Angustidontus

Last updated

Angustidontus
Temporal range: FrasnianEarly Carboniferous, 380–340  Ma
Angustidontus seriatus.png
Life restoration of A. seriatus
Angustidontus.jpg
Appendage of A. seriatus
Scientific classification
Kingdom:
Phylum:
Subphylum:
Class:
Order:
Family:
Genus:
Angustidontus

Cooper, 1936
Type species
Angustidontus seriatus
Cooper, 1936
Synonyms
  • Angustidontus gracilisCooper, 1936
  • Angustidontus weihmannaeCopeland & Bolton, 1960
  • Angustidontus moravicus Chlupáč  [ cs; de ], 1978

Angustidontus is a genus of predatory pelagic crustaceans from the Late Devonian and Early Carboniferous periods, classified as part of the subclass Eumalacostraca. Fossils of the genus have been recovered in relative abundance from Canada, Germany, the Czech Republic, Poland, Belarus, Ukraine and large parts of the United States, including Oklahoma, Ohio, Indiana, Kentucky, Montana, Utah, Nevada.

Contents

The major eumalacostracan lineages had already diverged from each other during the Devonian, but their early evolutionary history remains relatively unknown due to a poor fossil record, making fossils of Angustidontus and other early eumalacostracans important for scientific study. Historically of uncertain classification, studies on the paleobiology of Angustidontus have allowed researchers to place it between the eumalacostracan orders Amphionidacea and Decapoda.

Description

Angustidontus was a predatory angustidontid crustacean, measuring about 6 centimetres (2.4 inches) in length (9 cm, 3.5 in if the large maxillipeds, that is, appendages or "limbs" used for feeding, are counted). [1] It had one pair of grasping maxillipeds and seven pairs of pereiopods (appendages that acted primarily as walking legs). The first to fifth pair of pereiopods were subchelate (grasping, pincer-like) and short, ending in a hooked and enlarged dactylus (final leg segment, "tip"). The sixth and seventh pairs were thinner and longer, ending in simpler and smaller dactyli. The fifth and sixth pleonal (of the pleon, the abdomen) somites (body segments) expanded laterally, with some partial overlap over the telson (the posteriormost division of the body). [2]

Angustidontus had large grasping appendages, modified from the first or second thoracopods (appendages attached to the thorax), which represent some of the earliest maxillipeds within the Eucarida. These maxillipeds were likely used through being folded downwards to strike at prey, then hold the prey and prevent it from wriggling itself free. [2] Schramidontus , the only known close relative of Angustidontus, also possessed a second smaller pair of maxillipeds that it could use to bring prey to the maxillae, maxillulae (similar structures preceding the maxillae) and its large mandibles, but these are absent in Angustidontus. [2] Instead, Angustidontus used the next four pairs of thoracopods (which were short and possessed strong claws and serrated gnathobases, that is, modified and expanded bases to aid feeding) to tear apart prey and transport it to the mouth. [1]

History of research

The genus Angustidontus was named by American geologist Chalmer Lewis Cooper in 1936, together with the family "Angustidontidae". Cooper described the fossils, consisting of the serrated appendages, as fossil jaws of actinopterygian fish. [3] Since then, the appendages of Angustidontus have been the subject of much debate on its classification. In the 1950s, it was suggested that the fossils instead represented eurypterid chelicerae, possibly of something closely related to Pterygotus . [4]

In 1960, Canadian geologists Murray John Copeland and Thomas Edward Bolton considered the fossils to instead represent gill rakers of fish or be "claws similar to those on the second maxilliped of the stomatopod Squilla "; furthermore, the appendage was noticed to have had some kind of "ball and socket" joint type of articulation. [5] Though it was noted by several prominent researchers that Angustidontus did not likely represent a eurypterid, it was treated as such, albeit with reservations, by most subsequent authors. [1] Exceptions were American geologist Jean Milton Berdan, who concluded in 1964, after studying multiple Angustidontus appendages, that the "rami of Angustidontus are almost certainly part of an arthropod rather than a vertebrate but are not necessarily part of a eurypterid"; and Norwegian paleontologist and geologist Leif Størmer, who agreed in 1966 that the fossils were not eurypterid, but that they "were of uncertain affinity, possibly decapod crustaceans". [6]

