Cited by 138Astro and Planetary ScienceGeological and Geochemical AnalysisPlanetary Science and Exploration

The DOI matches its Crossref record; 92 of the 98 references it cites were found in a registry or an index.

Illusory Late Heavy Bombardments

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Boehnke, Patrick, Harrison, T. Mark·2016·Proceedings of the National Academy of Sciences

Abstract

Significance: The vast majority of evidence marshaled for the Late Heavy Bombardment comes from 40 Ar/ 39 Ar age spectra of Apollo samples, interpreted through “plateau” ages, which show an apparent cluster at ∼3.9 Ga. Whether such data can be uniquely inverted to constrain impact histories in the Earth−Moon system has never been tested. We show that diffusive loss of 40 Ar from a monotonically declining impactor flux coupled with the early and episodic nature of lunar crust formation tends to create clustered distributions of apparent 40 Ar/ 39 Ar ages at ca. 3.9 Ga. Instead, these 40 Ar/ 39 Ar data can be reconciled with a continuously decreasing bollide flux. Thus, impacts may have played a minimal role in terrestrial habitability, early Earth dynamics, and the formation of Hadean zircons.

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6 of the 98 references couldn’t be matched to a known paper.

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  1. P Boehnke, MT Heizler, TM Harrison, OM Lovera, PH Warren, Avoiding interpretative pitfalls in analysis of 40Ar/39Ar step-heating data from thermally disturbed meteoritic and lunar samples. Proc Lunar Planet Sci Conf 45, 2545 (2014).
  2. DA Minton, AP Jackson, E Asphaug, CI Fassett, JE Richardson, Debris from borealis basin formation as the primary impactor population of Late Heavy Bombardment. Workshop on Early Solar System Impact Bombardment III (Solar Syst Explor Res Virtual Inst, Moffett Field, CA), pp. 3033 (2015).
  3. EC Alexander, SB Kahl, 40Ar-39Ar studies of lunar breccias. Proc Lunar Planet Sci Conf 5, 1353–1373 (1974).
  4. OA Schaeffer, GA Schaeffer, 39Ar-40Ar ages of lunar rocks. Proc Lunar Planet Sci Conf 8, 840–842 (1977).
  5. G Turner, PH Cadogan, The history of lunar bombardment inferred from 40Ar-39Ar dating of highland rocks. Proc Lunar Planet Sci Conf 6, 1509–1538 (1975b).
  6. G Turner, PH Cadogan, CJ Yonge, Argon selenochronology. Proc Lunar Planet Sci Conf 4, 1889–1914 (1973).
  7. D York, WJ Kenyon, RJ Doyle, 40Ar-39Ar ages of Apollo 14 and 15 samples. Proc Lunar Planet Sci Conf 3, 1613–1622 (1972).

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Metadata

Authors
Boehnke, P., & Harrison, T. M.
Affiliations
University of California, Los Angeles (US)
Venue
Proceedings of the National Academy of Sciences
Published
2016-09-12
Volume
113
Issue
39
Pages
10802-10806
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W2519355055
Cited by
138
References
98
Citations by year
2026: 8 · 2025: 12 · 2024: 15 · 2023: 12 · 2022: 13 · 2021: 8 · 2020: 22 · 2019: 20 · 2018: 13 · 2017: 13
FWCI
7.11
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion)
  • Europe PMC (PubMed Central) (publishedVersion)
  • PubMed Central (publishedVersion)
  • PubMed (publishedVersion)
Funders
National Science Foundation (EAR-0948724, EAR-1339051)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
Keywords
Late Heavy Bombardment, plateau ages, argon diffusion, lunar impact history, Apollo samples, lunar magmatism

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