An abrupt change in the African monsoon at the end of the Younger Dryas-Reference-Cited by-同舟云学术

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An abrupt change in the African monsoon at the end of the Younger Dryas

Published:2007-03 Issue:3 Volume:8 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Talbot Michael R.¹,Filippi Maria Letizia²,Jensen Niels Bo³,Tiercelin Jean-Jacques⁴

Affiliation:

1. Department of Earth Sciences; University of Bergen; Allégt. 41,; 5007; Bergen; Norway

2. Museo Tridentino Scienze Naturali; Via Calepina 14,; I-38100; Trento; Italy

3. IRIS Research; Thormølens Gt. 55,; 5008; Bergen; Norway

4. UMR CNRS 6538 “Domaines Océaniques”; Institute Universitaire Européen de la Mer; Place Nicolas Copernic,; F-29280; Plouzané; France

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference97 articles.

1. Glacial millennial-scale fluctuations in central African precipitation recorded in terrigenous sediment supply and freshwater signals offshore Cameroon;Adegbie;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2003

2. The Younger Dryas cold interval as viewed from central Greenland;Alley;Quat. Sci. Rev.,2000

3. Abrupt increase in snow accumulation at the end of the Younger Dryas;Alley;Nature,1993

4. New evidence for a reduced water balance in East Africa during the Last Glacial Maximum: Implication for model-data comparison;Barker;Quat. Sci. Rev.,2003

5. Late Quaternary climatic variability in intertropical Africa

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