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• W2062610075 abstract "Research Article| July 01, 2001 JINZHANGIA, A NEW STAFFELLID FUSULINOIDEA FROM THE MIDDLE PERMIAN DAAOZI FORMATION OF THE BAOSHAN BLOCK, WEST YUNNAN, CHINA Katsumi Ueno Katsumi Ueno 1 Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka 814-0180 JAPAN 1Email: katsumi@fukuoka-u.ac.jp Search for other works by this author on: GSW Google Scholar Author and Article Information Katsumi Ueno 1 Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka 814-0180 JAPAN 1Email: katsumi@fukuoka-u.ac.jp Publisher: Cushman Foundation for Foraminiferal Research Received: 27 Jul 2000 Accepted: 06 Feb 2001 First Online: 03 Mar 2017 Online ISSN: 1943-264X Print ISSN: 0096-1191 © 2001 Journal of Foraminiferal Research Journal of Foraminiferal Research (2001) 31 (3): 233–243. https://doi.org/10.2113/31.3.233 Article history Received: 27 Jul 2000 Accepted: 06 Feb 2001 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation Katsumi Ueno; JINZHANGIA, A NEW STAFFELLID FUSULINOIDEA FROM THE MIDDLE PERMIAN DAAOZI FORMATION OF THE BAOSHAN BLOCK, WEST YUNNAN, CHINA. Journal of Foraminiferal Research 2001;; 31 (3): 233–243. doi: https://doi.org/10.2113/31.3.233 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract Permian foraminifers are reported and illustrated for the first time from the lower part of the Daaozi Formation of the Baoshan Block, West Yunnan, China. The Baoshan Block is a Gondwana-derived continental fragment that is believed to be a key to understanding Gondwana dispersion and Asian accretion during Paleozoic and Mesozoic time. Its Late Paleozoic foraminifers have been poorly documented until now. The Daaozi assemblage is dominated by oval staffellids representing the new genus, Jinzhangia, with J. shengi Ueno, n. sp. as the type species, and several other smaller foraminifers, including Pachyphloia robustaformis Wang, Okimuraites? cf. O. guvenci (Altiner), and Kamurana? sp. Although these foraminifers do not provide a precise age determination, associated corals reveal a Murgabian age for the assemblage.Among the oval and fusiform staffellids from Eurasia, only Leella armenica Rozovskaya from the Middle Permian of Transcaucasia should be referable to the new genus Jinzhangia. Thus, Jinzhangia apparently is restricted to Baoshan and Transcaucasia, which are parts of the Cimmerian continent and which was paleogeo-graphically independent of both Gondwanaland and the Cathaysian blocks, such as Indochina and Yangtze, during Permian and Triassic time. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2062610075 title "JINZHANGIA, A NEW STAFFELLID FUSULINOIDEA FROM THE MIDDLE PERMIAN DAAOZI FORMATION OF THE BAOSHAN BLOCK, WEST YUNNAN, CHINA" @default.
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