Impact of climate change on the transition of Neanderthals to modern humans in Europe

Two speleothem stable isotope records from East-Central Europe demonstrate that Greenland Stadial 12 (GS12) and GS10—at 44.3–43.3 and 40.8–40.2 ka—were prominent intervals of cold and arid conditions. GS12, GS11, and GS10 are coeval with a regional pattern of culturally (near-)sterile layers within...

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Detalles Bibliográficos
Autores principales: Staubwasser, Michael, Drăgușin, Virgil, Onac, Bogdan P., Assonov, Sergey, Ersek, Vasile, Hoffmann, Dirk L., Veres, Daniel
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2018
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6140518/
https://www.ncbi.nlm.nih.gov/pubmed/30150388
http://dx.doi.org/10.1073/pnas.1808647115

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6140518/
https://www.ncbi.nlm.nih.gov/pubmed/30150388
http://dx.doi.org/10.1073/pnas.1808647115

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