10.1371/journal.pone.0112855.g003 Sarah J. Ivory Sarah J. Ivory Michael M. McGlue Michael M. McGlue Geoffrey S. Ellis Geoffrey S. Ellis Anne-Marie Lézine Anne-Marie Lézine Andrew S. Cohen Andrew S. Cohen Annie Vincens Annie Vincens Vegetation and weathering indicators from drill core MAL05-2A.YD, Younger Dryas. H1, Heinrich event 1. Public Library of Science 2014 summer rainfall climate change Southeast Africa Tropical climate Terrigenous sediment mass accumulation rates YD Last Deglacial Transition chemical weathering intensity erosion Lake Malawi vegetation 2014-11-18 05:06:51 Figure https://plos.figshare.com/articles/figure/_Vegetation_and_weathering_indicators_from_drill_core_MAL05_2A_YD_Younger_Dryas_H1_Heinrich_event_1_/1246046 <p>(A) pollen percentages of Poaceae and (B) arboreal vegetation types (afromontane forest, tropical seasonal forest, miombo woodland), (C) XRD clay mineral percentages of smectite, kaolinite, and illite+chlorite, ratio of kaolinite to smectite (K/S), (D) ratio of silt to clay (silt/clay), and (E) terrigenous mass accumulation rate, and (F) δ<sup>18</sup>O from diatoms and TEX-86 temperature from piston cores M98-1P and M98-2PG from the northern basin of Lake Malawi from Barker et al. (2007) and Powers (2005), respectively.</p>