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Encyclopedia > Placodermi
Placodermi
Fossil range: Early/Mid Silurian - Late Devonian

Conservation status
Extinct (fossil)
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Subphylum: Vertebrata
Infraphylum: Gnathostomata
Class: Placodermi
McCoy, 1848
Orders

Antiarchi
Arthrodira
Brindabellaspida †
Petalichthyida †
Phyllolepida †
Ptyctodontida †
Rhenanida †
Acanthothoraci †
?Pseudopetalichthyida †
?Stensioellida †
The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... For the Celtic language, see Southwestern Brythonic language; for the residents of the English county, see Devon. ... Image File history File links Size of this preview: 501 × 600 pixelsFull resolution (800 × 958 pixels, file size: 366 KB, MIME type: image/jpeg) My reconstruction of various Late Devonian placoderms The gigantic predatory arthrodire Dunkleosteus telleri prepares to seize its smaller cousin, Gorgonichthys clarki, while a school of Ctenurella... The conservation status of a species is an indicator of the likelihood of that species continuing to survive either in the present day or the future. ... For other uses, see Fossil (disambiguation). ... For other uses, see Scientific classification (disambiguation). ... For other uses, see Animal (disambiguation). ... Typical Classes See below Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates. ... This article does not cite any references or sources. ... Classes Placodermi Chondrichthyes Acanthodii Osteichthyes Gnathostomata is the group of vertebrates with jaws. ... In scientific classification used in biology, the order (Latin: ordo, plural ordines) is a rank between class and family (termed a taxon at that rank). ... The Antiarchi (Opposite anus) were the 2nd most successful order of placoderms known, after the Arthrodira. ... For other uses, see Extinction (disambiguation). ... Arthrodira is an order of extinct armored jawed fishes of the Placodermi class who flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. ... Brindabellaspis stensioi (Erik Stensiös Brindabella Ranges Shield) was a long-snouted placoderm from the Early Devonian of the Taemas-Wee Jasper reef in Australia. ... The Petalichthyida was an order of small, flattened placoderm fish. ... Orders Arthrodira † (?sister or containing group) Phyllolepida † The order Phyllolepida (leaf scales) was an order of flattened placoderms found throughout the world, with fossils being found in Devonian strata. ... The Ptyctodontids (Beak-teeth) were a group of unarmored placoderms. ... Genus ?Ohioaspis † Asterosteus † Gemuendina † Jagorina † Bolivosteus † Rhenanida (Rhine (fish)) was an order of primitive, lightly armored (relatively speaking) placoderms. ... Families Weejasperaspididae † Palaeacanthaspidae † // The Acanthothoraci (Spine Chests) were a group of chimaera-like placoderms who were closely related to the rhenanid placoderms. ... Species Pseudopetalichthys problematica† Paraplesiobatis heinrichsi † Nessariostoma granulosa †< The Pseudopetalichthyida was a group of extinct, skate-like fishes known only from rare fossils in Lower Devonian strata in Hunsrück, Germany. ... Stensioella heintzi (Heintzs Little Stensio) was an enigmatic placoderm of arcane affinity. ...

The Placodermi are armoured prehistoric fishes known from fossils dating from the late Silurian to the end of the Devonian Period. Their head and thorax were covered by articulated armoured plates and the rest of the body was scaled or naked, depending on the species. Placoderms were among the first of the jawed fish, their jaws likely evolving from the first of their gill arches. The first identifiable Placoderms evolved in the late Silurian; they then began a dramatic decline during the Late Devonian extinctions, with most species disappearing, until the very end of the Devonian, when the class had gone extinct. The first appearance of late Silurian placoderm fossils, in China, show the fishes already differentiated into Antiarchs and Arthrodires; apparently Placoderm diversity originated long before the Devonian, somewhere in the early to middle Silurian, possibly in China (where the aforementioned Late Silurian fragments have been found), though earlier fossils of basal Placodermi have yet to be discovered in these particular strata. Prehistoric fish are various groups of fishes that lived before recorded history. ... For other uses, see Fossil (disambiguation). ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... For the Celtic language, see Southwestern Brythonic language; for the residents of the English county, see Devon. ... “Human Head” redirects here. ... Diagram of a tsetse fly, showing the head, thorax and abdomen The thorax is a division of an animals body that lies between the head and the abdomen. ... Human jaw front view Human jaw left view Human jaw top view The jaw is either of the two opposable structures forming, or near the entrance to, the mouth. ... For other uses, see Fish (disambiguation). ... For other uses, see Gill (disambiguation). ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... Comparison of the three episodes of extinction in the Late Devonian (Late D) to other mass extinction events in Earths history. ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... The Antiarchi (Opposite anus) were the 2nd most successful order of placoderms known, after the Arthrodira. ... Arthrodira is an order of extinct armored jawed fishes of the Placodermi class who flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. ...

