Cited by 13Origins and Evolution of LifePaleontology and Stratigraphy of FossilsEarth Systems and Cosmic Evolution

The Moon‐Forming Impact and the Autotrophic Origin of Life

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Mrnjavac, Natalia, Wimmer, Jessica L. E., Brabender, Max, Schwander, Loraine, Martin, William F.·2023·ChemPlusChem

Abstract

The Moon‐forming impact vaporized part of Earth's mantle, and turned the rest into a magma ocean, from which carbon dioxide degassed into the atmosphere, where it stayed until water rained out to form the oceans. The rain dissolved CO 2 and made it available to react with transition metal catalysts in the Earth's crust so as to ultimately generate the organic compounds that form the backbone of microbial metabolism. The Moon‐forming impact was key in building a planet with the capacity to generate life in that it converted carbon on Earth into a homogeneous and accessible substrate for organic synthesis. Today all ecosystems, without exception, depend upon primary producers, organisms that fix CO 2. According to theories of autotrophic origin, it has always been that way, because autotrophic theories posit that the first forms of life generated all the molecules needed to build a cell from CO 2, forging a direct line of continuity between Earth's initial CO 2‐rich atmosphere and the first microorganisms. By modern accounts these were chemolithoautotrophic archaea and bacteria that initially colonized the crust and still inhabit that environment today.

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Crossref · 10.1002/cplu.202300270

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  • In water and in the absence of enzymes, solid-state metals generate methyl groups from H2 and CO2, producing formate, acetate, pyruvate and methane, replacing the function of over 100 enzymes.

    “In water and in the absence of enzymes, the solid‐state metals generate methyl groups from H2 and CO2, producing formate, acetate, pyruvate and methane, replacing the function of over 100 enzymes [76].”
  • These reactions generate the backbone of carbon and energy for metabolism.

    “These reactions generate the backbone of carbon and energy for metabolism [102].”

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References 230 · Cited by 13

Authors
Mrnjavac, N., Wimmer, J. L. E., Brabender, M., Schwander, L., & Martin, W. F.
Affiliations
Heinrich Heine University Düsseldorf (DE)
Corresponding author
Mrnjavac, Natalia
Venue
ChemPlusChem
Publisher
Wiley
Published
2023-10-19
Volume
88
Issue
11
Pages
e202300270-e202300270
ISSN
2192-6506 (ISSN-L)
OpenAlex
W4387439919
Cited by
13
References
230
Citations by year
2026: 4 · 2025: 1 · 2024: 8
FWCI
0.33
Type
journal article
Language
en
Open access
Locations
  • ChemPlusChem (publishedVersion, cc-by-nc)
  • PubMed (publishedVersion)
  • PubMed Central (acceptedVersion, cc-by-nc)
Funders
  • Deutsche Forschungsgemeinschaft (MA 1426/21-1)
  • Volkswagen Foundation (96742)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Earth Systems and Cosmic Evolution
Keywords
Moon-forming impact, magma ocean, CO2 degassing, early Earth atmosphere, ocean formation, transition metal catalysts, organic synthesis, primary producers, chemolithoautotrophic bacteria, microbial metabolism
MeSH terms
Atmosphere, Carbon Dioxide, Moon, Ecosystem, Earth, Planet

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