Axelrodichthys

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Axelrodichthys
Temporal range: Albian- early Maastrichtian
~112–71.5  Ma
Axelrodichthys araripensis - Naturmuseum Senckenberg - DSC02202.JPG
Axelrodichthys araripensis
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Sarcopterygii
Class: Actinistia
Order: Coelacanthiformes
Family: Mawsoniidae
Genus: Axelrodichthys
Maisey, 1986
Species
  • A. araripensisMaisey, 1986
  • A. lavocati ? (Tabaste, 1963)
  • A. maiseyiCarvalho et al., 2013
  • A. megadromosCavin et al., 2016

Axelrodichthys is an extinct genus of mawsoniid coelacanth from the Cretaceous of Africa, North and South America, and Europe. Several species are known, the remains of which were discovered in the Lower Cretaceous (Aptian-Albian) of Brazil, [1] North Africa, [2] and possibly Mexico, [3] [4] as well as in the Upper Cretaceous of Morocco (Cenomanian), [5] Madagascar (ConiacianSantonian) [2] and France (Lower Campanian to Lower Maastrichtian). [6] [7] The Axelrodichthys of the Lower Cretaceous frequented both brackish and coastal marine waters (lagoon-coastal environment) while the most recent species lived exclusively in fresh waters (lakes and rivers). [6] [7] The French specimens are the last known fresh water coelacanths. [7] Most of the species of this genus reached 1 metre (3 ft 3 in) to 2 metres (6 ft 7 in) in length. [1] Axelrodichthys was named in 1986 by John G. Maisey in honor of the American ichthyologist Herbert R. Axelrod. [1]

Contents

Description

Axelrodichthys araripensis Axelrodichthys araripensis 1.JPG
Axelrodichthys araripensis

Like its close relative Mawsonia , Axelrodichthys is a coelacanth with an elongated, low, and wide skull, whose skull roof and cheek bones are characterized by strong ornamentation. [7] It differs from Mawsonia mainly in its more elongated parieto nasal shield, the development of the descending process of the supratemporal, and by the shape and arrangement of the cheek and lower jaw bones. On the latter, the two posterior branches of the dentary are similar in length in Axelrodichthys while the lower branch of the bifurcation is much longer than the upper in Mawsonia. The contact area with the angular is also more extensive in Axelrodichthys. [8]

Taxonomy

Several species of Axelrodichthys have been described. The validity of some of them is discussed and other specimens are left in open nomenclature because they are represented by specimens too incomplete for specific determinations. The genus includes the following taxa:

Reconstruction of the skull and head of Axelrodichthys megadromos. A, Braincase in right lateral view with the left suspensorium and lower jaw in medial view; B, skull with suspensorium, cheek and opercular elements in right lateral view; C, skull roof in dorsal view; D, ethmosphenoid portion in ventral view. Axelrodichthys megadromos.jpg
Reconstruction of the skull and head of Axelrodichthys megadromos. A, Braincase in right lateral view with the left suspensorium and lower jaw in medial view; B, skull with suspensorium, cheek and opercular elements in right lateral view; C, skull roof in dorsal view; D, ethmosphenoid portion in ventral view.

Paleoecology

Axelrodichthys lived in different environments depending the species and the time. During the Lower Cretaceous, the species A. araripensis inhabited both brackish and coastal marine waters of western Gondwana. Indeed, the Romualdo Formation, where this species mainly comes from, was deposited in a coastal lagoon influenced by cycles of marine transgressions and regressions and a variable supply of fresh water. [9] At the end of the Upper Cretaceous, the species A. megadromos lived exclusively in fresh water (lakes and rivers), on the Ibero-Armorican island, an insular landmass made up of much of France and the Iberian peninsula. [6] [7] [18] All the sites that yielded this species show no marine influence. Lower Campanian specimens come from lacustrine deposits, and Upper Campanian and Lower Maastrichtian specimens were found in river and floodplain sediments. [19] [6] [7] The remains of Axelrodichthys from the Upper Cretaceous of Morocco and Madagascar also come from freshwater sediments. [5] [2] The arrival of the genus Axelrodichthys in the continental ecosystems of southwestern Europe probably occurred as a result of land connections that provided fluvial links between Europe and Gondwana. [18]

