2016
DOI: 10.1016/j.cretres.2015.07.003
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Diversity and faunal changes in the latest Cretaceous dinosaur communities of southwestern Europe

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Cited by 47 publications
(35 citation statements)
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“…In southwestern Europe, a dinosaur faunal replacement is well documented at the end of the Cretaceous 71 . According to this major faunal change, the upper Campanian-lower Maastrichtian plant-eating dinosaurs, characterized by rhabdodontid ornithopods, nodosaurid ankylosaurs and titanosaurian sauropod taxa, were replaced by numerous new hadrosauroids and titanosaurian taxa.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…In southwestern Europe, a dinosaur faunal replacement is well documented at the end of the Cretaceous 71 . According to this major faunal change, the upper Campanian-lower Maastrichtian plant-eating dinosaurs, characterized by rhabdodontid ornithopods, nodosaurid ankylosaurs and titanosaurian sauropod taxa, were replaced by numerous new hadrosauroids and titanosaurian taxa.…”
Section: Discussionmentioning
confidence: 99%
“…New taxa reached the Ibero-Armorican domain at some time around the early Maastrichtian-late Maastrichtian boundary. Furthermore, fossil evidence suggest that both associations coexisted for some time 71 . This faunal change can be also recognized on the basis of dinosaur ootaxa (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…3) With more fossils and a better grasp of the ages and relationships of the formations they are found in, more rigorous statistical studies of dinosaur diversity change will become possible. These have been hugely successful in western North America (e.g., Sheehan et al 1991, Pearson et al 2001, 2002, Fastovsky and Sheehan 2005, Campione and Evans 2011, Brusatte et al 2012, 2015a, Larson et al 2016 and Spain (e.g., Vila et al 2016), and are currently in progress in Romania (e.g., Csiki-Sava et al 2016b). Only through detailed, layer-by-layer sampling, constrained by a robust timescale, can changes in diversity, abundance, and evolutionary rates be calculated over time.…”
Section: Challenges and Future Directionsmentioning
confidence: 99%
“…This debate persists because the fossil record of latest Cretaceous dinosaurs is incomplete and heavily biased, with only a few regions of the globe preserving an abundance of well-studied and welldated dinosaurs from the several million years before the asteroid impact. Almost all of these sites are in the northern hemisphere, chief among them the Maastrichtian Hell Creek Formation and equivalents in western North America (e.g., Hartman et al 2002, Fastovsky andBercovici 2016), as well as similar-aged localities in Spain (e.g., Vila et al 2016) and Romania (e.g., CsikiSava et al 2015CsikiSava et al , 2016b. Very little is known about the final non-avian dinosaurs of the southern continents, and this gaping hole in our knowledge makes it very difficult to conclusively test whether the dinosaur extinction was a sudden, global event or a more drawn out affair that may have proceeded at different paces in different regions.…”
Section: Introductionmentioning
confidence: 99%
“…The study of the faunas in the Iberico-Armorican Island has evidenced a 10ma dinosaur succession with a gradual faunal turnover. In this, the pre-turnover dinosaur assemblages (mainly titanosaurids, rhabdodontids, and nodosaurids) were replaced by post-turnover assemblages, where lambeosaurine hadrosauroids featured predominantly (Vila et al, 2016). Lambeosaurines in Europe are represented by four taxa: Pararhabdodon isonensis Casanovas- Casadellas et al, 1993, Arenysaurus ardevoli Pereda-Superbiola et al, 2009, Blasisaurus canudoi Cruzado-Caballero et al, 2010 and Canardia garonnensis Prieto-Márquez et al, 2013, belonging to three different tribes (Prieto-Márquez et al, 2013).…”
mentioning
confidence: 99%