Marsdenichthys

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Marsdenichthys
Temporal range: Late Devonian
Scientific classification
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Marsdenichthys

Long, 1985
Species
  • M. longioccipitusLong, 1985 (type)

Marsdenichthys is an extinct genus of Devonian tetrapodomorph. Fossils have been found from Mount Howitt in Victoria, Australia from strata that are Givetian-Frasnian in age. [1] Mount Howitt is an important site that has been the source of many tetrapodomorph fossils, including Beelarongia and Howittichthys , both of which were first described from the locality. [2] [3]

Specimens of Marsdenichthys have been found from Mount Howitt. Mount-howitt-summit.jpg
Specimens of Marsdenichthys have been found from Mount Howitt.

Marsdenichthys was first named in 1985 on the basis of material collected from Mount Howitt. The genus was initially described as a member of the family Eusthenopteridae (now known as the Tristichopteridae), the first known from the southern hemisphere. [4] However, the classification of Marsdenichthys within Tetrapodomorpha has often been debated and there is not yet a consensus on the exact phylogenetic relationships of the genus. [1]

Classification

When it was originally described as a tristichopterid by Long (1985), Marsdenichthys was considered to be the basalmost member of the family, based on such characters as the presence of extratemporal bones, the size ratio between the parietals and postparietals, and the presence of rounded scales with an internal median boss. [4] At the time, this feature was thought to be unique to tristichopterids, but Long suggested that Marsdenichthys could be considered a specialized "osteolepidid" if the scale morphology was later found to be present in members of the family. Osteolepididae is now known to be paraphyletic along with the superorder Osteolepiformes, [5] but several "non-tristichopterid osteolepiformes" have since been found with the scale morphology previously seen only in Marsdenichthys. These include the genera Medoevia , Canowindra , and Rhizodopsis . [1]

Based on scale ornamentation, Marsdenichthys was assigned to the family Rhizodopsidae by Long (1999). [6] However, the only phylogenetic analyses that included Marsdenichthys either placed it with Eusthenopteron in a clade within a monophyletic Osteolepiformes, [7] a polytomy with Eusthenopteron basal to Megalichthys , [8] or a polytomy basal to Medoevia and Gogonasus . [9] It is possible that the classification of Marsdenichthys remains unresolved because there is a lack of derived characters in the incomplete Mount Howitt specimens. However, Holland et al. (2010) recently described new specimens from Mount Howitt that preserve previously unknown derived characters, mainly in the cheek and palate. [1] However, because Holland et al. (2010) did not provide a phylogenetic analysis using the new specimens, the classification of Marsdenichthys remains unresolved.

Related Research Articles

<span class="mw-page-title-main">Tetrapod</span> Superclass of the first four-limbed vertebrates and their descendants

A tetrapod is any four-limbed vertebrate animal of the superclass Tetrapoda. Tetrapods include all extant and extinct amphibians and amniotes, with the latter in turn evolving into two major clades, the sauropsids and synapsids. Some tetrapods such as snakes, legless lizards, and caecilians had evolved to become limbless via mutations of the Hox gene, although some do still have a pair of vestigial spurs that are remnants of the hindlimbs.

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

Sarcopterygii — sometimes considered synonymous with Crossopterygii — is a taxon of the bony fish known as the lobe-finned fish or sarcopterygians, characterised by prominent muscular limb buds (lobes) within the 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 (lepidotrichia) supporting the fins.

<i>Eusthenopteron</i> Extinct genus of tetrapodomorphs

Eusthenopteron is a genus of prehistoric sarcopterygian which has attained an iconic status from its close relationships to tetrapods. Early depictions of this animal show it emerging onto land; however, paleontologists now widely agree that it was a strictly aquatic animal. The genus Eusthenopteron is known from several species that lived during the Late Devonian period, about 385 million years ago. Eusthenopteron was first described by J. F. Whiteaves in 1881, as part of a large collection of fishes from Miguasha, Quebec. Some 2,000 Eusthenopteron specimens have been collected from Miguasha, one of which was the object of intensely detailed study and several papers from the 1940s to the 1990s by paleoichthyologist Erik Jarvik.

<i>Panderichthys</i> Genus of fishes (fossil)

Panderichthys is a genus of extinct sarcopterygian from the late Devonian period, about 380 Mya. Panderichthys, which was recovered from Frasnian deposits in Latvia, is represented by two species. P. stolbovi is known only from some snout fragments and an incomplete lower jaw. P. rhombolepis is known from several more complete specimens. Although it probably belongs to a sister group of the earliest tetrapods, Panderichthys exhibits a range of features transitional between tristichopterid lobe-fin fishes and early tetrapods. It is named after the German-Baltic paleontologist Christian Heinrich Pander. Possible tetrapod tracks dating back to before the appearance of Panderichthys in the fossil record were reported in 2010, which suggests that Panderichthys is not a direct ancestor of tetrapods, but nonetheless shows the traits that evolved during the fish-tetrapod evolution

<i>Hyneria</i> Extinct genus of tetrapodomorphs from the Devonian

Hyneria is a genus of large prehistoric predatory lobe-finned fish which lived in freshwater during the Devonian period (Famennian).

