Cited by 474Origins and Evolution of LifeGeological and Geochemical AnalysisPaleontology and Stratigraphy of Fossils

Potentially biogenic carbon preserved in a 4.1 billion-year-old zircon

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Bell, Elizabeth A., Boehnke, Patrick, Harrison, T. Mark, Mao, Wendy L.·2015·Proceedings of the National Academy of Sciences

Abstract

Significance: Evidence for carbon cycling or biologic activity can be derived from carbon isotopes, because a high 12 C/ 13 C ratio is characteristic of biogenic carbon due to the large isotopic fractionation associated with enzymatic carbon fixation. The earliest materials measured for carbon isotopes at 3.8 Ga are isotopically light, and thus potentially biogenic. Because Earth’s known rock record extends only to ∼4 Ga, earlier periods of history are accessible only through mineral grains deposited in later sediments. We report 12 C/ 13 C of graphite preserved in 4.1-Ga zircon. Its complete encasement in crack-free, undisturbed zircon demonstrates that it is not contamination from more recent geologic processes. Its 12 C-rich isotopic signature may be evidence for the origin of life on Earth by 4.1 Ga.

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Crossref · 10.1073/pnas.1517557112

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  • Graphite inside a 4.1-Ga-old zircon has a biogenic-like δ13C of −24 per mil, although lack of context means an abiotic origin cannot be eliminated.

    “graphite inside a 4.1-Ga-old zircon has a biogenic-like δ13C of −24 per mil (‰) (19), although lack of context means that an abiotic origin cannot be eliminated.”

    From The Archean atmosphere (2020) · cites this paper as [19]

  • Life evolved relatively early in Earth history, with putative evidence pointing to a biosphere as early as 4.1 Ga and more convincingly by 3.7 Ga.

    “It is now generally accepted that life evolved relatively early in Earth history, with putative evidence pointing to the existence of a biosphere as early 4.1 Ga (see Bell et al., 2015) and more convincingly by 3.7 Ga.”
  • The 12C-enrichment in these inclusions may be taken as plausible unequivocal evidence for microbial life on Earth before 4.1 Ga.

    “The 12 C-enrichment found within these inclusions may thus be taken as plausible unequivocal evidence for the existence of microbial life on Earth before 4.1 Ga, during the epoch of comet and asteroid impacts.”

    From Cause of Cambrian Explosion - Terrestrial or Cosmic? (2018) · cites this paper as Bell et al., 2015

  • Detrital zircons 4.1 Ga from the Jack Hills region of Western Australia contain micron-sized graphite spheres with an isotopic signature of biogenic carbon.

    “Further, detrital zircons 4.1 Ga, discovered in rocks belonging to a geological outcrop in the Jack Hills region of Western Australia, have been found to contain micron-sized graphite spheres with an isotopic signature of biogenic carbon (Bell et al., 2015).”

    From Cause of Cambrian Explosion - Terrestrial or Cosmic? (2018) · cites this paper as Bell et al., 2015

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Research works printed but not linked: 1

  1. House CH, et al. (2000) Carbon isotopic composition of individual Precambrian mi- crofossils. Geology 28(8):707-710.

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Authors
Bell, E. A., Boehnke, P., Harrison, T. M., & Mao, W. L.
Affiliations
  • University of California, Los Angeles (US)
  • Stanford University (US)
Venue
Proceedings of the National Academy of Sciences
Published
2015-10-19
Volume
112
Issue
47
Pages
14518-14521
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W2161420691
Cited by
474
References
42
Citations by year
2026: 24 · 2025: 37 · 2024: 27 · 2023: 28 · 2022: 32 · 2021: 35 · 2020: 54 · 2019: 69 · 2018: 54 · 2017: 63 · 2016: 44 · 2015: 5
FWCI
31.49
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion)
  • PubMed Central (publishedVersion)
  • PubMed (publishedVersion)
  • OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) (submittedVersion)
Funders
  • Simons Foundation (293529)
  • National Science Foundation (NSF-EAR-0948724, NSF-EAR-1055454)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
biogenic carbon, detrital zircon, graphite inclusions, carbon isotopes, early Earth biosphere, origin of life, Jack Hills, Archean
MeSH terms
Carbon, Zirconium, Silicates, Earth, Planet

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