Fig. 2From: Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)Key Spumellarian species encountered at Site U1429. 1–4 Actinomma leptodermum (Jørgensen) (sample 346-U1429A-7H6-27-29 cm); 5–6 Actinomma boreale Cleve (sample 346-U1429A-7H6-27-29 cm); 7 Actinomma medianum Nigrini (sample 346-U1429A-1H1-27-29 cm); 8-9 Spongodiscus cf. resurgens Ehrenberg (sample 346-U1429A-1H1-27-29 cm); 10-11 Larcopyle weddelium Lazarus, Faust and Popova (sample 346-U1429A-7H6-27-29 cm); 12 Spongosphaera streptacantha Haeckel (sample 346-U1429A-1H1-27-29 cm); 14 Druppatractus irregularis Popofsky (sample 346-U1429A-1H1-27-29 cm); 15-17 Phorticium polycladum Tan and Tchang (sample 346-U1429A-1H1-27-29 cm); 13 Larcopyle cf. buetschlii Dreyer (sample 346-U1429A-7H6-27-29 cm); 18 Tetrapyle circularis Haeckel (sample 346-U1429A-7H6-27-29 cm); 19–21 Tetrapyle fruticosa (Tan and Chen) (sample 346-U1429A-7H6-27-29 cm)Back to article page