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Structure, fonctionnement, évolution des communautés benthiques ...

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tel-00009359, version 1 - 1 Jun 2005<br />

Chapitre 3 - Fonctionnement du réseau trophique benthique de la Grande Vasière<br />

At a second level (figure 2) a group of five taxa was clearly separated from all others. This<br />

group is composed of benthic suspension feeders, zooplankton and suprabenthic crustacea; (TL close<br />

to 2 and δ 13 C close to –20‰). A difference of 3.4‰ in the δ 15 N value is observed between POM<br />

values and values for ascidians and the crustacean C. subterranea, two taxa considered in the literature<br />

as suspension feeders exploiting the water layer above sediment. Such a difference is also found for<br />

zooplankton and suprabenthos which are known to feed on POM of the water column. Moreover this<br />

validates the value of the enrichment factor retained in the equation used to determine trophic level<br />

and confirms that these taxa are the primary consumers.<br />

Subgroup 2b is composed of two bivalves and a burrowing crustacean with a TL close to 2.5<br />

(δ 15 N: 8-10‰). A 3.8‰ δ 13 C gap between the consumers of the pelagic primary production and these<br />

others microphageous species reveals that they feed on different types of organic particles. This range<br />

of δ 13 C differences between POM and benthic consumers, and between benthic suspension and deposit<br />

feeders, has already been observed in offshore (Hobson et al. 1995, 2002) and coastal (Herman et al.<br />

2000) benthic ecosystems.<br />

The bivalve A. opercularis is a filter feeder species which feeds on organic particles in<br />

suspension in the two first centimeters of the water layer just above the sediment surface, while<br />

N. sulcata is a surface deposit-feeder. The position of the Pectinidae species in this “benthic deposit<br />

feeder group” indicates that suspension feeders must be carefully considered in energy budget and<br />

functional analyses and that behavior and nutritional anatomical organs are not always sufficient to<br />

affect species in trophic groups. Furthermore, we can deduce that in the ecosystem of the Great Mud<br />

Bank, either the quality of the suspended particles change drastically in the first centimeters of the<br />

water layer above the sediment and that this change is sufficiently stable in time to induce different<br />

isotopic signatures in the tissue of consumers and/or that these species could differ in particle selection<br />

efficiency. A. opercularis lies on the sediment and could possibly ingest a higher rate of interface<br />

superficial film than ascidians, which have inhalant siphons a few centimeters above the interface. In<br />

the same manner, the polychaeta H. fauveli is positioned to feed at the apex of its tube erected four or<br />

five centimeters above the sediment. Owens (1987) found that the δ 15 N of plant species increased<br />

throughout the decomposition process and when considering specifically phytoplankton the amount of<br />

total N decreased in conjunction with the decomposition of phytoplankton cells, whereas δ 15 N<br />

abundance increased gradually in residual organic matter (Wada and Hattori 1991). As no primary<br />

production can occur at a mean depth of 110 m in the Great Mud Bank ecosystem, the diet of deposit<br />

feeders must be composed exclusively of deposited material both detritic and recycled from the<br />

benthic organisms. This feeding pattern is quite different from that of coastal shallow ecosystems in<br />

which microphytobenthos can be an important food source for deposit feeders (Riera et al. 1996;<br />

Middelburg et al. 2000). Such differences within the benthic primary consumers were shown by<br />

Herman et al. (2000) for a small tidal flat where suspension feeders (mainly on a planktonic algal diet)<br />

showed δ 13 C values 4 to 6‰ less than those of deposit feeders (mainly on a benthic microalgal diet).<br />

Goering et al. (1990) and Hobson et al. (1995) suggested that deposited phytoplankton was enriched in<br />

13<br />

C in the bottom nepheloid layer due to recycling across the microbial loop. The different feeding<br />

behaviors of the species may also be a factor accounting for the observed differences in δ 13 C. As some<br />

species are non-selective and others selective microphages. In the latter case, particle selection may be<br />

based on quality as well as size. Some bivalves have a diet based not only on deposited material,<br />

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