File:Chrispaulia (10.5852-ejt.2021.755.1405) Figure 13.png

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English: Fig. 13. A–C. Chrispaulia radiatus (Spencer, 1905) (BGS 108650), arm of individual in abactinal, lateral and actinal views, respectively (the original of Gale 2005: fig. 5). — D–E, H–O. Chrispaulia spinosa sp. nov. D–E. Holotype (Nds LH 105.107), arm fragment in lateral and actinal views, respectively. H–O. Isolated ossicles, all paratypes. H–I, N. Median superomarginals (NHMUK PI EE 17998, 18003). J–K. Distal superomarginals in lateral view (NHMUK PI EE 17999–18000). L–M. Distal inferomarginals in lateral view (NHMUK PI EE 18001–18002). O. Oral ossicle, in radial aspect (NHMUK PI EE 18004). — F–G. Chrispaulia wrightorum sp. nov., holotype, reconstructed distal arm, in abactinal and lateral views, respectively (NHMUK PI EE 17997). Provenance: A–C. Cenomanian (Lower Chalk), Dover, Kent, United Kingdom. D–E. Lower Hauterivian (Endemoceras amblygonium ammonite Zone), Engelbostel near Hannover, Germany. F–G. Albian, Hunstanton Formation, Speeton, Yorkshire, United Kingdom. H–O. Upper 3 m of Tealby Clay, Hauterivian, Nettleton, Lincolnshire, United Kingdom. Scale bars: A–G = 5 mm; H–O = 1 mm.
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Source Gale, A. S., & Jagt, J. W. (2021). The fossil record of the family Benthopectinidae (Echinodermata, Asteroidea), a reappraisal. European Journal of Taxonomy, 755(1), 149-190. https://doi.org/10.5852/ejt.2021.755.1405
Author Gale & Jagt (2021)
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current04:59, 7 August 2023Thumbnail for version as of 04:59, 7 August 20232,397 × 3,177 (5.1 MB)Christian Ferrer (talk | contribs){{Information | description = {{en|1=Fig. 13 (next page). A–C. ''Chrispaulia radiatus'' (Spencer, 1905) (BGS 108650), arm of individual in abactinal, lateral and actinal views, respectively (the original of Gale 2005: fig. 5). — D–E, H–O. ''Chrispaulia spinosa'' sp. nov. D–E. Holotype (Nds LH 105.107), arm fragment in lateral and actinal views, respectively. H–O. Isolated ossicles, all paratypes. H–I, N. Median superomarginals (NHMUK PI EE 17998, 18003). J–K. Distal superomarginals in latera...

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