A Bayesian AMS C chronology of the Classic Maya Center of Uxbenká, Belize

Archaeologists require precise chronologies of cultural change to understand the nature and timing, and causes and effects, of ecological and social transformations. The Uxbenká Archaeological Project (UAP) has made chronology building a main goal, employing epigraphic data, artifact seriation, and high-precision AMS ¹⁴C dating. With more than 60 ¹⁴C dates with measurement errors below ±25 ¹⁴C yr, primarily on single charcoal specimens, Uxbenká may be the most intensively dated Classic Period site in the tropical Maya Lowlands. Here we take the next step, combining this rich chronometric dataset with associated stratigraphic information in OxCal's Bayesian framework to generate a high-resolution chronology of Uxbenká's early development and expansion in southern Belize. We show how archaeologists may take advantage of complex architectural stratigraphy to constrain broad calibrated ranges during the Classic Period, and to estimate dates for observed construction events that can not be directly dated (e.g., clearing/leveling plazas, laying plaster floors, renovating/rebuilding structural elements). Our analysis confirms the antiquity of the ceremonial Stela Plaza (Group A), where first construction is estimated between 60 cal BC and cal AD 220 and is associated with a Pre-Classic structure obscured by later construction and reorientation of the group to a N-S alignment ca. AD 150–310. The analysis also indicates initial leveling and construction at plaza Group B from cal AD 60–310 and Group D from cal AD 20–240, both earlier than previously assumed. Though Late Classic contexts are not as well represented by direct dates, architectural modifications are documented at all three plaza groups after AD 550, including the extensive plastering, laying paving stones, and construction of facades on existing structures. The resulting chronology revises our previous thinking on the mode of settlement and development of Classic Maya society at Uxbenká and indicates specific areas of investigation to elucidate events in the Late and Terminal Classic at the site, including political and social fragmentation and the abandonment of the urban core late in the Classic Period.     

Recent Discoveries in the Classic Maya Palace Complex of Nim li Punit,Belize

Nim li Punit is a small Classic Maya (ca. a.d. 150–830) center of Toledo District, Belize. Here I describe excavations of two buildings within the royal palace group: Structures 7 and 8. Structure 8 was built in four stages all dating to the Early to Late/Terminal Classic period. It probably served as a council house. Structure 7 was the residential palace and was built in two stages. An Early Classic burial demonstrates indirect interaction with Teotihuacan. During the Terminal Classic period, the shape of Structure 7 was altered, numerous caches were placed there, and Tomb 5 was dedicated. It contained many important artifacts including a modeled effigy vase displaying the wind god, a chert eccentric, and the second largest piece of carved jade excavated legally in Belize. This, the Nim li Punit “wind jewel,” contains a long historical text and was worn by Late Classic kings. I argue that the pectoral tied Maya kings through ritual performance to breath, winds, rain, agriculture, and life.     

Survey,Settlement, and Population History at the Ancient Maya Site of Pacbitun,Belize

Abstract

Survey and excavations of mounds on the outskirts of the site of Pacbitun in western Belize provide insights into the ancient Maya settlement pattern at this medium-sized regional center. This research employed two methods: analysis of structural remains from four separate 1000 m transect surveys,and a subsequent complete (100%) survey of intervening and adjacent quadrant areas. The overlap of quadrant zones with portions of the transect units permits an examination of the accuracy of transect surveys. Excavation of a 22% sample of all identified mounds provides chronological and functional information. An estimate of 200 persons for the resident elite population of the Epicenter of Pacbit un is offered. Initial settlement occurred in the Epicenter of the site during the Middle Preclassic period (900–300 B.C.), with a population rise through time until the final phase of the Late Classic period (A.D. 700–900), when density reached 550 persons (periphery Zone) to 950 persons (Core Zone) per sq km. The impact on settlement size and distribution of topography, soils,water resources,and intensive agriculture (hillside terracing) is assessed and found to be significant. At the time of florescence,the population of the 9 sq km site is estimated to have been about 5000–6000 persons. This population estimate is compared with several coeval lowland Maya centers,and found to be reasonable for a medium-sized, Late Classic Maya center.     

