Ontogenic Decrease of δ13C in Bivalve Shell:Evidence of Vital Effect

摘要：

INTRODUCTION Stable isotope geochemistry of biogenic carbonates, especially the bivalve shell, has become a key tool in paleoclimate and paleoenvironment reconstruction. The oxygen isotopic signatures of bivalve shell have been used to reconstruct both water temperature and salinity. The interpretation of stable carbon isotopic composition of shell (δ13Cs) remains contentious (Gillikin et al., 2007; Dettman et al., 1999).

作者: Yan Hui Wu Guoxi Li Zhongxuan Dong Dongping Zheng Jinggang

作者单位: College of Urban Planning and Environment Science, Xuchang University, Xuchang 461000, China State K College of Urban Planning and Environment Science, Xuchang University, Xuchang 461000, China

会议类型: 国际会议

会议名称: The International Conference of Geobiology(地球生物学国际研讨会)

会议地点: 武汉

会议语种:英文

页码: 271-273

在线出版日期: 2010-06-03（万方平台首次上网日期，不代表论文的发表时间）