FN Archimer Export Format
PT J
TI Evidence for the 8,200 a BP cooling event in the middle Okinawa Trough
BT 
AF YU, H
   XIONG, Y
   LIU, Z
   BERNE, Serge
   HUANG, C
   JIA, G
AS 1:1;2:2;3:3;4:4;5:5;6:6;
FF 1:;2:;3:;4:PDG-DOP-DCB-GM-LES;5:;6:;
C1 Rice Univ, Dept Earth Sci, Houston, TX 77005 USA.
   Univ Houston, Dept Geosci, Houston, TX 77204 USA.
   SOA, Inst Oceanog 1, Marine Geol Div, Qingdao, Peoples R China.
   IFREMER, F-29280 Plouzane, France.
   Natl Cheng Kung Univ, Dept Earth Sci, Tainan 701, Taiwan.
   Chinese Acad Sci, Guangzhou Inst Geochem, Ghangzhou 510640, Peoples R China.
C2 UNIV RICE, USA
   UNIV HOUSTON, USA
   SOA, CHINA
   IFREMER, FRANCE
   UNIV NATL CHENG KUNG NCKU, TAIWAN
   CHINESE ACAD SCI, CHINA
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-int-hors-europe
   copubli-sud
IF 1.186
TC 19
UR https://archimer.ifremer.fr/doc/2008/publication-4207.pdf
LA English
DT Article
AB Based on new and existing data on oxygen isotopes, alkenone-surface seawater temperature trends, planktonic foraminifers, lithology, and clay mineral composition of piston cores, a distinct cooling event has been identified around 8,200 cal a B.P. in the middle Okinawa Trough, northwest Pacific. This corresponds to the 8,200 a B.P. cooling event recorded in many places of the Northern Hemisphere. During this event, the local temperature decreased by 1 degrees C, and the delta O-18 value increased by 0.6%omicron. A strengthened Asian winter monsoon is the most probable cause for this event, which thus adds further credibility to the contention that we are dealing here with a global phenomenon.
PY 2008
PD JUL
SO Geo-Marine Letters
SN 0276-0460
PU Springer
VL 28
IS 3
UT 000255255000001
BP 131
EP 136
DI 10.1007/s00367-007-0095-x
ID 4207
ER

EF