In the vast, icy expanse of Antarctica, a surprising discovery is challenging our understanding of life in extreme environments. Blue ice areas, once thought to be barren stretches of ice sheet, are now revealed as thriving hotspots of essential nutrients, diverse microbial activity and complex hydrology.
By: Aga Nowak, Elisabeth Isaksson, Stephen Hudson, Håkon Sandven, Geir Moholdt, Anne Urset, Øyvind Sunde and Synnøve Elvevold // Norwegian Polar Institute
Andrew Hodson // University Centre in Svalbard
Børge Hamre // University of Bergen
Arwyn Edwards and Sara ME Rassner // Aberystwyth University, Wales
David Pearce // Northumbria University, England

Imagine standing at the Norwegian Antarctic Station Troll in Dronning Maud Land. You are surrounded by a seemingly lifeless landscape of wind-polished blue ice. Yet beneath your feet, a hidden world teems with life and water.
During the austral summer of 2019/2020, researchers from the Norwegian Polar Institute and the University Centre in Svalbard embarked on an expedition that would overturn long-held assumptions about these blue ice areas (BIAs).
In just 62 km2 of the Jutulsessen blue ice they identified over 856 000 micro-habitats called cryoconite holes. That astounding number covered 14% of the BIA. These cryoconite holes, water-filled depressions on the ice surface, form when dark debris absorbs solar radiation, creating localised melting. Cold Antarctic temperatures make the water at the top of the hole freeze and form a protective lid that then allows water inside to remain liquid.
A frozen desert comes to life
What makes cryoconite holes remarkable is their role as oases for diverse microbial life in this frozen desert. What is more, thanks to biogeochemical processes occurring in the holes, they are also powerplants for nutrient and carbon production at a scale that has never been imagined.
Cryoconite holes in Jutulsessen are not just isolated pockets of water, microbes and nutrients. They’re interconnected by subsurface drainage networks, allowing transport of that water, nutrients, and microorganisms across the ice sheet.
The team also discovered that cryoconite holes form differently in BIAs than in other regions. Unlike on glaciers, their formation and chemical signature on the ice sheet are controlled by ice flow and bedrock geology along the ice movement.

Did you know?
Blue ice areas (highlighted in red) cover 235 000 km2 of the Antarctic fringe, an area larger than the United Kingdom.
Blue ice areas are also known as important sites for meteorite collection, containing about 25% of the meteorites found worldwide.

Nature’s ice-cold greenhouse
In addition to the holes themselves, unique physical properties of the blue ice enable creation of a natural greenhouse effect. Here, sunlight can penetrate deep into the ice, causing internal melting even at 10 meters below the surface, transforming ice into hidden bodies of water.
The hydrological connectivity in BIAs has important implications for our understanding of ice sheet hydrology and its potential response to climate change. As warming continues, these networks can play an increasingly significant role in ice sheet dynamics and the transport of nutrients to downstream ecosystems.
As climate change continues to reshape polar regions, understanding these complex ecosystems becomes increasingly crucial. The BIOICE project, funded by the Research Council of Norway, is at the forefront of this vital research, shedding light on the hidden life thriving in Earth’s coldest environment.
Beyond Earth
The discovery of thriving near-surface microbial communities in such extreme conditions should also catch the attention of astrobiologists investigating icy moons with hidden oceans—moons like Jupiter’s Europa and Enceladus.
BIOICE’s findings not only reshape our understanding of Antarctic ecosystems, but open new avenues for research in polar science and our understanding of limits for life. As we continue to explore these unique environments, who knows what other surprises will be revealed?
Further reading
Nowak A, Isaksson E, Sunde Ø et al (2024) Antarctic Blue Ice Areas are hydrologically active, nutrient rich and contain microbially diverse cryoconite holes. Commun Earth Environ 5: 345.