Decreased atmospheric iron solubility during the Last Glacial Maximum in the high latitude Southern Hemisphere
Decreased atmospheric iron solubility during the Last Glacial Maximum in the high latitude Southern Hemisphere
Aaron Chesler1, Bess G Koffman2, Dominic Winski3,4, Karl J Kreutz3, Erich C Osterberg5, Mark Wells6, Michael Handley1, David Ferris7, Zayta Renay Thundercloud5, Jihong Cole-Dai8, Aaron E Putnam9,10 and Natalie Harmon9, (1)University of Maine, Climate Change Institute, Orono, ME, United States, (2)Colby College, Department of Geology, Waterville, United States, (3)University of Maine, School of Earth and Climate Sciences, Orono, United States, (4)University of Maine, Climate Change Institute and School of Earth and Climate Sciences, Orono, United States, (5)Dartmouth College, Department of Earth Sciences, Hanover, NH, United States, (6)University of Maine, School of Marine Sciences, Orono, United States, (7)Dartmouth College, Hanover, United States, (8)South Dakota State University, Department of Chemistry and Biochemistry, Brookings, SD, United States, (9)University of Maine, School of Earth and Climate Sciences, Orono, ME, United States, (10)University of Maine, Climate Change Institute, Orono, United States