Coronodon

Last updated

Coronodon
Temporal range: Oligocene
~(Rupelian-Chattian),
~30–23.5  Ma
Coronodon anterolateral at Mace Brown Museum of Natural History.jpg
Coronodon anterolateral at Mace Brown Museum of Natural History
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Artiodactyla
Infraorder: Cetacea
Parvorder: Mysticeti
Genus: Coronodon
Geisler et al., 2017
Type species
Coronodon havensteini
Geisler et al., 2017
Other species
  • C. newtonorumBoessenecker et al., 2023
  • C. planifronsBoessenecker et al., 2023

Coronodon (meaning "crown tooth") is a genus of toothed (transitional) baleen whales from the Early Oligocene Ashley and Chandler Bridge formations of South Carolina. The genus contains three species: the type species C. havensteini, and additional species C. newtonorum and C. planifrons.

Contents

Description

Skeletal composite and size of Coronodon compared to a scuba diver Coronodon skeletal.png
Skeletal composite and size of Coronodon compared to a scuba diver

It was about the same size as Dorudon , measuring 4.9 m (16 ft) long and weighing 1,150 kg (2,540 lb). The rostrum of Coronodon is wide, judging by its straight sides and short mandibular symphysis. Despite being similar to some archaeocetes in having a rostrum that is twisted counterclockwise in anterior view, it differs in having posterior teeth with subequal cusps and an upturned anterior process of the maxilla. Coronodon differs from other toothed mysticetes in having anterior lower molars labially overlapping posterior lower molars. [1] [2]

Classification

Coronodon falls basally within Mysticeti, being closely related to the unnamed taxon ChM PV 5720 and more primitive than "Metasqualodon" symmetricus, Aetiocetidae, Mammalodontidae and Llanocetus . [1] [2]

Paleoecology

Coronodon is very unusual among archaic toothed mysticetes due to its dentition. The incisors are caniniform, and the wear patterns on both the incisors and the P2 (second premolar on the right side of the mandible) indicate that this whale was well suited to capturing larger prey items and piercing flesh. This sort of dentition is common in basilosaurid whales, who fed utilizing exclusively pursuit predation. However, Coronodon differs from its ancestors in that the molars possess more cusps and are more tightly packed together. The molars also have reduced support from the alveolar bone, and the apices of the three main cusps on the molars and premolars meet one another at a 155° angle in the upper and lower jaws, opposed to an 82° and a 98° angle in Cynthiacetus and Dorudon respectively. [1] This would have diminished the shearing capabilities of the molars. The lack of oral processing occurring in the molar region is further evident by wear patterns on the labial side of the teeth, but little to no wear close to the cutting surfaces. [1] This is unlike the molar teeth of basilosaurids, which possess wear patterns indicative of shearing flesh at the back of the mouth.

In its initial description, Coronodon was implied to have used its unusual postcanine teeth to facilitate dental filtration. Apart from the unusual shape and orientation of the teeth, evidence of dental filtration can be found in its skull. The rostrum in Coronodon is much wider than those of archaeocetes and primitive odontocetes, and the mandibular symphysis is shorter. Additionally, the rostrum has very loose sutures, which would have allowed Coronodon to expand the size of its oral cavity in a manner similar to extant mysticetes. [1]

Together, these features suggest that Coronodon employed a mixed feeding strategy, swapping from pursuit predation to ram feeding when necessary, and using its enlarged molar teeth as a sieve to capture prey when filter feeding.

Paleoenvironment

C. havensteini is found in the Ashley Formation, whereas C. planifrons and C. newtonorum are found in the Chandler Bridge Formation. The genus has a fossil range from 30 to 23.5 million years ago, from the Early to Late Oligocene. These formations would have been underwater at this time, and a wide assemblage of marine vertebrates have been discovered there. Many primitive odontocetes, such as Ankylorhiza , Xenorophus , and Albertocetus have been found in both formations in Oligocene aged deposits. Other fossil organisms that have been found in these formations include various sea turtles, sirenians, primitive mysticetes, the giant bird Pelagornis and bony and cartilaginous fishes of many sorts, including the megatoothed shark genus Otodus .

Related Research Articles

<span class="mw-page-title-main">Evolution of cetaceans</span>

The evolution of cetaceans is thought to have begun in the Indian subcontinent from even-toed ungulates (Artiodactyla) 50 million years ago (mya) and to have proceeded over a period of at least 15 million years. Cetaceans are fully aquatic marine mammals belonging to the order Artiodactyla and branched off from other artiodactyls around 50 mya. Cetaceans are thought to have evolved during the Eocene, the second epoch of the present-extending Cenozoic Era. Molecular and morphological analyses suggest Cetacea share a relatively recent closest common ancestor with hippopotami and that they are sister groups. Being mammals, they surface to breathe air; they have five finger bones (even-toed) in their fins; they nurse their young; and, despite their fully aquatic life style, they retain many skeletal features from their terrestrial ancestors. Research conducted in the late 1970s in Pakistan revealed several stages in the transition of cetaceans from land to sea.

