Constraints on surface temperature 3.4 billion years ago based on triple oxygen isotopes of cherts from the Barberton Greenstone Belt, South Africa, and the problem of sample selection

Donald R. Lowe; Daniel E. Ibarra; Nadja Drabon; C. Page Chamberlain

doi:10.2475/11.2020.02

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Constraints on surface temperature 3.4 billion years ago based on triple oxygen isotopes of cherts from the Barberton Greenstone Belt, South Africa, and the problem of sample selection

Donald R. Lowe, Daniel E. Ibarra, Nadja Drabon and C. Page Chamberlain

American Journal of Science November 2020, 320 (9) 790-814; DOI: https://doi.org/10.2475/11.2020.02

Donald R. Lowe

*Department of Geological Sciences, Stanford University, Stanford, California 94305, USA

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For correspondence: drlowe@stanford.edu

Daniel E. Ibarra

*Department of Geological Sciences, Stanford University, Stanford, California 94305, USA

**Department of Earth and Planetary Science, University of California, Berkeley, Berkeley, California

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Nadja Drabon

*Department of Geological Sciences, Stanford University, Stanford, California 94305, USA

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C. Page Chamberlain

*Department of Geological Sciences, Stanford University, Stanford, California 94305, USA

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American Journal of Science

Vol. 320, Issue 9

1 Nov 2020

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Constraints on surface temperature 3.4 billion years ago based on triple oxygen isotopes of cherts from the Barberton Greenstone Belt, South Africa, and the problem of sample selection

Donald R. Lowe, Daniel E. Ibarra, Nadja Drabon, C. Page Chamberlain

American Journal of Science Nov 2020, 320 (9) 790-814; DOI: 10.2475/11.2020.02

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Constraints on surface temperature 3.4 billion years ago based on triple oxygen isotopes of cherts from the Barberton Greenstone Belt, South Africa, and the problem of sample selection

Donald R. Lowe, Daniel E. Ibarra, Nadja Drabon, C. Page Chamberlain

American Journal of Science Nov 2020, 320 (9) 790-814; DOI: 10.2475/11.2020.02

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