Asynchrony between Antarctic temperature and CO(2) associated with obliquity over the past 720,000 years

The δD temperature proxy in Antarctic ice cores varies in parallel with CO(2) through glacial cycles. However, these variables display a puzzling asynchrony. Well-dated records of Southern Ocean temperature will provide crucial information because the Southern Ocean is likely key in regulating CO(2)...

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Detalles Bibliográficos
Autores principales: Uemura, Ryu, Motoyama, Hideaki, Masson-Delmotte, Valérie, Jouzel, Jean, Kawamura, Kenji, Goto-Azuma, Kumiko, Fujita, Shuji, Kuramoto, Takayuki, Hirabayashi, Motohiro, Miyake, Takayuki, Ohno, Hiroshi, Fujita, Koji, Abe-Ouchi, Ayako, Iizuka, Yoshinori, Horikawa, Shinichiro, Igarashi, Makoto, Suzuki, Keisuke, Suzuki, Toshitaka, Fujii, Yoshiyuki
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5840396/
https://www.ncbi.nlm.nih.gov/pubmed/29511182
http://dx.doi.org/10.1038/s41467-018-03328-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5840396/
https://www.ncbi.nlm.nih.gov/pubmed/29511182
http://dx.doi.org/10.1038/s41467-018-03328-3

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