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Recovery from multi‐millennial natural coastal hypoxia in the Stockholm Archipelago, Baltic Sea, terminated by modern human activity

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Academic year: 2021

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Fig. 1. Bathymetric map of the Baltic Sea, including locations of the Baltic proper, Gulf of Bothnia, Gulf of Finland, and locations of the study sites of van Helmond et al
Fig. 3. Overview of TEX 86 L values, BIT-index values and TEX 86 L -based sea surface temperature (SST) reconstructions, using the Baltic Sea calibration by Kabel et al
Fig. 4. Age-depth model for Erstaviken. Yellow dots represent 210 Pb dates (constant rate of supply model; Appleby and Oldfield, 1978) for the top sediments (Gemini core)
Fig. 5. Sedimentary concentrations of organic carbon (C org ), molybdenum (Mo), lead (Pb), and zinc (Zn) and TEX 86 L -based sea surface temperature (SST) reconstructions, using the Baltic Sea calibration (Kabel et al
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