%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture non répertoriées par l'AERES
%A Bard, E.
%A Hamelin, B.
%A Arnold, M.
%A Montaggioni, L.
%A Cabioch, Guy
%A Faure, G.
%A Rougerie, Francis
%T Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge
%D 1996
%L fdi:010006546
%G ENG
%J Nature
%K QUATERNAIRE ; RECIF CORALLIEN ; NIVEAU MARIN ; SEDIMENTOLOGIE ; LITHOLOGIE ; PALEOENVIRONNEMENT ; PALEOCLIMAT
%K TAHITI
%N 6588
%P 241-244
%R 10.1038/382241a0
%U https://www.documentation.ird.fr/hor/fdi:010006546
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_6/b_fdi_45-46/010006546.pdf
%V 382
%W Horizon (IRD)
%X The timing of the last deglaciation is important to our understanding of the dynamics of large ice sheets and their effects on the Earth's surface. Moreover, the disappearance of the glacial ice sheets was responsible for dramatic increases in freshwater fluxes to the oceans, which probably disturbed the ocean's thermohaline circulation and, hence, global climate. Sea-level increase bear witness to the melting of continental ice sheets, but only two such records - from Barbados and New Guinea corals - have been accurately dated. But these corals overlie active subduction zones, where tectonic movements are large and often discontinuous (especially in New Guinea), so the apparent sea-level records may be contamined by a complex tectonic component. Here we date fossil corals from Tahiti, which is far from plate boundaries (and thus is likely to be tectonically relatively stable) and remote from the locations of large former ice sheets. The resulting record indicates a large sea-level jump shortly before 13,800 calendar years BP, which correponds to meltwater pulse 1 A in the Barbados coral records. The timing of this event is more accurately constrained in the Tahiti record, revealing that the meltwater pulse coincides with a short and intense climate cooling event that followed the initiation of the Bolling-Allerod warm period, but preceded the Younger Dryas cold event by about 1 000 years. (Résumé d'auteur)
%$ 064GEOQUA