UNM Research on Disintegration of Maya Political Systems and Climate Change Featured in “Science”

The cover story in the jour­nal “Sci­ence” this week fea­tures long-term research by an inter­na­tional group of anthro­pol­o­gists and earth and cli­mate sci­en­tists, includ­ing researchers from the Uni­ver­sity of New Mex­ico, who took a care­ful look at the impact of cli­mate change on Maya polit­i­cal sys­tems. Their paper, “Devel­op­ment and Dis­in­te­gra­tion of Maya Polit­i­cal Sys­tems in Response to Cli­mate Change,” explores the effect of vari­a­tions in rainfall.

To doc­u­ment the rain­fall amounts, the group ana­lyzed a sta­lag­mite from Yok Balum cave in Belize. They pre­cisely tracked an increase in rain­fall between A.D. 450 and 600, then a decline in rain­fall, punc­tu­ated by a series of short droughts 200 years later.

This cor­re­lates with explo­sive growth and rapid expan­sion of Maya states across the low­lands, the pro­lif­er­a­tion of kings, and of carved mon­u­ments that talk about their suc­cesses,” said Keith Prufer, asso­ciate pro­fes­sor of Anthro­pol­ogy at UNM and one of the prin­ci­pal investigators. “Starting around the mid­dle of the sev­enth cen­tury you see a decline in rain­fall, cor­re­spond­ing with increas­ing inci­dents of war­fare between com­pet­ing states. There were a series of short droughts simul­ta­ne­ous with a col­lapse of poli­ties in the south­ern low­lands of Belize and Guatemala.  The north­ern part of the Maya cul­ture in the Yucatan Penin­sula con­tin­ued to flour­ish well into the ninth cen­tury when a mas­sive pro­tracted drought begin­ning in the 11th cen­tury cor­re­sponds with a dra­matic col­lapse at Chichen Itza and may have pre­vented the recov­ery of extant com­plex polit­i­cal systems.”

The pre­cise chrono­log­i­cal recon­struc­tion of the cli­mate record was con­ducted at the Radi­ogenic Iso­tope Lab­o­ra­tory at UNM Earth and Plan­e­tary Sci­ences, directed by Prin­ci­pal Inves­ti­ga­tor Yemane Asmerom along with Senior Research Sci­en­tist Vic­tor Polyak and anthro­pol­ogy doc­toral stu­dent Val­o­rie Aquino. Some of the tech­ni­cal work was done by Aquino who drilled tiny trenches in the sta­lag­mite and mea­sured ratios of Ura­nium and Tho­rium iso­topes from pow­ders to accu­rately date the age of dif­fer­ent lay­ers linked to cli­mate change.

The link between changes in cli­mate and cul­ture, espe­cially as it relates to the Maya Civ­i­liza­tion, has been of long-standing sci­en­tific inter­est,” said Asmerom. “What makes our find­ings in this regard unique is the fact that we can doc­u­ment tim­ing of cli­mate tran­si­tions with unprece­dented pre­ci­sion, thanks to tech­ni­cal devel­op­ments in uranium-series dat­ing for which our lab is one of the lead­ing labs in the world, and the very detailed and exhaus­tive field-based work done by our groups.”

Prufer says the group was uniquely able to doc­u­ment the effects of cli­mate change on the rise and col­lapse of an entire cul­ture. But the research team wants to move further.

One of the goals is to see if we could begin to model human responses to cli­mate change in ways that could apply gen­er­ally,” he says. “The Maya are an excel­lent empir­i­cal case study given the long his­tory of archae­o­log­i­cal research in the area and the pres­ence of explicit texts detail­ing the activ­i­ties of kings and dates when they were in power.”

Co-authors of the arti­cle include Dou­glas Ken­nett, Penn State; Sebas­t­ian F.M. Bre­it­en­bach, Eid­genös­sis­che Tech­nis­che Hochschule Zürich, Zurich, Switzerland; Jaime Awe, National Insti­tute of Cul­ture and His­tory, Belize; James Bal­dini, Uni­ver­sity of Durham, UK; Patrick Bartlein, Uni­ver­sity of Ore­gon; Bren­dan Cul­leton, Claire Ebert, and Christo­pher Jazwa, Penn State; Martha Macri, Uni­ver­sity of Cal­i­for­nia, Davis; Nor­bert Mar­wan, Pots­dam Insti­tute for Cli­mate Impact Research, Ger­many; Har­riet Rid­ley, Uni­ver­sity of Durham; Har­ald Sodemann, Eidgenössische Tech­nis­che Hochschule Zürich; Bruce Win­ter­halder, Uni­ver­sity of Cal­i­for­nia, Davis; and Ger­ald Haug, Eid­genös­sis­che Tech­nis­che Hochschule Zürich.

The study was funded by the U.S. National Sci­ence Foun­da­tion, Euro­pean Research Coun­cil, Swiss National Sci­ence Foun­da­tion, Ger­man Sci­ence Foun­da­tion and the Alpha­wood Foundation.

Media con­tacts: Keith Prufer (505) 918‑6763; email: kmp@unm.edu or Yemane Asmeron (505) 379‑4850; email: asmerom@unm.edu

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