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植物硅酸体研究及其在第四纪地质学中的应用

  • 刘显凡 ,
  • 阳正熙 ,
  • 李佑国 ,
  • 刘家铎 ,
  • 吴德超 ,
  • 张成江
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  • 中国科学院兰州地质研究所 兰州 730000
吉利明,男,1963年1月出生,助理研究员,主要从事微体古生物学和有机地球化学研究。

收稿日期: 1996-04-19

  修回日期: 1996-06-07

  网络出版日期: 1997-02-01

基金资助

气体地球化学国家重点实验室基金资助项目

STUDY OF PHYTOLITH AND ITS APPLICATION TO QUATERNARY GEOLOGY

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  • Lanzhou Institute of Geology,Chinese Academy of Sciences,Lanzhou 730000

Received date: 1996-04-19

  Revised date: 1996-06-07

  Online published: 1997-02-01

摘要

第三系及其以上地层中广泛存在着大量由陆生高等植物所产生的植物硅酸体。由于源自不同植物的硅酸体具有不同的形态类型组合,因此沉积物中硅酸体组合的研究,不仅可以划分对比地层,而且可通过古植被恢复来探讨古生态环境,这方面的作用在第四纪地质研究中已得到成功的应用。此外,硅酸体内赋存的有机
碳的同位素研究可以使地质时代和古气候研究达到定量或半定量化。

本文引用格式

刘显凡 , 阳正熙 , 李佑国 , 刘家铎 , 吴德超 , 张成江 . 植物硅酸体研究及其在第四纪地质学中的应用[J]. 地球科学进展, 1997 , 12(1) : 51 -57 . DOI: 10.11867/j.issn.1001-8166.1997.01.0051

Abstract

There are plenty of phytoliths came from higher plants in the sediments of Tertiary and Quaternary. Because the phytoliths sourced from different plants with different morphologic assemblages, not only the strata can be divided and correlated but also the paleo-climates can be restored with the recoveries of paleobotanic communities by the analyses of stratigraphic phytoliths. In the way, a lot of works have been done in the research of Quaternary geology. In addition, the studies of isotope geochemistry of organic carbon in phytoliths can make the dissections of geologicages and paleoclimates quantitative.

参考文献

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