Angustidontus often occurs together with Concavicaris , another Devonian crustacean. Concavicaris fossils tend to lack the appendages, whilst Angustidontus fossils often lack the cephalothoracic shield because of its weak sclerotisation. This caused some confusion, and some researchers have suggested that the two would represent different parts of the same animal. [7] Expeditions to fossil localities in Nevada where Concavicaris and Angustidontus were reported to have occurred together by Cooper in 1936 yielded more information on the appendages of Concavicaris and allowed it to be determined that the appendages of Angustidontus did not represent appendages of Concavicaris. With hundreds of specimens being collected, proper research could be conducted on Angustidontus for the first time with the discovery of the first complete specimens. [1]

The new specimens allowed researchers to determine that Angustidontus was a peracarid malacostracan crustacean, and that Concavicaris simply represented a separate animal that was part of a larger Late Devonian fauna including a large amount of different invertebrates, such as worms, cephalopods, bivalves, brachipods and sponges. The appendages which had caused confusion in the past were revealed to be the first thoracopods, but greatly elongated and adapted to be used in feeding. [1]

Classification

A generalized bauplan of a malacostracan crustacean. The cephalon and thorax was fused in Angustidontus as a single cephalothoracic shield and the first thoracopod had developed into a maxilliped. General malacostracan en.svg
A generalized bauplan of a malacostracan crustacean. The cephalon and thorax was fused in Angustidontus as a single cephalothoracic shield and the first thoracopod had developed into a maxilliped.

Angustidontus is classified as part of the extinct family Angustidontidae together with the freshwater genus Schramidontus from Belgium. This family is the only classified as part of the eucarid order Angustidontida. Angustidontids are diagnosed as eucarids that possess carapaces and stalked eyes with scale-like exopods (the external branch of the two comprising a biramous appendage) on the second antennae, an elongated pleion and a tail fan. These features make the group distinct from most eumalacostracan crustaceans and they are classified as part of the Eucarida due to their carapace being fused to thoracic segments 1–7. [2]

Some additional species of Angustidontus other than the type species A. seriatus were previously named. These were A. gracilis (Cooper, 1936), A. moravicus (Chlupáč  [ cs; de ], 1978) and A. weihmannae (Copeland & Bolton, 1960), which were separated from each other by the pattern of the teeth on their maxillipeds. They were all considered synonymous with A. seriatus by British and Polish paleontologists William David Ian Rolfe and Jerzy Dzik in 2006 as fossils of these species presented highly variable patterns. Rolfe and Dzik determined that tooth pattern was not a valid criterion for distinguishing species, with only the type species A. seriatus remaining as valid. Still, based on the morphology of different fossil mandibles, fossil material from the Early Famennian of Poland may represent two possible additional species. [1]

The cladogram below is based on the relationships of the Eucarida assumed by French paleontologists Pierre Guériau, Sylvain Charbonnier and Gaël Clément in 2014, based on the gradual modification of the first thoracopods into the maxillipeds seen in Decapoda. [2]

Eucarida

Euphausiacea

Amphionidacea

Angustidontida

Angustidontus

Schramidontus

Decapoda

Paleoecology

Environment

The life environment of Angustidontus was low in diversity, but might have been very high in biological productivity. Fossil animals found in association with Angustidontus are exclusively open sea pelagic creatures, such as conodonts, cephalopods, ostracods, concavicarids and fish. The bottom regions were likely slightly benthose with a soft and muddy environment; the latter was likely anaerobic and poisonous, with abundant hydrogen sulfide, which would have prevented decomposition and allowed for fossils to be preserved. [1]

Concavicarids, pelagic crustaceans of uncertain classification found in association with Angustidontus, also had chelicerae-like appendages and were covered in protective spines. They were predators, with known stomach contents including cephalopod remains as well as shark and teleost fish vertebrae. The appendages of concavicarids like Concavicaris differed in functionality from those of Angustiodontus and were thus likely used to catch other kinds of prey than what was eaten by Angustidontus. Concavicarids may not only have occupied a different niche, but an entirely different level in the water column. [1]

