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Deep ocean carbonate ion increase during mid Miocene CO(2) decline
Characterised by long term cooling and abrupt ice sheet expansion on Antarctica ~14 Ma ago, the mid Miocene marked the beginning of the modern ice-house world, yet there is still little consensus on its causes, in part because carbon cycle dynamics are not well constrained. In particular, changes in...
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| 主要な著者: | , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group
2014
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3935200/ https://ncbi.nlm.nih.gov/pubmed/24569646 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep04187 |
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