Uppermost Devonian-Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area, South Mongolia

doi:10.1016/j.palwor.2022.10.004

	Uppermost Devonian-Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area, South Mongolia
	Byambajav, Uugantsetseg 1,2,3; Qie, Wen-Kun 1; Yarinpil, Ariunchimeg 3; Batkhuyag, Enkhdalai 4; Choindonjamts, Erdenejargal 4,5; Puntsag, Delgerzaya 3
刊名	PALAEOWORLD
	2023-09-01
卷号	32 期号:3 页码:411-428
关键词	Biostratigraphy Conodont Devonian-Carboniferous boundary Shombon Member
ISSN号	1871-174X
DOI	10.1016/j.palwor.2022.10.004
通讯作者	Qie, Wen-Kun(wkqie@nigpas.ac.cn)
英文摘要	In southwestern Mongolia, conodonts from the Indert Formation at its type locality in Shine Jinst were investigated to improve regional and global correlation of the uppermost Devonian-lowermost Carboniferous. The abundance and diversity of the conodont fauna is quite low in general, whereas representatives of Siphonodella, Protognathodus, Pseudopolygnathus, Polygnathus and Bispathodus have been collected from the Indert-Uul section. Five conodont biointervals, from the Bi. costatus-Pr. kockeli Interregnum (ckI) to the Siphonodella sandbergi Zone, could be recognized from the top Heermorit Member and the lower part of the Shombon Member, while the middle and upper parts of the Shombon Member cannot be zoned based on the conodonts. Absence of index fossils Si. sulcata, Pr. kuehni and Pr. kockeli hampered precise recognition of the Devonian-Carboniferous boundary (DCB) at Indert-Uul, but this transition is well delineated by typical uppermost Famennian and Tournaisian conodont assemblages. The DCB is tentatively placed at the base of the Shombon Member, consistent with the lithological boundary and the resuming of carbonate production during the DCB transitional interval. & COPY; 2022 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
资助项目	CAS-TWAS scholarship in China ; CAS-TWAS scholarship in China ; Institute of Paleontology and Geology of the Mongolian Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences[XDB26000000] ; National Natural Science Foundation of China[41772004] ; State Key Laboratory of Palaeobiology and Stratigraphy[20152102]
WOS关键词	CARBON-ISOTOPE STRATIGRAPHY ; BOUNDARY ; SECTION ; AGE ; BIOSTRATIGRAPHY ; SEQUENCE ; SHALE ; GOBI
WOS研究方向	Paleontology
语种	英语
出版者	ELSEVIER
WOS记录号	WOS:001044017300001
资助机构	CAS-TWAS scholarship in China ; CAS-TWAS scholarship in China ; Institute of Paleontology and Geology of the Mongolian Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; National Natural Science Foundation of China ; State Key Laboratory of Palaeobiology and Stratigraphy
内容类型	期刊论文
源URL	[http://ir.nigpas.ac.cn/handle/332004/42614]
专题	中国科学院南京地质古生物研究所
通讯作者	Qie, Wen-Kun
作者单位	1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China 2.Univ Sci & Technol China, 96 Jinzhai Rd, Hefei 230026, Peoples R China 3.Mongolian Acad Sci, Inst Paleontol, POB 46-650,S Danzan St 3-1, Ulaanbaatar 15160, Mongolia 4.Mongolian Acad Sci, Inst Geol, Lab Union St, Ulaanbaatar 18080, Mongolia 5.Natl Univ Mongolia, Sch Arts & Sci, Dept Geol & Geophys, Ulaanbaatar, Mongolia
推荐引用方式 GB/T 7714	Byambajav, Uugantsetseg,Qie, Wen-Kun,Yarinpil, Ariunchimeg,et al. Uppermost Devonian-Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area, South Mongolia[J]. PALAEOWORLD,2023,32(3):411-428.
APA	Byambajav, Uugantsetseg,Qie, Wen-Kun,Yarinpil, Ariunchimeg,Batkhuyag, Enkhdalai,Choindonjamts, Erdenejargal,&Puntsag, Delgerzaya.(2023).Uppermost Devonian-Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area, South Mongolia.PALAEOWORLD,32(3),411-428.
MLA	Byambajav, Uugantsetseg,et al."Uppermost Devonian-Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area, South Mongolia".PALAEOWORLD 32.3(2023):411-428.