Prey

There are no taxonomically identifiable gut contents in any Angustidontus specimen. There are some known small fossil pieces found in association to Angustidontus specimens that may represent cephalopod jaws or conches of thin-shelled molluscs. The specimen NMNH 530451 preserves a spiral imprint that might represent the larval conch of a goniatite. Angustidontus might thus have fed on cephalopods. Another likely prey item based on its presence in Late Devonian pelagic environments are conodonts. [1]

See also

Related Research Articles

<span class="mw-page-title-main">Malacostraca</span> Largest class of crustaceans

Malacostraca is the second largest of the six classes of pancrustaceans just behind hexapods, containing about 40,000 living species, divided among 16 orders. Its members, the malacostracans, display a great diversity of body forms and include crabs, lobsters, crayfish, shrimp, krill, prawns, woodlice, amphipods, mantis shrimp, tongue-eating lice and many other less familiar animals. They are abundant in all marine environments and have colonised freshwater and terrestrial habitats. They are segmented animals, united by a common body plan comprising 20 body segments, and divided into a head, thorax, and abdomen.

<span class="mw-page-title-main">Decapoda</span> Order of crustaceans

The Decapoda or decapods are an order of crustaceans within the class Malacostraca, and includes crabs, lobsters, crayfish, shrimp, and prawns. Most decapods are scavengers. The order is estimated to contain nearly 15,000 extant species in around 2,700 genera, with around 3,300 fossil species. Nearly half of these species are crabs, with the shrimp and Anomura including hermit crabs, porcelain crabs, squat lobsters making up the bulk of the remainder. The earliest fossils of the group date to the Devonian.

<span class="mw-page-title-main">Eurypterid</span> Order of arthropods (fossil)

Eurypterids, often informally called sea scorpions, are a group of extinct arthropods that form the order Eurypterida. The earliest known eurypterids date to the Darriwilian stage of the Ordovician period 467.3 million years ago. The group is likely to have appeared first either during the Early Ordovician or Late Cambrian period. With approximately 250 species, the Eurypterida is the most diverse Paleozoic chelicerate order. Following their appearance during the Ordovician, eurypterids became major components of marine faunas during the Silurian, from which the majority of eurypterid species have been described. The Silurian genus Eurypterus accounts for more than 90% of all known eurypterid specimens. Though the group continued to diversify during the subsequent Devonian period, the eurypterids were heavily affected by the Late Devonian extinction event. They declined in numbers and diversity until becoming extinct during the Permian–Triassic extinction event 251.9 million years ago.

<i>Pterygotus</i> Extinct genus of eurypterid

Pterygotus is a genus of giant predatory eurypterid, a group of extinct aquatic arthropods. Fossils of Pterygotus have been discovered in deposits ranging in age from Middle Silurian to Late Devonian, and have been referred to several different species. Fossils have been recovered from four continents; Australia, Europe, North America and South America, which indicates that Pterygotus might have had a nearly cosmopolitan (worldwide) distribution. The type species, P. anglicus, was described by Swiss naturalist Louis Agassiz in 1839, who gave it the name Pterygotus, meaning "winged one". Agassiz mistakenly believed the remains were of a giant fish; he would only realize the mistake five years later in 1844.

<span class="mw-page-title-main">Eucarida</span> Superorder of crustaceans

Eucarida is a superorder of the Malacostraca, a class of the crustacean subphylum, comprising the decapods, krill, and Angustidontida. They are characterised by having the carapace fused to all thoracic segments, and by the possession of stalked eyes.

<i>Hibbertopterus</i> Extinct genus of arthropods

Hibbertopterus is a genus of eurypterid, a group of extinct aquatic arthropods. Fossils of Hibbertopterus have been discovered in deposits ranging from the Devonian period in Belgium, Scotland and the United States to the Carboniferous period in Scotland, Ireland, the Czech Republic and South Africa. The type species, H. scouleri, was first named as a species of the significantly different Eurypterus by Samuel Hibbert in 1836. The generic name Hibbertopterus, coined more than a century later, combines his name and the Greek word πτερόν (pteron) meaning "wing".

