Journal
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
Volume 112, Issue 47, Pages 14518-14521Publisher
NATL ACAD SCIENCES
DOI: 10.1073/pnas.1517557112
Keywords
Hadean; carbon isotopes; early Earth; zircon; origin of life
Categories
Funding
- National Science Foundation (NSF)-Division of Earth Sciences (EAR) [1055454]
- Simons Collaboration on the Origin of Life Postdoctoral Fellowship
- NSF-EAR [0948724]
- Instrumentation and Facilities Program of EAR, NSF
- Directorate For Geosciences
- Division Of Earth Sciences [1055454, 0948724] Funding Source: National Science Foundation
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Evidence of life on Earth is manifestly preserved in the rock record. However, the microfossil record only extends to similar to 3.5 billion years (Ga), the chemofossil record arguably to similar to 3.8 Ga, and the rock record to 4.0 Ga. Detrital zircons from Jack Hills, Western Australia range in age up to nearly 4.4 Ga. From a population of over 10,000 Jack Hills zircons, we identified one >3.8-Ga zircon that contains primary graphite inclusions. Here, we report carbon isotopic measurements on these inclusions in a concordant, 4.10 +/- 0.01-Ga zircon. We interpret these inclusions as primary due to their enclosure in a crack-free host as shown by transmission X-ray microscopy and their crystal habit. Their delta C-13(PDB) of -24 +/- 5% is consistent with a biogenic origin and may be evidence that a terrestrial biosphere had emerged by 4.1 Ga, or similar to 300 My earlier than has been previously proposed.
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