Radioactive and Stable Paleoatmospheric Methane Isotopes across the Last Deglaciation and Early Holocene from Taylor Glacier, Antarctica
Michael Dyonisius1, Vasilii V Petrenko2, Andrew Wyatt Smith3, Benjamin Hmiel4, Isaac J Vimont5, Quan Hua6, Bin Yang7, James A Menking8, Sarah Shackleton9, Rachael Rhodes8,10, Daniel Baggenstos11, Thomas K Bauska8,12, Michael Bock13, Jonas Beck13, Barbara Seth13, Christina M Harth9, Ross Beaudette9, Jochen Schmitt13, Edward J Brook14, Ray F Weiss9, Hubertus Fischer13 and Jeffrey P Severinghaus15, (1)University of Colorado Boulder, Institute of Arctic and Alpine Research, Boulder, United States, (2)University of Rochester, Earth and Environmental Sciences, Rochester, NY, United States, (3)RSMAS, Ocean Sciences, Miami, FL, United States, (4)University of Rochester, Department of Earth and Environmental Sciences, Rochester, United States, (5)Institute of Arctic and Alpine Research, University of Colorado, Boulder, United States, (6)Australian Nuclear Science and Technology Organisation (ANSTO), Kirrawee DC, NSW, Australia, (7)Centre for Accelerator Science, Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, Australia, (8)Oregon State University, Corvallis, OR, United States, (9)Scripps Institution of Oceanography, La Jolla, CA, United States, (10)University of Cambridge, Department of Earth Science, Cambridge, United Kingdom, (11)Climate and Environmental Physics and Oeschger Center for Climate Research, University of Bern, Bern, Switzerland, (12)University of Cambridge, Godwin Laboratory for Palaeoclimate Research, Cambridge, United Kingdom, (13)University of Bern, Physics Institute, Bern, Switzerland, (14)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, (15)Scripps Institution of Oceanography, La Jolla, United States
