Excavations at the ancient Maya city of Holmul, Petén, have led to the discovery of a building decorated with an intricately carved and painted plaster frieze. The iconography of the frieze portrays seated lords, mountain spirits, feathered serpents, and gods of the underworld engaged in the apparent rebirth of rulers as sun gods. Large emblems carved on the side of the building identify the structure as a shrine for ancestor veneration. A dedicatory text carved along the bottom of the frieze contains a king list and references to the political and familial ties of the ruler who commissioned the temple. Together, the iconography and text of this structure provide evidence of function and meaning. They also shed new light on a century during Classic Maya history known as the Tikal “Hiatus,” for which a limited number of texts are available. The information derived from this monument also broadens our understanding of the nature of hegemonic relationships among Classic Maya states.

Exchange goods contribute to social complexity and identity construction, but our knowledge of past practices associated with the circulation and consumption of such goods is limited. We explore the polished black ceramics of the San Pedro de Atacama oasis in northern Chile, which were widely traded during the first seven centuries A.D. In particular, we consider the relationships established between the agricultural and pastoral communities of the highland oases and the marine hunter-gatherers who inhabited the Pacific coast in order to examine the circulation and consumption of exotics as prestige goods.

This paper explores certain methodological issues relevant to the interpretation of archaeological data derived from surface survey. Recognizing the significance of survey to the study of regional settlement patterns, I argue that how we classify these data bears directly on our ability to reconstruct the past. Comparison of site typologies created by the Seibal and Copán projects with their excavation results provides a way to evaluate the accuracy of site classifications based on surface features. I discuss the effectiveness of the typologies in capturing variation pertinent to the study of social organization and site function, and consider the importance of variation within sites, within types, and across types not expressed in the typologies to suggest that such elaborate typologies assume a higher degree of data visibility than is generally possible. The analysis underscores the critical role excavation plays in mesoamerican archaeology as a source of data unavailable through survey.

Incised-engraved pottery and clays from the Malpaso Valley region of northwest Mexico are chemically characterized to investigate the nature of residential organization of the capital settlement, La Quemada, during the Epiclassic period, ca. A.D. 600-900. Scanning-electron microprobe analysis of 115 pottery and 10 clay samples from settlements in the valley, and from middens associated with the civic-ceremonial core of La Quemada and flanking residential terraces, identifies locations of pottery production and indicates patterns of pottery circulation. The distribution of pottery at La Quemada, manufactured in specific outlying settlements, suggests that the social composition of the polity was reproduced in microcosm at the site, and that activities in civic-ceremonial zones involved a greater degree of separation among social groups than those in flanking residential areas.

This paper contributes to scholarship on continental fish exploitation in arid zones in South America by exploring fish consumption by humans in prehispanic times using available zooarchaeological evidence from two wetlands in central western Argentina: Llancanelo and Guanacache lagoons. Analyzing the exploitation of this resource lets us discuss the intensification process that has been proposed for this area. Ichthyoarchaeological and archaeofaunistic information is integrated and compared to reveal that the oldest incidence of fish exploitation (ca. 3000 years B.P.) is from the Llancanelo lagoon. Fish consumption seems to have been practiced since the first occupations in both the wetlands and may reflect an adaptation to the new environment. Contrary to our expectations, temporal trends in abundance and diversity indexes do not show differences between the areas in intensification processes. We conclude that fish represent a major resource for sustenance both in Guanacache and in Llancanelo lagoons, although its exploitation was complemented with consumption of other small animals.

This article examines the significance of outlying groups in the spatial organization of Classic Maya settlements. The relative scarcity of textual records concerning outlying groups has often made it difficult for researchers to analyze in detail the political interactions between individuals associated with these groups and the royal authority. The recent discovery of a hieroglyphic stairway at the Guzmán Group, an outlying group of El Palmar, Campeche, Mexico, provides an exceptional opportunity for understanding the constitutive process of spatial organization during the Late and Terminal Classic periods (ca. A.D. 600-900). Epigraphic studies of the Guzmán Group stairway have identified a main individual who emphasized his genealogical ties to lakam (banner-bearer) officials and his political relationship with foreign rulers of Copán and Calakmul. The results of archaeological and epigraphic studies suggest that the Guzmán Group was a locus for negotiating power and ideology among different social actors.

