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Pre-Colombian Jamaica: Caribbean Archeology and Ethnohistory

by Phillip Allsworth-Jones

by Phillip Allsworth-Jones

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180 / Appendix A.<br />

viduals, one adult <strong>and</strong> one juvenile. In addition, three shark vertebra beads were<br />

found in the vicinity. No other remains of shark were found, <strong>and</strong> in Carlson’s<br />

opinion these beads were not manufactured at the site. They very likely accompanied<br />

the human remains.<br />

A total of 4,202 bones make up the analyzed assemblage, representing a<br />

minimum number of individuals (MNI) of 154. Excluding the pig, the vertebrate<br />

fauna consists of the following species: 24 fishes <strong>and</strong> sharks, two mammals,<br />

four birds, <strong>and</strong> two reptiles. Most numerous in terms of MNI were fish,<br />

with 103 individuals, followed by hutía with 34 individuals. The most common<br />

fish were freshwater sleepers (Eliotridae) followed by groupers (Serranidae).<br />

As Carlson points out, this is not surprising, granted the site’s immediate<br />

proximity both to numerous rivers <strong>and</strong> to Annotto Bay. She states that 72 percent<br />

of the usable meat weight in the diet was provided by marine species <strong>and</strong><br />

25 percent by hutía. It should be noted that the reptiles included two individuals<br />

attributed to the <strong>Jamaica</strong>n giant galliwasp (Celestus occiduus) <strong>and</strong> there<br />

was at least one parrot, either black or yellow billed (Amazona agilis/ collaria).<br />

Both species are endemic, <strong>and</strong>, as Carlson remarks, they would presumably<br />

have been captured for their feathers.<br />

References: AJ 1970, 1:1, 2; 1972, 2:2; 1978, 1:3 <strong>and</strong> Figure 1; 1982, 1:6;<br />

1982, 4:6, 7, 9; 1984, 4:40; Carlson 2004; Cassidy 1988; Osborne 1973; Padrón<br />

1952; R<strong>and</strong>el 1960; Yates <strong>and</strong> Thompson 1959–1960.<br />

Green Castle (Y25)<br />

Reported by Miss Jean Crum- Ewing in 1978 <strong>and</strong> mapped by Lee in that year.<br />

Also known as Davey Hill #1. Lee recorded that the property road at that time<br />

cut through midden material for a distance of 100 m, the maximum depth of<br />

deposit observed by him being about 60 cm. The finds were said to be located<br />

in a matrix of gray- black soil, above a subsoil of buff marl grading into coral<br />

limestone. Artifacts remarked upon by Lee included pottery with cross-hatched<br />

incised decoration, both plain <strong>and</strong> filleted rim sherds, griddles, flint flakes, <strong>and</strong><br />

hammerstones of igneous or metamorphic rock. One s<strong>and</strong>stone net sinker was<br />

found on the surface. A joint team from UWI <strong>and</strong> Murray State University carried<br />

out excavations in 1999–2001 ( Allsworth- Jones <strong>and</strong> Wesler 2003).<br />

Six trenches have been excavated. The three westernmost trenches were<br />

shallow <strong>and</strong> yielded very little information. The northernmost trench was also<br />

quite shallow <strong>and</strong> was affected by erosion <strong>and</strong> deflation. The mid trench on the<br />

eastern side <strong>and</strong> the southernmost trench, however, were very productive. The<br />

southernmost trench produced the most complete stratigraphy, to a maximum

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