<p>(A) June insolation at 30°N [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0170989#pone.0170989.ref062" target="_blank">62</a>]. (B) Speleothem δ<sup>18</sup>O record of Soreq Cave, Israel [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0170989#pone.0170989.ref063" target="_blank">63</a>]. (C) Saharan dust record from core M51/3_SL143 in the Aegean Sea documented by the kaolinite/chlorite ratio [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0170989#pone.0170989.ref016" target="_blank">16</a>]. (D) Saharan dust record from core M40/4_SL71 in the Ionian Sea documented by the kaolinite/chlorite ratio, with dust pulses D1 to D6 (for high resolution see <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0170989#pone.0170989.g002" target="_blank">Fig 2</a>). Grey bars indicate sapropel layers (S). Younger Dryas (YD), Heinrich Events (H) and other cold events (o–t) are labelled [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0170989#pone.0170989.ref019" target="_blank">19</a>]. MIS = Marine Isotope Stage.</p
