The sediments themselves are an extraordinary scientific resource. In 1966, engineers drilling through the Greenland Ice Sheet at Camp Century accidentally recovered 3.44 meters of sediment from the ice-bed interface, material that then languished in freezer storage for decades before modern analytical techniques caught up with it. The core’s upper layers, dated by luminescence methods to approximately 416,000 plus or minus 38,000 years ago, correspond to Marine Isotope Stage 11, an interglacial period renowned among paleoclimate scientists for its unusual length and relative mildness. Deeper units in the core are far older, likely dating to the Pliocene or early Pleistocene, between roughly 1.4 and 3.2 million years ago, making the Camp Century archive one of the few terrestrial windows into Greenland’s climate deep past.

To reconstruct temperature, the researchers turned to branched glycerol dialkyl glycerol tetraethers, or brGDGTs, membrane lipids produced by bacteria that live in soils and lake sediments. The chemical structure of these compounds varies systematically with temperature, allowing scientists to use them as molecular thermometers. Chemical fingerprints in the Camp Century samples, including a branched-to-isoprenoid tetraether index above 0.97 and distributions closely matching those of modern high-latitude lakes, indicated that the lipids were produced primarily in aquatic settings rather than soils. This makes sense given the modern landscape of northwestern Greenland, where shallow lakes dot more than 80 percent of the ice-free terrain in some areas. The team applied two temperature calibrations developed specifically from Arctic lake datasets, propagating calibration errors and analytical uncertainty into their final estimates.

The temperature results were striking in their consistency. Across the MIS 11 sediments, inferred temperatures for the months above freezing ranged from about 4.4 to 6.7 degrees Celsius, with mean anomalies of 4.3 to 5.2 degrees above the elevation-corrected modern baseline. Even the older, deeper units told a similar story, with anomalies of roughly 4.1 to 4.5 degrees. Because the Camp Century bed sits at only about 530 meters above sea level today, the researchers carefully corrected for the fact that an ice-free landscape would sit higher, around 810 meters after the crust rebounded from the removed ice load, applying lapse rates of roughly minus 5 degrees Celsius per kilometer. All units, spanning millions of years, pointed to interglacial summers in northwestern Greenland that were consistently warmer than the late twentieth century but broadly similar to each other.

The water isotope evidence added a second, equally important dimension. The team measured the hydrogen isotope composition of plant waxes, specifically n-alkanoic acids, preserved in the sediments. Long-chain waxes from terrestrial plants record summer precipitation isotopes modified by evaporation in leaves, while mid-chain waxes from aquatic plants reflect lake water, which in open Arctic basins largely mirrors summer precipitation. By combining these precipitation isotope reconstructions with the independently derived temperatures, the researchers could subtract the effect of local condensation temperature and estimate the isotope composition of the atmospheric vapor itself. Summer vapor during MIS 11 was 22 plus or minus 18 per mil enriched in deuterium relative to modern values, a signal the authors interpret as a substantially greater contribution of moisture evaporated and transpired locally rather than transported from distant oceans.

This moisture story is physically intuitive. Today, only about 30 percent of summer moisture arriving near Pituffik, the nearest meteorological station, comes from nearby land and seas in the high-latitude Arctic; the remaining 70 percent travels from remote Atlantic and Pacific sources, arriving isotopically depleted after long distillation. During MIS 11, with the ice sheet margin more than 100 kilometers inland of the coast, a vast expanse of vegetated tundra replaced reflective ice. Reduced snow and ice cover and expanded plant biomass would have boosted summer evapotranspiration across Greenland and neighboring North America, flooding the regional atmosphere with isotopically heavy, locally sourced vapor. The deuterium enrichment recorded at Camp Century is far larger than the modest Holocene vapor anomaly observed at nearby Secret Lake, suggesting the ice-free footprint during MIS 11 exceeded anything the Holocene produced.

Placing Camp Century in context required a careful meta-analysis of published Greenland paleoclimate records, standardized to the same 1950 to 2000 baseline. Eight Holocene brGDGT records from southwestern Greenland showed warm-season anomalies of about 3 plus or minus 2 degrees, two to three degrees cooler than the Camp Century reconstruction, though the difference may partly reflect the northwestern site’s higher latitude. Chironomid-based July temperature reconstructions, which capture peak summer rather than the full above-freezing season, suggested Holocene anomalies near 7 degrees, while Last Interglacial estimates from northwestern Greenland reached nearly 10 degrees, clearly warmer than MIS 11. The comparison also highlighted a methodological subtlety: brGDGTs record the temperature of all months above freezing, a season that lengthens as climate warms, so their anomalies are inherently smaller than July-based proxies under identical forcing. Accounting for these seasonal biases, the authors conclude that MIS 11 summers in northwestern Greenland resembled, or slightly exceeded, peak Holocene warmth.

