Can we better constrain the timing of GNAIW variability in the Western Equatorial Atlantic and its relationship to high North Atlantic Climate during the last deglaciation?

Thomas P Guilderson, Lawrence Livermore National Laboratory, Center for Accelerator Mass Spectrometry, Livermore, CA, United States, Katherine A Allen, University of Maine, Earth & Climate Sciences, Orono, ME, United States, Mea S Cook, Williams College, Geosciences, Williamstown, MA, United States, Virginia J Ettwein, University College London, London, United Kingdom and Jordan P Landers