128,000-year-old Tibetan ice extends the climate record by 100,000 years
Scientists from Ohio State University recovered ice cores from the Tibetan plateau dating to at least 128,000 years ago — extending the regional glacial record by more than 100,000 years and capturing Earth's climate across two complete glacial cycles, including a previous warm period comparable to the present.
- Ice survived the last interglacial warm period, challenging models predicting full deglaciation on the plateau
- Isotopic record allows direct comparison of a previous warm period with present-day warming rates
- Discovery at high-altitude sites that are melting fastest makes the recovery an urgent scientific priority