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>