Prokaryotes stimulate mineral H2 formation for the deep biosphere and subsequent thermogenic activity

Parkes, Ronald John, Linnane, Cathal David, Webster, Gordon ORCID: https://orcid.org/0000-0002-9530-7835, Sass, Henrik ORCID: https://orcid.org/0000-0001-8740-4224, Weightman, Andrew John ORCID: https://orcid.org/0000-0002-6671-2209, Hornibrook, Ed R. C. and Horsfield, Brian 2011. Prokaryotes stimulate mineral H2 formation for the deep biosphere and subsequent thermogenic activity. Geology 39 (3) , pp. 219-222. 10.1130/G31598.1

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Abstract

The deep subseafloor biosphere contains two-thirds of Earth's prokaryotic biomass this may indicate the presence of novel mechanisms of energy generation as temperatures increase in the subsurface. In sediment slurry experiments (0–100 °C) with a range of common minerals and rocks (including basalt and quartz), there is significant H2 formation at elevated temperatures, but only in the presence of prokaryotes. This stimulates further prokaryotic activity, typical of deep sediments (sulfate reduction, acetogenesis, and CO2 production, plus continuing methanogenesis), and Bacteria and Archaea representative of many deep sediment types develop. H2 and acetate formation is particularly stimulated above 70 °C. This prokaryotic activity even enhances reactions when temperatures are raised to thermogenic levels (∼125–155 °C), including hydrocarbon generation. Mechanochemistry may be important for mineral H2 formation; this is enhanced by prokaryotes (biomechanochemistry), and subsurface stress and fracturing, which is widespread on Earth.

Item Type:	Article
Date Type:	Publication
Status:	Published
Schools:	Biosciences Earth and Environmental Sciences
Subjects:	Q Science > QE Geology Q Science > QR Microbiology
Publisher:	Geological Society of America
ISSN:	0091-7613
Funders:	NERC
Last Modified:	02 Dec 2022 11:16
URI:	https://orca.cardiff.ac.uk/id/eprint/7563

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