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...

Полное описание

Сохранить в:
Библиографические подробности
Опубликовано в: :Proc Natl Acad Sci U S A
Главные авторы: 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.
Формат: Artigo
Язык:Inglês
Опубликовано: National Academy of Sciences 2017
Предметы:
Physical Sciences
Online-ссылка: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
Метки: Добавить метку
Нет меток, Требуется 1-ая метка записи!

Схожие документы