投稿中心

审稿中心

编辑中心

期刊出版

网站地图

友情链接

引用本文:薛滨,王苏民,沈吉,羊向东,马燕.呼伦湖东露天矿剖面有机碳的总量及其稳定碳同位素和古环境演化.湖泊科学,1994,6(4):308-316. DOI:10.18307/1994.0403
Xue Bin,Wang Sumin,Shen Ji,Yang Xiangdong,Ma Yan.Total organic carbon and its stable carbon isotope and paleoenvironmental evolution of donglutian coal profile, Hulun Lake. J. Lake Sci.1994,6(4):308-316. DOI:10.18307/1994.0403
【打印本页】   【HTML】   【下载PDF全文】   查看/发表评论  【EndNote】   【RefMan】   【BibTex】
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 5015次   下载 2409 本文二维码信息
码上扫一扫!
分享到: 微信 更多
呼伦湖东露天矿剖面有机碳的总量及其稳定碳同位素和古环境演化
薛滨, 王苏民, 沈吉, 羊向东, 马燕
中国科学院南京地理与湖泊研究所, 南京210008
摘要:
湖泊沉积物中有机碳的总量(TOC)取决于湖泊的初始生产力及有机质沉积后的保存能力,而有机碳的稳定同位素(δ13C)值则反映了不同来源有机质的组成以及流域古植被状况。本文通过对内蒙呼伦湖东露天煤矿剖面TOC及δ13C值的垂直分布的研究,结合剖面的沉积特征及孢粉、硅藻分析结果,讨论了呼伦湖地区末次冰期以来古气候古环境演化过程。结果表明有机碳的总量及其稳定碳同位素可作为分析古气候环境的一种有效的代用指标。
关键词:  湖泊沉积物  有机碳总量  有机碳稳定同位素  古环境演化  呼伦湖
DOI:10.18307/1994.0403
分类号:
基金项目:国家自然科学基金项目(49172119)
Total organic carbon and its stable carbon isotope and paleoenvironmental evolution of donglutian coal profile, Hulun Lake
Xue Bin, Wang Sumin, Shen Ji, Yang Xiangdong, Ma Yan
Nanjing Institute of Geography and Linndology, Chinese Academy of Sciences, Nanjing210008
Abstract:
Total organic carbon (TOC) in lake sediments depends on the input of organic matter, the primary production of lake itself and its preservation potency while the stable isotope value (δ13C) of organic carbon reflects the combination of different sources of organic matter and the paleovegetation in the drainage area-According to the vertical distribution of TOC and δ13C, combined with the sedimentary characteristics, sporo-pollen and diatom from Dongiutian coalfild of Hulun Lake, Inner Mongolia, the paleoenvironmental evolution of this region since last Glaciation has been reconstructed as follows: the lake pioneering period of LGM or a bit later, cold and dry;the highest lake level period of the second half of Post Glacial (13000-10900 a B.P.), temperate and wet;Younger Dryas Period(10900-10600a B.P.), cold and dry;the higher lake level period at the beginning of Holocene (10600-10000a B.P.), temperate and wet;the in ter mediate-low lake level in the Early Holocene (10000-7200a B.P.), temperate and dry;the higher lake level of Middle Holocene (7200-5000a B.P.), warm and wet;the strong shrinkage period in the late Middle Holocene (5000-3000a B.P.), temperate and dry.
Key words:  Lake sediments  total organic carbon  stable isotope of oranic carbon  paleoenvironmental evolution  Hulun Lake
分享按钮