Ice rafted debris and reconstructed sea surface temperature of ODP Hole 104-642B
The mid-Piacenzian warm period (3.264-3.025 Ma) of the Pliocene epoch has been proposed as a possible reference for future warm climate states. However, there is significant disagreement over the magnitude of high latitude warming between data and models for this period of time, raising questions ab...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2016
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.858944 https://doi.org/10.1594/PANGAEA.858944 |