scholarly journals Folkecology and commons management in the Maya Lowlands

1999 ◽  
Vol 96 (13) ◽  
pp. 7598-7603 ◽  
Author(s):  
S. Atran ◽  
D. Medin ◽  
N. Ross ◽  
E. Lynch ◽  
J. Coley ◽  
...  
Radiocarbon ◽  
2021 ◽  
pp. 1-26
Author(s):  
Julie A Hoggarth ◽  
Brendan J Culleton ◽  
Jaime J Awe ◽  
Christophe Helmke ◽  
Sydney Lonaker ◽  
...  

ABSTRACT Deposits linked to abandonment have been widely recorded across the Maya lowlands, associated with the final activities occurring in ceremonial areas of Classic Maya centers. Various models have been applied to explain the activities that lie behind the formation of these contexts, including those linked to rapid abandonment (e.g., warfare) and others focused on more protracted events (termination rituals, and/or pilgrimages). Here, we assess Bayesian models for three chronological scenarios of varying tempo to explain the formation of peri-abandonment deposits at Baking Pot, Belize. Using stratigraphic information from these deposits, hieroglyphic dates recovered on artifacts, and direct dates on human skeletal remains and faunal remains from distinct layers in three deposits in Group B at Baking Pot, we identify multiple depositional events that spanned the eighth to ninth centuries AD. These results suggest that the processes associated with the breakdown of institutionalized rulership and its command of labor to construct and maintain ceremonial spaces were protracted at Baking Pot, with evidence for the final depositional activity dated to the mid-to-late ninth century. This interval of deposition was temporally distinct from the earlier deposition(s) in the eighth century. Together, these data offer a detailed view of the end of the Classic period at Baking Pot, in which the ceremonial spaces of the site slowly fell into disuse over a period of more than a century.


2021 ◽  
Vol 258 ◽  
pp. 106904
Author(s):  
Benjamin Keenan ◽  
Anic Imfeld ◽  
Kevin Johnston ◽  
Andy Breckenridge ◽  
Yves Gélinas ◽  
...  

1970 ◽  
Vol 69 (6) ◽  
pp. 354-363
Author(s):  
Mildred Berman

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.


2014 ◽  
Vol 103 ◽  
pp. 19-25 ◽  
Author(s):  
David Wahl ◽  
Roger Byrne ◽  
Lysanna Anderson

Sign in / Sign up

Export Citation Format

Share Document