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- W2034247742 endingPage "e42135" @default.
- W2034247742 startingPage "e42135" @default.
- W2034247742 abstract "Prior studies of Mesozoic biodiversity document a diversity peak for dinosaur species in the Campanian stage of the Late Cretaceous, yet have failed to provide explicit causal mechanisms. We provide evidence that a marked increase in North American dinosaur biodiversity can be attributed to dynamic orogenic episodes within the Western Interior Basin (WIB). Detailed fossil occurrences document an association between the shift from Sevier-style, latitudinally arrayed basins to smaller Laramide-style, longitudinally arrayed basins and a well substantiated decreased geographic range/increased taxonomic diversity of megaherbivorous dinosaur species. Dispersal-vicariance analysis demonstrates that the nearly identical biogeographic histories of the megaherbivorous dinosaur clades Ceratopsidae and Hadrosauridae are attributable to rapid diversification events within restricted basins and that isolation events are contemporaneous with known tectonic activity in the region. SymmeTREE analysis indicates that megaherbivorous dinosaur clades exhibited significant variation in diversification rates throughout the Late Cretaceous. Phylogenetic divergence estimates of fossil clades offer a new lower boundary on Laramide surficial deformation that precedes estimates based on sedimentological data alone." @default.
- W2034247742 created "2016-06-24" @default.
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- W2034247742 creator A5055285748 @default.
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- W2034247742 date "2012-08-02" @default.
- W2034247742 modified "2023-10-12" @default.
- W2034247742 title "Mountain Building Triggered Late Cretaceous North American Megaherbivore Dinosaur Radiation" @default.
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- W2034247742 doi "https://doi.org/10.1371/journal.pone.0042135" @default.
- W2034247742 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/3410882" @default.
- W2034247742 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/22876302" @default.
- W2034247742 hasPublicationYear "2012" @default.
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