Hostname: page-component-848d4c4894-x24gv Total loading time: 0 Render date: 2024-06-02T14:07:54.730Z Has data issue: false hasContentIssue false
  • English
  • Français

Middle Devonian conodonts from the Wadleigh Limestone, southeastern Alaska

Published online by Cambridge University Press:  20 May 2016

Norman M. Savage
Norman M. Savage*
Affiliation:
Department of Geological Sciences, University of Oregon, Eugene 97403
Get access Rights & Permissions [Opens in a new window]

Abstract

Conodonts from two localities on the western shore of Alberto Island, southeastern Alaska, include Polygnathus alexanderensis n. sp., P. angustipennatus, P. borealis n. sp., P. praetrigonicus n. sp., P. robusticostatus, P. pseudofoliatus, P. linguiformis linguiformis gamma form of Bultynck, P. parawebbi beta form of Chatterton, P. angusticostatus, P. costatus costatus, Polygnathus sp. B of Savage, 1977, Tortodus kockelianus australis, and T. kockelianus kockelianus. The faunas are considered to be of middle to late Eifelian (kockelianus Zone) age. On Prince of Wales Island, just north of Staney Creek, exposures of Wadleigh Limestone include the conodonts Polygnathus trigonicus, P. kennettensis, P. alexanderensis, P. angustipennatus, P. parawebbi beta form, P. eiflius, P. linguiformis linguiformis gamma form, P. borealis, P. angusticostatus, P. robusticostatus, P. costatus costatus, P. pseudofoliatus, Tortodus kockelianus australis, and T. kockelianus kockelianus, also suggesting a middle to late Eifelian (kockelianus Zone) age. Conodonts from the west end of the easternmost of the Alberto Islands include Polygnathus linguiformis linguiformis gamma form, P. parawebbi beta form, P. xylus ensensis, and Ozarkodina brevis, indicating a late Eifelian to early Givetian (ensensis to varcus Zones) age. The presence of Polygnathus kennettensis, P. parawebbi beta form, and P. borealis suggests a biogeographic affinity with other parts of western North America during Eifelian time.

