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High-resolution records of thermocline in the Okinawa Trough since about 10000 aBP 被引量:7

High-resolution records of thermocline in the Okinawa Trough since about 10000 aBP
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摘要 The present paper uses planktonic foraminifera and their stableisotopes to study the changes in the depth of thermocline (DOT) in the Okinawa Trough since the last 10000 a based on the analysis of Core B-3GC in the northern Okinawa Trough, together with that of the core in the southern Okinawa Trough. As results show, the thermocline was shallow before 6400 aBP, and deepened afterward, then became shallow again from 4000 to 2000 aBP. The DOT fluctuations display a positive correlation with those of sea surface temperature (SST). In addition, the changes in the northern Okinawa Trough are similar to those in the southern trough, implying a possible connection with the variation of the Kuroshio Current. The changes of SST and DOT suggest that the Kuroshio Current changed its intensity or main axis from 4000 to 2000 aBP and around about 6400 aBP respectively. Moreover, the changes of DOT from 8200 to 6400 aBP may indicate a gradual intensification of the Kuroshio Current. The present paper uses planktonic foraminifera and their stable isotopes to study the changes in the depth of thermocline (DOT) in the Okinawa Trough since the last 10000 a based on the analysis of Core B-3GC in the northern Okinawa Trough, together with that of the core in the southern Okinawa Trough. As results show, the thermocline was shallow before 6400 aBP, and deepened afterward, then became shallow again from 4000 to 2000 aBP. The DOT fluctuations display a positive correlation with those of sea surface temperature (SST). In addition, the changes in the northern Okinawa Trough are similar to those in the southern trough, implying a possible connection with the variation of the Kuroshio Current. The changes of SST and DOT suggest that the Kuroshio Current changed its intensity or main axis from 4000 to 2000 aBP and around about 6400 aBP respectively. Moreover, the changes of DOT from 8200 to 6400 aBP may indicate a gradual intensification of the Kuroshio Current.
出处 《Science China Earth Sciences》 SCIE EI CAS 2001年第3期193-200,共8页 中国科学(地球科学英文版)
基金 This work was supported by the National Natural Science Foundation of China (Grant Nos. 49999560, 49776289) the Program for the Young Scientific and Technological Stars of Shanghai (Grant No. 98QG14043).
关键词 冲绳马槽 thermocline (点) 的深度 海表面温度(SST ) 自台湾东面的菲律宾海流向日本的暖流电流 PLANKTONIC 有孔虫类 稳定的同位素 Okinawa Trough depth of thermocline (DOT) sea surface temperature (SST) Kuroshio Current planktonic foraminifera stable isotopes
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参考文献14

  • 1Li Baohua, Zhao Quanhong, Jian Zhimin (Laboratory of Marine Geology, Tongji University, Shanghai 200092, China)Wang Yongji, (First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China)Chen Ronghua (Second Institute of Oceanograp.Paleoceanographic events of the southern Okinawa Trough during last 20 000 years[J].Acta Oceanologica Sinica,1998,17(4):519-530. 被引量:5
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