Cosmine

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Cosmine is a spongy, bony material that makes up the dentine-like layers in the scales of the lobe-finned fishes of the class Sarcopterygii. Fish scales that include layers of cosmine are known as cosmoid scales . [1]

Contents

Description

As traditionally described, [2] cosmine consists of a layer of dentine covered by a continuous sheet of enamel. Pulp cavities, which secrete dentine tubules, are surrounded by a complex polygonal network of 'pore cavities' which pierce the overlying enamel layer, giving cosmine its characteristic dotted appearance. [3] The pulp cavities and pore chambers are connected by a complex, reticulated pore canal network which continues into a layer of vascular bone beneath the dentine. The exact configuration of the pore canal network and shape of the pore chambers differs between various taxa, although the general organization into a single layer of enamel over dentine with pore canals with vascular bone underneath remains consistent, at least within the Sarcopterygii. [3]

History

Cosmine was first described in the Osteolepiform Megalichthys hibberti by Williamson in 1849, in a purely descriptive, pre-Darwinian, non-evolutionary framework. [4] Goodrich [5] expanded on Williamson's descriptions, hypothesizing a transition from a monoodontode scale (like a chondryicthian placoid scale) to a complex polyodontode scale through fusion of discrete units. Gross' 1956 monograph [3] provided the most elaborate description of cosmoid tissues detailing differences between the shape and configuration of pore canals within different clades of lobe finned fishes. Further descriptions of cosmine growth and development were advanced by Tor Ørvig, [6] dealing specifically with the pattern of squamation, or scale formation across the body of a fish. Ørvig rationalized the observed patterns of cosmine in the fossil record with putative losses of the tissue in coelacanths and extant lungfish [6] proposing that coelacanths, for example, retained a juvenile scale morphology through pedomorphosis. Keith Thomson later analyzed specific growth structures on the cosmine sheet- 'blisters' or 'islands' where cosmine had broken down, and deduced an electroceptive function for the pore chambers. Comparisons with electroceptive organs in extant sarcopterygians, however, have contradicted Thomson's functional hypothesis. [7]

Phylogenetics

New fossils from China have altered current understanding of early fish evolution. Many of these fossils have been identified on the basis of histological characteristics, such as Meemannia eos, classified as an early diverging sarcopterygian on the basis of a pore canal system similar to cosmine. [8] However, later studies on cranial characters [9] have indicated that Meemannia is likely a basal actinopterygian. Newer imaging studies [10] including synchrotron tomography show that pore canal systems in association with dentine occur outside the crown sarcopterygian clade, implying an older synapomorphy of Osteichthyes as opposed to a definitive sarcopterygian trait. The exact phylogenetic significance of cosmine (as classically described) remains unclear.

See also

Related Research Articles

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Chondrichthyes is a class of jawed fish that contains the cartilaginous fish or chondrichthyans, which all have skeletons primarily composed of cartilage. They can be contrasted with the Osteichthyes or bony fish, which have skeletons primarily composed of bone tissue. Chondrichthyes are aquatic vertebrates with paired fins, paired nares, placoid scales, conus arteriosus in the heart, and a lack of opercula and swim bladders. Within the infraphylum Gnathostomata, cartilaginous fishes are distinct from all other jawed vertebrates.

<span class="mw-page-title-main">Osteichthyes</span> Diverse group of fish with skeletons of bone rather than cartilage

Osteichthyes, also known as osteichthyans or commonly referred to as the bony fish, is a diverse superclass of vertebrate animals that have endoskeletons primarily composed of bone tissue. They can be contrasted with the Chondrichthyes and the extinct placoderms and acanthodians, which have endoskeletons primarily composed of cartilage. The vast majority of extant fish are members of Osteichthyes, being an extremely diverse and abundant group consisting of 45 orders, over 435 families and 28,000 species. It is the largest class of vertebrates in existence today, encompassing most aquatic vertebrates, as well as all semi-aquatic and terrestrial vertebrates.

<span class="mw-page-title-main">Scale (zoology)</span> Small rigid plate that grows out of an animals skin

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<span class="mw-page-title-main">Lungfish</span> A type of lobefinned fishes

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<span class="mw-page-title-main">Sarcopterygii</span> Class of fishes

Sarcopterygii — sometimes considered synonymous with Crossopterygii — is a clade of vertebrate animals which includes a group of bony fish commonly referred to as lobe-finned fish. These vertebrates are characterised by prominent muscular limb buds (lobes) within their fins, which are supported by articulated appendicular skeletons. This is in contrast to the other clade of bony fish, the Actinopterygii, which have only skin-covered bony spines supporting the fins.

<span class="mw-page-title-main">Dentin</span> Calcified tissue of the body; one of the four major components of teeth

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<i>Psarolepis</i> Extinct genus of fishes

Psarolepis is a genus of extinct bony fish which lived around 397 to 418 million years ago. Fossils of Psarolepis have been found mainly in South China and described by paleontologist Xiaobo Yu in 1998. It is not known certainly in which group Psarolepis belongs, but paleontologists agree that it probably is a basal genus and seems to be close to the common ancestor of lobe-finned and ray-finned fishes. In 2001, paleontologist John A. Long compared Psarolepis with onychodontiform fishes and refer to their relationships.

