FN Archimer Export Format
PT J
TI Phase relationship between sea level and abrupt climate change
BT 
AF SIERRO, Francisco J.
   ANDERSEN, Nils
   BASSETTI, Maria-Angela
   BERNE, Serge
   CANALS, Miquel
   CURTIS, Jason H.
   DENNIELOU, Bernard
   ABEL FLORES, Jose
   FRIGOLA, Jaime
   GONZALEZ-MORA, Beatriz
   GRIMALT, Joan O.
   HODELL, David A.
   JOUET, Gwenael
   PEREZ-FOLGADO, Marta
   SCHNEIDER, Ralph
AS 1:1;2:2;3:3;4:3,6;5:4;6:5;7:6;8:1;9:4;10:1;11:7;12:5;13:6;14:1;15:8;
FF 1:;2:;3:PDG-DOP-DCB-GM-LES;4:PDG-DOP-DCB-GM-LES;5:;6:;7:PDG-DOP-DCB-GM-LES;8:;9:;10:;11:;12:;13:PDG-DOP-DCB-GM-LES;14:;15:;
C1 Univ Salamanca, Dept Geol, Salamanca 37071, Spain.
   Univ Kiel, Leibniz Lab Radiometr Dating & Isotope Res, D-24118 Kiel, Germany.
   Univ Perpignan, Lab IMAGES BatU, F-66860 Perpignan, France.
   Univ Barcelona, GRC Marine Geosci, Dept Stratig Paleontol & Marine Geosci, E-08028 Barcelona, Spain.
   Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA.
   IFREMER, GM, Lab Environm Sedimentaires, F-29280 Plouzane, France.
   Inst Environm Assessment & Water Res IDAEA, Dept Environm Chem, Barcelona 08034, Spain.
   Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany.
C2 UNIV SALAMANCA, SPAIN
   UNIV KIEL, GERMANY
   UNIV PERPIGNAN, FRANCE
   UNIV BARCELONA, SPAIN
   UNIV FLORIDA, USA
   IFREMER, FRANCE
   IDAEA, SPAIN
   UNIV KIEL, GERMANY
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
IF 4.245
TC 61
UR https://archimer.ifremer.fr/doc/2009/publication-6969.pdf
LA English
DT Article
CR IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
   PROMESS 1
BO Marion Dufresne
   Bavenit
AB Direct traces of past sea levels are based on the elevation of old coral reefs at times of sea level high-stands. However, these measurements are discontinuous and cannot be easily correlated with climate records from ice cores. In this study we show a new approach to recognizing the imprint of sea level changes in continuous sediment records taken from the continental slope at locations that were continuously submerged, even during periods of sea level lowstand. By using a sediment core precisely synchronized with Greenland ice cores, we were able to recognize major floods of the Mediterranean continental shelf over the past 270 kyr. During the last glacial period five flooding events were observed at the onset of the warmest Greenland interstadials. Consistent correspondence between warm climate episodes and eustatic sea level rises shows that these global flooding events were generated by pronounced melting of the Northern Hemisphere ice sheets, due to rapid intensification of Atlantic Meridional Overturning Circulation. The method described in this study opens a new perspective for inter-hemi spheric synchronization of marine climate records if applied in other continental margins from the Southern Hemisphere or the equatorial regions. (C) 2009 Elsevier Ltd. All rights reserved.
PY 2009
PD DEC
SO Quaternary Science Reviews
SN 0277-3791
PU Elsevier
VL 28
IS 25-26
UT 000271872200023
BP 2867
EP 2881
DI 10.1016/j.quascirev.2009.07.019
ID 6969
ER

EF