| Li Baohua,Zhao Quanhong,Wang Yongji,Jian Zhimin,Chen Ronghua.Paleoceanographic events of the southern Okinawa Trough during last 20 000 years[J].Acta Oceanologica Sinica,1998,(4):519-530 |
| Paleoceanographic events of the southern Okinawa Trough during last 20 000 years |
| Paleoceanographic events of the southern Okinawa Trough during last 20 000 years |
| 投稿时间：1997-09-26 修订日期：1997-12-08 |
| DOI： |
| 中文关键词: Planktonic foraminifera Okinawa Trough palepceanographic events |
| 英文关键词:Planktonic foraminifera Okinawa Trough palepceanographic events |
| 基金项目: |
| 作者 | 单位 | | Li Baohua | Laboratory of Marine Geology, Tongji University, Shanghai 200092, China | | Zhao Quanhong | Laboratory of Marine Geology, Tongji University, Shanghai 200092, China | | Wang Yongji | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Jian Zhimin | Laboratory of Marine Geology, Tongji University, Shanghai 200092, China | | Chen Ronghua | Second Institute of Oceanography, State Oceanic Administration, Hangzhou, 310012 China |
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| 中文摘要: |
| Two high resolution down-mres(92-255,92-170) are used to study the paleoceanographic events of the southern Okinawa Trough during the last 20 000 years.Planktonic foraminifera are quantitatively analyzed and three paleoceanographic events are recognized.Glacial/post-glacial variations in sea surface temperature(SST),water masses,and upper water mlumn structure are the most important environmental changes recorded by planktonic foramirtifera.There is also an abrupt climatic event(about 10 710-9 170 a BP) during the Termination Ⅰ,planktonic foraminifera(PF) δ18O and SST have a same return pattern,but benthic foraminifera(BF) δ18O doesn't have.Discrepancy between PF δ18O and BF δ18O may reflect that the sea surface water is more sensitive to abrupt,short term envirorunental change than the sea bottom water.High-resolution strata also suggest a middle-Holocene Pulleniatina obliquiloculata minimum event. |
| 英文摘要: |
| Two high resolution down-mres(92-255,92-170) are used to study the paleoceanographic events of the southern Okinawa Trough during the last 20 000 years.Planktonic foraminifera are quantitatively analyzed and three paleoceanographic events are recognized.Glacial/post-glacial variations in sea surface temperature(SST),water masses,and upper water mlumn structure are the most important environmental changes recorded by planktonic foramirtifera.There is also an abrupt climatic event(about 10 710-9 170 a BP) during the Termination Ⅰ,planktonic foraminifera(PF) δ18O and SST have a same return pattern,but benthic foraminifera(BF) δ18O doesn't have.Discrepancy between PF δ18O and BF δ18O may reflect that the sea surface water is more sensitive to abrupt,short term envirorunental change than the sea bottom water.High-resolution strata also suggest a middle-Holocene Pulleniatina obliquiloculata minimum event. |
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