<i>Carcinosoma</i> Extinct genus of arthropods

Carcinosoma is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Carcinosoma are restricted to deposits of late Silurian age. Classified as part of the family Carcinosomatidae, which the genus lends its name to, Carcinosoma contains seven species from North America and Great Britain.

<i>Acutiramus</i> Extinct genus of arthropods

Acutiramus is a genus of giant predatory eurypterid, an extinct group of aquatic arthropods. Fossils of Acutiramus have been discovered in deposits of Late Silurian to Early Devonian age. Eight species have been described, five from North America and two from the Czech Republic. The generic name derives from Latin acuto and Latin ramus ("branch"), referring to the acute angle of the final tooth of the claws relative to the rest of the claw.

<i>Jaekelopterus</i> Extinct Devonian genus of the Eurypterida (sea scorpions)

Jaekelopterus is a genus of predatory eurypterid, a group of extinct aquatic arthropods. Fossils of Jaekelopterus have been discovered in deposits of Early Devonian age, from the Pragian and Emsian stages. There are two known species: the type species J. rhenaniae from brackish to fresh water strata in the Rhineland, and J. howelli from estuarine strata in Wyoming. The generic name combines the name of German paleontologist Otto Jaekel, who described the type species, and the Greek word πτερόν (pteron) meaning "wing".

<i>Adelophthalmus</i> Genus of arthropods (fossil)

Adelophthalmus is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Adelophthalmus have been discovered in deposits ranging in age from the Early Devonian to the Early Permian, which makes it the longest lived of all known eurypterid genera, with a total temporal range of over 120 million years. Adelopththalmus was the final genus of the Eurypterina suborder of eurypterids and consisted the only known genus of swimming eurypterids from the Middle Devonian until its extinction during the Permian, after which the few surviving eurypterids were all walking forms of the suborder Stylonurina.

<i>Palmichnium</i>

Palmichnium is an ichnofossil genus, interpreted as a eurypterid trackway. It has been found by many places around the world, such as Australia, Canada, United States and Wales.

<span class="mw-page-title-main">Pterygotidae</span> Extinct family of eurypterids

Pterygotidae is a family of eurypterids, an extinct group of aquatic arthropods. They were members of the superfamily Pterygotioidea. Pterygotids were the largest known arthropods to have ever lived with some members of the family, such as Jaekelopterus and Acutiramus, exceeding 2 metres (6.6 ft) in length. Their fossilized remains have been recovered in deposits ranging in age from 428 to 372 million years old.

Aciculopoda is an extinct prawn which existed in what is now Oklahoma approximately 360 million years ago. It was described in 2010 on the basis of a single fossil from Oklahoma. The single species, Aciculopoda mapesi, was named by Rodney Feldmann and Carrie Schweitzer in honour of Royal Mapes, a paleontologist who discovered the type specimen. It is only the third unambiguous fossil decapod from before the Mesozoic.

Phylogeny of Malacostraca is the evolutionary relationships of the largest of the six classes of crustaceans, containing about 40,000 living species, divided among 16 orders. Its members display a great diversity of body forms. Although the class Malacostraca is united by a number of well-defined and documented features, which were recognised a century ago by William Thomas Calman in 1904, the phylogenetic relationship of the orders which compose this class is unclear due to the vast diversity present in their morphology. Molecular studies have attempted to infer the phylogeny of this clade, resulting in phylogenies which have a limited amount of morphological support. To resolve a well-supported eumalacostracan phylogeny and obtain a robust tree, it will be necessary to look beyond the most commonly utilized sources of data.

<i>Eusarcana</i> Extinct genus of sea scorpions

Eusarcana is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Eusarcana have been discovered in deposits ranging in age from the Early Silurian to the Early Devonian. Classified as part of the family Carcinosomatidae, the genus contains three species, E. acrocephalus, E. obesus and E. scorpionis, from the Silurian-Devonian of Scotland, the Czech Republic and the United States respectively.

