FN Archimer Export Format
PT J
TI Dominant Northern Hemisphere climate control over millennial-scale glacial sea-level variability
BT 
AF ARZ, Helge W.
   LAMY, Frank
   GANOPOLSKI, Andrey
   NOWACZYK, Norbert
   PAETZOLD, Juergen
AS 1:1;2:1;3:;4:1;5:3;
FF 1:;2:;3:;4:;5:;
C1 Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany.
   Potsdam Inst Climate Impact Res, D-14473 Potsdam, Germany.
   Univ Bremen, Res Ctr Ocean Margins, D-28359 Bremen, Germany.
C2 GFZ GERMAN RES CTR GEOSCI, GERMANY
   PIK, GERMANY
   UNIV BREMEN, GERMANY
IF 4.11
TC 149
UR https://archimer.ifremer.fr/doc/00236/34700/33072.pdf
LA English
DT Article
CR IMAGES 1-MD101
BO Marion Dufresne
AB Based on a radiocarbon and paleomagnetically dated sediment record from the northern Red Sea and the exceptional sensitivity of the regional changes in the oxygen isotope composition of sea water to the sea-level-dependent water exchange with the Indian Ocean, we provide a new global sea-level reconstruction spanning the last glacial period. The sea-level record has been extracted from the temperature-corrected benthic stable oxygen isotopes using coral-based sea-level data as constraints for the sea-level/oxygen isotope relationship. Although, the general features of this millennial-scale sea-level records have strong similarities to the rather symmetric and gradual Southern Hemisphere climate patterns, we observe, in constrast to previous findings, pronounced sea level rises of up to 25 in to generally correspond with Northern Hemisphere warmings as recorded in Greenland ice-core interstadial intervals whereas sea-level lowstands mostly occur during cold phases. Corroborated by CLIMBER-2 model results, the close connection of millennial-scale sea-level changes to Northern Hemisphere temperature variations indicates a primary climatic control on the mass balance of the major Northern Hemisphere ice sheets and does not require a considerable Antarctic contribution.
PY 2007
PD FEB
SO Quaternary Science Reviews
SN 0277-3791
PU Pergamon-elsevier Science Ltd
VL 26
IS 3-4
UT 000245779200005
BP 312
EP 321
DI 10.1016/j.quascirev.2006.07.016
ID 34700
ER

EF