Cueva la Conga, recorded in June 2006, is the first limestone cave in Nicaragua reported to contain prehistoric rock paintings, culturally modified natural formations called speleothems, and artifacts. Located in northcentral Nicaragua in the Department of Jinotega, Cueva la Conga is the farthest south on the Mesoamerican periphery that a cave of this type has been reported, and it extends our knowledge of ritual cave use, including cave painting and speleothem modification, to include Nicaragua. Radiocarbon analysis of charcoal in five samples of the paint, the first such dating of Nicaraguan rock art, yielded calibrated dates from cal A.D. 680—905 to cal A.D. 1403—1640. The baseline data provided by Cueva la Conga are of great importance for regional rock art analysis and for our growing understanding of regional and Nicaraguan prehistory. More archaeological survey and excavations in the area will be key in establishing a firm cultural context for the rock art and ritual cave use found at Cueva la Conga.

As dates of earliest use of Theobroma cacao in ancient Mesoamerica are established, interest is shifting to how cacao was used. One approach is to consider combinations of ingredients—the recipes for ancient cacao use. Beverages made from cacao seeds and maize have a long history in Mesoamerica. We began testing the hypothesis that there is qualitative evidence of this beverage type in the Postclassic archaeological record in a region where such a beverage, tejate, is a culturally significant food today. We looked for evidence of tejate ingredients in residue samples from eight Postclassic and one contemporary vessel from the Valley of Oaxaca, Mexico. Detection of morphologically specific maize phytoliths was accomplished by taxonomic analysis and comparison with a reference collection. Tejate ingredients Pouteria sapota and Quararibea funebris were also processed for phytolith detection. Testing for methylxanthines characteristic of Theobroma species used high-performance liquid chromatography-mass spectrometry. Four vessels were positive for maize phytoliths; three were positive for theobromine; two were positive for both maize and cacao. No diagnostic phytoliths were identified for the other tejate ingredients. Our hypothesis was supported; still, many challenges are present in the search for a deeper understanding of ancient cacao usage in this region of Mesoamerica.

Initial Spanish colonization of the Central Andes and efforts to transform indigenous society were highly dependent on local social and geographic conditions. In the Colca Valley of southern Peru, Franciscan friars established a series of doctrinas (settlements for the conversion and doctrinal instruction of the indigenous population) at former Inka imperial outposts during the mid-1540s. The inhabitants of one of these doctrinas—the site today known as Malata (ca. A.D. 1545–1573)— were subject to one of the earliest mendicant evangelical campaigns in the Central Andean highlands. In addition to religious indoctrination and significant spatial reconfiguration of the village, Spaniards attempted to alter systems of domestic production related to the rearing and consumption of animals. They also imposed new tribute demands. Despite considerable transformations of the architecture and attendant changes in daily life at Malata, zooarchaeological analysis of faunal remains from a variety of contexts provides no indication of the introduction of Eurasian animals to Malata nor the alteration of either indigenous husbandry practices or the consumption of food animals. Ceramic iconography and the abundance of weaving tools suggest that Spaniards built on the local system of camelid husbandry to extract textiles and metallurgical goods as tribute during the first generation of colonial occupation.

This paper addresses objections raised in an article by Bennetzen et al. (2000) in response to MacNeish and Eubanks (2000). Bennetzen et al. interpret the findings reported by MacNeish and Eubanks as opposition to the teosinte hypothesis for the origin of maize. However, by demonstrating a mutagenic mechanism that could have generated the genetic diversity essential for the transition from teosinte to maize, and the subsequent explosive evolution of maize in the archaeological record, the Tripsacum-diploperennis introgression derivatives confirm that teosinte is a progenitor of maize. Although Bennetzen et al. claim that the Tripsacum- diploperennis crosses are not credible, DNA fingerprinting verified that the hybrids contain genes from their teosinte and Tripsacum parents. Archaeobotanical remains of teosinte, Tripsacum, and hybrid specimens have been reported from Tamaulipas and Oaxaca. One of the "hybrid" specimens from Tamaulipas is virtually identical to an experimental Tripsacum-diploperennis segregate. The ability to experimentally reproduce forms that closely resemble archaeological specimens lends compelling support to the hypothesis that intergeneric hybridzation gave rise to the mutations that, through human selection, transformed teosinte into domesticated maize.