<i>Necrogammarus</i> Extinct genus of arthropods

Necrogammarus salweyi is the binomial name applied to an arthropod fossil discovered in Herefordshire, England. The fossil represents a fragmentary section of the underside and an appendage of a pterygotid eurypterid, a group of large and predatory aquatic arthropods that lived from the late Silurian to the late Devonian. The Necrogammarus fossil is Late Silurian in age and its generic name means "dead lobster", deriving from Ancient Greek νεκρός and Latin gammarus ("lobster").

<span class="mw-page-title-main">Angustidontidae</span> Extinct family of crustaceans

Angustidontidae is an extinct family of eucarid crustaceans and the sole representatives of the order Angustidontida. They were predators ranging in size from about 4 to 9 centimetres in length and lived during the Late Devonian and Early Carboniferous periods.

Schramidontus is a genus of crustaceans from the Late Devonian period found in Strud, Belgium, closely related to Angustidontus and classified as part of the order Angustidontida. It is an important genus because of its position in the eumalacostracan family tree and the insight study of the genus may give of the origin of the Decapoda. The generic name derives from Frederick Schram, who helped the scientific community in the field of the Palaeozoic malacostracans and the suffix -idontus in relation to the similarities between Schramidontus and Angustidontus. The specific name is from Labas, a stream that flows near Strud quarry, where the genus was discovered.

<i>Borchgrevinkium</i> Extinct genus of arthropods

Borchgrevinkium is an extinct genus of chelicerate arthropod. A fossil of the single and type species, B. taimyrensis, has been discovered in deposits of the Early Devonian period in the Krasnoyarsk Krai, Siberia, Russia. The name of the genus honors Carsten Borchgrevink, an Anglo-Norwegian explorer who participated in many expeditions to Antarctica. Borchgrevinkium represents a poorly known genus whose affinities are uncertain.

<i>Dvulikiaspis</i> Extinct genus of arthropods

Dvulikiaspis is a genus of chasmataspidid, a group of extinct aquatic arthropods. Fossils of the single and type species, D. menneri, have been discovered in deposits of the Early Devonian period in the Krasnoyarsk Krai, Siberia, Russia. The name of the genus is composed by the Russian word двуликий (dvulikij), meaning "two-faced", and the Ancient Greek word ἀσπίς (aspis), meaning "shield". The species name honors the discoverer of the holotype of Dvulikiaspis, Vladimir Vasilyevich Menner.

References

  1. 1 2 3 4 5 6 7 8 9 Rolfe, William; Dzik, Jerzy (2006). "Angustidontus, a Late Devonian pelagic predatory crustacean". Transactions: Earth Sciences. 97: 75–96. doi:10.1017/S0263593300001413.
  2. 1 2 3 4 5 Guériau, Pierre; Charbonnier, Sylvain; Clément, Gaël (2014). "Angustidontid crustaceans from the Late Devonian of Strud (Namur Province, Belgium): Insights into the origin of Decapoda". Neues Jahrbuch für Geologie und Paläontologie – Abhandlungen . 273: 327–337. doi:10.1127/0077-7749/2014/0434.
  3. Cooper, Chalmer L. (1936). "Actinopterygian Jaws from the Mississippian Black Shales of the Mississippi Valley". Journal of Paleontology . 10 (2): 92–94. JSTOR   1298344.
  4. Raasch, Gilbert O. (1956). "Late Devonian and/or Mississippian faunal succession in Stettler area, Alberta". Journal of the Alberta Society of Petroleum Geologists. 4 (5): 112–118.
  5. Copeland, Murray J.; Bolton, Thomas E. (1960). "The Eurypterida of Canada". Bulletin. Geological Survey of Canada (60): 13–47.
  6. Smith, J. Fred Jr.; Ketner, Keith B. (1975). "Stratigraphy of Paleozoic rocks in the Carlin-Pinon Range area, Nevada". Professional Paper. ISSN   2330-7102.
  7. Koch, Lutz; Gröning, Elke; Brauckmann, Carsten (2003). "Suttropcarididae n. fam. (Phyllocarida, Crustacea) aus dem Ober-Devon des Sauerlandes (Rheinisches Schiefergebirge)". Neues Jahrbuch für Geologie und Paläontologie, Monatshefte (in German). 2003: 415–427.