New species of Silurian acanthodians from the Mackenzie Mountains, Canada

Two new acanthodian taxa are described. The ischnacanthid Xylacanthus kenstewarti is based on large, dentigerous jaws, and Granulacanthus joenelsoni is based on isolated spines. The isolated remains of these species are similar in that they both possess pustulose denticles or tubercles, either on th...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Hanke, Gavin F, Wilson, Mark VH, Lindoe, L Allan
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2001
Subjects:
Online Access:http://dx.doi.org/10.1139/e01-039
http://www.nrcresearchpress.com/doi/pdf/10.1139/e01-039
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spelling crcansciencepubl:10.1139/e01-039 2024-09-15T18:18:10+00:00 New species of Silurian acanthodians from the Mackenzie Mountains, Canada Hanke, Gavin F Wilson, Mark VH Lindoe, L Allan 2001 http://dx.doi.org/10.1139/e01-039 http://www.nrcresearchpress.com/doi/pdf/10.1139/e01-039 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 38, issue 11, page 1517-1529 ISSN 0008-4077 1480-3313 journal-article 2001 crcansciencepubl https://doi.org/10.1139/e01-039 2024-07-25T04:10:07Z Two new acanthodian taxa are described. The ischnacanthid Xylacanthus kenstewarti is based on large, dentigerous jaws, and Granulacanthus joenelsoni is based on isolated spines. The isolated remains of these species are similar in that they both possess pustulose denticles or tubercles, either on the mesial ridge (X. kenstewarti) or on the fin spines (G. joenelsoni). Jaws of X. kenstewarti are similar in size to those of Xylacanthus minutus, Ischnacanthus kingi, and I. wickhami and smaller than those of X. grandis. The jaws of X. kenstewarti are most similar to those of X. minutus, but are distinguished from this and other ischnacanthid species by a tapering patch of pustulose denticles that is widest midway along the jaw, mesial denticles that are simple blisterlike structures, the monocuspid, striated primary teeth that are subcircular in cross section, and a posterodorsal process that is enlarged. The spines of G. joenelsoni have distinctive tubercular ornamentation. Tubercles, or nodular ornaments on fin spines, are characteristic of primitive acanthodians, but the slender shape of the spines, the low number of spine ribs, and the fine striations posterior to the main ribs of each spine suggest that G. joenelsoni is a relatively advanced acanthodian. Xylacanthus kenstewarti and G. joenelsoni are from the Silurian (Wenlock or Ludlow) of the southern Mackenzie Mountains. Xylacanthus kenstewarti represents the earliest representative of the genus, the earliest unequivocal remains of a gnathostome from the Mackenzie Mountains, and extends the known geographical range of the genus from the Mackenzie Mountains east to Spitsbergen. Article in Journal/Newspaper Mackenzie mountains Spitsbergen Canadian Science Publishing Canadian Journal of Earth Sciences 38 11 1517 1529
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Two new acanthodian taxa are described. The ischnacanthid Xylacanthus kenstewarti is based on large, dentigerous jaws, and Granulacanthus joenelsoni is based on isolated spines. The isolated remains of these species are similar in that they both possess pustulose denticles or tubercles, either on the mesial ridge (X. kenstewarti) or on the fin spines (G. joenelsoni). Jaws of X. kenstewarti are similar in size to those of Xylacanthus minutus, Ischnacanthus kingi, and I. wickhami and smaller than those of X. grandis. The jaws of X. kenstewarti are most similar to those of X. minutus, but are distinguished from this and other ischnacanthid species by a tapering patch of pustulose denticles that is widest midway along the jaw, mesial denticles that are simple blisterlike structures, the monocuspid, striated primary teeth that are subcircular in cross section, and a posterodorsal process that is enlarged. The spines of G. joenelsoni have distinctive tubercular ornamentation. Tubercles, or nodular ornaments on fin spines, are characteristic of primitive acanthodians, but the slender shape of the spines, the low number of spine ribs, and the fine striations posterior to the main ribs of each spine suggest that G. joenelsoni is a relatively advanced acanthodian. Xylacanthus kenstewarti and G. joenelsoni are from the Silurian (Wenlock or Ludlow) of the southern Mackenzie Mountains. Xylacanthus kenstewarti represents the earliest representative of the genus, the earliest unequivocal remains of a gnathostome from the Mackenzie Mountains, and extends the known geographical range of the genus from the Mackenzie Mountains east to Spitsbergen.
format Article in Journal/Newspaper
author Hanke, Gavin F
Wilson, Mark VH
Lindoe, L Allan
spellingShingle Hanke, Gavin F
Wilson, Mark VH
Lindoe, L Allan
New species of Silurian acanthodians from the Mackenzie Mountains, Canada
author_facet Hanke, Gavin F
Wilson, Mark VH
Lindoe, L Allan
author_sort Hanke, Gavin F
title New species of Silurian acanthodians from the Mackenzie Mountains, Canada
title_short New species of Silurian acanthodians from the Mackenzie Mountains, Canada
title_full New species of Silurian acanthodians from the Mackenzie Mountains, Canada
title_fullStr New species of Silurian acanthodians from the Mackenzie Mountains, Canada
title_full_unstemmed New species of Silurian acanthodians from the Mackenzie Mountains, Canada
title_sort new species of silurian acanthodians from the mackenzie mountains, canada
publisher Canadian Science Publishing
publishDate 2001
url http://dx.doi.org/10.1139/e01-039
http://www.nrcresearchpress.com/doi/pdf/10.1139/e01-039
genre Mackenzie mountains
Spitsbergen
genre_facet Mackenzie mountains
Spitsbergen
op_source Canadian Journal of Earth Sciences
volume 38, issue 11, page 1517-1529
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e01-039
container_title Canadian Journal of Earth Sciences
container_volume 38
container_issue 11
container_start_page 1517
op_container_end_page 1529
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