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The Organization of Chipped-Stone Economies at Piedras Negras ...

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understanding <strong>of</strong> m<strong>at</strong>erial percentages. <strong>The</strong> rows with question marks next to them are<br />

obsidians th<strong>at</strong> were guessed <strong>at</strong> due to unusual vari<strong>at</strong>ions in visual characteristics. All <strong>of</strong><br />

the non-El Chayal obsidians are only found in small quantities with Ixtepeque (1.7% by<br />

count and .9% by weight) and San Martín Jilotepeque (1.31% by count and 1.46% by<br />

weight) representing the other two most prominent sources. <strong>The</strong> percentage <strong>of</strong> El Chayal<br />

obsidian from general excav<strong>at</strong>ions (96.51% by count and 95.74% by weight) is slightly<br />

lower than for cached obsidian (97.86% by count and 97.13% by weight), with a total <strong>of</strong><br />

96.61% by count and 96.37% by weight for all recorded obsidian artifacts. Obsidian from<br />

caches represents 7.15% <strong>of</strong> all obsidian by count and 46.45% by weight, while obsidian<br />

artifacts from general excav<strong>at</strong>ions are 92.85% by count and 53.55% by weight. <strong>The</strong><br />

reason for this gre<strong>at</strong> disparity is th<strong>at</strong> exhausted cores and other large pieces <strong>of</strong> production<br />

debitage were used to make the eccentrics <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>. This p<strong>at</strong>tern is discussed<br />

further in Chapter 7 and 8.<br />

Other p<strong>at</strong>terns are revealed when the m<strong>at</strong>erials are examined by area <strong>of</strong> the site<br />

(Table 4.5), and by ceramic phase (Table 4.6). <strong>The</strong> general tendency is th<strong>at</strong> non-El<br />

Chayal, Gu<strong>at</strong>emalan obsidians appear to be imported with less frequency over time, such<br />

as San Martín Jilotepeque obsidian. However, Ixtepeque obsidian becomes more frequent<br />

over time, especially in the Chacalhaaz phase. With the onset <strong>of</strong> the L<strong>at</strong>e Classic,<br />

Mexican obsidians become more frequent <strong>at</strong> the site, but then disappear with the end <strong>of</strong><br />

the Chacalhaaz phase and the possible decline <strong>of</strong> the royal dynasty. <strong>The</strong>se basic p<strong>at</strong>terns<br />

resemble others from the Maya area (Clark and Nelson 1998), though with a higher<br />

percentage <strong>of</strong> El Chayal obsidian than most places.<br />

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