Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)

Members of the Chondrichthyes (Elasmobranchii and Holocephali) are distinguished by their largely cartilaginous endoskeletons, which comprise an uncalcified core overlain by a mineralized layer; in the Elasmobranchii (sharks, skates, rays) most of this mineralization takes the form of calcified poly...

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Main Authors: Pears, Jacob B., Johanson, Z., Trinajstic, Kate, Dean, M.N., Boisvert, Catherine
Format: Journal Article
Language:English
Published: FRONTIERS MEDIA SA 2020
Subjects:
Online Access:http://purl.org/au-research/grants/arc/LE130100053
http://hdl.handle.net/20.500.11937/87689
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author Pears, Jacob B.
Johanson, Z.
Trinajstic, Kate
Dean, M.N.
Boisvert, Catherine
author_facet Pears, Jacob B.
Johanson, Z.
Trinajstic, Kate
Dean, M.N.
Boisvert, Catherine
author_sort Pears, Jacob B.
building Curtin Institutional Repository
collection Online Access
description Members of the Chondrichthyes (Elasmobranchii and Holocephali) are distinguished by their largely cartilaginous endoskeletons, which comprise an uncalcified core overlain by a mineralized layer; in the Elasmobranchii (sharks, skates, rays) most of this mineralization takes the form of calcified polygonal tiles known as tesserae. In recent years, these skeletal tissues have been described in ever increasing detail in sharks and rays, but those of Holocephali (chimaeroids) have been less well-studied, with conflicting accounts as to whether or not tesserae are present. During embryonic ontogeny in holocephalans, cervical vertebrae fuse to form a structure called the synarcual. The synarcual mineralizes early and progressively, anteroposteriorly and dorsoventrally, and therefore presents a good skeletal structure in which to observe mineralized tissues in this group. Here, we describe the development and mineralization of the synarcual in an adult and stage 36 elephant shark embryo (Callorhinchus milii). Small, discrete, but irregular blocks of cortical mineralization are present in stage 36, similar to what has been described recently in embryos of other chimaeroid taxa such as Hydrolagus, while in Callorhinchus adults, the blocks of mineralization are more irregular, but remain small. This differs from fossil members of the holocephalan crown group (Edaphodon), as well as from stem group holocephalans (e.g., Symmorida, Helodus, Iniopterygiformes), where tesserae are notably larger than in Callorhinchus and show similarities to elasmobranch tesserae, for example with respect to polygonal shape.
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spelling curtin-20.500.11937-876892022-03-03T02:27:55Z Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes) Pears, Jacob B. Johanson, Z. Trinajstic, Kate Dean, M.N. Boisvert, Catherine Science & Technology Life Sciences & Biomedicine Genetics & Heredity Holocephali Callorhinchus tesserae mineralization evolution stem group Holocephali TESSELLATED SKELETON CALCIFIED CARTILAGE SHARKS CALCIFICATION EVOLUTION FEATURES DOGFISH ORIGIN GROWTH FISH Members of the Chondrichthyes (Elasmobranchii and Holocephali) are distinguished by their largely cartilaginous endoskeletons, which comprise an uncalcified core overlain by a mineralized layer; in the Elasmobranchii (sharks, skates, rays) most of this mineralization takes the form of calcified polygonal tiles known as tesserae. In recent years, these skeletal tissues have been described in ever increasing detail in sharks and rays, but those of Holocephali (chimaeroids) have been less well-studied, with conflicting accounts as to whether or not tesserae are present. During embryonic ontogeny in holocephalans, cervical vertebrae fuse to form a structure called the synarcual. The synarcual mineralizes early and progressively, anteroposteriorly and dorsoventrally, and therefore presents a good skeletal structure in which to observe mineralized tissues in this group. Here, we describe the development and mineralization of the synarcual in an adult and stage 36 elephant shark embryo (Callorhinchus milii). Small, discrete, but irregular blocks of cortical mineralization are present in stage 36, similar to what has been described recently in embryos of other chimaeroid taxa such as Hydrolagus, while in Callorhinchus adults, the blocks of mineralization are more irregular, but remain small. This differs from fossil members of the holocephalan crown group (Edaphodon), as well as from stem group holocephalans (e.g., Symmorida, Helodus, Iniopterygiformes), where tesserae are notably larger than in Callorhinchus and show similarities to elasmobranch tesserae, for example with respect to polygonal shape. 2020 Journal Article http://hdl.handle.net/20.500.11937/87689 10.3389/fgene.2020.571694 English http://purl.org/au-research/grants/arc/LE130100053 http://creativecommons.org/licenses/by/4.0/ FRONTIERS MEDIA SA fulltext
spellingShingle Science & Technology
Life Sciences & Biomedicine
Genetics & Heredity
Holocephali
Callorhinchus
tesserae
mineralization
evolution
stem group Holocephali
TESSELLATED SKELETON
CALCIFIED CARTILAGE
SHARKS
CALCIFICATION
EVOLUTION
FEATURES
DOGFISH
ORIGIN
GROWTH
FISH
Pears, Jacob B.
Johanson, Z.
Trinajstic, Kate
Dean, M.N.
Boisvert, Catherine
Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title_full Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title_fullStr Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title_full_unstemmed Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title_short Mineralization of the Callorhinchus Vertebral Column (Holocephali; Chondrichthyes)
title_sort mineralization of the callorhinchus vertebral column (holocephali; chondrichthyes)
topic Science & Technology
Life Sciences & Biomedicine
Genetics & Heredity
Holocephali
Callorhinchus
tesserae
mineralization
evolution
stem group Holocephali
TESSELLATED SKELETON
CALCIFIED CARTILAGE
SHARKS
CALCIFICATION
EVOLUTION
FEATURES
DOGFISH
ORIGIN
GROWTH
FISH
url http://purl.org/au-research/grants/arc/LE130100053
http://hdl.handle.net/20.500.11937/87689