Abstract:<p>Speleothem fluid inclusions contain relics of past precipitation water, which constitute a powerful tool for studying the past hydrological cycle. Analyses of hydrogen and oxygen isotopes of the water stored in fluid inclusions allow the reconstruction of paleoclimate information such as temperature. A previous study has shown the potential of speleothems from Milandre Cave to address temperature-related issues such as the so-called &#8220;Holocene temperature conundrum&#8221;.… Show more
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