Abstract

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.

Highlights

  • Cretaceous continental actinopterygian faunas from southern South America are scarce compared to marine ones

  • Neopterygians from La Cantera Formation have been assigned to the order Pholidophoriformes (Berg, 1937) since 1969 (Flores, 1969)

  • Such assignment was based on unreliable generalized characters found in many actinopterygians (Arratia, 2000, 2013), such as specimen size, the presence of bones covered by ganoine, and ganoid scales

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Summary

Introduction

Cretaceous continental actinopterygian faunas from southern South America are scarce compared to marine ones. Neopterygians from La Cantera Formation have been assigned to the order Pholidophoriformes (Berg, 1937) since 1969 (Flores, 1969) Such assignment was based on unreliable generalized characters found in many actinopterygians (Arratia, 2000, 2013), such as specimen size, the presence of bones covered by ganoine, and ganoid scales. These were the common traits for identifying “pholidophoriforms”, a group interpreted as non-monophyletic (Arratia, 2000, 2013). Detailed descriptions (micro- and macromorphology) of these structures could be a tool for helping to clarify taxonomic assignments and possible relationships of fishes from the La Cantera Formation

Geological setting
Material
Methods
Macromorphology
Micromorphology and histology
Comparison with scales of other Teleosteomorpha and other Neopterygii
Findings
Conclusions
Full Text
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