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dc.contributor.author
Gasparini, Germán Mariano  
dc.contributor.author
Tonni, Eduardo Pedro  
dc.contributor.other
Miotti, Laura Lucia  
dc.contributor.other
Salemme, Monica Cira  
dc.contributor.other
Hermo, Dario Omar  
dc.date.available
2025-04-11T13:11:06Z  
dc.date.issued
2022  
dc.identifier.citation
Gasparini, Germán Mariano; Tonni, Eduardo Pedro; Quaternary of Tierra del Fuego and southernmost Patagonia; Springer; 2022; 127-158  
dc.identifier.isbn
978-3-030-92503-1  
dc.identifier.uri
http://hdl.handle.net/11336/258583  
dc.description.abstract
In the Fuego-Patagonian region, except for a very few exceptions, no mammals that may be clearly correlated with those characterizing the upper most Miocene-Early Pleistocene units of the extra-Patagonian area (Montehermosan, Chapadmalalan, Marplatan and Ensenadan stages) have been recorded. The remains of the Late Pleistocene in Patagonia are diverse and relatively frequent, but almost restricted to those representing approximately the last 15,000 years, many of which are directly or indirectly associated with archaeological sites. The goals of this contribution are: 1- to present an updated revision of the information about Late Pleistocene and Middle Holocene fauna records in archaeological/palaeontological sites of the Fuego-Patagonian region (43º 30´-55º 30´S), and 2- to comments the climatic conditions that occurred in Patagonia during this period. During the Antarctic Cold Reversal, several species of pampean herbivore megamammals expanded their distribution to reach the south of Patagonia and Tierra del Fuego. These herbivores were accompanied by their potential predators. This expansion of the distribution towards high latitudes can be attributed to environmental conditions that favored the increase of primary productivity. However towards the end of the Pleistocene and beginning of the Holocene, these mammals became extinct. In Patagonia, the extinction of megamammals occurred with a combination of climatic change and human presence. Although it is unlikely that human predation was the sole cause of extinction of all large/megafauna, it may have reduced population sizes of some large/megamammals, particularly in environmental change conditions. Human settlement in South America could have occurred since ca.18,500 and 14,500 years cal BP. Extinctions occurred prior to, during and after human colonization. There is some evidence of extinct fauna surviving into the Early Holocene, implying that some megamammals and large mammals persisted for some millennial alongside people.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Springer  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
LATE PLEISTOCENE  
dc.subject
EARLY HOLOCENE  
dc.subject
ARCHAEOLOGICAL SITES  
dc.subject
PALAEONTOLOGICAL SITES  
dc.subject.classification
Paleontología  
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente  
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS  
dc.title
Quaternary of Tierra del Fuego and southernmost Patagonia  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.type
info:eu-repo/semantics/bookPart  
dc.type
info:ar-repo/semantics/parte de libro  
dc.date.updated
2025-04-09T10:13:24Z  
dc.journal.pagination
127-158  
dc.journal.pais
Países Bajos  
dc.description.fil
Fil: Gasparini, Germán Mariano. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina  
dc.description.fil
Fil: Tonni, Eduardo Pedro. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/978-3-030-92503-1_5  
dc.conicet.paginas
535  
dc.source.titulo
Archaeology of Piedra Museo Locality: An open window to the early peopling of Patagonia