Quaternary Science Advances 3 (2021) 100016
Quaternary Science Advances 3 (2021) 100016 Contents lists available at ScienceDirect Quaternary Science Advances journal homepage: www.journals.elsevier.com/quaternary-science-advances Persistent millennial-scale climate variability in Southern Europe during Marine Isotope Stage 6 G.P. Wilson a,*, M.R. Frogley b, P.D. Hughes c, K.H. Roucoux d, V. Margari e, T.D. Jones f, M.J. Leng g,h, P.C. Tzedakis e a Department of Geography & International Development, University of Chester, Chester, CH1 4BJ, UK b Department of Geography, University of Sussex, Brighton, BN1 9QJ, UK c Department of Geography, The University of Manchester, Manchester, M13 9PL, UK d School of Geography & Sustainable Development, University of St Andrews, St Andrews, KY16 9AL, UK e Environmental Change Research Centre, Department of Geography, University College London, London, WC1E 6BY, UK f AECOM, Birmingham, B4 6AT, UK g National Environmental Isotope Facility, British Geological Survey, Nottingham, NG12 5GG, UK h School of Biosciences, University of Nottingham, Nottingham, LE12 5RD, UK ARTICLE INFO ABSTRACT Keywords: Exploring the mode and tempo of millennial-scale climate variability under evolving boundary conditions can Marine Isotope Stage 6 provide insights into tipping points in different parts of the Earth system, and can facilitate a more detailed Southern Europe understanding of climate teleconnections and phase relationships between different Earth system components. Millennial-scale climate variability Here we use fossil diatom and stable carbon and oxygen isotope analysis of lake sediment deposits (core I-284) from the Ioannina basin, NW Greece, to explore in further detail millennial-scale climate instability in southern Europe during Marine Isotope Stage 6 (MIS 6; ca.
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