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Elasmosauridae
Elasmosauridae
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Elasmosauridae
Temporal range: Hauterivian-Maastrichtian, 130–66.0 Ma[1][2]
Reconstructed skeleton of Elasmosaurus platyurus in the Rocky Mountain Dinosaur Resource Center in Woodland Park, Colorado.
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Sauropterygia
Order: Plesiosauria
Superfamily: Plesiosauroidea
Clade: Xenopsaria
Family: Elasmosauridae
Cope, 1869
Genera
Synonyms
  • Cimoliasauridae
    Delair, 1959

Elasmosauridae, often called elasmosaurs or elasmosaurids, is an extinct family of plesiosaurs that lived from the Hauterivian stage of the Early Cretaceous to the Maastrichtian stage of the Late Cretaceous period (c. 130 to 66 mya). The taxon was initially erected in 1869 by Edward Drinker Cope to include the type genus Elasmosaurus with the related Cimoliasaurus, although he did not argued in detail why. Over the following years, many authors recognized this classification on the basis of predominantly postcranial features, becoming one of the three groups in which plesiosaurs were often classified during the 19th century, along with the Pliosauridae and the Plesiosauridae. However, most of these traits led to many genera since recognized as belonging to other plesiosaur families being classified as elasmosaurids. Another family historically considered as distinct, the Cimoliasauridae, has since 2009 been recognized as a junior synonym of the Elasmosauridae. Along with the Polycotylidae, elasmosaurids represent the few plesiosauroids that lived until the Cretaceous–Paleogene extinction event.

With a maximum length ranging from 5 to 12 m (16 to 39 ft) depending on the genera, elasmosaurids have a streamlined body with paddle-like limbs, mostly having a short tail, a small head, and an extremely long neck. The necks of these marine reptiles are supported by a very large number of cervical vertebrae, Elasmosaurus and Albertonectes being the only known vertebrates to have more than 70. The skull of elasmosaurids appears mainly slender and triangular, the majority of them having large fang-like teeth at the front, and smaller teeth towards the back. The Aristonectinae subgroup nevertheless has different morphological traits, having more numerous but smaller teeth and having a shorter neck. Elasmosaurids were well adapted for aquatic life, and used their flippers for swimming. Contrary to earlier depictions, their necks were not very flexible, and could not be held high above the water surface. It is unknown what their long necks were used for, but they may have had a function in feeding. Elasmosaurids probably ate small fish and marine invertebrates, seizing them with their long teeth, and may have used gastroliths (stomach stones) to help digest their food.

Morphology

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Reconstruction of a long-necked blue marine reptile on a white background.
Reconstruction of a long-necked gray marine reptile on a white background.
Life restorations of Elasmosaurus (top) and Aristonectes (bottom). The first represents the "typical" morphology of elasmosaurids, while the second represents the slightly different morphology of the aristonectines.

Like many plesiosaurs, elasmosaurids are easily recognizable by their compact, streamlined bodies, long paddle-like limbs, short tails, proportionately small heads, and very elongated necks.[2] The oldest known representative, Jucha, dating from the Hauterivian stage of the Lower Cretaceous,[1] would have measured 5 m (16 ft) long.[6] Most representatives dating from more recent periods nevertheless adopt sizes ranging from more than 8 m (26 ft) in length.[7] The largest known member of this family, Albertonectes, would have reached a length of 12.1 metres (40 ft) with a body mass of 4.8 metric tons (5.3 short tons).[8] A referred specimen of Aristonectes that was discovered in Seymour Island, Antarctica, numbered as MLP 89-III-3-1, is view to be one of the largest and heaviest plesiosaurs identified to date, estimated in 2019 at between 11 and 11.9 metres (36 and 39 ft) long for body mass of 10.7–13.5 metric tons (11.8–14.9 short tons).[9][a]

The skull of elasmosaurids are mainly slender and triangular in shape. The lateral edges of the orbits are characterized by a convex lateral edge. A large majority of representatives of the group have a their generally heterodont (irregular throughout the jaws) dentition, with the teeth becoming progressively smaller from front to back, with the larger ones shaped like large fangs. These representatives have generally five teeth in the premaxillae (which form the front of the upper jaw), 14 teeth in the maxillae (the largest tooth bearing bone of the upper jaw), and between 17 and 19 in the dentary bones (the main part of the lower jaw). Aristonectines teeth are more numerous but are considerably smaller, having a homodont dentition, all the teeth being similar in shape.[2]

