Biogeochemical implications of the ubiquitous colonization of marine habitats and redox gradients by Marinobacter species.

A number of studies suggest Marinobacter may be significant in ‘low-temperature’ hydrothermal systems, defined by low-temperature hydrothermalism (e.g., ~8 to ~40°C, McCollom and Shock, 1997 ) or ambient seawater temperatures (e.g., ~2° in the deep ocean).

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