2013
DOI: 10.1016/j.quaint.2012.09.015
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Extinction of a gomphothere population from Southeastern Brazil: Taphonomic, paleoecological and chronological remarks

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Cited by 22 publications
(4 citation statements)
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“…7 ka ago [110][111][112]. These estimates largely post-date our obtained timing for the giant anteater's population expansion, but a local extinction (death event) of a gomphothere population in the Águas de Araxá of the CE biome occurred about 55 ka ago [113].…”
Section: Discussionsupporting
confidence: 60%
“…7 ka ago [110][111][112]. These estimates largely post-date our obtained timing for the giant anteater's population expansion, but a local extinction (death event) of a gomphothere population in the Águas de Araxá of the CE biome occurred about 55 ka ago [113].…”
Section: Discussionsupporting
confidence: 60%
“…Even though two hypotheses (climatic change and human action) are frequently evoked to explain South American megafauna extinction, the causal mechanism for the extinction of N. platensis is still under discussion. There is currently only one study suggesting a climatic cause for the extinction of Notiomastodon platensis, but this is an earlier (~60 ka) extirpation, possibly not related to the extinction of proboscideans in the Pleistoce-neeHolocene transition (Avilla et al, 2013). However, that event is consistent with a hypothesis that the sum of several regional disappearances along the Late Pleistocene led to the extinction of proboscideans in South America (Ficcarelli et al, 1997).…”
Section: Origin Chronostratigraphy and Extinctionsupporting
confidence: 63%
“…Thus, this indicates that Notiomastodon platensis was present, at least, by the Early Pleistocene (Ensenadan) in South America (Soibelzon, 2008). Although N. platensis is recorded continuously from the Early Pleistocene to earliest Holocene (11 ± 6 ka; Dantas et al, 2013), most remains are from the Late Pleistocene, such as those from the Aguas de Arax a assemblage (60 ± 5 ka; Simpson and Paula Couto, 1957;Avilla et al, 2013), Chuí Creek, in Southern Brazil (44 ± 3 ka, 52 ± 7 and 80 ± 10 ka, Lopes et al, 2013), Tanque Loma (23.4e18 ka; Lindsey and Lopez, 2015), Quebrada Colorada, Chimborazo, in Ecuador (41.0e40.0 ka; Rom an-Carri on, unpublished results), Monte Verde (11.8 ± 200 ka and 13.5 ± 250 ka; Dillehay, 1989;Labarca Encina and Alberdi, 2011;Recabarren et al, 2014), Nochaco, Regi on de Los Lagos (16.1 ± 750 ka, Recabarren et al, 2014) and Mupulmo, Osorno, in Chile (18,700 ± 900 ka; Recabarren et al, 2014).…”
Section: Origin Chronostratigraphy and Extinctionmentioning
confidence: 99%
“…The records of Notiomastodon platensis are distributed from the Ensenadan (early Pleistocene) to the early Holocene and occur all over the South American continent, with more than 140 localities, but there are no records in Bolivia, Guyana, French Guyana and Suriname (Prado et al, 2005;Avilla et al, 2013;Dantas et al, 2013;Mothé et al, in press). In this study, we describe the first record of Notiomastodon platensis in the department of Tarija, Bolivia.…”
Section: Introductionmentioning
confidence: 99%