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. 2017 Jan 27;12(1):e0170989. doi: 10.1371/journal.pone.0170989

Fig 4. Correlation of M40/4_SL71 dust record with other proxy climate data.

Fig 4

(A) June insolation at 30°N [62]. (B) Speleothem δ18O record of Soreq Cave, Israel [63]. (C) Saharan dust record from core M51/3_SL143 in the Aegean Sea documented by the kaolinite/chlorite ratio [16]. (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 Fig 2). Grey bars indicate sapropel layers (S). Younger Dryas (YD), Heinrich Events (H) and other cold events (o–t) are labelled [19]. MIS = Marine Isotope Stage.