High reactivity of deep biota under anthropogenic CO2 injection into basalt

Trias, Rosalia; Ménez, Bénédicte; le Campion, Paul; Zivanovic, Yvan; Lecourt, Léna; Lecoeuvre, Aurélien; Schmitt-Kopplin, Philippe; Uhl, Jenny; Gislason, Sigurður R.; Alfreðsson, Helgi A.; Mesfin, Kiflom G.; Snæbjörnsdóttir, Sandra Ó.; Aradóttir, Edda S.; Gunnarsson, Ingvi; Matter, Juerg M.; Stute, Martin; Oelkers, Eric H.; Gérard, Emmanuelle

doi:10.1038/s41467-017-01288-8

Title: High reactivity of deep biota under anthropogenic CO₂ injection into basalt

Journal Article · Fri Oct 20 00:00:00 EDT 2017 · Nature Communications

DOI:https://doi.org/10.1038/s41467-017-01288-8· OSTI ID:1499988

Trias, Rosalia ^[1];

^[1]; le Campion, Paul ^[1]; Zivanovic, Yvan ^[2]; Lecourt, Léna ^[1]; Lecoeuvre, Aurélien ^[3]; Schmitt-Kopplin, Philippe ^[4]; Uhl, Jenny ^[4]; Gislason, Sigurður R. ^[5]; Alfreðsson, Helgi A. ^[5]; Mesfin, Kiflom G. ^[5]; Snæbjörnsdóttir, Sandra Ó. ^[5]; Aradóttir, Edda S. ^[6]; Gunnarsson, Ingvi ^[6]; Matter, Juerg M. ^[7]; Stute, Martin ^[8]; Oelkers, Eric H. ^[9]; Gérard, Emmanuelle ^[1]

CNRS and Univ. Paris Diderot (France). Paris Inst. of Earth Physics (IPGP). Research Center on the Geological Storage of CO2
Univ. Paris-Sud, Orsay (France). Inst. of Integrative Biology of the Cell
CNRS and Univ. Paris Diderot (France). Paris Inst. of Earth Physics (IPGP)
Helmholtz-Zentrum Muenchen-German Research Center for Environmental Health, Neuherberg (Germany). Research Unit Analytical Biogeochemistry
Univ. of Iceland, Reykjavik (Iceland). Inst. of Earth Sciences
Reykjavik Energy (Iceland)
Univ. of Southampton (United Kingdom). Ocean and Earth Science; Columbia Univ., Palisades, NY (United States). Lamont-Doherty Earth Observatory
Columbia Univ., Palisades, NY (United States). Lamont-Doherty Earth Observatory; Barnard College, New York, NY (United States)
Univ. of Iceland, Reykjavik (Iceland). Inst. of Earth Sciences; Paul Sabatier Univ., Toulouse (France); Univ. College London (United Kingdom). Earth Sciences

Basalts are recognized as one of the major habitats on Earth, harboring diverse and active microbial populations. Inconsistently, this living component is rarely considered in engineering operations carried out in these environments. This includes carbon capture and storage (CCS) technologies that seek to offset anthropogenic CO₂ emissions into the atmosphere by burying this greenhouse gas in the subsurface. Here, we show that deep ecosystems respond quickly to field operations associated with CO₂ injections based on a microbiological survey of a basaltic CCS site. Acidic CO₂-charged groundwater results in a marked decrease (by ~ 2.5–4) in microbial richness despite observable blooms of lithoautotrophic iron-oxidizing Betaproteobacteria and degraders of aromatic compounds, which hence impact the aquifer redox state and the carbon fate. Host-basalt dissolution releases nutrients and energy sources, which sustain the growth of autotrophic and heterotrophic species whose activities may have consequences on mineral storage.

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Research Organization:: Columbia Univ., Palisades, NY (United States); CNRS and Univ. Paris Diderot (France); Univ. Paris-Sud, Orsay (France)

Sponsoring Organization:: USDOE Office of Fossil Energy (FE); Total S.A. (France); Schlumberger; French Environment and Energy Management Agency (ADEME) (France); French National Research Agency (ANR) (France); European Union (EU)

Grant/Contract Number:: FE0004847; ANR-08-PCO2-003-03; ANR-14-CE01-0008-01; 624382

OSTI ID:: 1499988

Journal Information:: Nature Communications, Vol. 8; ISSN 2041-1723

Publisher:: Nature Publishing GroupCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 35 works

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