2018
DOI: 10.1016/j.jasrep.2018.01.035
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Chemical and mineralogical characteristics of the pigments of archaeological rupestrian paintings from the Salão dos Índios site, in Piauí, Brazil

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Cited by 5 publications
(7 citation statements)
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“…Red and yellow pigments are typically associated with iron-oxide related minerals, specifically, hematite and goethite 23,24 . It is well known that, under heating, goethite dehydrates forming hematite, which has been shown to be initially formed as micro or nano domains.…”
Section: Resultsmentioning
confidence: 99%
“…Red and yellow pigments are typically associated with iron-oxide related minerals, specifically, hematite and goethite 23,24 . It is well known that, under heating, goethite dehydrates forming hematite, which has been shown to be initially formed as micro or nano domains.…”
Section: Resultsmentioning
confidence: 99%
“…Phosphorous (P) can also indicate the presence of alteration deposits, attributed to organic material from the decomposition of small-sized building insects or their excrements. 7,29 The occurrence of these deposits is quite common in open-air sites, as in the case of the archaeological Site of Ema, since they are more vulnerable to problems of natural origin. Perhaps, for this reason, the SE1901 sample presented the highest signal intensity for this element.…”
Section: Ed-xrfmentioning
confidence: 99%
“…1,10 As a source of gypsum was not found nearby the site, the hypothesis that the rupestrian art was made from pigments based on this mineral and then taken to Ema Site by precolonial painters cannot be discarded, since they maintained a nomadic lifestyle (hunter-gatherers), and the Araripe sedimentary basin, rich in this mineral, is located just over 200 kilometers from the city of Inhuma. 30 Although the literature 1,17,29,31,32 indicates pyrolusite (MnO 2 ) as one of the substances responsible for the black coloration of natural mineral pigments, observed in some rupestrian paintings, this possibility was discarded, due to the absence of an analytical signal for manganese (Mn) in the sample SE1903. This suggests that this pigment may have been prepared from carbonized organic materials (bones or vegetables).…”
Section: Ed-xrfmentioning
confidence: 99%
“…Of the five frequency shifts, only one peak at 155 cm −1 was found in the KR1 sample. The Raman peaks at 397 and 413 cm −1 (dos Santos et al, 2018) were assigned to hematite, although phases of hematite were absent in the XRD. Hematite occurs in nature and can exist as impurities in the main pigment materials.…”
Section: Paint Layer (Pigment Samples)mentioning
confidence: 99%