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18.5ka以来冲绳海槽中部沉积物碎屑态来源和古环境变化的常量元素记录

蔡明江 李铁刚 于心科 陈红瑾 徐兆凯

海洋地质前沿2017,Vol.33Issue(5):22-31,10.
海洋地质前沿2017,Vol.33Issue(5):22-31,10.DOI:10.16028/j.1009-2722.2017.05003

18.5ka以来冲绳海槽中部沉积物碎屑态来源和古环境变化的常量元素记录

PROVENANCE OF DETRITAL DEPOSITS AND PALEOENVIRONMENTAL CHANGES IN THE MIDDLE OKINAWA SINCE 18.5 KA: EVIDENCE FROM MAJOR ELEMENTS

蔡明江 1李铁刚 2于心科 3陈红瑾 4徐兆凯1

作者信息

  • 1. 中国科学院海洋研究所海洋地质与环境重点实验室,青岛266071
  • 2. 中国科学院大学,北京100049
  • 3. 国家海洋局第一海洋研究所海洋沉积与环境地质国家海洋局重点实验室,青岛266061
  • 4. 青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室,青岛266061
  • 折叠

摘要

Abstract

Major elements and grain sizes for 151 detrital samples collected from the core KX12-3 at the middle Okinawa Trough were studied for reconstruction of sediment provenance and paleoenvironment over the time of last 18.5 ka.Upon the variations in major element compositions,the core is divided to two distinct depositional units,Segment 1 (Z1;18.5-9.6 ka) and Segment 2 (Z2;<9.6 ka).Deposits of the Z1 (18.5-9.6 ka) are dominated by terrigenous detrital sediments from large Chinese rivers (e.g.the Changjiang and the Huanghe).The detrital sediments of the Z2 have same provenances dominated by these Chinese rivers,but mixed with some fine-grained materials from Taiwan,which may have been transported to the study area by the Kuroshio Current.The K-Ah volcanic eruption happened at 7.3 ka is also recorded in the core.Integrated study of correlation analyses,R-type factor,and major-element ratio show that the vertical change in major elements are mainly controlled by inputs of nearby terrestrial materials,whereas the contribution from hydrothermal activity and volcanism is little.In particular,the contribution of nearby terrestrial provenance shows an obvious trend which could be well correlated with the sea level fluctuation and the evolution of the Kuroshio Current.Furthermore,a prominent decline in Fe2O3 、MgO、Fe/Ti、Mg/Ti values and finer grain size that occurred 5.0-3.5 ka may be linked to a suppression of the Kuroshio Current,or the shifting out of the current from the study area.

关键词

冲绳海槽中部/沉积物碎屑态/常量元素/海平面波动/黑潮

Key words

middle Okinawa Trough/detrital sediment fraction/major elements/sea level fluctuation/Kuroshio Current

分类

海洋科学

引用本文复制引用

蔡明江,李铁刚,于心科,陈红瑾,徐兆凯..18.5ka以来冲绳海槽中部沉积物碎屑态来源和古环境变化的常量元素记录[J].海洋地质前沿,2017,33(5):22-31,10.

基金项目

国家自然科学基金委员会—山东省人民政府海洋科学研究中心联合资助项目(U1606401) (U1606401)

国家自然科学基金(41376064,41106043,41676038) (41376064,41106043,41676038)

国家海洋局全球变化与海气相互作用专项(GASI-GEOGE-06-02,GASI-GEOGE-02) (GASI-GEOGE-06-02,GASI-GEOGE-02)

海洋地质前沿

OACSCDCSTPCD

1009-2722

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