Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica

Temnospondyl amphibians are common in non-marine Triassic assemblages, including in the Fremouw Formation (Lower to Middle Triassic) of Antarctica. Temnospondyls were among the first tetrapods to be collected from Antarctica, but their record from the lower Fremouw Formation has long been tenuous. O...

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Published in:Journal of Paleontology
Main Authors: Bryan M. Gee, Peter J. Makovicky, Christian A. Sidor
Format: Text
Language:English
Published: The Paleontological Society 2022
Subjects:
Online Access:https://doi.org/10.1017/jpa.2021.115
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spelling ftbioone:10.1017/jpa.2021.115 2024-06-02T07:58:38+00:00 Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica Bryan M. Gee Peter J. Makovicky Christian A. Sidor Bryan M. Gee Peter J. Makovicky Christian A. Sidor world 2022-06-06 text/HTML https://doi.org/10.1017/jpa.2021.115 en eng The Paleontological Society doi:10.1017/jpa.2021.115 All rights reserved. https://doi.org/10.1017/jpa.2021.115 Text 2022 ftbioone https://doi.org/10.1017/jpa.2021.115 2024-05-07T00:48:07Z Temnospondyl amphibians are common in non-marine Triassic assemblages, including in the Fremouw Formation (Lower to Middle Triassic) of Antarctica. Temnospondyls were among the first tetrapods to be collected from Antarctica, but their record from the lower Fremouw Formation has long been tenuous. One taxon, ‘Austrobrachyops jenseni,’ is represented by a type specimen comprising only a partial pterygoid, which is now thought to belong to a dicynodont. A second taxon, ‘Cryobatrachus kitchingi,’ is represented by a type specimen comprising a nearly complete skull, but the specimen is only exposed ventrally, and uncertainty over its ontogenetic maturity and some aspects of its anatomy has led it to be designated as a nomen dubium by previous workers. Here, we redescribe the holotype of ‘C. kitchingi,’ an undertaking that is augmented by tomographic analysis. Most of the original interpretations and reconstructions cannot be substantiated, and some are clearly erroneous. Although originally classified as a lydekkerinid, the purported lydekkerinid characteristics are shown to be unfounded or no longer diagnostic for the family. We instead identify numerous features shared with highly immature capitosaurs, a large-bodied clade documented in the upper Fremouw Formation of Antarctica and elsewhere in the Lower Triassic. Additionally, we describe a newly collected partial skull from the lower Fremouw Formation that represents a relatively mature, small-bodied individual, which we provisionally refer to Lydekkerinidae; this specimen represents the most confident identification of a lydekkerinid from Antarctica to date. Text Antarc* Antarctica BioOne Online Journals Journal of Paleontology 96 3 658 683
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description Temnospondyl amphibians are common in non-marine Triassic assemblages, including in the Fremouw Formation (Lower to Middle Triassic) of Antarctica. Temnospondyls were among the first tetrapods to be collected from Antarctica, but their record from the lower Fremouw Formation has long been tenuous. One taxon, ‘Austrobrachyops jenseni,’ is represented by a type specimen comprising only a partial pterygoid, which is now thought to belong to a dicynodont. A second taxon, ‘Cryobatrachus kitchingi,’ is represented by a type specimen comprising a nearly complete skull, but the specimen is only exposed ventrally, and uncertainty over its ontogenetic maturity and some aspects of its anatomy has led it to be designated as a nomen dubium by previous workers. Here, we redescribe the holotype of ‘C. kitchingi,’ an undertaking that is augmented by tomographic analysis. Most of the original interpretations and reconstructions cannot be substantiated, and some are clearly erroneous. Although originally classified as a lydekkerinid, the purported lydekkerinid characteristics are shown to be unfounded or no longer diagnostic for the family. We instead identify numerous features shared with highly immature capitosaurs, a large-bodied clade documented in the upper Fremouw Formation of Antarctica and elsewhere in the Lower Triassic. Additionally, we describe a newly collected partial skull from the lower Fremouw Formation that represents a relatively mature, small-bodied individual, which we provisionally refer to Lydekkerinidae; this specimen represents the most confident identification of a lydekkerinid from Antarctica to date.
author2 Bryan M. Gee
Peter J. Makovicky
Christian A. Sidor
format Text
author Bryan M. Gee
Peter J. Makovicky
Christian A. Sidor
spellingShingle Bryan M. Gee
Peter J. Makovicky
Christian A. Sidor
Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
author_facet Bryan M. Gee
Peter J. Makovicky
Christian A. Sidor
author_sort Bryan M. Gee
title Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
title_short Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
title_full Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
title_fullStr Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
title_full_unstemmed Upside down: ‘Cryobatrachus’ and the lydekkerinid record from Antarctica
title_sort upside down: ‘cryobatrachus’ and the lydekkerinid record from antarctica
publisher The Paleontological Society
publishDate 2022
url https://doi.org/10.1017/jpa.2021.115
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op_rights All rights reserved.
op_doi https://doi.org/10.1017/jpa.2021.115
container_title Journal of Paleontology
container_volume 96
container_issue 3
container_start_page 658
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