THE BENTHIC INFAUNA AND BENTHIC RESPIRATION OFF THE BANC-DARGUIN (MAURITANIA, NORTHWEST AFRICA)

Citation
Gca. Duineveld et al., THE BENTHIC INFAUNA AND BENTHIC RESPIRATION OFF THE BANC-DARGUIN (MAURITANIA, NORTHWEST AFRICA), Hydrobiologia, 258, 1993, pp. 107-117
Citations number
29
Categorie Soggetti
Marine & Freshwater Biology
Journal title
ISSN journal
00188158
Volume
258
Year of publication
1993
Pages
107 - 117
Database
ISI
SICI code
0018-8158(1993)258:<107:TBIABR>2.0.ZU;2-W
Abstract
In May 1988, a study was made of the benthic community structure and b enthic respiratory activity along two transects across the Mauritanian shelf off Banc d'Arguin. The main emphasis of the present paper is pu t on the macrobenthos, but results of a gross analysis of the meibenth os are discussed as well. Macrofaunal and meiofaunal density showed no consistent decrease with distance from the shore. The composition of the macrofauna taxa appeared to be closely correlated with sediment pa rameters and less so with depth. The highest macrofaunal biomass was f ound at the northern edge of the Banc d'Arguin, and the lowest biomass along the outer shelf. The biomass levels on the shelf match the ones reported for the northern Cap Blanc area where, in contrast to the se asonal upwelling in the investigated area, upwelling takes place all y ear round. Benthic respiration rates on the offshore shelf were relati vely high at the nearshore stations and low near the shelf break. Expe rimental evidence suggests that the low O2 levels in the upwelling wat er covering part of shelf, inhibited benthic respiration. The high res piratory activity at some northern inshore stations coincided with the presence of oxygen-rich coastal water. In this area benthic respirati on surpassed the level previously reported for the enriched Cap Blanc area. On the basis of our respiration data, an estimate is made of the total carbon demand of the benthic community on the shelf in May and this quantity is compared with the measurements of daily primary produ ction.