Little is known about the diet of mawsoniids. Although tiny teeth are present on the palate and the inner part of the mandible, the mouths of these fish are mostly toothless. As a result, some authors have speculated that they swallowed their preys using suction, such as the present-day Latimeria . [20] Other scientists have suggested that they may be filter feeders. [20] The description in 2018 of an articulated specimen of A. araripensis that swallowed a whole fish appears to confirm the suction technique. [21]

Phylogeny

A phylogenetic analysis of the mawsoniids published in 2020 found a polytomy grouping together the Cretaceous genera " Lualabaea ", Axelrodichthys, and Mawsonia , as well as the Jurassic marine genus Trachymetopon . The genus "Lualabaea" could be congeneric with Axelrodichthys. [7]

Outgroup

Diplurus

Parnaibaia

Chinlea

Trachymetopon liassicum

"Mawsonia" lavocati

Mawsonia

Axelrodichthys + " Lualabaea "

Related Research Articles

<span class="mw-page-title-main">Coelacanth</span> Order of lobe-finned fishes

Coelacanths are an ancient group of lobe-finned fish (Sarcopterygii) in the class Actinistia. As sarcopterygians, they are more closely related to lungfish and tetrapods than to ray-finned fish.

<i>Sarcosuchus</i> Extinct genus of reptiles

Sarcosuchus is an extinct genus of crocodyliform and distant relative of living crocodilians that lived during the Early Cretaceous, from the late Hauterivian to the early Albian, 133 to 112 million years ago of what is now Africa and South America. The genus name comes from the Greek σάρξ (sarx) meaning flesh and σοῦχος (souchus) meaning crocodile. It was one of the largest pseudosuchians, with the largest specimen of S. imperator reaching approximately 9–9.5 metres (29.5–31.2 ft) long and weighing up to 3.45–4.3 metric tons. It is known from two species; S. imperator from the early Albian Elrhaz Formation of Niger, and S. hartti from the Late Hauterivian of northeastern Brazil. Other material is known from Morocco and Tunisia and possibly Libya and Mali.

<i>Chinlea</i> Extinct genus of coelacanths

Chinlea is an extinct genus of late Triassic Mawsoniid coelacanth fish found in and named after the Chinle Formation that crops out in the southwestern states of Arizona and New Mexico. The word “Chinle” comes from the Navajo word meaning "flowing out", referencing the location where water flows out of the Canyon de Chelly. They were also possibly found in the Dockum Group.

<span class="mw-page-title-main">Latimeriidae</span> Family of fishes

Latimeriidae is the only extant family of coelacanths, an ancient lineage of lobe-finned fish. It contains two extant species in the genus Latimeria, found in deep waters off the coasts of southern Africa and east-central Indonesia. In addition, several fossil genera are known from the Mesozoic of Europe, the Middle East, and the southeastern United States, dating back to the Triassic.

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

Ichthyodectiformes is an extinct order of marine stem-teleost ray-finned fish. The order is named after the genus Ichthyodectes, established by Edward Drinker Cope in 1870. Ichthyodectiforms are usually considered to be some of the closest relatives of the teleost crown group.

<i>Mawsonia</i> (fish) Extinct genus of coelacanths

Mawsonia is an extinct genus of prehistoric coelacanth fish. It is amongst the largest of all coelacanths, with one quadrate specimen possibly belonging to an individual measuring 5.3 metres in length. It lived in freshwater and brackish environments from the late Jurassic to the mid-Cretaceous of South America, eastern North America, and Africa. Mawsonia was first described by British paleontologist Arthur Smith Woodward in 1907.

<i>Holophagus</i> Extinct genus of coelacanths

Holophagus is an extinct genus of coelacanth belonging to Latimeriidae. The type species, Holophagus gulo, is known from the Lower Jurassic marine Lias of England. Some authors have considered the genus restricted to the Lias of England.

