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  2. Changes in climate and geography. The Upper Paleolithic covered the second half of the Last glacial period from 50,000 to 10,000 before present, until the warming of the Holocene. Ice core data from Antarctica and Greenland.

  3. Sep 22, 2023 · Likewise, we posit that major climate amelioration and pronounced forestation precipitated H. sapiens dispersal into Baikal Siberia 45 ka ago, as chronicled by the appearance of the Initial Upper Paleolithic. INTRODUCTION.

  4. Jul 1, 2011 · Precisely how Upper Palaeolithic human ecology was shaped by changing climate during the Pleniglacial remains a matter of debate, for while this generally cold period is now understood to include complex and often rapid flux in climate, there are still considerable difficulties in resolving climatic variations at particular times and places ...

    • David Beresford-Jones, Sean Taylor, Clea Paine, Alexander Pryor, Jiří Svoboda, Jiří Svoboda, Martin ...
    • 2011
  5. Jan 16, 2018 · The Upper Paleolithic (ca 40,000-10,000 years BP) was a period of great transition in the world. The Neanderthals in Europe became edged out and disappeared by 33,000 years ago, and modern humans began to have the world to themselves. While the notion of a "creative explosion" has given way to a recognition of a long history of the development ...

  6. Nov 1, 2019 · In Southwestern France, the final Mousterian took place in a relatively temperate environment 19 while the Upper Paleolithic is marked by a progressive climatic degradation that reached its...

    • William Rendu, William Rendu, Sylvain Renou, Marie-Cécile Soulier, Solange Rigaud, Morgan Roussel, M...
    • 2019
  7. Mar 14, 2023 · We find that the observed changes in faunal assemblages during the European Late Upper Paleolithic are consistent with climate-driven animal habitat shifts impacting the natural abundances...

  8. The European Upper Palaeolithic, after all, encompassed some 30,000 years and spanned thousands of kilometres, and must be viewed against the context of dramatically unstable climates which were often severe and thus posed significant adaptive pressures.

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