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Evolution of Old World Equus and origin of the zebra-ass clade
Evolution of the genus Equus has been a matter of long debate with a multitude of hypotheses. Currently, there is no consensus on either the taxonomic content nor phylogeny of Equus. Some hypotheses segregate Equus species into three genera, Plesippus, Allohippus and Equus. Also, the evolutionary ro...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2021
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8114910/ https://www.ncbi.nlm.nih.gov/pubmed/33980921 http://dx.doi.org/10.1038/s41598-021-89440-9 |
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author | Cirilli, Omar Pandolfi, Luca Rook, Lorenzo Bernor, Raymond L. |
author_facet | Cirilli, Omar Pandolfi, Luca Rook, Lorenzo Bernor, Raymond L. |
author_sort | Cirilli, Omar |
collection | PubMed |
description | Evolution of the genus Equus has been a matter of long debate with a multitude of hypotheses. Currently, there is no consensus on either the taxonomic content nor phylogeny of Equus. Some hypotheses segregate Equus species into three genera, Plesippus, Allohippus and Equus. Also, the evolutionary role of European Pleistocene Equus stenonis in the origin of the zebra-ass clade has been debated. Studies based on skull, mandible and dental morphology suggest an evolutionary relationship between North American Pliocene E. simplicidens and European and African Pleistocene Equus. In this contribution, we assess the validity of the genera Plesippus, Allohippus and Equus by cladistic analysis combined with morphological and morphometrical comparison of cranial anatomy. Our cladistic analysis, based on cranial and postcranial elements (30 taxa, 129 characters), supports the monophyly of Equus, denies the recognition of Plesippus and Allohippus and supports the derivation of Equus grevyi and members of the zebra-ass clade from European stenonine horses. We define the following evolutionary steps directly relevant to the phylogeny of extant zebras and asses: E. simplicidens–E. stenonis–E. koobiforensis–E. grevyi -zebra-ass clade. The North American Pliocene species Equus simplicidens represents the ancestral stock of Old World Pleistocene Equus and the zebra-ass clade. Our phylogenetic results uphold the most recent genomic outputs which indicate an age of 4.0–4.5 Ma for the origin and monophyly of Equus. |
format | Online Article Text |
id | pubmed-8114910 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-81149102021-05-12 Evolution of Old World Equus and origin of the zebra-ass clade Cirilli, Omar Pandolfi, Luca Rook, Lorenzo Bernor, Raymond L. Sci Rep Article Evolution of the genus Equus has been a matter of long debate with a multitude of hypotheses. Currently, there is no consensus on either the taxonomic content nor phylogeny of Equus. Some hypotheses segregate Equus species into three genera, Plesippus, Allohippus and Equus. Also, the evolutionary role of European Pleistocene Equus stenonis in the origin of the zebra-ass clade has been debated. Studies based on skull, mandible and dental morphology suggest an evolutionary relationship between North American Pliocene E. simplicidens and European and African Pleistocene Equus. In this contribution, we assess the validity of the genera Plesippus, Allohippus and Equus by cladistic analysis combined with morphological and morphometrical comparison of cranial anatomy. Our cladistic analysis, based on cranial and postcranial elements (30 taxa, 129 characters), supports the monophyly of Equus, denies the recognition of Plesippus and Allohippus and supports the derivation of Equus grevyi and members of the zebra-ass clade from European stenonine horses. We define the following evolutionary steps directly relevant to the phylogeny of extant zebras and asses: E. simplicidens–E. stenonis–E. koobiforensis–E. grevyi -zebra-ass clade. The North American Pliocene species Equus simplicidens represents the ancestral stock of Old World Pleistocene Equus and the zebra-ass clade. Our phylogenetic results uphold the most recent genomic outputs which indicate an age of 4.0–4.5 Ma for the origin and monophyly of Equus. Nature Publishing Group UK 2021-05-12 /pmc/articles/PMC8114910/ /pubmed/33980921 http://dx.doi.org/10.1038/s41598-021-89440-9 Text en © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Cirilli, Omar Pandolfi, Luca Rook, Lorenzo Bernor, Raymond L. Evolution of Old World Equus and origin of the zebra-ass clade |
title | Evolution of Old World Equus and origin of the zebra-ass clade |
title_full | Evolution of Old World Equus and origin of the zebra-ass clade |
title_fullStr | Evolution of Old World Equus and origin of the zebra-ass clade |
title_full_unstemmed | Evolution of Old World Equus and origin of the zebra-ass clade |
title_short | Evolution of Old World Equus and origin of the zebra-ass clade |
title_sort | evolution of old world equus and origin of the zebra-ass clade |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8114910/ https://www.ncbi.nlm.nih.gov/pubmed/33980921 http://dx.doi.org/10.1038/s41598-021-89440-9 |
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