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1.
Nature ; 534(7606): 249-53, 2016 06 09.
Artigo em Inglês | MEDLINE | ID: mdl-27279222

RESUMO

Recent excavations at the early Middle Pleistocene site of Mata Menge in the So'a Basin of central Flores, Indonesia, have yielded hominin fossils attributed to a population ancestral to Late Pleistocene Homo floresiensis. Here we describe the age and context of the Mata Menge hominin specimens and associated archaeological findings. The fluvial sandstone layer from which the in situ fossils were excavated in 2014 was deposited in a small valley stream around 700 thousand years ago, as indicated by (40)Ar/(39)Ar and fission track dates on stratigraphically bracketing volcanic ash and pyroclastic density current deposits, in combination with coupled uranium-series and electron spin resonance dating of fossil teeth. Palaeoenvironmental data indicate a relatively dry climate in the So'a Basin during the early Middle Pleistocene, while various lines of evidence suggest the hominins inhabited a savannah-like open grassland habitat with a wetland component. The hominin fossils occur alongside the remains of an insular fauna and a simple stone technology that is markedly similar to that associated with Late Pleistocene H. floresiensis.


Assuntos
Arqueologia , Meio Ambiente , Fósseis , Hominidae , Datação Radiométrica , Animais , Argônio , Clima , Espectroscopia de Ressonância de Spin Eletrônica , Pradaria , História Antiga , Indonésia , Radioisótopos , Comportamento de Utilização de Ferramentas , Dente/química , Erupções Vulcânicas/história , Áreas Alagadas
2.
Science ; 321(5896): 1648, 2008 Sep 19.
Artigo em Inglês | MEDLINE | ID: mdl-18801991

RESUMO

Climate models predict extensive and severe degradation of permafrost in response to global warming, with a potential for release of large volumes of stored carbon. However, the accuracy of these models is difficult to evaluate because little is known of the history of permafrost and its response to past warm intervals of climate. We report the presence of relict ground ice in subarctic Canada that is greater than 700,000 years old, with the implication that ground ice in this area has survived past interglaciations that were warmer and of longer duration than the present interglaciation.

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