A beryllium-10 chronology of late-glacial moraines in the upper Rakaia valley, Southern Alps, New Zealand supports Southern-Hemisphere warming during the Younger Dryas
Lamont–Doherty Earth Observatory of Columbia University, 61 Rt. 9W, Palisades, NY, United States; Department of Earth and Environmental Sciences, Columbia University, New York, NY, United States; School of Earth and Climate Sciences and Climate Change Institute, University of Maine, Orono, ME, United States; GNS Science, Private Bag 1930, Dunedin, New Zealand; Department of Geography, University of Sheffield, Sheffield, United Kingdom; Department of Earth and Planetary Sciences, University of California, Berkeley, CA, United States; Department of Earth Science & Engineering, Imperial College London, South Kensington Campus, London, United Kingdom; Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA, United States; Idaho National Laboratory, Idaho Falls, ID, United States; School of Earth and Environmental Sciences, University of Manchester, Manchester, United Kingdom
Recommended Citation:
Koffman T.N.B.,Schaefer J.M.,Putnam A.E.,et al. A beryllium-10 chronology of late-glacial moraines in the upper Rakaia valley, Southern Alps, New Zealand supports Southern-Hemisphere warming during the Younger Dryas[J]. Quaternary Science Reviews,2017-01-01,170