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Santander, February 19th-22nd 2008 - Aranzadi

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Of Shell and Sand: Coastal Habitat Availability and Human Foraging Strategies at Punta Candelero (Humacao, Puerto Rico)<br />

275<br />

using heavy machinery after Miguel Rodríguez’s<br />

archaeological intervention in the late 1980s and<br />

early 1990s, and was then covered with a thick layer<br />

of rubble fill (up to a metre thick in some areas).<br />

Recent development has widely impacted the<br />

region, and the original topography has been severely<br />

modified. The shoreline is classified as of moderate<br />

to high erosion risk, based on wave intensity.<br />

The littoral presents a wide and rich mosaic of<br />

habitats very close to the shore. Modern benthic<br />

habitats, as classified by the National Oceanic and<br />

Atmospheric Administration’s Biogeography Team<br />

(NOAA 2001), include various types of consolidated<br />

substrates such as bedrock, corals and other<br />

reefs, as well as sandy shores, sea grass habitats<br />

and patches of macroalgae (Figure 4).<br />

Figure 3. Punta Candelero showing the location of the suggested 'shell middens'.<br />

White dots mark the sampled units for this study (Satellite image modified<br />

from Google Earth 2004 image, 18°05’33.50”N 65°47’26.76”W).<br />

2007 due to proposed development on the land<br />

plot. This project intervened only on the north section<br />

of the site, which had been identified by<br />

Miguel Rodríguez as “Cuevas zone” of the Late<br />

Saladoid Period, estimating its date to 400 – 800<br />

AD (Rodríguez-López 1991).<br />

Radiocarbon dates from charred wood samples<br />

from features excavated during the 2006 project<br />

range between 660 – 1020 Cal AD (Beta<br />

Analytic Laboratory, 2σ calibration) (see Ramos-<br />

Vélez et al. 2007 for details on the dates and their<br />

calibration). All samples were within Cuevas<br />

Period context. During his excavations in the late<br />

1980s, M. Rodríguez obtained a similar date<br />

range, but he found the dates confusing<br />

(Rodríguez-López 1991) because they are too late<br />

compared with the accepted Saladoid chronology<br />

established by Irving Rouse (Rouse 1992). The<br />

radiocarbon dates obtained by M. Ramos confirm<br />

the late character of the Saladoid occupation on<br />

Punta Candelero (Ramos et al. 2007). Similar<br />

dates have been obtained from other characteristically<br />

Saladoid sites, which challenge Rouse’s<br />

chronology based on ceramic typology (see<br />

Ramos-Vélez et al. 2007 for discussion).<br />

1.2. Modern Context<br />

The modern ecological conditions of the foreland<br />

are degraded. Most of its surface was levelled<br />

1.3. Palaeolandscape<br />

According to the geoarchaeological study<br />

(Rivera-Collazo 2007b), Punta Candelero’s environmental<br />

and landscape setting contemporaneous<br />

with the occupation at the site was complex<br />

and rich. The foreland was formed as part of the<br />

depositional processes of Candelero River mouth,<br />

forming a deltaic environment with a possible<br />

sandbar separating the river from the sea and<br />

making it flow south. Although more data is necessary,<br />

the available information suggests that the<br />

sea level at the time of occupation could have<br />

been about 20 – 30cm lower than today. Swampy<br />

deposits between the site and the sea seem to be<br />

associated with the ancient river channel, contemporary<br />

with the site’s occupation. The immediate<br />

landscape included riparian, estuarine and marine<br />

environments within just a few minutes walk.<br />

Terrestrial resources were not far away either, possibly<br />

consisting of dense tropical forests.<br />

Deltas are excellent examples of ecotonal conditions,<br />

presenting the conjunction between marine,<br />

terrestrial and riparian environments. Ecotones<br />

yield a very high ratio of different types of resources,<br />

maximizing returns and minimizing risks for<br />

foragers (Dincauze 2000). According to the<br />

Optimal Foraging Theory (OFT) (Borgerhoff<br />

Mulder 2004, Cronk 1991, Pyke 1984), site location<br />

inside an ecotonal resource patch would facilitate<br />

the exploitation of local microenvironments with<br />

minimum risk and time investment (Binford 1980,<br />

Perlman 1980, Raab 1992, Thomas 2007). If the<br />

inhabitants of Punta Candelero were behaving in<br />

accordance with the OFT, then the shells of Punta<br />

Candelero should evidence exploitation of environments<br />

in the immediate vicinity of the site.<br />

MUNIBE Suplemento - Gehigarria 31, 2010<br />

S.C. <strong>Aranzadi</strong>. Z.E. Donostia/San Sebastián

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