石笋碳酸盐假性热释光：古环境的新指标

廖金; 胡超涌; 李成展; 张格格; 高金荣; 黄俊华

doi:10.3799/dqkx.2014.042

Volume 39 Issue 4

Apr. 2014

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Article Navigation > Earth Science > 2014 > 39(4): 443-450

Liao Jin, Hu Chaoyong, Li Chengzhan, Zhang Gege, Gao Jinrong, Huang Junhua, 2014. Spurious Thermoluminescence from Stalagmite: A New Paleoenvironmental Proxy. Earth Science, 39(4): 443-450. doi: 10.3799/dqkx.2014.042

Citation:

Liao Jin, Hu Chaoyong, Li Chengzhan, Zhang Gege, Gao Jinrong, Huang Junhua, 2014. Spurious Thermoluminescence from Stalagmite: A New Paleoenvironmental Proxy. Earth Science, 39(4): 443-450. doi: 10.3799/dqkx.2014.042

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Spurious Thermoluminescence from Stalagmite: A New Paleoenvironmental Proxy

doi: 10.3799/dqkx.2014.042

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2013-07-14
Publish Date: 2014-04-15

Abstract

Abstract

Thermoluminescence from marine carbonate is found to be sensitively responding to the earth climate change of glacial-interglacial stage, which implies a novel proxy for paleoceanography. Yet it is to be confirmed by studies as to whether it is suitable for the terrestrial sediments. In this study, thermoluminescence and oxygen isotopic composition have been carried out on stalagmite CX-1 from Chuanxin cave, Qingjiang valley, Hubei Province, China, to determine the physical links between the climate and thermoluminescence intensity. It is found that thermoluminescence glow in air environment is mainly contributed by chemiluminescence derived from oxidation of the organic matter from stalagmite carbonates. Therefore, thermoluminescence is closely related to organic matter content of stalagmite derived from the degradation of organic matter in soil and the degradation rate is related to soil temperature controlled by the insolation. The variations of TL (total luminescence intensity) and δ¹⁸O show similar features which can reasonably be associated with climate change. Therefore, stalagmite thermoluminescence can act as a new proxy for terrestrial paleoenvironment.
- stalagmite,
- thermoluminescence,
- luminescent organic matter,
- oxygen isotope,
- solar insolation,
- climate change,
- sediments

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References(49)

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Spurious Thermoluminescence from Stalagmite: A New Paleoenvironmental Proxy

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