CONTINENTAL-SHELF UPWELLING AND BENTHIC OSTRACODA IN THE BENGUELA SYSTEM (SOUTHEASTERN ATLANTIC-OCEAN)

Authors
Citation
Rv. Dingle, CONTINENTAL-SHELF UPWELLING AND BENTHIC OSTRACODA IN THE BENGUELA SYSTEM (SOUTHEASTERN ATLANTIC-OCEAN), Marine geology, 122(3), 1995, pp. 207-225
Citations number
44
Categorie Soggetti
Oceanografhy,Geology,"Geosciences, Interdisciplinary
Journal title
ISSN journal
00253227
Volume
122
Issue
3
Year of publication
1995
Pages
207 - 225
Database
ISI
SICI code
0025-3227(1995)122:3<207:CUABOI>2.0.ZU;2-W
Abstract
The distribution of benthic Ostracoda (micro-crustacea) on the contine ntal shelf off southwestern Africa is controlled by sea-floor physical and chemical parameters, which in turn can be correlated with the pos itions of quasi-permanent upwelling cells of the Benguela System. The linkage between benthic and surface physico-chemical environments (and consequently between benthos and surface parameters) is not direct, h owever, being modulated by equatorward motion in the upper water colum n, benthic poleward water-motion, fluvial input and cross-shelf advect ion of off-shelf water. These phenomena, and in particular the intensi ty of surface upwelling, show a sharp distinction about approximately 27 S, so that the ostracod faunas in the Northern Benguela Region are relatively sparse and dominated by Palmoconcha walvisbaiensis, (Hartma nn) and Cytherella namibensis, Dingle, while in the Southern Benguela Region the faunas are more diverse and dominated by Pseudokeijella lep ralioides, (Brady) and Ruggieria cytheropteroides, (Brady). When minor taxa are also considered, each cell in the Benguela upwelling system is shown to be associated with a unique ostracod fauna which can be re lated to its in particular environmental characteristics.