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Article: New fossil discovery along the section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner, Inner Mongolia

TitleNew fossil discovery along the section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner, Inner Mongolia
Authors
KeywordsAr Horqin Banner
Late Late Permian
Linxi Formation
New discovery
Issue Date2013
Citation
Geological Bulletin of China, 2013, v. 32, n. 8, p. 1269-1276 How to Cite?
AbstractThe section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner of Inner Mongolia is one of typical sections in northeastern China. Abundant fossils such as sporopollen, conchostracan, bivalves and megaplants were found along the section. Among them, sporopollen were discovered for the first time and named Kraeuselisporites spinulosus-Alisporites communis assemblage. Meanwhile, the conchostracans are named Palaeolimnadia-Cyclotunguzites assemblage. The fossil assemblages of Linxi Formation along the section can be correlated with those in Wutonggou Formation and the lower and middle part of Guodikeng Formation along the Dalongkou section in Jimsar, Xinjiang. Therefore, the Linxi Formation at Taohaiyingzi is late Late Permian in age, and can be correlated only to the upper part of the Linxi Formation in the type section in Guandi Town, Linxi County of Inner Mongolia, northeastern China.
Persistent Identifierhttp://hdl.handle.net/10722/326949
ISSN
2023 SCImago Journal Rankings: 0.262

 

DC FieldValueLanguage
dc.contributor.authorZheng, Yue Juan-
dc.contributor.authorZhang, Jian-
dc.contributor.authorChen, Shu Wang-
dc.contributor.authorHuang, Xin-
dc.contributor.authorZhang, Li Jun-
dc.contributor.authorWang, Wu Li-
dc.date.accessioned2023-03-31T05:27:42Z-
dc.date.available2023-03-31T05:27:42Z-
dc.date.issued2013-
dc.identifier.citationGeological Bulletin of China, 2013, v. 32, n. 8, p. 1269-1276-
dc.identifier.issn1671-2552-
dc.identifier.urihttp://hdl.handle.net/10722/326949-
dc.description.abstractThe section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner of Inner Mongolia is one of typical sections in northeastern China. Abundant fossils such as sporopollen, conchostracan, bivalves and megaplants were found along the section. Among them, sporopollen were discovered for the first time and named Kraeuselisporites spinulosus-Alisporites communis assemblage. Meanwhile, the conchostracans are named Palaeolimnadia-Cyclotunguzites assemblage. The fossil assemblages of Linxi Formation along the section can be correlated with those in Wutonggou Formation and the lower and middle part of Guodikeng Formation along the Dalongkou section in Jimsar, Xinjiang. Therefore, the Linxi Formation at Taohaiyingzi is late Late Permian in age, and can be correlated only to the upper part of the Linxi Formation in the type section in Guandi Town, Linxi County of Inner Mongolia, northeastern China.-
dc.languageeng-
dc.relation.ispartofGeological Bulletin of China-
dc.subjectAr Horqin Banner-
dc.subjectLate Late Permian-
dc.subjectLinxi Formation-
dc.subjectNew discovery-
dc.titleNew fossil discovery along the section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner, Inner Mongolia-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-84883769437-
dc.identifier.volume32-
dc.identifier.issue8-
dc.identifier.spage1269-
dc.identifier.epage1276-

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