A Late Archean Sulfidic Sea Stimulated by Early Oxidative Weathering of the Continents

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Summary

Findings indicate that euxinic conditions may have been common on a variety of spatial and temporal scales both before and immediately after the Paleoproterozoic rise in atmospheric oxygen, hinting at previously unexplored texture and variability in deep ocean chemistry during Earth’s early history.

Type
article
Published
2009-10-30
Cited by
281
References
30

Keywords

Anoxic waters, Weathering, Atmospheric oxygen, Archean, Hydrothermal vent

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