2011
DOI: 10.1016/j.palaeo.2010.10.044
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An investigation into the internal and external variables acting on crystallinity index using Fourier Transform Infrared Spectroscopy on unaltered and burned bone

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Cited by 81 publications
(76 citation statements)
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References 34 publications
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“…As can be seen, there is a general trend with increased cremation intensity of increasing CI and a drop in C/P. This is in keeping with previously published work (such as Thompson et al 2009;2010). Despite the relatively large standard deviations present (a likely feature of sample size) it is possible to distinguish archaeological unburned bone from archaeological burned bone.…”
Section: Figures 9-11supporting
confidence: 86%
See 1 more Smart Citation
“…As can be seen, there is a general trend with increased cremation intensity of increasing CI and a drop in C/P. This is in keeping with previously published work (such as Thompson et al 2009;2010). Despite the relatively large standard deviations present (a likely feature of sample size) it is possible to distinguish archaeological unburned bone from archaeological burned bone.…”
Section: Figures 9-11supporting
confidence: 86%
“…The colour of each bone was recorded using Munsell soil colour charts (2000). Each sample was taken using a scalpel from the periosteal surface of the anterior distal third of a femoral diaphysis and was stored in a sealed test tube as recommended by Thompson et al (2010). Inhumed samples, from the same anatomical locations, were used as a control for the study.…”
Section: Ftir Analysismentioning
confidence: 99%
“…A baseline correction is usually applied between 750 and 450 cm −1 (Shemesh, 1990;Thompson et al, 2011). As crystal size increases, A 565 and A 605 increase -since they correspond to two anti-symmetric bending vibration bands of phosphate, v 4 PO 4 (Lebon et al, 2010;Thompson et al, 2013) -whilst A 595 decreases, resulting in an overall CI increase .…”
Section: Methods Of Measuring Heat-induced Crystallinity Changementioning
confidence: 99%
“…Los resultados fueron bastante variables, con valores IC entre 2,8 y 6,3. Como los valores IC en materia ósea completamente recristalizada suelen caer entre 5,0 y 7,0, para evitar cualquier riesgo de contaminación postdeposicional por absorción de carbonatos exógenos, se estableció un valor umbral de 5,0 (Thompson et al 2009;Thompson et al 2011). Muestras con un valor IC bajo este umbral se excluyeron del programa, lo que ocasionó la invalidación de la mayoría de las muestras preseleccionadas.…”
Section: Estrategia Y Problemas Del Muestreounclassified