Social-Political Manifestations of the Terminal Classic

Author(s):  
Palma J. Buttles ◽  
Fred Valdez
Keyword(s):  
1998 ◽  
Vol 9 (1) ◽  
pp. 167-182 ◽  
Author(s):  
Charles Suhler ◽  
Traci Ardren ◽  
David Johnstone

AbstractResearch at the ancient Maya city of Yaxuna, located in the heart of the Yucatan Peninsula, has provided sufficient data to suggest a preliminary chronological framework for the cultural development of this large polity. Primary ceramic and stratigraphie data are presented to support a five-phase scheme of cultural history, encompassing the Middle Formative through Postclassic periods (500 b.c.–a.d. 1250). In addition to chronological significance, the political ramifications of a pan-lowland ceramic trade are addressed. Yaxuna experienced an early florescence in the Late Formative–Early Classic periods, when it was the largest urban center in the central peninsula. A second renaissance in the Terminal Classic period was the result of Yaxuna's role in an alliance between the Puuc and Coba, in opposition to growing Itza militancy. This paper proposes a chronological framework for the cultural development of one northern Maya region in order to facilitate an understanding of this area as part of the overall history of polity interaction and competition in the Maya lowlands.


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.


2012 ◽  
Vol 23 (1) ◽  
pp. 93-119 ◽  
Author(s):  
Brent K.S. Woodfill ◽  
Stanley Guenter ◽  
Mirza Monterroso

AbstractThe Cave of Hun Nal Ye, located in central Guatemala, was discovered unlooted by a local landowner in 2005 and was immediately subject to investigation by the authors. The cave contained ritual remains dating to between the Terminal Pre-classic and Terminal Classic. In addition to allowing a detailed reconstruction of ritual activity in the northern highlands, its presence along the Great Western Trade Route allows archaeologists to examine hypotheses about interregional trade during the Classic period. In particular, changes in the ritual assemblage between the Early and Late Classic indicate that the cave was an important trade shrine for merchants and travelers passing between the highlands and lowlands until ca. A.D. 550, at which point it became a local shrine used to reinforce elite power. These changes are then linked to larger patterns occurring in other parts of the trade route, especially to Tikal and the kingdoms along the Pasión and Usumacinta rivers.


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.


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.


2014 ◽  
Vol 25 (1) ◽  
pp. 115-137 ◽  
Author(s):  
Kerry Lynn Sagebiel

AbstractPrevious interpretations of the occupation history of La Milpa, Belize, which were based on preliminary ceramic data, suggested that occupation of the site fluctuated dramatically from the Late Preclassic to the Terminal Classic (400 b.c.–a.d. 850). It was determined that the modest Late Preclassic village became a large Early Classic city with regal-ritual architecture and carved monuments. In Late Classic I, it appeared the site was nearly abandoned. Its reoccupation and exponential growth in Late Classic II was followed by rapid abandonment before the end of the Late Classic III/Terminal Classic. New ceramic analyses utilizing attribute analysis with an emphasis on formal modes has clarified the sequence and, in turn, softened the occupation curves. This article provides descriptions of the Late Classic I, II, and III ceramics, along with revised percentage frequency graphs of La Milpa's occupation history based primarily on the work of the La Milpa Archaeological Project (1992–2002).


1984 ◽  
Vol 49 (4) ◽  
pp. 815-820 ◽  
Author(s):  
Norman Hammond ◽  
Mary D. Neivens ◽  
Garman Harbottle

Forty-nine obsidian artifacts from a Classic period residential group at Nohmul, northern Belize, have been analyzed by neutron activation analysis. The majority of the samples originated from Ixtepeque, and the remainder from El Chayal. Increasing prominence of the Ixtepeque source from the Late Classic into the Terminal Classic (i.e., before and after ca. A.D. 800) suggests greater use of a coastal distribution route known to have originated in the Formative and to have remained in use through the colonial period.


Author(s):  
Charles W. Golden ◽  
Andrew K. Scherer

In chapter 11, Charles Golden and Andrew Scherer discuss how the political and economic landscapes in the western lowlands impacted the monumental landscape of the Late and Terminal Classic periods along the Usumacinta River. These landscapes shaped, and were shaped by, dynastic power struggles between the kingdoms of Palenque, Piedras Negras, Tonina, and Yaxchilan, and impacted the function and flow of goods and people across the region. Drawing on epigraphic research, excavation results, ground survey, and remotely sensed data gathered during 15 field seasons of regional survey, the authors emphasize the movement of people and goods; movement was affected by friction resulting from the physicality and political dynamics of the landscape. It was this friction—and attempts to increase or reduce it through warfare and marriage alliances—that shaped travel and trade during the Classic period and, in turn, was crafted in stone at Piedras Negras and Yaxchilan. For the authors, the representations of lords and ladies, allies and captives, carved on lintels, stairs, and stelae at Piedras Negras and Yaxchilan are truly monumental landscapes.


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