Fig. 7From: Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)Temporal fluctuation of various radiolarian abundances: a benthic foraminifera isotope curve of Sagawa et al. (2018), b radiolarian absolute abundance, c insolation at 65° N (Paillard et al. 1996), d coastal water species (%), e KC-related species (%), and f continental shelf species (%)Back to article page