Scientists Discover Large Fan-Shaped Geological Structure Buried Under East Antarctica

On June 4, 2026, a team of geophysicists announced they had identified something hiding in plain sight beneath the East Antarctic Ice Sheet: a massive fan-shaped system of subglacial basins, stretching across a significant portion of the continent, formed by tectonic forces that pulled the Earth's crust apart from a single pivot point near the South Pole. The structure, dubbed the East Antarctic Fan-shaped Basin Province (EAFBP), was published in Nature Geoscience and represents a unifying framework for features that had been individually studied for decades but never recognized as parts of a single geological system [1][2].

What They Found

The EAFBP encompasses some of the most prominent subglacial features on the continent: the Wilkes Subglacial Basin, the Aurora Subglacial Basin, and the basin containing Lake Vostok — Earth's largest known subglacial lake [1][3]. These are not small features. The Wilkes Basin alone stretches roughly 1,400 to 1,600 kilometers in length and up to 600 kilometers in width, covering approximately 400,000 square kilometers [4]. The Aurora Basin is even larger, estimated at around 750,000 square kilometers, with bedrock sitting an average of 1.25 kilometers below present-day sea level [5]. Together with adjacent basins, the fan-shaped province spans a semi-continental area radiating outward from a focal point near the South Pole, all buried under ice exceeding three kilometers thick in places [1][2][6].

The research team, led by Dr. Egidio Armadillo of the University of Genoa and including Dr. Guy Paxman of Durham University, describes the structure as potentially "one of the largest examples of rotational extension ever seen in continental crust" [3][6]. Their key insight was not the discovery of any single basin — each had been mapped before — but rather the recognition that these basins form a coherent, interconnected system with a common tectonic origin.

How They Saw It

The discovery did not rely on a single survey or instrument. Instead, the researchers integrated multiple existing datasets: subglacial topography measurements from ice-penetrating radar, gravity and magnetic anomaly maps, seismic reflection profiles, and crustal and lithospheric models [1][2][3]. Dr. Paxman's contribution included calculating the "rebounded topography" of East Antarctica — what the land surface would look like if the weight of the ice sheet were removed, accounting for roughly one kilometer of crustal uplift [3][6].

This raises a question about whether the finding reflects genuinely new science or the reanalysis of existing data. The individual datasets have been available for years — some for decades. Airborne radar surveys of subglacial topography date back to the 1970s, and comprehensive compilations like Bedmap2 (2013) and Bedmap3 (2025) have progressively improved resolution [7]. The answer appears to be that the data existed but had not been synthesized through the lens of rotational extension. The researchers applied a tectonic model to connect observations that others had treated as separate features.

Source: OpenAlex

Data as of Jan 1, 2026CSV

Research into Antarctic subglacial topography has grown substantially, with over 4,400 papers published since 2011 according to OpenAlex data, peaking at 420 publications in 2023. The field has accumulated a large body of observations, but integrative tectonic interpretations — connecting individual features into continental-scale frameworks — remain relatively rare.

The Rotational Extension Model

The formation mechanism the team proposes is distributed rotational extension, a process in which continental crust gradually stretches outward from a central pivot point. The researchers compare it to a hand: the base of the thumb serves as the fixed point, while the fingers spread apart, creating triangular gaps between them [1][3]. Those triangular gaps correspond to the V-shaped subglacial basins that compose the fan.

The process is analogous to the opening of a folding fan — hence the name — and the team argues it occurred before and during the breakup of the Gondwana supercontinent, the ancient landmass that included what is now Antarctica, Australia, India, Africa, and South America [1][2]. Multiple tectonic phases likely contributed, linked both to Gondwana's internal evolution and to the later separation of Antarctica from Australia, which began around 45 million years ago [3][6].

This interpretation carries significant implications. If confirmed, the rotational extension model unites previously disparate observations — from the geometry of subglacial basins to the uplift of the Gamburtsev and Transantarctic Mountains — into a single tectonic narrative [8]. It would also represent one of the largest documented examples of this type of crustal deformation, which has been observed at smaller scales in places like the Gulf of California and the Aegean Sea, but never at a continental scale.

