FN Archimer Export Format
PT J
TI Sea surface temperature across the Subarctic North Pacific and marginal seas through the past 20,000 years: A paleoceanographic synthesis
BT 
AF Davis, Catherine V.
   Myhre, Sarah E.
   Deutsch, Curtis
   Caissie, Beth
   Praetorius, Summer
   Borreggine, Marisa
   Thunell, Robert
AS 1:1;2:2,3;3:3;4:4;5:5;6:3;7:1;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 School of Earth, Oceans, And the Environment, University of South Carolina, 701 Sumter St, Columbia, SC, USA
   Future of Ice Initiative, University of Washington, 1492 NE Boat St., Seattle, WA, 98105, USA
   School of Oceanography, University of Washington, 1503 NE Boat St., Seattle, WA, 98105, USA
   Department of Geological and Atmospheric Sciences, Iowa State University, 253 Science, Ames, IA, 50011, USA
   U.S. Geological Survey, 345 Middlefield Rd, Menlo Park, CA, 94025, USA
C2 UNIV S CAROLINA, USA
   UNIV WASHINGTON, USA
   UNIV WASHINGTON, USA
   UNIV IOWA, USA
   GEOL SURVEY, USA
IF 4.112
TC 5
UR https://archimer.ifremer.fr/doc/00646/75814/76758.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76759.xml
   https://archimer.ifremer.fr/doc/00646/75814/76760.docx
   https://archimer.ifremer.fr/doc/00646/75814/76761.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76762.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76763.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76764.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76765.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76766.pdf
   https://archimer.ifremer.fr/doc/00646/75814/76767.docx
LA English
DT Article
CR MD 122 / WEPAMA
   MD 126 / MONA
BO Marion Dufresne
DE ;Sea surface temperature;North Pacific;Bering sea;Sea of Okhotsk;Deglaciation
AB Deglacial sea surface conditions in the subarctic North Pacific and marginal seas are the subject of increasing interest in paleoceanography. However, a cohesive picture of near-surface oceanography from which to compare inter and intra-regional variability through the last deglaciation is lacking. We present a synthesis of sea surface temperature covering the open North Pacific and its marginal seas, spanning the past 20 ka using proxy records from foraminiferal calcite (δ18O and Mg/Ca) and coccolithophore alkenones (Uk’37). Sea surface temperature proxies tend to be in agreement through the Holocene, though Uk’37 records are often interpreted as warmer than adjacent δ18O or Mg/Ca records during the Last Glacial Maximum and early deglaciation. In the Sea of Okhotsk, Holocene discrepancies between δ18O and Uk’37 may be the result of changes in near-surface stratification. We find that sea-surface warming occurred prior to the onset of the Bølling-Allerød (14.7 ka) and coincident with the onset of the Holocene (11.7 ka) in much of the North Pacific and Bering Sea. Proxy records also show a cold reversal roughly synchronous with the Younger Dryas (12.9–11.7 ka). After the onset of the Holocene, the influence of an intensified warm Kuroshio Current is evident at higher latitudes in the Western Pacific, and an east-west seesaw in sea surface temperature, likely driven by changes in the strength of the North Pacific Gyre, characterizes the open interglacial North Pacific. 
PY 2020
PD OCT
SO Quaternary Science Reviews
SN 0277-3791
PU Elsevier BV
VL 246
UT 000582428500009
DI 10.1016/j.quascirev.2020.106519
ID 75814
ER

EF