Causes of ice age intensification across the Mid-Pleistocene Transition

During the Mid-Pleistocene Transition (MPT; 1,200–800 kya), Earth’s orbitally paced ice age cycles intensified, lengthened from ∼40,000 (∼40 ky) to ∼100 ky, and became distinctly asymmetrical. Testing hypotheses that implicate changing atmospheric CO(2) levels as a driver of the MPT has proven diffi...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
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.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2017
Assuntos:
Physical Sciences
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5740680/
https://ncbi.nlm.nih.gov/pubmed/29180424
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1702143114
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