| 青藏高原北部新生代湖相碳酸盐岩碳氧同位素特征及古环境意义 |
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| 引用本文： | 伊海生,林金辉,周恳恳,李军鹏.青藏高原北部新生代湖相碳酸盐岩碳氧同位素特征及古环境意义[J].古地理学报,2007,9(3):303-312. |
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| 作者姓名： | 伊海生 林金辉 周恳恳 李军鹏 |
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| 作者单位： | 1.成都理工大学沉积地质研究院 四川成都610059;2.成都理工大学材料与化学化工学院 四川成都610059 |
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| 基金项目： | 国家自然科学基金
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高等学校博士学科点专项科研项目 |
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| 摘 要： | 对青藏高原北部地区新生代陆相地层中湖相碳酸盐岩进行了系统采样分析，以碳氧同位素作为古环境和古气候变化的替代指标,试图从古湖泊演化的角度，阐明高原新生代早期环境演变历史和过程。研究结果表明，该区所有分析样品中生物碎屑灰岩类样品的δ18O和δ13C显示最低值，反映它们沉积在一个水体滞留时间短的开放性淡水湖泊系统中。泥晶灰岩类样品的δ18O和δ13C之间具有正相关关系，表明它们发育在蒸发作用明显的封闭性咸水湖泊体系中，而叠层石灰岩类明显富集13C可能与微生物活动有关。从始新世到渐新世至中新世，湖相碳酸盐岩δ18O值具有逐渐增大的趋势，δ13C则由古近纪的负值变为新近纪的正值，反映该区古湖泊系统经历了一个由开放到封闭的过程，预示古近纪到新近纪之交高原古气候格局发生了重大变革。
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| 关 键 词： | 青藏高原 新生代 碳氧同位素 湖相碳酸盐岩 古气候 古环境 |
| 文章编号： | 1671-1505（2007）03-0303-10 |
| 修稿时间： | 2006-07-282006-11-20 |
Carbon and oxygen isotope characteristics and palaeoenvironmental implication of the Cenozoic lacustrine carbonate rocks in northern Qinghai-Tibetan Plateau |
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| Yi Haisheng,Lin Jinhui,Zhou Kenken,Li Junpeng.Carbon and oxygen isotope characteristics and palaeoenvironmental implication of the Cenozoic lacustrine carbonate rocks in northern Qinghai-Tibetan Plateau[J].Journal of Palaeogeography,2007,9(3):303-312. |
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| Authors: | Yi Haisheng Lin Jinhui Zhou Kenken Li Junpeng |
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| Institution: | 1.Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu610059,Sichuan;2.College of Materials and Chemistry Chemical Engineering, Chengdu University of Technology, Chengdu610059,Sichuan |
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| Abstract: | Through systematic sampling and analyses of the lacustrine carbonate rocks in the Cenozoic continental strata in the northern Qinghai Tibetan Plateau, by using the carbon and oxygen isotopes as proxies, the environmental evolution of the Early Cenozoic is revealed according to the palaeo lacustrine evolu￣tion. The results indicate that the δ18O and δ13C in the bioclastic limestone samples have the lowest values in all the samples in this area, reflecting that they were deposited in an open freshwater lacustrine environment with a short period of water residence. There is a positive relation between the δ18O and δ13C in the micritic limestone samples, reflecting that they were deposited in an obvious closed saline water laustrine environment. The obviously enriching of δ13C in stromatolitic limestones may be related to the microbial activities. The δ18O value of the lacustrine carbonate rocks gradually increased from Eocene to Oligocene and then to Miocene. The δ13C changed from a negative value in the Paleogene to a positive value in the Neogene, which reflects that the lacustrine system in this area evolved from an open system to a closed one. Thus the prediction can be made that the palaeoclimate changed greatly throughout the Paleogene Neogene period. |
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| Keywords: | Qinghai-Tibetan Plateau Cenozoic carbon and oxygen isotopes lacustrine carbonate rocks palaeoclimate palaeoenvironment |
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