Stalagmite-inferred European westerly drift with centennial-scale variability in marine isotope stage 5a

Yun-Chuan Chung1,2, Laurie Menviel3, Arianna Marchionne4, Horng-Sheng Mii5, Véronique Michel6, Patricia Valensi7, Xiuyang Jiang8, Patrick Simon9, Elena Rossoni-Notter9, Abdelkader Moussous9, Heikki Seppä10, Yu-Tang Chien11, Chung-Che Wu12, Hsun-Ming Hu13 and Chuan-Chou Shen14, (1)National Taiwan University, High‐precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Research Center for Future Earth, Taipei, Taiwan, (2)University of Helsinki, Department of Geosciences and Geography, Helsinki, Finland, (3)University of New South Wales, Climate Change Research Centre, Sydney, NSW, Australia, (4)University of Helsinki, Department of Mathematics and Statistics, Helsinki, Finland, (5)National Taiwan Normal Univ., Taipei, Taiwan, (6)Université Côte d’Azur, CNRS, CEPAM, Nice, France, (7)Département de Préhistoire, MNHN Paris, CNRS, 75013, Paris, France; Musée de Préhistoire, 06690 Tourrette-Levens, France, Paris, France, (8)Fujian Normal University, Fuzhou, China, (9)Musée d’Anthropologie préhistorique de Monaco, Monaco, Monaco, (10)University of Helsinki, Helsinki, Finland, (11)National Science and Technology Center for Disaster Reduction, New Taipei City, Taiwan, (12)ETH Zurich, Department of Chemistry and Applied Biosciences, Zurich, Switzerland, (13)National Taiwan University, High‐precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geoscience, Taipei, Taiwan, (14)High‐precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, Taipei, Taiwan
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