Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments?-Reference-Cited by-同舟云学术

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Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments?

Published:2024-10 Issue: Volume:643 Page:118900
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Swain Anshuman^ORCID,Kaufman Alan J.^ORCID,Kalinowski Marcin,Yarwood Stephanie A.^ORCID,Fagan William F.

Publisher

Elsevier BV

Reference85 articles.

1. Earth's great oxidation event facilitated by the rise of sedimentary phosphorus recycling;Alcott;Nat. Geosci.,2022

2. A whiff of oxygen before the great oxidation event?;Anbar;Science,2007

3. Proterozoic ocean chemistry and evolution: a bioinorganic bridge?;Anbar;Science,2002

4. Evolution of atmospheric xenon and other noble gases inferred from Archean to Paleoproterozoic rocks;Avice;Geochim. Cosmochim. Acta,2018

5. The rise of oxygen and siderite oxidation during the Lomagundi event;Bachan;Proc. Natl. Acad. Sci.,2015

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