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Geology; August 2006; v. 34; no. 8; p. 685-688; DOI: 10.1130/G22571.1
© 2006 Geological Society of America
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Dietary controls on extinction versus survival among avian megafauna in the late Pleistocene

Kena Fox-Dobbs1, Thomas A. Stidham2, Gabriel J. Bowen3, Steven D. Emslie4 and Paul L. Koch5

1 Earth Sciences Department, University of California–Santa Cruz, Santa Cruz, California 95064, USA
2 Department of Biology, Texas A&M University, College Station, Texas 77843, USA
3 Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907, USA
4 Biology and Marine Biology Department, University of North Carolina Wilmington, Wilmington, North Carolina 28403, USA
5 Earth Sciences Department, University of California–Santa Cruz, Santa Cruz, California 95064, USA

The late Pleistocene extinction decimated terrestrial megafaunal communities in North America, but did not affect marine mammal populations. In coastal regions, marine megafauna may have provided a buffer that allowed some large predators or scavengers, such as California condors (Gymnogyps californianus), to survive into the Holocene. To track the influence of marine resources on avifaunas we analyzed the carbon, nitrogen, and hydrogen isotope composition of collagen from late Pleistocene vultures and raptors, including species that survived the extinction (condor, bald eagle, golden eagle) and extinct species (teratorn, black vulture). At the Rancho La Brea and McKittrick tar pits of southern California, isotope values for extinct teratorns (Teratornis merriami, n = 10) and black vultures (Coragyps occidentalis, n = 8) show that they fed entirely in a terrestrial C3 ecosystem. In contrast, La Brea condors cluster into two groups, one with a terrestrial diet (n = 4), and the other with a strong marine influence (n = 5). At localities in the American southwest, Texas, and Florida, where condors became extinct, they have isotope values indicating entirely terrestrial diets (n = 10). Our results suggest that dependence upon terrestrial megafaunal carrion as a food source led to the extinction of inland California condor populations and coastal populations of teratorns and black vultures at the Pleistocene-Holocene boundary, whereas use of marine foods allowed coastal condor populations to survive.

Key Words: California condor • paleoecology • stable isotopes • late Pleistocene extinction




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Proc R Soc BHome page
J. K Bump, K. Fox-Dobbs, J. L Bada, P. L Koch, R. O Peterson, and J. A Vucetich
Stable isotopes, ecological integration and environmental change: wolves record atmospheric carbon isotope trend better than tree rings
Proc R Soc B, October 7, 2007; 274(1624): 2471 - 2480.
[Abstract] [Full Text] [PDF]




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