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The multiple chronological techniques applied to the Lake Suigetsu SG06 sediment core,central Japan
Authors:Richard A Staff  Takeshi Nakagawa  Gordon Schlolaut  Michael H Marshall  Achim Brauer  Henry F Lamb  Christopher Bronk Ramsey  Charlotte L Bryant  Fiona Brock  Hiroyuki Kitagawa  Johannes van der Plicht  Rebecca L Payne  Victoria C Smith  Darren F Mark  Alison Macleod  Simon P E Blockley  Jean‐Luc Schwenninger  Pavel E Tarasov  Tsuyoshi Haraguchi  Katsuya Gotanda  Hitoshi Yonenobu  Yusuke Yokoyama  Suigetsu Project Members
Institution:1. Research Laboratory for Archaeology and the History of Art (RLAHA), University of Oxford, , Oxford, OX1?3QY UK;2. Department of Geography, University of Newcastle, , Newcastle‐upon‐Tyne, NE1?7RU UK;3. Section 5.2: Climate Dynamics and Landscape Evolution, German Research Center for Geoscience (GFZ), , Telegrafenberg, D‐14473 Potsdam Germany;4. Institute of Geography and Earth Sciences, Aberystwyth University, , Aberystwyth, SY23?3DB UK;5. NERC Radiocarbon Facility – Environment (NRCF‐E), , East Kilbride, G75?0QF UK;6. Department of Earth and Environmental Sciences, Nagoya University, , Nagoya, 464‐8601 Japan;7. Department of Isotope Research, Energy and Sustainability Research Institute, University of Groningen, , 9747 AG Groningen, Netherlands;8. NERC Argon Isotope Facility, Scottish Universities Environmental Research Centre, , East Kilbride, G75?0QF UK;9. Department of Geography, Royal Holloway, University of London, , Egham, TW20?0EX UK;10. Institute of Geological Sciences, Palaeontology, Freie Universit?t Berlin, , 12249 Berlin, Germany;11. Department of Biology and Geosciences, Osaka City University, , 3‐3‐138 Sugimoto, Japan;12. Faculty of Policy Informatics, Chiba University of Commerce, , Chiba, 272‐8512 Japan;13. College of Education, Naruto University of Education, , Naruto, 772‐8502 Japan;14. Atmosphere and Ocean Research Institute, Department of Earth and Planetary Sciences, University of Tokyo, , Chiba, 277‐8564 Japan;15. http://www.suigetsu.org
Abstract:The varved sediment of Lake Suigetsu (central Japan) provides a valuable opportunity to obtain high‐resolution, multi‐proxy palaeoenvironmental data across the last glacial/interglacial cycle. In order to maximize the potential of this archive, a well‐constrained chronology is required. This paper outlines the multiple geochronological techniques being applied – namely varve counting, radiocarbon dating, tephrochronology (including argon–argon dating) and optically stimulated luminescence (OSL) – and the approaches by which these techniques are being integrated to form a single, coherent, robust chronology. Importantly, we also describe here the linkage of the floating Lake Suigetsu (SG06) varve chronology and the absolute (IntCal09 tree‐ring) time scale, as derived using radiocarbon data from the uppermost (non‐varved) portion of the core. This tie‐point, defined as a distinct (flood) marker horizon in SG06 (event layer B‐07–08 at 1397.4 cm composite depth), is thus derived to be 11 255 to 11 222 IntCal09 cal. years BP (68.2% probability range).
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