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Distributions of Microbial Activities in Deep Subseafloor Sediments

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TLDR
Diverse microbial communities and numerous energy-yielding activities occur in deeply buried sediments of the eastern Pacific Ocean and these sedimentary communities may supply dissolved electron donors and nutrients to the underlying crustal biosphere.
Abstract
Diverse microbial communities and numerous energy-yielding activities occur in deeply buried sediments of the eastern Pacific Ocean. Distributions of metabolic activities often deviate from the standard model. Rates of activities, cell concentrations, and populations of cultured bacteria vary consistently from one subseafloor environment to another. Net rates of major activities principally rely on electron acceptors and electron donors from the photosynthetic surface world. At open-ocean sites, nitrate and oxygen are supplied to the deepest sedimentary communities through the underlying basaltic aquifer. In turn, these sedimentary communities may supply dissolved electron donors and nutrients to the underlying crustal biosphere.

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Oceanic methane biogeochemistry.

TL;DR: It is shown that thermodynamic and kinetic constraints largely prevent large-scale methanogenesis in the open ocean water column, and the role of anaerobic oxidation of methane has changed from a controversial curiosity to a major sink in anoxic basins and sediments.
Journal ArticleDOI

Manganese- and Iron-Dependent Marine Methane Oxidation

TL;DR: It is shown that microorganisms from marine methane-seep sediment in the Eel River Basin in California are capable of using manganese and iron to oxidize methane, revealing that marine AOM is coupled, either directly or indirectly, to a larger variety of oxidants than previously thought.
Journal ArticleDOI

Bacteria and archaea on Earth and their abundance in biofilms

TL;DR: It is proposed that biofilms drive all biogeochemical processes and represent the main way of active bacterial and archaeal life and are the most prominent and influential type of microbial life.
Journal ArticleDOI

Global distribution of microbial abundance and biomass in subseafloor sediment

TL;DR: This work shows that total microbial cell abundance in subseafloor sediment varies between sites by ca.
References
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Journal ArticleDOI

Prokaryotes: The unseen majority

TL;DR: The number of prokaryotes and the total amount of their cellular carbon on earth are estimated to be 4-6 x 10(30) cells and 350-550 Pg of C (1 Pg = 10(15) g), respectively, which is 60-100% of the estimated total carbon in plants.
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Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis

TL;DR: Pore water profiles of total CO 2, pH, PO 3−4, NO − 3 plus NO − 2, SO 2− 4, S 2−, Fe 2+ and Mn 2+ have been obtained in cores from pelagic sediments of the eastern equatorial Atlantic under waters of moderate to high productivity as mentioned in this paper.
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The deep hot biosphere

TL;DR: There are strong indications that microbial life is widespread at depth in the crust of the Earth, just as such life has been identified in numerous ocean vents as discussed by the authors, and such life is not dependent on solar energy and photosynthesis for its primary energy supply, and it is essentially independent of the surface circumstances.
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Recent studies on bacterial populations and processes in subseafloor sediments: A review

TL;DR: The authors showed that in the presence of readily degradable organic substrates, actively growing bacteria can move faster than sediment deposition; hence, these bacteria are not necessarily trapped and buried.
Journal ArticleDOI

Metabolic Activity of Subsurface Life in Deep-Sea Sediments

TL;DR: Global maps of sulfate and methane in marine sediments reveal two provinces of subsurface metabolic activity: a sulfate-rich open-ocean province, and an ocean-margin province where sulfate is limited to shallow sediments.
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