%0 Dataset
%T Reconstruction of Ocean Redox  Environment During the Late Permian Wuchiapingian, Northern Margin of Upper Yangtze
%J National Cryosphere Desert Data Center
%I National Cryosphere Desert Data Center(www.ncdc.ac.cn)
%U http://www.ncdc.ac.cn/portal/metadata/66d86954-2a48-490d-8401-378c2fa16c7b
%W NCDC
%R 10.12072/ncdc.geochem.db6688.2024
%A YONG runan
%A SUN shi 
%K In the Late Permian;Abnormal Ce;ocean hypoxia;biological recovery;Upper Yangtze
%X In order to clarify the relationship between shallow sea redox changes and biological recovery in the Late Permian, and to reveal the deep connection between oceanic hypoxia and contemporaneous climate tectonic events, a study was conducted on the Wujiaping period of the Shangsi section on the northern edge of the Yangtze River in the Late Permian. A total of 38 samples were collected, including 23 samples from the Wujiaping Formation and 15 samples from the lower part of the Dalong Formation. Divide all samples into two parts for (1) carbon oxygen isotope analysis and (2) analysis of major and trace elements in carbonate rocks.