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Two of the largest crude oil-polluted areas in the world are the semi-enclosed Mediterranean and Red Seas, but the effect of chronic pollution remains incompletely understood on a large scale. We compared the influence of environmental and geographical constraints and anthropogenic forces (hydrocarbon input) on bacterial communities in eight geographically separated oil-polluted sites along the coastlines of the Mediterranean and Red Seas. The differences in community compositions and their biodegradation potential were primarily associated (P < 0.05) with both temperature and chemical diversity. Furthermore, we observed a link between temperature and chemical and biological diversity that was stronger in chronically polluted sites than in pristine ones where accidental oil spills occurred. We propose that low temperature increases bacterial richness while decreasing catabolic diversity and that chronic pollution promotes catabolic diversification. Our results further suggest that the bacterial populations in chronically polluted sites may respond more promptly in degrading petroleum after accidental oil spills.

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The thermal springs of Zerka Ma'in, with waters emerging at temperatures up to 63 degrees C, have been of interest to biologists already from the beginning of the 19th century. These waters, springing out from below ground and flowing into the hypersaline Dead Sea, form an isolated environment from a biogeographic point of view. We have investigated the molecular diversity of the cyanobacteria in the springs. The diversity discovered was large, defining operational taxonomic units (OTUs) by a cutoff of 97% similarity; 10 major OTUs were found, including an as yet unidentified cluster of cyanobacteria. The various patterns of similarities of our sequences to others obtained from different thermal environments worldwide led us to rethink the common theories in biogeography. Based on the data obtained, we suggest that there is no constant geographical separation of microorganisms; however, local speciation does occur at a rate dictated mainly by local community dynamics and the rate of entrance of new organisms into the ecosystem.