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On the origins of life’s homochirality: Inducing enantiomeric excess with spin-polarized electrons

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Ozturk, S. Furkan, Sasselov, Dimitar D.·2022·Proceedings of the National Academy of Sciences

Abstract

Life as we know it is homochiral, but the origins of biological homochirality on early Earth remain elusive. Shallow closed-basin lakes are a plausible prebiotic environment on early Earth, and most are expected to have significant sedimentary magnetite deposits. We hypothesize that ultraviolet (200- to 300-nm) irradiation of magnetite deposits could generate hydrated spin-polarized electrons sufficient to induce enantioselective prebiotic chemistry. Such electrons are potent reducing agents that drive reduction reactions where the spin polarization direction can enantioselectively alter the reaction kinetics. Our estimate of this chiral bias is based on the strong effective spin-orbit coupling observed in the chiral-induced spin selectivity (CISS) effect, as applied to energy differences in reduction reactions for different isomers. In the original CISS experiments, spin-selective electron transmission through a monolayer of double-strand DNA molecules is observed at room temperature-indicating a strong coupling between molecular chirality and electron spin. We propose that the chiral symmetry breaking due to the CISS effect, when applied to reduction chemistry, can induce enantioselective synthesis on the prebiotic Earth and thus facilitate the homochiral assembly of life's building blocks.

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  • Spontaneous homochiral symmetry breaking happened in a heterogeneous rather than a homogeneous environment such as space interstellar clouds, deep sea smokers or hydrothermal pools, where organic and inorganic compounds could have interacted due to external forces like radiation, heat or both.

    “To our understanding, spontaneous homochiral symmetry breaking happened in a heterogeneous rather than a homogeneous environment such as space interstellar clouds, deep sea smokers or hydrothermal pools, where organic (carbon-based compounds) and inorganic (essentially minerals) compounds could have interacted due to external forces like radiation, heat or both.”

    From The Origin and Early Evolution of Life: Homochirality Emergence in Prebiotic Environments (2023) · cites this paper as Ozturk and Sasselov, 2022

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Authors
Ozturk, S. F., & Sasselov, D. D.
Affiliations
Harvard University (US)
Corresponding author
Ozturk, S. Furkan
Venue
Proceedings of the National Academy of Sciences
Published
2022-07-05
Volume
119
Issue
28
Pages
e2204765119-e2204765119
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W4221157426
Cited by
119
References
9
Citations by year
2026: 25 · 2025: 33 · 2024: 34 · 2023: 22 · 2022: 5
FWCI
9.40
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion, cc-by)
  • PubMed Central (publishedVersion, cc-by)
  • PubMed (publishedVersion)
  • arXiv (Cornell University) (submittedVersion)
  • arXiv (Cornell University) (cc-by)
Funders
Simons Foundation (290360)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Space Science and Extraterrestrial Life
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
homochirality, origin of life, enantiomeric excess, polarized electrons, magnetite, UV irradiation, chirality-induced spin selectivity, spin-orbit coupling, asymmetric reduction, prebiotic chemistry, early Earth, chiral symmetry breaking
MeSH terms
DNA, Electrons, Stereoisomerism, Earth, Planet, Ferrosoferric Oxide

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