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The composition of the caudal skeleton of teleosts (Actinopterygil: Osteichthyes)

Identifieur interne : 001756 ( Istex/Corpus ); précédent : 001755; suivant : 001757

The composition of the caudal skeleton of teleosts (Actinopterygil: Osteichthyes)

Auteurs : Hans-Peter Schultze ; Gloria Arratia

Source :

RBID : ISTEX:6A8863E181E8414BF797B3F98EB27E5B23886FC6

English descriptors

Abstract

The diural caudal skeleton of teleostean actinopterygians develops phylogeneticaily and ontogenetically from a polyural skeleton. The reduction of the polyural anlage to four, three, two or fewer centra in the adult caudal skeleton takes different pathways in different genera (e.g. compare Elops and Albula) and groups of teleosts. As a result, ural centra are not homologous throughout the teleosts. By numbering the ural centra in a homocercal tail in polyural fashion, one can demonstrate these and the following differences. The ventral elements (hypurals) always occur in sequential series, whereas the dorsal elements (epurals and uroneurals) may alter like the ural centra. The number of epurals, five or four in fossil primitive teleosts, is reduced in other primitive and advanced teleosts, but the same epurals are not always lost. The number of uroneurals, seven in fossil teleosts, is reduced in living teleosts, but it has not been demonstrated that the first uroneural is always derived from the neural arch of the same ural centrum. The landmark in the homocercal tail is the preural centrum I which can be identified by (1) bifurcation of the caudal artery and vein in its ventral element, the parhypural, (2) its position directly caudal to the preural centrum (PU2) which supports the lowermost principal caudal ray with its haemal spine, (3) carrying the third hypaxial element ventral to the course of arteria and vena pinnalis, and (4) by carrying the first haemal spine (parhypural) below the dorsal end of the ventral cartilage plate. The study of the development of the vertebral column reveals that teleosts have different patterns of centrum formation. A vertebral centrum is a complete or partial ring of mineralized, cartilaginous or bony material surrounding at least the lateral sides of the notochord. A vertebral centrum may be formed by arcocentrum alone, or arcocentral arcualia and chordacentrum, or arco‐, chorda‐ and autocentrum, or arcocentral arcualia and autocentrum. This preliminary research demonstrates that a detailed ontogenetic interpretation of the vertebral centra and of the caudal skeleton of different teleosts may be useful tools for further interpretations of teleostean interrelationships.

Url:
DOI: 10.1111/j.1096-3642.1989.tb00547.x

Links to Exploration step

ISTEX:6A8863E181E8414BF797B3F98EB27E5B23886FC6

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<affiliation>Museum of Natural History and Department of Systematics and Ecology, The University of Kansas, Lawrence, Kansas 66045‐2245</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">GLORIA</namePart>
<namePart type="family">ARRATIA</namePart>
<affiliation>Museum of Natural History and Department of Systematics and Ecology, The University of Kansas, Lawrence, Kansas 66045‐2245</affiliation>
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<roleTerm type="text">author</roleTerm>
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<typeOfResource>text</typeOfResource>
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<publisher>Blackwell Publishing Ltd</publisher>
<place>
<placeTerm type="text">Oxford, UK</placeTerm>
</place>
<dateIssued encoding="w3cdtf">1989-11</dateIssued>
<edition>Received May 1988, accepted for publication December 1988</edition>
<copyrightDate encoding="w3cdtf">1989</copyrightDate>
</originInfo>
<language>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
</language>
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<internetMediaType>text/html</internetMediaType>
<extent unit="references">114</extent>
</physicalDescription>
<abstract lang="en">The diural caudal skeleton of teleostean actinopterygians develops phylogeneticaily and ontogenetically from a polyural skeleton. The reduction of the polyural anlage to four, three, two or fewer centra in the adult caudal skeleton takes different pathways in different genera (e.g. compare Elops and Albula) and groups of teleosts. As a result, ural centra are not homologous throughout the teleosts. By numbering the ural centra in a homocercal tail in polyural fashion, one can demonstrate these and the following differences. The ventral elements (hypurals) always occur in sequential series, whereas the dorsal elements (epurals and uroneurals) may alter like the ural centra. The number of epurals, five or four in fossil primitive teleosts, is reduced in other primitive and advanced teleosts, but the same epurals are not always lost. The number of uroneurals, seven in fossil teleosts, is reduced in living teleosts, but it has not been demonstrated that the first uroneural is always derived from the neural arch of the same ural centrum. The landmark in the homocercal tail is the preural centrum I which can be identified by (1) bifurcation of the caudal artery and vein in its ventral element, the parhypural, (2) its position directly caudal to the preural centrum (PU2) which supports the lowermost principal caudal ray with its haemal spine, (3) carrying the third hypaxial element ventral to the course of arteria and vena pinnalis, and (4) by carrying the first haemal spine (parhypural) below the dorsal end of the ventral cartilage plate. The study of the development of the vertebral column reveals that teleosts have different patterns of centrum formation. A vertebral centrum is a complete or partial ring of mineralized, cartilaginous or bony material surrounding at least the lateral sides of the notochord. A vertebral centrum may be formed by arcocentrum alone, or arcocentral arcualia and chordacentrum, or arco‐, chorda‐ and autocentrum, or arcocentral arcualia and autocentrum. This preliminary research demonstrates that a detailed ontogenetic interpretation of the vertebral centra and of the caudal skeleton of different teleosts may be useful tools for further interpretations of teleostean interrelationships.</abstract>
<subject lang="en">
<genre>keywords</genre>
<topic>KEY WORDS: ‐Morphology ‐ ontogeny ‐ caudal skeleton ‐ teleosts ‐ actinopterygians ‐ osteichthyans</topic>
</subject>
<relatedItem type="host">
<titleInfo>
<title>Zoological Journal of the Linnean Society</title>
</titleInfo>
<genre type="journal">journal</genre>
<identifier type="ISSN">0024-4082</identifier>
<identifier type="eISSN">1096-3642</identifier>
<identifier type="DOI">10.1111/(ISSN)1096-3642</identifier>
<identifier type="PublisherID">ZOJ</identifier>
<part>
<date>1989</date>
<detail type="volume">
<caption>vol.</caption>
<number>97</number>
</detail>
<detail type="issue">
<caption>no.</caption>
<number>3</number>
</detail>
<extent unit="pages">
<start>189</start>
<end>231</end>
<total>43</total>
</extent>
</part>
</relatedItem>
<identifier type="istex">6A8863E181E8414BF797B3F98EB27E5B23886FC6</identifier>
<identifier type="DOI">10.1111/j.1096-3642.1989.tb00547.x</identifier>
<identifier type="ArticleID">ZOJ189</identifier>
<recordInfo>
<recordContentSource>WILEY</recordContentSource>
<recordOrigin>Blackwell Publishing Ltd</recordOrigin>
</recordInfo>
</mods>
</metadata>
<serie></serie>
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