(This is a guest post by Gary Feinman)
Published in the journal Science, Medina-Elizalde and Rohling’s (2012) quantitative analysis
of Terminal Classic period Maya (AD 800-1000) climatic shifts is a welcome
refinement of the extent of a late 1st millennium episode of
climatic change. Yet the authors' speculations regarding the fall of inland
Maya settlements (the so-called Maya Collapse) is fraught with failures in
logic and limitations in hypothesis evaluation that too often are characteristic
of natural scientists delving naively into the causes and complexities of
societal change. Even more problematic is the repeated license given by one of
the world’s premier science journals to this kind of disciplinary overreach at
a time when extremely few articles by archaeologists are offered this broadly
visible platform.
Medina-Elizalde and Rohling begin
with the premise that drought precipitated the collapse of these inland
centers. But, when finding precipitation declines of only 40%, they do not
reconsider their presumed causality, instead inferring that the Maya polities
were so fragile that even the estimated rainfall declines were enough to
generate collapse. These findings then underpin their policy warning that even
minor climatic shifts may fatally endanger contemporary states facing present
climatic shifts.
Left entirely unconsidered in their
historical reconstructions of causality are the numerous other factors, from
warfare to shifts in pan-Mesoamerican exchange patterns, that have been
advanced as keys to the fall of the Classic Maya states. The consideration,
evaluation, and elimination of alternative hypotheses are central to truly
scientific inquiry, and their absence from this work only reinforces the
preconceived bias that the prehispanic Maya were not sufficiently ingenious to
respond to natural environmental fluctuations. It is crucial to recognize that
Maya polities in northern Yucatán and coastal Belize, some of the driest parts
of the Maya domain, thrived during and after the decline of inland settlements
and populations.
Also problematic are the advanced
policy implications. While I share concerns about anthropogenic environmental
and climatic changes that hazard the modern world, the authors’ perspectives
view humans as incapable of forging effective responses to external
perturbations. And yet, those of us dedicated to understanding our species’
history recognize that we have repeatedly established cooperative networks at
various scales to address and forestall similar challenges. If modern societies
fail and fall, the responsibilities will be borne in part by our cooperative,
competitive, and leadership networks and arrangements rather than merely the
consequence of declines in rainfall.
At its current best, contemporary
archaeological practice strives for serious evaluations of the causes and
consequences of social actions and change. Repeatedly we have seen that through
history rarely have climatic perturbations alone been both the proximate and
ultimate causes of significant shifts in human settlement and catastrophic
upheavals in political organization (e.g., Middleton 2012). Given the problems
faced by our species today, the publishers of Science ought to lend their weighty profile and give greater voice
to those of us endeavoring to understand the repertoire of behaviors that
humans and their social groupings have derived and innovated to address the
suite of challenges that they have faced. Many of those historical episodes may
bear key insights for addressing the hazards and challenges that we as a
species and a society face today.
References
Cited
Medina-Elizalde, Martín, and Eelco J.
Rohling
2012 Collapse of Classic Maya
Civilization related to modest reduction in precipitation. Science 335:956-959.
Middleton, Guy D.
2012 Nothing lasts forever:
environmental discourses on the collapse of past societies. Journal of Archaeological Research 20. In press (available online).
Gary M. Feinman
The Field Museum

















