Late Archean euxinic conditions before the rise of atmospheric oxygen
Life on Earth is thought to have coevolved with the chemistry of the oceans and atmosphere, and the shift from an anoxic to an oxic world across the Archean-Proterozoic boundary represents a fundamental step in this process. In order to understand the relative influence of biological and geological...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/25183 |