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Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)
通讯作者Suttner, Thomas James([email protected])
Suttner, Thomas James1,2; Uugantsetseg, Byambajav3,4,5; Ariunchimeg, Yarinpil3; Manchuk, Nuramkhaan6; Kido, Erika2; Erdenejargal, Choindonjamts7,8; Buyantegsh, Batsaikhan3; Enkhbaatar, Batkhuyag3,8; Zorig, Enkhtaivan3
2023-06-01
发表期刊NEWSLETTERS ON STRATIGRAPHY
ISSN0078-0421
页码24
摘要The Late Devonian-early Carboniferous aged Indert Formation near Shine Jinst (southern Mongolia) is subdivided into the Heermorit and Shombon members. A systematic collection of the few marine carbonaterich levels from the Heermorit Member resulted in a low-diverse conodont assemblage indicating the late Famennian Bispathodus ultimus conodont Biozone at the Tsagaankhaalga-2 section. Supplemental conodont data from the Yamaan Us section support early Tournaisian age for the lowermost limestone beds of the above deposited Shombon Member. In total, twelve species in seven genera are identified and include Apatognathus, Mehlina, Pandorinellina, Polygnathus (including the new taxon Polygnathus communis tomurtogooi n. ssp.), Pseudopolygnathus, transitional forms of Polygnathus-Siphonodella and Siphonodella. The significance and palaeogeographic distribution of the markedly increased occurrence of intergeneric transitional forms before and during the Late Devonian Hangenberg Event and regionally lacking evidence of the end-Famennian Protognathodus kockeli conodont Biozone and associated early protognathodid assemblage below the Devonian/ Carboniferous boundary are discussed.
关键词Devonian Carboniferous boundary Famennian Tournaisian biotic crisis conodonts biodiversity
DOI10.1127/nos/2023/0760
收录类别SCI
语种英语
关键词[WOS]NW CHINA IMPLICATIONS ; CARBONIFEROUS BOUNDARY ; WEST JUNGGAR ; NORTHERN ; EVOLUTION ; STRATIGRAPHY ; OCEAN ; AREA
资助项目Institute of Paleontology of the Mongolian Academy of Sciences ; Ministry of Mining and Heavy industry, Mongolia[2019/7] ; Czech Geological Survey[311410]
WOS研究方向Geology
WOS类目Geology
WOS记录号WOS:001013930700001
项目资助者Institute of Paleontology of the Mongolian Academy of Sciences ; Ministry of Mining and Heavy industry, Mongolia ; Czech Geological Survey
出版者GEBRUDER BORNTRAEGER
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/42441
专题中国科学院南京地质古生物研究所
通讯作者Suttner, Thomas James
作者单位1.Czech Geol Survey, Geol 6, Prague 5, Czech Republic
2.Appalachian State Univ, Dept Geol & Environm Sci, 572 Rivers St, Boone, NC 28608 USA
3.Mongolian Acad Sci, Inst Paleontol, POB 46-650,S Danzan St 3-1, Ulaanbaatar 15160, Mongolia
4.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China
5.Univ Sci & Technol China, 96 Jinzhai Rd, Hefei 230026, Peoples R China
6.Branch Mongolian Univ Sci & Technol, Erdenet Inst Technol, Div Erdenet Min Corp SOE, POB 985,Otgonbileg St, Bayan Undur Soum, Orkhon Province, Mongolia
7.Mongolian Acad Sci, Inst Geol, Lab Union St Songinokhairkhan Dist, Ulaanbaatar 18080, Mongolia
8.Natl Univ Mongolia, Sch Art & Sci, Dept Geol & Geophys, Ulaanbaatar, Mongolia
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GB/T 7714
Suttner, Thomas James,Uugantsetseg, Byambajav,Ariunchimeg, Yarinpil,et al. Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)[J]. NEWSLETTERS ON STRATIGRAPHY,2023:24.
APA Suttner, Thomas James.,Uugantsetseg, Byambajav.,Ariunchimeg, Yarinpil.,Manchuk, Nuramkhaan.,Kido, Erika.,...&Zorig, Enkhtaivan.(2023).Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia).NEWSLETTERS ON STRATIGRAPHY,24.
MLA Suttner, Thomas James,et al."Case study on Hangenberg Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation, Shine Jinst region, southern Mongolia)".NEWSLETTERS ON STRATIGRAPHY (2023):24.
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