1995
DOI: 10.3354/meps121039
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Peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya off Greenland:documenting close benthic-pelagic coupling in the Westwind Trough

Abstract: Composition, abundance, and diversity of peracarids (Crustacea) were investigated over a period of 3 mo in the Northeast Water Polynya (NEW), off Greenland. Samples were collected from May to July 1993 during expeditions ARK IX/2 and 3 using an epibenthic sledge on RV 'Polarstern' Within the macrobenthic community peracarids were an important component of the shelf fauna and occurred in high abundance in this area together with polychaetes, molluscs and brittle stars. A total of 38322 specimens were sampled fr… Show more

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Cited by 74 publications
(43 citation statements)
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“…Some littoral species undertake nictemeral migrations (Macquart-Moulin, 1991) and recently, vertical movements have also been observed for a few deep sea species (Cartes and Sorbe, 1997). This behavioural pattern would support the presumed contribution of cumaceans, as other suprabenthic crustaceans (Brandt 1993(Brandt , 1995, to the bioturbation and resuspension in the benthic ecosystem. Moreover cumaceans are a food source for fishes (Kurian and Radhadevi, 1983) and other macrobenthic invertebrates (Cartes, 1993).…”
Section: Introductionmentioning
confidence: 53%
“…Some littoral species undertake nictemeral migrations (Macquart-Moulin, 1991) and recently, vertical movements have also been observed for a few deep sea species (Cartes and Sorbe, 1997). This behavioural pattern would support the presumed contribution of cumaceans, as other suprabenthic crustaceans (Brandt 1993(Brandt , 1995, to the bioturbation and resuspension in the benthic ecosystem. Moreover cumaceans are a food source for fishes (Kurian and Radhadevi, 1983) and other macrobenthic invertebrates (Cartes, 1993).…”
Section: Introductionmentioning
confidence: 53%
“…al., 2005). Peracarids (Amphipoda, Cumacea, Isopoda, Mysidacea and Tanaidacea) are, in general, common elements of soft bottom macrobenthos LOURIDO et al, 2008) from shallow habitats to the abyssal plains of the world oceans, often presenting high abundance and diversity (BRANDT, 1995). They are considered good indicators of water and sediment quality (CORBERA & CARDELL, 1995;ALFONSO et al, 1998;G MEZ GESTEIRA & DAUVIN, 2000) and it has been repeatedly pointed out that the knowledge of their assemblages may be useful to interpret changes in benthic communities for environmental management purposes CONLAN, 1994;BIERNBAUM, 1979).…”
Section: Introductionmentioning
confidence: 99%
“…Various hypotheses have been developed to explain such a richness of life at depths between 100 and 800 m in water at -1.5°C, which is ice covered almost year-round. These are: 1) The low concentration of terrigenous inorganic suspended material, greater quantities of which might otherwise disturb the fragile filtering mechanisms, 2) The low abundance of true benthic predators, which elsewhere exert a higher pressure on invertebrates to use ecological niches within the sediment, 3) The coastal current that guarantees a continuous supply of fresh phytodetritus for a certain period of the year (Brandt 1995, Gili et al 2002, 4) Habitat heterogeneity and niche fragmentation caused by epibiotic relationships (Gutt & Schickan 1998, Brandt et al 1997, 5) The presence of a sediment with a wide range of particle sizes which allows the successful recruitment of young stages, and 6) Specific vicarious events, e.g. the "climate diversity pumps" (Clarke & Crame 1997a), which are mainly caused by glacial advance and retreat around the continent and split formerly homogenous populations.…”
Section: Mentmentioning
confidence: 99%