Grounding-Zone Retreat and Marine Sediment Transport from Holocene to Present along Thwaites Glacier in the Eastern Amundsen Sea
Grounding-Zone Retreat and Marine Sediment Transport from Holocene to Present along Thwaites Glacier in the Eastern Amundsen Sea
Rachel Warren Clark1, Julia Wellner1, Claus-Dieter Hillenbrand2, Rebecca L Totten3, Asmara Lehrmann4, Victoria Fitzgerald4, James A Smith2, Laura Barnett5, Michael Michael Comas1, Georgina Garcia-Barrera6, Mary Catherine Hambrick6, Becky Hopkins7, James Kirkham8, Allison Lepp9, James Marschalek10, Elaine Mawbey2, Santiago Munevar Garcia11, John B Anderson12, Julia Villafranca6, Alastair GC Graham13, Kelly Hogan2, Robert D Larter2, Frank Oliver Nitsche14, Lauren Miller Simkins11 and Lukas Wacker15, (1)University of Houston, Houston, TX, United States, (2)NERC British Antarctic Survey, Cambridge, United Kingdom, (3)University of Alabama, Geological Sciences, Tuscaloosa, AL, United States, (4)University of Alabama, Geological Sciences, Tuscaloosa, United States, (5)Woods Hole Oceanographic Institution, Woods Hole, United States, (6)University of Houston, Houston, United States, (7)University of Southampton, Southampton, United Kingdom, (8)University of Cambridge, Cambridge, United Kingdom, (9)University of Virginia, Department of Environmental Sciences, Charlottesville, VA, United States, (10)Imperial College London, London, United Kingdom, (11)University of Virginia, Department of Environmental Sciences, Charlottesville, United States, (12)Rice University, Department of Earth, Environmental and Planetary Sciences, Houston, United States, (13)University of South Florida St. Petersburg, St Petersburg, FL, United States, (14)Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, United States, (15)ETH Swiss Federal Institute of Technology Zurich, Laboratory for Ion Beam Physics, Department of Physics, Zurich, Switzerland