2015/07/24 by Alan Cooper, Chris Turney, Konrad A Hughen +3 · 4 citations
Earth and Planetary Sciences · Environmental Science · Social Sciences · #Biology #Climate change #Ecology #Extinction (optical mineralogy) #Geography #Geology #Geology and Paleoclimatology Research #Holocene #Isotope Analysis in Ecology #Megafauna #Paleontology #Pleistocene #Pleistocene-Era Hominins and Archaeology #Population
paper · doi:10.1126/science.aac4315
openalex publication_date 2015/07/24 · openalex created_date 2016/06/24 · openalex updated_date 2026/07/23
The mechanisms of Late Pleistocene megafauna extinctions remain fiercely contested, with human impact or climate change cited as principal drivers. We compared ancient DNA and radiocarbon data from 31 detailed time series of regional megafaunal extinctions and replacements over the past 56,000 years with standard and new combined records of Northern Hemisphere climate in the Late Pleistocene. Unexpectedly, rapid climate changes associated with interstadial warming events are strongly associated with the regional replacement or extinction of major genetic clades or species of megafauna. The presence of many cryptic biotic transitions before the Pleistocene/Holocene boundary revealed by ancient DNA confirms the importance of climate change in megafaunal population extinctions and suggests that metapopulation structures necessary to survive such repeated and rapid climatic shifts were susceptible to human impacts.