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. 2016 Nov 8;6:36334. doi: 10.1038/srep36334

Figure 3. Direct comparison between the benthic δ18>O LR04 stack59, MEDSTACK planktic δ18O data39, arboreal pollen from Tenaghi Philippon31, arboreal pollen (Pinus, JuniperusandBetula are excluded) from the Lake Ohrid core34, U-ratio and <2 μm fractions from the Stalać section (plotted versus age, abscissa), U-ratio and <2 μm fractions from the Ruma section 26 (the only section with existing grain-size record spanning the last three glacial-interglacial cycle in Middle Danube Basin; plotted vs. depth).

Figure 3

Note the differences between scales on the plots presenting Stalać and Ruma grain-size data. Tephra layers are marked with yellow lines; “CI” refers to the Campanian Ignimbrite/Y-5 tephra layer and “L2” refers to the L2 tephra layer.