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Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

From: Millennial-scale oscillations in the Kuroshio–Oyashio boundary during MIS 19 based on the radiolarian record from the Chiba composite section, central Japan

Fig. 4

Comparisons among paleoceanographic proxies: a Oxygen isotope record (δ18O) of planktonic and benthic foraminifera (Haneda et al. 2020). Pale blue indicates the range of values for Globigerina bulloides18OGb, upper limit) and Globorotalia inflata18OGi, lower limit) from the Yoro River and Yoro-Tabuchi sections. Dark blue solid line indicates average of δ18OGb and δ18OGi. Dashed lines with solid circles and × symbols indicate δ18OGb and δ18OGi from the Kokusabata, Yanagawa and Urajiro sections, and the dark-blue dashed line without dots shows their average. b Variations of the Tr index. Pale red line indicates original plots, and their three-point moving average is shown as a red line for the high-resolution interval. c Total radiolarian abundance changes. Yellow line shows the original plots and the dark line indicates moving average over three points. Gray bands indicate intervals of multiple maxima of the Tr curve for the high-resolution interval

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