One of the most easily recognizable characteristics of elasmosaurids is their long neck formed by a fairly considerable number of cervical vertebrae, of which a large majority of genera have between 50 and 70. The type genus Elasmosaurus and its close relative Albertonectes are the only representatives currently known to have more than 70, precisely 72 and 76 respectively, an unequaled number among all known vertebrates.[10][11] In spite of their many neck vertebrae, the necks of elasmosaurids were less than half as long as those of the longest-necked sauropod dinosaurs.[12] Additionally, the Aristonectinae subgroup has cervical vertebrae that are wider than they are long, and their necks are therefore shorter than those of other representatives. Apart from aristonectines, other elasmosaurids have a longitudinal ridge on the cervical vertebrae which served to anchor the neck musculature. One of the identifying features of elasmosaurids is that their shoulder girdle has a large heart-shaped opening located between the coracoids, known as the intercoracoid embayment. As with other plesiosaurs, they have swimming paddles made up of very long digits. The paddles at the front (the pectoral paddles) were longer than those at the back (the pelvic paddles). Since the last tail-vertebrae of elasmosaurids were fused into a structure similar to the pygostyle of birds, it is possible this supported a tail-fin, but the shape it would have had is unknown.[2]

Classification

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Early three-family classification

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Though Edward Drinker Cope had originally recognized Elasmosaurus as a plesiosaur, in an 1869 paper he placed it, with Cimoliasaurus and Crymocetus, in a new order of sauropterygian reptiles. He named the group Streptosauria, or "reversed lizards", due to the orientation of their individual vertebrae supposedly being reversed compared to what is seen in other vertebrate animals.[13][14] He subsequently abandoned this idea in his 1869 description of Elasmosaurus, where he stated he had based it on Leidy's erroneous interpretation of Cimoliasaurus. In this paper, he also named the new family Elasmosauridae, containing Elasmosaurus and Cimoliasaurus, without comment. Within this family, he considered the former to be distinguished by a longer neck with compressed vertebrae, and the latter by a shorter neck with square, depressed vertebrae.[15]: 47 

In subsequent years, Elasmosauridae came to be one of three groups in which plesiosaurs were classified, the others being the Pliosauridae and Plesiosauridae (sometimes merged into one group).[16] In 1874 Harry Seeley took issue with Cope's identification of clavicles in the shoulder girdle of Elasmosaurus, asserting that the supposed clavicles were actually scapulae. He found no evidence of a clavicle or an interclavicle in the shoulder girdle of Elasmosaurus; he noted that the absence of the latter bone was also seen in a number of other plesiosaur specimens, which he named as new elasmosaurid genera: Eretmosaurus, Colymbosaurus, and Muraenosaurus.[17] Richard Lydekker subsequently proposed that Elasmosaurus, Polycotylus, Colymbosaurus, and Muraenosaurus could not be distinguished from Cimoliasaurus based on their shoulder girdles, and advocated their synonymization at the genus level.[18][19]

Seeley noted in 1892 that the clavicle was fused to the coracoid by a suture in elasmosaurians, and was apparently "an inseparable part" of the scapula. Meanwhile, all plesiosaurs with two-headed neck ribs (the Plesiosauridae and Pliosauridae) had a clavicle made only of cartilage, such that ossification of the clavicle would turn a "plesiosaurian" into an "elasmosaurian".[20] Samuel Wendell Williston doubted Seeley's usage of neck ribs to subdivide plesiosaurs in 1907, opining that double-headed neck ribs were instead a "primitive character confined to the early forms".[21] Charles Andrews elaborated on differences between elasmosaurids and pliosaurids in 1910 and 1913. He characterized elasmosaurids by their long necks and small heads, as well as by their rigid and well-developed scapulae (but atrophied or absent clavicles and interclavicles) for forelimb-driven locomotion. Meanwhile, pliosaurids had short necks but large heads, and used hindlimb-driven locomotion.[22][23]

