Uvigerina spp. minor element and derived δ¹⁸Oseawater records over the Mid-Pleistocene Transition (500-1500 kyr), DSDP Hole 94-607

During the Mid-Pleistocene Transition (MPT), the dominant glacial-interglacial cyclicity as inferred from the marine d18O records of benthic foraminifera (d18Obenthic) changed from 41 kyr to 100 kyr years in the absence of a comparable change in orbital forcing. Currently, only two Mg/Ca-derived, hi...

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Bibliographic Details
Main Authors: Ford, Heather L, Sosdian, Sindia M, Rosenthal, Yair, Raymo, Maureen E
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.864108
https://doi.org/10.1594/PANGAEA.864108