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Aletopelta coombsi
Taxonomy
Aletopelta coombsi was named by Ford and Kirkland (2001). Its type specimen is SDNHM 33909, a partial skeleton (eight teeth, fragmentary scap- ulae, partial humerus, partial ulna, possible fragment of right ?radius, ulna, partial left and possibly right ischium, femora, t), and it is a 3D body fossil. Its type locality is Carlsbad Ankylosaur (SDNHM Loc. 3392), which is in a Campanian offshore mudstone/sandstone in the Point Loma Formation of California.
It was considered a nomen dubium by Vickaryous et al. (2004).
It was considered a nomen dubium by Vickaryous et al. (2004).
Synonymy list
| Year | Name and author |
|---|---|
| 2001 | Aletopelta coombsi Carpenter p. 457 |
| 2001 | Aletopelta coombsi Ford and Kirkland pp. 240-241 figs. 12.1-12.12 |
| 2007 | Aletopelta coombsi Burns p. 54A |
| 2008 | Aletopelta coombsi Burns p. 1102 |
| 2013 | Aletopelta coombsi Kirkland et al. p. 7 |
| 2014 | Aletopelta coombsi Penkalski p. 628 |
| 2014 | Aletopelta coombsi Rivera-Sylva and Carpenter p. 174 |
| 2015 | Aletopelta coombsi Peecook and Sidor p. 3 |
| 2016 | Aletopelta coombsi Arbour and Currie p. 397–398 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Aletopelta coombsi Ford and Kirkland 2001
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| V. M. Arbour and P. J. Currie 2016 | Differs from all other ankylosaurs in possessing the following combination of characters: hexagonal pelvic osteoderms forming semi-continuous sheet over the pelvis; unlike Glyptodontopelta, pelvic osteoderms do not have dendritic surface texture; unlike Stegopelta, first cervical half ring is composed of osteoderms fused to underlying bony band, not closely appressed adjacent osteoderms. |