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Crossing the Borders: New Methods and Techniques in the Study of Archaeological Materials from the Caribbean

by Corrine L. Hoffman, et. al.

by Corrine L. Hoffman, et. al.

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96 / Benoît Bérard<br />

thick flakes produced dur<strong>in</strong>g <strong>the</strong> first phase. This work is realized by <strong>the</strong> bipolar<br />

technique us<strong>in</strong>g a preferential strik<strong>in</strong>g platform (Figure 7.2a). The knappers try to<br />

obta<strong>in</strong> small straight flakes. That second phase <strong>of</strong> <strong>the</strong> débitage, which is recurrent<br />

<strong>and</strong> well organized, is realized more carefully. The very small size <strong>of</strong> some cores<br />

implies <strong>the</strong> use <strong>of</strong> some specific prehensile systems.<br />

Different elements can be highlighted <strong>in</strong> that short presentation. The method<br />

<strong>of</strong> reduction is relatively simple. The reduction process is very short, <strong>and</strong>, <strong>in</strong> general,<br />

only a few products are obta<strong>in</strong>ed (especially dur<strong>in</strong>g <strong>the</strong> first phase). However,<br />

<strong>the</strong> method used is really efficient <strong>and</strong> quick: a m<strong>in</strong>imum <strong>of</strong> time <strong>and</strong> <strong>of</strong> percussion<br />

<strong>in</strong>stances is necessary to obta<strong>in</strong> a small set <strong>of</strong> flakes. Even though <strong>the</strong> early<br />

Cedrosan Saladoid reduction strategies are simple <strong>and</strong> poorly organized, <strong>the</strong>y are<br />

not entirely opportunistic. This is proven by <strong>the</strong> clear articulation exist<strong>in</strong>g between<br />

<strong>the</strong> two goals described above. Ra<strong>the</strong>r than opportunism, <strong>the</strong> débitage reveals<br />

that <strong>the</strong> knappers have a large freedom <strong>of</strong> action, freedom l<strong>in</strong>ked with a<br />

low level <strong>of</strong> social <strong>and</strong> cultural <strong>in</strong>vestment. The most characteristic element is <strong>the</strong><br />

knapp<strong>in</strong>g <strong>of</strong> <strong>the</strong> small flakes by <strong>the</strong> bipolar technique. I will try to see now if that<br />

cultural <strong>in</strong>vestment is sufficient to support our comparative study.<br />

Huecan Saladoid Knapp<strong>in</strong>g Technology<br />

The presentation here <strong>of</strong> <strong>the</strong> Huecan Saladoid reduction technique is based on <strong>the</strong><br />

analysis <strong>of</strong> a collection com<strong>in</strong>g <strong>from</strong> <strong>the</strong> site <strong>of</strong> La Cathédrale de Basse- Terre <strong>in</strong><br />

Guadeloupe. The site was excavated <strong>in</strong> 2002 under <strong>the</strong> direction <strong>of</strong> Bonnissent <strong>and</strong><br />

Romon. 3 It is composed <strong>of</strong> an Early Ceramic Age occupation partially disturbed by<br />

a colonial cemetery. The débitage rema<strong>in</strong>s presented here come <strong>from</strong> <strong>the</strong> test pits 1<br />

(a 2 x 2 m test pit) <strong>and</strong> 7 (a 3 x 5 m test pit). Two occupational levels, none clearly<br />

<strong>in</strong>dividualized, constitute <strong>the</strong> Amer<strong>in</strong>dian occupation <strong>of</strong> that site. Follow<strong>in</strong>g <strong>the</strong><br />

analysis <strong>of</strong> <strong>the</strong> ceramic rema<strong>in</strong>s (Bonnissent <strong>in</strong> Bonnissent <strong>and</strong> Romon 2004), <strong>the</strong><br />

lower level is associated to <strong>the</strong> Huecan Saladoid subseries <strong>and</strong> <strong>the</strong> upper one is considered<br />

as a mix or a transitional level associat<strong>in</strong>g elements l<strong>in</strong>ked to <strong>the</strong> Huecan<br />

<strong>and</strong> <strong>the</strong> Cedrosan subseries. At this stage, I have not been able to identify a pert<strong>in</strong>ent<br />

technical variation <strong>in</strong> <strong>the</strong> lithic collection associated with that chronological<br />

or spatial division, <strong>the</strong>refore I will make a global presentation <strong>of</strong> <strong>the</strong> débitage rema<strong>in</strong>s<br />

com<strong>in</strong>g <strong>from</strong> <strong>the</strong> two test pits <strong>and</strong> <strong>the</strong> two levels. Two hundred <strong>and</strong> forty<br />

eight pieces <strong>of</strong> débitage constitute that collection.<br />

The raw materials used are ma<strong>in</strong>ly Long Isl<strong>and</strong> (Antigua) fl<strong>in</strong>t (64 percent).<br />

This type <strong>of</strong> fl<strong>in</strong>t is characterized by <strong>the</strong> presence <strong>of</strong> a white chalky cortex <strong>and</strong><br />

a clear brown to dark gray color. Long Isl<strong>and</strong> is <strong>the</strong> major source <strong>of</strong> siliceous raw<br />

materials for <strong>the</strong> nor<strong>the</strong>rn part <strong>of</strong> <strong>the</strong> Lesser Antilles (see Knippenberg this volume).<br />

Igneous stones (<strong>and</strong>esite <strong>and</strong> basalt, 10 percent), red jasper (7 percent), <strong>and</strong><br />

a set <strong>of</strong> amorphous silicifications (sedimentary or hydro<strong>the</strong>rmal) compose <strong>the</strong> rest<br />

<strong>of</strong> <strong>the</strong> sample. Igneous stones can be found around 10 km away <strong>from</strong> <strong>the</strong> site to <strong>the</strong><br />

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