Biostratigraphic and palaeoenvironmental significance of Campanian-early Maastrichtian (Late Cretaceous) ostracods from the Jiaozhou Formation of Zhucheng, Shandong, China. (January 2019)

• Record Type: Journal Article
• Authors: Wang, He; Li, Sha; Zhang, Haichun; Cao, Meizhen; Horne, David J.
• Is Part Of: Cretaceous research. Volume 93(2019)
• Page Start: 4
• Page End: 21
• Publication Date: 2019-01
• Subjects: Jiaolai Basin -- China -- Jiaozhou Formation -- Campanian–Maastrichtian -- Ostracods -- Biostratigraphy -- Palaeoenvironment; Geology, Stratigraphic -- Cretaceous -- Periodicals; 551.77
• DOI: 10.1016/j.cretres.2018.08.023
• Languages: English
• ISSNs: 0195-6671

Abstract

Abstract: Cretaceous strata are well developed in the Jiaolai Basin (Jiaodong Peninsula, East China) and contain abundant fossils including hadrosaurids, tyrannosauroids, various types of dinosaur eggs, bivalves, gastropods, ostracods, clam shrimps, insects and plants. During a geological investigation in Zhucheng City, eastern Shandong Province, East China, a new exposure of part of the Jiaozhou Formation was discovered near Jiankou Village. This formation constitutes uppermost Cretaceous to earliest Paleogene strata (encompassing the K/Pg boundary) in the Jiaolai Basin. Samples from a new Jiankou section yielded abundant ostracods assigned to twelve genera and twenty-seven species, reported for the first time from the Jiaozhou Formation in this area. The assemblage is composed entirely of non-marine taxa, including species of Cypridea, Talicypridea and Candoniella . Ostracod biostratigraphy indicates this section to be Campanian to early Maastrichtian in age, but not including the K/Pg boundary commonly present in the upper part of the Jiaozhou Formation. Palaeoenvironmental analysis of the species composition of the assemblages obtained, combined with a study of valve ornamentation, suggests that during the late Campanian, an ephemeral pond or small ephemeral lake alternated with a permanent lake in the studied area, and during the Campanian to Maastrichtian interval, there was a seasonally expanding and shrinking lake with both permanent and ephemeral basins in the studied area.