Hostname: page-component-76fb5796d-r6qrq Total loading time: 0 Render date: 2024-04-25T16:35:27.967Z Has data issue: false hasContentIssue false

Triassic sponges (Sphinctozoa) from Hells Canyon, Oregon

Published online by Cambridge University Press:  02 September 2016

Baba Senowbari-Daryan
Affiliation:
Institute of Paläontology, University of Erlangen–Nürnberg, Loewenichstrasse 28, D-8520 Erlangen, West Germany
George D. Stanley Jr.
Affiliation:
Department of Geology, University of Montana, Missoula 59812

Abstract

Two Upper Triassic sphinctozoan sponges of the family Sebargasiidae were recovered from silicified residues collected in Hells Canyon, Oregon. These sponges are Amblysiphonella cf. A. steinmanni (Haas), known from the Tethys region, and Colospongia whaleni n. sp., an endemic species. The latter sponge was placed in the superfamily Porata by Seilacher (1962). The presence of well-preserved cribrate plates in this sponge, in addition to pores of the chamber walls, is a unique condition never before reported in any porate sphinctozoans. Aporate counterparts known primarily from the Triassic Alps have similar cribrate plates but lack the pores in the chamber walls. The sponges from Hells Canyon are associated with abundant bivalves and corals of marked Tethyan affinities and come from a displaced terrane known as the Wallowa Terrane. It was a tropical island arc, suspected to have paleogeographic relationships with Wrangellia; however, these sponges have not yet been found in any other Cordilleran terrane.

