We thank Mr Alan Crawford who owns Towai Farm for access to the site and Mr Nelson Parker for providing the kauri wood samples. Support was provided by the Australian Research Council (grants FL100100195, LP120100310 and DP130104156), the UK Natural Environment Research Council (grants NE/H009922/1 and NE/I007660/1) and GH was supported by Eva-Mayr-Stihl Foundation, Waiblingen, Germany, Deutsche Forschungsgemeinschaft DFG (HE3089/9-1) and the Federal Ministry of Education and Research (01DR12097). Lamont-Doherty Earth Observatory contribution number 8064. We also wish to thank Dr Gretel Boswijk for an assessment of the Towai tree-ring measurements and Dr Andrew Lorrey for his comments on an earlier version of the manuscript.
Climate Change Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales, Australia; Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, United States; Gondwana Tree-ring Laboratory, P. O. Box 14, Little River, Canterbury, New Zealand; GFZ German Research Centre for GeoSciences, Section 5.2, Telegrafenberg, Potsdam, Germany; Department of Geography, Exeter University, Devon, United Kingdom; Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, FL, United States; Waikato Radiocarbon Laboratory, University of Waikato, Private Bag 3105, Hamilton, New Zealand; Department of Earth System Science, University of California, Irvine, CA, United States; Research Laboratory for Archaeology and the History of Art, University of Oxford, Dyson Perrins Building, South Parks Road, Oxford, United Kingdom; Department of Geology—Quaternary Sciences, Lund University, Lund, Sweden; UMR CNRS 5805 EPOC – OASU, Univ. BordeauxPessac Cedex, France; Australian Nuclear Science and Technology Organisation (ANSTO), Locked Bag 2001, Kirrawee DC, New South Wales, Australia
Recommended Citation:
Palmer J.G.,Turney C.S.M.,Cook E.R.,et al. Changes in El Niño – Southern Oscillation (ENSO) conditions during the Greenland Stadial 1 (GS-1) chronozone revealed by New Zealand tree-rings[J]. Quaternary Science Reviews,2016-01-01,153