2023
DOI: 10.1016/j.jsames.2022.104163
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New records of Theropoda from a Late Cretaceous (Campanian-Maastrichtian) locality in the Magallanes-Austral Basin, Patagonia, and insights into end Cretaceous theropod diversity

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Cited by 7 publications
(5 citation statements)
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References 103 publications
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“…So far, and as previously noted in the literature, megaraptoridsynapomorphies are limited but are highly diagnostic [17,41]. In the speci c context of this study, two out of three analyses suggest that Morphotype 1 lacks strong a nities with the Megaraptoridae subclade.…”
Section: Cladistics and Multivariate Analysessupporting
confidence: 79%
“…So far, and as previously noted in the literature, megaraptoridsynapomorphies are limited but are highly diagnostic [17,41]. In the speci c context of this study, two out of three analyses suggest that Morphotype 1 lacks strong a nities with the Megaraptoridae subclade.…”
Section: Cladistics and Multivariate Analysessupporting
confidence: 79%
“…So far, and as previously noted in the literature, megaraptorid synapomorphies are limited but are highly diagnostic [19,44]. In the specific context of this study, two out of three analyses suggest that Morphotype 1 lacks strong affinities with the Megaraptoridae subclade.…”
Section: Cladistics and Multivariate Analysessupporting
confidence: 77%
“…Late Cretaceous faunas from Indomadagascar are better documented, where the absence of duck-billed dinosaurs is more compelling in suggesting these may have never arrived into particularly isolated regions of Gondwana. Additional discoveries from underexplored regions in the global south will continue to uncover important information on the similarities and differences among pre-extinction ecosystems of the world and whether they can be related to patterns of extinction upon the K-Pg asteroid impact ( 73 ).…”
Section: Discussionmentioning
confidence: 99%
“…The Dorotea Formation mainly comprises greenish gray and reddish brown sandstones with abundant conglomerate and siltstone lenses, thin beds of sandy calcareous concretions, and mudstones of 900 to 1200 m thickness ( 79 ). Along the succession, there are fossil-bearing levels with bivalves, ammonites, gastropods, sharks, plesiosaurs, mosasaurs, frogs, turtles, dinosaurs, mammals, fossil wood, and leaves ( 22 , 66 , 73 , 79 , 80 ).…”
Section: Methodsmentioning
confidence: 99%