New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada

A new Early Triassic coelacanth, Belemnocerca prolata, gen. et sp. nov., is described as a new member of the family Laugiidae. Although only one incomplete specimen is known, much can be deduced about its evolutionary relationships. In particular, the new coelacanth is most similar to one member of...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Wendruff, Andrew J., Wilson, Mark V.H.
Other Authors: Sues, Hans
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2013
Subjects:
Online Access:http://dx.doi.org/10.1139/cjes-2013-0010
http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2013-0010
http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2013-0010
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spelling crcansciencepubl:10.1139/cjes-2013-0010 2023-12-17T10:30:59+01:00 New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada Wendruff, Andrew J. Wilson, Mark V.H. Sues, Hans 2013 http://dx.doi.org/10.1139/cjes-2013-0010 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2013-0010 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2013-0010 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 50, issue 9, page 904-910 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 2013 crcansciencepubl https://doi.org/10.1139/cjes-2013-0010 2023-11-19T13:38:15Z A new Early Triassic coelacanth, Belemnocerca prolata, gen. et sp. nov., is described as a new member of the family Laugiidae. Although only one incomplete specimen is known, much can be deduced about its evolutionary relationships. In particular, the new coelacanth is most similar to one member of its family, Laugia groenlandica, in the asymmetry (dorsal lobe longer than ventral) and the gradually tapering shape of its caudal fin, though it differs in caudal fin ray count and anal fin position as well as in the size and shape of the supplementary lobe. Belemnocerca prolata is the westernmost occurrence of the family Laugiidae and only member of this family known to inhabit Panthalassa, west of the supercontinent Pangaea. The family Laugiidae has a temporal range from the Early Triassic to the Late Jurassic, and its members have been described from both Greenland and Germany. Article in Journal/Newspaper Greenland Canadian Science Publishing (via Crossref) Canada Greenland British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canadian Journal of Earth Sciences 50 9 904 910
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Wendruff, Andrew J.
Wilson, Mark V.H.
New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
topic_facet General Earth and Planetary Sciences
description A new Early Triassic coelacanth, Belemnocerca prolata, gen. et sp. nov., is described as a new member of the family Laugiidae. Although only one incomplete specimen is known, much can be deduced about its evolutionary relationships. In particular, the new coelacanth is most similar to one member of its family, Laugia groenlandica, in the asymmetry (dorsal lobe longer than ventral) and the gradually tapering shape of its caudal fin, though it differs in caudal fin ray count and anal fin position as well as in the size and shape of the supplementary lobe. Belemnocerca prolata is the westernmost occurrence of the family Laugiidae and only member of this family known to inhabit Panthalassa, west of the supercontinent Pangaea. The family Laugiidae has a temporal range from the Early Triassic to the Late Jurassic, and its members have been described from both Greenland and Germany.
author2 Sues, Hans
format Article in Journal/Newspaper
author Wendruff, Andrew J.
Wilson, Mark V.H.
author_facet Wendruff, Andrew J.
Wilson, Mark V.H.
author_sort Wendruff, Andrew J.
title New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
title_short New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
title_full New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
title_fullStr New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
title_full_unstemmed New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada
title_sort new early triassic coelacanth in the family laugiidae (sarcopterygii: actinistia) from the sulphur mountain formation near wapiti lake, british columbia, canada
publisher Canadian Science Publishing
publishDate 2013
url http://dx.doi.org/10.1139/cjes-2013-0010
http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2013-0010
http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2013-0010
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
geographic Canada
Greenland
British Columbia
geographic_facet Canada
Greenland
British Columbia
genre Greenland
genre_facet Greenland
op_source Canadian Journal of Earth Sciences
volume 50, issue 9, page 904-910
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/cjes-2013-0010
container_title Canadian Journal of Earth Sciences
container_volume 50
container_issue 9
container_start_page 904
op_container_end_page 910
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