Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM, 56 Ma) was a phase of rapid global warming associated with massive carbon input into the ocean–atmosphere system from a <sup>13</sup>C-depleted reservoir. Many midlatitude and high-latitude sections have been studied and document changes in salinity, hy...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Copernicus Publications
2018-01-01
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| Rangatū: | Climate of the Past |
| Urunga tuihono: | https://www.clim-past.net/14/39/2018/cp-14-39-2018.pdf |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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