Contents

Fossil record

The first identifiable placoderms left remains that date back to the mid to late Silurian; the placoderms ultimately disappeared in the Late Devonian extinctions. The first appearance of late Silurian placoderm fossils, in China, show the fishes already differentiated into Antiarchs and Arthrodires, along with the other, more primitive groups; apparently Placoderm diversity originated long before the Devonian, somewhere in the middle or early Silurian, though earlier fossils of basal Placodermi, have yet to be discovered in these particular strata. A caveat to the reader: the Silurian fossil record of the placoderms is literally fragmented. All known Silurian placoderms are known only from fragments, either as scraps of armor, or isolated scales, of which some have been tentatively identified as either antiarch or arthrodire due to histological similarities. Although they have been identified, all of the Silurian arthrodire and antiarch species have yet to be formally described or even named. Paradoxically, the best known, or rather, most commonly cited example of an Silurian placoderm, Wangolepis of Silurian China, is known only from a few fragments that currently defy attempts to place them in any of the recognized placoderm orders. The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... Comparison of the three episodes of extinction in the Late Devonian (Late D) to other mass extinction events in Earths history. ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... The Antiarchi (Opposite anus) were the 2nd most successful order of placoderms known, after the Arthrodira. ... Arthrodira is an order of extinct armored jawed fishes of the Placodermi class who flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. ...


Paleontologists and placoderm specialists suspect that the scarcity of the Silurian fossil record of placoderms is so due to placoderms living in environments unconductive to their preservation, rather than a genuine scarcity. This hypothesis helps to explain the placoderms' seemingly miraculous appearance and diversity at the very beginning of the Devonian.


In stark contrast to the Silurian, during the Devonian, the placoderms went on to inhabit and dominate almost all known aquatic ecosystems, both freshwater and saltwater. Despite their dominance, the diversity of the placoderms ultimately suffered many casualties during the extinction event at the Frasnian-Famennian boundary, during the Late Devonian. The rest of the surviving species then died out entirely during the Devonian/Carboniferous extinction event, with not a single species surviving into the Carboniferous. The Frasnian Age is one of two ages in the Late Devonian Period. ... The Famennian Age is one of two ages in the Late Devonian Period. ... In the geological timescale, the Late Devonian epoch (from 385. ... The Carboniferous is a major division of the geologic timescale that extends from the end of the Devonian period, about 359. ...


Ecology and lifestyles

Many placoderms, particularly the Rhenanida, Petalichthyida, Phyllolepida, and Antiarchi, were bottom-dwellers. As such, to paraphrase from what was said in Palaeos, Placodermi has been popularly misinterpreted as being a tribe of bottom-feeding snails and garbage trucks, nevermind that the placoderms were the dominant vertebrate group during the Devonian. One must remember that the vast majority of placoderms were predators, many of which lived at or near the bottom. Many, primarily the Arthrodira were mid- to upperwater dwellers, and were active predators. The largest known arthrodire, Dunkleosteus telleri, was an 8 to 11 meter long predator and was presumed to have a nearly worldwide distribution, as its remains have been found in Europe, North America and Morocco. In fact, it is regarded as the world's first vertebrate super-predator. Other, smaller arthrodires, such as Fallacosteus and Rolfosteus of Gogo, had streamlined, bullet-shaped head armor, strongly crediting the idea that many, if not most, arthrodires were active swimmers, rather than passive ambush-hunters whose armor practically anchored them to the seafloor. Genus ?Ohioaspis † Asterosteus † Gemuendina † Jagorina † Bolivosteus † Rhenanida (Rhine (fish)) was an order of primitive, lightly armored (relatively speaking) placoderms. ... The Petalichthyida was an order of small, flattened placoderm fish. ... Orders Arthrodira † (?sister or containing group) Phyllolepida † The order Phyllolepida (leaf scales) was an order of flattened placoderms found throughout the world, with fossils being found in Devonian strata. ... The Antiarchi (Opposite anus) were the 2nd most successful order of placoderms known, after the Arthrodira. ... This article or section does not cite its references or sources. ... Arthrodira is an order of extinct armored jawed fishes of the Placodermi class who flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. ... Binomial name (Newberry, 1873) Dunkleosteus (formerly known as Dinichthys) was a large Placoderm (armoured prehistoric fish) that lived in the late Devonian period, about 360 – 415 million years ago. ... This article does not cite any references or sources. ... Rolfosteus canningensis is an extinct species of arthrodire placoderm from the late Devonian of the Gogo Reef formation in Australia. ...


