Tinirau clackae

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Tinirau clackae
Temporal range: Middle Devonian, 387  Ma
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Tinirau clackae.png
Holotype fossil and interpretive drawing of Tinirau clackae
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Sarcopterygii
Clade: Tetrapodomorpha
Clade: Eotetrapodiformes
Genus: Tinirau
Swartz, 2012
Species:
T. clackae
Binomial name
Tinirau clackae
Swartz, 2012
Synonyms

Bruehnopteron murphyiSchultze & Reed (2012)? [1]

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. [2]

Contents

Description

3D reconstruction of T. clackae Tinirau clackae NT.jpg
3D reconstruction of T. clackae

Tinirau was a fairly large, predatory fish about a meter long and with a deep, compact body. The head was large, with large terminal mout and numerous teeth. The tail was heterocercal. The remaining fins with the exception of the pectoral fins were situated behind the middle of the body similar to the situation seen in pikes, giving the animal a large tail surface suitable for great bursts of speed.

It shares many advanced features with later tetrapodomorphs in the pelvic limb bones and glenoids (shoulder sockets). By the time Tinirau appeared, many stem tetrapods had already developed the three major hindlimb bones of tetrapods: the femur, tibia, and fibula. While derived stem tetrapods like Panderichthys had hindlimb configurations very similar to the first land-living tetrapods, some early forms such as Eusthenopteron possessed a prominent postaxial process of the fibula hanging over the fibulare bone below it. Tinirau is the earliest known stem tetrapod to have a significantly reduced postaxial process, and a fibula more like those of later tetrapods. [2]

Like those of the Late Devonian Panderichthys and Ichthyostega , the glenoid of Tinirau is elongated along the anteroposterior (forward-backward) axis of the body. The lengthening of the glenoid corresponds with a flattening of the proximal end of the humerus, a feature common in the forelimbs of more advanced stem tetrapods. Although the pectoral limb bones and girdle were not strong enough to support the weight of Tinirau out of water, glenoid lengthening and other changes to the proximal forelimb were among the first steps in the transformation from pectoral fin to forelimb. [2]

History

Remains of Tinirau were first discovered by paleontologist Joseph T. Gregory in 1970, who then worked for the University of California Berkeley. Gregory and his field team found these fossils near the Simpson Park Mountains in Eureka County, Nevada. They came from a deposit called the Red Hill I beds, which date to the upper Givetian stage of the Middle Devonian. The Red Hill I beds include a series of limestone and mudstone, likely deposited in an outer continental shelf marine environment. Six fossils are known, all preserving bones of the skull. Two fossils preserve postcranial bones in articulation. The holotype specimen, UCMP 118605, is a mostly complete skeleton. [2]

Tinirau clackae was named by paleontologist Brian Swartz in 2012 after Tinirau, who in Polynesian legend is the guardian of ocean life, and whose form is half human and half fish. The connection alludes to the features in Tinirau that are transitional between fish, representing life in the water, and tetrapods, representing life on land. The specific name honors Jennifer A. Clack, an English paleontologist who has made many contributions to the study of stem tetrapods. [2]

Phylogeny

In phylogenetic terms, Tinirau is positioned more crownward, or closer to Tetrapoda, than other stem tetrapods like megalichthyiforms and tristichopterids. In its first description, the phylogenetic analysis of Swartz placed Tinirau as a branch directly connected to the stem of Tetrapoda. In other words, it is a close relative of the lineage leading to land vertebrates (a prehistoric taxon can rarely be identified as an ancestor of another taxon, but is instead considered a side branch in a larger lineage). Eusthenopteron, traditionally considered a direct ancestor of tetrapods, or a close relative of such an ancestor, was placed deep within the family Tristichopteridae, away from the tetrapod stem. Below is a cladogram modified from Swartz (2012) showing the placement of Tinirau: [2]

