Small mammal remains from Cueva Huenul 1, northern Patagonia, Argentina: Taphonomy and paleoenvironments since the Late Pleistocene

2012 ◽  
Vol 278 ◽  
pp. 22-31 ◽  
Author(s):  
Fernando J. Fernández ◽  
Pablo Teta ◽  
Ramiro Barberena ◽  
Ulyses F.J. Pardiñas
2021 ◽  
Vol 36 (2) ◽  
pp. 224-238
Author(s):  
Louis Arbez ◽  
Aurelien Royer ◽  
Danielle Schreve ◽  
Remi Laffont ◽  
Serge David ◽  
...  

Geology ◽  
2012 ◽  
Vol 41 (2) ◽  
pp. 267-270 ◽  
Author(s):  
J. M. Lopez-Garcia ◽  
H.-A. Blain ◽  
J. I. Morales ◽  
C. Lorenzo ◽  
S. Banuls-Cardona ◽  
...  

2002 ◽  
Vol 15 (6) ◽  
pp. 657-667 ◽  
Author(s):  
G Román-Ross ◽  
P.J Depetris ◽  
M.A Arribére ◽  
S Ribeiro Guevara ◽  
G.J Cuello

1980 ◽  
Vol 58 (8) ◽  
pp. 1507-1511 ◽  
Author(s):  
James A. Burns

The first fossil remains of Lemmus sibiricus south of Beringia are reported from a rock shelter called January Cave in the Front Ranges of the Rocky Mountains, southwestern Alberta, Canada. The 45 specimens were excavated along with several thousands of isolated small mammal teeth and fragmentary bones. Dated by both radiocarbon and thermoluminescence methods to span the last 22 000 – 23 000 years, a late Pleistocene-through-present sequence is provided. Argument is made for the existence of a southern relict population of this lemming prior to a northward, postglacial dispersal into British Columbia and the Yukon Territory.


2014 ◽  
Vol 339-340 ◽  
pp. 62-75 ◽  
Author(s):  
Juan Rofes ◽  
Xabier Murelaga ◽  
Blanca Martínez-García ◽  
Salvador Bailon ◽  
Juan Carlos López-Quintana ◽  
...  

2014 ◽  
Vol 82 (1) ◽  
pp. 198-208 ◽  
Author(s):  
Mauro N. Tammone ◽  
Adan Hajduk ◽  
Pablo Arias ◽  
Pablo Teta ◽  
Eileen A. Lacey ◽  
...  

AbstractComparisons of historical and modern assemblages of mammals can yield important insights into patterns and processes of environmental change. Here, we present the first analyses of small mammal assemblages present in northern Patagonia during the last glacial maximum (LGM). Using remains obtained from owl pellets excavated from an archeological cave site (Arroyo Corral I, levels VII–V, carbon dates of 22,400–21,530 cal yr BP), we generate estimates of the minimum number of individuals for all species detected; these estimates, in turn are used to determine relative species abundances. Comparisons of these data with similar analyses of small mammal remains obtained from a second archeological site (ACoII, levels IV–V, carbon dates of 10,010–9220 cal yr BP) as well as from modern owl pellets reveal pronounced changes in relative species abundance since the LGM. In particular, Euneomys chinchilloides and Ctenomys sociabilis – the predominant species during the LGM – declined markedly, suggesting a change from open, bare habitat punctuated by patches of wet meadows and shrubs to the more densely vegetated mosaic of ecotone habitats found in this region today. These data provide important new insights into the environmental changes that have occurred in northern Patagonia over the last 20,000 years.


2019 ◽  
Vol 488 (3) ◽  
pp. 277-281
Author(s):  
M. A. Erbajeva ◽  
A. A. Shchetnikov ◽  
A. Yu. Kazansky ◽  
G. G. Matasova ◽  
F. I. Khenzykhenova ◽  
...  

The currant paper presents the preliminary results of the multidisciplinary study of the new Pleistocene section Ulan-Zhalga (51°29′40.75″ С, 107°20′18.11″ В) discovered in the Western Transbauikalaia in 2017. On the base of the paleontological, paleomagmetic, and lithological data the early, middle and late Pleistocene sediments were recognized in the section. The analysis of the rich small mammal fossils resulted in to trace the paleoenvironmental and climatic changes in the region during the Quaternary. The unique alternation of the 19 faunistic horizons and 11 fossil soils in the whole section, the high correlation of the paleomagnetic and paleontological data allow us to refer the studied section Ulan-Zhalga to addition new late Cenozoic Key section of the south Eastern Siberia. The new geological and paleontological data would be important for paleogeographical reconstruction and biostratigraphic analysis.


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