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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Bibliografiset tiedot
Julkaisussa:Nat Commun
Päätekijät: 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
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Nature Publishing Group UK 2018
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Article
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC5840396/
https://ncbi.nlm.nih.gov/pubmed/29511182
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-03328-3
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