SELECTIVE MEMORY: MONUMENTAL POLITICS OF THE YAXUNÁ E GROUP IN THE FIRST MILLENNIUM B.C.

In seeking continuities and disjuncture from the precedents of past authorities, the Mesoamerican emergent ruling class during the Formative period were active agents in directing changes to monumental space, suggesting that memory played a vital role in developing an early shared character of Maya lifeways (1000 b.c. to a.d. 250). The trend is most visible in the civic ceremonial complexes known as E Groups, which tend to show significant patterns of continuity (remembering) and disjuncture (forgetting). This article uses the northern lowland site of Yaxuná in Yucatan, Mexico, to demonstrate the use of early selective strategies to direct collective memory. While there are E Groups in the northern Maya lowlands, few Formative period examples are known, making Yaxuná a critical case study for comparative assessment with the southern lowlands. One implication of the Yaxuná data is that the broader pattern of Middle Formative E Groups resulted from sustained social, religious, political, and economic interaction between diverse peer groups across eastern Mesoamerica. With the emergence of institutionalized rulership in the Maya lowlands during the Late Formative, local authorities played a significant role in directing transformations of E Groups, selectively influencing their meanings and increasingly independent trajectories through continuity and disjuncture.

Lidar survey of ancient Maya settlement in the Puuc region of Yucatan, Mexico

The application of lidar remote-sensing technology has revolutionized the practice of settlement and landscape archaeology, perhaps nowhere more so than in the Maya lowlands. This contribution presents a substantial lidar dataset from the Puuc region of Yucatan, Mexico, a cultural subregion of the ancient Maya and a distinct physiographic zone within the Yucatan peninsula. Despite the high density of known sites, no large site has been fully surveyed, and little is known about intersite demography. Lidar technology allows determination of settlement distribution for the first time, showing that population was elevated but nucleated, although without any evidence of defensive features. Population estimates suggest a region among the most densely settled within the Maya lowlands, though hinterland levels are modest. Lacking natural bodies of surface water, the ancient Puuc inhabitants relied upon various storage technologies, primarily chultuns (cisterns) and aguadas (natural or modified reservoirs for potable water). Both are visible in the lidar imagery, allowing calculation of aguada capacities by means of GIS software. The imagery also demonstrates an intensive and widespread stone working industry. Ovens visible in the imagery were probably used for the production of lime, used for construction purposes and perhaps also as a softening agent for maize. Quarries can also be discerned, including in some cases substantial portions of entire hills. With respect to agriculture, terrain classification permits identification of patches of prime cultivable land and calculation of their extents. Lidar imagery also provides the first unequivocal evidence for terracing in the Puuc, indeed in all northern Yucatan. Finally, several types of civic architecture and architectural complexes are visible, including four large acropolises probably dating to the Middle Formative period (700–450 B.C.). Later instances of civic architecture include numerous Early Puuc Civic Complexes, suggesting a common form of civic organization at the beginning of the Late Classic demographic surge, (A.D. 600–750).

LACUSTRINE DYNAMICS AND TLATEL-TYPE SETTLEMENTS FROM MIDDLE FORMATIVE TO LATE AZTEC IN THE EASTERN PART OF LAKE TEXCOCO, MEXICO

In the territories of the former lakes in the Basin of Mexico, a tlatel was an insular settlement associated with the exploitation of lacustrine resources. This study examines the stratigraphy and geomorphological context of three tlateles in the eastern part of the former Lake Texcoco and correlates their phases of development with regional paleoclimatic trends from the seventh century b.c. to the sixteenth century. The results of this research indicate that fluvio-lacustrine (i.e., deltaic) sedimentation and freshwater springs in the lake basin were important features for the establishment of tlatel settlements in the highly dynamic and saline lacustrine environment. The formation and abandonment of the studied tlateles correlate with changes in other settlements and developments recorded in other parts of Lake Texcoco. Sites and sediments in the eastern part of Lake Texcoco provide proxy information on the lacustrine changes that accompanied the development of Tenochtitlan and other lacustrine settlements in its western part.

