Despite the fact that the Taíno people of the Caribbean were the first Native Americans to encounter and coexist with Europeans after 1492, there has been almost no archaeology of Taíno response to that encounter. This study explores the reasons for (and consequences of) this neglect, and their larger implications for American contact-period archaeology. It also challenges prevailing historical models of Taíno social disintegration, drawing upon six years of archaeological work at the En Bas Saline site in Haiti, the only extensively excavated Taíno townsite occupied both before and after contact. Our results, organized by a household-scale analytical framework emphasizing Taíno constructions of gender and class, suggest that there were few major alterations to traditional Taíno social practice during the post-contact period, and most of these were related to activities thought to have been the domain of non-elite Taíno men. It is suggested that the relatively nonspecialized gender roles among the Taíno, as well as the clearly differentiated nature of their social classes, may have served as mitigating factors in the disruption of Taíno cultural practice under Spanish domination. This work also reveals a marked Taíno resistance to the incorporation of European cultural elements, which provides a striking contrast to the Spanish patterns documented in contact-era European towns, and underscores the critical importance of incorporating gender relations into studies of culture contact.

The prehistoric Hohokam conducted a great variety of activities in the spaces between their villages, including social gatherings and ceremonial observances as well as economic and subsistence practices. Recent full-coverage pedestrian survey along the middle Gila River in central Arizona indicates that nonresidential sites are more numerous and cover considerably greater area than residential settlements. Unfortunately, in the Hohokam region researchers are not always able to distinguish residential sites from activity areas based on features observable on the surface. In this study, quantitative measures of artifact density and diversity of surface collections from artifact scatters are used to distinguish residential sites from nonresidential sites. This is accomplished by assessing the extent to which their assemblages resemble artifact collections from known habitations, campsites, or specialized or diverse activity loci. Differences in artifact density and diversity enable many ambiguous artifact scatters to be classified into these general functional site types. Knowing the distribution of site types relative to elements of the natural and cultural landscapes can provide insight into past social and ecological or economic behaviors not offered by site-specific approaches. The study concludes that considering both the physical and cultural dimensions of landscapes significantly increases the research value of nonresidential sites for understanding the use and meaning of spaces between villages.

“Brownware” pottery technologies became widely used in the Great Basin around 600 years ago. A significant increase in the use of small seeds within the subsistence economy took place about the same time. I suggest that these two events are linked, that people consciously chose to focus on seeds because they could be privatized, that is, they could be individually owned and were not subject to unrestricted sharing. Pots were an integral component of this process because they could be individually made and owned and could be used within domiciles, placing food preparation and storage out of view from others in the community. Privatization of a staple food resource may have been a response to increased population size and, hence, the number of freeloaders, new village kinship organizations, and a desire to create surplus on the part of aggrandizers.

This paper tests existing models of coastal subsistence strategies and settlement patterns of the late prehistoric inhabitants of the Southeastern U.S. Atlantic coastal plain. Excavations at Grove's Creek Site (09CH71), Skidaway Island, Georgia were conducted to determine the season of occupation of the site. Paleoethnobotanical and zooarchaeological data were used to determine the subsistence strategies of the inhabitants. Stable isotope analysis of oyster shells is combined with the faunal and botanical data to determine the seasons of occupation of the site. The most notable discovery was the diversity of agricultural plants. Paleoethnobotanical data indicate a spring through autumn occupation, and the stable isotope data indicate winter through summer. Faunal data suggest occupation from spring through early winter. Therefore, the site was occupied year-round. This information, coupled with other data from the Southeastern U.S. Atlantic Coast, suggests a revision to existing subsistence and settlement pattern models. Coastal peoples lived in permanent villages and relied on a mix of agriculture, hunting, fishing, and gathering. Short trips were likely made to procure some resources, but there was not an extensive seasonal round.

