Inconsistency between records of δ18O and trace element ratios from stalagmites : evidence for increasing mid–late Holocene moisture in arid central Asia

• المؤلفون الرئيسيون: Liu, Xiaokang, Liu, Jianbao, Shen, Chuan-Chou, Yang, Yan, Chen, Jianhui, Chen, Shengqian, Wang, Xianfeng, Wu, Chung-Che, Chen, Fahu
• مؤلفون آخرون: Asian School of the Environment
• التنسيق: مقال
• اللغة: English
• منشور في: 2020
• الموضوعات: Science::Geology; Arid Central Asia; Holocene Moisture/Precipitation
• الوصول للمادة أونلاين: https://hdl.handle.net/10356/144998
• المؤسسة: Nanyang Technological University

The interpretation of trace element/calcium ratios of speleothems as indicators of local hydroclimatic variability in the vicinity of caves has led to controversy in reconstructing the evolution of moisture conditions in arid central Asia (ACA) during the Holocene. Here we present records of Mg/Ca,...