Abiotic redox reactions in hydrothermal mixing zones: Decreased energy availability for the subsurface biosphere

Hot Temperature 550 Hydrothermal vent Bioenergetics Biogeochemistry 01 natural sciences Hydrothermal Vents 13. Climate action Physical Sciences Subsurface biosphere Seawater 14. Life underwater Oxidation-Reduction Hydrogen 0105 earth and related environmental sciences
DOI: 10.1073/pnas.2003108117 Publication Date: 2020-08-12T23:50:12Z
ABSTRACT
Significance Hydrothermal fluid geochemistry exerts a key control on subseafloor microbial community structure and function. However, the effects of metabolic activity, thermal decomposition biomass, abiotic reactions remain unconstrained. Depletions in molecular hydrogen enrichments methane submarine hydrothermal mixing zones have been interpreted to reflect influence an active biosphere. In contrast, our work reveals that these chemical shifts are driven by thermogenic processes at temperatures beyond limit for life. These findings critical implications constraining extent which global geochemical cycles can sustain deep biosphere, budget.
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