西太平洋帕劳砗磲高分辨率氧同位素记录及其指示的气候环境变化

文汉锋, 赵楠钰, 刘成程, 周鹏超, 王国桢, 晏宏. 西太平洋帕劳砗磲高分辨率氧同位素记录及其指示的气候环境变化[J]. 海洋地质与第四纪地质, 2021, 41(1): 1-13. doi: 10.16562/j.cnki.0256-1492.2020101101
引用本文: 文汉锋, 赵楠钰, 刘成程, 周鹏超, 王国桢, 晏宏. 西太平洋帕劳砗磲高分辨率氧同位素记录及其指示的气候环境变化[J]. 海洋地质与第四纪地质, 2021, 41(1): 1-13. doi: 10.16562/j.cnki.0256-1492.2020101101
WEN Hanfeng, ZHAO Nanyu, LIU Chengcheng, ZHOU Pengchao, WANG Guozhen, YAN Hong. High-resolution oxygen isotope records of Tridacna gigas from Palau, Western Pacific and its climatic and environmental implications[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 1-13. doi: 10.16562/j.cnki.0256-1492.2020101101
Citation: WEN Hanfeng, ZHAO Nanyu, LIU Chengcheng, ZHOU Pengchao, WANG Guozhen, YAN Hong. High-resolution oxygen isotope records of Tridacna gigas from Palau, Western Pacific and its climatic and environmental implications[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 1-13. doi: 10.16562/j.cnki.0256-1492.2020101101

西太平洋帕劳砗磲高分辨率氧同位素记录及其指示的气候环境变化

  • 基金项目: 国家自然科学基金“利用砗磲重建南海北部小时分辨率气候变化初探”(41877399),“地质新时代的人类世:时限、特征与影响”(41991250);中国科学院战略性先导科技专项B类(XDB40000000);中国科学院“西部之光”人才培养引进计划
详细信息
    作者简介: 文汉锋(1995―),男,硕士研究生,研究方向为砗磲地球化学,E-mail:whfloess2019@163.com
    通讯作者: 晏宏(1986―),男,研究员,主要从事热带-亚热带气候环境变化研究,E-mail:yanhong@ieecas.cn
  • 中图分类号: P532,P736.4

High-resolution oxygen isotope records of Tridacna gigas from Palau, Western Pacific and its climatic and environmental implications

More Information
  • 砗磲是海洋中最大的双壳类贝壳,其碳酸盐壳体通常具有年纹层和天纹层,是一种理想的高分辨率古气候研究载体。氧同位素是砗磲古气候研究中最常用的指标之一,但在将其应用于古气候重建之前,通常需要对其现代地球化学过程进行准确的校准。帕劳群岛位于西太平洋暖池西北边缘,其珊瑚礁盘具有丰富的砗磲壳体资源,为开展古气候研究提供了丰富的材料。在本次研究中,对采自帕劳群岛的现代活体库氏砗磲(Tridacna gigas)PL-1的内层壳体进行了高分辨率氧同位素分析,同时利用该砗磲较为清晰的天生长纹层对氧同位素的年代学框架进行了标定。结果表明,该砗磲壳体的氧同位素没有明显的变化趋势,说明砗磲个体的生命效应对氧同位素没有显著影响;砗磲壳体氧同位素没有清晰的年周期变化,常出现不规则的毛刺状峰值。结合现代器测资料分析发现,帕劳砗磲内层壳体的氧同位素记录了热带太平洋ENSO活动对该区域水文气候变化的影响。该研究结果表明,帕劳砗磲内层壳体天生长纹层和氧同位素,具有用于开展高分辨率古气候研究的潜力。

  • 加载中
  • 图 1  西北太平洋2月(最冷月)与6月(最暖月)平均SST分布(1955—2017年)和帕劳位置示意图

    Figure 1. 

    图 2  帕劳器测资料和ENSO指数的对比(1995—2015年)

    Figure 2. 

    图 3  1995—2015年帕劳多年月平均SSS(a)、SST(b)和降水(c)

    Figure 3. 

    图 4  帕劳砗磲PL-1壳体(a)、内层薄片(b)及内层激光共聚焦图像(c)

    Figure 4. 

    图 5  PL-1内层δ18Oc(a)、δ18Oc年龄模型(b)、12点插值的δ18Oc(c)、内层壳体的年生长速率(d)

    Figure 5. 

    图 6  PL-1 δ18Oc年振幅和年生长速率的相关性

    Figure 6. 

    图 7  格点SST和SODA SSS(a)、实测SST和δ18Ow(b)对δ18Oc年振幅的贡献

    Figure 7. 

    图 8  12点δ18Oc与SST(a),SSS(b),降水(c)之间的对比

    Figure 8. 

    图 9  δ18OA(a)与SSTA(b)、降水异常(c)、SSSA(d)、MEI(e)、SOI(f)的对比

    Figure 9. 

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出版历程
收稿日期:  2020-10-11
修回日期:  2020-11-07
刊出日期:  2021-02-28

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