Refinement of plesiosaur taxonomy

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Although the placement of Elasmosaurus in the Elasmosauridae remained uncontroversial, opinions on the relationships of the family became variable over subsequent decades. Williston created a revised taxonomy of plesiosaurs in a monograph on the osteology of reptiles (published posthumously in 1925). He provided a revised diagnosis of the Elasmosauridae; aside from the small head and long neck, he characterized elasmosaurids by their single-headed ribs; scapulae that meet at the midline; clavicles that are not separated by a gap; coracoids that are "broadly separated" in their rear half; short ischia; and the presence of only two bones (the typical condition) in the epipodialia (the "forearms" and "shins" of the flippers). He also removed several plesiosaurs previously considered to be elasmosaurids from this family due to their shorter necks and continuously meeting coracoids; these included Polycotylus and Trinacromerum (the Polycotylidae), as well as Muraenosaurus, Cryptoclidus, Picrocleidus, Tricleidus, and others (the Cryptoclididae).[24]

In 1940 Theodore White published a hypothesis on the interrelationships between different plesiosaurian families. He considered Elasmosauridae to be closest to the Pliosauridae, noting their relatively narrow coracoids as well as their lack of interclavicles or clavicles. His diagnosis of the Elasmosauridae also noted the moderate length of the skull (i.e., a mesocephalic skull); the neck ribs having one or two heads; the scapula and coracoid contacting at the midline; the blunted rear outer angle of the coracoid; and the pair of openings (fenestrae) in the scapula–coracoid complex being separated by a narrower bar of bone compared to pliosaurids. The cited variability in the number of heads on the neck ribs arises from his inclusion of Simolestes to the Elasmosauridae, since the characteristics of "both the skull and shoulder girdle compare more favorably with Elasmosaurus than with Pliosaurus or Peloneustes." He considered Simolestes a possible ancestor of Elasmosaurus.[25] Oskar Kuhn adopted a similar classification in 1961.[26]: 4 

Samuel Paul Welles took issue with White's classification in his 1943 revision of plesiosaurs, noting that White's characteristics are influenced by both preservation and ontogeny. He divided plesiosaurs into two superfamilies, the Plesiosauroidea and Pliosauroidea, based on neck length, head size, ischium length, and the slenderness of the humerus and femur (the propodialia). Each superfamily was further subdivided by the number of heads on the ribs, and the proportions of the epipodialia. Thus, elasmosaurids had long necks, small heads, short ischia, stocky propodialia, single-headed ribs, and short epipodialia.[27]: 196–207  Pierre de Saint-Seine in 1955 and Alfred Romer in 1956 both adopted Welles' classification.[26]: 4  In 1962 Welles further subdivided elasmosaurids based on whether they possessed pelvic bars formed from the fusion of the ischia, with Elasmosaurus and Brancasaurus being united in the subfamily Elasmosaurinae by their sharing of completely closed pelvic bars.[28]: 4 

Per Ove Persson, however, considered Welles' classification too simplistic, noting in 1963 that it would, in his opinion, erroneously assign Cryptoclidus, Muraenosaurus, Picrocleidus, and Tricleidus to the Elasmosauridae. Persson refined the Elasmosauridae to include traits such as the crests on the sides of the neck vertebrae; the hatchet-shaped neck ribs at the front of the neck; the fused clavicles; the separation of the coracoids at the rear; and the rounded, plate-like pubis. He also retained the Cimoliasauridae as separate from the Elasmosauridae, and suggested, based on comparisons of vertebral lengths, that they diverged from the Plesiosauridae in the Late Jurassic or Early Cretaceous.[26]: 7  However, David S. Brown noted in 1981 that the variability of neck length in plesiosaurs made Persson's argument unfeasible, and moved the aforementioned genera back into the Elasmosauridae; he similarly criticized Welles' subdivision of elasmosaurids based on the pelvic bar. Brown's diagnosis of elasmosaurids included the presence of five premaxillary teeth; the ornamentation of teeth by longitudinal ridges; the presence of grooves surrounding the occipital condyles; and the broad-bodied scapulae meeting at the midline.[29]: 336  In 2009, F. Robin O'Keefe and Hallie Street synonymized the Cimoliasauridae with the Elasmosauridae, noting that most of the diagnostic traits previously established to distinguish them are also found in elasmosaurids.[30]