Country Roads: Travel,Visibility, and Late Classic Settlement in the Southern Maya Mountains

Mayanist archaeology has long been concerned with creating and evaluating explanatory models for the locations of ancient sites relative to one another and to the physical geography of the Maya world. This study combines epigraphic data and spatial analyses to explore motivations for settlement location and to interrogate territorial strategies in Late Classic (a.d. 600–830) kingdoms in the southern Maya Mountains, around the modern towns of Dolores and Poptún, Guatemala. Least-cost path analyses were used to model natural travel corridors and their relationship with site location was assessed. In conjunction, viewshed analyses were applied to evaluate the importance of visual connections to likely travel routes. The results are considered in the context of the socio-politics and economics of the region, and raise questions about the character of and interconnections between travel, exchange, settlement location, and mechanisms for reinforcing territorial claims in the Late Classic Southern Maya Mountains.     

Competition and conflict in the Upper Belize River Valley: Insights from the ancient Maya minor center of Callar Creek,Belize

Political relationships typically entail competition and conflict. Within the ancient Maya world, the Upper Belize River Valley (UBRV) offers one example of an arena of intense political contestation, and recent investigations at the minor center of Callar Creek offer insights into this complex and occasionally antagonistic political landscape. During the Late and Terminal Classic periods (a.d. 600–900), for example, those living at the Callar Creek center appear to have affiliated themselves with the larger center of Buenavista, but not to have developed political ties with those in surrounding hinterland communities. Indeed, Callar Creek provides an example in which the political fortunes of a minor center and its surrounding hinterlands followed divergent paths. Furthermore, a termination event suggests that part of the Callar Creek center was purposefully destroyed by adversaries in the Terminal Classic period, and that discordant relationships in the UBRV at times turned violent.     

Coastal Maya Obsidian Tool Use and Socio-Economy in the Late Postclassic-Early Spanish Colonial Period at San Pedro,Ambergris Caye,Belize

Microscopic use-wear analysis of the obsidian artifacts recovered from Late Postclassic-Early Spanish Colonial occupations at the site of San Pedro yields useful information for interpreting Maya socio-economic activities. Obsidian traded into the community was used for a variety of tasks with emphasis placed on subsistence and domestic manufacture associated with marine resources, including intermittent and contingent crafting. Trade in obsidian and marine resources likely provided San Pedro community members access to inland economic networks and enabled the acquisition of resources not found on the caye. Microwear on chert and obsidian tools indicates relative stability in the traditional lives of the San Pedro Maya in the 15th–17th centuries a.d. Although the San Pedranos likely suffered to some degree from coastal raiding and the introduction of epidemic diseases by the Spaniards, their off-shore location provided them some protection from the upheaval experienced by the Maya in mainland communities.     

Sociopolitical network interactions: A case study of the Classic Maya

The organization of Classic Maya society emerged from diverse and overlapping social interactions which shaped a dynamic political landscape. Vying for power, elites legitimized their status by claiming ancestry from various supernaturals and engaged in conspicuous displays of competition, warfare, and ritual practice which were often recorded on stone monuments. By examining the inscribed relationships between Maya centers, we chart organizational changes in sociopolitical networks throughout the Classic period. Methods derived from social network analysis are used to examine temporal changes in the distribution and centralization of political power through different network interactions. We examine the intersection of antagonistic, diplomatic, subordinate, and kinship relationships and discuss how these overlapping networks contributed to dynamic changes in the Classic period. This case study demonstrates how current network analysis techniques can contribute to archaeological studies of the scalar dynamics and organizational changes of past social and political systems.     

Using Actor-Network Theory to Characterize the Production of Ancient Maya Caching Events at Cerro Maya (Cerros,Belize)

Inspired by actor-network theory, this research uses an operationalized archaeological actor-network approach to characterize and examine human-object relationships associated with ritual caching deposits (votive bundles of objects) at the site of Cerro Maya (formerly Cerros), Belize. Designed to be broadly applicable for archaeological studies, our archaeological actor-network approach made it possible to inductively examine, characterize, and diachronically compare the complex arrays of human and nonhuman relationships. In contrast to previous studies that characterized caches mainly in symbolic terms, we treated caches as traces of the small-scale actor-networks that emerged during the production of ancient Maya caching events. More specifically, our actor-network methodology made it possible to characterize caches and caching events in terms of the relationships between materials, temporality, objects, places, and groups of people, their intentions, and actions. The inductive and diachronic focus of approach also allowed us to compare arrays of caching actor-networks over time while considering the social affect that caching events had on subsequent caching events and the site’s social development. This approach demonstrates that even simple artifact clusters can be viewed as proxies for highly complex networks of interlinked social relations that play roles in shaping important historical interactions and social orders over time.

