POST-PRINT TEPHROCHRONOLOGY AND THE EXTENDED INTIMATE (INTEGRATION OF ICE‐CORE, MARINE AND TERRESTRIAL RECORDS) EVENT STRATIGRAPHY 8-128 KA B2K. Simon Blockleya *, Anna Bourneb Achim Brauerc, Siwan Daviesb, Mark Hardimand, Poppy Hardinga, Christine Lanee, Alison MacLeoda, Ian Matthewsa, Sean Pyne O’Donnellf, Sune Olander Rasmusseng, Sabine Wulfb, Giovani Zanchettah a. Centre for Quaternary Research, Royal Holloway, University of London, Egham Hill, Surrey, TW20 0EX, UK b. Department of Geography, Swansea University, Singleton Park, Swansea SA2 8PP, Wales, UK c. GFZ German Research Centre for Geosciences, Telegrafenberg, Building C, 14473 Potsdam d. Department of Geography, University of Portsmouth, Buckingham Building, Lion Terrace, Portsmouth, PO1 3HE, UK e. Geography, University of Manchester, Arthur Lewis Building, Oxford Road, Manchester, M13 9PL, UK f. School of Geography, Archaeology and Palaeoecology, Queen’s University, Belfast BT7 1 NN, Northern Ireland. UK g. Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen, Denmark h. Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy *Corresponding Author: Tel.: +44 1784 443405. E-mail address:
[email protected] (S.P.E. Blockley). Abstract The comparison of palaeoclimate records on their own independent timescales is central to the work of the INTIMATE (INTegrating Ice core, MArine and TErrestrial records) network. For the North Atlantic region, an event stratigraphy has been established from the high- precision Greenland ice-core records and the integrated GICC05 chronology. This stratotype provides a palaeoclimate signal to which the timing and nature of palaeoenvironmental change recorded in marine and terrestrial archives can be compared.