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Isotopic evidence for long term warmth in the Mesozoic
Atmospheric CO(2) concentrations appear to have been considerably higher than modern levels during much of the Phanerozoic and it has hence been proposed that surface temperatures were also higher. Some studies have, however, suggested that Earth's temperature (estimated from the isotopic compo...
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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
2013
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3595697/ https://ncbi.nlm.nih.gov/pubmed/23486483 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep01438 |
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