海洋地质与第四纪地质2024，Vol.44Issue(4)：41-53,13.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
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
摘要
Abstract
Tridacna shells,known for their distinct growth bands,serve as excellent proxies for recording tropical marine climate changes.The δ18O and δ13C in Tridacna shells have been applied in the Quaternary paleoclimate research.However,most previous researches focused on the inner layer,while the outer layer received less attention.We conducted a comprehensive analysis at a monthly resolution δ18O,δ13C tests on both the inner and outer layers,as well as daily growth band scans on the inner layer of modern Tridacna squamosa from the Xisha Islands in the South China Sea.Results reveal that the outer layer exhibited higher δ18O values than the inner layer.In addition,both shells displayed similar variation patterns,being primarily influenced by sea surface temperature(SST),and indicating that the δ18O of the outer layer could reliably indicate climate and environmental changes.In contrast,significant differences in δ13C value were observed between the inner and outer layers.The inner layer displayed a noticeable annual cycle in δ13C value.By comparing the inner layer δ13C,climatic and environmental parameters,and daily growth rate(DGR),we determined that the seasonal variations in inner layer δ13C were linked to the primary productivity and the life activities of Tridacna.Meanwhile,the δ13C of the outer layer,which is relatively negative compared to the inner layer,exhibited a continuous downward trend without seasonal changes.This discrepancy may be attributed to the sampling path deviating from the maximum growth axis.关键词
砗磲/δ13C/δ18O/气候变化/南海Key words
Tridacna/δ13C/δ18O/climate change/South China Sea分类
海洋科学引用本文复制引用
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):41-53,13.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) （42103083）
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) （2021M693149）
