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A New Global Palaeobiogeographical Model for the Late Mesozoic and Early Tertiary

Martín D. Ezcurra, +1 more
- 01 Jul 2012 - 
- Vol. 61, Iss: 4, pp 553-566
TLDR
A new biogeographical model for late Mesozoic terrestrial ecosystems is proposed in which Europe and "Gondwanan" territories possessed a common Eurogondwanans fauna during the earliest Cretaceous, and tree reconciliation analyses (TRAs) were performed based onBiogeographical signals provided by a supertree of late Meszoic archosaurs.
Abstract
Late Mesozoic palaeobiogeography has been characterized by a distinction between the northern territories of Laurasia and the southern landmasses of Gondwana. The repeated discovery of Gondwanan lineages in Laurasia has led to the proposal of alternative scenarios to explain these anomalous occurrences. A new biogeographical model for late Mesozoic terrestrial ecosystems is here proposed in which Europe and "Gondwanan" territories possessed a common Eurogondwanan fauna during the earliest Cretaceous. Subsequently, following the Hauterivian, the European territories severed from Africa and then connected to Asiamerica resulting in a faunal interchange. This model explains the presence of Gondwanan taxa in Laurasia and the absence of Laurasian forms in the southern territories during the Cretaceous. In order to test this new palaeobiogeographical model, tree reconciliation analyses (TRAs) were performed based on biogeographical signals provided by a supertree of late Mesozoic archosaurs. The TRAs found significant evidence for the presence of an earliest Cretaceous Eurogondwanan fauna followed by a relatively short-term Gondwana-Laurasia dichotomy. The analysis recovered evidence for a biogeographical reconnection of the European territories with Africa and South America- Antarctica during the Campanian to Maastrichtian time-slice. This biogeographical scenario appears to continue through the early Tertiary and sheds light on the trans-Atlantic disjunct distributions of several extant plant and animal groups. (Archosauria; Atlantogea; Cretaceous; Eurogondwana; palaeobiogeography; Tertiary.)

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Citations
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Historical biogeography of the Isthmus of Panama.

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Island life in the Cretaceous - faunal composition, biogeography, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago

TL;DR: It is shown that there is no clear evidence that dinosaurs or other groups were undergoing long-term declines in Europe prior to the bolide impact, and the importance of the European record in understanding the end-Cretaceous extinction is discussed.
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Molecular and fossil evidence place the origin of cichlid fishes long after Gondwanan rifting

TL;DR: The results provide a revised macroevolutionary time scale for cichlids, imply a role for dispersal in generating the observed geographical distribution of this important model clade and add to a growing debate that questions the dominance of the vicariance paradigm of historical biogeography.
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Evolution of the carnivorous dinosaurs during the Cretaceous: The evidence from Patagonia

TL;DR: The most comprehensive fossil record of Cretaceous theropods from Gondwana, consisting of 31 nominal species belonging to singleton taxa and six families: Abelisauroids, Noasaurids, Carcharodontosauridae, Megaraptoridae nov. fam., Alvarezsaurusidae, and Unenlagiidae, is presented in this paper.

Component-compatibility in historical biogeography

TL;DR: The problems of reconstructing historical relationships for areas of endemism from distributional data for groups of taxa and the cladistic relationships among the members of those groups can be solved by applying the two principles of parsimony and mutual inclusion or exclusion (compatibility) of components.
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