Overview
- A research team led by Daniel H. James used oxygen-isotope analysis of a stalagmite from Grutas Tzabnah to produce the first sub-annual rainfall reconstruction for 871–1021 CE.
- The high-resolution record identifies eight wet-season droughts lasting at least three years during the Terminal Classic period.
- The most severe drought persisted for approximately 13 consecutive years between 929 and 942 CE, the longest recorded in the region.
- These drought episodes coincide with archaeological indicators of site abandonment and paused monument construction at major Maya centers such as Chichén Itzá and Labna.
- The dataset establishes a framework for precise synchronization of climate events with local archaeological chronologies and paves the way for additional cave-based records across the Yucatán.