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Distribution et synécologie des fonds à Gryphus vitreus (Brachiopoda) en Corse
Authors:C C Emig
Institution:(1) Station Marine d'Endoume (CNRS-RCP 728), rue de la Batterie-des-Lions, F-13007 Marseille, France
Abstract:In the Mediterranean Sea, the brachiopod Gryphus vitreus (Born) was collected off Corsica by dredging and trawling during three cruises (June 1983; April and July 1984) and from along the French continental coast by dredging during many cruises (1975–1985). The upper limit of its bathymetric distribution lies between 115 and 125 m (rarely, from 90 m), the lower limit between 140 and 200 m depth, forming a belt along the edge of the continental shelf. The horizontal distribution of G. vitreus varies from sim250 m to >4 km, and is directly related to geomorphological and hydrodynamic variations resulting from local topography and/or geographical location. The G. vitreus bottoms are bounded on the continental slope by the bathyal mud biocoenosis and on the shelf by the coastal detritic or shelf-edge detritic biocoenosis, both circalittoral. The bottoms correspond to a bathylittoral ecosystem characterized by (1) prevailing environmental conditions which result in a biotope characterized by coarse detritic sediment clogged by fine sand and mud with a high content of small hard substrates, by constant moderate bottom-currents which become weaker with increasing depth, and by small annual variations in temperature and salinity; the occurrence of an ostreobium sp. alga in the shell of G. vitreus indicates the involvement of the phytal system, as defined by Pérès (1982); (2) the G. vitreus biocoenosis, comprised of characteristic macrobenthic stocks (particularly polychaetes, mollusks, and epifaunal species on small hard substrates). Whatever the geomorphology, neighbouring circalittoral and bathyal biocoenoses have little influence on the G. vitreus biocoenosis, which displays a comparatively greater species richness and density. However, immigration of circalittoral species is encouraged by detrital sediments and water currents. The occurrence of this ecosystem as a distinct belt intercalated between circalittoral and bathyal zones is discussed. The ecosystem is considered to be ldquobathylittoralrdquo.
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