Stone tool producers in the Maya Lowlands had several types of raw materials from which to choose. Limestone, chert, and obsidian are the most naturally abundant, whereas chert and obsidian outnumber limestone in archaeological contexts. The presence of flaked-stone tools made of limestone is typically attributed to the scarcity of more suitable raw materials. Nevertheless, in chert-rich areas, such as the upper Belize River valley, limestone bifaces and production debitage are present. To understand their presence, we examine limestone biface production and use at Buenavista del Cayo.

The Preceramic archaeological record of highland Mesoamerica is biased toward rockshelter sites. We advocate more fieldwork in streamside settings, where open-air sites are likely to be found for reasons related both to the systemic context of hunter-gatherer lifeways and to the geoarchaeological context of site burial and preservation. Predicting site location requires attention to the peculiar nature and behavior of incised ephemeral streams (barrancas) and to the complex alluvial stratigraphic sequences that they leave behind. Four case studies—from the Mexican states ofTlaxcala, México, Morelos, and Oaxaca—reconstruct the geometry and age structure of late Quaternary alluvium from exposures in cutbanks, brickyards, and purposefully dug trenches. We identify deeply buried locales with the remains of extinct megafauna, intentionally set fires, and lithic debitage. We distinguish between geographical areas, stream reaches, and time intervals that do or do not hold much promise for further research. The fragmentary nature of the alluvial record and the paucity of sites can be explained by changes in stream behavior wrought by agricultural land use and are conditioned by the intensity and antiquity of agriculture in any given area. Deposits and sites of Paleoindian age may be more commonly preserved than those of Archaic age.

We report on the archaeometallurgical analysis of eight pieces of copper recovered from the Villa JMC-1 cemetery (Pitren Complex, Early Ceramic period) in the locality of Labranza, La Araucania. These artifacts provide the earliest evidence of metal use in southern Chile. They are also the southernmost prehispanic metal artifacts ever found in South America. These contextualized results complement those obtained from the analysis of an earring from Kilómetro 0—Enlace Temuco (El Vergel Complex, Late Ceramic period), an archaeological residential site dated to almost 500 years after the Labranza cemetery. Particle Induced X-ray Emission, X-ray radiography, and stereomicroscopy analyses allow us to offer an elemental characterization of the pieces, an assessment of their manufacturing process, and a comparison between the metals and alloys discovered. We follow with a discussion of proposals regarding cultural relations in the Araucania region during different time periods.

Although dendrochronological methods have the potential to provide precise calendar dates, they are virtually absent in Mesoamerican archaeological research. This absence is due to several long-standing, but erroneous, assumptions: that tree rings in this region do not reflect annual growth and environmental variability, that an adequate number of samples do not exist, and that tree-ring measurements cannot be useful without modern trees to link prehispanic chronologies. In this article we present data from the sites of La Quemada and Los Pilarillos, located in the Malpaso Valley, Zacatecas, to demonstrate that suitable archaeologically derived samples of dendrochronologically useful species do exist, that the samples from these sites are measurable and cross-datable, and that the tree rings can yield precise calendar dates using a method that “wiggle-matches” radiocarbon dates on tree-ring sequences. The work demonstrates the potential of these methods to address chronological, and, in the future, climatic questions, which have so far eluded archaeological work in the region.

The introduction of the type-variety system as a means of classifying Maya ceramics had considerable success in promoting communication among researchers. There was hope that it would prove to be possible to devise a single unitary system of ceramic analysis based on type-variety. We believe that such a hope was doomed to failure. Ceramic complexity is too great to be subsumed in any single typological system. Attempts to incorporate the many variables involved within a type-variety analysis have usually resulted in neglect of some and the loss of important information. Instead, we advocate the use of multiple systems of classification. We suggest that at least three separate classifications should be done based on (1) surface finish, (2) vessel shapes (forms), and (3) pastes. For ceramics having highly decorated vessels, another separate classification of decoration is desirable. A final and vitally important objective is to investigate covariation among the classifications of shape, surface, decoration, and paste. We believe that these relationships can be seen more clearly by the use of multiple classifications than by incorporating all into a single typological system in which such variation is all too often hidden.

