Distinct bacterial communities were found in the sediments of the northwest African upwelling area a t 17 and 2 l o N compared to a n area with low upwelling intensities at 29 and 35"N. The bacterial cominunity of the central upwelling area at 17/21N consisted of approximately equal proportions of Gram-negative strains belonging mainly to the genera Alterornonas and Vibrio; most of them were psychrophlles. This could be due to the upwelhng of cold water masses in this region, where sediment temperatures were on average 2C lower than in the northern part of this upwelling area. Here, Gram-positive psychrotrophic Bacillus strains predominated, tolerating growth temperatures higher than 24C A high proportion of these Bacillus stralns fermented various carbohydrates and sugar alcohols and uulized citrate as sole source of carbon and energy. In contrast, the abilities to utilize some glycosides, starch, chitin, fats and proteins, to degrade various N-compounds like DNA or arginine, and to reduce nitrates to nitrites were more pronounced in strains from the central upwelling area.
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H-J Rüger (1989) studied this question.
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