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Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

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Figure

Figure 1. Schematic overview of the main components of theoceanic (thick arrows) and atmospheric (thin arrows) circulationover southern Africa (modified from Truc et al., 2013)
Table 1. AMS radiocarbon analyses of bulk TOC and carbonate material from core GeoB18308-1
Figure 3. Left: core log of GeoB18308-1 (internal structures withrecorded colors) demonstrating the presence of an event deposit(blue box)
Table 2. n-Alkane isotopic composition and distribution descriptive parameters averaged (with standard deviation).
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