Evidence for archaeal methanogenesis within veins at the onshore serpentinite-hosted Chimaera seeps, Turkey

Autor(en)

Jennifer Zwicker, Daniel Birgel, Wolfgang Bach, Sylvain Richoz, Daniel Smrzka, Bernhard Grasemann, Susanne Gier, Christa Schleper, Simon Karl-Maria Rasso Rittmann, Erdal Kosun, Jörn Peckmann

Abstrakt

Serpentinite-hosted ecosystems are potential sites where life may first have evolved on Earth. Serpentinization reactions produce strongly reducing and highly alkaline fluids that are typified by high concentrations of molecular hydrogen (H2) and methane (CH4), which can be used as an energy source by chemosynthetic life. Low-temperature serpentinization at slow-spreading mid-ocean ridges provides an ideal environment for rich microbial communities. Similar environments have also been discovered on land, where present-day low temperature serpentinization occurs during the circulation of groundwater through exposed ophiolites, triggering the production of CH4 and H2, as well as the precipitation of secondary carbonate minerals. The rock samples analyzed here are from the Chimaera seeps in Turkey, representing serpentinized peridotites that are cross-cut by veins composed of brucite and hydromagnesite. Hydromagnesite features a mean δ13C value of −19.8‰ caused by kinetic isotope fractionation during air-groundwater exchange of CO2, followed by CO2 hydroxylation to bicarbonate within the groundwater. Geochemical modeling revealed that mixing of Mg- and Ca-rich groundwaters is required for hydromagnesite formation at the expense of brucite. Within the carbonate-hydroxide veins the lipid biomarkers pentamethylicosane (PMI) and squalane with δ13C values of +10‰ and +14‰, respectively, and unsaturated derivatives thereof were identified. Archaeol, sn2-hydroxyarchaeol, and sn3-hydroxyarchaeol are other prominent archaeal biomarkers in the veins, also revealing high δ13C values from +6 to +13‰. These isotope patterns combined with the absence of crocetane – a biomarker for methanotrophic archaea – reveal that the microbial communities of the Chimaera seeps performed methanogenesis from a CO2-limited pool rather than methanotrophy. Moreover, bacterial dialkyl glycerol diethers (DAGEs) with unusually high δ13C values (−9 to −2‰) and minor monoalkyl glycerol monoethers (MAGEs) were identified, suggesting that bacterial sulfate reduction is also active at the Chimaera site. This study reveals that archaeal methanogenesis and bacterial sulfate reduction may be prominent at onshore peridotite-hosted sites, and that biogenic CH4 may contribute to abiotic CH4 emissions from terrestrial seeps.

Organisation(en)

Institut für Geologie

Externe Organisation(en)

Universität Hamburg, Lund University, Akdeniz University, Universität Bremen, Karl-Franzens-Universität Graz

Journal

Chemical Geology

Band

483

Seiten

567-580

Anzahl der Seiten

14

ISSN

0009-2541

DOI

https://doi.org/10.1016/j.chemgeo.2018.03.027

Publikationsdatum

04-2018

Peer-reviewed

Ja

ÖFOS 2012

105128 Geomikrobiologie, 105105 Geochemie, 105120 Petrologie

Schlagwörter

ASJC Scopus Sachgebiete

Geochemistry and Petrology, Geology

Sustainable Development Goals

SDG 15 – Leben an Land

Link zum Portal

https://ucrisportal.univie.ac.at/de/publications/3101bd98-f061-4384-b3dc-110b0ef3db72