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4 results for “Stanleycaris”
Fig. 5 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 5. Radiodontan euarthropod Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada. A. ROM 59975 (paratype). B. ROM 59976 (paratype). Abbreviation: Pn, podomere n.
Fig. 4. Lobopodian Aysheaia pedunculata Walcott, 1911, USNM 365608 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 4. Lobopodian Aysheaia pedunculata Walcott, 1911, USNM 365608 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; in cross-polarized light (A), cross-polarized light, red and yellow channels reduced (B).
Fig. 3 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 3. Comparison between terminal spines and vetral blades of Stanleycaris and oral papillae and lobopodous limbs of Aysheaia. A. Stanleycaris sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, Drumian), Utah, USA; anterior end showing recurved terminal spines (A1), ventral blade (A2). B. Aysheaia pedunculata Walcott, 1911, USNM 189199 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; anterior end showing anterior appendages and oral papillae. C, D. Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada. C. ROM 59975 (paratype), ventral blade. D. USNM 83942, trunk section and lobopods. Abbreviation: Pn, podomere n.
Fig. 1. A in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 1. A. Radiodontan euarthropod Stanleycaris sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, Drumian), Utah, USA; non-polarized light (A1), cross-polarized light, red and yellow channels reduced (A2), cross polarized light (A3), cross-polarized light, red and yellow channels enhanced (A4). B. Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010, ROM 59944 (holotype) from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; cross-polarized light (B1), black and white (B2). dorsal spines the anterior end, as also observed in in Stanleycaris hirpex (compare Fig. 3A2 and 3C). The ventral blades lack compaction wrinkles often preserved on limbs of A. pedunculata P1 P7 P11 P4 (Figs. 3D, 4; Ma et al. 2014: fig. 5B). The terminal spines at the anterior end of the specimen are short, recurved, and terminal P1 spines have a sharp termination. This morphology is similar to that of the spines in S. hirpex, and quite unlike the straight and sediment less robust oral papillae of A. pedunculata (compare Fig. 3A1 layer auxiliary spines and 3B). It should be noted that Robison (1985) studied the 5 mm ventral blades specimen before the extent of radiodontan frontal appendage Fig. 2. Explanatory drawing of radiodontan euarthropod Stanleycaris morphological diversity was known (e.g., Daley and Budd sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, 2010; Caron et al. 2010), and so lacked the appropriate con- Drumian), Utah, USA. Hachure direction indicates lower sediment level. text for correctly interpreting KUMIP 153923. Dotted lines indicate expected path of incomplete ventral blades.
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