Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera
Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera
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海因里希事件在冲绳海槽的印记:来自氧同位素和浮游有孔虫的证据
DOI:
10.1016/s0031-0182(01)00332-7
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发表时间:
2001-12
期刊:
影响因子:
--
通讯作者:
Michael A. et al
中科院分区:
文献类型:
--
作者:
Tiegang Li;Zhenxia Liu;Michael A. et al
Planktonic foraminiferal faunas, oxygen isotope and modern analog technique sea surface temperature records were obtained in piston core DGKS9603 (28°08.869′N, 127°16.238′E, water depth 1100 m) collected from the middle Okinawa Trough. During the last glaciation, four cold events were identified and correlate Heinrich events (HE) H2–5 of the last 45 ka. During the last deglaciation, core DGKS9603 has begun to be influenced by the Kuroshio since about 16 cal ka BP. Three weakenings of this warm current occurred at about 2.8–5.3, 11.4 and 15.5 cal ka BP respectively. Among the three fluctuations, the oldest one is synchronous with HE1 and could be a response to the strong cooling observed in the North Atlantic Ocean. The fluctuation occurring at about 11.4 cal ka ago corresponds to the Younger Dryas within the age error bars. Our observations provide new evidence that the HEs documented from Greenland and the northern North Atlantic had a global climatic impact. Changes in the intensity of the East Asian monsoon could be the main mechanism responsible for the paleoceanographic variations observed in the Okinawa Trough.
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DOI:
10.1007/bf02047433
发表时间:
1971-03
期刊:
Journal of the International Association for Mathematical Geology
影响因子:
--
作者:
J. E. Klovan;J. Imbrie
通讯作者:
J. E. Klovan;J. Imbrie
影响因子:
1.9
作者:
H. Ujiié;Y. Ujiié
通讯作者:
H. Ujiié;Y. Ujiié
影响因子:
--
作者:
D. Andreasen;A. Ravelo
通讯作者:
D. Andreasen;A. Ravelo
影响因子:
64.8
作者:
BOND, G;BROECKER, W;BONANI, G
通讯作者:
BONANI, G
DOI:
10.4116/jaqua.37.211
发表时间:
1998-07
期刊:
The Quaternary Research (daiyonki-kenkyu)
影响因子:
--
作者:
Luejiang Wang;T. Oba
通讯作者:
Luejiang Wang;T. Oba