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Nafi, Mutwakil, Wenchen, Xia, Ning, Zhang (2006) Late Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China. Canadian Journal of Earth Sciences, 43 (2) 121-133 doi:10.1139/e05-097

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Reference TypeJournal (article/letter/editorial)
TitleLate Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China
JournalCanadian Journal of Earth Sciences
AuthorsNafi, MutwakilAuthor
Wenchen, XiaAuthor
Ning, ZhangAuthor
Year2006 (February 1)Volume43
Issue2
PublisherCanadian Science Publishing
DOIdoi:10.1139/e05-097Search in ResearchGate
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Mindat Ref. ID484149Long-form Identifiermindat:1:5:484149:8
GUID0
Full ReferenceNafi, Mutwakil, Wenchen, Xia, Ning, Zhang (2006) Late Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China. Canadian Journal of Earth Sciences, 43 (2) 121-133 doi:10.1139/e05-097
Plain TextNafi, Mutwakil, Wenchen, Xia, Ning, Zhang (2006) Late Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China. Canadian Journal of Earth Sciences, 43 (2) 121-133 doi:10.1139/e05-097
In(2006, February) Canadian Journal of Earth Sciences Vol. 43 (2) Canadian Science Publishing
Abstract/Notes Four neogondolellid conodont interval zones were recognized across the Changhsingian stage at Ganxi section, western Hubei Province, south China. They are in ascending order: the Clarkina wangi Zone, the Clarkina changxingensis changxingensis Zone, the Clarkina changxingensis yini Zone, and the Clarkina meishanensis meishanensis Zone. The present study suggests that the base of the Changhsingian can be defined by the first appearance datum (FAD) of Clarkina wangi within an evolutionary lineage from Clarkina longicuspidata to Clarkina wangi. The WuchiapingianChanghsingian boundary can be placed at the base of bed 104 at Ganxi section, south China because of the first occurrence of Clarkina wangi.


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