Depositional environments for stratiform witherite deposits in the Lower Cambrian black shale sequence of the Yangtze Platform, southern Qinling region, SW China: Evidence from redox-sensitive trace element geochemistry

• Published in: Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2014-03, Vol.398, p.125-131
• Main Authors: Pi, Dao-Hui, Jiang, Shao-Yong, Luo, Li, Yang, Jing-Hong, Ling, Hong-Fei
• Format: Article
• Language: English
• Subjects: China; Qinling; Redox condition; Redox-sensitive metals; Witherite deposits
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2013.09.029

A very large stratiform witherite mineralization occurs in Lower Cambrian black shales and siliceous rocks in the southern Qinling region of SW China. Two types of witherite ores are divided according to their colors, i.e., the white ores and the dark-gray ores. We analyzed a number of redox-sensitive trace elements in both the white and dark-gray ores from various witherite deposits. The redox-sensitive metal concentrations and the distribution of the two types of ores provide good evidence for their depositional redox conditions in the Early Cambrian ocean in the southern Qinling region. Our geochemical data suggest that both the dark-gray and white witherite ores may have been deposited in reducing environments, with the dark-gray ores deposited in an anoxic–euxinic environment, whereas the white ores deposited under a suboxic–anoxic condition. •Large witherite deposits occur in the Lower Cambrian strata in China.•Two types of witherite ores are recongnized.•Redox-sensitive trace elements in the witherite ores are studied.•The dark-gray witherite ores deposited in an anoxic–euxinic environment.