THE NORTHERN MAYA COLLAPSE AND ITS AFTERMATH

2003 ◽  
Vol 14 (1) ◽  
pp. 151-156 ◽  
Author(s):  
Anthony P. Andrews ◽  
E. Wyllys Andrews ◽  
Fernando Robles Castellanos

Recent adjustments to the chronology of the northern Maya Lowlands have brought about a closer alignment of the decline of Terminal Classic/Early Postclassic Yucatecan polities with the collapse of the southern Maya states. The collapse of the entire Classic-period societal structure throughout the lowlands can now be compressed into a 200- or 250-year period and seen as a progressive chain of events that began in the south and culminated with the fall of Chichen Itza in the eleventh century. This new reconstruction has led us to propose eliminating the Early Postclassic period, the existence of which was based largely on a purportedly late occupation of Chichen Itza. We assign this final occupation of the Itza capital to the Terminal Classic period, which ended sometime in the eleventh century in the northern Maya Lowlands.

2001 ◽  
Vol 12 (2) ◽  
pp. 149-166 ◽  
Author(s):  
Kevin J. Johnston ◽  
Andrew J. Breckenridge ◽  
Barbara C. Hansen

Magnetic, palynological, and paleoecological data indicate that in the Río de la Pasión drainage, one of the most thoroughly investigated areas of the southern Maya lowlands, a refugee population remained in the Laguna Las Pozas basin long after the Classic Maya collapse and the Terminal Classic period, previously identified by archaeologists as eras of near-total regional abandonment. During the Early Postclassic period, ca. A. D. 900 to 1200, agriculturalists colonized and deforested the Laguna Las Pozas basin for agriculture while adjacent, abandoned terrain was undergoing reforestation. After discussing the archaeological utility of magnetic analyses, we conclude that following the Maya collapse, some refugee populations migrated to geographically marginal non-degraded landscapes within the southern lowlands not previously occupied by the Classic Maya.


1982 ◽  
Vol 47 (3) ◽  
pp. 596-614 ◽  
Author(s):  
Diane Z. Chase ◽  
Arlen F. Chase

Excavations undertaken during 1978 and 1979 at Nohmul, Belize are believed to cast new light on the demise of the Maya. Investigations revealed Terminal Classic-San Jose V material intermixed with Late Classic to Early Postclassic Yucatec material in a single-unit refuse deposit. More importantly, striking architectural similarities exist between structures at Nohmul and Chichen-Itza; Structure 20 at Nohmul proved to be of the “patio-quad” type known previously only from Chichen-Itza, and Structure 9 of Nohmul may be put forth as a “Caracol” (Chichen-Itza Structure 3C15) counterpart. On the basis of excavations at Nohmul, it is implied that there is an association between Toltec Chichen-Itza (Sotuta) and the Terminal Classic periods to the south (San Jose V-Tepeu 3), in that the two are overlapping, if not coeval. Should this be the case, new alternatives relating to the Maya collapse must be considered.


1987 ◽  
Vol 52 (2) ◽  
pp. 367-382 ◽  
Author(s):  
Bruce H. Dahlin ◽  
Robin Quizar ◽  
Andrea Dahlin

Based on published lexicostatistical dates, two intervals in the prehistory of southern Mesoamerica stand out as fertile periods in terms of the generation of new languages: the Terminal Preclassic/early Early Classic Periods, and the Early Postclassic Period. After comparing archaeological evidence with language distributions within the subregions of southern Mesoamerica during the first of these periods, we conclude that the cultural processes during both periods had the same potential for producing rapid rates of linguistic divergences. Just as rapid proliferation of linguistic divisions was symptomatic of the well-known collapse of Late Classic Maya civilization, so it can be taken as a sign of a collapse of Terminal Preclassic civilization. Both collapses were characterized by severe population reductions, site abandonments, an increasing balkanization in material culture, and disruption of interregional communication networks, conditions that were contributory to the kind of linguistic isolation that allows language divergences. Unlike in the Terminal Classic collapse episode, small refuge zones persisted in the Early Classic Period that served as sources of an evolving classicism; these refuge zones were exceptions, however, not the rule. Although the collapse of each site had its own proximate cause, we suggest that the enormous geographical range covered by these Early Classic Period site failures points to a single ultimate cause affecting the area as a whole, such as the onset of a prolonged and devastating climatic change.


