Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon

Twenty-one species of corals and three species of spongiomorphs occur in a series of richly fossiliferous, molluscan-dominated beds with silicified bioclasts in the Upper Triassic Martin Bridge Limestone of Hells Canyon, Oregon. Two of these, Maeandrostylis grandiseptus and Recticostastraea wallowae...

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Published in:Journal of Paleontology
Main Authors: Stanley, George D., Whalen, Michael T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1989
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022336000036490
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000036490
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spelling crcambridgeupr:10.1017/s0022336000036490 2024-09-15T18:17:06+00:00 Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon Stanley, George D. Whalen, Michael T. 1989 http://dx.doi.org/10.1017/s0022336000036490 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000036490 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 63, issue 6, page 800-819 ISSN 0022-3360 1937-2337 journal-article 1989 crcambridgeupr https://doi.org/10.1017/s0022336000036490 2024-08-07T04:04:16Z Twenty-one species of corals and three species of spongiomorphs occur in a series of richly fossiliferous, molluscan-dominated beds with silicified bioclasts in the Upper Triassic Martin Bridge Limestone of Hells Canyon, Oregon. Two of these, Maeandrostylis grandiseptus and Recticostastraea wallowaensis are new species. Recticostastraea is designated as a new genus. The fauna is early Norian and occurs in the island arc Wallowa terrane, one of many tectonostratigraphic terranes in western North America. Like other examples, it appears to have developed independently of the North American craton and to have links with Wrangellia. The fossil corals and spongiomorphs are para-autochthonous, occurring in a series of tempestite beds. They are interpreted to have inhabited a shallow-water carbonate platform that developed around a tropical island arc following cessation of volcanic activity. The corals and spongiomorphs are associated with abundant gastropods and a diverse epifaunal suspension-feeding bivalve fauna. Relative to the corals, branching spongiomorphs, Spongiomorpha ramosa , are more abundant and occur with relatively common branching, sheet to plate-like, colonial corals. Solitary corals are relatively rare. The associated bedded limestone includes a variety of shallow-water microfacies but throughout the Hells Canyon sequence, reef structure is absent. Together, the 24 coral and spongiomorph taxa show mixed paleogeographic affinities with Upper Triassic faunas known only from alpine regions of the western Tethys (five species), the Pamir Mountains, U.S.S.R. (two species), and the island of Timor (one species). Five additional species are pan-Tethyan and exceptionally cosmopolitan, but 11 species (45.8%) occur only in displaced terranes. Of these, a significant component (six species) is endemic to the Wallowa terrane. At least four Hells Canyon taxa, previously thought endemic to North American terranes, have recently been reported from the high-latitude Koryak terrane of northeastern U.S.S.R., a ... Article in Journal/Newspaper Koryak Cambridge University Press Journal of Paleontology 63 6 800 819
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collection Cambridge University Press
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language English
description Twenty-one species of corals and three species of spongiomorphs occur in a series of richly fossiliferous, molluscan-dominated beds with silicified bioclasts in the Upper Triassic Martin Bridge Limestone of Hells Canyon, Oregon. Two of these, Maeandrostylis grandiseptus and Recticostastraea wallowaensis are new species. Recticostastraea is designated as a new genus. The fauna is early Norian and occurs in the island arc Wallowa terrane, one of many tectonostratigraphic terranes in western North America. Like other examples, it appears to have developed independently of the North American craton and to have links with Wrangellia. The fossil corals and spongiomorphs are para-autochthonous, occurring in a series of tempestite beds. They are interpreted to have inhabited a shallow-water carbonate platform that developed around a tropical island arc following cessation of volcanic activity. The corals and spongiomorphs are associated with abundant gastropods and a diverse epifaunal suspension-feeding bivalve fauna. Relative to the corals, branching spongiomorphs, Spongiomorpha ramosa , are more abundant and occur with relatively common branching, sheet to plate-like, colonial corals. Solitary corals are relatively rare. The associated bedded limestone includes a variety of shallow-water microfacies but throughout the Hells Canyon sequence, reef structure is absent. Together, the 24 coral and spongiomorph taxa show mixed paleogeographic affinities with Upper Triassic faunas known only from alpine regions of the western Tethys (five species), the Pamir Mountains, U.S.S.R. (two species), and the island of Timor (one species). Five additional species are pan-Tethyan and exceptionally cosmopolitan, but 11 species (45.8%) occur only in displaced terranes. Of these, a significant component (six species) is endemic to the Wallowa terrane. At least four Hells Canyon taxa, previously thought endemic to North American terranes, have recently been reported from the high-latitude Koryak terrane of northeastern U.S.S.R., a ...
format Article in Journal/Newspaper
author Stanley, George D.
Whalen, Michael T.
spellingShingle Stanley, George D.
Whalen, Michael T.
Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
author_facet Stanley, George D.
Whalen, Michael T.
author_sort Stanley, George D.
title Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
title_short Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
title_full Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
title_fullStr Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
title_full_unstemmed Triassic corals and spongiomorphs from Hells Canyon, Wallowa terrane, Oregon
title_sort triassic corals and spongiomorphs from hells canyon, wallowa terrane, oregon
publisher Cambridge University Press (CUP)
publishDate 1989
url http://dx.doi.org/10.1017/s0022336000036490
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000036490
genre Koryak
genre_facet Koryak
op_source Journal of Paleontology
volume 63, issue 6, page 800-819
ISSN 0022-3360 1937-2337
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0022336000036490
container_title Journal of Paleontology
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