Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska
Conodont faunas from the upper part of the Wadleigh Limestone, Alexander terrane, southeastern Alaska, are of Frasnian to early Famennian age and include the new taxa Polygnathus aspelundi nanus n. subsp., Polygnathus decorosus dutroi n. subsp., Polygnathus elegantulus sparus n. subsp., Polygnathus...
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Language: | English |
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Cambridge University Press (CUP)
1992
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Online Access: | http://dx.doi.org/10.1017/s0022336000033795 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033795 |
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crcambridgeupr:10.1017/s0022336000033795 2024-05-19T07:46:17+00:00 Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska Savage, Norman M. 1992 http://dx.doi.org/10.1017/s0022336000033795 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033795 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 66, issue 2, page 277-292 ISSN 0022-3360 1937-2337 journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0022336000033795 2024-04-25T06:51:44Z Conodont faunas from the upper part of the Wadleigh Limestone, Alexander terrane, southeastern Alaska, are of Frasnian to early Famennian age and include the new taxa Polygnathus aspelundi nanus n. subsp., Polygnathus decorosus dutroi n. subsp., Polygnathus elegantulus sparus n. subsp., Polygnathus gracilis n. subsp. A, Polygnathus n. sp. A, Palmatolepis subrecta youngquisti n. subsp., and Icriodus subterminus uyenoi n. subsp. Four distinct age-determined faunal assemblages are recognized. The lowest is assigned to the Lower Palmatolepis rhenana Zone (the chronozones of Ziegler and Sandberg, 1990, are treated herein as time-rock equivalent assemblage zones). The next is exposed on three small islands just south of Wadleigh Island and is correlated with part of the Lower to Upper Palmatolepis rhenana Zones. The third assemblage, on the eastern side of Wadleigh Island from close to the top of the section, is correlated with part of the Palmatolepis linguiformis Zone. Nearby and overlying this is the fourth assemblage, which is correlated with part of the Lower Palmatolepis triangularis Zone and thus appears to be within the lower Famennian. These Wadleigh Limestone conodont faunas have affinities with faunas from equivalent horizons of the cratonic regions of the Northwest Territories and Alberta in Western Canada and to other faunas globally. The more provincial conodont taxa lend weak but positive support to brachiopod faunal evidence that places the Alexander terrane close to the North American craton during the Late Devonian. Article in Journal/Newspaper Northwest Territories Alaska Cambridge University Press Journal of Paleontology 66 2 277 292 |
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Open Polar |
collection |
Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Conodont faunas from the upper part of the Wadleigh Limestone, Alexander terrane, southeastern Alaska, are of Frasnian to early Famennian age and include the new taxa Polygnathus aspelundi nanus n. subsp., Polygnathus decorosus dutroi n. subsp., Polygnathus elegantulus sparus n. subsp., Polygnathus gracilis n. subsp. A, Polygnathus n. sp. A, Palmatolepis subrecta youngquisti n. subsp., and Icriodus subterminus uyenoi n. subsp. Four distinct age-determined faunal assemblages are recognized. The lowest is assigned to the Lower Palmatolepis rhenana Zone (the chronozones of Ziegler and Sandberg, 1990, are treated herein as time-rock equivalent assemblage zones). The next is exposed on three small islands just south of Wadleigh Island and is correlated with part of the Lower to Upper Palmatolepis rhenana Zones. The third assemblage, on the eastern side of Wadleigh Island from close to the top of the section, is correlated with part of the Palmatolepis linguiformis Zone. Nearby and overlying this is the fourth assemblage, which is correlated with part of the Lower Palmatolepis triangularis Zone and thus appears to be within the lower Famennian. These Wadleigh Limestone conodont faunas have affinities with faunas from equivalent horizons of the cratonic regions of the Northwest Territories and Alberta in Western Canada and to other faunas globally. The more provincial conodont taxa lend weak but positive support to brachiopod faunal evidence that places the Alexander terrane close to the North American craton during the Late Devonian. |
format |
Article in Journal/Newspaper |
author |
Savage, Norman M. |
spellingShingle |
Savage, Norman M. Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
author_facet |
Savage, Norman M. |
author_sort |
Savage, Norman M. |
title |
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
title_short |
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
title_full |
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
title_fullStr |
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
title_full_unstemmed |
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska |
title_sort |
late devonian (frasnian and famennian) conodonts from the wadleigh limestone, southeastern alaska |
publisher |
Cambridge University Press (CUP) |
publishDate |
1992 |
url |
http://dx.doi.org/10.1017/s0022336000033795 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033795 |
genre |
Northwest Territories Alaska |
genre_facet |
Northwest Territories Alaska |
op_source |
Journal of Paleontology volume 66, issue 2, page 277-292 ISSN 0022-3360 1937-2337 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0022336000033795 |
container_title |
Journal of Paleontology |
container_volume |
66 |
container_issue |
2 |
container_start_page |
277 |
op_container_end_page |
292 |
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1799486434289123328 |