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1.
Science ; 344(6190): 1358-63, 2014 Jun 20.
Artigo em Inglês | MEDLINE | ID: mdl-24948730

RESUMO

Seventeen Middle Pleistocene crania from the Sima de los Huesos site (Atapuerca, Spain) are analyzed, including seven new specimens. This sample makes it possible to thoroughly characterize a Middle Pleistocene hominin paleodeme and to address hypotheses about the origin and evolution of the Neandertals. Using a variety of techniques, the hominin-bearing layer could be reassigned to a period around 430,000 years ago. The sample shows a consistent morphological pattern with derived Neandertal features present in the face and anterior vault, many of which are related to the masticatory apparatus. This suggests that facial modification was the first step in the evolution of the Neandertal lineage, pointing to a mosaic pattern of evolution, with different anatomical and functional modules evolving at different rates.


Assuntos
Fósseis , Homem de Neandertal/anatomia & histologia , Homem de Neandertal/genética , Crânio/anatomia & histologia , Animais , Encéfalo/anatomia & histologia , Extinção Biológica , Deriva Genética , Humanos , Tamanho do Órgão , Isolamento Reprodutivo , Espanha
2.
Proc Natl Acad Sci U S A ; 101(26): 9936-41, 2004 Jun 29.
Artigo em Inglês | MEDLINE | ID: mdl-15210963

RESUMO

Beginning ca. A.D. 1400, Polynesian farmers established permanent settlements along the arid southern flank of Haleakala Volcano, Maui, Hawaiian Islands; peak population density (43-57 persons per km(2)) was achieved by A.D. 1700-1800, and it was followed by the devastating effects of European contact. This settlement, based on dryland agriculture with sweet potato as a main crop, is represented by >3,000 archaeological features investigated to date. Geological and environmental factors are the most important influence on Polynesian farming and settlement practices in an agriculturally marginal landscape. Interactions between lava flows, whose ages range from 3,000 to 226,000 years, and differences in rainfall create an environmental mosaic that constrained precontact Polynesian farming practices to a zone defined by aridity at low elevation and depleted soil nutrients at high elevation. Within this productive zone, however, large-scale agriculture was concentrated on older, tephra-blanketed lava flows; younger flows were reserved for residential sites, small ritual gardens, and agricultural temples.


Assuntos
Agricultura/história , Arqueologia , Evolução Cultural , Meio Ambiente , Clima , Ecossistema , Sedimentos Geológicos/química , Havaí , História do Século XV , História do Século XVI , História do Século XVII , História do Século XVIII , História do Século XIX , Habitação , Polinésia/etnologia , Solo/análise , Fatores de Tempo , Água
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