Competing Hypotheses and Outstanding Questions

The researchers acknowledge that important questions remain open, particularly "the precise age of the structure and the geodynamic mechanisms that generated it" [3]. While the rotational extension model is the central hypothesis of the paper, alternative explanations for individual basins have been discussed in the literature. The Wilkes Basin, for instance, has been linked to a hypothesized impact crater — the Wilkes Land crater — though this remains controversial and unconfirmed [4]. Volcanic activity and other forms of tectonic rifting have also been proposed for specific sub-features.

The skeptical case centers on data quality. Mapping subglacial topography through kilometers of ice is inherently uncertain. Radar flight lines can be spaced tens of kilometers apart in remote interior regions, and the gaps between them are filled using interpolation methods — kriging, spline fitting, or mass-conservation algorithms [7][9]. These approaches produce surfaces that can be "unrealistically smooth" and may not accurately represent features like narrow troughs or small ridges [9]. Bedmap3 and BedMachine Antarctica have improved resolution, but uncertainties of hundreds of meters persist in the ice sheet interior [7][9].

Whether the fan-shaped pattern could be an artifact of how sparse data was interpolated, rather than a reflection of true bedrock geometry, is a legitimate question. However, the researchers' use of multiple independent datasets — gravity, magnetics, and seismics in addition to radar-derived topography — provides cross-validation that pure interpolation artifacts would be unlikely to reproduce consistently across all data types.

Why It Matters: Ice Sheet Stability and Sea Level

The shape of the bedrock beneath an ice sheet is not merely of geological interest. It directly controls how ice flows, where subglacial water collects, and how vulnerable the ice sheet is to warming oceans and rising air temperatures.

The basins composing the EAFBP sit well below sea level. The Aurora Basin's floor averages 1.25 kilometers below sea level [5]. This is significant because ice grounded below sea level on a bed that deepens inland is susceptible to a process called marine ice sheet instability (MISI): once the grounding line — the boundary where ice lifts off the bedrock and begins floating — retreats into deeper terrain, increased ice discharge can trigger further retreat in a self-reinforcing cycle [10][11].

Source: Nature (2022), ASOC

Data as of Jun 4, 2026CSV

The stakes are enormous. The entire East Antarctic Ice Sheet contains enough ice to raise global sea levels by approximately 53.3 meters [10]. While the full ice sheet is not at imminent risk of collapse, individual basins within the EAFBP hold significant volumes. The Aurora Basin alone could contribute roughly 5.1 meters of sea-level rise, while the Wilkes Basin holds about 3 meters' worth [5][10]. The Totten Glacier system, which drains part of the EAFBP, contains as much ice as the entire West Antarctic Ice Sheet — approximately 3.5 meters of sea-level equivalent [10][12].

Current projections suggest the combined Antarctic Ice Sheet will contribute between 3 and 34 centimeters to sea-level rise by 2100, with a median around 11–12 centimeters [10][13]. Most models assume the East Antarctic Ice Sheet will remain broadly stable through this century, with increased snowfall partly offsetting dynamic losses. But these models depend on bedrock topography as a key input. If the EAFBP reveals that sub-basins are more deeply interconnected than previously modeled — potentially allowing warm ocean water to penetrate further inland through connected troughs — ice loss projections could shift upward.

The researchers note that the bedrock structure "continues to influence ice flow today, controlling the distribution of subglacial basins and lakes," and "could potentially affect the stability of parts of the Antarctic Ice Sheet that are particularly sensitive to climate change" [1][3]. Major outlet glaciers — including Totten, Denman, Byrd, Beardmore, and David — align with structural features of the EAFBP, suggesting that "structural geology fundamentally controls glacial drainage patterns" [8].

Lessons from Past Warm Periods

The Pliocene epoch, roughly 5.3 to 2.6 million years ago, offers the closest geological analog to projected end-of-century temperatures. During Pliocene warm intervals, global temperatures were comparable to those forecast under current emissions trajectories, and atmospheric CO₂ concentrations were similar to today's levels [14].

