A short-term, post-Lomagundi positive C isotope excursion at C. 2.03 Ga recorded by the Wooly Dolomite, Western Australia.
It is generally accepted that carbon isotope variations in seawater were muted between c. 2.06 Ga, after the end of the Lomagundi carbon isotope excursion (LCIE), and c. 1.3 Ga. Evidence is presented here that c. 30 myr after the end of the LCIE, the biogeochemical cycle of carbon experienced a shor...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Geological Society Publishing House
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/49903 |