One of the most prominent but least understood demographic phenomena in the precontact Southwest is the disappearance of the Hohokam from the valleys of southern Arizona. Despite extensive research, no widely accepted explanation has been offered. We argue that the failure to identify a satisfactory cause is due to excessive focus on catastrophic phenomena and terminal occupations, and a lack of attention to gradual demographic processes. Based on a combination of macro-regional population studies and local research in the lower San Pedro River valley, we present an explanation for gradual population decline precipitated by social and economic coalescence beginning in the late A.D. 1200s. In the southern Southwest an influx of immigrants from the north led to a shift from a dispersed, extensive settlement/subsistence strategy to increased conflict, aggregation, and economic intensification. This shift resulted in diminished health and transformation from population growth to decline. Over approximately 150 years gradual population decline resulted in small remnant groups unable to maintain viable communities. Small, terminal populations were ultimately unable to continue identifiable Hohokam cultural traditions and consequently disappeared from the archaeological record of southern Arizona, either through migration or a shift in lifestyle that rendered them archaeologically invisible.

In late 2001, investigators excavated a solitary Middle Archaic burial from the Plains-Prairie border in east-central Kansas. The burial was contained in a dissected colluvial apron at the foot of the valley wall, in a soil horizon that began accumulating around 9000 B.P. Burial goods include deer bone, a drill, and a side-notched projectile point/knife, the morphology of which is consistent with side-notched Middle Archaic points of the North American Central Plains and Midwest. Use-wear analysis shows that the stone tools were used before being placed with the burial and were not manufactured specifically as burial goods. A radiocarbon assay of the deer bone in direct association with the burial yielded a radiocarbon age of 6160 ± 35 B.P. This is one of only a few burials older than 5,000 years in the region. Comparison of this burial to other coeval regional burials shows similarities in burial practices.

Plasma oxidation was used to obtain radiocarbon dates on six different materials from a naturally mummified baby bundle from the Lower Pecos River region of southwest Texas. This bundle was selected because it was thought to represent a single event and would illustrate the accuracy and precision of the plasma oxidation method. Five of the materials were clearly components of the original bundle with 13 dates combined to yield a weighted average of 2135 ±11 B.P. Six dates from a wooden stick of Desert Ash averaged 939 ± 14 B.P, indicating that this artifact was not part of the original burial. Plasma oxidation is shown to be a virtually nondestructive alternative to combustion. Because only sub-milligram amounts of material are removed from an artifact over its exposed surface, no visible change in fragile materials has been observed, even under magnification. The method is best applied when natural organic contamination is unlikely and serious consideration of this issue is needed in all cases. If organic contamination is present, it will have to be removed before plasma oxidation to obtain accurate radiocarbon dates.

The purpose of this paper is to report the occurrence of obsidian artifacts from Early Woodland contexts in southwestern Wisconsin. During 1995 excavations at the Tillmont site (47CR460), seven obsidian flakes were recovered from a deeply buried paleosol in association with a virtually “pure” component of the Indian Isle phase, a local variant of the Early Woodland Marion Culture (Stoltman 1990:242–244). Geochemical analyses of four of the flakes confirm that Obsidian Cliff, Wyoming, was the source, demonstrating that this distinctive material was in use among Woodland peoples of the Midwest several centuries before the commencement of the Hopewell Interaction Sphere.

An inscribed stone reportedly excavated by an employee of the Smithsonian Institution from a burial mound in eastern Tennessee, and published by Cyrus Thomas in his 1894 landmark report, has been promoted by transatlantic contact enthusiasts as incontrovertible proof of Precolumbian Old World contacts. The inscription is fraudulent, having been copied from a Masonic treatise. We present the source of the inscription and discuss other circumstances concerning the stone and its purported discovery.

In many regions, fluctuations have occurred through time in the local 14C activity of seawater. Evaluating these shifts and their effects on 14C age estimates is difficult, and, as a result, archaeologists working in coastal settings tend to preferentially date charcoal samples over shell. Our research on 18 charcoal–shell pairs from Puget Sound and Gulf of Georgia archaeological sites helps elucidate the spatial and temporal dynamics associated with marine reservoir effects in the Pacific Northwest. This analysis suggests that between 0 and 500 B.P. the regional correction value (ΔR) is 400 years, which agrees with the modern value determined by Stuiver and others. Between 500 and 1200 B.P., however, ΔR dips close to zero, possibly reflecting a decrease in offshore upwelling. From 1200 to 3000 B.P., ΔR returns to 400 years. These data are presented as a Puget Sound/Gulf of Georgia regional correction curve for the late Holocene, which local researchers may use to calibrate dates of marine shell. In addition, we detail our methods for constructing calibration curves and present guidelines for archaeologists working in other coastal settings to develop calibration curves for their regions.