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4 results for “Phymosomatoida”
FIGURE 1 in Late Cretaceous phymosomatids and the true identity of Cidarites granulosus Goldfuss, 1829 (Echinoidea, Phymosomatoida)
FIGURE 1. Camera-lucida drawings of plating style in Phymosoma granulosum (Goldfuss, 1829), based on GZG.STR.018536 from the lower Maastrichtian of Wittenfelde Quarry, Rügen, northeast Germany (see also Fig. 3A–C); A, interambulacral zone; B, ambulacral zone. Scale bar equals 2 mm.
FIGURE 2 in Late Cretaceous phymosomatids and the true identity of Cidarites granulosus Goldfuss, 1829 (Echinoidea, Phymosomatoida)
FIGURE 2. Phymosoma granulosum (Goldfuss, 1829), lectotype (RFWUIP 1335), of early to early late Maastrichtian age, locality unknown; A, oral view; B, ambital view; C, oral detail; D, detail of ambitus. A, B, natural size x 1,6; scale bar in C, D equals 2 mm.
FIGURE 7 in Late Cretaceous phymosomatids and the true identity of Cidarites granulosus Goldfuss, 1829 (Echinoidea, Phymosomatoida)
FIGURE 7. Geographic distribution of Phymosoma granulosum (Goldfuss, 1829) and Phymosoma ravni sp. nov. as currently understood.
FIGURE 4 in Late Cretaceous phymosomatids and the true identity of Cidarites granulosus Goldfuss, 1829 (Echinoidea, Phymosomatoida)
FIGURE 4. Phymosoma ravni sp. nov.; A, GZG.STR.018629, lower Maastrichtian, Promoisel Quarry, Rügen, Germany, test with spines. Phymosoma granulosum (Goldfuss, 1829); B, GZG.STR.018585, lower Maastrichtian, Wittenfelde Quarry, Rügen, Germany, accumulation of spines; C, D, MB.E 6867, lower Maastrichtian (Trigonosemus pulchellus Zone), Promoisel Quarry, Rügen, Germany, lower third of spine and spine in cross-section, respectively. All specimens coated with ammonium chloride prior to photography; natural size (B), x 1.2 (A), x 2 (C) and x 3 (D).
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