Fig. 3From: Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)Key Nassellarian species encountered at Site U1429. 1–2 Botryostrobus auritus (Ehrenberg) (sample 346-U1429A-7H6-27-29 cm); 3–5 Cycladophora davisiana Ehrenberg (sample 346-U1429C-10H4-27-29 cm); 6–9 Arachnocorallium calvata Petrushevskaya group (sample 346-U1429A-7H6-27-29 cm); 10, 14 Phormospyris spp. (10. sample 346-U1429C-10H4-27-29 cm, 11 sample 346-U1429A-7H6-27-29 cm); 11–13 Arachnocorys castanoides Tan and Tchang (sample 346-U1429A-1H1-27-29 cm); 15–17 Pseudocubus obeliscus Haeckel (sample 346-U1429A-7H6-27-29 cm); 21-24 Lithomelissa setosa Jørgensen (sample 346-U1429A-7H6-27-29 cm); 18-19 Pseudodictyophimus gracilipes (Bailey) (sample 346-U1429C-10H4-27-29 cm); 20 Plectacantha oikiskos (Jørgensen) (Sample 346-U1429A-7H6-27-29 cm); 26 Dimelissa thoracites (Haeckel) (sample 346-U1429A-1H1-27-29 cm); 25 Phormacantha hystrix Jørgensen Back to article page