Assessing the causes of Late Pleistocene extinctions on the continents

被引:657
作者
Barnosky, AD [1 ]
Koch, PL
Feranec, RS
Wing, SL
Shabel, AB
机构
[1] Univ Calif Berkeley, Dept Integrat Biol, Berkeley, CA 94720 USA
[2] Univ Calif Berkeley, Museum Paleontol, Berkeley, CA 94720 USA
[3] Univ Calif Berkeley, Museum Vertebrate Zool, Berkeley, CA 94720 USA
[4] Univ Calif Santa Cruz, Dept Earth Sci, Santa Cruz, CA 95064 USA
[5] Smithsonian Inst, Natl Museum Nat Hist, Washington, DC 20560 USA
关键词
D O I
10.1126/science.1101476
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
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页码:70 / 75
页数:6
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