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Variation of stalagmite growth rate and its paleoclimatic significance in Sanbao cave, Hubei Province over the past 640,000 years

In the past few decades, great progress has been made in the study of stalagmite paleoclimate. Compared with the geochemical indicators such as stalagmite δ18O, the average growth rate of stalagmite is a physical indicator, which can directly reflect the wet and dry changes of the external climate,...

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Hlavní autoři: Ying JIANG, Wei WEI, Xiaoyi FENG, Han ZHANG, He ZHU, Jinguo DONG
Médium: Artigo
Jazyk:Inglês
Vydáno: Institute of Karst Geology,Chinese Academy of Geological Science 2023-06-01
Edice:Carsologica Sinica
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On-line přístup:http://zgyr.karst.ac.cn/article/doi/10.11932/karst2021y31?pageType=en
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