In a dark chamber beneath Yucatán, a stalagmite recorded the rise and strain of a civilization. By sampling oxygen isotopes layer by layer in Grutas Tzabnah, a team led by the University of Cambridge reconstructed rainfall for individual wet and dry seasons between 871 and 1021 CE, the Terminal Classic of Maya history. Reported in Science Advances, the record reveals eight multi year wet season droughts, including an extraordinary stretch of thirteen consecutive years. If you rely on rain timed to planting, what happens when the wet season fails again and again? The answer, this study suggests, is written both in stone and in the fate of Maya cities.
What The Stalagmite Shows
- Eight wet season droughts lasted at least three years between 871 and 1021 CE.
- The longest drought persisted for thirteen consecutive years.
- Subannual resolution let researchers isolate wet versus dry season signals, the time window that decides crop success or failure.
- Replicated patterns align with earlier stalagmite and lake records, strengthening confidence in the chronology.
Why Seasonality Matters
Stalagmites grow in annual layers as mineral rich water drips to the cave floor. The isotopes shift with the seasons, letting scientists read the wet season specifically. That is the critical window for maize and other staples. As lead author Dr Daniel H. James put it, “Knowing the annual average rainfall doesn’t tell you as much as knowing what each individual wet season was like.” He added, “Being able to isolate the wet season allows us to accurately track the duration of wet season drought, which is what determines if crops succeed or fail.”
Climate And Culture, In Sync And Out Of Step
During the Terminal Classic, dynasties ended and southern cities were abandoned as power shifted north. The precisely dated droughts provide a tighter frame for comparing environmental stress with cultural change. At major northern sites like Chichén Itzá and Uxmal, monument construction and date inscriptions halted at different times during these drought sequences. “This doesn’t necessarily mean that the Maya abandoned Chichén Itzá during these periods of severe drought, but it’s likely that they had more immediate things to worry about than constructing monuments, such as whether the crops they relied on would succeed or not,” James said.
From Cave Drips To City Timelines
The team counted 186 annual laminae with subannual sampling of each layer for δ18O. They anchored the chronology with multiple U Th ages, then compared it with archaeological datasets and other regional climate archives, including prior records from the same cave and Belize. Earlier lake sediment studies captured big swings, but not year by year wet season detail at specific sites. The new record closes that gap.
Method As Narrative
Stalagmites turn drops into dates. Each light and dark band is a season. Each shift in isotopes marks a swing toward drought or wet years. The result is a seasonal climate diary that can be read alongside the public diaries of cities, their stelae and building phases. “It hasn’t been possible to directly compare the history of individual Maya sites with what we previously knew about the climate record,” James said. “Lake sediment is great when you want to look at the big picture, but stalagmites allow us to access the fine grained detail that we’ve been missing.”
“This period in Maya history has been a cause of fascination for centuries,” said James. “There have been multiple theories as to what caused the collapse, such as changing trade routes, war or severe drought, based on the archaeological evidence the Maya left behind. But in the past few decades, we’ve started to learn quite a lot about what happened to the Maya and why, by combining the archaeological data with quantifiable climate evidence.”
Implications Beyond The Past
Seasonal precision helps modern planners too. Many regions still depend on a predictable onset of rains. Subannual cave records can show how long multi year wet season failures persisted and how societies adapted or strained. The team notes that stalagmites may also record tropical storm signals, opening new lines of risk analysis for today’s drought vulnerable communities.
Study Details
Title: Classic Maya response to multiyear seasonal droughts in Northwest Yucatán, Mexico
Authors: Daniel H. James, Stacy A. Carolin, Sebastian F. M. Breitenbach, Julie A. Hoggarth, Fernanda Lases Hernández, Erin A. Endsley, Jason H. Curtis, Christina D. Gallup, Susan Milbrath, David A. Hodell, and colleagues
Field site: Grutas Tzabnah, near Tecoh, Yucatán, Mexico. See background on Grutas Tzabnah and regional centers like Uxmal.
Citation
Science Advances, 13 August 2025. DOI: 10.1126/sciadv.adw7661
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