Titlebook: Handbook of Paleoanthropology; Winfried Henke,Ian Tattersall Reference work 2015Latest edition Springer-Verlag Berlin Heidelberg 2015 Foss

Fibrin

Taphonomic and Diagenetic Processeshe rule. The transition of organic remains from the biosphere to the lithosphere (=taphonomy) comprises the successive steps of necrology, biostratinomy, burial, and diagenesis. Focusing on the taphonomy of vertebrate skeletons, fossil types, and the main processes leading to preservation and/or des

Cholecystokinin

Contribution of Stable Light Isotopes to Paleoenvironmental Reconstructiont isotope evidence. We begin with an exploration of some of the gaps to which isotope approaches may be applied to good effect and follow with an overview of the principles and the materials typically available for analysis. The results for carbon isotope ratios of pedogenic carbonates and faunal en

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Limousine

Erythropoietin

Quaternary Geology and Paleoenvironmentsn Hemisphere. The earliest such glaciation, at about 2.6 Ma, is now recognized as one step in a worldwide cooling trend that began some 38 million years ago when the world ocean first felt the effect of the great Antarctic ice sheet. With the loss of ocean warmth, the cycles in the Earth’s orbit tha

進取心

Quaternary Deposits and Paleositesre preserved only very rarely. Whether or not fossils are well preserved depends not only on their own composition but also on the nature of the deposits that enclose them, which as a rule are sediments of the Pliocene, Pleistocene, or Holocene age. Numerous methods are now available for chronometri

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燒烤

https://doi.org/10.1007/978-3-642-39979-4Fossils and Molecular Biology; Human Evolution; Paleoanthropology; Primate Evolution

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Winfried Henke,Ian TattersallFirst comprehensive handbook on paleoanthropology taking a multifaceted and multidisciplinary approach.Three volumes cover the breadth and depth of a vast topic.All volumes available in print and onli