Type
Research Article
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

Dieci, G., Antonacci, A., and Zardini, R. 1968. Le spugne cassiane (Trias medio-superiore) della regione dolomitica attorno a Cortina d'Ampezzo. Bollettino della Societa Paleontologica Italiana, 7:94155.Google Scholar
Finks, R. M. 1983. Pharetronida: Inozoa and Sphinctozoa, p. 5569. In Broadhead, T. W. (ed.), Sponges and Spongiomorphs, Notes for a Short Course. University of Tennessee, Department of Geological Sciences, Studies in Geology 7.Google Scholar
Flügel, E. 1981. Paleoecology and facies of Upper Triassic reefs in the Northern Calcareous Alps, p. 291359. In Toomey, D. F. (ed.), European Fossil Reef Models. Society of Economic Paleontologists and Mineralogists Publication 30.Google Scholar
Flügel, H. W. 1972. Catalogus Fossilium Austriae: ein systematisches Verzeichnis aller auf österreichischen Gebiet festgestellten Fossilien. Österreichische Akademie Wissenschaften, III(a–b):131.Google Scholar
Haas, O. 1909. Bericht über neue Aufsammlungen in den Zlambach-Mergeln der Fischerwiese bei Alt-Aussee. Beiträge zur Paläontologie und Geologie, Österreich-Ungarns und des Orients, 22:143167.Google Scholar
Harmsen, F. J., and Stanley, G. D. Jr. 1986. Sedimentological history of early Mesozoic rocks, central Peru. 12th International Sedimentological Congress, Canberra, Australia, Abstracts Volume, p. 1330.Google Scholar
Körner, K. 1937. Marine (Cassianer-Raibler) Trias am Nevado Acrotambo (Nord-Peru). Paläontographica A, 86:145240.Google Scholar
Kristan-Tollmann, E., and Tollmann, A. 1983. Tethys-Faunenelemente in der Trias der USA. Mitteilungen Österreichischen Geologischen Gesellschaft, 76:213272.Google Scholar
Laube, G. D. 1865. Die Fauna der Schichten von St. Cassian. I. Abteilung. Denkschrift Kaisers Akademie Wissenschaften, mathematisch-naturwissenschaft Klasse, 24:223296.Google Scholar
Newton, C. R. 1986. Late Triassic bivalves of the Martin Bridge Limestone, Hells Canyon, Oregon: taphonomy, paleoecology, paleozoogeography. U.S. Geological Survey Professional Paper 1435:722.Google Scholar
Newton, C. R., Whalen, M. T., Thompson, J. B., Prins, N., and Delalla, D. 1987. Systematics and paleoecology of Norian (Late Triassic) bivalves from a tropical island arc: Wallowa Terrane, Oregon. The Paleontological Society, Memoir 22, 83 p.Google Scholar
Ott, E. 1967. Segmentierte Kalkschwämme (Sphinctozoa) aus der alpinen Mitteltrias und ihre Bedeutung als Riff bildner im Wettersteinkalk. Bayerische Akademie Wissenschaften, mathematisch-naturwissenschaft Klasse Abhandlungen N.F., 131:196.Google Scholar
Rauff, H. 1938. Über einige Kalkschwämme aus der Trias der peruanischen Kordillere nebst einem Anhang über Stellispongia und ihre Arten. Palaeontologische Zeitschrift, 20:177214.Google Scholar
Reid, R. P. 1985. The facies and evolution of an Upper Triassic reef complex in northern Canada. Unpubl. Ph.D. dissertation, University of Miami, Miami, Florida, 437 p.Google Scholar
Rigby, J. K., and Potter, A. W. 1986. Ordovician sphinctozoan sponges from the eastern Klamath Mountains, northern California. The Paleontological Society, Memoir 20, 47 p.Google Scholar
Russo, F. 1981. Nuove spugne calcarea triassiche di Campo (Cortina d'Ampezzo, Belluno). Bollettino della Societa Paleontologica Italiana, 20:317.Google Scholar
Saleeby, J. B. 1983. Accretionary tectonics of the North American Cordillera. Annual Review of Earth and Planetary Sciences, 15:4573.Google Scholar
Seilacher, A. 1962. Die Sphinctozoa, eine Gruppe fossiler Kalkschwämme. Akademie Wissenschaften Literatur, Abhandlungen mathematisch-naturwissenschaften Klasse, 10:720790.Google Scholar
Senowbari-Daryan, B., and Reid, R. P. 1987. Upper Triassic sponges (Sphinctozoa) from southern Yukon, Stikinia Terrane. Canadian Journal of Earth Sciences, 24:882902.CrossRefGoogle Scholar
Senowbari-Daryan, B., and Schäfer, P. 1983. Zur Sphinctozoen-Fauna der obertriadischen Riff kalke (“Pantokratorkalke”) von Hydra, Griechenland. Geologica et Palaeontographica, 17:179205.Google Scholar
Senowbari-Daryan, B., and Schäfer, P. 1986. Sphinctozoans (calcareous sponges) from Norian reefs of Sicily (Italy). Facies, 14:235284.Google Scholar
Stanley, G. D. Jr. 1979. Paleoecology, structure, and distribution of Triassic coral buildups in western North America. University of Kansas Paleontological Contributions, Article 65, 58 p.Google Scholar
Stanley, G. D. Jr. 1980. Triassic carbonate buildups of western North America: comparisons with the alpine Triassic of Europe. Rivista Italiana di Paleontologia e Stratigrafia, 85:877894.Google Scholar
Stanley, G. D. Jr. 1982. Triassic carbonate development and reef building in western North America. Geologische Rundschau, 71:10571075.Google Scholar
Stanley, G. D. Jr. 1986. Late Triassic coelenterate faunas of western Idaho and northeastern Oregon: implications for biostratigraphy and paleogeography. U.S. Geological Survey Professional Paper 1435:2329.Google Scholar
Stanley, G. D. Jr. and Senowbari-Daryan, B. 1986. Upper Triassic Dachsteintype, reef limestone from the Wallowa Mountains, Oregon: first reported occurrence in the United States. Palaios, 1:172177.Google Scholar
Steinmann, G. 1882. Pharetronen-Studien. Neues Jahrbuch Mineralogie, Geologie und Paläontologie, II:139191.Google Scholar
Vallier, T. L. 1967. The geology of part of the Snake River canyon and adjacent areas in northeastern Oregon and western Idaho. Unpubl. Ph.D. dissertation, Oregon State University, Corvallis, 267 p.Google Scholar
Vallier, T. L. 1977. The Permian and Triassic Seven Devils Group, western Idaho and northeastern Oregon. U.S. Geological Survey Bulletin, 1437, 58 p.Google Scholar
Whalen, M. T. 1985. Carbonate petrology and paleontology of Upper Triassic limestone of the Wallowa Terrane, Oregon and Idaho. Unpubl. , University of Montana, Missoula, 151 p.Google Scholar