Antarctica’s irregular heartbeat shows signs of rapid melting
Geoscientists led by Universities of Leicester and Southampton create new climate record for early Antarctic ice ages
University of Leicester
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Photographs taken by the researchers during a subsequent expedition to the Antarctic aboard the same research vessel.
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Periods of sudden melting in the Antarctic ice sheet have been unearthed in a new climate record from over 20 million years ago by geoscientists led by the University of Leicester and the University of Southampton.
Published in the journal Nature Communications, the new study reveals how sensitive our planet’s early ice ages were to the effect of the Earth’s eccentric orbit around the Sun, suggesting the Antarctic ice sheet is less stable than has been assumed.
It also provides a glimpse of how the Antarctic may behave in a world without the Greenland Ice Sheet, which will melt if emissions continue unabated.
Records show that the Antarctic ice sheet has varied in size throughout its history. These variations in size occur regularly, just like a heartbeat. Existing records from different places in the ocean show different ‘rhythms’ in the heartbeat of early Antarctic ice ages. This should not be possible because the imprint of the waxing and waning of the Antarctic ice sheet on the climate record should be identical everywhere in the ocean, just as it should not be possible that your leg has a different pulse rate than your arm.
These heartbeat rhythms are caused by the shape of Earth’s orbit around the Sun over the course of hundreds of thousands to millions of years. On a more eccentric orbit, the Earth’s distance from the Sun will vary more throughout the year, exposing it to more heat when it is close in, and less when it is further away. The increasing heat changes Earth’s climate system, causing the ice sheet to melt, sometimes rapidly. When the Earth’s orbit is more circular, the ice sheet is more stable and less melting occurs.
This new study, funded by UK Research and Innovation/Natural Environment Research Council and the German Science Foundation (DFG) examines the period between 28 and 20 million years ago, when Earth was warmer than today and only the Antarctic ice sheets existed. Using data obtained from geological cores recovered by an expedition of the Integrated Ocean Drilling Program (IODP), the research presents a new benchmark climate record to compare existing records to help scientists improve the accuracy of their climate models reconstructing past climate change. These insights into the past help them understand the impact of the melting of the Antarctic Ice Sheet in the future.
Lead author Dr Tim van Peer, from the University of Leicester School of Geography, Geology and the Environment, said: “From our research, we can see that the Antarctic ice sheet is more unstable than previously thought. We demonstrate how sensitive the geologically early Antarctic ice sheet was to changes in Earth’s orbit and axis.
“Past climate changes rapidly ended some of the early Antarctic ice ages and caused large amounts of melt. ‘Rapidly’ is on geological time scales, not as rapid as we can expect to happen during modern climate change.
“We cannot assume that the modern-day Antarctic ice sheet is stable. If climate emissions continue unabated, we are on course to melt a large amount of the Antarctic ice sheet. We need to mitigate climate change by reducing our emissions. This is the only way to not cross tipping points in the stability of the Antarctic ice sheet.”
The research analysed samples from geological cores obtained from the northwest Atlantic Ocean as part of an IODP expedition in 2012. Microorganisms from these cores record the chemistry of the ocean in the form of oxygen isotopes in their shells. By measuring the oxygen isotope ratio, the scientists can work out if the ice sheet has grown or shrunk, and establish a timeline from the depth of that sample in the cores.
Professor Paul Wilson, Principal Investigator on the project at the University of Southampton, said: “It may be a surprising thing to learn that we take the pulse of the Antarctic ice sheet by doing some simple chemistry on pinhead-sized fossil shells from the deep sea floor on the other side of the world. But the really beautiful thing is that we can do it back through the geological record over tens of millions of years. Earth science is about time travel into the past and we are always learning lessons to help us understand our future"
IODP is a publicly-funded international marine research program supported by 21 countries, which explores Earth's history and dynamics recorded in seafloor sediments and rocks, and monitors sub-seafloor environments. Through multiple platforms – a feature unique to IODP – scientists sample the deep biosphere and sub-seafloor ocean, environmental change, processes and effects, and solid Earth cycles and dynamics. This specific research uses samples collected during Expedition 342 and has taken years of work from the combined efforts of a multinational partnership (mainly UK and Germany).
The University of Leicester has been involved in IODP since the 1980s and participated in dozens of expeditions around the world. Over the last year, University of Leicester scientists participated in IODP Expedition 389 ‘Hawai’ian Drowned Reefs’ and Expedition 405 ‘Tracking Tsunamigenic Slip Across the Japan Trench (JTRACK)’.
Photographs taken by the researchers during a subsequent expedition to the Antarctic aboard the same research vessel.
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About the University of Leicester
The University of Leicester is the Daily Mail University of the Year 2025 and shortlisted for University of the Year for both the Times Higher Education Awards 2024 and the Times and Sunday Times Good University Guide 2025.
The University is led by discovery and innovation – an international centre for excellence renowned for research, teaching and broadening access to higher education. It is among the Top 30 universities in the Times Higher Education (THE)’s Research Excellence Framework (REF) 2021 rankings with 89% of research assessed as world-leading or internationally excellent, with wide-ranging impacts on society, health, culture, and the environment. In 2023, the University received an overall Gold in the Teaching Excellence Framework (TEF) 2023, making it one of a small number of institutions nationally to achieve TEF Gold alongside a top 30 REF performance. The University is home to more than 20,000 students and approximately 4,000 staff.
Journal
Nature Communications
Article Title
Eccentricity pacing and rapid termination of the early Antarctic ice ages
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