Modern phylogenetic context

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Carpenter's 1997 phylogenetic analysis of plesiosaurs challenged the traditional subdivision of plesiosaurs based on neck length. He found that Libonectes and Dolichorhynchops shared characteristics such as an opening on the palate for the vomeronasal organ, the plate-like expansions of the pterygoid bones, and the loss of the pineal foramen on the top of the skull, differing from the pliosaurs. While polycotylids had previously been part of the Pliosauroidea, Carpenter moved polycotylids to become the sister group of the elasmosaurids based on these similarities, thus implying that polycotylids and pliosauroids evolved their short necks independently.[31]

F. Robin O'Keefe likewise included polycotylids in the Plesiosauroidea in 2001 and 2004, but considered them more closely related to the Cimoliasauridae and Cryptoclididae in the Cryptocleidoidea.[16][32][33] Some analyses continued to recover the traditional groupings. In 2008 Patrick Druckenmiller and Anthony Russell moved the Polycotylidae back into the Pliosauroidea, and placed Leptocleidus as their sister group in the newly named Leptocleidoidea;[34] Adam Smith and Gareth Dyke independently found the same result in the same year.[35] However, in 2010 Hilary Ketchum and Roger Benson concluded that the results of these analyses were influenced by inadequate sampling of species. In the most comprehensive phylogeny of plesiosaurs yet, they moved the Leptocleidoidea (renamed the Leptocleidia) back into the Plesiosauroidea as the sister group of the Elasmosauridae;[36] subsequent analyses by Benson and Druckenmiller recovered similar results, and named the Leptocleidoidea–Elasmosauridae grouping as Xenopsaria.[37][38]

The content of Elasmosauridae also received greater scrutiny. Since its initial assignment to the Elasmosauridae, the relationships of Brancasaurus had been considered well supported, and it was recovered by O'Keefe's 2004 analysis[32] and Franziska Großmann's 2007 analysis.[39] However, Ketchum and Benson's analysis instead included it in the Leptocleidia,[36] and its inclusion in that group has remained consistent in subsequent analyses.[37][38][40] Their analysis also moved Muraenosaurus to the Cryptoclididae, and Microcleidus and Occitanosaurus to the Plesiosauridae;[36] Benson and Druckenmiller isolated the latter two in the group Microcleididae in 2014, and considered Occitanosaurus a species of Microcleidus.[38] These genera had all previously been considered to be elasmosaurids by Carpenter, Großmann, and other researchers.[41][39][42][43]

Within the Elasmosauridae, Elasmosaurus itself has been considered a "wildcard taxon" with highly variable relationships.[44] Carpenter's 1999 analysis suggested that Elasmosaurus was more basal (i.e. less specialized) than other elasmosaurids with the exception of Libonectes.[41] In 2005 Sachs suggested that Elasmosaurus was closely related to Styxosaurus,[45] and in 2008 Druckenmiller and Russell placed it as part of a polytomy with two groups, one containing Libonectes and Terminonatator, the other containing Callawayasaurus and Hydrotherosaurus.[34] Ketchum and Benson's 2010 analysis included Elasmosaurus in the former group.[36] Benson and Druckenmiller's 2013 analysis (below, left) further removed Terminonatator from this group and placed it as one step more derived (i.e., more specialized).[37] In Rodrigo Otero's 2016 analysis based on a modification of the same dataset (below, right), Elamosaurus was the closest relative of Albertonectes, forming the Styxosaurinae with Styxosaurus and Terminonatator.[40] Danielle Serratos, Druckenmiller, and Benson could not resolve the position of Elasmosaurus in 2017, but they noted that Styxosaurinae would be a synonym of Elasmosaurinae if Elasmosaurus did fall within the group.[44] In 2020, O'Gorman formally synonymized Styxosaurinae with Elasmosaurinae based on the inclusion of Elasmosaurus within the group, and also provided a list of diagnostic characteristics for the clade.[3] In 2021 a new topology placed Cardiocorax as a sister taxon of Libonectes, representing an older lineage of elasmosaurids in the Maastrichtian.[46]

