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OmniScriptum Structure et fonctionnement du récif corallien: Rôle des sédiments dans le transfert de matière et d'énergie (Omn.Univ.Europ.)

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Description

Les récifs coralliens sont des écosystèmes très productifs. Alors que les coraux et les poissons ont fait l'objet de nombreuses études, le rôle des sédiments reste encore méconnu. Afin d'évaluer leur implication, 3 thématiques ont été développées. 1- La caractérisation physicochimique des eaux et des sédiments a montré un état de perturbation limité. 2- L'étude du métabolisme a mis en évidence des sédiments hétérotrophes (respiration > production brute). Les caractéristiques physicochimiques et métaboliques du récif reflètent une double influence océan-terre: les stations les plus productives et hétérotrophes se situent dans l'arrière-récif où l'influence océanique est minime. 3- La macrofaune est un groupe minoritaire dans le réseau trophique, sa distribution est fonction de l'hydrodynamisme. Par opposition, la mégafaune est largement représentée surtout dans les sédiments très productifs. En conclusion, les sédiments jouent un rôle clé dans le fonctionnement du récif corallien: ils soutiennent le développement d'une faune importante permettant de stocker, de transformer, de produire de la matière et de l'énergie qui seraient alors perdues sous l'effet de l'hydrodynamisme.

Product Specifications

Format
paperback
Domain
Amazon UK
Release Date
19 November 2010
Listed Since
22 November 2010

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