Tetrapodomorpha  

Kenichthys

Rhizodontidae

Canowindridae

Marsdenichthys

Canowindra

Koharalepis

Beelarongia

Megalichthyiformes

Gogonasus

Gyroptychius

Osteolepis

Medoevia

Megalichthyidae

Eotetrapodiformes
Tristichopteridae

Spodichthys

Tristichopterus

Eusthenopteron

Jarvikina

Cabonnichthys

Mandageria

Eusthenodon

Tinirau

Platycephalichthys

Elpistostegalia

Panderichthys

Tiktaalik

Elpistostege

Elginerpeton

Ventastega

Acanthostega

Ichthyostega

Whatcheeriidae

Colosteidae

Crassigyrinus

Baphetidae

Tetrapoda

Total-group Lissamphibia

Embolomeri

Other stem amniotes

On the other hand, Parfitt et al. (2014) considered it more likely that Tinirau was a member of the family Tristichopteridae. [1]

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>Ichthyostega</i> Extinct genus of tetrapodomorphs

Ichthyostega is an extinct genus of limbed tetrapodomorphs from the Late Devonian of what is now Greenland. It was among the earliest four-limbed vertebrates ever in the fossil record and was one of the first with weight-bearing adaptations for terrestrial locomotion. Ichthyostega possessed lungs and limbs that helped it navigate through shallow water in swamps. Although Ichthyostega is often labelled a 'tetrapod' because of its limbs and fingers, it evolved long before true crown group tetrapods and could more accurately be referred to as a stegocephalian or stem tetrapod. Likewise, while undoubtedly of amphibian build and habit, it is not a true member of the group in the narrow sense, as the first modern amphibians appeared in the Triassic Period. Until finds of other early stegocephalians and closely related fishes in the late 20th century, Ichthyostega stood alone as a transitional fossil between fish and tetrapods, combining fish and tetrapod features. Newer research has shown that it had an unusual anatomy, functioning more akin to a seal than a salamander, as previously assumed.

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

Acanthostega is an extinct genus of stem-tetrapod, among the first vertebrate animals to have recognizable limbs. It appeared in the late Devonian period about 365 million years ago, and was anatomically intermediate between lobe-finned fishes and those that were fully capable of coming onto land.

<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>Hynerpeton</i> Extinct species of amphibian

Hynerpeton is an extinct genus of early four-limbed vertebrate that lived in the rivers and ponds of Pennsylvania during the Late Devonian period, around 365 to 363 million years ago. The only known species of Hynerpeton is H. bassetti, named after the describer's grandfather, city planner Edward Bassett. Hynerpeton is known for being the first Devonian four-limbed vertebrate discovered in the United States, as well as possibly being one of the first to have lost internal (fish-like) gills.

<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.

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

Crassigyrinus is an extinct genus of carnivorous stem tetrapod from the Early Carboniferous Limestone Coal Group of Scotland and possibly Greer, West Virginia.

<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.

<i>Tulerpeton</i> Extinct genus of amphibians

Tulerpeton is an extinct genus of Devonian four-limbed vertebrate, known from a fossil that was found in the Tula Region of Russia at a site named Andreyevka. This genus and the closely related Acanthostega and Ichthyostega represent the earliest tetrapods.

<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.

A limb is a jointed, muscled appendage of a tetrapod vertebrate animal used for weight-bearing, terrestrial locomotion and physical interaction with other objects. The distalmost portion of a limb is known as its extremity. The limbs' bony endoskeleton, known as the appendicular skeleton, is homologous among all tetrapods, who use their limbs for walking, running and jumping, swimming, climbing, grasping, touching and striking.

<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">Stegocephali</span> Clade of tetrapodomorphs

Stegocephali is a clade of vertebrate animals containing all fully limbed tetrapodomorphs. It is equivalent to a broad definition of the superclass Tetrapoda: under this broad definition, the term "tetrapod" applies to any animal descended from the first vertebrate with four limbs each with five digits in the extremity (pentadactyly), rather than fins of their sarcopterygian relatives.

<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">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 Matthew Parfitt; Zerina Johanson; Sam Giles; Matt Friedman (2014). "A large, anatomically primitive tristichopterid (Sarcopterygii: Tetrapodomorpha) from the Late Devonian (Frasnian) Alves Beds, Upper Old Red Sandstone, Moray, Scotland". Scottish Journal of Geology. 50 (1): 79–85. doi:10.1144/sjg2013-013. S2CID   129313060.
  2. 1 2 3 4 5 6 Swartz, B. (2012). "A marine stem-tetrapod from the Devonian of Western North America". PLOS ONE. 7 (3): e33683. doi: 10.1371/journal.pone.0033683 . PMC   3308997 . PMID   22448265.