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Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO(2) change
Large amplitude variations in atmospheric CO(2) were associated with glacial terminations of the Late Pleistocene. Here we provide multiple lines of evidence suggesting that the ∼20 p.p.m.v. overshoot in CO(2) at the end of Termination 2 (T2) ∼129 ka was associated with an abrupt (≤400 year) deepeni...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5333367/ https://www.ncbi.nlm.nih.gov/pubmed/28239149 http://dx.doi.org/10.1038/ncomms14595 |