<i>Basilosaurus</i> Prehistoric cetacean genus from the Late Eocene epoch

Basilosaurus is a genus of large, predatory, prehistoric archaeocete whale from the late Eocene, approximately 41.3 to 33.9 million years ago (mya). First described in 1834, it was the first archaeocete and prehistoric whale known to science. Fossils attributed to the type species B. cetoides were discovered in the United States. They were originally thought to be of a giant reptile, hence the suffix "-saurus", Ancient Greek for "lizard". The animal was later found to be an early marine mammal, which prompted attempts at renaming the creature, which failed as the rules of zoological nomenclature dictate using the original name given. Fossils were later found of the second species, B. isis, in 1904 in Egypt, Western Sahara, Morocco, Jordan, Tunisia, and Pakistan. Fossils have also been unearthed in the southeastern United States and Peru.

<i>Dorudon</i> Genus of ancient whales

Dorudon ("spear-tooth") is a genus of extinct basilosaurid ancient whales that lived alongside Basilosaurus 40.4 to 33.9 million years ago in the Eocene. It was a small whale, with D. atrox measuring 5 metres (16 ft) long and weighing 1–2.2 metric tons. Dorudon lived in warm seas around the world and fed on small fish and mollusks. Fossils have been found along the former shorelines of the Tethys Sea in present-day Egypt and Pakistan, as well as in the United States, New Zealand and Western Sahara.

<span class="mw-page-title-main">Archaeoceti</span> Paraphyletic group of primitive cetaceans from Early Eocene to Late Oligocene

Archaeoceti, or Zeuglodontes in older literature, is a paraphyletic group of primitive cetaceans that lived from the Early Eocene to the late Oligocene. Representing the earliest cetacean radiation, they include the initial amphibious stages in cetacean evolution, thus are the ancestors of both modern cetacean suborders, Mysticeti and Odontoceti. This initial diversification occurred in the shallow waters that separated India and Asia 53 to 45 mya, resulting in some 30 species adapted to a fully oceanic life. Echolocation and filter-feeding evolved during a second radiation 36 to 35 mya.

<i>Zygorhiza</i> Genus of mammals

Zygorhiza ("Yoke-Root") is an extinct genus of basilosaurid early whale known from the Late Eocene of Louisiana, Alabama, and Mississippi, United States, and the Bartonian to the late Eocene of New Zealand . Specimens reported from Europe are considered Dorudontinae incertae sedis.

<i>Janjucetus</i> Extinct genus of mammals

Janjucetus is an extinct genus of cetacean, and a basal baleen whale (Mysticeti), from the Late Oligocene around 25 million years ago (mya) off south-east Australia, containing one species J. hunderi. Unlike modern mysticetes, it possessed large teeth for gripping and shredding prey, and lacked baleen, and so was likely to have been a predator that captured large single prey animals rather than filter feeding. However, its teeth may have interlocked, much like those of the modern-day filter-feeding crabeater seal, which would have allowed some filter-feeding behaviour. Its hunting behaviour was probably similar to the modern-day leopard seal, probably eating large fish. Like baleen whales, Janjucetus could not echolocate; however, it did have unusually large eyes, and so probably had an acute sense of vision. The only specimen was found on the Jan Juc beach, where the remains of the extinct whales Mammalodon, Prosqualodon and Waipatia have also been discovered.

Mammalodon is an extinct genus of archaic baleen whale belonging to the family Mammalodontidae.

<span class="mw-page-title-main">Mammalodontidae</span> Extinct family of mammals

Mammalodontidae is a family of extinct whales known from the Oligocene of Australia and New Zealand.

Dental anatomy is a field of anatomy dedicated to the study of human tooth structures. The development, appearance, and classification of teeth fall within its purview. Tooth formation begins before birth, and the teeth's eventual morphology is dictated during this time. Dental anatomy is also a taxonomical science: it is concerned with the naming of teeth and the structures of which they are made, this information serving a practical purpose in dental treatment.

<i>Aetiocetus</i> Extinct genus of mammals

Aetiocetus is a genus of extinct basal mysticete, or baleen whale that lived 33.9 to 23.03 million years ago, in the Oligocene in the North Pacific ocean, around Japan, Mexico, and Oregon, U.S. It was first described by Douglas Emlong in 1966 and currently contains known four species, A. cotylalveus, A. polydentatus, A. tomitai, and A. weltoni. These whales are remarkable for their retention of teeth and presence of nutrient foramina, indicating that they possessed baleen. Thus, Aetiocetus represents the transition from teeth to baleen in Oligocene mysticetes. Baleen is a highly derived character, or synapomorphy, of mysticetes, and is a keratinous structure that grows from the palate, or roof of the mouth, of the whale. The presence of baleen is inferred from the fossil record in the skull of Aetiocetus. Aetiocetus is known from both sides of the Pacific Ocean: it was first documented in Oregon, United States, but it is also known from Japan and Mexico. The genus is currently constrained to the Northern hemisphere and has little value in biostratigraphic studies of the Oligocene due to its limited occurrences across the Pacific.

