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Alpine Ice Core Reveals 12,000 Years of Climate Clues as Antarctic Cores Land in Europe

The study charts past aerosol, temperature and vegetation shifts in the Alps to improve climate forecasts with Antarctic cores poised to extend records back 1.5 million years.

© British Antarctic Survey
Image
An ice sample on the melter during continuous ice core chemical analyses in the lab (credit: Sylvain Masclin).
The ice core storage cave at the research station in Antarctica

Overview

  • Analysis of a 40-meter Mont Blanc Dôme du Goûter core published in PNAS Nexus confirms the oldest intact Alpine ice record spanning the last glacial maximum through the Holocene.
  • Ice-age dust levels in the Alpine core are eight times higher than in the Holocene and sea-salt proxies indicate stronger westerly winds over Europe during colder periods.
  • Phosphorus concentrations trace 12,000 years of vegetation change, showing forest expansion in the early Holocene followed by declines linked to agriculture and rising industrial emissions.
  • A 2,800-meter Little Dome C core has arrived at British Antarctic Survey labs for high-resolution analysis aimed at reconstructing up to 1.5 million years of temperature, greenhouse gas and marine productivity data.
  • Belgian teams’ shallow blue-ice samples—potentially dating to 100,000 years ago—will guide future deep drilling efforts in Antarctica to access multi-million-year climate archives.