<span class="mw-page-title-main">Mawsoniidae</span> Extinct family of coelacanths

Mawsoniidae is an extinct family of prehistoric coelacanth fishes which lived during the Triassic to Cretaceous periods. Members of the family are distinguished from their sister group, the Latimeriidae by the presence of ossified ribs, a coarse rugose texture on the dermatocranium and cheek bones, the absence of the suboperculum and the spiracular, and reduction or loss of the descending process of the supratemporal. Mawsoniids are known from North America, Europe, South America, Africa, Madagascar and Asia. Unlike Latimeriidae, which are exclusively marine, Mawsoniidae were also native to freshwater and brackish environments. Mawsoniids represent among the youngest known coelacanths, with the youngest known remains of the freshwater genus Axelrodichthys from France and an indeterminate marine species from Morocco being from the final stage of the Cretaceous, the Maastrichtian, roughly equivalent in age to the youngest known fossils of latimeriids. Species of Mawsonia and Trachymetopon are known to have exceeded 5 metres in length, making them among the largest known bony fish to have ever existed.

The Yezo Group is a stratigraphic group in Hokkaido, Japan and Sakhalin, Russia which is primarily Late Cretaceous in age. It is exposed as roughly north–south trending belt extending 1,500 kilometres through central Hokkaido from Urakawa to Cape Sōya and Sakhalin from the south coast to Alexandrovsk-Sakhalinsky District. It consists of marine forearc basin sediments, typically turbiditic and bioturbated mudstones and sandstones with subordinate conglomerate primarily deposited on the continental shelf and slope of the ancient Yezo subduction margin. It forms a continuous depositional sequence with the Sorachi Group, which overlies the Horokanai Ophiolite. The sequence gradually shallows upwards with the terminal Hakobuchi Formation representing a fluvial-inner shelf environment.

<span class="mw-page-title-main">Kem Kem Group</span>

The Kem Kem Group is a geological group in the Kem Kem region of eastern Morocco, whose strata date back to the Cenomanian stage of the Late Cretaceous. Its strata are subdivided into two geological formations, with the lower Ifezouane Formation and the upper Aoufous Formation, with the Gara Sbaa Formation and Douira Formation used in the southern Tafilalt region. It is exposed on an escarpment along the Algeria–Morocco border.

Lualabaea is an extinct genus of prehistoric coelacanth, belonging to the family Mawsoniidae, containing the single species L. lerichei. It has been found in Late Jurassic or Berriasian aged deposits in the Democratic Republic of the Congo.

<i>Trachymetopon</i> Extinct genus of fishes

Trachymetopon is an extinct genus of prehistoric coelacanth from the Jurassic of Europe. Fossils have been found in the Early Jurassic Posidonia Shale of Germany the Middle Jurassic Marnes de Dives of France, and probably the Late Jurassic Kimmeridge Clay of England. Only one species has been named, Trachymetopon liassicum, described by Henning in 1951 from an almost complete specimen found in the Lower Toarcian of Ohmden in Baden-Württemberg. Another specimen is known from the same site, and two older specimens come from the Sinemurian of Holzmaden. The holotype of this species is 1.6 metres in length. A giant specimen of an undetermined species of Trachymetopon found at the Middle Jurassic Falaises des Vaches Noires of Normandy. This specimen, composed of a 53 cm long palatoquadrate, belongs to an individual 4 metres (13 ft) in length. A basisphenoid found in a museum in Switzerland that likely originates from the same locaity probably belonged to an individual around 5 m (16 ft) long, making Trachymetopon the largest of all coelacanths alongside Mawsonia. A study published in 2015 revealed that this coelacanth belongs to the Mawsoniidae. Trachymetopon is one of the few known mawsoniids to have been exclusively marine, while most of the other members of the group have lived in fresh and brackish waters.

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<i>Megalocoelacanthus</i> Extinct genus of coelacanths

Megalocoelacanthus dobiei is an extinct species of giant latimeriid coelacanth lobe-finned fish which lived during the Lower Campanian epoch until possibly the early Maastrichtian in the Late Cretaceous period in Appalachia, the Western Interior Seaway and Mississippi Embayment. Its disarticulated remains have been recovered from the Eutaw Formation, Mooreville Chalk Formation, and Blufftown Formation of Alabama, Mississippi, and Georgia, and also from the Niobrara Formation of Kansas. Although no complete skeleton is known, careful examination of skeletal elements demonstrate it is closely related to the Jurassic-aged coelacanthid Libys. The species is named for herpetologist James L. Dobie. It has been estimated to have been 3.5—4.5 meters in length.

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References

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Further reading