Barnosky, Anthony D. et al. (2004): Assessing the causes of late Pleistocene extinctions on the continents

Leg/Site/Hole:
Identifier:
2004-083964
georefid

10.1126/science.1101476
doi

Creator:
Barnosky, Anthony D.
University of California at Berkeley, Department of Integrative Biology, Berkeley, CA, United States
author

Koch, Paul L.
University of California at Santa Cruz, United States
author

Feranec, Robert S.
Smithsonian Institution, United States
author

Wing, Scott L.
author

Shabel, Alan B.
author

Identification:
Assessing the causes of late Pleistocene extinctions on the continents
2004
Science
American Association for the Advancement of Science, Washington, DC, United States
306
5693
70-75
One of the great debates about extinction is whether humans or climatic change caused the demise of the Pleistocene megafauna. Evidence from paleontology, climatology, archaeology, and ecology now supports the idea that humans contributed to extinction on some continents, but human hunting was not solely responsible for the pattern of extinction everywhere. Instead, evidence suggests that the intersection of human impacts with pronounced climatic change drove the precise timing and geography of extinction in the Northern Hemisphere. The story from the Southern Hemisphere is still unfolding. New evidence from Australia supports the view that humans helped cause extinctions there, but the correlation with climate is weak or contested. Firmer chronologies, more realistic ecological models, and regional paleoecological insights still are needed to understand details of the worldwide extinction pattern and the population dynamics of the species involved.
English
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Quaternary geology; Cenozoic; Chordata; climate change; correlation; dynamics; extinction; global; human activity; Mammalia; Ocean Drilling Program; paleoclimatology; paleoecology; Pleistocene; Quaternary; simulation; Tetrapoda; upper Pleistocene; Vertebrata;

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