地球科学进展 ›› 2012, Vol. 27 ›› Issue (3): 276 -283. doi: 10.11867/j.issn.1001-8166.2012.03.0276

综述与评述 上一篇    下一篇

生物标志物稳定氢同位素研究进展及在海洋古环境重建中的应用
袁子能 1,2,邢磊 1,2*,张海龙 1,2,赵美训 1,2   
  1. 1.中国海洋大学海洋化学理论与工程技术教育部重点实验室,山东青岛266100;2.中国海洋大学海洋有机地球化学研究所,山东青岛266100
  • 收稿日期:2011-11-30 修回日期:2012-01-19 出版日期:2012-03-10
  • 通讯作者: 邢磊(1975-),男,山东烟台人,副教授,主要从事海洋有机地球化学研究. E-mail:xinglei@ouc.edu.cn
  • 基金资助:

    国家重点基础研究发展计划项目“我国陆架海生态环境演变过程、机制及未来变化趋势预测”(编号:2010CB428901);国家自然科学基金重大国际合作研究项目“人类活动和气候变化对我国边缘海有机碳汇影响的有机分子记录”(编号:41020164005);中国海洋大学实验室研究基金项目“海洋沉积物中单体类脂生物标志物(Alkenones)氢稳定同位素(δD)测定”(编号:201151017)资助.

Progress of Biomarker Stable Hydrogen Isotope  and Its Application to Marine Paleoenvironmental Reconstruction

Yuan Zineng 1,2,Xing Lei 1,2,Zhang Hailong 1,2,Zhao Meixun 1,2   

  1. 1.Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao266100, China; 2. Institute of Marine Organic Geochemistry, Ocean University of China, Qingdao266100, China
  • Received:2011-11-30 Revised:2012-01-19 Online:2012-03-10 Published:2012-03-10

生物标志物稳定氢同位素是一种比较新的古环境指标,越来越多的研究者利用生物标志物稳定氢同位素重建了陆地和海洋中古水循环的变化。在陆地上,生物标志物δD值可以用来重建降雨δD值、古海拔以及蒸散作用大小或者湖泊水的输入输出平衡。在海洋中,生物标志物δD值的变化能更好地反映与其相关的生物和环境信息。培养实验以及现场数据显示生物标志物δD值能很好地反映表层海水δD值以及表层海水盐度的变化。许多研究者也利用海洋中生物标志物δD值重建了长时间尺度降雨量以及表层海水盐度的变化。对近年来生物标志物稳定氢同位素的研究进展,尤其是在海洋古环境重建中的应用进行了总结。

As a new proxy, biomarker stable hydrogen isotope is  increasingly used to reconstruct hydrological cycles in the continents and ocean. In terrestrial environments, δD value of biomarkers can be used to reconstruct the δD value  in rainfall, ancient altitude and evapotranspiration or lake water balance. In marine environments, changes of δD value of biomarkers can be interpreted more clearly in the context of relevant biological and environmental information. Many culture experiments and field data indicate that δD value of biomarkers can reflect δD value of surface water, and changes of seawater salinity. Many researchers also use δD value  of marine biomarkers as a tool to reconstruct long term amounts of precipitation and surface seawater salinity. In this paper, the progress of biomarker stable hydrogen isotope of biomarkers and its  application to marine paleoenviromental reconstruction are summarized.

中图分类号: 

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