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Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years

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Figure

Figure 1. (a)text. Black arrows indicate the surface circulation patterns of the N Pacific (e.g., Stabeno and Reed, 1994)
Figure 2. (a)114KL; Meyer et al., 2016).2013).insolation at 65 Concentrations of �brGDGT of core 12KL
Figure 3. Fractional abundances of all nine brGDGT in core 12KL,given in percentage relative to the amount of �brGDGTs.
Figure 4. Comparison of proxy- and model-based inferences regarding glacial anomalies in temperature and atmospheric circulation over the(21 ka) relative to PI
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