The ice sheet implications are where the study becomes genuinely unsettling. Marine sediment records and ice sheet modeling indicate that the southern dome of the Greenland Ice Sheet retreated dramatically during MIS 11, an interglacial whose warm phase lasted on the order of 30,000 years, far longer than the briefer but sometimes warmer stages 9 and 5, during which the ice sheet apparently persisted. The new Camp Century data show that northwestern Greenland experienced similarly moderate temperatures during MIS 11, yet the site was ice-free, something it never was even during the warmest Holocene millennia. Modeling work cited by the authors demonstrates that sustained moderate summer anomalies over roughly 16,000 years can produce substantial mass loss. The lesson is that duration matters as much as magnitude: a climate only modestly warmer than the Holocene, maintained for tens of millennia, was sufficient to push the ice sheet margin deep inland.

That lesson lands with force in the twenty-first century. Projections assessed by the Intergovernmental Panel on Climate Change suggest the Arctic will experience mean annual surface temperatures 3.0 to 10.6 degrees Celsius above the 1950 to 2000 baseline by 2100, a range whose lower bound already brackets the Camp Century MIS 11 reconstruction. Modern warming at high latitudes is concentrated in winter, which may moderate summer-season anomalies, but cloud and ice-albedo feedbacks in the latest climate models substantially increase the ice sheet’s sensitivity to any given amount of warming. Unlike MIS 11, today’s warming is being driven by greenhouse gas emissions on a timescale of centuries rather than orbital cycles, and it will not naturally subside on geological timescales unless emissions fall. The Camp Century sediments, preserved by accident beneath the ice and rescued from Cold War storage, thus deliver a message that is both ancient and urgently contemporary: to protect the Greenland Ice Sheet and the 7.4 meters of global sea level rise it holds in reserve, humanity must limit not only how hot summers become but how long the warmth endures.

Subject of Research: Reconstruction of summer temperature and moisture sources in northwestern Greenland during Marine Isotope Stage 11 using subglacial biomarkers from Camp Century

Article Title: Holocene-like summer climate during Marine Isotope Stage 11 in northwestern Greenland

Article References: Holocene-like summer climate during Marine Isotope Stage 11 in northwestern Greenland. (n.d.). https://doi.org/10.5194/cp-22-1757-2026

Image Credits: AI Generated

DOI: 10.5194/cp-22-1757-2026

Keywords: Greenland Ice Sheet, Camp Century, Marine Isotope Stage 11, biomarkers, brGDGTs, plant waxes, paleoclimate, sea level rise, interglacial, hydrogen isotopes, Arctic warming, subglacial sediments

The research team, led by Jebasinski and colleagues, meticulously analyzed marine sediment cores collected from key sites surrounding the Antarctic continent. These cores hold tiny chemical and physical clues etched into layers of sediment, essentially serving as a time capsule documenting ocean conditions across thousands of years. By measuring isotopic variations and sediment composition, the scientists reconstructed a detailed timeline revealing recurrent periods when the WAIS experienced significant retreat and thinning, coinciding with phases of increased ocean warming and changes in Southern Ocean circulation during MIS 11.

Marine Isotope Stage 11 is recognized as one of the most prolonged and warm interglacial periods in Earth’s recent history, with climatic conditions paralleling projections for current and future global warming scenarios. Understanding the behavior of polar ice sheets during such past warm intervals is critical because it enables scientists to anticipate how modern ice sheets might respond to ongoing anthropogenic climate forcing. The indication that WAIS destabilization was not a singular event, but rather repeated throughout MIS 11, suggests far greater dynamism in ice sheet response than previously appreciated.

The study’s findings challenge prevailing views which often consider ice sheet retreat during interglacial periods as a one-time or slow onset process. Instead, the evidence indicates that the WAIS was prone to multiple episodes of rapid ice loss and possible collapse over timescales of several thousand years, driven by complex interactions between atmospheric warming, oceanic temperature changes, and subsurface melting by warm circumpolar deep waters. The role of the Southern Ocean is thus emphasized as a critical driver in ice shelf disintegration and grounding line retreat.

