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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2017
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5740680/
https://www.ncbi.nlm.nih.gov/pubmed/29180424
http://dx.doi.org/10.1073/pnas.1702143114

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5740680/
https://www.ncbi.nlm.nih.gov/pubmed/29180424
http://dx.doi.org/10.1073/pnas.1702143114

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