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Dialogues in Cuban Archaeology

by L. Antonio Curet, Shannon Lee Dawdy, and Gabino La Rosa Corzo

by L. Antonio Curet, Shannon Lee Dawdy, and Gabino La Rosa Corzo

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Early Ceramics <strong>in</strong> the Caribbean / 107<br />

larities with some of the early pottery of the Valdivia phase of Ecuador (Meggers<br />

et al. 1965), as well as with the well-known styles of northeastern Venezuela<br />

known as Santa Ana and Tocuyano (Sanoja 2001:4). Accord<strong>in</strong>g to<br />

Sanoja, the material of Camay exhibits characteristics that correspond to socalled<br />

Periods B (4300–4000 b.p. or 2350–2050 b.c.) and C (4000–3400 b.p.<br />

or 2050–1450 b.c.) of Valdivia. This suggests a chronological correlation that,<br />

if con¤rmed, would substantially revise the theories of the peopl<strong>in</strong>g of the<br />

Venezuelan northeast, the Andean region, and Lake Maracaibo, besides shedd<strong>in</strong>g<br />

light on some of the particularities that characterize the later ceramic<br />

styles of the region. This new perspective makes the Venezuelan northeast a<br />

nuclear center whose cultural <strong>in</strong>®uences would have contributed to shap<strong>in</strong>g<br />

the aborig<strong>in</strong>al societies of much of northeastern South America. The groups<br />

of the Camay and Quibor valleys may have begun to develop tribal or neolithic<br />

social characteristics <strong>in</strong> the second millennium b.c. and <strong>in</strong>itiated the<br />

transition toward complex hierarchical social forms around the ¤rst millennium<br />

(Sanoja 2001:17–18; see Arvelo 1995 for a different position on the social<br />

developments <strong>in</strong> this sequence).<br />

In Central America, some shell middens like Monagrillo (4500–3200 b.p.<br />

or 2550–1250 b.c.), located <strong>in</strong> the Gulf of Panama, have evidence of a ceramic<br />

<strong>in</strong>dustry related to the use and exploitation of nearby resources <strong>in</strong> the mangrove<br />

swamp. The pottery at this site supports the impression that this location<br />

was home to an important phase <strong>in</strong> the dispersion and exchange of ceramic<br />

traditions <strong>in</strong> the Americas. A marked similarity between this ¤rst<br />

Panamanian pottery and that from sites <strong>in</strong> Colombia, such as Puerto Hormiga,<br />

supports this view (Veloz Maggiolo 1991). 1 To this we have to add the<br />

bene¤ts of the mar<strong>in</strong>e resources that <strong>in</strong> some general ways may have <strong>in</strong>®uenced<br />

the shifts of the ¤rst forag<strong>in</strong>g/ceramic groups under similar conditions.<br />

In general, the shell middens with ceramics from Colombia, the coast of<br />

Venezuela, Guyana, and Panama may re®ect a phase of growth and <strong>in</strong>tensi¤cation<br />

of forag<strong>in</strong>g lifeways <strong>in</strong> the cont<strong>in</strong>ental or river<strong>in</strong>e Caribbean, characterized<br />

by experimentation with some horticultural practices and the manufactur<strong>in</strong>g<br />

of wood-work<strong>in</strong>g <strong>in</strong>struments and tools. Assemblages of simple<br />

pottery appear to be correlated with an <strong>in</strong>crease <strong>in</strong> site size and the production<br />

of gr<strong>in</strong>d<strong>in</strong>g tools. All this seems to be <strong>in</strong> agreement with the transformations<br />

that took place <strong>in</strong> the economy of forag<strong>in</strong>g societies, <strong>in</strong> which the consumption<br />

of vegetable foods shifted from marg<strong>in</strong>al importance to become a central<br />

production process. It is important to keep <strong>in</strong> m<strong>in</strong>d that <strong>in</strong> spite of the peculiarities<br />

of each site, pottery is an element present at each one. While this does

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