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Cosmic dust fertilization of glacial prebiotic chemistry on early Earth

Abstract:
Earth’s surface is deficient in available forms of many elements considered limiting for prebiotic chemistry. In contrast, many extraterrestrial rocky objects are rich in these same elements. Limiting prebiotic ingredients may, therefore, have been delivered by exogenous material; however, the mechanisms by which exogeneous material may be reliably and non-destructively supplied to a planetary surface remains unclear. Today, the flux of extraterrestrial matter to Earth is dominated by fine-grained cosmic dust. Although this material is rarely discussed in a prebiotic context due to its delivery over a large surface area, concentrated cosmic dust deposits are known to form on Earth today due to the action of sedimentary processes. Here we combine empirical constraints on dust sedimentation with dynamical simulations of dust formation and planetary accretion to show that localized sedimentary deposits of cosmic dust could have accumulated in arid environments on early Earth, in particular glacial settings that today produce cryoconite sediments. Our results challenge the widely held assumption that cosmic dust is incapable of fertilizing prebiotic chemistry. Cosmic dust deposits may have plausibly formed on early Earth and acted to fertilize prebiotic chemistry.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41550-024-02212-z

Authors

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Role:
Author
ORCID:
0000-0003-2659-644X
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Role:
Author
ORCID:
0000-0003-4842-5721
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Institution:
University of Oxford
Oxford college:
Merton College
Role:
Author
ORCID:
0000-0003-2130-8576
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Role:
Author
ORCID:
0000-0001-7165-2215


Publisher:
Nature Research
Journal:
Nature Astronomy More from this journal
Volume:
8
Issue:
5
Pages:
556-566
Publication date:
2024-02-19
Acceptance date:
2024-01-26
DOI:
EISSN:
2397-3366


Language:
English
Pubs id:
1678504
Local pid:
pubs:1678504
Source identifiers:
1985990
Deposit date:
2024-07-20
ARK identifier:
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