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| | SCOPE 21 - The Major Biogeochemical Cycles and Their Interactions, Chapter 19, Interactions Between the Carbon and ... (Site not responding. Last check: 2007-11-03) |
 | | This appears to be a common microbial behaviour in the marine environment where, due to the powerful buffering capacity of the CO system, acidophilic and obligately sulphur oxidizing bacteria are not able to produce a pH low enough for a successful competition with the non-acidophilic bacteria (Tuttle and Jannasch, 1973). |
 | | Chemosynthesis based on the bacterial oxidation of hydrogen, ammonia, nitrite, iron, and possibly manganese may occur in marine and non-marine environments alike. |
 | | S for the electron source and, except for some assimilatory sulphate reduction, is not involved in the direct interaction between the sulphur and carbon cycles as shown in Figure 19.1. |
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