Climate and the collapse of Maya civilization

Gerald H. Haug, Detlef Günther, Larry C. Peterson, Daniel Mikhail Sigman, Konrad A. Hughen, Beat Aeschlimann

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617 Scopus citations

Abstract

In the anoxic Cariaco Basin of the southern Caribbean, the bulk titanium content of undisturbed sediment reflects variations in riverine input and the hydrological cycle over northern tropical South America. A seasonally resolved record of titanium shows that the collapse of Maya civilization in the Terminal Classic Period occurred during an extended regional dry period, punctuated by more intense multiyear droughts centered at approximately 810, 860, and 910 A.D. These new data suggest that a century-scale decline in rainfall put a general strain on resources in the region, which was then exacerbated by abrupt drought events, contributing to the social stresses that led to the Maya demise.

Original languageEnglish (US)
Pages (from-to)1731-1735
Number of pages5
JournalScience
Volume299
Issue number5613
DOIs
StatePublished - Mar 14 2003

All Science Journal Classification (ASJC) codes

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    Haug, G. H., Günther, D., Peterson, L. C., Sigman, D. M., Hughen, K. A., & Aeschlimann, B. (2003). Climate and the collapse of Maya civilization. Science, 299(5613), 1731-1735. https://doi.org/10.1126/science.1080444