A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin

A dermal bone from the late Famennian of Ketleri in Latvia, identified as a probable tetrapod postorbital by Oleg Lebedev and stored in the Museum für Naturkunde Berlin, is described in detail. Its tetrapod status is confirmed based on the dermal sculpture consisting of polygonal pits and radially a...

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Main Author: F. Witzmann
Format: Article
Language:English
Published: Copernicus Publications 2010-08-01
Series:Fossil Record
Online Access:http://www.foss-rec.net/13/297/2010/fr-13-297-2010.pdf
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spelling doaj-7b6bc5639282415e925707bad2e623e62020-11-24T20:52:39ZengCopernicus PublicationsFossil Record2193-00662193-00742010-08-0113229730210.5194/fr-13-297-2010A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde BerlinF. Witzmann0Museum für Naturkunde Berlin, Invalidenstraße 43, 10115 Berlin, GermanyA dermal bone from the late Famennian of Ketleri in Latvia, identified as a probable tetrapod postorbital by Oleg Lebedev and stored in the Museum für Naturkunde Berlin, is described in detail. Its tetrapod status is confirmed based on the dermal sculpture consisting of polygonal pits and radially aligned ridges and furrows. The sculpture resembles that of Devonian tetrapods but is nevertheless not as regular as in most post-Devonian forms. The bone can be designated as a postorbital because of its concave anterior margin, the lateral line that shows no bifurcation, and the ossification centre that is located in the dorsal portion of the bone. The lateral line (i.e., the postorbital branch of the infraorbital line) forms an open, deep sulcus in the ventral portion of the postorbital but is enclosed within the bone in the dorsal portion and opens through pores to the surface. This morphology of the postorbital branch is unique among basal tetrapods. The bone might belong to the tetrapod <i>Ventastega curonica</i> Ahlberg et al., 1994 that is known from the same strata at Ketleri, however, since the postorbital is unknown in this taxon, this cannot be stated with certainty. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.201000002" target="_blank">10.1002/mmng.201000002</a>http://www.foss-rec.net/13/297/2010/fr-13-297-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Witzmann
spellingShingle F. Witzmann
A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
Fossil Record
author_facet F. Witzmann
author_sort F. Witzmann
title A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
title_short A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
title_full A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
title_fullStr A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
title_full_unstemmed A skull fragment of a Devonian tetrapod with a unique lateral line morphology in the collection of the Museum für Naturkunde Berlin
title_sort skull fragment of a devonian tetrapod with a unique lateral line morphology in the collection of the museum für naturkunde berlin
publisher Copernicus Publications
series Fossil Record
issn 2193-0066
2193-0074
publishDate 2010-08-01
description A dermal bone from the late Famennian of Ketleri in Latvia, identified as a probable tetrapod postorbital by Oleg Lebedev and stored in the Museum für Naturkunde Berlin, is described in detail. Its tetrapod status is confirmed based on the dermal sculpture consisting of polygonal pits and radially aligned ridges and furrows. The sculpture resembles that of Devonian tetrapods but is nevertheless not as regular as in most post-Devonian forms. The bone can be designated as a postorbital because of its concave anterior margin, the lateral line that shows no bifurcation, and the ossification centre that is located in the dorsal portion of the bone. The lateral line (i.e., the postorbital branch of the infraorbital line) forms an open, deep sulcus in the ventral portion of the postorbital but is enclosed within the bone in the dorsal portion and opens through pores to the surface. This morphology of the postorbital branch is unique among basal tetrapods. The bone might belong to the tetrapod <i>Ventastega curonica</i> Ahlberg et al., 1994 that is known from the same strata at Ketleri, however, since the postorbital is unknown in this taxon, this cannot be stated with certainty. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.201000002" target="_blank">10.1002/mmng.201000002</a>
url http://www.foss-rec.net/13/297/2010/fr-13-297-2010.pdf
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