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1.
J Hum Evol ; 65(2): 168-84, 2013 Aug.
Artigo em Inglês | MEDLINE | ID: mdl-23830175

RESUMO

The Sierra de Atapuerca, northern Spain, is known from many prehistoric and palaeontological sites documenting human prehistory in Europe. Three major sites, Gran Dolina, Galería and Sima del Elefante, range in age from the oldest hominin of Western Europe dated to 1.1 to 1.3 Ma (millions of years ago) at Sima del Elefante to c.a. 0.2 Ma on the top of the Galería archaeological sequence. Recently, a chronology based on luminescence methods (Thermoluminescence [TL] and Infrared Stimulated Luminescence [IRSL]) applied to cave sediments was published for the Gran Dolina and Galería sites. The authors proposed for Galería an age of 450 ka (thousands of years ago) for the units lower GIII and GII, suggesting that the human occupation there is younger than the hominid remains of Sima de los Huesos (>530 ka) around 1 km away. In this paper, we present new results obtained by combined Electron Spin Resonance/Uranium-series (ESR/U-series) dating on 20 herbivorous teeth from different levels at the Galería site. They are in agreement with the TL results for the upper part of the stratigraphic sequence (GIV and GIIIb), in the range of between 200 and 250 ka. But for the GIIIa to GIIb levels, the TL ages become abruptly older by 200 ka while ESR ages remain relatively constant. Finally, the TL and ESR data agree in the lowest part of the section (GIIa); both fall in the range of around 350-450 ka. Our results suggest a different interpretation for the GII, GIII and GIV units of Galería and the upper part of Gran Dolina (TD10 and TD11) than obtained by TL. The ESR/U-series results are supported by a Bayesian analysis, which allows a better integration between stratigraphic information and radiometric data.


Assuntos
Espectroscopia de Ressonância de Spin Eletrônica/métodos , Fósseis , Medições Luminescentes/métodos , Datação Radiométrica/métodos , Dente/química , Animais , Teorema de Bayes , Cronologia como Assunto , Sedimentos Geológicos/química , Hominidae , Cavalos , Ruminantes , Espanha , Urânio/química
2.
Proc Natl Acad Sci U S A ; 107(46): 19726-30, 2010 Nov 16.
Artigo em Inglês | MEDLINE | ID: mdl-21041630

RESUMO

The Mauer mandible, holotype of Homo heidelbergensis, was found in 1907 in fluvial sands deposited by the Neckar River 10 km southeast of Heidelberg, Germany. The fossil is an important key to understanding early human occupation of Europe north of the Alps. Given the associated mammal fauna and the geological context, the find layer has been placed in the early Middle Pleistocene, but confirmatory chronometric evidence has hitherto been missing. Here we show that two independent techniques, the combined electron spin resonance/U-series method used with mammal teeth and infrared radiofluorescence applied to sand grains, date the type-site of Homo heidelbergensis at Mauer to 609 ± 40 ka. This result demonstrates that the mandible is the oldest hominin fossil reported to date from central and northern Europe and raises questions concerning the phyletic relationship of Homo heidelbergensis to more ancient populations documented from southern Europe and in Africa. We address the paleoanthropological significance of the Mauer jaw in light of this dating evidence.


Assuntos
Fósseis , História Antiga , Hominidae/anatomia & histologia , Datação Radiométrica/métodos , Animais , Espectroscopia de Ressonância de Spin Eletrônica , Alemanha , Humanos , Raios Infravermelhos , Mandíbula/anatomia & histologia , Mandíbula/diagnóstico por imagem , Radiografia , Dente/anatomia & histologia , Dente/diagnóstico por imagem , Urânio
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