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Lepisosteus bemisi
Taxonomy
Lepisosteus bemisi was named by Grande (2010). Its type specimen is FMNH PF15182, a skeleton, and it is a 3D body fossil. Its type locality is 18-inch-layer, F1-locality, which is in a Lostcabinian lacustrine - large limestone in the Green River Formation of Wyoming.
Synonymy list
Year | Name and author |
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2010 | Lepisosteus bemisi Grande p. 249 figs. 174-195 |
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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.
†Lepisosteus bemisi Grande 2010
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Diagnosis
Reference | Diagnosis | |
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L. Grande 2010 | Lepisosteus bemisi sp. nov. differs from all other species of lepisosteid in (A) normally having 14 principal caudal rays (occasionally 13), and (B) normally having four branchiostegal rays (x = 3.7, r = 3-4, = 6). Also, it differs from other species of Lepisosteus in the following characters C-F. (C) Like L. osseus but unlike L oculatus, L. platyrhincus, and L. platostomus, the head length is relatively long, with a length of more than 34% of standard length. (D) The preorbitai to postorbital length ratio, like L. osseus, is normally greater than 2. (E) Its mandible is relatively shorter than in L. osseus. (F) The width to length ratios of several of the skull bones are greater than in L. osseus. |
Measurements
No measurements are available
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Source: o = order, subp = subphylum | |||||
References: Carroll 1988, Hendy et al. 2009 |
Age range: Lostcabinian or 54.90000 to 50.50000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Lostcabinian | USA (Wyoming) | Lepisosteus bemisi (type locality: 187019) |