It was originally thought that the placoderms went extinct due to competition from the first bony fish, as well as the early sharks, due to a combination of the supposed inherent superiority of the bony fish and sharks, as well as the presumed sluggishness of the placoderms themselves. Since then, though, as more accurate summaries of prehistoric organisms have been developed, it is now presumed that the last placoderms died out one by one as each of their ecological communities suffered due to the environmental catastrophes during the Devonian/Carboniferous extinction event.


Placoderms and specialists

The earliest studies of placoderms were published by Louis Agassiz, in his five volumes on fossil fishes, 1833 – 1843. In those days, the placoderms were thought to be shelled jawless fish akin to ostracoderms. Some naturalists even suggested that they were shelled invertebrates, or even turtle-like vertebrates. The work of Dr. Erik Stensiö, at the Swedish Museum of Natural History, Stockholm, from the late 1920s established the details of placoderm anatomy, and identified them as true jawed fishes related to sharks. He took fossil specimens with well-preserved skulls, and ground them away, one-tenth of a millimeter at a time. Between each grinding, he made an imprint in wax. Once the specimens had been completely ground away (and ironically, completely destroyed as a result), he made enlarged, three-dimensional models of the skulls in order to examine the anatomical details more thoroughly. Many other placoderm specialists suspected that Stensiö was trying to shoehorn placoderms into a relationship with sharks, but with more fossil specimens found, especially the exceptionally well-preserved fossils from the Gogo Reef formation in Australia, Stensiö's theory of sharks and placoderms as sister groups is accepted as fact. Louis Agassiz After the 1906 San Francisco earthquake, Stanford President David Starr Jordan wrote, Somebody—Dr. Angell, perhaps—remarked that Agassiz was great in the abstract but not in the concrete. ... Erik Helge Osvald Stensiö (2 October 1891 – 11 January 1984) was a Swedish paleozoologist. ... The Swedish Museum of Natural History (in Swedish Naturhistoriska riksmuseet), in Stockholm, was founded in 1819 by the Royal Swedish Academy of Sciences, but goes back to the collections acquired mostly through donations by the Academy since its foundation in 1739. ... For other uses, see Shark (disambiguation). ... For other uses, see Shark (disambiguation). ... For other uses, see Fossil (disambiguation). ...


See also

  • Ostracoderm
  • Pterichthyodes - a genus of antiarch placoderm.
  • Gemuendina stuertzi - a species of flattened placoderm
  • Titanichthys agassizi - a species of planktivorous placoderm
  • Dunkleosteus terrelli - a species of giant, carnivorous placoderm
  • Stensioella heintzi - possible placoderm

This article or section does not cite its references or sources. ... Pterichthyodes is a genus of placoderm fishes from the Devonian period, now all extinct. ... The Antiarchi (Opposite anus) were the 2nd most successful order of placoderms known, after the Arthrodira. ... Gemuendina stuertzi (Stuertzs Gemünden (fish)) was an early placoderm species of the order Rhenanida, of the seas of Early Devonian Germany. ... Binomial name Synonyms Brontichthys Titanichthys agassizi was a giant, aberrant marine placoderm from the Late Devonian. ... Binomial name (Newberry, 1873) Synonyms Genus: Dinichthys Ponerichthys Species: Dinichthys canadensis Dunkleosteus (formerly known as Dinichthys) was a large Placoderm (armoured prehistoric fish) that lived in the late Devonian period, about 360 – 415 million years ago. ... Stensioella heintzi (Heintzs Little Stensio) was an enigmatic placoderm of arcane affinity. ...

External links

References

  • Janvier, Philippe. Early Vertebrates Oxford, New York: Oxford University Press, 1998. ISBN 0-19-854047-7
  • Long, John A. The Rise of Fishes: 500 Million Years of Evolution Baltimore: The Johns Hopkins University Press, 1996. ISBN 0-8018-5438-5
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Placodermi

  Results from FactBites:
 
Placodermi - Wikipedia, the free encyclopedia (235 words)
The Placodermi are armoured prehistoric fishes known from fossils dating from the late Silurian to the end of the Devonian Period.
Their head and thorax were covered by articulated armoured plates and the rest of the body was scaled or naked.
Introduction to the Placodermi Extinct armored fishes with jaws
Abebooks Search Results - Placodermi (1060 words)
On the Placodermi of the Upper Devonian of East Greenalnd.
On the Placodermi of the Upper Devonian of East Greenland.
On the Placodermi of the Upper Devonian of East Greenland II.
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