Causes of ice age intensification across the Mid-Pleistocene Transition

Conflicting sets of hypotheses highlight either the role of ice sheets or atmospheric carbon dioxide (CO2) in causing the increase in duration and severity of ice age cycles ∼1 Mya during the Mid-Pleistocene Transition (MPT). We document early MPT CO2 cycles that were smaller than during recent ice...

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Bibliographic Details
Published in:Proceedings of the National Academy of Sciences
Main Authors: Chalk, Thomas B., Hain, Mathis P., Foster, Gavin L., Rohling, Eelco J., Sexton, Philip F., Badger, Marcus P. S., Cherry, Soraya G., Hasenfratz, Adam P., Haug, Gerald H., Jaccard, Samuel L., Martínez-García, Alfredo, Pälike, Heiko, Pancost, Richard D., Wilson, Paul A.
Format: Text
Language:English
Published: National Academy of Sciences 2017
Subjects:
Physical Sciences
Southern Ocean
Ice Sheet
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5740680/
http://www.ncbi.nlm.nih.gov/pubmed/29180424
https://doi.org/10.1073/pnas.1702143114
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Summary:Conflicting sets of hypotheses highlight either the role of ice sheets or atmospheric carbon dioxide (CO2) in causing the increase in duration and severity of ice age cycles ∼1 Mya during the Mid-Pleistocene Transition (MPT). We document early MPT CO2 cycles that were smaller than during recent ice age cycles. Using model simulations, we attribute this to post-MPT increase in glacial-stage dustiness and its effect on Southern Ocean productivity. Detailed analysis reveals the importance of CO2 climate forcing as a powerful positive feedback that magnified MPT climate change originally triggered by a change in ice sheet dynamics. These findings offer insights into the close coupling of climate, oceans, and ice sheets within the Earth System.

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