Temperature reconstruction for the Mid-Pleistocene Transition based on deep-dwelling foraminifera of IODP Site339-U1385

The mid-Pleistocene Transition (MPT; approx. 1.2-0.7 Ma), is characterized by growing Northern Hemisphere ice sheets and the shift from a 41 kyr to a 100 kyr glacial-interglacial cyclicity. Concomitant to the growth of large ice sheets, atmospheric and oceanic circulation pattern have changed. One k...

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Bibliographic Details
Main Authors: Bahr, André, Kaboth, Stefanie, Hodell, David A, Zeeden, Christian, Fiebig, Jens, Friedrich, Oliver
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.882374
https://doi.org/10.1594/PANGAEA.882374