Temporal range: Early Jurassic, 183–125Ma
|Fossil specimen of L. elvensis|
†L. elvensis (Blainville, 1818) (orig. Cyprinus)
Lepidotes (previously known as Lepidotus) is an extinct genus of semionotid neopterygian ray-finned fish from the Jurassic period (Toarcian age) and Early Cretaceous. Fossils have been found in marine sediments of France, England, and Germany, and in Early Cretaceous sediments of Brazil and Bornholm, Denmark (Jydegaard Formation). It lived from the Rhaetian of the Triassic until the Cenomanian of the Cretaceous. In 1895, many species were assigned to it by Arthur Smith Woodward. They include, L. elvensis, L. semiserratus, L. tuberculatus, L. gallineki, L. leedsi, L. latifrons, L. haydeni, L. occidentalis, L. macrocheirus, L. subovatus, L. minor, L. affinis, L. unguiculatus, L. laevis, L. maximus, L. mantelli, L. degenhardti, L. hauchecorni, L. mawsoni, L. notopterus and L.? pustulatus. Numerous additional species have been assigned to it which Woodward considered indistinguishable from others.
Inhabiting both freshwater lakes and shallow seas, Lepidotes was typically about 30 centimetres (12 in) long. The body was covered with thick, enamelled scales. Batteries of peg-like teeth enabled Lepidotes to crush the shells of its molluscan prey.
Lepidotes was one of the earliest fish in which the upper jawbones were no longer attached to the jugal bone. This allowed the jaws to be stretched into a 'tube' so that the fish could suck in prey from a greater distance than in previous species. This system is still seen in some modern fish, such as carp.
Lepidotes scales are ovular in shape, and are 18.5 millimetres (0.73 in) long and 3 millimetres (0.12 in) thick at the thickest point. The scales are smooth and shiny on the external surface, with only a few small depressions scattered toward the centre that are shaped like punctures.
Many characteristics were identified by Woodward in 1895, and they are listed below:
- a fusiform trunk only moderately compressed;
- the fact that the marginal teeth are compressed;
- the presence of stouter inner teeth that are smooth;
- ossified ribs;
- very large fin-fulera on all fins;
- that all paired fins are small;
- short and deep dorsal and anal fins;
- very robust, smooth or feebly oriented scales;
- flank scales that are not much deeper than wide;
- scales ventrally nearly as deep as broad;
- and the presence of inconspicuous dorsal and ventral ridge-scales.
L. elvensis is the type species of Lepidotes. It was described by Ducrotay de Blainville in 1818. It is known from an almost complete specimen housed in the Paris Museum of Natural History. The specimen measures up to 75 centimetres (2.46 ft) long. The specimen is from the Upper Lias, in Bavaria. The specimens P. 7406, P. 7407, P. 7408, P. 2014, P. 2054, P. 3529a, P. 3529b, 18992, 18993/94 19662, 32421, and 32422 have all been assigned to this species. The external bones of this species are smooth, but some have sparsely-placed coarse tuberculations (protuberances). The frontal bone is more than twice the length of the parietal in the specimens. It also has a comparatively narrow marginal symphysis (articulation).
This species was named by Agassiz in 1837 and is known from some incomplete remains. It has been classified as closely related to L. elvensis. It is more elongate than L. elvensis, being four times as long as tall. It also has more sharply angulated sutures between its parietals, and the parietals are also proportionally longer. It is known from the specimens P. 1127, P. 7409, P. 2012, P. 2012a, P. 3527, P. 3528, P. 3528a, P. 5213, P. 5228, P. 6394, P. 7410, and 35556, all from the Upper Lias of Yorkshire.
L. gallineki is known from only an imperfect internal cast of the head and neck, assigned to Lepidotes by Michael (1863). The estimated length of the species is 90 centimetres (3.0 ft). The eternal bones are almost all apparently smooth. On the hinder margin, the scales are smooth and not serrated. The specimen was from the Rhaetic of Upper Silesia.
This species, named in 1837 by Louis Agassiz, is known from a single suboperculum (scale-shaped lower opercular bone). It includes an assortment of unidentified remains from Stonesfield Slate. The formation dates back to the Bathonian of England. The only certain remain that can be assigned to L. tuberculatus is the suboperculum, so all the other material is considered to be unlikely to belong to it. The specimens provisionally assigned to L. tuberculatus by Woodward are P. 471, P. 1111, P. 1111a, P. 3524, P. 7411, 28606, 28607, 30569, 37219, 47141, and 47980.
L. macrocheirus was described by Sir Philip Egerton in 1845. It could grow up to 70 centimetres (28 in) long. The trunk of the specimens are very robust, and the head measures one fifth of the total length. Like in L. elvensis, the parietals measure less than half of the frontals. The frontals are three times as long as the are wide. It possessed slightly tumid, but styliform marginal teeth. The inner teeth were large and obtuse, but there pedicles were only moderately high. The species lacked any signs of ring-vertebrae. The fin-fulcra were large, but on the medial fins they were slender. The specimens assigned to it are P. 6839, P. 6899, P. 6900, P. 7412, and P. 7413, from the Oxfordian of England.
L. occidentalis is known from five ovular scales, described by Joseph Leidy in 1860. The enamel surfacing of all five scales is shiny and smooth. The largest of the scales is 100 millimetres (3.9 in) long, and the smallest in 50 millimetres (2.0 in).
L. haydeni is a species known from a single, rectangular scale, described by Leidy in 1860. The scale is 130 millimetres (5.1 in) long and 89 millimetres (3.5 in) wide. The covering of the scale is small, rectangular squares. The root of the scale projects toward the front of one of the long sides. The specific name honors Dr. Hayden, who discovered many remains, including the only scale of L. haydeni.
L. latifrons was named and described by Arthur Smith Woodward in 1893. It is known from bones and scales from the head and trunk regions. It measured to about 1 metre (3.3 ft) long. The scales of this species are large and smooth. There are no traces of rings on the vertebrae. The marginal teeth are slender and styliform. The protion of the dentary that bears teeth is deepened near the symphysis. It is known from a few, mostly complete specimens, P. 6841, P. 6838, and P. 6840. The specimens date to the Oxfordian of Huntingdonshire.
- Agassiz, L. (1832), Untersuchungen über die fossilen Fische der Lias-Formation. Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefaktenkunde 3: 145
- López-Arbarello, A. (2012). "Phylogenetic Interrelationships of Ginglymodian Fishes (Actinopterygii: Neopterygii)." PLoS ONE, 7(7): e39370. doi:10.1371/journal.pone.0039370
- Woodward, A.S. (1895). "Catalogue of the Fossil Fishes in the British Museum (Natural History)" 2. British Museum of Natural History Department of Geology. pp. 77–119. doi:10.5962/bhl.title.61854.
- Hunterian Museum Geology Collections. "Lepidotes".
- John G. Maisey, Discovering Fossil Fishes, 1996:150, 152.
- Bonde, N.; Cristiansen, P. (2003). "New dinosaurs from Denmark". Comptes Rendus Paleovol. 2 (13). doi:10.1016/S1631-0683(03)00009-5.
- Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 37. ISBN 1-84028-152-9.
- Lambe, L.M. (1902). "New Genera and Species from the Belly River Series (mid cretaceous)". Canadian Palaeonto1. Geological Survey of Canada 3: 25–81.
- Leidy, J. (1860). "Notices of Remains of Extinct Reptiles and Fishes, Discovered by Dr. F. V. Hayden in the Bad Lands of the Judith River, Nebraska Territory". Proceedings of the Academy of Natural Sciences of Philadelphia 8: 16. JSTOR 4059129.