UPPER DEVONIAN CONODONTS FROM THE TIMAN-PECHORA REGION, RUSSIA, AND CORRELATION WITH A FRASNIAN COMPOSITE STANDARD

Citation
G. Klapper et al., UPPER DEVONIAN CONODONTS FROM THE TIMAN-PECHORA REGION, RUSSIA, AND CORRELATION WITH A FRASNIAN COMPOSITE STANDARD, Journal of paleontology, 70(1), 1996, pp. 129-150
Citations number
69
Categorie Soggetti
Paleontology
Journal title
ISSN journal
00223360
Volume
70
Issue
1
Year of publication
1996
Pages
129 - 150
Database
ISI
SICI code
0022-3360(1996)70:1<129:UDCFTT>2.0.ZU;2-P
Abstract
A Frasnian composite standard provides a refined scaling for the thirt een-fold conodont zonation first developed in the Montagne Noire, Fran ce, but since replicated in North America, Australia, and now the Tima n-Pechora region of Russia. Zones 4-13 are identifiable in seven cores from the Ukhta area of southern Timan and a core from the Bagan Field of the Khoreyver Basin. Scaling of the zones through graphic correlat ion demonstrates the diachronism in different sections of the bases of many conodont species, including those of zonally defining Palmatolep is. This can be effectively shown in a correlation diagram scaled to a composite standard based on graphic correlation, whereas it is obscur ed by the assumption of synchronism inherent in conventional zonal cor relation charts. Newly described species occurring in the Timan-Pechor a region and elsewhere are Ozarkodina nonaginta, Ancyrognathus amplica vus, Mesotaxis johnsoni, Palmatolepis amplificata, P. mucronata, P. or mistoni, and P. timanensis. A number of other species described earlie r from the region also occur outside Russia, mainly in Canada and Aust ralia. Distribution patterns in the composite standard indicate close faunal connections between the Timan-Pechora, western Canada, and West ern Australia.