Wetland research in northern Belize provides the earliest evidence for development of agriculture in the Maya Lowlands. Pollen data confirm the introduction of maize and manioc before 3000 B.C. Dramatic deforestation, beginning ca. 2500 B.C. and intensifying in wetland environments ca. 1500-1300 B.C., marks an expansion of agriculture, which occurred in the context of a mixed foraging economy. By 1000 B.C. a rise in groundwater levels led farmers to construct drainage ditches coeval with the emergence of Maya complex society ca. 1000-400 B.C. Field manipulations often involved minor modifications of natural hummocks. Canal systems are not as extensive in northern Belize as previously reported, nor is there evidence of artificially raised planting platforms. By the Classic period, wetland fields were flooded and mostly abandoned.

Many societies use architecture for symbolic expression, and often buildings or other constructions constitute maps of a culture's worldview. Archaeological identification of such ideational expressions is receiving renewed attention, in the Maya area as in many other regions. Excavations in 1988-1989 in Groups 8L-10 through 8L-12, Copán, Honduras, were designed to examine a particular model of ancient Maya site planning and spatial organization, in which the principles of architectural arrangement and their directional associations derive from Maya cosmology. This paper describes the model and its archaeological evaluation at Copán and discusses interpretive implications of the specific results obtained, in the context of other ongoing studies in epigraphy, iconography, and archaeology.

How the ancient Maya of the central Yucatecan Lowlands managed their water and land resources remains poorly known, although crucial to an understanding of ancient political economy. Recent archival research and field data suggest the widespread use of artificially altered, natural depressions for the collection and containment of water, both for potable consumption and agricultural ends. During the Classic period (A. D. 250-900) several of the principal cities in the Maya area constructed their largest architecture and monuments at the summit of hills and ridges. Associated with these elevated centers—”water mountains”—were sizable, life-sustaining reservoirs quarried into their summits. The effect of this town-planning design was the centralization of a primary and fundamental resource. Although elite managers controlled the water source, other decentralizing forces prevented anything similar to Wittfogel's “total power.” However, by ritually appropriating the everyday and mundane activities associated with water by the sustaining population, elites used high-performance water ritual as manifest in the iconography to further centralize control. The significance of modifying the urban landscape in the partial image of the ordinary water hole defines the extraordinary in Maya ritual.

Recent archaeological investigations along the lower Negro and upper Xingu Rivers in the Brazilian Amazon provide important new evidence bearing on long-standing debates about the size and permanence of Amerindian settlements in the region. Preliminary regional surveys and more in-depth study of selected large (30-50 ha) sites, particularly analyses of the associations between structural features, anthropogenically altered soils, and artifact distributions, lead us to conclude that large, permanent settlements, likely associated with fairly dense regional populations, existed prehistorically in both areas. These findings cast doubt on the view that environmental limitations prevented sedentism and demographic growth among Amerindian populations throughout much or all of the region. Specifically, we conclude that fully sedentary and relatively large populations emerged in a variety of Amazonian settings prehistorically, not necessarily correlated with the distribution of one or another narrowly defined ecological variable (e. g., high fertility soils). Thus, a critical evaluation of core concepts in Amazonian anthropology, such as the várzea/terra firme dichotomy or tropical forest culture, is advised.

This study addresses the political and military structure of early Teotihuacan through the analysis of oxygen-isotope ratios in skeletal phosphate from 41 victims of a sacrifice associated with the Feathered Serpent Pyramid. Oxygen-isotope ratios are markers of geographic identity. A comparison of bone and enamel values, which provides a contrast between environments experienced during growth and those of adulthood, illustrates that at least four different regions are represented in this sample. Those identified as soldiers had either lived locally since childhood or had moved to Teotihuacan from several foreign locations. Most had lived in Teotihuacan for a prolonged period before their death. This pattern suggests foreign “recruitment” or mercenary behavior. The women had either lived all their lives in Teotihuacan or had moved from there to a foreign location. Most of the individuals in the center of the pyramid (burial 14) did not come from Teotihuacan, nor had they lived in the city long before their deaths. We suggest that the choice of victims was meant to demonstrate Teotihuacan's powerful ideology to the rest of the Mesoamerican world. Notably, this isotopic evidence of physical interaction between Teotihuacan and foreign regions considerably predates the currently existing archaeological evidence.

