Paleoclimatologist: Speleothems (mineral deposits such as stalagmites) in a highland cavern preserve distinct annual layers with oxygen isotope ratios () that fluctuate in response to rainfall. Analysis of a stalagmite spanning the eleventh to thirteenth centuries reveals a pronounced forty-year interval of highly enriched values, indicative of diminished local precipitation. Because historical agricultural annals from the adjacent low-lying river valley record widespread crop failures and village abandonment during this identical forty-year window, researchers conclude that a prolonged regional drought caused the abandonment of these agrarian settlements.
Statement: The finding that drought-sensitive teak trees throughout the adjacent river valley exhibited an unprecedented suppression in annual growth-ring widths during the same forty-year interval logically strengthens the paleoclimatologist's conclusion.
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