Background: Current global warming affects the composition and dynamics of mammalian communities and can increase extinction risk; however, long-term effects of warming on mammals are less understood. Dietary reconstructions inferred from stable isotopes of fossil herbivorous mammalian tooth enamel document environmental and climatic changes in ancient ecosystems, including C3/C4 transitions and relative seasonality. Methodology/Principal Findings: Here, we use stable carbon and oxygen isotopes preserved in fossil teeth to document the magnitude of mammalian dietary shifts and ancient floral change during geologically documented glacial and interglacial periods during the Pliocene (,1.9 million years ago) and Pleistocene (,1.3 million years...
Oxygen and carbon isotope compositions of teeth were measured for a variety of fossil herbivores, om...
The role of environmental change in the late Pleistocene megafaunal extinctions remains a key questi...
Patterns of climate and C4 plant abundance in the southwestern United States during the last glaciat...
Current global warming affects the composition and dynamics of mammalian communities and can increas...
transitions and relative seasonality. grass consumption, inter-faunal dietary partitioning, increas...
Mammoths and mastodons are common in Pleistocene deposits, yet these proboscideans and many other an...
Mid-Pleistocene vertebrates in North America are scarce but important for recognizing the ecological...
The end of the late Pleistocene (~10,000 years ago) witnessed the extinction of over seventy percent...
Mean annual temperature reported by the Intergovernmental Panel on Climate Change increases at least...
As humans radiated across the Americas, we restructured New World ecosystems by driving 100+ ecologi...
The end of the late Pleistocene (∼10,000 years ago) witnessed the extinction of over seventy percent...
Stable isotopes of mammoths and mastodons have the potential to illuminate ecological changes in lat...
Climate change and humans are proposed as the two key drivers of total extinction of many large mamm...
Climate change alters species distributions, causing plants and animals to move north or to higher e...
Geochemical tools, including the analysis of stable isotopes from fossil mammals, are often used to ...
Oxygen and carbon isotope compositions of teeth were measured for a variety of fossil herbivores, om...
The role of environmental change in the late Pleistocene megafaunal extinctions remains a key questi...
Patterns of climate and C4 plant abundance in the southwestern United States during the last glaciat...
Current global warming affects the composition and dynamics of mammalian communities and can increas...
transitions and relative seasonality. grass consumption, inter-faunal dietary partitioning, increas...
Mammoths and mastodons are common in Pleistocene deposits, yet these proboscideans and many other an...
Mid-Pleistocene vertebrates in North America are scarce but important for recognizing the ecological...
The end of the late Pleistocene (~10,000 years ago) witnessed the extinction of over seventy percent...
Mean annual temperature reported by the Intergovernmental Panel on Climate Change increases at least...
As humans radiated across the Americas, we restructured New World ecosystems by driving 100+ ecologi...
The end of the late Pleistocene (∼10,000 years ago) witnessed the extinction of over seventy percent...
Stable isotopes of mammoths and mastodons have the potential to illuminate ecological changes in lat...
Climate change and humans are proposed as the two key drivers of total extinction of many large mamm...
Climate change alters species distributions, causing plants and animals to move north or to higher e...
Geochemical tools, including the analysis of stable isotopes from fossil mammals, are often used to ...
Oxygen and carbon isotope compositions of teeth were measured for a variety of fossil herbivores, om...
The role of environmental change in the late Pleistocene megafaunal extinctions remains a key questi...
Patterns of climate and C4 plant abundance in the southwestern United States during the last glaciat...