1992
DOI: 10.1016/0031-0182(92)90140-z
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Changes of mammal assemblages in the pampean region (Argentina) and their relation with the Plio-Pleistocene boundary

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Cited by 98 publications
(98 citation statements)
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“…This high genetic variability at nuclear (RAPD) and mtDNA at both populations can reflect the historically large population sizes and their recent decline. The abundance of this species in the past can be deduced from archaeological sites where it is commonly found (Tonni et al, 1992). Its exploitation and consequent population decline can also be easily deduced when we check the numbers of pelts exported from Rio de La Plata in the nineteen century: about 2,130,000 only between 1860 and 1870 (Thornback and Jenkins, 1982).…”
Section: Discussionmentioning
confidence: 99%
“…This high genetic variability at nuclear (RAPD) and mtDNA at both populations can reflect the historically large population sizes and their recent decline. The abundance of this species in the past can be deduced from archaeological sites where it is commonly found (Tonni et al, 1992). Its exploitation and consequent population decline can also be easily deduced when we check the numbers of pelts exported from Rio de La Plata in the nineteen century: about 2,130,000 only between 1860 and 1870 (Thornback and Jenkins, 1982).…”
Section: Discussionmentioning
confidence: 99%
“…According to Tonni & Figalgo (1978), during Pleistocene the climatic conditions alternated between arid or semi-arid and humid. The predominance of dry and cold climate in the late Pleistocene is suggested by the presence of fossil pollen especially from the Brassicaceae (Quattrocchio et al, 2008), and of fossil of extant mammals from Patagonian and Central sub-regions, associated to arid or semi-arid and cold weathers (Microcavia australis and Pediolagus salinicola) (Tonni, 1981(Tonni, , 1985Tonni et al, 1992;Prado & Alberdi, 2010).…”
Section: Cluster Analysismentioning
confidence: 99%
“…Three specimens (MMMP 162S, 26S, 48S) came from these marine cliffs north of Mar del Plata City. In this area, sediments have been referred to the Ensenadan, Bonaerian, Lujanian, and Platan (Tonni et al, 1992;Cione and Tonni, 1995;1999). Recent magnetostratigraphic studies by Bidegain et al (1998) show that a change from chron C1r to C1n can be identified 7 m above the top of the cliff (3 m from the base).…”
Section: Ensenadanmentioning
confidence: 99%