Taxonomy, biostratigraphic and paleoecological aspects of non-marine ostracod fauna from the Jinju Formation (Albian) of the Gyeongsang Basin, South Korea

被引:8
|
作者
Choi, Byung-Do [1 ]
Jia, Baoyan [2 ,3 ,4 ]
Huh, Min [5 ,6 ]
Jung, Jongyun [5 ,6 ]
Wang, Yaqiong [2 ,3 ]
机构
[1] Daegu Natl Sci Museum, Dalseong Yuga Eup 43023, Daegu, South Korea
[2] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China
[3] Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, 39 East Beijing Rd, Nanjing 210008, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[5] Chonnam Natl Univ, Fac Earth Syst & Environm Sci, Gwangu 61186, South Korea
[6] Chonnam Natl Univ, Korea Dinosaur Res Ctr, Gwangu 61186, South Korea
基金
新加坡国家研究基金会; 美国国家科学基金会;
关键词
Taxonomy; Cypridoidea; Biostratigraphy; Paleoecology; Albian; CRETACEOUS SINDONG GROUP; GENUS CYPRIDEA BOSQUET; JIUFOTANG FORMATIONS; INNER-MONGOLIA; CHINA; YIXIAN; PALEOENVIRONMENT; STRATIGRAPHY; EVOLUTION; COAST;
D O I
10.1016/j.cretres.2021.104944
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A total of seven species belonging to six genera of cypridoidean ostracods were recovered from three sections (Jeongchon, Hotan, and Tapri) of the Albian Jinju Formation from the Gyeongsang Basin, South Korea: Scabriculocypris yanbianensis, Cypridea khandae sp. nov., Cypridea samesi, Mongolocypris kohi, Lycopterocypris? cf. celsa, Candona sp., and Djungarica sp. Based on its morphology, C. khandae sp. nov. is considered to be the first record of the Cypridea alta-group in Korea. Although many species are endemic to the Jinju Formation, the occurrence of Scabriculocypris yanbianensis indicates that this fauna was linked with the contemporaneous fauna of the Tongfosi Formation of the Yanji Basin, northeast China. Based on previous studies and newly collected specimens, the taphonomic features of the sections indicate the presence of two distinct thanatocoenoses: a low-energy autochthonous thanatocoenosis (Jeongchon and Tapri sections) and a slightly higher energy thanatocoenosis (Hotan section). Finally, the absence of cytheroidean and darwinuloidean ostracods could be explained by the presence of unstable lake/temporal waterbodies and their low competitiveness. (c) 2021 Elsevier Ltd. All rights reserved.
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页数:16
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