Fig. 4From: Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)Radiolarian absolute abundance. The number of taxa (S), dominance index (D), and Shannon-Wiener diversity index (H′) are shown over time and compared to the benthic foraminifera isotope curve of Sagawa et al. (2018). Red lines indicate median valuesBack to article page