A trematosauroid temnospondyl from the Middle Triassic of Jordan

A well-preserved mandible from the Lower Anisian Mukheiris Formation from near the Dead Sea (Jordan) proves the presence of tetrapods in the region. It is identified as a stereospondyl lower jaw sharing synapomorphies with the Trematosauroidea. It has the following combination of features: (1) Mecke...

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Main Author: R. R. Schoch
Format: Article
Language:English
Published: Copernicus Publications 2011-08-01
Series:Fossil Record
Online Access:http://www.foss-rec.net/14/119/2011/fr-14-119-2011.pdf
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spelling doaj-76cab907681e4925b42c55408643d7652020-11-24T22:57:05ZengCopernicus PublicationsFossil Record2193-00662193-00742011-08-0114211912710.5194/fr-14-119-2011A trematosauroid temnospondyl from the Middle Triassic of JordanR. R. Schoch0Staatliches Museum für Naturkunde Stuttgart, Rosenstein 1, 70191 Stuttgart, GermanyA well-preserved mandible from the Lower Anisian Mukheiris Formation from near the Dead Sea (Jordan) proves the presence of tetrapods in the region. It is identified as a stereospondyl lower jaw sharing synapomorphies with the Trematosauroidea. It has the following combination of features: (1) Meckelian fenestra almost one-third the length of the ramus, (2) postglenoid area posterodorsally rising and robust, as long as glenoid facet, (3) preglenoid process substantially higher than medial margin of adductor chamber, (4) all teeth anteriorly and posteriorly carinate, and (5) symphysis without additional tooth rows, with a pair of unequal fangs as part of the dentary arcade, which contains unusually large teeth. The Jordan specimen shares most character-states with South African <i>Microposaurus</i> (size of teeth, bicarinate structure) and the Russian <i>Inflectosaurus</i> (preglenoid process, PGA). Phylogenetic analysis finds it to nest with <i>Microposaurus</i>, whereas <i>Inflectosaurus</i> forms an unresolved polytomy with other trematosauroids. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.201100002" target="_blank">10.1002/mmng.201100002</a>http://www.foss-rec.net/14/119/2011/fr-14-119-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. R. Schoch
spellingShingle R. R. Schoch
A trematosauroid temnospondyl from the Middle Triassic of Jordan
Fossil Record
author_facet R. R. Schoch
author_sort R. R. Schoch
title A trematosauroid temnospondyl from the Middle Triassic of Jordan
title_short A trematosauroid temnospondyl from the Middle Triassic of Jordan
title_full A trematosauroid temnospondyl from the Middle Triassic of Jordan
title_fullStr A trematosauroid temnospondyl from the Middle Triassic of Jordan
title_full_unstemmed A trematosauroid temnospondyl from the Middle Triassic of Jordan
title_sort trematosauroid temnospondyl from the middle triassic of jordan
publisher Copernicus Publications
series Fossil Record
issn 2193-0066
2193-0074
publishDate 2011-08-01
description A well-preserved mandible from the Lower Anisian Mukheiris Formation from near the Dead Sea (Jordan) proves the presence of tetrapods in the region. It is identified as a stereospondyl lower jaw sharing synapomorphies with the Trematosauroidea. It has the following combination of features: (1) Meckelian fenestra almost one-third the length of the ramus, (2) postglenoid area posterodorsally rising and robust, as long as glenoid facet, (3) preglenoid process substantially higher than medial margin of adductor chamber, (4) all teeth anteriorly and posteriorly carinate, and (5) symphysis without additional tooth rows, with a pair of unequal fangs as part of the dentary arcade, which contains unusually large teeth. The Jordan specimen shares most character-states with South African <i>Microposaurus</i> (size of teeth, bicarinate structure) and the Russian <i>Inflectosaurus</i> (preglenoid process, PGA). Phylogenetic analysis finds it to nest with <i>Microposaurus</i>, whereas <i>Inflectosaurus</i> forms an unresolved polytomy with other trematosauroids. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.201100002" target="_blank">10.1002/mmng.201100002</a>
url http://www.foss-rec.net/14/119/2011/fr-14-119-2011.pdf
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