The Cerro Azul Formation (La Pampa Province, Argentina) comprises a rich verte- brate fauna of small mammals dominated by notoungulates and rodents. The fauna pertains to the Late Miocene specifically to the Huayquerian Stage/Age. Taphonomic analysis of micro-mammals from Estancia Re locality evidenced that the faunal assem- blage was accumulated by the activity of a predator. This assemblage was compared with others from the Cerro Azul Formation in Telen and Caleufu localities (La Pampa Province), previously interpreted as products of predator activities. These microfossil accumulations differ from assemblages attributed to pellets and faeces produced by modern predators (nocturnal and diurnal bird raptors and carnivore mammals). However, ...
This study provides a taphonomic and paleoenvironmental analysis of the micromammal (˂1 kg) accumula...
The present study analyses small mammal bone and tooth accumulations recovered in three open-air arc...
A new mammalian assemblage from the Late Miocene Palo Pintado Formation in Northwestern Argentina is...
The taphonomic results on the fossil macromammal assemblage from Caleufú (La Pampa Province, Argenti...
A continental assemblage of fossil mammals from the Santa Cruz Formation (early Miocene, Burdigalian...
The taphonomic results on the fossil macromammal assemblage from Caleufú (La Pampa Province, Argenti...
Quaternary continental deposits of South America are characterized by the abundance and diversity of...
The first Late Holocene mammal assemblage (mainly micromammals) of La Pampa Province was found in Qu...
The present study analyses the taphonomic features of recent small mammal bone and teeth accumulatio...
Microvertebrates are a major component of many assemblages recovered from the Quaternary of the Arge...
We describe new remains of notoungulates from the Cerro Azul Formation (late Miocene) in La Pampa Pr...
The distinctive characteristic of theMonte Desert, the most arid rangeland of Argentina, is reflecte...
The lower Miocene Santa Cruz Formation (dated to ~18–16 Ma) of Southern Patagonia, Argentina, preser...
The present study analysed the taphonomic characteristics of small mammal bone accumulations produce...
The Plains vizcacha (Lagostomus maximus) is one of the largest rodents in South America. They live i...
This study provides a taphonomic and paleoenvironmental analysis of the micromammal (˂1 kg) accumula...
The present study analyses small mammal bone and tooth accumulations recovered in three open-air arc...
A new mammalian assemblage from the Late Miocene Palo Pintado Formation in Northwestern Argentina is...
The taphonomic results on the fossil macromammal assemblage from Caleufú (La Pampa Province, Argenti...
A continental assemblage of fossil mammals from the Santa Cruz Formation (early Miocene, Burdigalian...
The taphonomic results on the fossil macromammal assemblage from Caleufú (La Pampa Province, Argenti...
Quaternary continental deposits of South America are characterized by the abundance and diversity of...
The first Late Holocene mammal assemblage (mainly micromammals) of La Pampa Province was found in Qu...
The present study analyses the taphonomic features of recent small mammal bone and teeth accumulatio...
Microvertebrates are a major component of many assemblages recovered from the Quaternary of the Arge...
We describe new remains of notoungulates from the Cerro Azul Formation (late Miocene) in La Pampa Pr...
The distinctive characteristic of theMonte Desert, the most arid rangeland of Argentina, is reflecte...
The lower Miocene Santa Cruz Formation (dated to ~18–16 Ma) of Southern Patagonia, Argentina, preser...
The present study analysed the taphonomic characteristics of small mammal bone accumulations produce...
The Plains vizcacha (Lagostomus maximus) is one of the largest rodents in South America. They live i...
This study provides a taphonomic and paleoenvironmental analysis of the micromammal (˂1 kg) accumula...
The present study analyses small mammal bone and tooth accumulations recovered in three open-air arc...
A new mammalian assemblage from the Late Miocene Palo Pintado Formation in Northwestern Argentina is...