FN Archimer Export Format
PT J
TI Deglacial patterns of South Pacific overturning inferred from 231Pa and 230Th
BT 
AF Ronge, Thomas A.
   Lippold, Jörg
   Geibert, Walter
   Jaccard, Samuel L.
   Mieruch-Schnülle, Sebastian
   Süfke, Finn
   Tiedemann, Ralf
AS 1:1;2:2;3:1;4:4,5;5:1;6:2;7:1,3;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Department of Marine Geology, Alfred-Wegener-Institut Helmholtz Zentrum für Polar-und Meeresforschung, PO Box 120161, 27515, Bremerhaven, Germany
   Institut für Geowissenschaften, Universität Heidelberg, 69120, Heidelberg, Germany
   MARUM Center for Marine Environmental Sciences, Universität Bremen, 28334, Bremen, Germany
   Institut für Geologie & Oeschger Center for Climate Change Research, Universität Bern, 3012, Bern, Switzerland
   Institute of Earth Sciences, University of Lausanne, 1015, Lausanne, Switzerland
C2 INST A WEGENER, GERMANY
   UNIV HEIDELBERG, GERMANY
   UNIV BREMEN MARUM, GERMANY
   UNIV BERN, SWITZERLAND
   UNIV LAUSANNE, SWITZERLAND
IN DOAJ
IF 4.997
TC 4
UR https://archimer.ifremer.fr/doc/00729/84133/89063.pdf
   https://archimer.ifremer.fr/doc/00729/84133/89064.docx
LA English
DT Article
CR IMAGES 3-IPHIS-MD106
   VT 90 / SOUC
BO Marion Dufresne
AB The millennial-scale variability of the Atlantic Meridional Overturning Circulation (AMOC) is well documented for the last glacial termination and beyond. Despite its importance for the climate system, the evolution of the South Pacific overturning circulation (SPOC) is by far less well understood. A recently published study highlights the potential applicability of the 231Pa/230Th-proxy in the Pacific. Here, we present five sedimentary down-core profiles of 231Pa/230Th-ratios measured on a depth transect from the Pacific sector of the Southern Ocean to test this hypothesis using downcore records. Our data are consistent with an increase in SPOC as early as 20 ka that peaked during Heinrich Stadial 1. The timing indicates that the SPOC did not simply react to AMOC changes via the bipolar seesaw but were triggered via Southern Hemisphere processes. 
PY 2021
PD OCT
SO Scientific Reports
SN 2045-2322
PU Springer Science and Business Media LLC
VL 11
IS 1
UT 000707419500019
DI 10.1038/s41598-021-00111-1
ID 84133
ER

EF