Terrestrial hot-spring travertine: An important window into paleoclimate reconstruction
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摘要:
研究目的 陆地热泉钙华作为火山、地热区常见的陆相碳酸盐岩沉积物/岩被广泛用于恢复古环境，但其中可反映古气候信息的代用指标多受复杂外界条件变化控制，因此利用热泉钙华进行古气候信息提取有待深入研究。
研究方法 本文对当前热泉钙华在重建古气候信息方面的成功案例进行了总结，并梳理了与热泉钙华沉积相关的各类气候、非气候影响因素。
研究结果 研究认为针对热泉钙华进行古气候恢复代用指标的选取，目前较为可行的有C-O同位素、主微量元素，孢粉学数据由于孢粉保存的局限性，可作为佐证信息，配合其他气候代用指标来检验古气候意义的正确与否，同时需将热泉钙华中各项气候代用指标与生物地层学、冰芯、石笋等相对成熟的古气候研究手段进行对比，使各类古气候替代指标相互验证，从而更好的解读热泉钙华中古气候信息。
结论 利用热泉钙华中的各项气候代用指标进行可靠的古气候信息提取与恢复具有可行性。
Abstract:This paper is the result of hydrogeological and environmental geological survey engineering.
Objective Terrestrial hydrothermal spring travertine, as a common terrestrial carbonate sediment/rock in volcanic and geothermal areas, is widely used to restore paleoenvironment, but the proxy indicators that can reflect paleoclimate information are mostly controlled by complex external conditions. The extraction of paleoclimate information from hot spring travertine requires further research.
Methods This paper summarizes the current successful cases of hydrothermal travertine in reconstructing paleoclimate information, and sorts out various climatic and non- climatic influencing factors related to the deposition of hydrothermal travertine.
Results The authors believe that C- O isotopes, major and trace elements are more feasible for the selection of palaeoclimate restoration proxies for hydrothermal travertine. The palynological data can be used as corroborative information due to the limitation of sporopollen preservation, and can be used in conjunction with other climate proxies. indicators to test whether the palaeoclimate significance is correct or not. At the same time, it is necessary to compare various climatic proxies in thermal spring travertine with relatively mature paleoclimate research methods such as biostratigraphy, ice cores, stalagmites, etc., so that various paleoclimate proxies can be verified with each other, so as to better obtain the information on the medieval climate of the hot spring travertine.
Conclusion It is feasible to extract and restore reliable paleoclimate information by using various climatic proxies in hot spring travertine.
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图 1 土耳其西南部Denizli地区热泉钙华C和O同位素曲线（据Toker et al., 2015修改）
Figure 1.
图 2 西班牙Guadix-Baza盆地钙华上部地层δ18O与δ13C数据综合解释（据Prado-Pérez et al., 2013修改）
Figure 2.
图 3 西班牙Alicún de las Torres钙华碳氧同位素变化代表的气候场景与古气候意义（据Prado-Pérez et al., 2013修改）图中X轴和Y轴分别表示δ13C、δ18O值的古气候含义
Figure 3.
图 5 土耳其西南部Denizli地区花粉图与晚更新世和全新世阶段同位素曲线（据Toker et al., 2015修改）
Figure 5.
表 1 常用碳酸盐岩氧同位素恢复古温度方程
Table 1. common oxygen isotopic thermometers used in carbonate systems
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表 2 腾冲古钙华水温计算结果与现代热泉水温比较
Table 2. Comparison of the calculations of ancient travertine versus modern water temperatures in Tengchong
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朱大岗, 孟宪刚, 邵兆刚, 杨朝斌, 韩建恩, 余佳, 孟庆伟, 吕荣平. 2006. 西藏阿里札达盆地早更新世早期沉积及其古气候与古环境变化[J]. 中国地质, 33(6): 1276-1284. doi: 10.3969/j.issn.1000-3657.2006.06.010 http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20060610&flag=1
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