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Fossil Record A palaeontological open-access journal of the Museum für Naturkunde
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Volume 19, issue 1
Foss. Rec., 19, 61-81, 2016
https://doi.org/10.5194/fr-19-61-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Foss. Rec., 19, 61-81, 2016
https://doi.org/10.5194/fr-19-61-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Jan 2016

Research article | 20 Jan 2016

Scale morphology and specialized dorsal scales of a new teleosteomorph fish from the Aptian of West Gondwana

P. G. Giordano1, G. Arratia2, and H.-P. Schultze2 P. G. Giordano et al.
  • 1Universidad Nacional de San Luis, Chacabuco 917, San Luis, CP: 5700, Argentina
  • 2Biodiversity Institute, University of Kansas, 1345 Jayhawk Blvd., Lawrence, Kansas, 66045, USA

Abstract. Scales of a new species of Teleosteomorpha from the continental Aptian of the south of South America are studied. These neopterygians are from the La Cantera Formation in central Argentina, and were previously identified as Pholidophoriformes. They present ganoid scales; most of them are rhombic with well-developed peg-and-socket articulations and possessing a smooth surface. They have a straight posterior margin, but occasionally, some scales of the flank have a sinuous posterior margin with one or two serrations. The shape of the scales varies along the body from large, rectangular and deeper than long scales behind the head to the preanal region to smaller and rhomboidal scales in the caudal region. There are a few horizontal rows along the flank and about 32 lateral line scales. Thick, round ganoid scales are present in the prepelvic region close to the ventral margin. The round and rhombic scales present growth lines, which form concentric ridges on the external side. A characteristic row of deep scales forms the dorsal margin on each side of the body; a row of median ridge scales is not present. This is a unique feature of the studied fishes. Scutes covered with unornamented ganoine precede the pelvic, dorsal, and anal fins, as well as the dorsal and ventral margins of the caudal fin. The posterior margin of the dorsal lobe of the caudal fin is formed by a single line of scales, which continues and covers the base of the first principal caudal ray. Histological studies reveal a lepisosteoid-scale type with multiple ganoine layers, lack of dentine, and the presence of canaliculi of Williamson. The macro- and micromorphology of the scales shows features that are found in other teleosteomorphs, but also in other neopterygians.

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This work is based on scales of a new group of Cretaceous South American fishes. Detail studies about scales are very useful, considering that many fossil fishes are known because of their squamation. Comparisons with other Mesozoic fishes were made. Among main conclusions are that these fishes present lepisosteoid-type scales (with enamel but without dentine) and in particular paired dorsal scales in the position where other fishes commonly have median dorsal ridge scales.
This work is based on scales of a new group of Cretaceous South American fishes. Detail studies...
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