From the Gulf of Aden along a transect to the central-northern Red Sea the abundance and taxonomic composition of metazoan plankton was studied during the southwest monsoon period (summer 1987). Samples were taken with 0.055 mm mesh nets down to a maximum depth of 1050 m. In the epipelagic zone, a distinct decrease in total plankton abundance was observed from south to north, which was much more pronounced in biomass (by a factor of up to 10) as compared to numbers (by a factor of 2). This could partly be explained by differences in the taxonomic and/or size composition of the planktonic fauna. Among non-calanoid copepods, 40 out of 75 species or taxa investigated decreased in abundance from south to north. Sixteen of these species were completely absent in the central-northern area Nineteen species or taxa, ho'ivever, showed the opposite feature of a higher abundance in the central-northern Red Sea. The stations were grouped according to sim~larities in the taxonomic composition of non-calanoid copepods in the epipelagic zone. The following 3 geographical regions could be separated: (1) Gulf of Aden and Strait of Bab a1 Mandab; (2) southern Red Sea, and (3) central-northern Red Sea. In the meso-and bathypelagic zones, regional differences were not evident. The results are discussed in relation to hydrographic conditions during summer 1987.
No takes yet. Share an insight, caveat, or question.
Ruth Böttger-Schnack (1995) studied this question.
Synapse has enriched 2 closely related papers on similar clinical questions. Consider them for comparative context: