A Decrease to Low Carbonate Clumped Isotope Temperatures in Cryogenian Strata
Preglacial and synglacial low-latitude carbonate sediments of the Elbobreen Formation, NE Svalbard, preserve facies changes associated with low-latitude glacial advance in Cryogenian “Snowball Earth” episodes (717–635 Ma). We present the first application of carbonate clumped (Δ47) isotope thermomet...
Main Authors: | , , , |
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Other Authors: | |
Format: | Article |
Language: | English |
Published: |
American Geophysical Union (AGU)
2021
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Online Access: | https://hdl.handle.net/1721.1/131285 |