A hydrogen-dependent geochemical analogue of primordial carbon and energy metabolism

Preiner, Martina; Igarashi, Kensuke; Muchowska, Kamila; Yu, Mingquan; Varma, Sreejith J.; Kleinermanns, Karl; Nobu, Masaru K.; Kamagata, Yoichi; Tüysüz, Harun; Moran, Joseph; Martin, William F.

doi:10.1038/s41559-020-1125-6

A hydrogen-dependent geochemical analogue of primordial carbon and energy metabolism

Citer cette référence

PREINER, Martina, IGARASHI, Kensuke, MUCHOWSKA, Kamila, YU, Mingquan, VARMA, Sreejith J., KLEINERMANNS, Karl, NOBU, Masaru K., KAMAGATA, Yoichi, TÜYSÜZ, Harun, MORAN, Joseph et MARTIN, William F., 2020. A hydrogen-dependent geochemical analogue of primordial carbon and energy metabolism. Nature Ecology & Evolution. 2 avril 2020. Vol. 4, n° 4pp. 534-542. DOI 10.1038/s41559-020-1125-6.

Accès libre Peer reviewed
Version acceptée pour publication (post-print auteur)
Paternité - Pas d'utilisation commerciale - Partage selon les Conditions Initiales [CC] [BY] [NC] [SA]
Auteurs	Martina Preiner Kensuke Igarashi Kamila Muchowska Mingquan Yu Sreejith J. Varma Karl Kleinermanns Masaru K. Nobu Yoichi Kamagata Harun Tüysüz Joseph Moran William F. Martin
Unité de recherche du site	Institut de Science et d'Ingénierie Supramoléculaires - ISIS - UMR7006
Langue	en
Volume	4
Numéro	4
Page de début	534
Page de fin	542
Date de première publication	2020-04-02
ISSN	2397-334X
Titre de la source (revue, livre…)	Nature Ecology & Evolution
Résumé	Hydrogen gas, H2, is generated by alkaline hydrothermal vents through an ancient geochemical process called serpentinization in which water reacts with iron containing minerals deep within the Earth's crust. H2 is the electron donor for the most Show moreHydrogen gas, H2, is generated by alkaline hydrothermal vents through an ancient geochemical process called serpentinization in which water reacts with iron containing minerals deep within the Earth's crust. H2 is the electron donor for the most ancient and the only energy releasing route of biological CO2 fixation, the acetyl-CoA pathway. At the origin of metabolism, CO2 fixation by hydrothermal H2 within serpentinizing systems could have preceded and patterned biotic pathways. Here we show that three hydrothermal minerals—greigite (Fe3S4), magnetite (Fe3O4) and awaruite (Ni3Fe)—catalyse the fixation of CO2 with H2 at 100°C under alkaline aqueous conditions. The product spectrum includes formate (up to 200 mM), acetate (up to 100 µM), pyruvate (up to 10 µM), methanol (up to 100 µM), and methane. The results shed light on both the geochemical origin of microbial metabolism and on the nature of abiotic formate and methane synthesis in modern hydrothermal vents. Show less
DOI	10.1038/s41559-020-1125-6
Titre abrégé de la source	Nat Ecol Evol
Type de publication	article
Type de publication	ACL
Topic	Chimie/Autre
Unité de recherche extérieure au site	nstitute for Molecular Evolution, University of Düsseldorf, Düsseldorf, Germany Bioproduction Research Institute, National Institute of Advanced Industrial Science and Technology, Sapporo, Japan Max-Planck-Institut für Kohlenforschung, Mülheim an der Ruhr, Germany Charité—Universitätsmedizin Berlin, Laboratory ‘Biochemistry and System Biology of the Metabolism’, Berlin, Germany Institute for Physical Chemistry, University of Düsseldorf, Düsseldorf, Germany Bioproduction Research Institute, National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan Institute for Molecular Evolution, University of Düsseldorf, Düsseldorf, Germany
Fonction	aut
Identifiant ORCID	278516133
Identifiant idREF	184481198
Audience	International
Envoyer vers HAL	5
URL	https://univoak.eu/islandora/object/islandora:106644