冲绳海槽二万年以来沉积物中烯酮化合物与古温度的研究

卢冰; 潘建明; 陈荣华; 唐运千; 施晓来

冲绳海槽二万年以来沉积物中烯酮化合物与古温度的研究

国家海洋局第二海洋研究所, 国家海洋局海底科学重点实验室, 杭州 310012

基金项目: 浙江省自然科学基金资助项目(编号:495031)

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出版历程
- 收稿日期: 1998-03-13
- 修回日期: 1999-06-21

Study on the paleotemperature and alkenon, in sediment from the Okinawa Trough during the last 20000 a

Second Institute of Oceanography, State Ocenic Administration; Key Lab of Submarine Geoscience of State Ocenic Administration, Hangzhou 310012

摘要

摘要: 应用烯酮化合物的不饱和比值U₃₇^k计算得出冲绳海槽海水古温度波动幅度在15.9～26.2℃之间,平均为22.9℃,和冬季实测表层水温22.0℃相接近,探讨了U₃₇^k值在冲绳海槽指示的古海水温度和季节有关,主要反映在冬季。
- 沉积物 /
- 烯酮化合物 /
- 超微化石 /
- 古温度
Abstract: The sea surface temperature is estimated by the U₃₇^K value (the unsaturated ratio of alkenone) in sediment from the Okinawa Trough during the last 20000 a.They range from 15.9 to 96.2℃,the average is 22.9℃.The sea surface temperature in winter is 22℃.It indicates that the sea surface temperature from U₃₇^K is close to the above value.
- Sediment /
- alkenone /
- manofossils /
- paleotemperature

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参考文献(20)

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