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

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section, and then were prepared and reduced in a number <strong>of</strong> (Figure 6.3) different<br />

ways.<br />

One <strong>of</strong> the most popular ways <strong>Piedras</strong> <strong>Negras</strong> knappers reduced imported cores<br />

was the pressure reduction <strong>of</strong> blade-cores on one or more sides. <strong>The</strong> best evidence for this<br />

reduction str<strong>at</strong>egy is exhausted cores th<strong>at</strong> fe<strong>at</strong>ure a lenticular cross section with pressure<br />

scars on one face <strong>of</strong> the core and percussion scars on the other (Figure 6.1, upper row).<br />

Consequently, the cross section <strong>of</strong> the core changed through its use-life, probably most<br />

<strong>of</strong>ten from circular to oval, and finally, to a nearly lenticular or “fl<strong>at</strong>” morphology. Small<br />

percussion flakes and blades were removed during the initial prepar<strong>at</strong>ion <strong>of</strong> the core and<br />

after pressure reduction had already begun.<br />

Percussion blades and flakes from household fill and royal caches, which were<br />

further modified into eccentrics, indic<strong>at</strong>e th<strong>at</strong> there was a system<strong>at</strong>ic method <strong>of</strong> core<br />

prepar<strong>at</strong>ion and core maintenance <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>. First, wide percussion flakes were<br />

removed from one face <strong>of</strong> the core (Figures 6.3 and 6.5) to isol<strong>at</strong>e a centrally loc<strong>at</strong>ed<br />

pl<strong>at</strong>form (Figure 6.3). Next, a long, thin blade was removed from the central working<br />

face <strong>of</strong> the core (Figure 6.6). If necessary, flakes and blades were removed from the distal<br />

end <strong>of</strong> the core to complete regulariz<strong>at</strong>ion (Figure 6.7). This spare regulariz<strong>at</strong>ion str<strong>at</strong>egy<br />

was all th<strong>at</strong> was required to begin the pressure reduction <strong>of</strong> the core. <strong>The</strong> best examples<br />

<strong>of</strong> these kinds <strong>of</strong> initial production-debitage come from Yaxche period caches. Since the<br />

obsidian eccentrics from this time are little modified, they retain much <strong>of</strong> the original<br />

evidence <strong>of</strong> blade production and core prepar<strong>at</strong>ion on their dorsal surfaces (Figure 6.8).<br />

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