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English: Figure 2. Assemblage of Titanokorys gainesi gen. et sp. nov., paratype ROMIP 65741. (a) Overview of slab, showing close association of H-element and partial appendage with an assemblage of Cambroraster falcatus consisting of an H-element and pair of appendages; (b) detail of T. gainesi; (c) close-up of endites from frontal appendage; (d) close-up of endites from frontal appendage of C. falcatus; (e) close-up of anterior margin of H-element, showing ornamentation. Ap, anterolateral processes; EnX, endite no. X; He, H-element; He-C, H-element of C. falcatus; Fa, frontal appendage; Fa-C, frontal appendage of C. falcatus; Ri, ridges associated with a reticulated pattern; Sa, sagittal spine; Se, secondary spines on endites; Sp, spiniform distal endites; Ts, Terminal spine; Tu, tubercles. Scale bars, (a,b) = 20 mm; (c–e) = 5 mm.
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Source Caron, J.-B.; Moysiuk, J. (2021-09-08). A giant nektobenthic radiodont from the Burgess Shale and the significance of hurdiid carapace diversity. Royal Society Open Science 8 (9): 210664. doi:10.1098/rsos.210664.
Author Jean-Bernard Caron, Joseph Moysiuk

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current02:01, 20 July 2022Thumbnail for version as of 02:01, 20 July 20221,654 × 1,932 (1.9 MB)Junnn11 (talk | contribs)Uploaded a work by Jean-Bernard Caron, Joseph Moysiuk from Caron, J.-B.; Moysiuk, J. (2021-09-08). [https://royalsocietypublishing.org/doi/10.1098/rsos.210664#d1e1128 A giant nektobenthic radiodont from the Burgess Shale and the significance of hurdiid carapace diversity]. Royal Society Open Science 8 (9): 210664. doi:10.1098/rsos.210664. with UploadWizard

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