Vegetation and weathering indicators from drill core MAL05-2A.YD, Younger Dryas. H1, Heinrich event 1.
Sarah J. Ivory
Michael M. McGlue
Geoffrey S. Ellis
Anne-Marie Lézine
Andrew S. Cohen
Annie Vincens
10.1371/journal.pone.0112855.g003
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>
2014-11-18 05:06:51
summer rainfall
climate change
Southeast Africa Tropical climate
Terrigenous sediment mass accumulation rates
YD
Last Deglacial Transition
chemical weathering intensity
erosion
Lake Malawi vegetation