Type
Research Article
Information
Journal of Paleontology , Volume 69 , Issue 3 , May 1995 , pp. 540 - 555
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Barnes, C. R., and Fåhraeus, L. E. 1975. Provinces, communities, and the proposed nectobenthic habit of Ordovician conodontophorids. Lethaia, 8:133–149.CrossRefGoogle Scholar
Bassler, R. S. 1925. Classification and stratigraphic use of conodonts. Geological Society of America Bulletin, 36:218–220.Google Scholar
Bergström, S. M. 1973. Ordovician conodont biogeography, p. 47–58. In Hallam, A. (ed.), Atlas of Palaeobiogeography. Elsevier Scientific Publishing Co., Amsterdam.Google Scholar
Bergström, S. M. 1983. Biogeography, evolutionary relationships and biostratigraphic significance of Ordovician platform conodonts. Fossils and Strata, 15:35–58.CrossRefGoogle Scholar
Bischoff, G., and Ziegler, W. 1957. Die Conodontenchronologie des Mitteldevons und des tiefsten Oberdevons. Hessischen Landesamtes Bodenforschung Abhandlungen, 22, 136 p.Google Scholar
Branson, E. B., and Mehl, M. G. 1933. Conodont studies. University of Missouri Studies, 8:1–349.Google Scholar
Bultynck, P. 1970. Révision stratigraphique et paléontologique (Brachiopodes et Conodontes) de la coupe type du Couvinien. Mémoires de l'Institut Géologique de l'Université de Louvain, 26, 152 p.Google Scholar
Bultynck, P. 1976. Comparative study of Middle Devonian conodonts from north Michigan (U.S.A.) and the Ardennes (Belgium-France). Geological Association of Canada, Special Paper 15:119–141.Google Scholar
Chatterton, B. D. E. 1974. Middle Devonian conodonts from the Harrogate Formation, southeastern British Columbia. Canadian Journal of Earth Sciences, 11:1461–1484.CrossRefGoogle Scholar
Chatterton, B. D. E. 1979. Aspects of late Early and Middle Devonian conodont biostratigraphy of western and northwestern Canada. Geological Association of Canada, Special Paper 18:161–231.Google Scholar
Fåhraeus, L. E. 1976. Possible Early Devonian conodontophorid provinces. Palaeogeography, Palaeoclimatology, Palaeoecology, 19:201–217.CrossRefGoogle Scholar
Hass, W. H. 1959. Conodonts from the Chappel Limestone of Texas. U.S. Geological Survey, Professional Paper 295-J:365–369.Google Scholar
Hinde, G. J. 1879. On conodonts from the Chazy and Cincinnati Group of the Cambro-Silurian, and from the Hamilton and Genesee Shale of the Devonian, in Canada and the United States. Quarterly Journal of the Geological Society of London, 35:351–369.CrossRefGoogle Scholar
Klapper, G. 1971. Sequence within the conodont genus Polygnathus in the New York lower Middle Devonian. Geologica et Paleontologica, 5:59–79.Google Scholar
Klapper, G. 1977. Ozarkodina brevis , p. 263–265. In Ziegler, W. (ed.), Catalogue of Conodonts, Volume 3. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart.Google Scholar
Klapper, G. 1991. Polygnathus xylus ensensis , p. 155–157. In Ziegler, W. (ed.), Catalogue of Conodonts, Volume 5. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart.Google Scholar
Klapper, G., and Johnson, J. G. 1980. Endemism and dispersal of Devonian conodonts. Journal of Paleontology, 54:400–455.Google Scholar
MacFarlane, J. M. 1923. Fishes: the Source of Petroleum. The Macmillan Company, New York, 451 p.Google Scholar
Pedder, A. E. H., Jackson, J. H., and Ellenor, D. W. 1970. An interim account of the Middle Devonian Timor Limestone of northeastern New South Wales. Proceedings of the Linnean Society of New South Wales, 94:242–272.Google Scholar
Savage, N. M. 1976. Middle Devonian species of Polygnathus from the Kennett Formation, northern California. Journal of Paleontology, 50:374–379.Google Scholar
Savage, N. M. 1977. Middle Devonian (Eifelian) conodonts of the genus Polygnathus from the Wadleigh Limestone, southeastern Alaska. Canadian Journal of Earth Sciences, 14:1343–1355.CrossRefGoogle Scholar
Savage, N. M. 1987. New polygnathid conodonts from the Frasnian (Upper Devonian) of southeastern Alaska. Canadian Journal of Earth Sciences, 24:2323–2328.CrossRefGoogle Scholar
Savage, N. M. 1989. Devonian faunas and major depositional events in the southern Alexander terrane, southeastern Alaska, p. 257–264. In McMillan, N. J., Embry, A. F., and Glass, D. J. (eds.), Devonian of the World. Canadian Society of Petroleum Geologists, Memoir 14(3).Google Scholar
Savage, N. M. 1990a. Conodonts of Caradocian (Late Ordovician) age from the Cliefden Caves Limestone, southeastern Australia. Journal of Paleontology, 64:821–831.CrossRefGoogle Scholar
Savage, N. M. 1990b. Paleozoic faunal affinities of the Alexander terrane, southeast Alaska. Geological Society of America, Abstracts with Programs, 15:A321.Google Scholar
Savage, N. M. 1992. Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska. Journal of Paleontology, 66:277–292.CrossRefGoogle Scholar
Savage, N. M., and Amundson, C. T. 1979. Middle Devonian (Givetian) conodonts from central Oregon. Journal of Paleontology, 53:1395–1400.Google Scholar
Savage, N. M., and Baxter, M. In press. Late Devonian (Frasnian) brachiopods from the Wadleigh Limestone, southeastern Alaska. Journal of Paleontology.Google Scholar
Savage, N. M., and Funai, C. A. 1980. Devonian conodonts of probable early Frasnian age from the Coronados Islands of southeastern Alaska. Journal of Paleontology, 54:806–813.Google Scholar
Savage, N. M., and Gehrels, G. E. 1984. Early Devonian conodonts from Prince of Wales Island, southeastern Alaska. Canadian Journal of Earth Sciences, 21:1414–1425.CrossRefGoogle Scholar
Stauffer, C. R. 1940. Conodonts from the Devonian and associated clays of Minnesota. Journal of Paleontology, 14:417–435.Google Scholar
Sweet, W. C. 1988. The Conodonta: morphology, taxonomy, paleoecology, and evolutionary history of a long-extinct animal phylum. Oxford Monographs on Geology and Geophysics, No. 10, Oxford University Press, Oxford, 212 p.Google Scholar
Sweet, W. C., and Bergström, S. M. 1974. Provincialism exhibited by Ordovician conodont faunas. Society of Economic Paleontologists and Mineralogists, Special Publication 21:189–202.Google Scholar
Telford, P. G. 1972. Conodonts, p. 83–88. In Talent, J. A. et al., Provincialism and Australian Early Devonian faunas. Journal of the Geological Society of Australia, 19:81–97.Google Scholar
Uyeno, T. T. 1979. Devonian conodont biostratigraphy of Powell Creek and adjacent areas, western District of Mackenzie. Geological Association of Canada, Special Paper 18:233–257.Google Scholar
Uyeno, T. T. 1982. Systematic conodont paleontology, p. 73–80. In Norris, A. W., Uyeno, T. T., and McCabe, H. R., Devonian rocks of the Lake Winnipegosis-Lake Manitoba Outcrop Belt, Manitoba. Geological Survey of Canada, Memoir 392, 280 p.Google Scholar
Wang, R. 1992. Phylogenie und evolution der conodonten aus der Moyuela-Formation (Eifelium) in Keltiberien, Spanien. Neues Jahrbuch Geologie und Paläontologie Abhandlungen, 184:315–338.Google Scholar
Weddige, K. 1977. Die Conodonten der Eifel-Stufe im Typusgebiet und in benachbarten Faziesgebieten. Senckenbergiana Lethaea, 58:271–419.Google Scholar
Wittekindt, H. 1966. Zur Conodontenchronologie des Mitteldevons. Fortschritte in der Geologie von Rheinland und Westfalen, 9:621–646.Google Scholar
Youngquist, W. L. 1945. Upper Devonian conodonts from the Independence Shale(?) of Iowa. Journal of Paleontology, 19:355–367.Google Scholar
Ziegler, W., Klapper, G., and Johnson, J. G. 1976. Redefinition and subdivision of the varcus-Zone (Conodonts, Middle–?Upper Devonian) in Europe and North America. Geologica et Palaeontologica, 10:109–140.Google Scholar