Benthic and planktic foraminiferal Mg/Ca, Ba/Ca and local seawater d18O estimates

During the middle Miocene, Earth's climate changed from a global warm period (Miocene Climatic Optimum) into a colder one with the expansion of the Antarctic ice sheet. This prominent climate transition was also a period of drastic changes in global atmospheric circulation. The development of t...

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Bibliographic Details
Main Authors: Yang, Xueping, Groeneveld, Jeroen, Jian, Zhimin, Steinke, Stephan, Giosan, Liviu
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.910403
https://doi.org/10.1594/PANGAEA.910403