Fossils of plants, fungi, and insect parts preserved beneath the Greenland ice sheet have reinforced evidence that areas now covered by thick ice were once devoid of this cover in the geologically recent past.
In some of the samples studied at Camp Century, in the northwest of the island, dating indicated exposure to sunlight for approximately… 416 years.
The samples, re-examined by teams of US universities, from Denmark and other countries, preserved Traces of tundra in an unusual state of preservation..
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According to the researchers, this body of evidence suggests that not only peripheral areas, but also broader sectors of the ice sheet may have been exposed in relatively recent intervals of Greenland’s climate history.
Fossils beneath the Greenland ice
Two studies form the basis of this scientific debate.
The first, published in 2021, analyzed frozen sediments removed in 1966 under almost 1,4 kilometers of ice em Camp Century.
In this material, researchers identified branches, leaves, moss, and other plant remains preserved at the bottom of the core.
The second study, published in 2024, examined just a few centimeters of soil from the bottom of the ice core. GISP2, drilled in 1993 in the center of Greenland.
In this analysis, the following were described: willow wood, fungi, an Arctic poppy seed, and insect parts..
According to the authors, the findings indicate that not only the edge, but also more internal areas of the ice sheet have already become free of this layer.
This point altered the weight of the available evidence.
Until then, the hypothesis that Greenland had lost ice extensively in relatively recent periods was largely based on geochemical models and signals.
With the identification of preserved macrofossilsStudies have since presented direct evidence of exposed soil and vegetation in areas that now remain under a thick layer of ice.
Preservation of sediments at Camp Century
The preservation of materials is related to the environment in which they remained sealed.
In the case of Camp Century, the organic remains were frozen at the base of the core and protected from rapid decomposition processes.
This condition allowed delicate plant structures to remain recognizable under a microscope and, in some cases, visible to the naked eye.
When announcing the 2021 results, the University of Copenhagen stated that they were… The first macrofossils recovered from beneath the Greenland ice sheet, large enough to be observed without a microscope..
The data was highlighted by researchers as an indication of the material’s unusual preservation.
Another decisive element was the rediscovery of the samples.
The sediment drilled in 1966 had not been studied in depth at the time and passed through different storage facilities until it was rediscovered and re-evaluated using more recent techniques.
Therefore, a sample collected decades ago only gained scientific prominence after being subjected to new methods of analysis.
Dating the fossils and a new chronology
Initial analysis already indicated that the ice had receded at some point within the last million years.
Then, a study published in the journal ScienceIn 2023, this estimate was refined.
With the use of luminescence datingThe team concluded that the top layer of subglacial sediment at Camp Century was last exposed to sunlight in 1988. 416 years, with a margin of error of 38 years.
The authors associated this interval with marine isotopic stage 11, a prolonged interglacial period.
At Camp Century, researchers describe signs of tundra with vegetationincluding mosses, lichens and, in some reconstructions, the possible presence of trees such as firs and pines.
In the center of the island, the material analyzed in 2024 was also interpreted as indicative of a green tundra landscape.
What do studies indicate about the Greenland ice sheet?
Studies converge on one aspect: the Greenland ice sheet may be more sensitive to climate change than some scientific literature previously suggested.
In 2021, the team that analyzed Camp Century concluded that the site had been ice-free at least once within the last million years.
Three years later, work with the GISP2 core added direct evidence that the central Greenland It also lost ice in the recent geological past.

This broadened the scope of scientific interpretation.
Previous interpretations, in some models, treated ice cover as a more stable structure over extended periods.
The new findings, according to the researchers, indicate that the history of the ice cap is more dynamic than previously estimated.
However, the studies do not, by themselves, define a timeframe for a possible widespread loss of ice in the future.
What the authors claim is that Greenland responded significantly to natural warming periods in the past.
For this reason, this type of evidence has been incorporated into the debate about future projections of the cryosphere and the level of Mar.
Impact on the climate debate and sea level
The relevance of these fossils is linked to Greenland’s role in the global climate system.
The research teams point out that the island’s ice sheet contains enough volume to raise sea levels by approximately… 7 meters, in case of near-complete melting.
In this context, the evidence that large areas have already been ice-free in the relatively recent past has come to be treated as important data for the revision of long-term climate scenarios.
At the same time, the material preserved under the ice also expanded knowledge about ancient ecosystems in the region.
Since subglacial samples of this type are rare, each fragment of seed, wood, or fungus helps to reconstruct not only moments of ice retreat, but also the environmental conditions that existed in Greenland before the ice sheet advanced.
These studies have therefore been used by researchers to understand the relationship between climate, ice cover, and landscape over geological time.
Scientific interest focuses both on the climatic history and on the records of life preserved beneath one of the largest ice masses on the planet.