A person wearing a helmet, headlamp, and climbing harness descends a sand-colored, steep rock face in a cave using a black rope. The cave is narrow and uneven.

For their study, the Innsbruck researchers rappelled 20 meters into a narrow shaft and squeezed through a narrow opening to reach the deepest part of Devils Hole II, which reaches the water table.

580,000 Years of Cli­mate His­tory Revealed

An international research team led by Christoph Spötl from the University of Innsbruck, Austria, has compiled an extraordinary climate reconstruction based on data from a cave in Nevada, USA. The study provides unique insights into the climate history of one of the driest regions in North America – and shows how closely temperature, water availability, and vegetation are linked in arid regions.

“Devils Hole in the US offers a virtually unique opportunity to obtain long-term climate archives from calcite deposits,” emphasizes Christoph Spötl, head of the Quaternary Research Group at the Department of Geology of the University of Innsbruck. “Our many years of expertise in investigating such underground climate archives were crucial for obtaining and interpreting this extraordinary data.”

Rare climate archive tells Earth's history

In 2017, the Innsbruck expedition team succeeded in extracting a 1-meter-long drill core of calcite deposits from the deepest section of the Devils Hole II cave. Oxygen isotopes in the core document a continuous climate archive spanning 580,000 years—including the last six ice ages and the interglacial periods in between. “Our analysis shows an alternation between cool, wet ice ages and hot, dry interglacial periods,” says the study's lead author, Kathleen Wendt, now at the University of Toronto in Canada. “In the middle of some interglacial periods, there were abrupt drops in the groundwater level, which were accompanied by a significant decline in vegetation.”

The study also shows that winter rainstorms that are important for the region's water balance shifted far south during the ice ages. These shifts had a direct impact on groundwater and thus shaped living conditions in the southwestern United States in the long term. “This link between temperature, groundwater availability, and vegetation development is important for understanding future climate developments in arid regions,” explains Kathleen Wendt.

Two hands hold a long, narrow drill core made of shiny, semi-transparent rock with alternating white and brownish layers in a cave.

For hundreds of thousands of years, groundwater has been flowing through the cave and depositing calcite on the walls of the fissure, – visible here on a cylindrical drill core, similar to hard water deposits build up in drinking water pipes.

Leading role in paleoclimate research

The University of Innsbruck is one of the world's leading centers for paleoclimatology based on cave deposits. For decades, Innsbruck speleothem specialists have been regularly involved in pioneering work to access climate archives from hard-to-reach cave systems. Yuri Dublyansky, co-author of the current study, explains: “The fieldwork in Devils Hole was one of the most challenging projects we have ever been involved in. The combination of technical requirements and scientific opportunities was truly extraordinary.” Gina Moseley, cave explorer and award-winning expert at the University of Innsbruck, also emphasizes the importance of this work: “Such long-term archives are extremely rare – and therefore extremely valuable for studying natural climate change.”

In addition to the Innsbruck team, researchers from the USA, Great Britain and China were also involved in the study. The results were recently published in Nature Communications, and the study was financially supported by the Austrian Science Fund FWF, among others.

Publication: Controls on the southwest USA hydroclimate over the last six glacial-interglacial cycles. Kathleen A. Wendt, Stacy Carolin, Christo Buizert, Simon D. Steidle, R. Lawrence Edwards, Gina E. Moseley, Yuri Dublyansky, Hai Cheng, Chengfei He, Mellissa S. C. Warner & Christoph Spötl. Nature Communications 2025. DOI: 10.1038/s41467-025-64963-1

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