One of the innovative aspects of the research is the integration of high-resolution isotopic analyses with advanced sedimentology techniques that allowed unprecedented temporal resolution. This fine-scale approach revealed fluctuations in ice sheet stability that were previously obscured by coarser data sets. Notably, peak erosion periods corresponded tightly with periods of enhanced Southern Ocean upwelling and increased heat transfer to ice shelf bases, accelerating ice melt from below.

By pinpointing these recurrent destabilization events within MIS 11, the study also provides valuable calibration points for ice sheet and climate models. Modelers can now incorporate this detailed paleo-archive data to refine simulations of ice sheet dynamics under warming conditions, potentially improving predictions regarding thresholds for irreversible ice loss. As modeling efforts advance towards simulating ice sheet behavior over millennial timescales, such paleo-evidences become indispensable.

Furthermore, this research contributes to understanding the contribution of the Antarctic ice sheet to past sea level highs. MIS 11 is associated with global sea levels several meters above present, and repeated WAIS retreat would have been a significant mechanism contributing to these elevations. This challenges assumptions that Greenland was the dominant ice mass responsible for MIS 11 sea level peaks and underscores Antarctica’s crucial role in modulating ancient sea level fluctuations.

The implications of recurrent WAIS vulnerability extend beyond paleoclimatology. Today, the West Antarctic Ice Sheet remains one of the most precarious ice masses on Earth due to its grounding below sea level and exposure to warm ocean currents. This new evidence of past repeated collapses reinforces assessments that WAIS may rapidly respond to ongoing ocean warming, which is projected to accelerate in coming decades. Such rapid ice loss would have profound consequences for global sea levels, threatening coastal communities worldwide.

The study’s insights also highlight the need for continued and expanded Southern Ocean observations and monitoring. Understanding the complex feedbacks between ocean circulation, warm water intrusions, and ice shelf stability is critical to anticipating future changes. Coupled with robust ice sheet and climate modeling, data like those presented by Jebasinski et al. form a foundational basis for climate policy that accounts for ice sheet feedbacks in sea level projections.

The authors emphasize that while MIS 11’s climate was naturally driven by orbital variations in Earth’s orbit, the similarities to present anthropogenic warming are striking, especially regarding temperature magnitude and duration. This parallel offers a natural laboratory for studying long-term ice sheet responses absent confounding human influences. Yet, it also serves as a warning that the timeframes for ice sheet instability and associated sea level rise might be shorter than anticipated.

Moreover, the analytical techniques developed in this study pave the way for applying similar approaches to other marine sediment records globally. By expanding the geographical coverage, scientists may uncover additional episodes of ice sheet dynamics during other past warm intervals, helping to piece together a more complete history of polar ice sensitivity across glacial cycles.

This landmark study pushes the boundaries of our knowledge on Antarctic ice sheet history by revealing that the West Antarctic Ice Sheet was not static during one of the warmest interglacials but rather underwent episodic and likely rapid destabilizations. It underscores the urgency of understanding how today’s warming oceans impact ice sheet stability and the global climate system, reminding us that Antarctica’s glaciers have long played a pivotal role in shaping Earth’s environment and will continue to do so in a warming future.

Looking forward, the researchers call for deeper interdisciplinary studies combining paleoclimate data, ice sheet modeling, and oceanography to develop comprehensive frameworks for predicting ice sheet behavior under climate change. As sea levels rise inexorably, these insights are not merely academic; they form the foundation for adaptation measures critical to preserving coastal populations and ecosystems worldwide.

This new research opens a fascinating window into the prehistoric past of Antarctica’s ice sheets and, through this lens, provides vital clues for navigating humanity’s climate future. The story of ice, ocean, and climate interaction revealed in these Southern Ocean sediment records is a potent reminder of the complex vulnerabilities our planet faces as it warms.

Subject of Research: West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11

Article Title: Southern Ocean evidence for recurring West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11

Article References:
Jebasinski, L., Frick, D.A., Kapuge, A.K.I.U. et al. Southern Ocean evidence for recurring West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11. Nat Commun 16, 9138 (2025). https://doi.org/10.1038/s41467-025-65002-9

Image Credits: AI Generated