Interactive comment on “Surface-circulation change in the Southern Ocean across the Middle Eocene Climatic Optimum: inferences from dinoflagellate cysts and biomarker paleothermometry” by Margot J. Cramwinckel et al.

The Middle Eocene Climatic Optimum (MECO) is a global warming event at about 40 Ma that interrupted the long-term Cenozoic cooling trend. Up to now only a few studies have focused with enough resolution to evaluate the paleoenvironmental and paleobiotic consequences of this hyperthermal event. In th...

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Bibliographic Details
Main Author: Guerstein, Gladys Raquel
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications
Subjects:
Online Access:http://hdl.handle.net/11336/110498