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

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core such as is used in the Middle Usumacinta region (Lee and Hayden 1989). Similar<br />

unifaces have been recorded for the northern Maya Lowlands (Rovner and Lewenstein<br />

1997:34), but these may have been made from percussion flakes, and not blades. <strong>The</strong> few<br />

<strong>Piedras</strong> <strong>Negras</strong> examples were made from blades, and were reduced by a pressure-flaking<br />

technique th<strong>at</strong> only moder<strong>at</strong>ely affected the original blade. Some examples from outside<br />

the <strong>Piedras</strong> <strong>Negras</strong> area, which appear to be projectile points, may have also been used as<br />

drills, but microscopic use-wear analyses are needed to confirm these two functions.<br />

5.4.1.3.7: Small laurel leaf biface (see Figure 5.2 #28). This type was made from a small<br />

nodule reduction flake or a large, biface-thinning flake. It was reduced by pressure, and<br />

was finished with pressure. It was 8 cm or less in length. <strong>The</strong> distal and proximal ends are<br />

pointed and roughly symmetrical. A thin, lenticular cross section was the desired result <strong>of</strong><br />

the reduction process.<br />

This biface is the most common small biface <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong> and may have<br />

been used as a small knife, spear point, or as an <strong>at</strong>l<strong>at</strong>l dart point, especially for smaller<br />

versions. Some examples are small enough to be hafted as arrowheads, but none have<br />

been found in Postclassic contexts where arrow technologies might have existed in the<br />

Usumacinta region. Specimens from the <strong>Piedras</strong> <strong>Negras</strong> sample show use-wear evidence<br />

<strong>of</strong> cutting, which suggests th<strong>at</strong> even the smallest laurel-leaf bifaces also were used as<br />

knives <strong>at</strong> one point in their use-life. <strong>The</strong>y are finely pressure flaked and are made <strong>of</strong> fine<br />

microcrystalline quartzes, including he<strong>at</strong>-tre<strong>at</strong>ed local cherts and chalcedonies.<br />

184

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