Reconstructing the East Antarctic ice sheet during the Plio-Pleistocene using geochemical provenance analysis
Approximately five million years ago, during the early Pliocene, global temperatures were 2 – 4 ⁰C warmer-than-present and the cryosphere was reduced. During the subsequent Plio-Pleistocene, global temperatures gradually cooled and atmospheric carbon dioxide (CO2) concentrations decreased, accompani...
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Imperial College London
2018
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| Online Access: | https://dx.doi.org/10.25560/83552 http://spiral.imperial.ac.uk/handle/10044/1/83552 |