收稿日期: 2019-02-28
修回日期: 2019-07-14
网络出版日期: 2019-10-11
基金资助
有机地球化学国家重点实验室开放基金项目“东海闽浙沿岸全新世古环境;古气候演变的生物标志物记录”(SKLOG-201621);中国博士后科学基金面上项目“东海近岸全新世有机质来源及环境变化的生物标志物记录”(2018M642622)
Advances in Glycerol Dialkyl Glycerol Tetraethers and Long-Chain Alkyl Diols in the Marine Sediments: Implications for Paleoclimatic and Paleoenvironmental Changes
Received date: 2019-02-28
Revised date: 2019-07-14
Online published: 2019-10-11
Supported by
the State Key Laboratory of Organic Geochemistry Open Fund “Biomarker records of the Holocene paleoenvironmental and paleoclimatic evolution along the Zhejiang-Fujian coast in the East China Sea”(SKLOG-201621);The China Postdoctoral Science Foundation Funded Project “Biomarker records from the East China Sea coast: Implications for organic matter sources and environmental changes in Holocene”(2018M642622)
海洋沉积物中星罗棋布的脂类生物标志物分布特征，确切地记录了母源生物新陈代谢和有机组分运移转化的大量信息，常被用来重建古气候—环境变化。对利用边缘海沉积物中丰富的中心脂甘油双烷基甘油四醚（core-GDGTs）和长链二醇指示晚第四纪古气候—环境变化的研究进展进行了综述。指出厘清海洋沉积物中埋藏脂类生物标志物的“源—汇”过程是进行古气候—环境重建的前提。认为利用受早期成岩作用影响较小的多项指标可以增加重建古气候变化结果的准确性。在受大河影响显著的边缘海，可以根据海洋沉积物中core-GDGTs和长链二醇指标重建的古气候记录阐明古气候—环境变化引起的海陆联动变化机制，以期为预测未来温度和降雨变化提供可靠的技术手段及坚实的理论基础。
陈立雷 , 李凤 , 刘健 . 海洋沉积物中GDGTs和长链二醇的古气候—环境指示意义研究进展[J]. 地球科学进展, 2019 , 34(8) : 855 -867 . DOI: 10.11867/j.issn.1001-8166.2019.08.0855
Lipid biomarkers widely dotted in marine sediments, as their distribution characteristics accurately record huge information on the metabolism of the original organisms and migration and transformation of these organic components, are often used to reconstruct the paleoclimatic and paleoenvironmental conditions. This paper reviewed the progress in the study of paleoclimatic-environmental changes during the late Quaternary using abundant core lipids Glycerol Dialkyl Glyceryl Tetraethers (GDGTs) and long-chain alkyl diols in marginal sea sediments. It is pointed out that clarifying the “source-sink” process of lipid biomarkers buried in marine sediments is a prerequisite for paleoclimatic-environmental reconstruction. It is believed that the use of multiple indicators that are less affected by early diagenesis can increase the accuracy of reconstructing paleoclimatic changes. In the large-river dominated marginal seas, the mechanism of land-sea climate coupling evolution stimulated by the paleoclimatic-environmental changes can be elucidated based on paleoclimatic records reconstructed from core lipids GDGTs and long-chain alkyl diols in marine sediments. It is hoped that this paper can provide reliable technical means and a solid theoretical basis for predicting future temperature and rainfall changes.
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