2001
DOI: 10.1111/j.1095-8649.2001.tb00197.x
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Development of the bony skull in common sole: brief survey of morpho‐functional aspects of ossification sequence

Abstract: The postembryonic development of the bony cephalic skeleton in the common sole Solea solea, observed from hatching to the juvenile stage or postmetamorphic larva, appears to follow a similar chronological order to that observed in other Pleuronectiformes and Perciformes and the sequence in bone formation is a response to functional demands. At hatching, S. solea has no bony structure. On day 4, only the outlines of maxillaries and opercular bones are visible. On day 6, a thin parasphenoid appears between the o… Show more

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Cited by 40 publications
(39 citation statements)
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“…Brewster (1987) proposes an ethmoid/frontal process connection at peak metamorphosis in common sole ( Solea solea ), but it is unclear when this occurs. According to Wagemans & Vandewalle (2001) the frontal primordia are present in the symmetric common sole larvae at 12 days post‐hatching, but do not calcify until day 26 post‐hatch, when the eyes are fully migrated. The frontal processes are not mentioned until post‐metamorphosis when they are fully ossified and in contact with the lateral ethmoids in sole.…”
Section: Discussionmentioning
confidence: 99%
“…Brewster (1987) proposes an ethmoid/frontal process connection at peak metamorphosis in common sole ( Solea solea ), but it is unclear when this occurs. According to Wagemans & Vandewalle (2001) the frontal primordia are present in the symmetric common sole larvae at 12 days post‐hatching, but do not calcify until day 26 post‐hatch, when the eyes are fully migrated. The frontal processes are not mentioned until post‐metamorphosis when they are fully ossified and in contact with the lateral ethmoids in sole.…”
Section: Discussionmentioning
confidence: 99%
“…The incidence of skeletal deformities was determined in the cranium, vertebral column and caudal fin complex of 40 juveniles per replicate (n = 160 per diet) at 50 dph. Skeletal structures were identified and named according to Wagemans and Vandewalle (2001) and Gavaia et al. (2002).…”
Section: Methodsmentioning
confidence: 99%
“…Between 21·5 and 37·2 mm L T (20 and 30 dph), mineralization was observed in the following skeletal elements: the subopercle, supracleithrum, posttemporal, parietal and the dorsal‐scute row. These results are in contrast with those obtained in teleost fishes, which showed earlier mineralization in the above‐mentioned cranial structures (Gluckmann et al ., ; Wagemans & Vandewalle, ). In this study, the initial formation of dorsal, lateral and ventral rudimentary scute rows took place asynchronously with regard to age and fell within the values reported for other acipenserid species.…”
Section: Discussionmentioning
confidence: 99%