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dc.date.accessioned 2021-04-15T17:44:53Z
dc.date.available 2021-04-15T17:44:53Z
dc.date.issued 2001
dc.identifier.uri http://sedici.unlp.edu.ar/handle/10915/117178
dc.description.abstract The history of South American mammals has been episodic, apparently "stratified", and the "strata" relatively few in number and, as a rule, sharply and clearly separable. This is a consequence of the physical history of the continent. The fossil record shows that there were two great episodes characterized by drastic turnovers of mammal communities; both appear related to two of the most drastic physical changes withstood by the continent. The oldest episode is related to the separation of Africa from the other Gondwanan continents (shaping the primordial outlines of the eastern cost of the incipient Southern Atlantic Ocean), and to a sporadic connection of the South American plate with the North American plate. This led to the first great turnover: with the exception of two Gondwanan taxa (Monotremes and Gondwanatheres), and probably another one (Dryolestida), all the Gondwanan mammals (all non-tri- bosphenic taxa) became extinct, and were "replaced" by Laurasian tribosphenic marsupial and placental immigrants. Because of the early extinction (early Paleocene) of the Gondwanan non-tribosphenic survivors, and the subsequent isolation of the continent (including, at least, the Antarctic Peninsula) unique communities solely composed of quite endemic (native) marsupials and placentals were built up. As a consequence of the inter-American connection via the newborn Central America, an increasing biotic interchange began. The second great turnover, involving dispersal, extinction and survival, built up quite peculiar mammalian communities. These are the new basic mammal communities that, after the "Megafaunal Extinction" and the addition of a few and selected immigrants, distinguish the present Neotropical Region. Apparently this second great turnover was accomplished by replacement, not by displacement, as long thought. The failure to find mammals in rocks representing the K-T transition, has no record to analyze the modus operandi of the transcendental first turnover. en
dc.format.extent 151-156 es
dc.language en es
dc.subject South American land-mammals es
dc.subject K-T. Tertiary-Pleistocene es
dc.subject Dispersal es
dc.subject Turnover es
dc.subject Extinction es
dc.subject Survival es
dc.title The K-T and Tertiary-Pleistocene South American mammalian turnovers: similar phenomena? en
dc.type Articulo es
sedici.identifier.uri https://www.peapaleontologica.org.ar/index.php/peapa/article/view/234 es
sedici.identifier.issn 0328-347X es
sedici.creator.person Pascual, Rosendo es
sedici.creator.person Balarino, María Lucía es
sedici.creator.person Udrizar Sauthier, Daniel Edgardo es
sedici.subject.materias Paleontología es
sedici.description.fulltext true es
mods.originInfo.place Facultad de Ciencias Naturales y Museo es
sedici.subtype Articulo es
sedici.rights.license Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
sedici.rights.uri http://creativecommons.org/licenses/by-nc/4.0/
sedici.description.peerReview peer-review es
sedici.relation.journalTitle Publicación Electrónica de la Asociación Paleontológica Argentina es
sedici.relation.journalVolumeAndIssue vol. 7, no. 1 es


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