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      Extinction chronology of the woolly rhinoceros Coelodonta antiquitatis in the context of late Quaternary megafaunal extinctions in northern Eurasia

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      Quaternary Science Reviews
      Elsevier BV

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          Assessing the causes of late Pleistocene extinctions on the continents.

          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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            Late Quaternary Extinctions: State of the Debate

            Between fifty and ten thousand years ago, most large mammals became extinct everywhere except Africa. Slow-breeding animals also were hard hit, regardless of size. This unusual extinction of large and slow-breeding animals provides some of the strongest support for a human contribution to their extinction and is consistent with various human hunting models, but it is difficult to explain by models relying solely on environmental change. It is an oversimplification, however, to say that a wave of hunting-induced extinctions swept continents immediately after first human contact. Results from recent studies suggest that humans precipitated extinction in many parts of the globe through combined direct (hunting) and perhaps indirect (competition, habitat alteration) impacts, but that the timing and geography of extinction might have been different and the worldwide magnitude less, had not climatic change coincided with human impacts in many places.
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              U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years

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                Author and article information

                Journal
                Quaternary Science Reviews
                Quaternary Science Reviews
                Elsevier BV
                02773791
                September 2012
                September 2012
                : 51
                :
                : 1-17
                Article
                10.1016/j.quascirev.2012.06.007
                59894d63-1a0a-40d1-bd05-f35165273d5c
                © 2012

                http://www.elsevier.com/tdm/userlicense/1.0/

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