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Publication Details
AFRICAN RESEARCH NEXUS
SHINING A SPOTLIGHT ON AFRICAN RESEARCH
agricultural and biological sciences
Timing and dynamics of the last deglaciation from European and North African δ
13
C stalagmite profiles-comparison with Chinese and South Hemisphere stalagmites
Quaternary Science Reviews, Volume 25, No. 17-18, Year 2006
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Description
The last deglaciation and its climatic events, such as the Bølling-Allerød (BA) and the Younger-Dryas (YD), have been clearly recorded in the δ13C profiles of three stalagmites from caves from Southern France to Northern Tunisia. The three δ13C records, dated by thermal ionization mass spectrometric uranium-thorium method (TIMS), show great synchroneity and similarity in shape with the Chinese cave δ18O records and with the marine tropical records, leading to the hypothesis of an in-phase (between 15.5 and 16 ka ∼±0.5 ka) postglacial warming in the Northern Hemisphere, up to at least 45°N. The BA transition appears more gradual in the speleothem records than in the Greenland records and the Allerød seems warmer than the Bølling, showing here close similarities with other marine and continental archives. A North-South gradient is observed in the BA trend: it cools in Greenland and warms in our speleothem records. Several climatic events are clearly recognizable: a cooler period at about 14 ka (Older Dryas (OD)); the Intra-Allerød Cold Period at about ∼13.3 ka; the YD cooling onset between 12.7 and 12.9±0.3 ka. Similar to the BA, the YD displays a gradual climate amelioration just after its onset at 12.75±0.25 ka, up to the Preboreal, and is punctuated by a short climatic event at 12.15 ka. Even though the Southern Hemisphere stalagmite records seem to indicate that the postglacial warming started about ∼3 ka±1.8 ka earlier in New Zealand (∼41 °S), and about ∼1 to ∼2 ka earlier in South Africa (24.1 °S), large age uncertainties, essentially due to slow growth rates, make the comparison still perilous. The overall δ13C speleothem record seems to follow a baseline temperature increase controlled by the increase in insolation and punctuated by cold events possibly due to the N-America freshwater lake discharges. © 2006 Elsevier Ltd. All rights reserved.
Authors & Co-Authors
Genty, Dominique
France, Gif-sur-yvette
Laboratoire Des Sciences du Climat et de L'environnement
Canada, Montreal
Université du Québec à Montréal
Blamart, Dominique
France, Gif-sur-yvette
Laboratoire Des Sciences du Climat et de L'environnement
Ghaleb, Bassam
Canada, Montreal
Université du Québec à Montréal
Plagnes, Valérie
France, Paris
Milieux Environnementaux, Transferts et Interactions Dans Les Hydrosystèmes et Les Sols
Causse, Christiane
France, Paris
Cnrs Centre National de la Recherche Scientifique
Bakalowicz, Michel J.
France, Montpellier
Laboratoire Hydrosciences Montpellier
Zouari, Kamel
Tunisia, Sfax
Ecole Nationale D'ingénieurs de Sfax
Chkir, Najiba
Tunisia, Sfax
Ecole Nationale D'ingénieurs de Sfax
Hellstrom, John C.
Australia, Melbourne
University of Melbourne
Wainer, Karine A.I.
France, Gif-sur-yvette
Laboratoire Des Sciences du Climat et de L'environnement
Canada, Montreal
Université du Québec à Montréal
Bourges, François
France, Saint-girons
Géologie Environnement Conseil
Statistics
Citations: 274
Authors: 11
Affiliations: 8
Identifiers
Doi:
10.1016/j.quascirev.2006.01.030
ISSN:
02773791
Research Areas
Environmental
Study Locations
South Africa
Tunisia