HOME

TheInfoList



OR:

Rhenanida (" Rhine (fish)") is an
order Order, ORDER or Orders may refer to: * Categorization, the process in which ideas and objects are recognized, differentiated, and understood * Heterarchy, a system of organization wherein the elements have the potential to be ranked a number of d ...
of scaly placoderms. Unlike most other placoderms, the rhenanids' armor was made up of a mosaic of unfused scales and tubercles. The patterns and components of this "mosaic" correspond to the plates of armor in other, more advanced placoderms, suggesting that the ancestral placoderm had armor made of unfused components, as well. All rhenanids were flattened,
ray Ray may refer to: Fish * Ray (fish), any cartilaginous fish of the superorder Batoidea * Ray (fish fin anatomy), a bony or horny spine on a fin Science and mathematics * Ray (geometry), half of a line proceeding from an initial point * Ray (g ...
-like, bottom-dwelling predators that lived in marine environments.


Evolution

The rhenanids were once presumed to be the most primitive, or at least the closest to the ancestral placoderm, as their armor was made up of a mosaic of tubercles, as opposed to the solidified plates of "advanced" placoderms, such as antiarchs and arthrodires. Through comparing the skull anatomies of ''Jagorina pandora'' with those of antiarchs, the rhenanids are considered to be the sister group of the antiarchs (together with their respective
Acanthothoracid Acanthothoraci (''spine chests'') is an extinct group of chimaera-like placoderms who were closely related to the rhenanid placoderms. Superficially, the acanthoracids resembled scaly chimaeras, or (relatively) heavily armored ptyctodonts. Th ...
relatives).


Presence in the fossil record

The fossil record of Rhenanida is very sparse, with most fossils being isolated tubercles and skull fragments that are identified as being similar to ''
Gemuendina stuertzi ''Gemuendina stuertzi'' (named for Gemünden from where it was discovered) is a placoderm of the order Rhenanida, of the seas of Early Devonian Germany. In life, ''Gemuendina'' resembled a scaly ray with an upturned head, or a large-finned star ...
'', the most well-known rhenanid, known from several specimens from the Hunsruck slates. Given the rhenanids' worldwide distribution, this paupacity probably did not reflect a scarcity of living individuals (when the order was alive), but reflects the fact that rhenanid armor disintegrated into isolated fragments, and scattered soon after the owner's demise. Most fossils of rhenanids are from the Early
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...
, primarily in the United States and Germany. The recently discovered '' Nefudina qalibahensis'' is known from Northeastern Saudi Arabia. '' Asterosteus stenocephalus'' is known from Mid Devonian Ohio. Another species of rhenanid was '' Bolivosteus chacomensis'', of the Lower to Middle Devonian Malvinokaffric Fauna of Western
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
, in what is now Bolivia, South America. The youngest rhenanid, ''
Jagorina pandora ''Jagorina pandora'' is a rhenanid Rhenanida ("Rhine (fish)") is an order of scaly placoderms. Unlike most other placoderms, the rhenanids' armor was made up of a mosaic of unfused scales and tubercles. The patterns and components of this "m ...
'' is known from Upper Devonian Germany.


Taxonomy

There are five recognized species of rhenanids, in five
genera Genus ( plural genera ) is a taxonomic rank used in the biological classification of living and fossil organisms as well as viruses. In the hierarchy of biological classification, genus comes above species and below family. In binomial nomenclat ...
, ''Asterosteus stenocephalus'', ''Nefudina qalibahensis'', ''Gemuendina stuertzi'', ''Jagorina pandora'', and ''Bolivosteus chacomensis''. They are all placed within the family Asterosteidae, erected by Woodward in 1891: other families attributed to Rhenanida, i.e., Gemuendinidae and Jagorinidae, are considered synonyms. A sixth genus, '' Ohioaspis'', is of questionable status, as the first specimens were ichthyoliths that were originally described as being tubercles from a new species of ''Asterosteus''. Later examinations of these tubercles have led to the formation of two camps of experts, one of which that believe the three recognized species of ''Ohioaspis'' were rhenanids, while the other suggests that they were actually some sort of ostracoderm agnathans.


