Late Cretaceous ostracod fauna from the Shenjiatun section (Songliao Basin, Northeast China): Biostratigraphic and palaeoecological implications

被引:17
作者
Wang, Yaqiong [1 ]
Sames, Benjamin [2 ,5 ]
Liao, Huanyu [3 ,4 ]
Xi, Dangpeng [6 ]
Pan, Yanhong [1 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, CAS Key Lab Econ Stratig & Palaeogeog, 39 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China
[2] Univ Vienna, Dept Geodynam & Sedimentol, Geozentrum, Althanstr 14, A-1090 Vienna, Austria
[3] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, 39 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[5] SNOMNH, 2401 Chautauqua Ave, Norman, OK 73072 USA
[6] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Xueyuanlu 29, Beijing 100083, Peoples R China
基金
奥地利科学基金会;
关键词
Campanian; Nenjiang formation; Ostracoda; Palaeoenvironment; Taxonomy; Palaeobiology; THERIOSYNOECUM BRANSON 1936; TAXONOMY; AMERICA; SOUTH; CONSTRAINTS; EVOLUTION; SEQUENCES; CRUSTACEA; GENERA; GENUS;
D O I
10.1016/j.cretres.2017.05.001
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This work provides the first detailed taxonomic study of ostracod species from the Shenjiatun section (Nenjiang Formation, Songliao Basin, northeast China). Ten species belonging to seven genera are recognized. At the species level, this ostracod fauna shows a high degree of endemicity. The ontogeny of two species is recognized in this study, and sexual dimorphism within Daqingella arca is unequivocally recognized for the first time. The ostracod fauna suggests that this fossil-bearing sedimentary succession should be assigned to members 3-4 (Campanian) of the Nenjiang Formation (mainly Member 3) instead of representing 'Quaternary sediments' as previously thought. On the basis of the ostracod fauna, Member 3 of the Nenjiang Formation at Shenjiatun represents a shallow-littoral, lacustrine depositional environment that, at least in the upper part of Member 3, potentially included less stable conditions characterized by smaller, ephemeral waterbodies and increased (non-marine, oligohaline) salinities through evaporation. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:174 / 190
页数:17
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