treatments-rdf/data/4D/66/AD/4D66AD09FFBFD37A97B2FB62FBC148AC.ttl

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dc:creator "Halffter, Gonzalo; Zunino, Mario; Moctezuma, Victor; Sánchez-Huerta, José L." ;
dc:title "Onthophagus chevrolati Harold 1869" ;
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bibo:endPage "34" ;
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bibo:journal "Zootaxa" ;
bibo:pubDate "2019-04-16" ;
bibo:startPage "1" ;
bibo:volume "4586" ;
dc:creator "Halffter, Gonzalo; Zunino, Mario; Moctezuma, Victor; Sánchez-Huerta, José L." ;
dc:date "2019" ;
dc:title "The integration processes of the distributional patterns in the Mexican Transition Zone: Phyletic, paleogeographic and ecological factors of a case study" ;
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dc:description "FIGURE 9. Main orographic formations of Mexico. Original map prepared by Violeta Halffter and used on many occasions in the biogeographic studies of the Mexican Transition Zone. I, Sierra Madre Occidental; II, Sierra Madre Oriental; III, Mexican Plateau; IV, Trans-Mexican Volcanic Belt; V, Balsas Basin; VI, Sierra Madre del Sur; VII, Sierra Madre de Chiapas; VIII, Chiapas Highlands; IX, Guatemalan Plateau; X, Central American Nucleous." ;
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<http://dx.doi.org/10.5281/zenodo.2642588>
dc:description "FIGURE 8. Onthophagus mesoamericanus, male holotype dorsal view, currently a synonym of O. cyanellus." ;
fabio:hasRepresentation <https://zenodo.org/record/2642588/files/figure.png> ;
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<http://dx.doi.org/10.5281/zenodo.2642594>
dc:description "FIGURE 11. Graphic hypothesis of the phyletic diversification and relationships of the O. chevrolati species group in the Mexican Transition Zone. Tip names are the species complexes. The figure elucidates our ideas of the taxonomical relationships and evolution of this species group based on the male and female genitalia, external morphology and geographic distribution: 1. The ancestral line of the O. chevrolati species group must have arrived in what is now Mexico between the Eocene and the Miocene, as part of the most ancient fauna of northern origin. The ancestor of O. vespertilio early separated from the ancestral trunk (plesiomorphic genitalia characters). 2. The ancestral species of the O. hippopotamus species line and of the O. hippopotamus species complex dispersed throughout the Trans-Mexican Volcanic Belt prior to its current conformation (Miocene to Pliocene). The geomorphological evolution of this mountain system drived the processes of speciation in this complex. Its descendants adapted to the burrows of Geomyidae in the mountains. 3. Separation of the O. hippopotamus and O. brevifrons species complexes. The first evolved with the TMVB, with some expansion southwards and northwards (O. coproides reaching New Mexico and Arizona). The brevifrons species complex is found in the southeastern United States of America and north-northeastern Mexico. Both complexes are found in the mountains and associated with the protected environments of rodent nests: Geomyidae in the case of the O. hippopotamus and Neotoma species complexes, plus three species in caves in the case of the O. brevifrons species complex." ;
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