Waves of Political Ruptures during the Terminal Classic in the Pasión and Other Regions of the Maya Lowlands

Maya Kingship ◽  
2021 ◽  
pp. 51-63
Author(s):  
TAKESHI INOMATA
Keyword(s):  
Maya Lowlands ◽  
Terminal Classic

The Chronology of Yaxuna

1998 ◽  
Vol 9 (1) ◽  
pp. 167-182 ◽  
Author(s):  
Charles Suhler ◽  
Traci Ardren ◽  
David Johnstone
Keyword(s):  
Cultural History ◽  
Cultural Development ◽  
The Political ◽  
Ancient Maya ◽  
Urban Center ◽  
Maya Lowlands ◽  
Terminal Classic ◽  
History Of ◽  
Late Formative ◽  
Middle Formative

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.

scholarly journals Drought, agricultural adaptation, and sociopolitical collapse 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 ◽  
...  
Keyword(s):  
Carbon Isotope ◽  
Sediment Cores ◽  
Classic Period ◽  
Maya Lowlands ◽  
Agricultural Adaptation ◽  
Terminal Classic ◽  
Paleoclimate Records ◽  
Early Classic Period ◽  
Plant Wax ◽  
Terminal Classic Period

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.

Classic-to-Contact-Period Continuities in Maya Governance in Central Petén, Guatemala

Ethnohistory ◽  
2018 ◽  
Vol 65 (1) ◽  
pp. 25-50 ◽  
Author(s):  
Prudence M. Rice ◽  
Don S. Rice
Keyword(s):  
Power Sharing ◽  
Classic Period ◽  
Contact Period ◽  
Maya Lowlands ◽  
Archaeological Data ◽  
Terminal Classic ◽  
Governance Strategies ◽  
Per Se

Abstract This article integrates ethnohistorical and archaeological data in examining political continuities or structural equivalencies in the lakes region of central Petén (southern Maya lowlands) between the Late and Terminal Classic periods and the Postclassic and Spanish Contact periods. The equivalencies are of three kinds: “deep structures” (quadripartition), common political expediencies and functions (power-sharing and council houses), and temporal continuities per se (dual rulership). The article concludes that the rupture (“collapse”) between Classic and Postclassic political forms was only partial, and numerous structures and practices of late Petén Itza Maya geopolitical organization can be seen in earlier Classic-period phenomena. These underscore long-term continuities in governance strategies.

Paleoecological Evidence of an Early Postclassic Occupation in the Southwestern Maya Lowlands: Laguna Las Pozas, Guatemala

2001 ◽  
Vol 12 (2) ◽  
pp. 149-166 ◽  
Author(s):  
Kevin J. Johnston ◽  
Andrew J. Breckenridge ◽  
Barbara C. Hansen
Keyword(s):  
Classic Maya ◽  
Classic Period ◽  
Maya Lowlands ◽  
Postclassic Period ◽  
Refugee Population ◽  
Terminal Classic ◽  
Early Postclassic ◽  
Maya Collapse ◽  
Terminal Classic Period

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.

Maya political history - Ellen E. Bell, Marcello A. Canuto & Robert J. Sharer (ed.). Understanding Early Classic Copan. xvii+439 pages, 135 figures, 14 colour photographs, 11 tables. 2004. Philadelphia (PA): University of Pennsylvania Museum of Archaeology & Anthropology; 1-931707-51-0 hardback $59.95. - Vernon L. Scarborough, Fred ValdezJr . & Nicholas Dunning (ed.). Heterarchy, political economy, and the ancient Maya: the Three Rivers region of the east-central Yucatán peninsula. xx+172 pages, 54 figures, 4 tables. 2003. Tucson (AZ): University of Arizona Press; 0-8165-2273-1 hardback $55. - Matthew G. Looper. Lightning Warrior: Maya art and kingship at Quirigua. xi+265 pages, 241 figures, 12 tables. 2003. Austin (TX): University of Texas Press; 0-292-70556-5 hardback $59.95. - Arthur A. Demarest, Prudence M. Rice & Don S. Rice (ed.). The Terminal Classic in the Maya lowlands: collapse, transition, and transformation. xix+676 pages, 125 figures, 27 tables. 2004. Boulder (CO): University Press of Colorado; 0-87081-739-6 hardback. - C. Roger Nance, Stephen L. Whittington & Barbara E. Borg with George Guillemin & Sergio Rodas Manrique. Archaeology and ethnohistory of Iximché. xxiv+408 pages, 161 figures, 80 tables. 2003. Gainesville (FL): University Press of Florida; 0-8130-2633-4 hardback $65.

Antiquity ◽  
2005 ◽  
Vol 79 (303) ◽  
pp. 210-214
Author(s):  
Elizabeth Graham
Keyword(s):  
Political Economy ◽  
University Of Pennsylvania ◽  
Ancient Maya ◽  
Maya Lowlands ◽  
East Central ◽  
University Of Texas ◽  
Terminal Classic ◽  
University Of Arizona ◽  
Three Rivers Region ◽  
Three Rivers

Classic to Postclassic at Ek Balam, Yucatan: Architectural and Ceramic Evidence for Defining the Transition

1997 ◽  
Vol 8 (3) ◽  
pp. 237-254 ◽  
Author(s):  
George J. Bey ◽  
Craig A. Hanson ◽  
William M. Ringle
Keyword(s):  
Yucatan Peninsula ◽  
Complex Societies ◽  
Ancient Maya ◽  
General Study ◽  
Late Classic ◽  
Maya Lowlands ◽  
Contemporary Debate ◽  
Terminal Classic ◽  
Yucatán Peninsula ◽  
Ek Balam

The Classic-to-Postclassic transition in the Maya Lowlands is a focus of contemporary debate. At the site of Ek Balam, Yucatán, excavation of Structure GS-12 provided an architectural stratigraphy that spans this period. GS-12-sub was a Late Classic (Pure Florescent) building razed during the construction of GS-12-1, a C-shaped structure of a form generally identified with Postclassic occupations on the Yucatán Peninsula. At Ek Balam the building is associated with Cehpech-sphere ceramics and dated to the Terminal Classic. These data are in general agreement with the dating of such structures at other lowland sites including Uxmal. We contend that C-shaped structures, when found associated with Cehpech-sphere ceramics, are a horizon marker for the Terminal Classic-to-Postclassic transition on the Yucatán Peninsula, and that they illustrate the culture changes that occurred at this still poorly understood boundary. They may be the remains of administrative buildings used by the Maya following the cessation of monumental construction at major centers. Besides contributing to our understanding of the ancient Maya, the implications of this article extend to the general study of collapse and abandonment of complex societies.

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