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黄土高原现代表层黄土植物残体稳定同位素组成特征
引用本文:魏明建,董军让.黄土高原现代表层黄土植物残体稳定同位素组成特征[J].现代地质,1998,12(4):582-585.
作者姓名:魏明建  董军让
作者单位:中国科学院古脊椎与古人类研究所,国土资源部水文地质工程地质研究所
基金项目:国土资源部重点基础项目,国土资源部环境地质开放研究实验室联合资助课题
摘    要:在黄土高原选择了12个现代黄土堆积的典型地点,采集表层及5cm深度处的黄土样品,提取植物残体作稳定同位素分析。发现:(1)不同深度样品的植物残体δ13C值差异明显,可形成高分辨率的时间序列;(2)植物残体的δ13C值与气温的对应关系具有分区的特征,子午岭以西的黄土地区为负相关,其余地区比较复杂;(3)植物残体的δ13C值与降水的关系不密切。

关 键 词:黄土高原  植物残体  同位素  气候指标

ISOTOPE COMPOSITION CHARACTERISTICS OF VEGETATION RESIDUES IN MODERN LOESS DEPOSITION ON THE LOESS PLATEAU IN CHINA
Wei Mingjian,\ \ Dong Junshe,\ \ Zhang Jing,\ \ Zhang Junpai.ISOTOPE COMPOSITION CHARACTERISTICS OF VEGETATION RESIDUES IN MODERN LOESS DEPOSITION ON THE LOESS PLATEAU IN CHINA[J].Geoscience——Journal of Graduate School,China University of Geosciences,1998,12(4):582-585.
Authors:Wei Mingjian  \ \ Dong Junshe  \ \ Zhang Jing  \ \ Zhang Junpai
Institution:Wei Mingjian 1) \ \ Dong Junshe 2) \ \ Zhang Jing 3) \ \ Zhang Junpai 3)
Abstract:Authors chosen 12 typical sites of modern loess deposition in the Loess Plateau, taken samples at the surface and the 5cm depth from each site, and extract the vegetation residues for isotope analysis. The analysis result shows that: (1) the δ 13 C values of the samples from different depths vary obviously, it is very suitable for reconstructing the high resolution series; (2) the relationship between δ 13 C and the air temperature differs in different areas. In the west area to the Ziwuling Mountain it is reversed, in the other areas it is complex; (3) there is no definite relationship between δ 13 C and the annual precipitation.
Keywords:the Loess Plateau  vegetation residue  isotope composition  climate indicator  
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