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Observations dans les zones peu accessibles de l'environnement bathyal (biologie et geologie) grace a l'usage des soucoupes plongeantes ArchiMer
Roux, M.
On the bathyal slope for continental margins, steep and rocky substrates punctuated with cliffs and collapsing zones are frequently found. As survey and sampling with the classical technics from the sea surface is practically impossible in such an environment, in situ exploration with a submersible allows significant advances in ecology, with implications in paleoenvironment reconstruction. Mixing of material from shallow-water and deep-sea origins into bathyal sedimentation suggests that the so-called "fossil assemblages of outer platform" were frequently misinterpreted. Dense populations of animals closely related to fossil groups which were only considered as relict of the Past ("living fossils") and previously interpreted as shallow-water inhabitants...
Tipo: Text Palavras-chave: Continental margins; Bathyal zone; Diving; Cruises; Sedimentation; Biomass; Geology; Biology; Imaging techniques; Image processing; Marine technology; Underwater photography; Submersibles.
Ano: 1990 URL: http://archimer.ifremer.fr/doc/1990/acte-1138.pdf
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Striocadulud magdalenensis, a new deep-sea scaphopod (Mollusca: Scaphopoda:Gadilidae) from the Colombian Caribbean OceanDocs
Gracia-C., A.; Ardila, N.E..
We describe a new bathyal species of scaphopod beloning to the genus Striocadulus Emerson based on conchological and radular characters. The specimens were collected at a depth of 404-412 m off Bocas de Ceniza (Colombian Caribbean). Striocadulus magdalenensis new species can be distinguised from its other congeners by differences in its apical section, and both number and extent of longitudianl striae. This is the first record of this genus in the Atlantic Ocean.
Tipo: Journal Contribution Palavras-chave: Bathyal zone; Taxonomy; Marine molluscs; Bathyal zone; Taxonomy; Http://aims.fao.org/aos/agrovoc/c_840; Http://aims.fao.org/aos/agrovoc/c_7631.
Ano: 2009 URL: http://hdl.handle.net/1834/3613
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