     

Ancient Maya wood selection and forest exploitation: a view from the Paynes Creek salt works,Belize

Ancient building construction wood preserved in a peat bog below the seafloor in a shallow mangrove lagoon in Paynes Creek National Park, Belize, provides an exceptional record of Classic Maya wood use. Identifications of construction wood at Early Classic Chan B'i, and Late Classic Atz'aam Na, are reported and discussed to assess forest exploitation and species selection over time. Black mangrove (Avicennia germinans) dominates the Early Classic assemblage. The Late Classic assemblage is characterized by greater variability and an absence of mangrove species. When considered in the environmental context, identified species conform to principles of optimal foraging. The change in the wood assemblage over time suggests overexploitation of forest resources, resulting in deforestation of the local landscape and subsequent adaptation of foraging behavior. Deforestation is linked to the wider social context in which growing inland populations created demand for salt, putting greater pressure on the forest resources exploited by the Paynes Creek salt works for fuel and timber.     

Raman microprobe analysis of stucco samples from the buildings of Maya Classic Copan

Micro-Raman spectroscopy has been applied to painted stucco samples from three buildings at the Maya site of Copan, Honduras. The buildings, Clavel (AD 450–550), Ani (AD550–650) and Structure 10L-22 (AD730,) date from three phases of the Classic Period (AD400–820) acropolis construction. The red pigment has been identified as haematite and the stucco as a mixture of calcite particles dispersed throughout a calcite based lime wash stucco. The physical structure of the stucco changed through time, indicating a refining of production techniques over this period. By combining Micro-Raman spectroscopy with other micro-ATR infrared spectroscopy and environmental scanning electron microscopy a detailed investigation of the materials and production techniques used to decorate these buildings has been made. Differences in the mineralogy of the red pigment used on each building indicate a different geological pigment source for each period.     

A Filtered Past: Interpreting Salt Production and Trade Models from Two Remnant Brine-Enrichment Mounds at the Ancient Maya Paynes Creek Salt Works,Belize

The mounds at Witz Naab and Killer Bee are the only known remaining aboveground evidence of a once-thriving salt industry in Punta Ycacos Lagoon, a large saltwater system in Paynes Creek National Park, Belize. Over one hundred ancient Maya salt works dated to the Classic period (a.d. 300–900) have been submerged by sea-level rise in the lagoon. We have hypothesized that mounds were once numerous features on the landscape prior to a sea-level rise that occurred in the area during the Terminal Classic period. Lacking at these underwater sites are earthen mounds formed by discarded soil from the leaching process in which the salinity of seawater was enriched by leaching brine through salty soil. Enriching the salinity of seawater by leaching or by solar evaporation is virtually universal in ethnographic case studies. Data from the excavations are evaluated to interpret the ancient activities that produced the earthen mounds, scales of production, and how the coastal Maya of southern Belize participated in the larger Classic Maya economy.     

Chemical composition of architectural plaster at the Classic Maya kingdom of Piedras Negras,Guatemala

Architectural plaster from elite masonry structures at the Classic Maya kingdom of Piedras Negras, Guatemala, is examined. Chemical composition is determined through X-ray fluorescence and compared statistically. Based on this sample, it was observed that any single masonry building was coated with plaster made from a single source of limestone and limestone-based aggregate, but that architectural plaster from different buildings across the site varied in chemical composition. It is concluded that this pattern is best accounted for by a model of rotational labor obligations to the state, with spatially distinct groups being responsible for manufacturing plaster for specific buildings.     

Preliminary geochemical assessment of limestone resources and stone use at Maya sites in the Three Rivers Region,Belize

The carbonate bedrock of northwestern Belize is poorly understood from the standpoint of both geochemistry and the use of stone in prehispanic Maya sites for buildings and monuments. The friable nature of the rock in this topographically rugged area makes it especially difficult to distinguish monuments from bedrock spall, as little carving, if any, survives, and identification rests on location and positioning. The research presented here analyzed 63 limestone samples collected from two sites in the Three Rivers Region of Belize. ICP-MS and ICP-AES were used to characterize the major, minor, and trace element chemistry of the limestone bedrock of the region and determine the amount of geochemical variability. Another important objective was attempting to trace the movement of monument stone and determining whether it was imported from outside of the sites. Bedrock, quarries, and possible monuments were all sampled for these purposes. Bedrock proved to be similar across wide areas. However, at Chawak But'o'ob, along the flank of the Rio Bravo, changes downslope in Mg concentration suggest a leaching of the bedrock by meteoric waters based on differences in porosity. At Maax Na, a hilltop site, in contrast, such leaching is not as apparent. Many monuments at both sites were found to be composed of stone similar in chemistry to the local bedrock, including several of the identifiable stelae. However, our analyses also revealed that a few monuments at Maax Na were made of material with a different chemical composition, apparently from stone imported to the site. These results suggest that the Maya deliberately selected certain types of limestone for certain purposes, and may even have traded in non-local rock. Overall, the methods used in this pilot study indicate there is real potential in more intensive, regional assessments of the materials used at archaeological sites, even in areas where the local stone does not have a distinctive geochemical signature.     