THE HOUSEHOLD FUNCTIONS OF OBSIDIAN TOOLS FROM THE EARLY–MIDDLE FORMATIVE VILLAGE OF ALTICA, MEXICO

Functional determinations of stone tools gleaned through high-magnification usewear analysis enable archaeologists to reconstruct ancient household practices and identify diversity across regional domestic economies. A systematic obsidian usewear study with 300 specimens from the site of Altica, Mexico presented here reveals that tools from the Early–Middle Formative (1250–800 cal. b.c.) occupation were used for woodworking and subsistence-related activities. The high frequency of woodworking usewear patterns can be attributed to the construction and maintenance of the newly established settlement's households and agricultural plots. Combined with previous analyses of the site's paleoethnobotanical, osteological, and isotopic datasets, the usewear data further indicate a subsistence strategy that balanced foraging and non-intensive maize agriculture. Thanks to their proximity to the Otumba source and other sites exploiting it, Altica residents were able to employ a unifunctional tool-use approach with expedient percussion tools, which contrasts the multifunctional tool-use approaches documented at other Middle Formative sites.

Radiocarbon Evidence for Initial Early Formative Period Occupation in Coastal Oaxaca, Mexico

Seven AMS radiocarbon dates (1950–1525 cal BC) from controlled contexts demonstrate Early Formative period occupation in coastal Oaxaca, Mexico. These dated elements from the site of La Consentida include hearths, occupational surfaces, carbon adhering to pottery from a midden, and human bone collagen processed with XAD purification. They were excavated from primary contexts and do not represent redeposited materials. An eighth sample, dated to the Middle Formative period, is considered postoccupational. The diversity of dated deposits and features, their distribution, and their overlapping calibrated ranges indicate settlement by an initial Early Formative period village.

POTTERY TRADE AND THE FORMATION OF EARLY AND MIDDLE FORMATIVE STYLE HORIZONS AS SEEN FROM CENTRAL MEXICO

We explore the relationship between long-distance pottery trade and the formation of Early and Middle Formative style horizons in Mesoamerica. A sample of 1,154 ceramics mostly from Early and Middle Formative contexts in the central Mexican highlands was irradiated at the University of Missouri Research Reactor with a subsample (n = 313) for petrographic analysis. We conclude that: (1) most sites and regions display more than one process for making pottery; (2) there is a small amount of intraregional exchange among central Mexican sites, with the southeastern Basin of Mexico making the largest portion of pottery intended for trade within the region; and (3) interregional imports found at several sites likely come from the metamorphic region of southwestern Puebla with smaller numbers imported from the southern Gulf Coast, Morelos, and possibly Oaxaca. The trend over time from Early Formative to the end of the Middle Formative is one of decreasing intensity of long-distance interaction and decreasing geographic range of trade. These two trends contribute to the regional divergence of ceramic styles that peaks by the Late Formative in Mesoamerica.

BEFORE TEOTIHUACAN—ALTICA, EXCHANGE, INTERACTIONS, AND THE ORIGINS OF COMPLEX SOCIETY IN THE NORTHEAST BASIN OF MEXICO

For several decades, little research has been directed towards understanding the beginnings of complex society in the Teotihuacan Valley. Recent archaeological investigations at the Early–Middle Formative site of Altica provide a fresh perspective on dating the initial establishment of agricultural villages, early social and economic differentiation, and the development of intra-and interregional exchange networks to test comparative models of political economy.

ALTICA'S OBSIDIAN INDUSTRIES AND THEIR PLACE IN EARLY–MIDDLE FORMATIVE OBSIDIAN EXPLOITATION IN CENTRAL MEXICO

Survey and excavation conducted by Stoner and Nichols (2019) at Altica, located in the Basin of Mexico, recovered nearly 29,000 pieces of obsidian, most of which apparently came from the nearby Otumba source. Formal classification followed by attribute analysis revealed a number of distinct lithic industries represented in the collection, although most are represented by finished objects that do not appear to have been produced on site. Most of the material consists of flakes probably used as unmodified, informal tools and produced on expedient cores consisting of some nodules but mostly percussion blades, spent cores, and other artifacts recycled as secondary cores. I propose that Altica acquired its obsidian from workshops possibly located in an area where they apparently existed in later times and may have during the Early–Middle Formative, as well. Virtually all of the obsidian in the collection appears to have been used for domestic or subsistence activities and was not involved in production or exchange systems believed to have existed at that time. Two unusual caches containing macronodules provide some evidence to the contrary, suggesting that Altica may have been a transshipment center.