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...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2010
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.786601 https://doi.org/10.1594/PANGAEA.786601 |