FN Archimer Export Format
PT J
TI Global oceanic oxygenation controlled by the Southern Ocean through the last deglaciation
BT 
AF Wang, Yi
   Costa, Kassandra M.
   Lu, Wanyi
   Hines, Sophia K. V.
   Nielsen, Sune G.
AS 1:1,2,3;2:1;3:1;4:4;5:1,2,5;
FF 1:;2:;3:;4:;5:;
C1 Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
   NIRVANA Laboratories, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
   Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA.
   Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
   Centre de Recherches Pétrographiques et Géochimiques, CNRS, Université de Lorraine, 15 rue Notre Dame des Pauvres, 54501 Vandoeuvre lès Nancy, France.
C2 WHOI, USA
   WHOI, USA
   UNIV TULANE, USA
   WHOI, USA
   UNIV LORRAINE, FRANCE
IN DOAJ
IF 13.6
TC 0
UR https://archimer.ifremer.fr/doc/00872/98437/107870.pdf
   https://archimer.ifremer.fr/doc/00872/98437/107871.zip
   https://archimer.ifremer.fr/doc/00872/98437/107872.pdf
LA English
DT Article
CR IMAGES 3-IPHIS-MD106
BO Marion Dufresne
AB Ocean dissolved oxygen (DO) can provide insights on how the marine carbon cycle affects global climate change. However, the net global DO change and the controlling mechanisms remain uncertain through the last deglaciation. Here, we present a globally integrated DO reconstruction using thallium isotopes, corroborating lower global DO during the Last Glacial Maximum [19 to 23 thousand years before the present (ka B.P.)] relative to the Holocene. During the deglaciation, we reveal reoxygenation in the Heinrich Stadial 1 (~14.7 to 18 ka B.P.) and the Younger Dryas (11.7 to 12.9 ka B.P.), with deoxygenation during the Bølling-Allerød (12.9 to 14.7 ka B.P.). The deglacial DO changes were decoupled from North Atlantic Deep Water formation rates and imply that Southern Ocean ventilation controlled ocean oxygen. The coherence between global DO and atmospheric CO 2 on millennial timescales highlights the Southern Ocean’s role in deglacial atmospheric CO 2 rise. 
PY 2024
PD JAN
SO Science Advances
SN 2375-2548
PU American Association for the Advancement of Science (AAAS)
VL 10
IS 3
DI 10.1126/sciadv.adk2506
ID 98437
ER

EF