Megafaunal extinctions in the tropics
Questions of megafaunal (animals >44kg) extinctions during the Late Pleistocene and Holocene have been of extreme interest to the international archaeological and palaeontological communities, with it being variously argued that certain taxa were driven to extinction by human impacts, climatic change, disease, or even asteroid impacts. The potential impact of humans on various now extinct genera of large animals that once roamed the earth are linked to broader questions regarding the scale of our species’ impact on ecosystems. However, these discussions often neglect the species dynamics of entire ecologies, including smaller mammals and reptiles, and have generally been limited to Europe, the Americas, and Australia.
This project is committed to undertaking studies of human impacts on animal populations in the less-studied regions of island East Africa, South Asia, Southeast Asia, and Melanesia. In particular, we seek to refine chronologies of faunal decline and extinction, as well as continuity, in these less-studied regions using detailed radiocarbon and optically-stimulated luminescence methodologies. We are also working to develop a consortium of specialists applying different novel methods to study changing demography, biology, and ecology of these taxa around the world. We are also interested in the comparison of faunal extinctions on mainland versus island ecosystems.
Boivin, N.L., Zeder, M.A., Fuller, D.Q., Crowther, A., Larson, G., Erlandson, J.M., Denham, T. & M.D. Petraglia. 2016. Ecological consequences of human niche construction: examining long-term anthropogeniuc shaping of global species distributions. Proceedings of the National Academy of Sciences of the United States of America 113: 6388-6396.
Roberts, P., Delson, E., Miracle, P., Ditchfield, P., Roberts, R.G., Jacobs, Z., Blinkhorn, J., Ciochon, R.L., Fleagle, J.G., Frost, S.R., Gilbert, C.C., Gunnell, G.F., Harrison, T., Korisettar, R., & M.D. Petraglia. 2014. Continuity of mammalian fauna over the last 200,000 y in the Indian subcontinent. Proceedings of the National Academy of Sciences of the United States of America 111(16): 5848-5853.