热带西太平洋250 ka来浮游有孔虫<i>G.sacculifer</i>壳体质量变化特征及控制机理

秦秉斌; 李铁刚; 常凤鸣; 熊志方; 郝鹏

doi:10.3724/SP.J.1140.2014.03085

热带西太平洋250 ka来浮游有孔虫G.sacculifer壳体质量变化特征及控制机理

秦秉斌^1,2,
李铁刚^1, ,,
常凤鸣¹,
熊志方¹,
郝鹏^1,2

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

基金项目:

国家自然科学基金项目(41230959,41106042,41076030)

中国科学院战略性先导科技专项(XDA10010305)

国家海洋局基础研究项目

详细信息

作者简介:
秦秉斌(1989-),男,硕士生,主要从事古海洋与古环境研究,E-mail:qbbqbb@163.com

中图分类号: P736.4
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- 文章访问数: 1796
- HTML全文浏览量: 213
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出版历程
- 收稿日期: 2013-12-18
- 修回日期: 2014-03-08

SHELL WEIGHT CHANGES OF PLANKTONIC FORAMINIFERA G. sacculifer FROM THE TROPICAL WESTERN PACIFIC DURING THE LAST 250 ka AND CONTROLLING MECHANISMS

1. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071;
2. University of Chinese Academy of Sciences, Beijing 100049, China

摘要

摘要: 作为新兴的海水CO₃^2-替代性指标，浮游有孔虫壳体质量对于海洋碳循环研究具有重要意义。测定了热带西太平洋WP7孔250 ka以来表层浮游有孔虫G.sacculifer壳体质量。除了在MIS1和MIS4期外，壳体质量显示冰期重、间冰期轻的旋回特征，响应大气pCO₂变化，表明大气pCO₂变化是该海域浮游有孔虫壳体质量变化的主控因素。研究结果表明MIS4期间壳体质量异常低值可能是该时期加强的上升流和CaCO₃溶解事件共同导致。温度与营养盐浓度并不是壳体质量异常的主要原因，共生体则可能是影响因素。G.sacculifer壳体质量与大气pCO₂整体上良好的反相关关系表明其可以作为可靠的表层海水CO₃^2-替代性指标。
- 浮游有孔虫壳体质量 /
- 碳酸根离子浓度 /
- 大气pCO₂ /
- 热带西太平洋
Abstract: As a new proxy to reconstruct sea water[CO₃^2-] in the past, shell weight of planktonic foraminifera can provide clues to revealing ocean carbon cycle. Shell weights of G. sacculifer measured from a tropical western Pacific sediment core WP7 during the last 250 ka show higher values in glacial periods and lower values in interglacial periods responding to changes in CO₂ concentrations in the Antarctic Ice Core of Vostok, except in MIS1 and MIS4. Hence, shell weight variations in this sea area are mainly controlled by the CO₂ concentration in atmosphere. As a result of intensified upwelling and carbonate dissolution, shell weights have reduced during MIS4. Shell weights also can be affected by coexisting symbionts, but not the changes in temperature and surface nutrient levels. Shell weights of G. sacculifer exhibit a generally inverse relationship with CO₂ concentrations, and thus they can be used as a reliable proxy to trace variations in[CO₃^2-] of surface water.
- shell weights of planktonic foraminifera /
- carbonate ion concentration /
- atmospheric pCO₂ /
- tropical western Pacific

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