<i>Tiktaalik</i> Genus of extinct lobe-finned fish

Tiktaalik is a monospecific genus of extinct sarcopterygian from the Late Devonian Period, about 375 Mya, having many features akin to those of tetrapods. Tiktaalik is estimated to have had a total length of 1.25–2.75 metres (4.1–9.0 ft) based on various specimens.

<span class="mw-page-title-main">Tetrapodomorpha</span> Clade of vertebrates

The Tetrapodomorpha are a clade of vertebrates consisting of tetrapods and their closest sarcopterygian relatives that are more closely related to living tetrapods than to living lungfish. Advanced forms transitional between fish and the early labyrinthodonts, such as Tiktaalik, have been referred to as "fishapods" by their discoverers, being half-fish, half-tetrapods, in appearance and limb morphology. The Tetrapodomorpha contains the crown group tetrapods and several groups of early stem tetrapods, which includes several groups of related lobe-finned fishes, collectively known as the osteolepiforms. The Tetrapodomorpha minus the crown group Tetrapoda are the stem Tetrapoda, a paraphyletic unit encompassing the fish to tetrapod transition.

<span class="mw-page-title-main">Tristichopteridae</span> Extinct family of fishes

Tristichopterids (Tristichopteridae) were a diverse and successful group of tetrapodomorph fishes living throughout the Middle and Late Devonian. They first appeared in the Eifelian stage of the Middle Devonian. Within the group sizes ranged from a few tens of centimeters (Tristichopterus) to several meters.

Kenichthys is a genus of sarcopterygian fish from the Devonian period, and a member of the clade Tetrapodomorpha. The only known species of the genus is Kenichthys campbelli, the first remains of which were found in China in 1993. The genus is important to the study of the evolution of tetrapods due to the unique nature of its nostrils, which provide vital evidence regarding the evolutionary transition of fish-like nostrils to the tetrapod choanae.

<span class="mw-page-title-main">Rhizodontida</span> Extinct order of tetrapodomorphs

Rhizodontida is an extinct group of predatory tetrapodomorphs known from many areas of the world from the Givetian through to the Pennsylvanian - the earliest known species is about 377 million years ago (Mya), the latest around 310 Mya. Rhizodonts lived in tropical rivers and freshwater lakes and were the dominant predators of their age. They reached huge sizes - the largest known species, Rhizodus hibberti from Europe and North America, was an estimated 7 m in length, making it the largest freshwater fish known.

<i>Gogonasus</i> Extinct genus of tetrapodomorphs

Gogonasus was a lobe-finned fish known from three-dimensionally preserved 380-million-year-old fossils found from the Gogo Formation in Western Australia. It lived in the Late Devonian period, on what was once a 1,400-kilometre coral reef off the Kimberley coast surrounding the north-west of Australia. Gogonasus was a small fish reaching 30–40 cm (1 ft) in length.

<i>Eusthenodon</i> Extinct genus of tetrapodomorphs

Eusthenodon is an extinct genus of tristichopterid tetrapodomorphs from the Late Devonian period, ranging between 383 and 359 million years ago. They are well known for being a cosmopolitan genus with remains being recovered from East Greenland, Australia, Central Russia, South Africa, Pennsylvania, and Belgium. Compared to the other closely related genera of the Tristichopteridae clade, Eusthenodon was one of the largest lobe-finned fishes and among the most derived tristichopterids alongside its close relatives Cabonnichthys and Mandageria.

<i>Tristichopterus</i>

Tristichopterus, with a maximum length of sixty centimetres, is the smallest genus in the family of prehistoric lobe-finned fish, Tristichopteridae that was believed to have originated in the north and dispersed throughout the course of the Upper Devonian into Gondwana. Tristichopterus currently has only one named species, first described by Egerton in 1861. The Tristichopterus node is thought to have originated during the Givetian part of the Devonian. Tristichopterus was thought by Egerton to be unique for its time period as a fish with ossified vertebral centers, breaking the persistent notochord rule of most Devonian fish but this was later reinspected and shown to be only partial ossification by Dr. R. H. Traquair. Tristichopterus alatus closely resembles Eusthenopteron and this sparked some debate after its discovery as to whether it was a separate taxon.

<span class="mw-page-title-main">Osteolepiformes</span> Extinct order of fishes

Osteolepiformes, also known as Osteolepidida, is a group of prehistoric lobe-finned fishes which first appeared during the Devonian period. The order contains the families Canowindridae, Megalichthyidae, Osteolepididae and Tristichopteridae. The order is generally considered to be paraphyletic because the characters that define it are mainly attributes of stem tetrapodomorphs.

