Digging of another sort: Searching through the collections of the Natural History Museum of Los Angeles County for mammalian teeth to sample for stable isotope analysis

UMMP Postdoctoral Researcher Fabian Hardy, Research Scientist Catherine Badgley, and their colleagues set out to understand how mammals adapted to changing environments in the American southwest during the Miocene. The team gathered carbon and oxygen isotopic data from hoofed mammals and soil carbonates in the Mojave region from 17-8 million years ago to see if they could spot change in the mammals’ diets as the dominant kinds of plants changed over time. What they found was a surprise. Rather than switching diets, herbivores in the region tracked their preferred food resources and consumed familiar plants for at least 9 million years as forest-dominated settings changed to more open woodland and grassland habitats. These conservative diets suggest the mammal species were consuming plants from outside of the immediate basin where their fossils were preserved, highlighting the importance of habitat connectivity during periods of climate and vegetation change. Hardy’s results also provide tantalizing evidence for facultative drinking behavior–obtaining more water from leaves than drinking it directly–in extinct camels and pronghorn. If correct, this suggests an earlier evolution of the adaptation than previously known in these groups. The study, “Dietary fidelity of Miocene ungulates in the context of environmental change in the Mojave region, western North America”, appears in Palaeogeography, Palaeoclimatology, Palaeoecology.

While soil isotope data (panel B) indicates that C4 plants like grasses did increase in prominence within the Mojave region during the middle to late Miocene (17-8 Ma), tooth enamel isotope data indicates hoofed herbivores like pronghorn, camels, and horses mostly ignored the new plants and continued eating familiar foods (panel A), such as C3 shrubs and forbs.
Teeth belonging to ancient horses, camels, and pronghorn, to be sampled for isotopes of carbon and oxygen. These materials provide insight into the diets of extinct animals and the ecosystems they inhabited