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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Cambridge University Press (CUP)
1989
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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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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 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
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 |
container_volume |
63 |
container_issue |
6 |
container_start_page |
800 |
op_container_end_page |
819 |
_version_ |
1810455092168491008 |