Deep marine biosphere fuelled by increasing organic matter availability during burial and heating
Deep marine biosphere fuelled by increasing organic matter availability during burial and heating"
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Deep-sea sediments become apparently more hostile to life with increasing depth as temperature and pressure rise, and organic matter becomes increasingly recalcitrant. Demonstrations of high
bacterial populations in deep sediments1,2 may thus appear enigmatic. How, then, can the continued presence of active bacterial populations in deep sediments that are over 10 million years
old be explained? Although volatile fatty acids, particularly acetate, are important intermediates in the anaerobic degradation of organic matter3,4, their concentrations are kept very low
in sediments (
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Deep marine biosphere fuelled by increasing organic matter availability during burial and heatingDeep-sea sediments become apparently more hostile to life with increasing depth as temperature and pressure rise, and or...
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