2012 ◽  
Vol 23 (2) ◽  
pp. 345-364 ◽  
Author(s):  
T. Kam Manahan ◽  
Traci Ardren ◽  
Alejandra Alonso Olvera

AbstractWhile changing views of the sociopolitical history of the northern Maya lowlands now recognize that Chichen Itza's emergence as a major polity on an unprecedented scale occurred during the Terminal Classic period, rather than the Early Postclassic period, the ramifications of significant chronological overlap between Chichen Itza's rise and the demise of neighboring polities have been largely unexplored. The ancient Maya center of Xuenkal, located in the Cupul region about 45 km northeast of Chichen Itza, is one of the few known interior sites to contain substantial (and discrete) Cehpech and Sotuta occupations. The Proyecto Arqueológico Xuenkal (PAX) was initiated in 2004 to elucidate Chichen Itza's role in the history of the Cupul region and what role local Xuenkal elites may have played in negotiating regional political dynamics. As with many surrounding centers, it appears that Xuenkal's occupational history reached its zenith with the Late Classic–Terminal Classic Cehpech ceramic sphere. However, unlike neighboring sites associated with Cehpech, such as Ek' Balam or Yaxuna, Xuenkal also contained a substantial Sotuta settlement concentrated within the site core during the Terminal Classic period. These populations adapted into an evolving regional economy by dramatically increasing household production as compared to Late Classic groups. While Sotuta households were tightly integrated into Chichen Itza's regional economy, evidence for their direct state control is not readily apparent. We suggest that the relationship between Chichen Itza and regional communities was more dynamic than current models contend, and that Chichen Itza's political machinations across the peninsula must be considered in local contexts that varied across households, communities, and regions.


1998 ◽  
Vol 9 (2) ◽  
pp. 183-232 ◽  
Author(s):  
William M. Ringle ◽  
Tomás Gallareta Negrón ◽  
George J. Bey

AbstractContinuing analysis of the site of Chichen Itza suggests that its construction dates primarily to the Late Classic period, ca. a.d. 700–1000, rather than the Early Postclassic. This paper examines the implications of this redating for the well-known “Toltec” problem. Since Chichen largely antedated Tollan-phase Tula, we conclude that what is usually identified as Toltec imagery in fact dates to an earlier Epiclassic horizon extending from Morelos and Puebla to the Gulf Coast and Yucatan. Chichen Itza, we suggest, was the eastern node in a network of shrine centers dedicated primarily to Quetzalcoatl/Kukulcan. This network transcended political boundaries and included such sites as Cholula, Cacaxtla, El TajIn, Xochicalco, and ultimately Tula. The Quetzalcoatl cult is manifested by a specific complex of traits and seems to have expanded militarily with messianic vigor. Pilgrimage was also an important activity at these centers. This cult axis apparently continued into the Postclassic period, and was responsible for the distribution of the Mixteca-Puebla art style. In Yucatan, Mayapan would seem to have assumed Chichen's position as the major Yucatecan node, although accompanied by several new shrines along the Caribbean coast.


1998 ◽  
Vol 9 (1) ◽  
pp. 151-165 ◽  
Author(s):  
Patricia K. Anderson

AbstractA major impediment to understanding the Terminal Classic to Early Postclassic transition in northern Yucatan has been the lack of a reliable ceramic chronology defined from stratigraphic contexts at the site of Chichen Itza. The temporal relationship of Cehpech and Soluta ceramics is central to resolving the issue of the correct chronological placement of Chichen Itza. The results of stratigraphic excavations at Yula, a small site 5 km south of Chichen Itza, provide the strongest evidence to date that Cehpech and Sotuta ceramics were contemporaneous. Statistical analysis of pottery composition by stratum confirms a positive correlation between Sotuta and Cehpech, which are clearly differentiated from earlier pottery. Rather than following a linear sequence in which Cehpech precedes Sotuta, as suggested by R. E. Smith and other early researchers, these two slatewares represent coeval regional variation. Thus, the major occupation of Chichen Itza dates not to the Early Postclassic, but to the Terminal Classic. The results of this research contribute toward the redefinition of the Terminal Classic and Early Postclassic periods in the northern Maya lowlands.


