Quaternary Research Copyright © University of Washington. Published by Cambridge University Press, 2021. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. doi:10.1017/qua.2020.119 THEMATIC SET HEINRICH EVENTS Evidence for strong relations between the upper Tagus loess formation (central Iberia) and the marine atmosphere off the Iberian margin during the last glacial period Daniel Wolfa* , Thomas Kolbb, Karolin Ryborza, Susann Heinrichc, Imke Schäferd, Ruben Calvoe, Jesus Sancheze, Ulrich Hambachf, Roland Zechg, Ludwig Zöllerf, Dominik Fausta aTechnische Universität Dresden, Department of Geography, Dresden, 01062, Germany bJustus-Liebig-University Giessen, Department of Geography, Giessen, 35390, Germany cMax-Planck-Institute for Evolutionary Anthropology, Leipzig, 04103, Germany dUniversity of Bern, Institute of Geography and Oeschger Centre for Climate Change Research, Bern, 3012, Switzerland eUniversidad de Castilla La Mancha, Dpto. de Ingenieria Civil y de la Edificación, Ciudad Real, Spain fUniversity of Bayreuth, Department of Geography, Bayreuth, 95440, Germany gFriedrich-Schiller-Univerität Jena, Institute of Geography, Jena, 07743, Germany *Corresponding author. E-mail address:
[email protected] (RECEIVED April 28, 2020; ACCEPTED November 23, 2020) Abstract During glacial times, the North Atlantic