54. Sebens, K.P., 1985. Community ecology of vertical rock walls in the Gulf of Maine: small-scale processes and alternative community states. In The Ecology of Rocky Coasts: essays presented to J.R. Lewis, D.Sc. (ed. P.G. Moore & R. Seed), pp. 346-371. London: Hodder & Stoughton Ltd.

  55. Sebens, K.P., 1986. Spatial relationships among encrusting marine organisms in the New England subtidal zone. Ecological Monographs, 56, 73-96.

  56. Shears, N.T. Babcock, R.C. 2002. Marine reserves demonstrate top-down control of community structure on temperate reefs. Oecologia, 132, 131–142.

  57. Southward, A.J., Hiscock, K., Kerckhof, F., Moyse J. & Elfimov, A.S., 2004. Habitat and distribution of the warm water barnacle Solidobalanus fallax (Crustacea: Cirripedia). Journal of the Marine Biological Association of the United Kingdom, 84, 1169–1177.

  58. Tillin, H.M., Hull, S.C. & Tyler-Walters, H., 2010. Development of a sensitivity matrix (pressures-MCZ/MPA features). Report to the Department of the Environment, Food and Rural Affairs from ABPmer, Southampton and the Marine Life Information Network (MarLIN) Plymouth: Marine Biological Association of the UK., Defra Contract no. MB0102 Task 3A, Report no. 22., London, 145 pp.

  59. Tinsley, P., 2006. Worbarrow Reefs Sea Fan Project, 2003-2005 Dorset Wildlife Trust Report

  60. Tranter, P.R.G., Nicholson, D.N. & Kinchington, D., 1982. A description of spawning and post-gastrula development of the cool temperate coral, Caryophyllia smithi. Journal of the Marine Biological Association of the United Kingdom, 62, 845-854. DOI https://doi.org/10.1017/s0025315400044106

  61. White, H.K., Hsing, P.-Y., Cho, W., Shank, T.M., Cordes, E.E., Quattrini, A.M., Nelson, R.K., Camilli, R., Demopoulos, A.W. & German, C.R., 2012. Impact of the Deepwater Horizon oil spill on a deep-water coral community in the Gulf of Mexico. Proceedings of the National Academy of Sciences, 109 (50), 20303-20308.

  62. Whomersley, P. & Picken, G., 2003. Long-term dynamics of fouling communities found on offshore installations in the North Sea. Journal of the Marine Biological Association of the UK, 83 (5), 897-901.

  63. Wilson, J.B., 1975. The distribution of the coral Caryophyllia smithii S. & B. on the Scottish continental shelf. Journal of the Marine Biological Association of the United Kingdom, 55, 611-625.

  64. Wood. C., 2005. Seasearch guide to sea anemones and corals of Britain and Ireland. Ross-on-Wye: Marine Conservation Society.

  65. Zahn, R., Zahn, G., Müller, W., Kurelec, B., Rijavec, M., Batel, R. & Given, R., 1981. Assessing consequences of marine pollution by hydrocarbons using sponges as model organisms. Science of The Total Environment, 20 (2), 147-169.

Citation

This review can be cited as:

Readman, J.A.J., 2016. Mixed turf of hydroids and large ascidians with Swiftia pallida and Caryophyllia (Caryophyllia) smithii on weakly tide-swept circalittoral rock. In Tyler-Walters H. and Hiscock K. Marine Life Information Network: Biology and Sensitivity Key Information Reviews, [on-line]. Plymouth: Marine Biological Association of the United Kingdom. [cited 28-03-2024]. Available from: https://www.marlin.ac.uk/habitat/detail/34

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Last Updated: 07/07/2016