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

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probably was on a smaller scale than other production locales in <strong>Piedras</strong> <strong>Negras</strong> <strong>at</strong> th<strong>at</strong><br />

time. <strong>The</strong>se residential groups do not appear to be involved in obsidian blade production<br />

<strong>at</strong> any other time.<br />

In a similar way, PN24 and PN25 do not provide strong evidence <strong>of</strong> obsidian-<br />

blade production <strong>at</strong> any time. PN25, which is loc<strong>at</strong>ed on the east side <strong>of</strong> the acropolis,<br />

may have been involved in blade production during the Chacalhaaz phase, but only<br />

further excav<strong>at</strong>ion in this group can determine whether the initial production p<strong>at</strong>tern<br />

holds. For this study, however, PN25 is marked as a blade producer during Chacalhaaz<br />

times. PN24 is problem<strong>at</strong>ic in the sense th<strong>at</strong> there is such a low proportion <strong>of</strong> production<br />

debitage in the lithic samples. It is possible th<strong>at</strong> the residential group <strong>of</strong> PN24 was<br />

involved in blade production during the Yaxche phase, but it has a low production value<br />

score, and a low proportion <strong>of</strong> blade-production debitage to other obsidian artifacts. One<br />

possible explan<strong>at</strong>ion for the existence <strong>of</strong> scant production debitage in the PN24<br />

excav<strong>at</strong>ions is th<strong>at</strong> it was closely connected to the acropolis during Yaxche times (see<br />

Fitzsimmons and Muñoz 2001; Golden and Muñoz 2005). Royal garbage was deposited<br />

around this household group, and the production debitage may have origin<strong>at</strong>ed from<br />

acropolis. PN24 remains problem<strong>at</strong>ic as a producer for the Yaxche phase, but is an<br />

excellent example <strong>of</strong> a blade consumer during Chacalhaaz times.<br />

In contrast to the PN24 excav<strong>at</strong>ions, the residential groups <strong>of</strong> PN23 and PN33<br />

appear to have been involved in obsidian-blade production over a long period <strong>of</strong> time,<br />

and perhaps with a gre<strong>at</strong>er intensity than other areas <strong>of</strong> the site, especially the U Group<br />

(Oper<strong>at</strong>ion PN33). <strong>The</strong> U Group yielded almost three times more obsidian artifacts than<br />

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