In situ suspension feeding behaviour of the pearl oyster, Pinctada margaritifera: combined effects of body size and weather-related seston composition

Citation
S. Pouvreau et al., In situ suspension feeding behaviour of the pearl oyster, Pinctada margaritifera: combined effects of body size and weather-related seston composition, AQUACULTURE, 181(1-2), 2000, pp. 91-113
Citations number
55
Categorie Soggetti
Aquatic Sciences
Journal title
AQUACULTURE
ISSN journal
00448486 → ACNP
Volume
181
Issue
1-2
Year of publication
2000
Pages
91 - 113
Database
ISI
SICI code
0044-8486(20000101)181:1-2<91:ISSFBO>2.0.ZU;2-4
Abstract
In situ clearance rate (CR) and biodeposition of the black pearl oyster, Pi nctada margaritifera, were followed during several field experiments from 1 996 to 1998 in the lagoon of Takapoto. Serial measurements of total particu late matter (TPM, mg l(-1)), particulate inorganic matter (PLM, mg l(-1)), and particulate organic matter (POM, mg l(-1)) were related to meteorologic al conditions, especially wind speed. As a general case, POM and PLM increa sed with wind speed. Nevertheless, PLM increased faster than POM so that th e organic content (OC, %) of the TPM decreased progressively when wind spee d increased. These TPM variations induced direct changes in feeding process es of P. margaritifera. CR (l h(-1)) averaged 22 l h(-1) for a pearl oyster of 1 g dry tissue weight and varied with POM, PLM and dry tissue weight (W , g) according to the following equation: CR = 26.96 (PIM-0.42POMW0.61)-W-0 .96. This clearance activity appeared to be the highest of those mentioned for bivalve species in their natural habitats. Pseudofaecal (PF, mg h(-1)) production started for very low PIM load (i.e., 0.17 mg l(-1))and POM load (i.e., 0.28 mg l(-1))in water and followed the equation: PF = 32.6(POM - 0. 28)(PIM - 0.17)W-0.77. In other bivalve species, PF are generally observed for higher PIM or POM levels. These PF were mainly constituted of mineral m atter (more than 80% in weight). Faecal production (F, mg h(-1)) increased with seston load and reached progressively a plateau (i.e., maximal intesti nal transit time) as shown by the equation describing the faecal biodeposit ion F = 20 W-0.49(1 - e(-0.66) (TPM)). The quantity and the composition of the faecal biodeposit were in a range commonly found in literature. This wo rk confirms, by in situ experiments, previous results obtained in laborator y and especially that P. margaritifera has developed a trophic strategy whi ch consists of processing large amounts of water to gain sufficient energy in poor waters. But this work also showed that meteorological conditions ha ve indirect influences on feeding processes of pearl oyster by modifying si gnificantly the concentration and the composition of seston. (C) 2000 Elsev ier Science B.V. All rights reserved.