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Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: δ 18Osw estimate for Globigerinoides ruber from core-top sediments in the East China Sea

Fig. 5

Comparison of monthly variation in the predicted δ 18Oc values with the core-top δ 18Oc values. The solid lines show the monthly variation of the predicted δ 18Oc values within the water column. The dotted lines show the core-top δ 18Oc values of G. ruber. The predicted δ 18Oc values are calculated from temperature and salinity data (http://www.jodc.go.jp/) using a calcite equilibrium equation (Bemis et al. 1998). See details in the text

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