FN Archimer Export Format
PT J
TI A Southern Ocean trigger for Northwest Pacific ventilation during the Holocene?
BT 
AF RELLA, S. F.
   UCHIDA, M.
AS 1:1;2:1,2;
FF 1:;2:;
C1 Natl Inst Environm Studies, Ctr Environm Measurement & Anal, Tsukuba, Ibaraki 3058506, Japan.
   Japan Agcy Marine Earth Sci & Technol JAMSTEC, Res Inst Global Change, Yokosuka, Kanagawa 2370061, Japan.
C2 NIES, JAPAN
   JAMSTEC, JAPAN
IN DOAJ
IF 5.578
TC 18
UR https://archimer.ifremer.fr/doc/00291/40189/38732.pdf
   https://archimer.ifremer.fr/doc/00291/40189/38733.doc
LA English
DT Article
CR MD 128 / SWAF
BO Marion Dufresne
AB Holocene ocean circulation is poorly understood due to sparsity of dateable marine archives with submillennial-scale resolution. Here we present a record of mid-depth water radiocarbon contents in the Northwest (NW) Pacific Ocean over the last 12.000 years, which shows remarkable millennial-scale variations relative to changes in atmospheric radiocarbon inventory. Apparent decoupling of these variations from regional ventilation and mixing processes leads us to the suggestion that the mid-depth NW Pacific may have responded to changes in Southern Ocean overturning forced by latitudinal displacements of the southern westerly winds. By inference, a tendency of in-phase related North Atlantic and Southern Ocean overturning would argue against the development of a steady bipolar seesaw regime during the Holocene.
PY 2014
PD FEB
SO Scientific Reports
SN 2045-2322
PU Nature Publishing Group
VL 4
IS 4046
UT 000331397500001
BP 1
EP 11
DI 10.1038/srep04046
ID 40189
ER

EF