| 晚泥盆世弗拉斯期—法门期之交海水温度变化的同位素证据 |
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| 引用本文： | 王大锐,马学平,董爱正,朱德升.晚泥盆世弗拉斯期—法门期之交海水温度变化的同位素证据[J].地球学报,2001,22(2):141-144. |
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| 作者姓名： | 王大锐 马学平 董爱正 朱德升 |
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| 作者单位： | 中国石油天然气集团公司油气地球化学重点实验室，北京；中国石油勘探开发研究院，北京;北京大学地质学系;中国石油天然气集团公司油气地球化学重点实验室，北京；中国石油勘探开发研究院，北京;中国石油勘探开发研究院，北京 |
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| 摘 要： | 位于我国湖南省冷水江地区锡矿山矿区的老江冲剖面为发育良好的浅水台地相沉积，出露著名的上泥盆统弗拉斯-法门阶（Fr/Fa)界线，多年的地层古生物学工作已详细地了解了该区的古生物面貌，本研究采用了基不可一世保存完好的腕足动物Cyrospirifer uernemili壳体进行了稳定C、O同位素地球化学分析，δ^18O值为-8.4‰-9.6‰，δ^13C值为-2.2‰-0.5‰，二值在弗拉斯-法门阶交界处均发生了异常波动，将此值与其他地区的研究结果进行比较，可以认为，弗拉斯-法门期交界时所发生的剧烈而大范围的事件所造成的同位素波动可以作为大区域地层对比的标志，经过计算，推断从弗拉斯期末至法门期初，我国华南地区的古海洋发生了降温事件。
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| 关 键 词： | 晚泥盆世 弗拉斯—法门阶 稳定同位素组成 古气温 |
Isotopic Evidence for the Temperature Change of the Paleo-Ocean between Late Devonian Fransnian Period and Famennian Period in South China |
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| WANG Da-rui,MA Xue-ping,DONG Ai-zheng and ZHU De-sheng.Isotopic Evidence for the Temperature Change of the Paleo-Ocean between Late Devonian Fransnian Period and Famennian Period in South China[J].Acta Geoscientia Sinica,2001,22(2):141-144. |
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| Authors: | WANG Da-rui MA Xue-ping DONG Ai-zheng and ZHU De-sheng |
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| Institution: | Key Laboratory of Petroleum Geochemistry, China National Petroleum Corporation, Beijing; Research Institute of Petroleum Exploration and Development, Petro-China, Beijing;Department of Geology, Peking University;Key Laboratory of Petroleum Geochemistry, China National Petroleum Corporation, Beijing; Research Institute of Petroleum Exploration and Development, Petro-China, Beijing;Research Institute of Petroleum Exploration and Development, Petro-China, Beijing |
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| Abstract: | The shallow platform sedimentary facies is well-developed along the Laojiangchong section in Xikuangshan mine,Lengshuijiang area,Hunan Province,which includes the well-known Upper Devonian Fransian-Famennian(Fr/Fa) boundary.Long period of field studies and researches led the authors to reveal the palaeotnology as well as sedimentary associations and characteristics.The shells of brachiopod Cyrospirifer vernemili were analysed isotopically and by SEM in this study.The carbon and oxygen isotopic analyses (δ18O:-8.4‰～-9.6‰; δ13C: -2.2‰～0.5‰) show an abnormal shift around the boundary of Fr/Fa in South China,which can serve as a standard of regional tratigraphic correlation.Depending on the calculation of oxygen isotopes within the well preserved brachiopods,the authors drew the inference about temperature decreasing from late Fransian to early Famennian. |
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| Keywords: | Late Devonian Fransnian Famennian stage stable isotope composition paleotemperature |
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