Stable carbon and oxygen isotope record od IODP Hole 306-U1313

The Mid-Pleistocene transition (MPT) was the time when quasi-periodic (? 100 kyr), high-amplitude glacial variability developed in the absence of any significant change in the character of orbital forcing, leading to the establishment of the characteristic pattern of late Pleistocene climate variabi...

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Bibliographic Details
Main Authors: Ferretti, Patrizia, Crowhurst, Simon J, Hall, Michael A, Cacho, Isabel
Format: Dataset
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.786601
https://doi.org/10.1594/PANGAEA.786601