<i>Styloichthys</i> Extinct genus of fishes

Styloichthys is a prehistoric sarcopterygian, lobe-finned fish which lived during the Early Devonian (Lochkovian) period of East Yunnan, South China.

Andreolepis is an extinct genus of prehistoric fish, which lived around 420 million years ago. It was described by Walter Gross in 1968 based on scales found in the Hemse Formation in Gotland, Sweden. It is placed in the monogeneric family Andreolepididae and is generally regarded as a primitive member of the class Actinopterygii based on its ganoid scale structure; however some new research regards it as a stem group of osteichthyans.

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<span class="mw-page-title-main">Megalichthyidae</span> Extinct family of tetrapodomorphs

Megalichthyidae is an extinct family of tetrapodomorphs which lived from the Middle–Late Devonian to the Early Permian. They are known primarily from freshwater deposits, mostly in the Northern Hemisphere, but one genus (Cladarosymblema) is known from Australia, and the possible megalichthyid Mahalalepis is from Antarctica.

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<span class="mw-page-title-main">Fish scale</span> Rigid covering growing atop a fishs skin

A fish scale is a small rigid plate that grows out of the skin of a fish. The skin of most jawed fishes is covered with these protective scales, which can also provide effective camouflage through the use of reflection and colouration, as well as possible hydrodynamic advantages. The term scale derives from the Old French escale, meaning a shell pod or husk.

<span class="mw-page-title-main">Fish fin</span> Bony skin-covered spines or rays protruding from the body of a fish

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<span class="mw-page-title-main">Ganoine</span> Fish scale covering

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References

  1. Schultze, Hans-Peter (2016-01-01). "Scales, Enamel, Cosmine, Ganoine, and Early Osteichthyans". Comptes Rendus Palevol. 15 (1–2): 83–102. doi: 10.1016/j.crpv.2015.04.001 . ISSN   1631-0683.
  2. Williamson, W. C. (1849). "On the Microscopic Structure of the Scales and Dermal Teeth of Some Ganoid and Placoid Fish". Philosophical Transactions of the Royal Society of London. 139: 435–475. Bibcode:1849RSPT..139..435W. doi: 10.1098/rstl.1849.0023 . JSTOR   108487.
  3. 1 2 3 (geologist.), Walter Gross (1956). Über Crossopterygier und Dipnoer aus dem baltischen Oberdevon im Zusammenhang einer vergleichenden Untersuchung des Porenkanalsystems paläozoischer Agnathen und Fische (in German). Almqvist & Wiksell.
  4. Donoghue, Philip C.J. "Evolution of Development of the Vertebrate Dermal and Oral Skeletons: Unraveling Concepts, Regulatory Theories, and Homologies" (PDF).[ permanent dead link ]
  5. Goodrich, Edwin S. (1907-05-01). "On the Scales of Fish, Living and Extinct, and their importance in Classification". Proceedings of the Zoological Society of London. 77 (4): 751–773. doi:10.1111/j.1469-7998.1907.tb06953.x. ISSN   1469-7998.
  6. 1 2 Ørvig, Tor (1969-09-01). "Cosmine and Cosmine Growth". Lethaia. 2 (3): 241–260. doi:10.1111/j.1502-3931.1969.tb01850.x. ISSN   1502-3931.
  7. Bemis, William; Glenn Northcutt, R (2010-04-22). "Skin and Blood Vessels of the Snout of the Australian Lungfish, Neoceratodus forsteri, and their Significance for Interpreting the Cosmine of Devonian Lungfishes". Acta Zoologica. 73 (2): 115–139. doi: 10.1111/j.1463-6395.1992.tb00956.x .
  8. Zhu, Min; Yu, Xiaobo; Wang, Wei; Zhao, Wenjin; Jia, Liantao (2006). "A primitive fish provides key characters bearing on deep osteichthyan phylogeny". Nature. 441 (7089): 77–80. Bibcode:2006Natur.441...77Z. doi:10.1038/nature04563. ISSN   1476-4687. PMID   16672968. S2CID   1840338.
  9. Lu, Jing; Giles, Sam; Friedman, Matt; den Blaauwen, Jan L.; Zhu, Min (2016-06-20). "The Oldest Actinopterygian Highlights the Cryptic Early History of the Hyperdiverse Ray-Finned Fishes". Current Biology. 26 (12): 1602–1608. doi: 10.1016/j.cub.2016.04.045 . ISSN   0960-9822. PMID   27212403.
  10. Qu, Qingming; Sanchez, Sophie; Zhu, Min; Blom, Henning; Ahlberg, Per Erik (2017-05-01). "The origin of novel features by changes in developmental mechanisms: ontogeny and three-dimensional microanatomy of polyodontode scales of two early osteichthyans". Biological Reviews. 92 (2): 1189–1212. doi:10.1111/brv.12277. ISSN   1469-185X. PMID   27194072. S2CID   3497774.

Further reading