Multiple Waves of Political Disintegration in the Classic Maya Collapse: New Insights from the Excavation of Group D,Ceibal, Guatemala

In the study of the Classic Maya collapse around the 9th century a.d., scholars tend to emphasize its gradual nature. New data, however, point to multiple episodes of rapid social change that affected wide areas. We investigated these critical moments at Ceibal (Seibal), Guatemala, through intensive excavations in its Group D. This naturally defensible location was used as a primary elite complex, possibly including a royal palace, during the Late Classic period (a.d. 600–810). By refining the chronology, we have identified four episodes of political disruption, including the impact of a military defeat by the Dos Pilas dynasty in a.d. 735, the takeover of Ceibal by an illegitimate ruler in a.d. 771, the ritual destruction of various buildings at the Ceibal dynastic collapse around a.d. 810, and the final abandonment of Ceibal around a.d. 900. These finds provide significant insights into the process of political disintegration in the Maya lowlands.     

The Ballgame,Termination Ritual,and the Transformation of Classic Period Authority in the Mesoamerican Southern Gulf Lowlands

In the Gulf lowlands, Late Classic fluctuations were concomitant with the increasing importance of the Classic Veracruz style complex. A characteristic feature of the style was ballgame imagery on ballcourt panels, molded ceramics, and paraphernalia such as yokes, hachas, and palmas, as well as courts, markers, and stelae. Components of the Classic Veracruz style have been documented for the Gulf lowlands and adjoining regions of Mesoamerica. Few examples, however, derive from stratigraphic excavations of in situ deposits. We document the discovery, excavation, and initial interpretation of a monument-yoke-offering complex at Matacanela, located in the south-central Tuxtla Mountains. We present suggestive evidence for associated decapitation ritual. We conclude by assessing these data and generating hypotheses regarding the transitioning of authority. We situate the Matacanela complex within regional demographic, political, and economic transformations that occurred throughout the Classic period (ca. a.d. 300–800/1000), culminating in disruptions that may have been contentious.     

The correlation of surface and subsurface artifacts: A test case from Late and Terminal Classic Popola,Yucatan, Mexico

Abstract

Surface collections are commonly used by archaeologists to sample artifact assemblages, but the correlation of surface and subsurface artifacts is not fully understood. Cultural, taphonomic, and research-design factors that can affect the relationship of surface and subsurface deposits are reviewed and the correlation of surface and subsurface deposits is tested statistically with data from the site of Popola, Yucatan, Mexico, a Late and Terminal Classic period (a.d. 600–1100) village in the northern Maya lowlands. This study suggests that surface artifact density is not correlated with subsurface artifact density. Large-scale surface collections can characterize the overall assemblage of a site, but not any small area in particular. In shallow bioturbated soils there is no significant variation between surface and subsurface assemblages at any depth. Surface artifacts may be used to identify the presence of subsurface artifacts, but should not be used to suggest their absence.     

Late Prehistoric Mortuary Features in the Greater Illinois Area: A Discussion of Form,Function, and Ritual Use

Numerous Late Prehistoric nonburial mortuary features have been identified in the greater Illinois region. Often, and sometimes uncritically, these features have been referred to as “charnel houses” in the literature. To date, there has been no attempt to tie all of the information on these features together. This study critically examines the features’ attributes and provides possible explanations of how they were used in the context of mortuary ritual. Two major types of features have been identified. The first is an above-ground feature consisting of a scaffold or small structure supported by posts. The entire feature is surrounded by a lightly built wall or fence. The close association of secondary human remains with these features suggests that they were used to expose, store, or display them. The second type is an enclosed area or a lightly built structure constructed directly on the ground. Examples from the American Bottom differ from those noted elsewhere. In some instances, the two feature types were paired at a single site, suggesting that they had complementary functions. The presence of multiple examples of nearly identical features at some sites also suggests that the remains may have been segregated according to kin-group affiliation.