The ancient Maya once claimed an area about the size of Texas, with cities and fields that occupied what is now southern Mexico and northern Central America, including the countries of Guatemala, Belize, El Salvador and Honduras. The height of the Mayan civilization, known as the Classic period, extended from approximately A.D. 250 to at least 900.
For unknown reasons, the Classic Mayan civilization then collapsed. The population declined catastrophically to a fraction of its former size, and many of their great cities were left mostly abandoned for the jungle to reclaim.
Scientists have long drawn connections between the decline of the ancient Maya and environmental catastrophes, especially drought. Deforestation linked with farming could also have triggered disaster — for instance, reduced tree cover of the ground would have led to loss of fertile topsoil by erosion, as well as greater evaporation of water by sunlight, exacerbating drought.
However, while some locales remain abandoned for long periods, others recovered more quickly. This patchwork pattern of recovery might argue against environmental catastrophes being the sole determining factor behind the collapse of the Classic Mayan civilization — if they were, one might expect such catastrophes to affect all areas equally.
Moreover, archaeologists have pointed out that ancient Mayan societies may have been vulnerable to collapse by their very nature. They apparently funneled wealth to a small ruling elite topped by hereditary divine kings, who had virtually unlimited power but whose subjects expected generosity — a string of military defeats or seasonal droughts could greatly damage their credibility. The stability of this system was further threatened by polygamy among rulers, spawning numerous lineages that warred against each other, overall generating conditions ripe for collapse.
To learn more about the reasons behind the patchy apocalypse and recovery, scientists focused on social declines seen in the terminal part of the Classic period in the Mayan lowlands, ranging from A.D. 750 to 950. They also looked at downturns from A.D. 100 to 250, the terminal part of the "Pre-Classic" period.
Available data suggested the elevated parts of the Mayan lowlands, which include much of today's Yucatan Peninsula, were significantly more vulnerable to collapse and less likely to recover than lower-lying areas. Sites within this elevated region lacked perennial water sources and were more dependent solely on what rainwater they could capture and store, leaving them vulnerable to shifts in climate. In contrast, neighboring lower-lying areas had access to springs, perennial streams and sinkholes known as cenotes that were often filled with water.
Reoccupying elevated interior areas with large numbers of people would require intense labor to re-establish water management systems, helping to explain why they were left abandoned, the researchers noted. In contrast, dwelling in the neighboring, low-lying areas was less challenging, and evidence suggests that sites there were typically occupied continuously even when the major political and economic networks they were linked with collapsed.
At the same time, the Classic Maya would have implicated gods and their "divine" rulers for the collapse. In that way, their abandoned territories became thought of as chaotic, haunted places, and reclaiming any lands from the forest was at best done with great care and ritual. Survivors in outlying sites may often not have bothered. "Reoccupation called for a reordering of a most profound kind," the researchers write in the March 6 issue of the journal Proceedings of the National Academy of Sciences.
"I have little doubt that droughts and environmental degradation — for example, soil erosion or declining soil fertility — played roles in the collapse, defined here as a substantial and prolonged decline in population, of some sites or regions," said researcher Nicholas Dunning, a geographer at the University of Cincinnati. "There is also the important role played by the environmental setting of sites — for example, sites in the elevated interior region were significantly more vulnerable to drought cycles than those in surrounding lower-elevation areas where water was more abundant."
Read more at Discovery News
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