A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern

A new genus and species of lydekkerinid amphibian, Eolydekkerina magna , is described from the lower part of the Lystrosaurus Assemblage Zone of South Africa. Most distinctions between Eolydekkerina and Lydekkerina (other than those related to width of interorbital area and structure of choana and s...

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Published in:Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 1996
Subjects:
Online Access:http://dx.doi.org/10.1098/rstb.1996.0147
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1996.0147
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spelling crroyalsociety:10.1098/rstb.1996.0147 2024-09-15T17:46:44+00:00 A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern 1996 http://dx.doi.org/10.1098/rstb.1996.0147 https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1996.0147 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences volume 351, issue 1347, page 1635-1659 ISSN 0962-8436 1471-2970 journal-article 1996 crroyalsociety https://doi.org/10.1098/rstb.1996.0147 2024-07-29T04:23:16Z A new genus and species of lydekkerinid amphibian, Eolydekkerina magna , is described from the lower part of the Lystrosaurus Assemblage Zone of South Africa. Most distinctions between Eolydekkerina and Lydekkerina (other than those related to width of interorbital area and structure of choana and squamosal occipital flange) are linked to late growth stages and particularly preorbital elongation of the skull in the former genus. The developmental trends in Lydekkerina and the Lydekkerinidae in general are analysed by comparison with the cranial pattern of juvenile rhinesuchids. The evidence suggests that the Lydekkerinidae evolved from more fully developed capitosauroid (rhinesuchid-like) ancestors by gradual truncation of ontogeny in parallel with the acquisition of many advanced features, unknown in the Permian capitosauroids. The composition of the Lydekkerinidae is reviewed, and it is suggested that the family includes six to seven valid genera known from Antarctica, Greenland, India, Russia, South Africa and Tasmania. The smaller, and obviously most paedomorphic forms come from the reptile-dominated assemblages in which Lystrosaurus is abundant, whereas the larger ones belong to amphibian-dominated assemblages. Article in Journal/Newspaper Antarc* Antarctica Greenland The Royal Society Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 351 1347 1635 1659
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description A new genus and species of lydekkerinid amphibian, Eolydekkerina magna , is described from the lower part of the Lystrosaurus Assemblage Zone of South Africa. Most distinctions between Eolydekkerina and Lydekkerina (other than those related to width of interorbital area and structure of choana and squamosal occipital flange) are linked to late growth stages and particularly preorbital elongation of the skull in the former genus. The developmental trends in Lydekkerina and the Lydekkerinidae in general are analysed by comparison with the cranial pattern of juvenile rhinesuchids. The evidence suggests that the Lydekkerinidae evolved from more fully developed capitosauroid (rhinesuchid-like) ancestors by gradual truncation of ontogeny in parallel with the acquisition of many advanced features, unknown in the Permian capitosauroids. The composition of the Lydekkerinidae is reviewed, and it is suggested that the family includes six to seven valid genera known from Antarctica, Greenland, India, Russia, South Africa and Tasmania. The smaller, and obviously most paedomorphic forms come from the reptile-dominated assemblages in which Lystrosaurus is abundant, whereas the larger ones belong to amphibian-dominated assemblages.
format Article in Journal/Newspaper
title A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
spellingShingle A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
title_short A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
title_full A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
title_fullStr A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
title_full_unstemmed A new lydekkerinid (Amphibia, Temnospondyli) fro the lower Triassic of South Africa: implications for evolution of the early capitosauroid cranial pattern
title_sort new lydekkerinid (amphibia, temnospondyli) fro the lower triassic of south africa: implications for evolution of the early capitosauroid cranial pattern
publisher The Royal Society
publishDate 1996
url http://dx.doi.org/10.1098/rstb.1996.0147
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1996.0147
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
volume 351, issue 1347, page 1635-1659
ISSN 0962-8436 1471-2970
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rstb.1996.0147
container_title Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
container_volume 351
container_issue 1347
container_start_page 1635
op_container_end_page 1659
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