Marine sediment records show that the East Antarctic Ice Sheet was far more dynamic during these periods than its reputation for stability would suggest. Evidence indicates the ice sheet retreated hundreds of kilometers inland in the Wilkes Basin region during Pliocene warmth, with subglacially deformed sediments recording repeated advance and retreat of the grounding line [14][15]. A 2023 study also documented an ancient river landscape preserved beneath the East Antarctic ice — evidence of a time when the region was ice-free, with fluvial systems carving the terrain that now sits under kilometers of frozen water [16].

If the EAFBP's basins were shaped by tectonic forces that pre-date glaciation, and those same basins facilitated ice sheet retreat during past warm periods, the implication is concerning: the geological architecture that enabled Pliocene retreat still exists, and the climate forcing is now moving in that direction again.

Who Funds This, and Who Controls Access

The study was supported by the Italian National Antarctic Research Programme [3][6]. Italy is one of 29 consultative parties to the Antarctic Treaty, the 1959 agreement that designates Antarctica as a scientific preserve and bans military activity, mineral extraction, and nuclear testing [17][18].

Seven nations — Australia, New Zealand, the United Kingdom, France, Norway, Chile, and Argentina — maintain territorial claims over Antarctic territory, some of them overlapping. The treaty freezes these claims: no nation can expand existing claims or assert new ones while the agreement is in force [17][18]. The EAFBP straddles areas claimed by Australia (the Australian Antarctic Territory, which covers roughly 42 percent of the continent) and includes regions near the South Pole where claims converge.

For scientific research, the treaty guarantees freedom of investigation and free exchange of data [17]. But follow-up work on the EAFBP — particularly if it involved deep drilling into the bedrock — would enter more complex jurisdictional territory. The 1991 Madrid Protocol prohibits mineral resource activities not tied to scientific research [17]. While deep coring for geological samples would qualify as science, the distinction between scientific drilling and resource prospecting has become politically charged, particularly after reports in 2026 that Russian survey vessels may have been conducting seabed assessments in Antarctic waters under the guise of research [19].

The Long Road to Physical Samples

Confirming the tectonic origin of the EAFBP will ultimately require physical access to the bedrock — and that is among the most difficult undertakings in Earth science.

The precedent is sobering. The WAIS Divide ice core project, which drilled to 3,405 meters in the center of West Antarctica, operated from 2006 to 2013 — seven years of active drilling — and stopped 50 meters short of bedrock to avoid contaminating a potential subglacial water layer [20]. Accessing Lake Vostok, which sits beneath 3,769 meters of ice within the EAFBP itself, took Russian scientists two decades, from the start of drilling in 1990 to initial penetration in 2012, beset by funding shortages, equipment failures, and environmental concerns [21].

A dedicated campaign to core through the EAFBP's bedrock would likely require a decade or more of planning and execution, with costs in the tens of millions of dollars. The UK's attempt to access Lake Ellsworth in 2012–2013 using clean hot-water drilling technology failed due to technical problems [21]. The US successfully reached the much shallower Lake Whillans in the same season, but that lake sits under only about 800 meters of ice — a fraction of the depths involved in the EAFBP [21].

Alternative approaches — seismic surveys, targeted gravity measurements, or magnetotelluric profiling — could provide more detail about the structure's geology without the cost and complexity of drilling. But they cannot deliver the direct rock samples needed to determine the age, composition, and formation history of the basins with certainty.

What Comes Next

The immediate scientific agenda involves testing the rotational extension model against additional data. Higher-resolution aerogeophysical surveys, particularly in poorly mapped interior regions, could sharpen the picture of basin geometry and test whether the fan-shaped pattern holds up under finer scrutiny. Improved crustal thickness models from seismic experiments could independently constrain whether the thinning pattern is consistent with extension from a single pivot point.

For ice sheet modelers, the EAFBP presents both a challenge and an opportunity: a more detailed and geologically coherent map of the bed could improve projections but also introduce new sources of uncertainty, particularly around sub-basin connectivity and basal water routing.

The broader significance may be the simplest to state. For decades, the individual basins of East Antarctica were treated as separate features with separate histories. This study argues they are parts of one structure, shaped by one process, with shared implications for how the ice sheet above them behaves. If that framework holds, it changes how scientists think about the geological foundation of the world's largest ice sheet — and, by extension, how much of that ice is at risk.