Babiacetus is an extinct genus of early cetacean that lived during the late Lutetian middle Eocene of India . It was named after its type locality, the Harudi Formation in the Babia Hills, Kutch District, Gujarat, India.

Eomysticetus is an extinct genus of baleen whale from the late Oligocene (Chattian) Chandler Bridge Formation of South Carolina.

<i>Llanocetus</i> Genus of extinct toothed baleen whales

Llanocetus is a genus of extinct toothed baleen whales from the Late Eocene of Antarctica. The type species, Llanocetus denticrenatus, reached gigantic proportions, with the juvenile specimen reaching an estimated 8 m (26 ft) in length; a second, unnamed species, known only from three isolated premolar teeth, reached an estimated total body length of up to 12 m (39 ft). Like other contemporary baleen whales of the Eocene, Llanocetus completely lacked baleen in its jaws. It was probably a suction feeder like the modern beaked and pygmy right whales.

Eomysticetidae is a family of extinct mysticetes belonging to Chaeomysticeti. It is one of two families in the basal chaeomysticete clade Eomysticetoidea.

<span class="mw-page-title-main">Aetiocetidae</span> Extinct family of mammals

Aetiocetidae is an extinct family of toothed baleen whales known from the Oligocene. The whales are from the North Pacific Ocean and ranged in size from 3 to 8 metres long. Many of the described specimens were discovered from the Upper Oligocene of the Japanese Morawan Formation, the largest known one from the Morawan's Upper tuffaceous siltstone. Other formally described extinct toothed mysticetis from this time are smaller, from 3 to 4 metres in length. Mysticeti with true baleen are seen in fossils from the Upper Oligocene. The monophyly of the family is still uncertain, as are the evolutionary relationship between the early toothed baleen whales and the early and extant edentulous baleen whales. However, the cladistic analyses of Coronodon and Mystacodon seem to indicate that Aetiocetidae and Llanocetidae are more closely related to crown Mysticeti than to Mammalodontidae, Coronodon, and Mystacodon.

<i>Waharoa <span style="font-style:normal;">(whale)</span></i> Extinct species of whale

Waharoa is a genus of eomysticetid baleen whale from the Late Oligocene (Chattian) of New Zealand. It was identified with the discovery of Waharoa ruwhenua by Boessenecker and Fordyce (2015), which added a new genus and species to a monophyletic family Eomysticetidae.

Mystacodon is a genus of toothed baleen whale from the Late Eocene Yumaque Member of Paracas Formation of the Pisco Basin in southwestern Peru. It is the oldest known baleen whale, and was probably a suction feeder of small prey on the seafloor.

Yamatocetus canaliculatus is an extinct species of eomysticetid baleen whale from the Late Oligocene of Japan.

<i>Ankylorhiza</i> Extinct genus of toothed whales from the Oligocene epoch

Ankylorhiza is an extinct genus of toothed whale that lived in what is now the United States during the Oligocene epoch, between 29 and 23.5 million years ago. The type and only known species is A. tiedemani, though two fossil skeletons may represent an additional, second species within the genus. Ankylorhiza was about 4.8 meters (16 ft) long, with a long, robust skull bearing conical teeth that were angled forwards at the tip of the snout.

<i>Antaecetus</i> Extinct genus of pachycetine basilosaurid

Antaecetus is an extinct genus of pachycetine basilosaurid from the middle Eocene Aridal Formation of Morocco as well as the Fayum, Egypt. Antaecetus, although known from fewer remains in total, is markedly more complete than the closely related Pachycetus, with one specimen preserving large parts of the vertebral column up to the lumbar vertebrae and a well preserved skull. Based on these remains Antaecetus appears to have been smaller than Pachycetus, with a proportionally smaller head and much more gracile teeth. Both genera however share a highly osteosclerotic and pachyostotic skeleton, greatly increasing their weight and possibly serving as additional ballast. In turn the elongation and thickening of the vertebrae severely impacts the animals movement, most likely causing it to have been much slower and far less mobile than other archaeocetes. It has been proposed that Antaecetus was a slow moving inhabitant of shallow coastal waters, where it would ambush fish and marine molluscs. Only a single species of Antaecetus is known, Antaecetus aithai, which was originally described as a species of Pachycetus.

References

  1. 1 2 3 4 5 Geisler, Jonathan H; Boessenecker, Robert W; Brown, Mace; Beatty, Brian L (2017). "The Origin of Filter Feeding in Whales". Current Biology. 27 (13): 2036–2042.e2. doi: 10.1016/j.cub.2017.06.003 . PMID   28669761.
  2. 1 2 Boessenecker, R. W.; Beatty, B. L.; Geisler, J. H. (2023). "New specimens and species of the Oligocene toothed baleen whale Coronodon from South Carolina and the origin of Neoceti". PeerJ. 11: e14795. doi: 10.7717/peerj.14795 .