Serpentinization: Connecting geochemistry, ancient metabolism and industrial hydrogenation
Preiner, Martina; Xavier, Joana C.; Sousa, Filipa L.; Zimorski, Verena; Neubeck, Anna; Lang, Susan Q.; Greenwell, Chris; Kleinermanns, Karl; Tüysüz, Harun; McCollom, Tom M.; Holm, Nils G.; Martin, William F.
Joana C. Xavier
Filipa L. Sousa
Susan Q. Lang
Professor Chris Greenwell firstname.lastname@example.org
Head Of Department
Tom M. McCollom
Nils G. Holm
William F. Martin
Rock–water–carbon interactions germane to serpentinization in hydrothermal vents have occurred for over 4 billion years, ever since there was liquid water on Earth. Serpentinization converts iron(II) containing minerals and water to magnetite (Fe3O4) plus H2. The hydrogen can generate native metals such as awaruite (Ni3Fe), a common serpentinization product. Awaruite catalyzes the synthesis of methane from H2 and CO2 under hydrothermal conditions. Native iron and nickel catalyze the synthesis of formate, methanol, acetate, and pyruvate—intermediates of the acetyl-CoA pathway, the most ancient pathway of CO2 fixation. Carbon monoxide dehydrogenase (CODH) is central to the pathway and employs Ni0 in its catalytic mechanism. CODH has been conserved during 4 billion years of evolution as a relic of the natural CO2-reducing catalyst at the onset of biochemistry. The carbide-containing active site of nitrogenase—the only enzyme on Earth that reduces N2—is probably also a relic, a biological reconstruction of the naturally occurring inorganic catalyst that generated primordial organic nitrogen. Serpentinization generates Fe3O4 and H2, the catalyst and reductant for industrial CO2 hydrogenation and for N2 reduction via the Haber–Bosch process. In both industrial processes, an Fe3O4 catalyst is matured via H2-dependent reduction to generate Fe5C2 and Fe2N respectively. Whether serpentinization entails similar catalyst maturation is not known. We suggest that at the onset of life, essential reactions leading to reduced carbon and reduced nitrogen occurred with catalysts that were synthesized during the serpentinization process, connecting the chemistry of life and Earth to industrial chemistry in unexpected ways.
Preiner, M., Xavier, J. C., Sousa, F. L., Zimorski, V., Neubeck, A., Lang, S. Q., …Martin, W. F. (2018). Serpentinization: Connecting geochemistry, ancient metabolism and industrial hydrogenation. Life, 8(4), Article 41. https://doi.org/10.3390/life8040041
|Journal Article Type||Article|
|Acceptance Date||Sep 20, 2018|
|Online Publication Date||Sep 22, 2018|
|Publication Date||Sep 22, 2018|
|Deposit Date||Sep 20, 2018|
|Publicly Available Date||Sep 26, 2018|
|Peer Reviewed||Peer Reviewed|
Published Journal Article
Publisher Licence URL
© 2018 by the authors. Licensee MDPI, Basel, Switzerland. This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).