We use ceramic and obsidian data from the ancient Maya port site of Vista Alegre to discuss long-distance exchange during the Terminal Classic (c. AD 850–1100) period. This is a time often associated with increased international trade relations and the growth of Chichen Itza as a dominant regional power in the northern Maya lowlands. Critical to the increased volume of international trade were the merchants who transported goods along the coast of Yucatan in large trading canoes. By combining a macroscopic assessment of the ceramics with visual, XRF, and INAA analyses of the obsidian artifacts, we gain insight into the various socioeconomic forces at work moving goods around the Peninsula. Given the paucity of Terminal Classic settlement in the interior Yalahau region, Vista Alegre appears to be an isolated site during this period, approximately 40 km from the nearest coastal neighbor. This allows us to focus on coastal exchange as the sole means by which goods arrived at the site. Our preliminary data contribute to the growing literature on the role market economies played in the Maya area, and the increased opportunities this afforded coastal peoples as circum-peninsular trade became more common through time.

Banwari Trace, a well-stratified shell midden located in southeastern Trinidad, provides the oldest known archaeological evidence of human settlement in the West Indies and has been crucial to our understanding of the initial peopling of the greater Caribbean region. Detailed excavation profile descriptions, soil and faunal analyses, accelerator mass spectrometry radiocarbon and optically stimulated luminescence dating, and stable carbon isotope analyses provide an accurate chronology and paleoenvironmental framework for the natural and anthropogenic depositional history of this significant archaeological site. Our findings support the recognition of three Middle Holocene strata at Banwari Trace, which represent significant periods of midden deposition and environmental change at: ~7800–7900 cal BP (Level 3); ~6900–7400 cal BP (Level 2); and ~5500–6200 cal BP (Level 1). Stable carbon isotope analyses show the landscape was dominated by C3 vegetation throughout the Middle Holocene with a possible drying episode near the end of the Middle Holocene climatic optimum. Cedrosan potsherds discovered in the uppermost 25 cm (Level 0) suggest that a Late Holocene radiocarbon age of ~2770–2200 cal BP for charcoal from this stratum is valid and possibly contemporary with an apparently intrusive human burial recovered in 1971 at a depth of ~20 cm.

We present stable isotope and osteological data from human remains at Paloma, Chilca I, La Yerba III, and Morro I that offer new evidence for diet, lifestyle, and habitual mobility in the first villages that proliferated along the arid Pacific coast of South America (ca. 6000 cal BP). The data not only reaffirm the dietary primacy of marine protein for this period but also show evidence at Paloma of direct access interactions between the coast and highlands, as well as habitual mobility in some parts of society. By locating themselves at the confluence of diverse coastal and terrestrial habitats, the inhabitants of these early villages were able to broaden their use of resources through rounds of seasonal mobility, while simultaneously increasing residential sedentism. Yet they paid little substantial health penalty for their settled lifestyles, as reflected in their osteological markers of stature and stress, compared with their agriculturalist successors even up to five millennia later. Contrasting data for the north coast of Chile indicate locally contingent differences. Considering these data in a wider chronological context contributes to understanding how increasing sedentism and population density laid the foundations here for the emergence of Late Preceramic social complexity.

Recent investigations in the Casma Valley on the north-central coast of Peru have uncovered a series of circular and rectangular/square structures, each containing a central hearth associated with either four subfloor ventilation shafts or a single open ventilation trough. The structures date to the Late Preceramic period (2500-1800 B. C.) and the Initial period (1800-900 B. C.). All are small and were originally roofed with perishable materials to hold in heat and smoke from the central hearth. It seems likely that these ventilated hearths represent a coastal variant of the Kotosh Religious Tradition that has been well documented in the Peruvian Highlands. The structures probably served as ritual chambers for small groups of people, somewhat analogous to the sweathouses of various Native American groups.