西菲律宾海26万年来古生产力变化的颗石藻证据

安佰正, 李铁刚, 刘健, 孙晗杰, 徐兆凯, 唐正, 赵京涛. 西菲律宾海26万年来古生产力变化的颗石藻证据[J]. 海洋地质与第四纪地质, 2019, 39(3): 113-121. doi: 10.16562/j.cnki.0256-1492.2018052301
引用本文: 安佰正, 李铁刚, 刘健, 孙晗杰, 徐兆凯, 唐正, 赵京涛. 西菲律宾海26万年来古生产力变化的颗石藻证据[J]. 海洋地质与第四纪地质, 2019, 39(3): 113-121. doi: 10.16562/j.cnki.0256-1492.2018052301
AN Baizheng, LI Tiegang, LIU Jian, SUN Hanjie, XU Zhaokai, TANG Zheng, ZHAO Jingtao. Variations of primary productivity in the western Philippine Sea in the past 260000 years:evidence from coccolith[J]. Marine Geology & Quaternary Geology, 2019, 39(3): 113-121. doi: 10.16562/j.cnki.0256-1492.2018052301
Citation: AN Baizheng, LI Tiegang, LIU Jian, SUN Hanjie, XU Zhaokai, TANG Zheng, ZHAO Jingtao. Variations of primary productivity in the western Philippine Sea in the past 260000 years:evidence from coccolith[J]. Marine Geology & Quaternary Geology, 2019, 39(3): 113-121. doi: 10.16562/j.cnki.0256-1492.2018052301

西菲律宾海26万年来古生产力变化的颗石藻证据

  • 基金项目:
    国家自然科学基金项目“15万年以来热带西太平洋颗石藻碳酸钙输出通量演变及其影响因素”(41706070), “中更新世以来热带西太平洋颗石藻钙化作用研究”(41876041), “80万年来热带西太平洋上层水体pH和pCO2演变及影响机理”(41230959);青岛海洋科学与技术国家实验室鳌山科技创新计划项目(2016ASKJ13);中国科学院海洋地质与环境重点实验室开放基金“西太平洋上层水体现代颗石藻碳酸钙分布特征”(MGE2017KG03);山东省自然科学基金面上项目“山东半岛东部近岸中、晚全新世高分辨率环境演化过程研究”(ZR2016DM12)
详细信息
    作者简介: 安佰正(1984—),男,博士,主要从事古海洋学与古环境研究,E-mail: an_baizheng@126.com
    通讯作者: 李铁刚(1965—),男,研究员,主要从事古海洋与古环境研究,E-mail: tgli@fio.org.ac.cn
  • 中图分类号: P736

  • 文凤英编辑

Variations of primary productivity in the western Philippine Sea in the past 260000 years:evidence from coccolith

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  • 基于国际海洋古全球变化研究项目(IMAGES)在西菲律宾海本哈姆海台获取的高质量柱状沉积物岩芯MD06-3047(17°00.44′N、124°47.93′E),利用颗石藻下透光带属种Florisphaera profunda的相对丰度以及初级生产力转换函数,恢复了260 ka以来西菲律宾海上部水体营养跃层以及初级生产力的变化历史。发现该区域26万年以来初级生产力冰期-间冰期变化特征较不明显,冰期生产力平均值略高于间冰期。通过与前人已发表的指示东亚冬季风强弱的伊利石/蒙脱石记录和热带太平洋纬向表层海水温度梯度记录的对比,提出MIS 8期以来,热带西菲律宾海古生产力变化的主要受控因素在MIS 5a左右发生明显转变。在MIS 8后期至MIS 5a之间,初级生产力受到长期类ENSO过程的影响较为显著,当热带东西太平洋海水表层温度梯度较小的时期,认为热带太平洋处于类El Niño状态,此时西菲律宾海营养跃层相对较浅,生产力较高,反之则相反。而在MIS 5末期至末次冰消期时段,生产力受东亚冬季风的影响相对于长期ENSO过程更强,可能掩盖了后者的古生产力信号。冰期东亚冬季风加强,一方面,可以引起上部水体混合加强,增加下部营养物质向上的输送,另一方面大量风尘物质的输入可以刺激颗石藻的生长;反之在冰消期,水体混合较弱,风尘输入显著减少,生产力也随之降低。

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  • 图 1  MD06-3047岩芯站位图

    Figure 1. 

    图 2  260 ka以来MD06-3047岩芯F. profunda相对百分含量以及初级生产力变化曲线

    Figure 2. 

    图 3  MD06-3047站F. profunda百分含量与初级生产力频谱分析

    Figure 3. 

    图 4  西太平洋边缘海区260ka以来不同站位F.profunda百分含量对比

    Figure 4. 

    图 5  过去260ka以来西菲律宾海MD06-3047岩芯初级生产力及F. profunda相对百分含量变化与其他古环境指标对比图

    Figure 5. 

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收稿日期:  2018-05-23
修回日期:  2018-08-05
刊出日期:  2019-06-28

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