The long trail: A chimera-like fossil crustacean interpreted as decapoda, stomatopoda, amphipoda and finally isopoda

dc.contributor.authorPAZINATO, PAULA G.
dc.contributor.authorHAUG, CAROLIN
dc.contributor.authorROHN, ROSEMARIE [UNESP]
dc.contributor.authorADAMI-RODRIGUES, KAREN
dc.contributor.authorGHILARDI, RENATO PIRANI [UNESP]
dc.contributor.authorLANGER, MAX CARDOSO
dc.contributor.authorHAUG, JOACHIM T.
dc.contributor.institutionLMU Munchen
dc.contributor.institutionGeoBio-Center der LMU Munchen
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionUniversidade Federal de Pernambuco (UFPE)
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.date.accessioned2022-05-01T08:44:39Z
dc.date.available2022-05-01T08:44:39Z
dc.date.issued2021-07-01
dc.description.abstractThe process of interpreting and evaluating a fossil is a difficult task. Isopoda is a species-rich group of peracarid eumalacostracans which represent quite a challenge when found as fossils, independent of whether we are working with fragmentary or more complete specimens. Here we describe a new fossil species of crustacean, Platuropodus odysseus n. gen. n. sp., from the Irati Formation, Permian of Paraná Basin, Brazil. After misinterpretations, the fossil taxon is recognised here as a representative of Isopoda. The new species presents characters found in Phreatoicidea, Asellota and Oniscidea in a unique combination for the fossil and extant record, such as two pairs of sub-chelate anterior trunk appendages, a short region after the anus and flat uropods. This chimera-like morphology and a morphometric analysis of the sub-chelae indicate convergent evolution in the early diversification of Isopoda. The morphological diversification present in the Palaeozoic and Mesozoic fossil record of Eumalacostraca indicate a push of the past effect in different ingroups of Peracarida.en
dc.description.affiliationDepartment Biologie II LMU Munchen, Biozentrum, Großhaderner Str. 2
dc.description.affiliationGeoBio-Center der LMU Munchen, Richard-Wagner-Str. 10
dc.description.affiliationGeosciences Institute UNESP, Av. 24 A 1515
dc.description.affiliationUFPel, Praça Domingos Rodrigues 02
dc.description.affiliationSciences Faculty UNESP, Av. Eng. Luiz Edmundo Carrijo Coube 14-01
dc.description.affiliationFLCCL USP, Av. Bandeirantes 3900
dc.description.affiliationUnespGeosciences Institute UNESP, Av. 24 A 1515
dc.description.affiliationUnespSciences Faculty UNESP, Av. Eng. Luiz Edmundo Carrijo Coube 14-01
dc.format.extent211-229
dc.identifierhttp://dx.doi.org/10.13130/2039-4942/15699
dc.identifier.citationRivista Italiana di Paleontologia e Stratigrafia, v. 127, n. 2, p. 211-229, 2021.
dc.identifier.doi10.13130/2039-4942/15699
dc.identifier.issn2039-4942
dc.identifier.issn0035-6883
dc.identifier.scopus2-s2.0-85113355963
dc.identifier.urihttp://hdl.handle.net/11449/233431
dc.language.isoeng
dc.relation.ispartofRivista Italiana di Paleontologia e Stratigrafia
dc.sourceScopus
dc.subjectconvergent evolution
dc.subjectIsopoda
dc.subjectmorphometric analysis
dc.subjectParaná Basin
dc.subjectPeracarida
dc.subjectPermian
dc.titleThe long trail: A chimera-like fossil crustacean interpreted as decapoda, stomatopoda, amphipoda and finally isopodaen
dc.typeArtigo
unesp.departmentCiências Biológicas - FCpt

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