New research led by the University of Massachusetts Amherst definitively resolves a long-standing discrepancy in the geologic record that pitted studies of marine ice-sheet behavior against those that reconstructed past conditions on land. The research, published recently in the journal Geology, and funded by the National Science Foundation and the National Environment Research Council, lends additional weight to evidence that the Antarctic Ice Sheet is sensitive to small changes in CO2 levels and that, in the past, large portions of the ice sheet could have disappeared under CO2 levels similar to today.
There has been a decades-long debate amongst scientists who study the history of the Antarctic Ice Sheet, and it revolves around the discrepancy between marine data from the Ross Sea and data collected in the McMurdo Dry Valleys, an ice-free mountainous coastal region adjacent to the Ross Sea. In one corner stands marine records from the seafloor that have shown that the Antarctic Ice Sheet has repeatedly shrunk to a smaller-than-modern size across the last 10 million years, and that the ice-covered Ross Sea was periodically open ocean. This suggests that the Antarctic Ice Sheet is sensitive to relatively small CO2 and temperature fluctuations and receded during past warm periods.
In the other corner stands terrestrial studies of ancient and well-preserved landforms in the McMurdo Dry Valleys that reveal that cold-desert conditions on land were maintained across the same ten-million-year time period, which has led some researchers to conclude that a stable Antarctic Ice Sheet has persisted across multiple past warm periods, and therefore may be less susceptible to climate warming than the marine data suggests.
Read more at University of Massachusetts Amherst
Image: Anna Ruth Halberstadt conducting field research in Antarctica’s McMurdo Dry Valleys. (Credit: UMass Amherst)