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Early Miocene remains of Melissiodon from Mokrá-Quarry (Moravia, Czech Republic) shed light on the evolutionary history of the rare cricetid genus
Bonilla Salomón, Isaac (Comenius University in Bratislava. Department of Geology and Paleontology)
Čermák, Stanislav (Czech Academy of Sciences. Institute of Geology)
Hernández Luján, Àngel (Institut Català de Paleontologia Miquel Crusafont)
Jovells Vaqué, Sílvia (Institut Català de Paleontologia Miquel Crusafont)
Ivanov, Martin (Masaryk University. Department of Geological Sciences)
Sabol, Martin (Comenius University in Bratislava. Department of Geology and Paleontology)

Fecha: 2022
Resumen: Background: Melissiodon is a rare cricetid genus endemic to Europe, known from the Early Oligoceneto the Early Miocene. It is usually a very rare find, and even in the few localities where Melissiodon remains are found, those are scarce and fragmentary. Only a few Central European localities have yielded rich remains of the genus. Currently, two species are known from the Early Miocene: Melissiodon schlosseri, which is based on two teeth from the MN2 German locality of Haslach and only found in two other sites of similar age (Ulm-Uniklinik and La Chaux, from Germany and Switzerland respectively); and Melissiodon dominans, found in MN3 and MN4 localities across Europe, even though the scarce and fragmentary remains make some of these attributions dubious. For that reason, Melissiodon dominans has become a catch-all species. However, Mokrá-Quarry represents one of the best documented findings of Melissiodon remains from MN4 localities of Europe. Methods: The Melissiodon assemblage from Mokrá-Quarry has been studied thoroughly, providing metrics and detailed descriptions of all teeth positions, as well as complete comparisons with other MN3 and MN4 localities bearing Melissiodon remains. Results: In this work, new remains of Melissiodon have been identified as a new morphotype that clearly differs from Melissiodon dominans by its unique m1 morphology but still shows some resemblance with Melissiodon schlosseri. Based on that, we here propose the hypothesis of an evolutionary lineage starting from Melissiodon schlosseri, diverging from the lineage leading towards Melissiodon dominans. With this finding, there are at least two different taxa of Melissiodon known during the Early Miocene, prior to the genus extinction. This study arises the certainty that the evolution history of the genus is more complex than previously thought and that more studies are necessary to elucidate it, including a complete revision of the type material of Melissiodon dominans and Melissiodon schlosseri in the light of current knowledge of the genus, which will help to elucidate the attribution of the populations from Mokrá-Quarry. For the time being, the assemblage presented here is referred as Melissiodon aff. schlosseri.
Ayudas: Agencia Estatal de Investigación PID2020-117289GB-I00
Agència de Gestió d'Ajuts Universitaris i de Recerca 2017/SGR-116
Agència de Gestió d'Ajuts Universitaris i de Recerca 2019/BP-00154
Nota: Altres ajuts: CERCA Programme/Generalitat de Catalunya
Derechos: Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, fins i tot amb finalitats comercials, sempre i quan es reconegui l'autoria de l'obra original. Creative Commons
Lengua: Anglès
Documento: Article ; recerca ; Versió publicada
Materia: Melissiodontinae ; Melissiodon schlosseri ; Melissiodon dominans ; Burdigalian ; Carpathian Foredeep Basin ; Moravian Karst
Publicado en: PeerJ, Vol. 10 (August 2022) , art. e13820, ISSN 2167-8359

DOI: 10.7717/peerj.13820
PMID: 35966921


26 p, 9.4 MB

El registro aparece en las colecciones:
Documentos de investigación > Documentos de los grupos de investigación de la UAB > Centros y grupos de investigación (producción científica) > Ciencias > Institut Català de Paleontologia Miquel Crusafont (ICP)
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 Registro creado el 2023-02-17, última modificación el 2023-03-15



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