This study aims at assessing resource and habitat use, niche occupation and trophic interactions from a stable isotope perspective on fossil mammals from the Argentine Pampas during the Great American Biotic Interchange (GABI). We present stable isotope data of more than 400 samples belonging to 10 mammalian orders and spanning a temporal range from ~9.5 Ma to ~12 ky. Rodents, notoungulates and pilosians record an increase in the consumption of C4 plants, whereas litopterns and cingulates show δ13C values that remain mostly within a C3-dominated diet. Our stable isotope data indicates that the expansion of C4 vegetation opened up new niche opportunities, probably alleviating resource competition among endemic taxa. Gomphothere, equid and ca...
To explore the role of past environmental changes in shaping interspecific differences in genetic st...
The prehistoric pastoralist groups that inhabited the Dry Puna of Argentina employed a combination o...
An expansion of C4 grasslands occurred between 6 and 8 million years ago in the Great Plains of Nort...
This study aims at assessing resource and habitat use, niche occupation and trophic interactions fro...
Stable isotope analyses are powerful tools for reconstructing ancient ecologies and ecosystems, as t...
The sabretooth cat Smilodon populator was the largest felid in South America. It appears in the foss...
The aim of this work is to explore general trends and intra-site variability in human paleodiet from...
The modern South American mammalian assemblage was determined by the closure of the Panamaisthmus (~...
Carbon and oxygen stable isotope values in the dental enamel of fossils were used to infer the diet ...
This special volume brings together works that present cases of studies that combine analysis of sta...
Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from thr...
The diet of extinct giant Xenarthrans is a debated topic, especially for ground sloths, for which he...
The main goal of this work is to study the camelid herding and management strategies employed by the...
A late Miocene gomphothere from southeastern Peru documents the earliest occurrence of a North Ameri...
Previous researches have examined the zooarchaeological record to understand changes in human diet i...
To explore the role of past environmental changes in shaping interspecific differences in genetic st...
The prehistoric pastoralist groups that inhabited the Dry Puna of Argentina employed a combination o...
An expansion of C4 grasslands occurred between 6 and 8 million years ago in the Great Plains of Nort...
This study aims at assessing resource and habitat use, niche occupation and trophic interactions fro...
Stable isotope analyses are powerful tools for reconstructing ancient ecologies and ecosystems, as t...
The sabretooth cat Smilodon populator was the largest felid in South America. It appears in the foss...
The aim of this work is to explore general trends and intra-site variability in human paleodiet from...
The modern South American mammalian assemblage was determined by the closure of the Panamaisthmus (~...
Carbon and oxygen stable isotope values in the dental enamel of fossils were used to infer the diet ...
This special volume brings together works that present cases of studies that combine analysis of sta...
Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from thr...
The diet of extinct giant Xenarthrans is a debated topic, especially for ground sloths, for which he...
The main goal of this work is to study the camelid herding and management strategies employed by the...
A late Miocene gomphothere from southeastern Peru documents the earliest occurrence of a North Ameri...
Previous researches have examined the zooarchaeological record to understand changes in human diet i...
To explore the role of past environmental changes in shaping interspecific differences in genetic st...
The prehistoric pastoralist groups that inhabited the Dry Puna of Argentina employed a combination o...
An expansion of C4 grasslands occurred between 6 and 8 million years ago in the Great Plains of Nort...