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

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<strong>of</strong> the eccentrics from the site are deriv<strong>at</strong>ions from the mid-size biface trajectories <strong>of</strong> both<br />

local and imported m<strong>at</strong>erials, but some are made by slightly modifying biface-thinning<br />

flakes and nodule reduction flakes. Unifacial knives, unifacial scrapers, blade cores, and<br />

flake cores also are present <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>, but they are largely eclipsed by bifacial<br />

technologies. <strong>The</strong> two less functionally desirable types <strong>of</strong> debitage from nodule<br />

reduction, and also biface-thinning flakes, were <strong>of</strong>ten deposited in elite burial and cache<br />

contexts <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>. This p<strong>at</strong>tern resembles those from other sites in Mesoamerica,<br />

such as Teotihuacan and Tikal (Moholy-Nagy 1997).<br />

At <strong>Piedras</strong> <strong>Negras</strong> 4,557 chert artifacts and debitage pieces were found in<br />

commoner and elite contexts. More than 100 newly discovered chert eccentrics, mostly<br />

from cache deposits in royal structures, also are included in this total. Only one possible<br />

workshop dump <strong>of</strong> ~3,000 flakes was found in the South Group (Oper<strong>at</strong>ion 15), but they<br />

consist <strong>of</strong> l<strong>at</strong>e-stage, biface percussion-flakes and pressure flakes from biface reduction<br />

and resharpening. <strong>The</strong> only deposits containing debitage taken directly from a large-<br />

biface workshop were from royal architectural and burial contexts. <strong>The</strong> majority <strong>of</strong> biface<br />

thinning flakes and other production debitage comes from household fill and detritus left<br />

on abandoned house floors. Specific flakes mark production activities, and visual<br />

sourcing indic<strong>at</strong>es whether th<strong>at</strong> m<strong>at</strong>erial was <strong>of</strong> local or nonlocal origin.<br />

4.1.3.1: Distribution <strong>of</strong> microcrystalline quartzes. <strong>The</strong> m<strong>at</strong>erials I recorded for the<br />

<strong>Piedras</strong> <strong>Negras</strong> artifacts were chert (C), silicified limestone (SL), chalcedony (CH),<br />

dolomite and dolomitic limestone (D), petrified wood (PW), flint (F), and quartzite (QZ).<br />

103

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