A ~400 ka-multi-centennial record from Lake Petén Itzá reveals mechanisms of moisture transport across Central America

Liseth Perez1, Mona Stockhecke2, Sergio Cohuo-Durán3, Laura Macario-González4, Michelle Abstein5, Philipp Hoelzmann6, Florence Sylvestre7, Christine Paillés8, Alexander Correa-Metrio9, Jason H Curtis10, Mark Brenner11, Steffen Kutterolf12, Daniel Ariztegui13, Flavio Anselmetti14, David A Hodell15 and Antje Schwalb1, (1)Technical University of Braunschweig, Braunschweig, Germany, (2)University of Minnesota Duluth, Earth and Environmental Sciences Department, Duluth, MN, United States, (3)Tecnológico Nacional de México/I.T. de Chetumal, Chetumal, Mexico, (4)Tecnológico Nacional de México/I.T. de la Zona Maya, Quintana Roo, Mexico, (5)Institut für Geosysteme und Bioindikation, Technische Universität Braunschweig, Braunschweig, Germany, (6)Free University Berlin, Institute of Geography, Berlin, Germany, (7)CEREGE, Aix-en-Provence Cedex, France, (8)CEREGE, Aix-en-Provence, France, (9)Universidad Nacional Autonoma de Mexico, Departamento de Paleontología, Mexico City, Mexico, (10)University of Florida, Department of Geological Sciences, Gainesville, FL, United States, (11)University of Florida, Ft Walton Beach, FL, United States, (12)GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany, (13)University of Geneva, Geneva, Switzerland, (14)University of Bern, Bern, Switzerland, (15)University of Cambridge, Godwin Laboratory for Palaeoclimate Research, Cambridge, United Kingdom