<span class="mw-page-title-main">Elpistostegalia</span> Clade of tetrapodomorphs

Elpistostegalia or Panderichthyida is an order of prehistoric lobe-finned fishes which lived during the Middle Devonian to Late Devonian period. They represent the advanced tetrapodomorph stock, the fishes more closely related to tetrapods than the osteolepiform fishes. The earliest elpistostegalians, combining fishlike and tetrapod-like characters, are sometimes called fishapods, a phrase coined for the advanced elpistostegalian Tiktaalik. Through a strict cladistic view, the order includes the terrestrial tetrapods.

<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.

<span class="mw-page-title-main">Osteolepididae</span> Paraphyletic family of tetrapodomorphs

Osteolepididae is a family of primitive, fish-like tetrapodomorphs that lived during the Devonian period. The family is generally thought to be paraphyletic, with the traits that characterise the family being widely distributed among basal tetrapodomorphs and other osteichthyans. Some of genera historically placed in Osteolepididae have more recently been assigned to the family Megalichthyidae, which appears to be a monophyletic group.

<i>Tinirau clackae</i> Extinct species of tetrapodomorph

Tinirau is an extinct genus of sarcopterygian fish from the Middle Devonian of Nevada. Although it spent its entire life in the ocean, Tinirau is a stem tetrapod close to the ancestry of land-living vertebrates in the crown group Tetrapoda. Relative to more well-known stem tetrapods, Tinirau is more closely related to Tetrapoda than is Eusthenopteron, but farther from Tetrapoda than is Panderichthys. The type and only species of Tinirau is T. clackae, named in 2012.

<span class="mw-page-title-main">Eotetrapodiformes</span> Clade of tetrapodomorphs

Eotetrapodiformes is a clade of tetrapodomorphs including the four-limbed vertebrates and their closest finned relatives, two groups of stem tetrapods called tristichopterids and elpistostegalids.


Innovations conventionally associated with terrestrially first appeared in aquatic elpistostegalians such as Panderichthys rhombolepis, Elpistostege watsoni, and Tiktaalik roseae. Phylogenetic analyses distribute the features that developed along the tetrapod stem and display a stepwise process of character acquisition, rather than abrupt. The complete transition occurred over a period of 30 million years beginning with the tetrapodomorph diversification in the Middle Devonian.

References

  1. 1 2 3 4 Holland, T.; Long, J.; Snitting, D. (2010). "New information on the enigmatic tetrapodomorph fish Marsdenichthys longioccipitus (Long, 1985)". Journal of Vertebrate Paleontology. 30 (1): 68–77. Bibcode:2010JVPal..30...68H. doi: 10.1080/02724630903409105 .
  2. Long, J. A. (1987). "An unusual osteolepiform fish from the Late Devonian of Victoria, Australia". Palaeontology. 30: 839–852.
  3. Long, J. A.; Holland, T. (2008). "A possible elpistostegalid from the Devonian of Gondwana". Proceedings of the Royal Society of Victoria. 120: 182–192.
  4. 1 2 Long, J. (1985). "The structure and relationships of a new osteolepiform fish from the Late Devonian of Victoria, Australia". Alcheringa. 9: 1–22. doi:10.1080/03115518508618955.
  5. Ahlberg, P. E.; Johanson, Z. (1998). "Osteolepiforms and the ancestry of tetrapods". Nature. 395 (6704): 792–794. Bibcode:1998Natur.395..792A. doi:10.1038/27421. S2CID   4430783.
  6. Long, J. A. (1999). "A new genus of fossil coelacanth (Osteichthyes: Coelacanthiformes) from the Middle Devonian of southeastern Australia". Records of the Western Australian Museum. Supplement 57: 37–53.
  7. Cloutier, R.; Ahlberg, P. E. (1995). "Sarcopterygian interrelationships: How far are we from a phylogenetic consensus?". Geobios. 28: 241–248. Bibcode:1995Geobi..28..241C. doi:10.1016/s0016-6995(95)80121-9.
  8. Long, J. A.; Young, G. C.; Holland, T.; Senden, T. J.; Fitzgerald, E. M. G. (2006). "An exceptional Devonian fish from Australia sheds light on tetrapod origins". Nature. 444 (7116): 199–202. Bibcode:2006Natur.444..199L. doi:10.1038/nature05243. PMID   17051154. S2CID   2412640.
  9. Holland, T.; Long, J. A. (2009). "On the phylogenetic position of Gogonasus andrewsae Long 1985, within the Tetrapodomorpha". Acta Zoologica. 90 (Supplement 1): 285–296. doi:10.1111/j.1463-6395.2008.00377.x.