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Coloring and preservation state of faunal remains from the neanderthal levels of Kůlna Cave, Czech republic
Author(s) -
Michel Véronique,
Bocherens Hervé,
ThéryParisot Isabelle,
Valoch Karel,
Valensi Patricia
Publication year - 2006
Publication title -
geoarchaeology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.696
H-Index - 44
eISSN - 1520-6548
pISSN - 0883-6353
DOI - 10.1002/gea.20116
Subject(s) - cave , crystallinity , taphonomy , fourier transform infrared spectroscopy , chemistry , materials science , mineralogy , geology , archaeology , crystallography , geography , paleontology , physics , optics
Abstract The preservation process of faunal remains from the Middle Paleolithic levels of Kůlna Cave was studied within a taphonomic and palaeodietary framework. A visual examination of bones and teeth showed that they display a wide variety of colors. Chemical analyses (C, N, Fe, Mn) and a combination of analytical techniques, such as Fourier transform infrared (FT‐IR), X‐ray diffraction (XRD), and electron spin resonance (ESR) spectrometry, were conducted on 13 fossil remains. The crystallinity indexes, IR‐SF, XRD‐CI, XRD‐L200, the IR area band (Amide I), and the ESR analyses showed that the bones were not burned at a temperature higher than 200°C. This implies that the bone remains were not used as fuel by Neanderthals at Kůlna Cave. Coloring in these bones is largely due to the presence of Mn and Fe. © 2006 Wiley Periodicals, Inc.