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The oldest higher true crabs (Crustacea: Decapoda: Brachyura): insights from the Early Cretaceous of the Americas

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dc.contributor.author Luque, Javier en
dc.date.accessioned 2015-04-17T18:36:53Z
dc.date.available 2015-04-17T18:36:53Z
dc.date.issued 2015
dc.identifier.citation Luque, Javier. 2015. "<a href="https://repository.si.edu/handle/10088/25048">The oldest higher true crabs (Crustacea: Decapoda: Brachyura): insights from the Early Cretaceous of the Americas</a>." <em>Palaeontology</em>. 58 (2):251&ndash;263. <a href="https://doi.org/10.1111/pala.12135">https://doi.org/10.1111/pala.12135</a> en
dc.identifier.issn 1475-4983
dc.identifier.uri http://hdl.handle.net/10088/25048
dc.description.abstract Despite the extensive fossil record of higher crabs (Eubrachyura) from Late Cretaceous and Cenozoic rocks worldwide, their Early Cretaceous occurrences are scarce and fragmentary, obscuring our understanding of their early evolution. Until now, representatives of only two families of eubrachyuran-like crabs were known from the Early Cretaceous: Componocancridae and Tepexicarcinidae fam. nov., both monospecific lineages from the Albian (~110–100 Ma) of North and Central America, respectively. The discovery of Telamonocarcinus antiquus sp. nov. (Telamonocarcinidae) from the early Albian of Colombia, South America (~110 Ma), increases to three the number of known Early Cretaceous eubrachyuran-like families. The ages and geographical distributions of the oldest eubrachyuran-like taxa (i.e. Componocancridae, Telamonocarcinidae and Tepexicarcinidae fam. nov.) suggest that the oldest higher true crabs might have originated in the Americas; that they were already morphologically diverse by the late Early Cretaceous; and that their most recent common ancestor must be rooted in the Early Cretaceous, or even the Late Jurassic. en
dc.relation.ispartof Palaeontology en
dc.title The oldest higher true crabs (Crustacea: Decapoda: Brachyura): insights from the Early Cretaceous of the Americas en
dc.type Journal Article en
dc.identifier.srbnumber 131020
dc.identifier.doi 10.1111/pala.12135
rft.jtitle Palaeontology
rft.volume 58
rft.issue 2
rft.spage 251
rft.epage 263
dc.description.SIUnit STRI en
dc.citation.spage 251
dc.citation.epage 263


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