南海西沙群岛现代鳞砗磲内外层壳体稳定碳、氧同位素变化特征及其影响因素

梁承德, 韩韬, 赵楠钰, 文汉锋, 王国桢, 刘成程, 杨昊天, 耿鋆, 晏宏. 南海西沙群岛现代鳞砗磲内外层壳体稳定碳、氧同位素变化特征及其影响因素[J]. 海洋地质与第四纪地质, 2024, 44(4): 41-53. doi: 10.16562/j.cnki.0256-1492.2024012501
引用本文: 梁承德, 韩韬, 赵楠钰, 文汉锋, 王国桢, 刘成程, 杨昊天, 耿鋆, 晏宏. 南海西沙群岛现代鳞砗磲内外层壳体稳定碳、氧同位素变化特征及其影响因素[J]. 海洋地质与第四纪地质, 2024, 44(4): 41-53. doi: 10.16562/j.cnki.0256-1492.2024012501
LIANG Chengde, HAN Tao, ZHAO Nanyu, WEN Hanfeng, WANG Guozhen, LIU Chengcheng, YANG Haotian, GENG Jun, YAN Hong. Variation and influencing factors of δ13C and δ18O in the inner and outer layers of modern Tridacna squamosa from the Xisha Islands, South China Sea[J]. Marine Geology & Quaternary Geology, 2024, 44(4): 41-53. doi: 10.16562/j.cnki.0256-1492.2024012501
Citation: LIANG Chengde, HAN Tao, ZHAO Nanyu, WEN Hanfeng, WANG Guozhen, LIU Chengcheng, YANG Haotian, GENG Jun, YAN Hong. Variation and influencing factors of δ13C and δ18O in the inner and outer layers of modern Tridacna squamosa from the Xisha Islands, South China Sea[J]. Marine Geology & Quaternary Geology, 2024, 44(4): 41-53. doi: 10.16562/j.cnki.0256-1492.2024012501

南海西沙群岛现代鳞砗磲内外层壳体稳定碳、氧同位素变化特征及其影响因素

  • 基金项目: 国家自然科学基金“南海不同种类砗磲内、外层壳体的δ13C变化特征及其对气候环境的指示意义”(42103083),“砗磲地球化学与古气候古天气学”(42025304),“极端事件及其环境效应的地球化学示踪”(42221003);中国博士后科学基金面上资助“南海砗磲内、外层壳体碳同位素的变化特征及其环境指示意义”(2021M693149)
详细信息
    作者简介: 梁承德(1999—),男,硕士研究生,第四纪地质学专业,E-mail:liangchengde@ieecas.cn
    通讯作者: 韩韬(1992—),男,博士后,主要从事珊瑚与砗磲古气候研究,E-mail:hantao@ieecas.cn 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: P736.4

Variation and influencing factors of δ13C and δ18O in the inner and outer layers of modern Tridacna squamosa from the Xisha Islands, South China Sea

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  • 砗磲具有清晰的生长纹层,是记录热带海洋气候变化的良好载体,其壳体δ18O、δ13C已广泛应用于第四纪古气候研究。然而,目前大多数研究主要集中在内层壳体,关于外层壳体的研究十分稀少。本研究通过对采自南海西沙群岛浪花礁一个现代鳞砗磲的内外层壳体进行月分辨率δ18O、δ13C测试和内壳日生长纹层扫描,分析内外层壳体δ18O和δ13C的变化特征及其影响因素。结果显示该砗磲外壳δ18O比内壳δ18O更加偏正,但是两者都具有十分相似的变化特征,主要受到海表面温度的控制,表明砗磲内外层壳体δ18O能够可靠地指示气候环境的变化。砗磲内外层壳体δ13C存在较大的差异,其中内壳δ13C具有明显的年周期变化。通过对比分析砗磲内壳δ13C与日生长速率、气候环境参数,发现内壳δ13C的季节变化主要与初级生产力和砗磲自身生命活动有关。砗磲外壳δ13C相对于内壳δ13C较为偏负,表现出持续下降的趋势,且无季节性变化,这可能是由采样路径偏离最大生长轴导致的。

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  • 图 1  砗磲样品及其地理位置

    Figure 1. 

    图 2  2013—2018年砗磲的月平均碳、氧同位素记录、日生长速率与当地气候环境参数对比

    Figure 2. 

    图 3  砗磲日生长速率(DGR)和太阳辐射的关系

    Figure 3. 

    图 4  样品LHJ-2 内外层壳体δ18O、SST以及δ18OSW之间的关系

    Figure 4. 

    图 5  2013—2018年西沙群岛环境参数与样品LHJ-2壳体δ13C的对比

    Figure 5. 

    图 6  样品LHJ-2内壳δ13CIL、日生长速率以及各环境参数之间的相关性

    Figure 6. 

    图 7  样品LHJ-2外壳δ13COLpCO2及其δ13C的对比

    Figure 7. 

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出版历程
收稿日期:  2024-01-25
修回日期:  2024-05-07
录用日期:  2024-05-06
刊出日期:  2024-08-28

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