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Developments in Ceramic Materials Research

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Postclassic Maya <strong>Ceramic</strong> Advances 21<br />

Figure 8. Plot of cerium and cesium base-10 logged concentrations show<strong>in</strong>g the separation of the three<br />

Snail-Inclusion Paste ware chemical compositional groups. Samples were analyzed by INAA. Ellipses<br />

represent 90% confidence <strong>in</strong>tervals for group membership.<br />

In addition to reaffirm<strong>in</strong>g the differences with<strong>in</strong> each ware that were obta<strong>in</strong>ed from<br />

m<strong>in</strong>eralogical analyses, INAA is the best method by which to compare clays to pottery <strong>in</strong> an<br />

attempt to locate resource areas. In this study several clays (white, orange, yellow, and gray <strong>in</strong><br />

color) were obta<strong>in</strong>ed from around Lake Yaxhá and Lake Petén Itzá 2 <strong>in</strong> an attempt to <strong>in</strong>fer<br />

local resources used <strong>in</strong> pottery manufacture. The clays from around Lake Yaxhá plot with<strong>in</strong><br />

two Clemencia Cream Paste ware macro-groups (ash paste and non-ash paste) (Figure 9).<br />

Four clays demonstrate statistical membership 3 with<strong>in</strong> the non-ash paste ceramic group<br />

suggest<strong>in</strong>g that these clays could have been used to manufacture Clemencia Cream Paste<br />

ware pottery (Table 3).<br />

Clay sample LGC111 consistently plots with<strong>in</strong> the ash group, but because the sherd<br />

sample size for that group is small, statistical membership cannot be determ<strong>in</strong>ed with any<br />

certa<strong>in</strong>ty. In addition to the Clemencia Cream Paste wares, two clay samples (one orange and<br />

one yellow) were collected from private property near the archaeological site of Ch’ich’.<br />

They were projected aga<strong>in</strong>st the three chemical compositional groups of the Vitzil Orange-<br />

Red ware pottery.<br />

2 All but one of the white clays were sampled by Prudence M. Rice dur<strong>in</strong>g the Historical Ecology Project. Sample<br />

LGC111 was a non-naturally occurr<strong>in</strong>g deposit excavated from Structure 719 at Zacpetén. The red clays were<br />

collected <strong>in</strong> 2006 by the author from private land between the archaeological sites of Ch’ich’ and Tr<strong>in</strong>idad de<br />

Nosotros. The gray clay samples were collected <strong>in</strong> 1998 by the boat launch area at the archaeological site of<br />

Zacpetén.<br />

3 The threshold for statistical membership of clay samples with<strong>in</strong> ceramic sherd compositional groups is much<br />

lower than that for creat<strong>in</strong>g ceramic sherd compositional groups (typically above 5.000) because the addition<br />

of temper<strong>in</strong>g material to raw clays does changes the chemical composition so much so that there is rarely a<br />

match at the 5.000 level. Therefore, it is common practice at MURR to suggest that clays may represent<br />

sources for pottery manufacture if there is a probability above 0.300.

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