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Abstract: Manganese-rich calcite layers in a western Scotland speleothem record storm-driven hydroclimatic changes during the Little Ice Age (AGU25)

Manganese-rich calcite layers in a western Scotland speleothem record storm-driven hydroclimatic changes during the Little Ice Age

Kang Xie1, Martin R. Lee1, Cristina Persano1, John Faithfull2, Haiwei Zhang3, Hai Cheng3 and Dominik Fleitmann4, (1)School of Geographical and Earth Sciences,University of Glasgow, Glasgow, United Kingdom, (2)The Hunterian Museum, University of Glagsow, Glasgow, United Kingdom, (3)Institute of Global Environmental Change,Xi’an Jiaotong University, Xi'an, China, (4)Department of Environmental Sciences, University of Basel, Basel, Switzerland
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