Onsets of the Holocene and the Lateglacial Interstadial Have Different Mechanisms – Revealed by Robust Synchronisation of Suigetsu, NGRIP, Hulu and Other High-Resolution Archives.
Takeshi Nakagawa1, Richard Staff2, Christopher Bronk Ramsey2, Charlotte Bryant3, Gordon Schlolaut4, Achim Brauer5, Michael H Marshall6, Henry F. Lamb7, Pavel E Tarasov8, Tsuyoshi Haraguchi9, Katsuya Gotanda10, Takayuki Omori11, Hitoshi Yonenobu12, Yusuke Yokoyama13, Ryuji Tada14 and Suigetsu 2006 Project Members, (1)Ritsumeikan University, Kusatsu, Japan, (2)University of Oxford, Oxford, United Kingdom, (3)NERC Radiocarbon Facility, East Kilbride, United Kingdom, (4)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, (5)GFZ German Research Centre for Geosciences, Section 4.3 - Climate Dynamics and Landscape Evolution, Potsdam, Germany, (6)Cologne, Germany, (7)Aberystwyth University, Department of Geography and Earth Sciences, Aberystwyth, United Kingdom, (8)Freie Universität Berlin, Institute of Geological Sciences, Berlin, Germany, (9)Osaka City Univ, Osaka, Japan, (10)Chiba University of Commerce, Chiba, Japan, (11)University of Tokyo, Bunkyo-ku, Japan, (12)Naruto University of Education, Naruto, Japan, (13)The University of Tokyo, Atmosphere and Ocean Research Institute (AORI), Kashiwa, Japan, (14)The University of Tokyo, Department of Earth and Planetary Science, Graduate School of Science, Tokyo, Japan
