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Imagotaria downsi
Taxonomy
Imagotaria downsi was named by Mitchell (1968) [SBMNH = Santa Barbara Museum of Natural History]. Its type specimen is SBMNH 342, a partial skull, and it is a 3D body fossil. Its type locality is Great Lakes Carbon Co. quarry, which is in a Tortonian marine diatomite in the Monterey Formation of California. It is the type species of Imagotaria.
Synonymy list
Year | Name and author |
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1968 | Imagotaria downsi Mitchell p. 1844 figs. Fig. 1-15 |
1994 | Imagotaria downsi Deméré p. 113 |
2003 | Imagotaria downsi Deméré et al. p. 49 figs. Fig. 3.3 |
2008 | Imagotaria downsi Barnes p. 531 |
2011 | Imagotaria downsi Boessenecker p. 2 |
2013 | Imagotaria downsi Boessenecker and Churchill p. 10 fig. 8 |
2015 | Imagotaria downsi Boessenecker and Churchill figs. Fig. 2 |
2018 | Imagotaria downsi Berta p. 714 figs. Fig. 3 |
2018 | Imagotaria downsi Berta et al. p. 217 figs. Fig. 6 |
2018 | Imagotaria downsi Magallanes et al. p. 30 figs. Figure 14 |
2020 | Imagotaria downsi Biewer et al. figs. Figs. 4, 5 |
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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.
†Imagotaria downsi Mitchell 1968
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Diagnosis
Reference | Diagnosis | |
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J. N. Biewer et al. 2020 | Imagotaria downsi shares with other known odobenids a large, dorsoventrally elliptical narial opening with thick margins (c. 2[1]), dorsoventrally thick and lat- erally broad pterygoid strut (c. 13[2]), prominent antorbital process formed by frontal and maxilla (c. 15[1]), large epitympa- nic process (c. 23[1]), bony tentorium that is appressed to the pet- rosal (c. 29[1]), medial lip of distal trochlea greater in diameter than distal capitulum (c. 84[1]), and distal end of radius expanded (c. 85[1]). It can be differentiated from more basal odobenids like Pron. repenningi and Protot. primigenia, by a flattened and plate- like paroccipital process (c. 34[3]). It can be differentiated from all other more basal odobenids (i.e., basal odobenids excluding Pontolis and Os. eodon) by its shallow glenoid fossa (c. 26[1]), lack of a metaconid on its lower postcanines (c. 70[2]), and lack of a ventral tuberosity of the zygomatic root (c. 7[0]). The latter character also differentiates it from all neodobenians except G. pugnax. Imagotaria downsi can be distinguished from species of Pontolis and Os. eodon by an anterodorsally oriented mandib- ular foramen (c. 48[1]). It can be further differentiated from Pontolis by well-developed tooth enamel (c. 62[0], which also differentiates it from neodobenians), lower postcanines with rough lingual cingula (c. 67[1]), and talonid basins in the postca- nines (c. 69[0]). It can be distinguished from Os. eodon and Neo- dobenia by having a p2 with double or bilobed roots (c. 72[0]) and a double-rooted m1 (c. 79[0]). In addition to previously listed characters (c. 7, 62, 72, 79), I. downsi can be distinguished from Neodobenia by having a narrow interorbital bar (c. 17[1]), |
Measurements
No measurements are available
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Source: f = family, c = class, uc = unranked clade | |||||
References: Kohno et al. 1995, Hendy et al. 2009, Carreño and Cronin 1993 |
Age range: base of the Tortonian to the top of the Clarendonian or 11.63000 to 9.40000 Ma
Collections (19 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Clarendonian | USA (California) | Imagotaria downsi (84331) | |
Tortonian | Japan (Fukushima) | Pinnipedia indet. (227081) | |
Tortonian | USA (California) | Imagotaria downsi (40514 45489 52184 52213 type locality: 58988 59156 59157 59158 59159 59160 59161 152097 152101 215597 225292) Imagotaria downsi, Imagotaria downsi (13300) Imagotaria sp. (13062) |