A high-resolution history of the South American Monsoon from Last Glacial Maximum to the Holocene.

Citation data:

Scientific reports, ISSN: 2045-2322, Vol: 7, Page: 44267

Publication Year:
2017
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Repository URL:
http://ir.xjtu.edu.cn/item/406228
PMID:
28281650
DOI:
10.1038/srep44267
Author(s):
Novello, Valdir F., Cruz, Francisco W., Vuille, Mathias, Strikis, Nicolas M., Edwards, R. Lawrence, Cheng, Hai, Emerick, Suellyn, De Paula, Marcos S., Li, Xianglei, Barreto, Eline de S., Karmann, Ivo, Santos, Roberto V. Show More Hide
Publisher(s):
Springer Nature
Tags:
Multidisciplinary, Journal
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article description
The exact extent, by which the hydrologic cycle in the Neotropics was affected by external forcing during the last deglaciation, remains poorly understood. Here we present a new paleo-rainfall reconstruction based on high-resolution speleothem δO records from the core region of the South American Monsoon System (SAMS), documenting the changing hydrological conditions over tropical South America (SA), in particular during abrupt millennial-scale events. This new record provides the best-resolved and most accurately constrained geochronology of any proxy from South America for this time period, spanning from the Last Glacial Maximum (LGM) to the mid-Holocene.

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