Timeline of genera

ImageSize = width:1000px height:auto barincrement:15px PlotArea = left:10px bottom:50px top:10px right:10px Period = from:-416 till:-359.2 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:5 start:-416 ScaleMinor = unit:year increment:1 start:-416 TimeAxis = orientation:hor AlignBars = justify Colors = #legends id:CAR value:claret id:ANK value:rgb(0.4,0.3,0.196) id:HER value:teal id:HAD value:green id:OMN value:blue id:black value:black id:white value:white id:paleozoic value:rgb(0.6,0.75,0.55) id:cambrian value:rgb(0.49,0.63,0.33) id:ordovician value:rgb(0,0.57,0.44) id:silurian value:rgb(0.70,0.88,0.71) id:devonian value:rgb(0.8,0.55,0.22) id:earlydevonian value:rgb(0.90,0.71,0.43) id:middledevonian value:rgb(0.96,0.81,0.51) id:latedevonian value:rgb(0.96,0.89,0.71) id:carboniferous value:rgb(0.4,0.65,0.6) id:mississippian value:rgb(0.4,0.56,0.4) id:pennsylvanian value:rgb(0.8,0.77,0.53) id:permian value:rgb(0.94,0.25,0.24) id:mesozoic value:rgb(0.38,0.77,0.79) id:triassic value:rgb(0.51,0.17,0.57) id:jurassic value:rgb(0.2,0.7,0.79) id:cretaceous value:rgb(0.5,0.78,0.31) id:cenozoic value:rgb(0.95,0.98,0.11) id:paleogene value:rgb(0.99,0.6,0.32) id:neogene value:rgb(0.999999,0.9,0.1) id:quaternary value:rgb(0.98,0.98,0.50) BarData= bar:eratop bar:space bar:periodtop bar:space bar:NAM1 bar:NAM2 bar:NAM3 bar:NAM4 bar:NAM5 bar:space bar:period bar:space bar:era PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 shift:(7,-4) bar:periodtop from: -416 till: -411.2 color:earlydevonian text: Lochkovian from: -411.2 till: -407 color:earlydevonian text:
Pragian The Pragian is one of three faunal stages in the Early Devonian Epoch. It lasted from 410.8 ± 2.8 million years ago to 407.6 ± 2.8 million years ago. It was preceded by the Lochkovian Stage and followed by the Emsian Stage. The most important La ...
from: -407 till: -397.5 color:earlydevonian text: Emsian from: -397.5 till: -391.8 color:middledevonian text: Eifelian from: -391.8 till: -385.3 color:middledevonian text: Givetian from: -385.3 till: -374.5 color:latedevonian text: Frasnian from: -374.5 till: -359.2 color:latedevonian text: Famennian bar:eratop from: -416 till: -359.2 color:devonian text:
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...
PlotData= align:left fontsize:M mark:(line,white) width:5 anchor:till align:left color:earlydevonian bar:NAM1 from: -407 till: -403.83 text: Gemuendina color:earlydevonian bar:NAM2 from: -407 till: -385.3 text: Ohioaspis color:middledevonian bar:NAM3 from: -397.5 till: -391.8 text: Asterosteus color:middledevonian bar:NAM4 from: -397.5 till: -385.3 text: Bolivosteus color:latedevonian bar:NAM5 from: -378.1 till: -374.5 text: Jagorina PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 bar:period from: -416 till: -411.2 color:earlydevonian text: Lochkovian from: -411.2 till: -407 color:earlydevonian text:
Pragian The Pragian is one of three faunal stages in the Early Devonian Epoch. It lasted from 410.8 ± 2.8 million years ago to 407.6 ± 2.8 million years ago. It was preceded by the Lochkovian Stage and followed by the Emsian Stage. The most important La ...
from: -407 till: -397.5 color:earlydevonian text: Emsian from: -397.5 till: -391.8 color:middledevonian text: Eifelian from: -391.8 till: -385.3 color:middledevonian text: Givetian from: -385.3 till: -374.5 color:latedevonian text: Frasnian from: -374.5 till: -359.2 color:latedevonian text: Famennian bar:era from: -416 till: -359.2 color:devonian text:
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...


See also

* Batoidea


References


Paleos Rhenanida
* Janvier, Philippe. ''Early Vertebrates'' Oxford, New York: Oxford University Press, 1998. * Long, John A. ''The Rise of Fishes: 500 Million Years of Evolution'' Baltimore: The Johns Hopkins University Press, 1996. * {{Taxonbar, from=Q144336 Prehistoric fish orders Early Devonian first appearances