Ancient civic centers materialize ideas of proper spatial organization, among the Maya as in other societies. We argue that the position and arrangement of ancient Maya buildings and arenas emphatically express statements about cosmology and political order. At the same time, the clarity of original spatial expression is often blurred in the sites we observe archaeologically. Factors responsible for such blurring include multiple other influences on planning and spatial order, prominently the political life history of a civic center. Specifically, we argue here that centers with relatively short and simple political histories are relatively easy to interpret spatially. Those with longer development, but relatively little upheaval, manifest more elaborate but relatively robust and internally consistent plans. Sites with longer and more turbulent political histories, however, materialize a more complex cumulative mix of strategies and plausibly, therefore, of varying planning principles invoked by sequent ancient builders. We examine evidence for these assertions by reference to civic layouts at Copán, Xunantunich, Sayil, Seibal, and Tikal.

A puzzling aspect of Prehispanic soil erosion and sedimentation in the Maya Lowlands is the variation noted between different regions. In the Petexbatún region of Guatemala, recent investigations indicate great variation in sedimentation rates between watersheds of different sizes. In some places, soil erosion was slowed by stone terraces, possibly in conjunction with other conservation methods. A review of the surficial geology and other data on terraces from across the Maya Lowlands indicates that variations in the form and distribution of ancient agricultural terracing was probably the result of environmental variability and population pressure largely during the Late Classic period.

Analysis of plant remains recovered from excavations at Copán in western Honduras has provided substantive data regarding agroeconomic systems of the prehistoric inhabitants. The time span of the deposits ranges from the Gordon/Uir phase (900-400 B. C.), which may have been non-Maya, to the Coner phase (A. D. 700-900+), which encompasses the collapse of the Classic Maya cultural manifestation in the valley. Several traditionally recognized mesoamerican cultigens were identified including corn, beans, and several species of Cucurbitaceae. In addition, remains of a number of economic tree species were discovered, suggesting a reliance on arboriculture as part of the subsistence strategy. Pine charcoal predominated in all deposits and may have been the preferred wood for fuel and construction. Analysis of edible-plant-species distributions from low- and high-status Late Classic dwellings using the Shannon-Weaver index revealed that elite individuals had a higher diversity of available foods, a situation that may have led to nutritional stress among lower-status individuals and, ultimately, social unrest.

Market economies are notoriously difficult to identify in the archeological record. This is particularly true in the subtropical Maya lowlands of Mexico, Guatemala, and Belize because most utilitarian items and consumables were made of highly perishable materials. We explore the hypothesis that ancient marketplaces can be identified through analysis of chemical residues in soils from open and easily accessible spaces in and about ancient Maya cities. We compared soil chemical signatures from a credible ancient marketplace location in the specialized trade center of Chunchucmil, Yucatan, Mexico to those from a modern marketplace at Antigua, Guatemala. We found extraordinarily high concentrations of phosphorus and zinc in the soil of Chunchucmil's proposed marketplace and the same high concentrations correlate well with food preparation and vegetable sales areas at the modern marketplace. These methods hold promise in resolving the vexing question of how large ancient Maya urban populations were sustained.

La arqueología moderna ha enfocado su atención al estudio de las áreas de actividad para entender formas de vida y patrones de subsistencia. Esto ha conducido a que se manejen niveles de análisis cada vez más pequeños, tales como los estudios de microarqueología, la recuperación de información botánica por medio de la flotación de restos vegetales, y el estudio de fitolitos y polen. Hasta el momento, el análisis químico de los pisos representa la escala más pequeña de estudio, ya que se está tratando con iones y moléculas químicas invisibles, impregnadas en los pisos. Sin embargo, la interpretación arqueológica de estos datos necesita estar sustentada por estudios etnoarqueológicos para entender los patrones de contaminación de actividades universales como el comer, cocinar, almacenar, etcétera y poder extrapolarlos coherentemente a contextos arqueológicos.

El presente trabajo muestra la relación entre las actividades humanas practicadas in situ y la distribución de compuestos químicos orgánicos e inorgánicos que impregnan los pisos de un área habitacional localizada en el poblado de San Vicente Xiloxochitla, en Tlaxcala, México.

Las pruebas químicas aplicadas a 76 muestras identificaron las concentraciones de carbonatos, fosfatos, pH, hierro, calcio, albúmina, ácidos grasos y carbohidratos, además de registrar su color Munsell. Los mapas de distribución muestran que las mayores alteraciones producidas por la ocupación están relacionadas principalmente con las actividades alimenticias y con los desechos de los animales. El resto de las actividades tuvieron un impacto menor en el enriquecimiento químico de los pisos pero a pesar de ello resultan claramente reconocibles. Lo anterior constituye una prueba fehaciente del tipo de información que los compuestos químicos impregnados en los pisos pueden proporcionar en contextos arqueológicos, especialmente cuando los materiales sobre los pisos son escasos.

