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| Titre : |
Reconstruction of the Amazon basin effective moisture availability over the past 14,000 years.
|
| Est un extrait ou un tiré à part de : | |
| Auteur(s) : |
Mark A. Maslin, Auteur (et co-auteur)
Stephen J. Burns, Auteur (et co-auteur) |
| Type de document : | Tiré à part |
| Résumé : |
Quantifying the moisture history of the Amazon Basin is essential for understanding the cause of rain forest diversity and its potential as a methane source. We reconstructed the Amazon River outflow history for the past 14,000 years to provide a moisture budget for the river drainage basin. The oxygen isotopic composition of planktonic foraminifera recovered from a marine sediment core in a region of Amazon River discharge shows that the Amazon Basin was extremely dry during the Younger Dryas, with the discharge reduced by at least 40% as compared with that of today. After the Younger Dryas, a meltwaterdriven discharge event was followed by a steady increase in the Amazon Basin effective moisture throughout the Holocene. |
| Editeur(s) : | American Association for the Advancement of Science |
| Date de publication : | 2000 |
| Format : | pp. 2285-2287 / graph., carte., réf. |
| Note(s) : |
Vol.290 - n°5500 |
| Langue(s) : | Anglais |
| Lien vers la notice : | https://infodoc.agroparistech.fr/index.php?lvl=notice_display&id=165158 |
Exemplaires (1)
| Localisation | Emplacement | Pôle | Section | Cote | Support | Disponibilité |
|---|---|---|---|---|---|---|
| Kourou | ARCHIVES | AgroParisTech-Kourou | UMR.2410 | Papier | Empruntable Disponible |