2015 ◽  
Vol 26 (1) ◽  
pp. 113-126 ◽  
Author(s):  
Scott A. J. Johnson

AbstractThe Sotuta pottery complex has been used in the archaeology of the northern Maya lowlands to identify the Terminal Classic period and cultural association with Chichen Itza. The Sotuta complex, however, is made up of many pottery types, the majority of which are inappropriate markers of elite sociopolitical history. It is argued here that Sotuta-complex slate wares developed out of previous local slate wares regardless of the elite sociopolitical changes taking place with the arrival of the Itza. The wares produced and distributed by commoners were independent of elites and have been artificially chained to questions of elite political expansion for which they are inappropriate correlates.


2015 ◽  
Vol 112 (18) ◽  
pp. 5607-5612 ◽  
Author(s):  
Peter M. J. Douglas ◽  
Mark Pagani ◽  
Marcello A. Canuto ◽  
Mark Brenner ◽  
David A. Hodell ◽  
...  

Paleoclimate records indicate a series of severe droughts was associated with societal collapse of the Classic Maya during the Terminal Classic period (∼800–950 C.E.). Evidence for drought largely derives from the drier, less populated northern Maya Lowlands but does not explain more pronounced and earlier societal disruption in the relatively humid southern Maya Lowlands. Here we apply hydrogen and carbon isotope compositions of plant wax lipids in two lake sediment cores to assess changes in water availability and land use in both the northern and southern Maya lowlands. We show that relatively more intense drying occurred in the southern lowlands than in the northern lowlands during the Terminal Classic period, consistent with earlier and more persistent societal decline in the south. Our results also indicate a period of substantial drying in the southern Maya Lowlands from ∼200 C.E. to 500 C.E., during the Terminal Preclassic and Early Classic periods. Plant wax carbon isotope records indicate a decline in C4 plants in both lake catchments during the Early Classic period, interpreted to reflect a shift from extensive agriculture to intensive, water-conservative maize cultivation that was motivated by a drying climate. Our results imply that agricultural adaptations developed in response to earlier droughts were initially successful, but failed under the more severe droughts of the Terminal Classic period.


2001 ◽  
Vol 12 (2) ◽  
pp. 175-197 ◽  
Author(s):  
Donald McVicker ◽  
Joel W. Palka

In the early 1880s, a finely carved Maya shell picture plaque was found at the Toltec capital of Tula, central Mexico, and was subsequently acquired by The Field Museum in Chicago. The shell was probably re-carved in the Terminal Classic period and depicts a seated lord with associated Maya hieroglyphs on the front and back. Here the iconography and glyphic text of this unique artifact are examined, the species and habitat of the shell are described, and its archaeological and social context are interpreted. The Tula plaque is then compared with Maya carved jade picture plaques of similar size and design that were widely distributed throughout Mesoamerica, but were later concentrated in the sacred cenote at Chichen Itza. It is concluded that during the Late Classic period, these plaques played an important role in establishing contact between Maya lords and their counterparts representing peripheral and non-Maya domains. The picture plaques may have been elite Maya gifts establishing royal alliances with non-local polities and may have become prestige objects used in caches and termination rituals.


2005 ◽  
Vol 16 (2) ◽  
pp. 195-211 ◽  
Author(s):  
Christina M. Elson ◽  
Kenneth Mowbray

In 1931 and 1932, George Vaillant and Sigvald Linné excavated 34 burials and 17 offerings dating to the Early Postclassic period (a.d.900–1150). The features were located on the ruins of the Classic-period site of Teotihuacan and within the boundaries of a roughly 25–50 ha zone identified by the Teotihuacan Mapping Project as having a dense Early Postclassic-period occupation. The results of Vaillant's excavations have not been published. An examination of the Vaillant–Linné data sheds new light on Early Postclassic-period mortuary ritual and social organization. The identification of several types of burials shows that local people conducted primary and secondary mortuary rituals and indicates the presence of at least two social strata at the site. The content of the burials and offerings supports a division of the Early Postclassic period into two local phases, Mazapan (ca.a.d.900–1000) and Atlatongo (ca.a.d.1000–1100/1150), with these features dating to the earlier phase.


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