The influence of glaciers on iron cycling and export across a latitudinal gradient in Chilean Patagonian

Jon Hawkings1, Helena VALERIE Pryer2, Tim M Conway3, Elizabeth Shoenfelt4, Matthias Sieber5, Alexander Beaton6, Rodrigo Torres7, Giovanni Daneri7, Robert M Sherrell8, Vincent Roccanova9, Kaixuan Bu9, Katharine R Hendry10,11, Anne Kellerman12, Matthew Marshall13, Verena Häussermann14 and Jemma Wadham15, (1)University of Pennsylvania, Department of Earth and Environmental Science, Philadelphia, United States, (2)University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom, (3)University of South Florida, College of Marine Science, St. Petersburg, United States, (4)MIT, Earth, Atmospheric and Planetary Sciences, Cambridge, United States, (5)University of South Florida, College of Marine Science, St. Petersburg, FL, United States, (6)National Oceanography Centre, Ocean Technology and Engineering Group, Southampton, United Kingdom, (7)Centro de Investigación en Ecosistemas de la Patagonia, Coyhaique, Chile, (8)Rutgers University, Departments of Marine and Coastal Sciences and Earth and Planetary Sciences, New Brunswick, NJ, United States, (9)Rutgers University, Department of Marine and Coastal Sciences, New Brunswick, NJ, United States, (10)University of Bristol, School of Earth Sciences, Bristol, United Kingdom, (11)British Antarctic Survey, Cambridge, United Kingdom, (12)Florida State University, Earth, Ocean and Atmospheric Science, Tallahassee, FL, United States, (13)University of Bristol, School of Geographical Sciences, Bristol, United Kingdom, (14)Austral University of Chile, Institute of Marine and Limnological Sciences, Valdivia, Chile, (15)University of Bristol, Bristol Glaciology Centre, Bristol, United Kingdom