In this paper, I examine the role that irrigation played in the formation of the Southern Moche state in the Moche Valley, Peru. Specifically, I attempt to test Wittfogel and Steward's hydraulic model, which postulates that in certain arid environments, the managerial requirements of construction and maintenance of irrigation systems played a crucial role in the formation of centralized polities. I formulate and evaluate four hypotheses concerning the role of irrigation systems in the Moche Valley. Those hypotheses are then evaluated using settlement pattern data drawn from two surveys that cover the entire coastal section of the valley and provide information on 910 archaeological sites. Based on those data, I present a sequence of political development for the valley from the formation of the first autonomous village in the Late Preceramic period (2500–1800 B. C.) to the zenith of the Southern Moche state. Evaluation of the four hypotheses indicates that the managerial requirements of irrigation were relatively unimportant; rather, warfare, highland-coastal interaction, and political control of irrigation systems created opportunities for leaders to form a highly centralized, territorially expansive state sometime between A. D. 200 and 700.

We analyzed strontium isotopes in more than 500 samples of shell, bone, and dental enamel from modern and archaeological contexts throughout Mesoamerica. The results correspond closely with expectations based upon the local geology and earlier measurements of geological materials. The results show that isotopic variation is significant across Mesoamerica. Thus strontium isotope ratios in dental enamel, which mark the place of childhood residence, can be used not only to document mobility but also in some cases to determine geographic origin. We present five archaeological case studies to illustrate the anthropological significance and range of applications for this technique: the origins of individuals in the “Oaxaca Barrio” at Teotihuacan, a northern origin for the founder of Copan, a local king at Tikal, the regional origin of two of Palenque's rulers, and individuals of African birth in a colonial cemetery in Campeche.

In this paper, the imperial Inka ceramic assemblage is examined in terms of its functional and culinary significance. Information culled from ethnohistoric sources, archaeological reports, and ethnographic studies is used to draw functional inferences about Inka vessel forms and to outline the features of an imperial “haute cuisine.” In the Inka empire, the relationship between rulers and subjects was largely mediated through the prestation of food and drink. The elaboration of a distinctive state vessel assemblage suggests a conscious strategy aimed at creating material symbols of class difference in the context of state-sponsored feasting events. An empire-wide analysis of the distribution of Inka vessels indicates the particular importance of the tallnecked jar form (aríbalo) to state strategies in the provinces. Analyzing Inka pottery as culinary equipment highlights the links among food, politics, and gender in the processes of state formation. Such an approach also illuminates the important role of women in the negotiation and consolidation of Inka state power.

High-precision trace-element analyses for 208 geological samples representing 25 mesoamerican obsidian sources were obtained using instrumental neutron-activation analysis to measure a total of 28 elements per sample. These are the first detailed chemical studies ever published for many of the source areas. Especially intensive analyses were made for six sources in the states of Veracruz and Puebla in Mexico from the region of Pico de Orizaba volcano. In addition, source determinations are provided for 65 artifacts from the Olmec site of San Lorenzo Tenochtitlán, Veracruz. The investigations presented here constitute an important basis for associating obsidian artifacts with specific sources, thereby making possible the reconstruction of Prehispanic trade system.

The Tierra Blanca Joven (TBJ) eruption of the Ilopango caldera in central El Salvador was one of the largest Holocene volcanic events in Central America, and its ecological and cultural impacts were felt throughout El Salvador and adjoining areas of Guatemala and Honduras. Early radiocarbon measurements established a ca. A. D. 260 ± 114 calendar date for the eruption. However, a reevaluation of the original 14C dates, in addition to new AMS 14C assays, shows that the TBJ eruption occurred at least a century and a half later than originally estimated. The revised 14C composite supports an Early Classic Period calendar date for the eruption: 1 sigma = A. D. 421(429)526; 2 sigma = A. D. 408(429)536. A review of archaeological settlement, ceramic, and radiocarbon evidence from sites throughout the area of greatest devastation reveals a large-scale demographic collapse following the event. We believe that the population crash was caused both by the biophysical effects of the eruption and by the resulting disarticulation of the "Miraflores" cultural-economic sphere. The affected areas of El Salvador and south-eastern Guatemala did not completely recover until the seventh century A. D.

