Multi-core, multi-constraint chronostratigraphic framework over past 50,000 years places high-resolution Gulf of Alaska ocean-ice-sediment history into a global framework
Alan C Mix1, Maureen H Walczak2, Hirofumi Asahi3, Christina L Belanger4, Ellen A Cowan5, Jianghui Du6, Stewart Fallon7, L Keith Fifield8, Tim Hobern8, John M Jaeger9, Britta J.L. Jensen10, Jennifer L McKay11, June Padman12, Andrew Ross11, Sharon Sharon13, Joseph Stephen Stoner12 and Sarah Zellers14, (1)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, (2)Oregon State University, College of Earth, Ocean, and Atmospheric Science, Corvallis, United States, (3)KOPRI Korea Polar Research Institute, Incheon, Korea, Republic of (South), (4)Texas A&M University, Department of Geology & Geophysics, College Station, United States, (5)Appalachian State University, Boone, NC, United States, (6)Oregon State University, CEOAS, Corvallis, OR, United States, (7)The Australian National University, Research School of Earth Sciences, Canberra, Australia, (8)The Australian National University, Canberra, Australia, (9)University of Florida, Geological Sciences, Ft Walton Beach, FL, United States, (10)Royal Alberta Museum, Edmonton, AB, Canada, (11)CEOAS, Oregon State University, Corvallis, OR, United States, (12)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States, (13)Texas A&M University College Station, Geology & Geophysics, College Station, TX, United States, (14)University of Central Missouri, Physical Sciences, Warrensburg, MO, United States
