Mon: 090
Topics: 03.05 Advances in Paleoclimate Proxies and Their Applications

Deciphering the stable isotope (δ18O, δ13C) record of Holocene oyster shells from the Yangtze River Delta, China

Matthias Alberti¹, Sandro F. Veiga^2,3, Bo Chen⁴, Liang Hu⁵, Zheng Fang⁶, Baochun Zhou⁷, Yanhong Pan⁶

1: Geologisches und Mineralogisches Museum, Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Germany; 2: School of Atmospheric Sciences and Key Laboratory of Mesoscale Severe Weather/Ministry of Education and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, China; 3: Nanjing-Helsinki Institute in Atmospheric and Earth System Sciences, Nanjing University, Suzhou, China; 4: State Key Laboratory of Palaeobiology and Stratigraphy and Center for Excellence in Life and Paleoenvironment, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China; 5: Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China; 6: State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Centre for Research and Education on Biological Evolution and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, China; 7: Shanghai Natural History Museum, Shanghai, China