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FIGURE 14 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 14. Photographs of the encountered morphotypes of Larcospira tetragonicentrum n. sp. All are Pl-view at Type 1. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 17. The topotypes from the H.M.S. Challenger station 271. 1-6 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 17. The topotypes from the H.M.S. Challenger station 271. 1-6, Larcopyle cervicornis (Haeckel, 1887); 7-12, Larcopyle buetschlii buetschlii Dreyer, 1889. All are Pl-view at Type1. Scale bar equals 0.1 mm. All specimens are from H.M.S. Challenger Station 271 sample.
FIGURE 19 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 19. Photographs of the encountered morphotypes of Larcopyle buetschlii buetschlii Dreyer, 1889, sensu stricto. All are Fr-view at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 13 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 13. Photographs of the encountered morphotypes of Larcospira teres n. sp. All are Pl-view at Type 1. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 4 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 4. The diagrams of the absolute Cartesian coordinate (Type 1) and the relative Cartesian coordinate (Type 2). 1, Type 1; 2, Type 2.
FIGURE 1 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 1. Location of the sampling sites in the northeastern Indian Ocean. The surface current (thick arrows) is modified from Peng et al. (2015); the deep circulation (thin arrows) is modified from Kawagata et al. (2006); the isohaline showing surface salinity during June (mean of 93 years) is modified from Gupta et al. (2002). Abbreviations are as follows: AABW, Antarctic Bottom Water; CPDW, Circumpolar Deep Water; NIHSIW, North Indian High-salinity Intermediate Water; NMC, Northeast Monsoon Current; SMC, Southwest Monsoon Current.
FIGURE 12 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 12. Photographs of the encountered morphotypes of Larcospira quadrangula Haeckel, 1887 sensu stricto. All are Pl-view at Type 1. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 20 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 20. Photographs of the encountered morphotypes of Larcopyle buetschlii chenmuhongi n. subsp. All are Frview at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 15 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 15. Photographs of the encountered morphotypes of Pylodiscus spinulosus (Chen and Tan, 1989). All are Frview at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 8 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 8. Photographs of the encountered morphotypes of Tetrapyle circularis Haeckel, 1887. All are Pl-view at Type 1, Fr-view at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 11 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 11. Photographs of the encountered morphotypes of Tetrapyle spp. (juvenile form). 1-2 and 9, Lt-view at Type 1, Fr-view at Type 2; 3-5, 7-8, 11-12, Sg-view at Type 1, Fr-view at Type 2; 6 and 10, Pl-view at Type 1, Fr-view at Type 2; 13-14, Pl-view at Type 1, Ug-view at Type 2; 15-16, Sg-view at Type 1, Fr-view at Type 2; 17-18, Sg-view at Type 1, Ug-view at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 10 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 10. Photographs of the encountered morphotypes of Tetrapyle fruticosa (Tan and Chen, 1990) new combination. All are Pl-view at Type 1, Fr-view at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 7. The typical Tetrapyle octacantha specimens from the surface water from the southern Villefranche-surMer. 1 and 6 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 7. The typical Tetrapyle octacantha specimens from the surface water from the southern Villefranche-surMer. 1 and 6, Ug-view at Type 2; 2-3 and 8, Pr-view at Type 2; 4-7, Fr-view at Type 2. Scale bar equals 0.1 mm. The arrow marks indicate the major portal-spines.
FIGURE 9 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 9. Photographs of the encountered morphotypes of Tetrapyle circularis Haeckel, 1887. All are Pl-view at Type 1, Fr-view at Type 2. Scale bar equals 0.1 mm. All specimens are from YDY05-01.
FIGURE 6 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 6. Photographs of the encountered morphotypes of Tetrapyle octacantha Müller 1859 sensu stricto. All are Pl-view at Type 1, Fr-view at Type 2. Scale bar equals 0.1 mm. The arrow marks indicate the major portal-spines. All specimens are from YDY05-01.
FIGURE 2. Morphological terminology under a transmitted light microscope. 1-2 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 2. Morphological terminology under a transmitted light microscope. 1-2, for gate and girdle; 3-8, for different pylonioid systems.
FIGURE 5 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 5. The structure of central combination in genera Tetrapyle (1-3), Larcopyle (4) and Circodiscus (5). 1, Sgview at Type 1, Fr-view at Type 2; 2, Pl-view at Type 1, Fr-view at Type 2; 3, Lt-view at Type 1, Pr-view at Type 2. G1, G2, S1a, and S1a-girdle are the morphological terminology, of which the definitions have been shown in Table 1.
FIGURE 3 in Taxonomy and species diversity of Holocene pylonioid radiolarians from surface sediments of the northeastern Indian Ocean
FIGURE 3. The absolute and relative orientations of specimens under the pylonioid system. The symbol "*" indicates Type 2 Relative Cartesian Coordinates.
FIGURE 15 in The late Maastrichtian Belemnella kazimiroviensis group (Cephalopoda, Coleoidea) in the Middle Vistula valley (Poland) and the Maastricht area (the Netherlands, Belgium) - taxonomy and palaeobiological implications
FIGURE 15. Two-dimensional plot Lsn (standardised length form apex to the protoconch) vs. AV (ventral aspect) of guards of Bln. kazimiroviensis from central and southern Russia and Central Asia, as illustrated by Naidin (1975). The dashed lines indicate the variability of Bln. kazimiroviensis and Bln. skolozdrownae from the Maastricht and the Middle Vistula valley regions.
FIGURE 20 in The late Maastrichtian Belemnella kazimiroviensis group (Cephalopoda, Coleoidea) in the Middle Vistula valley (Poland) and the Maastricht area (the Netherlands, Belgium) - taxonomy and palaeobiological implications
FIGURE 20. Relationship of BI (Birkelund Index) vs Dp (dorso ventral diameter at the protoconch) (BI = Ls/Dp; compare with Figure 6) of guards of Bln. skolozdrownae from the Middle Vistula valley in Poland and the Maastricht area in the Dutch-Belgian border region, in addition to two specimens from Denmark (blank triangles) as illustrated in the scientific literature (Jeletzky, 1951, pl. 7, figure 1; Birkelund, 1957, pl. 6, figure 4).
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