The effect of cave ventilation on carbon and oxygen isotopic fractionation between calcite and drip water-Reference-Cited by-同舟云学术

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The effect of cave ventilation on carbon and oxygen isotopic fractionation between calcite and drip water

Published:2024-03 Issue: Volume:915 Page:169967
ISSN:0048-9697
Container-title:Science of The Total Environment
language:en
Short-container-title:Science of The Total Environment

Author:

Lyu Yina,Luo Weijun,Zeng Guangneng,Wang Yanwei,Chen Jia,Wang Shijie

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

China Postdoctoral Science Foundation

Guizhou Province Science and Technology Foundation

Science and Technology Program of Guizhou Province

Publisher

Elsevier BV

Reference92 articles.

1. Kinetic isotope effect in CO2 degassing: insight from clumped and oxygen isotopes in laboratory precipitation experiments;Affek;Geochim. Cosmochim. Acta,2014

2. Northwest European palaeoclimate as indicated by growth frequency variations of secondary calcite deposits;Baker;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1993

3. Very high-frequency and seasonal cave atmosphere PCO2 variability: implications for stalagmite growth and oxygen isotope-based paleoclimate records;Baldini;Earth Planet. Sci. Lett.,2008

4. Seasonal variations in modern speleothem calcite growth in Central Texas, U.S.A;Banner;J. Sediment. Res.,2007

5. Experimental definition of microclimatic conditions based on water transfer and porous media properties for the conservation of prehistoric constructions: Cueva Pintada at Galdar, Gran Canaria, Spain;Benavente;Environ. Geol.,2009

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