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Volcano- and climate-driven changes in atmospheric dust sources and fluxes since the Late Glacial in Central Europe

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Academic year: 2021

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Figure 1. Proxies versus age measured at Etang de la Gruère (Switzer-land). A: Ti concentration (log scale) in high-res-olution core and com-posite Nd isotope curve using both samples from high-resolution (white circles) and low-resolu-tion (gray
Figure 2. The ε Nd isotope signal as recorded in low-resolution Etang de la Gruère peat core, percentage of Plantago lanceolata, percent-age of terrigenous material in core from African Atlantic coast (de-Menocal et al., 2000), and modeled percentage

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