2012
DOI: 10.1016/j.jas.2012.02.036
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The first direct evidence of pre-columbian sources of palygorskite for Maya Blue

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Cited by 33 publications
(13 citation statements)
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References 39 publications
(73 reference statements)
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“…This is expected because it is well known that the Maya used palygorskite from this area to produce Maya blue (Arnold et al . 2012). The sample from Jiupetec belonging to the colonial period is similar to this group too, considering the R ‐value obtained.…”
Section: Discussionmentioning
confidence: 99%
“…This is expected because it is well known that the Maya used palygorskite from this area to produce Maya blue (Arnold et al . 2012). The sample from Jiupetec belonging to the colonial period is similar to this group too, considering the R ‐value obtained.…”
Section: Discussionmentioning
confidence: 99%
“…Third, the description of the texotli in the Florentine Codex is brief and lacks precision, being in line with the fact that Maya Blue was, in all likewood, not manufactured in the center of Mexico during the Late Postclassic. The painters of the Nahua codices possibly provided themselves with this prized blue from the Maya area through trade or tribute (Milbrath and Peraza Lope 2003:30, 35, 41), for the major deposits of palygorskite are located in the Sierra de Ticul (López et al 2005:26–27; Ortega 2003:11), in northern Yucatán, a region that was also engaged in a large-scale indigo production during the sixteenth century (Arnold 2005; Arnold et al 2012; Ruz 1979; Torres 1988). Last but not least, in the Florentine Codex chapter on colors, the texotli is described just before another ambiguous material called tecozahuitl , a word that designated some hybrid organic-inorganic colors made of clay and yellow dyes.…”
Section: Colorsmentioning
confidence: 99%
“…The plant contains an indoxy glucoside called indican, which is converted to indigo in the process. Palygorskite from Yucatán mines, which are thought to be source for making Maya blue in pre-Columbian times, is white in colour (Arnold et al 2012). Briefly, the structure of palygorskite can be characterized as ribbons of continuous tetrahedral and discontinuous octahedral that are joined by Si-O-Si bonds from which nanopores are formed along the fibre axis (Kuang et al 2004).…”
Section: Maya Bluementioning
confidence: 99%