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Increased ventilation of Antarctic deep water during the warm mid-Pliocene
The mid-Pliocene warm period is a recent warm geological period that shares similarities with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional Overturning Circulation must have been stronger, to explain a weak Atlantic meridional δ(13)C gradient and large nort...
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| Päätekijät: | , , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Nature Pub. Group
2013
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3586712/ https://ncbi.nlm.nih.gov/pubmed/23422667 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms2521 |
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