Abstract
Earth’s two remaining ice sheets, also called continental glaciers, are more active geochemists than we previously knew, according to a new study. Researchers led by Jon Hawkings, a biogeochemist at Florida State University and the German Research Center for Geosciences, measured the abundance of 17 trace elements in samples of meltwater from the Greenland Ice Sheet and a lake beneath the Antarctic Ice Sheet. They found that these water samples are more enriched in important micronutrients such as iron compared with rivers and the surrounding ocean ( Proc. Natl. Acad. Sci. U.S.A. 2020, DOI: 10.1073/pnas.2014378117 ). The trace elements can be found fully dissolved or suspended as nanoparticles, and they likely come from the bedrock beneath the frozen giants. That’s because ice sheets are “natural bulldozers” that pulverize landscapes as they move, and water trapped in subglacial lakes can liberate minerals from the surrounding rock, Hawkings says. “We didn’t have
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