CORDIS Project
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This research explores ocean circulation dynamics during historical greenhouse periods, focusing on the Cretaceous and Eocene epochs. By analyzing neodymium isotopes, it aims to understand past deep-water formation and its implications for current climate change.
Ocean circulation plays a dominant role in distributing heat over the planet and in providing oxygen for life in the deep sea.
The thermohaline circulation will likely be affected by global warming, in particular the current areas of deep water formation at high latitudes.
The thermal maxima of the Cretaceous (94 million years ago) and the Eocene (51 million years ago) are the two most important greenhouse climate phases of the last 100 million years and are seen as analogues to current climate…
UNIVERSITE DE RENNES
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