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Progress in Earth and Planetary Science
Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

From: Alkenone surface hydrographic changes of the subarctic Northwestern Pacific since the last glacial: proxy limitations and implications of non-thermal environmental influences

Fig. 4

Last glacial subarctic NW Pacific alkenone-SST changes and its linkage with high-to-low latitude climate variability. a Northern Atlantic climate variability represented by NGRIP ice core δ18O sequence (GICC05; North Greenland Ice Core Project members 2004); b western Bering Sea alkenone-SST records: SO 201-2-101KL, SO 201-2-85KL, and SO 201-2-77KL (Max et al. 2012); c off Kamchatka alkenone-SST records: SO 201-2-114KL, SO 201-2-12KL, and LV 63-41-2 (Max et al. 2012; This study); d the Okhotsk Sea alkenone-SST records: LV 29-114-3 and MD012412 (Max et al. 2012); and e East Asian monsoon climate variability represented by the Hulu cave δ18O sequence (Wang et al. 2004). Shaded intervals indicate LGM, HE 1, B/A, and YD. Arrow shows the 8.2 ka cooling event

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