TY - JOUR T1 - Tephrochronology and the extended intimate (integration of ice-core, marine and terrestrial records) event stratigraphy 8-128 ka b2k A1 - Blockley,Simon P. E. A1 - Bourne,Anna J. A1 - Brauer,Achim A1 - Davies,Siwan M. A1 - Hardiman,Mark A1 - Harding,Poppy R. A1 - Lane,Christine S. A1 - Macleod,Alison A1 - Matthews,Ian P. A1 - Pyne-O'Donnell,Sean D. F. A1 - Rasmussen,Sune O. A1 - Wulf,Sabine A1 - Zanchetta,Giovanni AD - Univ London, Royal Holloway, Ctr Quaternmy Res, Egham TW20 0EX, Surrey, England. AD - Swansea Univ, Coll Sci, Dept Geog, Swansea SA2 8PP, W Glam, Wales. AD - GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany. AD - Univ Portsmouth, Dept Geog, Portsmouth P01 3HE, Hants, England. AD - Univ Manchester, Manchester M13 9PL, Lancs, England. AD - Queens Univ Belfast, Sch Geog Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland. AD - Univ Copenhagen, Niels Bohr Inst, Ctr Ice & Climate, DK-2100 Copenhagen, Denmark. AD - Univ Pisa, Dipartimento Sci Terra, Pisa, Italy. UR - https://archimer.ifremer.fr/doc/00289/40028/ DO - 10.1016/j.quascirev.2014.11.002 KW - Event-stratigraphy KW - Tephrochronology KW - INTIMATE KW - Greenland ice cores KW - Palaeoenvironment KW - Palaeoclimate N2 - 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 GICCO5 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. To facilitate this wider comparison, without assuming synchroneity of climatic change/proxy response, INTIMATE has also focussed on the development of tools to achieve this. In particular the use of time-parallel marker horizons e.g. tephra layers (volcanic ash). Coupled with the recent temporal extension of the Greenland stratotype, as part of this special issue, we present an updated INTIMATE event stratigraphy highlighting key tephra horizons used for correlation across Europe and the North Atlantic. We discuss the advantages of such an approach, and the key challenges for the further integration of terrestrial palaeoenvironmental records with those from ice cores and the marine realm. Y1 - 2014/12/15 PB - Pergamon-elsevier Science Ltd JF - Quaternary Science Reviews SN - 0277-3791 VL - 106 SP - 88 EP - 100 ID - 40028 ER -