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Low mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals

Citation

Planavsky, NJ and Reinhard, CT and Wang, X and Thomson, D and McGoldrick, P and Rainbird, RH and Johnson, T and Fischer, WW and Lyons, TW, Low mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals, Science, 346, (6209) pp. 635-638. ISSN 0036-8075 (2014) [Refereed Article]

Copyright Statement

Copyright 2014 Science

DOI: doi:10.1126/science.1258410

Abstract

The oxygenation of Earth’s surface fundamentally altered global biogeochemical cycles and ultimately paved the way for the rise of metazoans at the end of the Proterozoic. However, current estimates for atmospheric oxygen (O2) levels during the billion years leading up to this time vary widely. On the basis of chromium (Cr) isotope data from a suite of Proterozoic sediments from China, Australia, and North America, interpreted in the context of data from similar depositional environments from Phanerozoic time, we find evidence for inhibited oxidation of Cr at Earth’s surface in the mid-Proterozoic (1.8 to 0.8 billion years ago). These data suggest that atmospheric O2 levels were at most 0.1% of present atmospheric levels. Direct evidence for such low O2 concentrations in the Proterozoic helps explain the late emergence and diversification of metazoans.

Item Details

Item Type:Refereed Article
Keywords:Precambrian, iron formation, atmosphere, chromium isotopes, animals
Research Division:Earth Sciences
Research Group:Geochemistry
Research Field:Inorganic Geochemistry
Objective Division:Expanding Knowledge
Objective Group:Expanding Knowledge
Objective Field:Expanding Knowledge in the Earth Sciences
Author:McGoldrick, P (Dr Peter McGoldrick)
ID Code:97197
Year Published:2014
Funding Support:Australian Research Council (CE0561595)
Web of Science® Times Cited:205
Deposited By:Earth Sciences
Deposited On:2014-12-05
Last Modified:2017-11-02
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