1989
DOI: 10.1080/00364827.1989.10413430
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Some aspects of the biology and ecology of the burrowing shrimpCallianassa subterranea(Montagu) (Thalassinidea) from the southern North Sea

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Cited by 72 publications
(59 citation statements)
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“…One individual of Amphiura filiformis can oxidize a surface of 35 cm2 to a depth of 3 cm in the sediment by extending its arms through the sediment to th.e sediment-water interface and by regular flushing of the feeding void with oxygen-rich water (Ockelmann & Muus 1978). The subsurfacedeposit feeding Callianassa subterranea is known for its extraordinary strong bioturbation capacity (Branch & Pringle 1987, Witbaard & Duineveld 1989) and ability to oxygenate the sediment (Koike & Mukai 1983, Dobbs & Guckert 1988, Forster & Graf 1995. The branched burrow systems of C. subterranea are continuously rebuilt and reach down to 80 cm into the sediment (Nickel & Atlunson 1995), resulting in sediment turnover rates of up to 12 kg m-2 d-'.…”
Section: Trophic Stucture In Relation To Food Quality and Abiotic Facmentioning
confidence: 99%
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“…One individual of Amphiura filiformis can oxidize a surface of 35 cm2 to a depth of 3 cm in the sediment by extending its arms through the sediment to th.e sediment-water interface and by regular flushing of the feeding void with oxygen-rich water (Ockelmann & Muus 1978). The subsurfacedeposit feeding Callianassa subterranea is known for its extraordinary strong bioturbation capacity (Branch & Pringle 1987, Witbaard & Duineveld 1989) and ability to oxygenate the sediment (Koike & Mukai 1983, Dobbs & Guckert 1988, Forster & Graf 1995. The branched burrow systems of C. subterranea are continuously rebuilt and reach down to 80 cm into the sediment (Nickel & Atlunson 1995), resulting in sediment turnover rates of up to 12 kg m-2 d-'.…”
Section: Trophic Stucture In Relation To Food Quality and Abiotic Facmentioning
confidence: 99%
“…8). The most important species, Callianassa subterranea, has been documented to be an extremely effective bioturbator reaching very high sediment turnover rates of 3.5 to 11 kg m-' yr-' (Witbaard & Duineveld 1989, Rowden & Jones 1993. On the basis of the Foraminifera record, Moodley (1990) found the FF sediments to be mixed up to 30 cm depth.…”
Section: Influence Of Bioturbation On the Distribution Of Organic Mattermentioning
confidence: 99%
“…Larger animals are of particular interest because they can account for the majority of the faunal effect. Populations of the burrowing shrimp Callianassa subterranea, for example, can account for 17% of the total oxygen utilization (TOU) of North Sea sediments (de Wilde et al 1984;Witbaard and Duineveld 1989). Booij et al (1994) calculated that burrow irrigation by the amphipod Corophium volutator and oligochaetes caused ϳ25% of the total O 2 flux into intertidal sediment of the western Wadden Sea.…”
mentioning
confidence: 99%
“…Thalassinidean shrimps construct burrows in intertidal and subtidal soft sediments (Posey 1985;Witbaard & Duineveld 1989). Their burrows are considered to be amongst the deepest (>50 cm) and most complex decapod burrows (Dworschak 1983;Atkinson & Taylor 1988), and are used for shelter, reproduction, and feeding; most thalassinideans live exclusively within the burrow, except for a brief pelagic stage (Griffis & Suchanek 1991).…”
Section: Introductionmentioning
confidence: 99%