FN Archimer Export Format
PT J
TI New constraints on European glacial freshwater releases to the North Atlantic Ocean
BT 
AF EYNAUD, Frederique
   MALAIZE, Bruno
   ZARAGOSI, Sebastien
   DE VERNAL, Anne
   SCOURSE, James
   PUJOL, Claude
   CORTIJO, Elsa
   GROUSSET, Francis E.
   PENAUD, Aurelie
   TOUCANNE, Samuel
   TURON, Jean-Louis
   AUFFRET, Gerard
AS 1:1;2:1;3:1;4:2;5:3;6:1;7:4;8:1;9:5;10:6;11:1;12:6;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:PDG-REM-GM-LGS;11:;12:PDG-DOP-DCB-GM-LES;
C1 Univ Bordeaux 1, EPOC, UMR 5805, F-33400 Talence, France.
   GEOTOP, Montreal, PQ, Canada.
   Bangor Univ, Sch Ocean Sci, Coll Nat Sci, Bangor, Anglesey, Wales.
   Lab Sci Climat & Environm, Gif Sur Yvette, France.
   IUEM UBO, Domaines Ocean, UMR 6538, Plouzane, France.
   IFREMER, Lab Environm Sedimentaires, Plouzane, France.
C2 UNIV BORDEAUX, FRANCE
   UNIV QUEBEC (UQAM-GEOTOP), CANADA
   UNIV BANGOR, UK
   LSCE, FRANCE
   UBO, FRANCE
   IFREMER, FRANCE
SI BREST
SE PDG-REM-GM-LGS
   PDG-DOP-DCB-GM-LES
IF 3.98
TC 23
TU CEA
   CNRS
   EPHE
   IFREMER
   IRD
   SCEF HYDROGRAPH OCEANOGRAPHIQUE MARINE
   UNIVERSITE BORDEAUX
   UNIVERSITE BREST
   UNIVERSITE BRETAGNE-SUD
   UNIVERSITE VERSAILLES
UR https://archimer.ifremer.fr/doc/00086/19762/20100.pdf
LA English
DT Article
CR IMAGES 1-MD101
   MD 128 / SWAF
BO Marion Dufresne
AB During the late Quaternary, both external and internal forcings have driven major climatic shifts from glacial to interglacial conditions. Nonlinear climatic steps characterized the transitions leading to these extrema, with intermediate excursions particularly well expressed in the dynamics of the Northern Hemisphere cryosphere. Here we document the impact of these dynamics on the north-eastern North Atlantic Ocean, focussing on the 35-10 ka interval. Sea-surface salinities have been reconstructed quantitatively based on two independent methods from core MD95-2002, recovered from the northern Bay of Biscay adjacent to the axis of the Manche paleoriver outlet and thus in connection with proximal European ice sheets and glaciers. Quantitative reconstructions deriving from dinocyst and planktonic foraminiferal analyses have been combined within a robust chronology to assess the amplitude and timing of hydrological changes in this region. Our study evidences strong pulsed freshwater discharges which may have impacted the North Atlantic Meridional Overturning Circulation.
PY 2012
PD AUG
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 39
UT 000208934000004
DI 10.1029/2012GL052100
ID 19762
ER

EF