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引用本文:王秋良,李长安,谢远云.江汉平原江陵地区9ka以来古气候演化的沉积记录.湖泊科学,2006,18(3):280-284. DOI:10.18307/2006.0314
WANG Qiuliang,LI Changan,XIE Yuanyun.Sedimentory records of paleoclimatic evolution in Jiangling, Jianghan Plain in the past 9ka. J. Lake Sci.2006,18(3):280-284. DOI:10.18307/2006.0314
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江汉平原江陵地区9ka以来古气候演化的沉积记录
王秋良1, 李长安1, 谢远云2
1.中国地质大学地球科学学院, 武汉 430074;2.哈尔滨师范大学地理系, 哈尔滨 150080
摘要:
对江汉平原江陵剖面沉积物中的总有机碳(TOC)、总氮(TN)、有机碳同位素δ13C值和粒度参数的分布特征与环境气候的关系进行了研究.结果表明:沉积物中有机碳、总氮较高,有机质的δ13C值偏负,沉积物的平均粒径较粗时,气候温暖湿润;反之,沉积物中有机碳、总氮较低,有机质的δ13C值偏正,沉积物的平均粒径较细时,气候温凉偏干.结合14C测年,判别江汉平原江陵地区的古气候演化过程:8900-6070aBP,为温湿时期;6000-4600aBP为相对冷干时期;4600-2500aBP为温暖湿润时期;2500aBP以来为温凉偏干时期.
关键词:  有机碳  有机碳同位素  粒度  古气候  江汉平原
DOI:10.18307/2006.0314
分类号:
基金项目:国家自然科学基金(40172061);国家重大基础研究项目(2003CB41520)联合资助
Sedimentory records of paleoclimatic evolution in Jiangling, Jianghan Plain in the past 9ka
WANG Qiuliang1, LI Changan1, XIE Yuanyun2
1.Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, P. R. China;2.Geography Department, Harbin Normal University, Harbin 150080, P. R. China
Abstract:
We analyzed the characteristics of organic matter TOC, TN and δ13 C value and sand sediment grain size from samples of Jianghan Plain and discussed its relationship with climatic circumstance. The results show that: the TOC and TN of the organic materials in sediments are higher, but the δ13 C are lower and grain sizes are coarser during warmer and wetter climatic episodes, On the other hand, during colder and dryer climatic episodes, the TOC and TN contents in sediments are lower. The δ13 C are lower and grain sizes are finer. With the results we reconstructed the evolution sequence of paleoclimate in Jianghan Plain region since 9000 aBP. It has four stages as follows: 8900-6070 aBP, warm and wet; 6070-4600 aBP, cold and dry; 4600-2500 aBP, warm and wet; 2500-500 aBP, cool and dry.
Key words:  Organic carbon  organic carbon isotope  grain size  paleoclimate  Jianghan Plain
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