Regression of the Tethys Sea (central Asia) during middle to late Eocene: Evidence from calcareous nannofossils of western Tarim Basin, NW China

doi:10.1016/j.marmicro.2022.102085

IVPP-IR > 中科院古脊椎所（2000年以后）

	Regression of the Tethys Sea (central Asia) during middle to late Eocene: Evidence from calcareous nannofossils of western Tarim Basin, NW China
	Wang, Xuejiao 1; Xi, Dangpeng 1,2; Watkins, David K.3; Self-Trail, Jean M.4; Tang, Zihua 5; Cao, Wenxin 6; Jiang, Tian 1,7; Kamran, Muhammad 1; Wan, Xiaoqiao 1
	2022-03-01
发表期刊	MARINE MICROPALEONTOLOGY
ISSN	0377-8398
卷号	171 页码:13
通讯作者	Xi, Dangpeng(xdp1121@163.com)
摘要	Calcareous nannofossil assemblages from middle to upper Eocene sediments of the western Tarim Basin indicate two important episodes of marine incursion into the basin. The first episode represents a period of shallowing upward in the Wulagen Formation, which is dated as Zone CNE13 (Lutetian) by the co-occurrence of Discoaster bifax, Chiasmolithus solitus, and common Reticulofenestra umbilicus. The presence of a diverse assemblage of discoasters in the basal Wulagen suggests deposition occurred in oligotrophic, warm water with a connection to the open ocean. Progressive shallowing over time led to the formation of a restricted basin in which only Coccolithus pelagicus could survive. The second major episode of marine incursion is preserved in the middle part of the Bashibulake Formation, which is dated as Zone CNE17 (Bartonian/Priabonian) based on the presence of common Cribrocentrum erbae. The interval between the two marine incursions was dominated by subaerial exposure and evaporation, resulting in the deposition of gypsum at the top of the Wulagen Formation. Although maximum regression at the end of the Lutetian is followed by sea-level rise at the beginning of the Bartonian globally, it is clear that local tectonics played a crucial role in regional marine incursions into the Tarim Basin during deposition of the Wulagen Formation.
关键词	Tarim Basin Tethys Eocene Nannofossils Regression Paleoenvironment
DOI	10.1016/j.marmicro.2022.102085
关键词[WOS]	KERGUELEN PLATEAU ; EVOLUTION ; RETREAT
收录类别	SCI
语种	英语
资助项目	National Natural Science Foundation of China[41790452] ; National Natural Science Foundation of China[41872009] ; National Natural Science Foundation of China[41688103] ; National Key R&D Program of China[2019YFC0605403] ; Fundamental Research Funds for the Central Universities[2652018134] ; State Key Laboratory of Palaeobiology and Stratigraphy[163115] ; Chinese `111' project[B20011] ; Chinese `111' project[IGCP 679]
项目资助者	National Natural Science Foundation of China ; National Key R&D Program of China ; Fundamental Research Funds for the Central Universities ; State Key Laboratory of Palaeobiology and Stratigraphy ; Chinese `111' project
WOS研究方向	Paleontology
WOS类目	Paleontology
WOS记录号	WOS:000776071400002
出版者	ELSEVIER
引用统计	被引频次：7[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/21418
专题	中科院古脊椎所（2000年以后）
通讯作者	Xi, Dangpeng
作者单位	1.China Univ Geosci, State Key Lab Biogeol & Environm Geol, Xueyuan Rd 29, Beijing 100083, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaentol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China 3.Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE 68588 USA 4.US Geol Survey, Natl Ctr 926a, Florence Bascom Geosci Ctr, Reston, VA 20192 USA 5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China 6.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 7.China Univ Geosci, Sch Ocean Sci, Xueyuan Rd 29, Beijing 100083, Peoples R China
推荐引用方式 GB/T 7714	Wang, Xuejiao,Xi, Dangpeng,Watkins, David K.,et al. Regression of the Tethys Sea (central Asia) during middle to late Eocene: Evidence from calcareous nannofossils of western Tarim Basin, NW China[J]. MARINE MICROPALEONTOLOGY,2022,171:13.
APA	Wang, Xuejiao.,Xi, Dangpeng.,Watkins, David K..,Self-Trail, Jean M..,Tang, Zihua.,...&Wan, Xiaoqiao.(2022).Regression of the Tethys Sea (central Asia) during middle to late Eocene: Evidence from calcareous nannofossils of western Tarim Basin, NW China.MARINE MICROPALEONTOLOGY,171,13.
MLA	Wang, Xuejiao,et al."Regression of the Tethys Sea (central Asia) during middle to late Eocene: Evidence from calcareous nannofossils of western Tarim Basin, NW China".MARINE MICROPALEONTOLOGY 171(2022):13.