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重庆芙蓉洞洞穴沉积物δ^13C、δ^18O特征及意义

ISSN号：0371-5736
期刊名称：《地质论评》
时间：0
分类：P588.2[天文地球—岩石学;天文地球—地质学] P532[天文地球—古生物学与地层学;天文地球—地质学]
作者机构：[1]西南大学地理科学学院,重庆400715, [2]成功大学地球科学系,台湾台南70101, [3]国土资源部岩溶动力学重点实验室,广西桂林541004, [4]台湾大学地质科学系,台北106, [5]武隆县风景名胜区管理局,重庆408500
相关基金：本文为国家自然科学基金资助项目（编号40672165,40672202）和重庆市科委院士专项（编号2003-7835）以及西南大学博士基金资助项目（编号SWUB2007030）的研究成果.致谢：感谢中国重庆市武隆县风景名胜区管理局、芙蓉洞景区管理处、武隆县气象局等单位对笔者等在芙蓉洞长期观测研究的大力支持.感谢汪永进教授、胡超涌教授、刘再华研究员、张平中教授、张美良研究员、覃嘉铭研究员等在2007年11月“全国岩溶科技创新大会”学术交流中对本文提出的许多宝贵意见.同时对审稿专家对本文提出的修改意见表示衷心感谢.

作者：李廷勇[1], 李红春[1,2], 李俊云[1], 袁道先[1,3], 王建力[1], 叶明阳[1], 唐亮亮[1], 沈川洲[4], 叶成礼[5]

关键词：重庆芙蓉洞, 洞穴沉积物, 氧碳稳定同位素, 平衡分馏, Furong cave, speleothems, oxygen and carbon stable isotopes, equilibrium Iractionation

中文摘要：

利用重庆芙蓉洞内各种新老沉积物的δ^13C、δ^18O以及对洞穴内的滴水、池水和洞外泉水的长期观测结果，发现芙蓉洞内的次生沉积物中氧同位素变化整体一致，处于稳定温度下（16℃）的平衡分馏状态。而且洞内滴水和池水的氧同位素也相当一致，反映了外界大气降水中氧同位素的年平均状态。芙蓉洞内各种沉积物中碳同位素变化范围很大，从0‰～-11‰均有分布。由于芙蓉洞内各种滴水以及池水中溶解无机碳（DIC）的δ^13C变化约在-8‰-11‰，显著偏轻于部分洞穴沉积物中的δ^13。通过研究从洞穴滴水到形成次生化学沉积物这个过程中的可能影响洞穴沉积物中碳同位索变化的因素，例如：洞穴温度、滴水高度和速率、CO2脱气、生物作用、矿物同质异相转换等，同时参考芙蓉洞内连续生长达37ka的FR5石笋的碳同位素记录，发现以上可能的影响因素都不能完全解释芙蓉洞内次生沉积物中碳同位素的异常偏重现象。虽然芙蓉洞内广泛存在文石与方解石共存的次生沉积物，但是综合分析表明这些沉积物的氧同位素处于平衡分馏状态，可以用来进行古气候研究。不过在利用石笋碳同位素解释古环境变化时需要慎重，特别是在讨论由文石或文石一方解石混合构成的次生沉积物时。

英文摘要：

We have monitored δ^18O and dissolved inorganic carbon （DIC） δ^13C values of dripwater of Furong Cave, Chongqing, between from Oct. , 2005, to June, 2007. We also measured δ^18O and δ^13C for other cavewaters, surface waters, and carbonate deposits collected from the cave and surrounding area. The data results show that stalagmites in this cave were deposited in oxygen isotopic equilibrium with its parent solution under relatively constant cave temperatures. The δ^18O values of drip waters from different seasons are relatively constant, and the newly deposited carbonates from different sites in the cave are nearly consistent. This means that the drip δ^18O and stalagmite δ^18O reflect the oxygen isotopic composition of weighted annual mean δ^18O of the local rainfall. The δ^13C of these newly deposited carbonates varies from 0‰- 11‰, whereas the DIC δ^13C in drip and pool water varies from -8‰-11‰. In addition, many stalagmite samples from this cave show strongly enriched δ^13C values, being much heavier than the δ^13C value of drip waters. The authors focus on the influencing factors on the δ^13C of speleothems by discussing all possible variables, such as cave temperature, dripping rate and height, degassing of CO2, evaporation, biological activity, and polymorphic transformation of aragonite and calcite. However, none of the fore-mentioned factors could explain the anomaly heavy δ^13C of speleothems in Furong Cave. Although it is common that speleothem in Furong Cave contains both aragonite and calcite in different proportions, these speleothems are still in equilibrium fractionation for oxygen isotopes and can be used for reconstruction of paleoclimate. It should be cautious to use the δ^13C as a proxy to interpretation the evolution of paleoenvironment before we clearly understand the controlling factors of δ^13C in a karst dynamic system, especially when speleothems contain aragonite.

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