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Romundina

Romundina is a small, heavily armored extinct genus of acanthothoracid placoderms which lived in shallow marine environments in the early Devonian (Lochkovian). The name Romundina honors Canadian geologist and paleontologist Dr. Rómundur (Raymond) Thorsteinsson of Calgary, Alberta, Canada. Romundina are believed to have lived on Earth between 400 and 419 million years ago. The closest known relative to Romundina is the acanthothoracid Radotina. The type and only described species is R. stellina.

Description and paleobiology
Dentition and the evolution of teeth Romundina is currently understood to be the first placoderm to develop primitive tooth-like structures. Originally, teeth were thought to arise following Placodermi but prior to crown Gnathostomata; however, recent research suggests that teeth may have arisen in derived placoderms such as Romundina. There is currently much debate surrounding whether these tooth-like structures as well as the gnathal plates they sit on can be seen as the true primitive condition of Gnathostome dentition. Some researchers see the tooth-like structures of extensions of a primitive crushing plate, which is common in Placoderms. These primitive tooth-like structures lie on supragnathal plates and have a multi-cuspid appearance suggesting some degree of tooth-to-tooth occlusion occurred. Additionally, synchrotron radiation X-ray tomographic microscopy reveals that these tooth-like tubercle structures likely consist of a dentine based core and an enameloid cap common to many extant fish groups; however, they lack internal vascularization. The most prominent of these "bridge" features is the positioning of the nasal capsule dorsally between the eyes, a feature only present in early to mid Placoderms. Romundina has been shown to unambiguously have a jaw, however the cranial anatomy and proportions of the brain are more closely aligned with those of jawless vertebrates. The entirety of Romundina was likely covered in irregularly shaped dermal scales, which is a characteristic unlike the more symmetrical scales that appear on Gnathostomes. Additionally, Romundina likely had a vascular spine which grew posteriorly and proximally from the cranial side of the spine just posterior of the head. This spine likely played a heavily defensive role and grew similarly to how scales grow in Gnathostomes. Furthermore, this defensive spine is made up of semidentine odontodes, dermal bone, and perichondral bone suggesting that it is derived from dermal plates. Diet and behavioral characteristics Romundina were small Placoderms and therefore had to rely on heavily armored skull and anterior sections of their body to fend off larger fish present at the same time. Corals and other shallow water organisms were also found alongside Romundina in the same formation on Prince of Wales Island suggesting that they too lived in relatively shallow water. Their small size is also consistent with a shallow water habitat. Research suggests that Romundina also ate mostly invertebrates such as crustaceans and worms. ''Romundina's large crushing tooth-like structures as well as the large gnathal plates would appear to be useful in eating organisms with hard shells such as crustaceans. Romundina likely did not migrate or swim long distances as all known specimens have been found in a relatively small range of area in Prince of Wales Island. This lack of geographical range also suggests that Romundina'' only lived in a highly specialized ecosystem. Overall, relatively little research has been done on the Paleobiology. == Discovery and classification ==
Discovery and classification
Discovery Romundina was discovered by a Norwegian paleontologist named Tor Ørvig in 1975. The fossil was discovered in rocks collected by geologist Dr. Rómundur Thorsteinsson that were later given to Ørvig to search for fossils. Dr. Thorsteinsson was a pioneer of geology in the Canadian Arctic. While working for the Institute of Sedimentary and Petroleum Geology, Dr. Thorsteinsson came across a formation which dated back to the Gedinnian age and had significant amounts of vertebrate and invertebrate fossils located on the Western part Prince of Wales Island in the Canadian Arctic. The rock sample, which was given to Tor Ørvig to study (and that Romundina was discovered in), was a layer which taken from the middle of a section of unnamed carbonate rocks from the locality C-8234. Ørvig prepared the specimen by using a combination of formic and acetic acid to eat away the rocks, leaving a fully preserved three-dimensional Romundina specimen. Additionally, the average water temperature would have been around 30 °C (86 °F) suggesting that Romundina tended to live in relatively warm waters when compared with the average water temperature today. Major geological formations namely the Reed Bay and Peel Sound Formations lie on the eastern side of the island and have similar fossilized organisms as the unnamed formations on the island's West side. This grade is likely due to an uplifting of rocks from lower Paleozoic and pre-Cambrian eras that exists off the eastern side of the island. As the rocks move westward across the island the sedimentary rock is eroded away revealing fossils from the Silurian and Silurian on the eastern side. Additionally, erosion of more sedimentary rock as it moves towards the west leading to a higher percentage of rock being dolomite then when compared to the eastern side of the formation, which explains the discrepancy in the rock composition across the formation. Classification Romundina is commonly characterized as being in the middle of the Placoderm grade. Much of the structural analysis of Romundina reinforces the hypothesis that Placoderms are a grade rather than a clade as they share characteristics of both crown Cyclostomes and crown Gnathostomes. Structural analysis of the possible tooth like structures tends to place Romundina close to crown Gnathostomes while looking at most of the skull and body structures place Romundina centrally among the Placoderm grade. The location of the nasal capsule on the skull is the most widely agreed upon and definitive feature that is shared among all Romundina stellina specimens yet has variations among the Placoderm grade as a whole and hence is used most often to place Romundina among other Placoderms. The following phylogenetic tree classifies Romundina similar to how they were classified in Dupret et al. (2014) published in Nature. }} == References ==
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