Andean scholars have long debated the nature of the relationship between two Middle Horizon (ca. A. D. 750-1000) Andean states; many assumed Tiwanaku dominated Wari and preceded Wari in time. Recent research at the Wari administrative center of Cerro Baúl in the only known region occupied by both states (the Moquegua Valley of southern Peru) indicates that Tiwanaku may not predate Wari in Moquegua and that, contrary to previous assertions, both states occupied the valley for the last three centuries of the Middle Horizon. In support of this position, I review recent excavations at Cerro Baúl. Then I present eight new 14C dates and summarize the evidence for two major construction episodes at Cerro Baúl. I interpret the local Wari construction chronology based on the 12 14C dates now available from excavation contexts and I suggest that the new data, in comparison with 24 published 14C dates from other Wari centers, support a later date for Middle Horizon 1B Wari expansion than previously postulated.

En las últimas dos décadas se ha producido un incremento notable de la información arqueológica sobre las Tierras Bajas sudamericanas. No obstante, el mapa arqueológico de este área sigue contando con algunos vacíos importantes para conocer las particularidades del registro en cada región específica y muchas regiones están aún poco estudiadas. Uno de estos vacíos corresponde al Delta del río Paraná, que en los últimos años ha empezado a ser objeto de investigaciones sistemáticas. En este artículo se realiza una revisión crítica del estado actual de las investigaciones en el Delta del Paraná y se sintetiza la evidencia obtenida en las nuevas investigaciones efectuadas por los autores en el Delta Superior. Se discuten además los patrones de uso del espacio deltaico durante el Holoceno Tardío. En este contexto, se aborda el desarrollo de la arquitectura en tierra en el marco de una perspectiva suprarregional y comparada, integrando en la discusión otros casos de áreas vecinas (Uruguay y sur de Brasil) en los que la ocupación intensiva de tierras bajas condujo a la construcción de montículos (localmente denominados cerritos). Finalmente se exploran las evidencias arqueológicas e históricas que sugieren cierto grado de desigualdad social entre las poblaciones humanas del Delta del Paraná.

The presence of cacao has been discovered in the state of Yucatan, Mexico. Cacao in this region has been mentioned since Prehispanic times by diverse chroniclers and investigators. Nonetheless, until the present, there did not exist concrete evidence of the existence of cacao in this area. Apparently, the climate and soil of Yucatan are not adequate for the natural growth of this species, which requires great humidity throughout the year and deep soils. Cacao was found in three sinkholes (k'o'op) to the south of Valladolid. The trees found are of a rare form of cacao only known in the Lacandon region in Chiapas: Theobroma cacao L. subspecies cacao forma lacandonica Cuatrecasas. A discussion of the importance of this discovery from the perspectives of biology, ecology, and history is presented. This discovery reinforces the importance of the present-day flora for understanding the management of vegetation in the past.

Utilizing data from six seasons of field research, this article focuses on the question of the technology and social organization of intensive agricultural production in the Andean state of Tiwanaku. Recent literature in Andean archaeology and ethnohistory asserts the dominance of local kin groups in the organization of agricultural production rather than supracommunity state authority. The analysis presented here takes issue with this perspective as applied to the core territory of the Tiwanaku state during the period from ca. A. D. 400 to 1000 (Tiwanaku IV-V). I conclude that in this period: (1) the technology of Tiwanaku intensive agricultural production turned on the creation of an artificial regional hydrological regime of canals, aqueducts, and groundwater regulation articulated with massive raised-field systems, and (2) the organization of agricultural production in this core territory entailed structured, hierarchical interaction between urban and rural settlements characterized by a substantial degree of political centralization and the mobilization of labor by social principles that reached beyond simple kinship relations.

Archaeological research over several decades has documented extensive areas of relict raised fields throughout the Americas. The existence of huge tracts of fields utilized in a context of complex political evolution has fostered a debate similar to the “hydraulic hypothesis” controversy, originated by Julian Steward and Karl Wittfogel over a generation ago. In this paper I assess recent research and offer a model that is tested with settlement and demographic data from the Juli-Pomata area of Lake Titicaca in southern Peru. The key variables of the model are differential levels of surplus production, the control of domestic labor by elite groups, and opportunistic economic strategies by the elite. The Juli-Pomata data support a causal link between complex political organization and the existence of labor-intensive raised-field systems. The simplistic explanations of the hydraulic hypothesis remain untenable, but I argue that more subtle causal relationships exist between political centralization and agricultural intensification.