Aristonectinae

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Aristonectinae is a subfamily of Elasmosauridae. It includes the Late Cretaceous plesiosaurs Aristonectes and Kaiwhekea, traditionally grouped with the Late Jurassic Tatenectes and Kimmerosaurus in the family Aristonectidae. They are distinguished by the fact that they have a very enlarged skull compared to the width of the body, a moderately short neck and more than 25 teeth in the maxilla.[47]

An alternative hypothesis suggested by F. Robin O'Keefe and Hallie Street in 2009 is that aristonectines instead belong to a familyAristonectidae—which is unrelated to elasmosaurids and is instead the sister group to Polycotylidae within the larger clade "Cryptocleidoidea".[48]

Paleobiology

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Drawing of two elasmosaurs underwater.
Restoration showing two Elasmosaurus swimming with straight necks

Elasmosaurids were fully adapted to life in the ocean, with streamlined bodies and long paddles that indicate they were active swimmers.[2] The unusual body structure of elasmosaurids would have limited the speed at which they could swim, and their paddles may have moved in a manner similar to the movement of oars rowing, and due to this, could not twist and were thus held rigidly.[49] Plesiosaurs were even believed to have been able to maintain a constant and high body temperature (homeothermy), allowing for sustained swimming.[50]

A 2015 study concluded that locomotion was mostly done by the fore-flippers while the hind-flippers functioned in maneuverability and stability;[51] a 2017 study concluded that the hind-flippers of plesiosaurs produced 60% more thrust and had 40% more efficiency when moving in harmony with the fore-flippers.[52] The paddles of plesiosaurs were so rigid and specialized for swimming that they could not have come on land to lay eggs like sea turtles. Therefore, they probably gave live-birth (viviparity) to their young like some species of sea snakes.[49] Evidence for live-birth in plesiosaurs is provided by the fossil of an adult Polycotylus with a single fetus inside.[53]

Elasmosaurid remains provide some evidence they were preyed upon. A humerus of an unidentified subadult elasmosaurid was found with bite marks matching the teeth of the shark Cretoxyrhina,[54] while a crushed Eromangasaurus skull[55] has tooth-marks matched to the pliosaur Kronosaurus.[56]

Neck movement and function

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Five gray silhouettes of elasmosaurs in different neck positions on a white background
Chart showing several hypotheses on the neck flexibility of elasmosaurids. A – Swan-like neck held upright, B – Ramrod straight neck held out directly in front, C – Downward curve for feeding on benthic prey items, D – Wide horizontal curve, E – Serpentine undulating position. Neck positions B–E would have been within the estimated neck flexibility ranges.[57]

Although followed by many common media depictions, more recent research showed that elasmosaurids were incapable of raising anything more than its head above the water. The weight of their long neck placed the center of gravity behind the front flippers. Thus, elasmosaurids could have raised their head and neck above the water only when in shallow water, where it could rest its body on the bottom. Also, the weight of the neck, the limited musculature, and the limited movement between the vertebrae would have prevented elasmosaurids from raising head and neck very high. The head and shoulders of theses animals probably acted as a rudder. If they moved the anterior part of the body in a certain direction, it would cause the rest of the body to move in that direction. Thus, elasmosaurids would have been unable to swim in one direction while moving its head and neck either horizontally or vertically in a different direction.[49]

One study found that the necks of elasmosaurids were capable of 75–177˚ of ventral movement, 87–155° of dorsal movement, and 94–176° of lateral movement, depending on the amount of tissue between the vertebrae, which probably increased in rigidness towards the back of the neck. The researchers concluded that lateral and vertical arches and shallow S-shaped curves were feasible in contrast to the "swan-like" S-shape neck postures that required more than 360° of vertical flexion.[57]

The exact function of the neck of elasmosaurids is unknown,[2] though it may have been important for hunting.[49] It has also been suggested that the long necks of plesiosaurs served as a snorkel and allowed them to breathe air while the body remained underwater. This is disputed as there would be large hydrostatic pressure differences, particularly for the extremely long-necked elasmosaurids. The neck anatomy of elasmosaurids was capable of making a gentle slope to allow them to breathe at the surface but would have required them to engage in energy-expensive swimming at the sub-surface. In addition, the longer neck would also have increased dead space, and the animals may have required larger lungs. The neck could have had other vulnerabilities, for example being a target for predators.[58]

Simulation of water flow on 3D models showed that more elongated necks, such as those of elasmosaurids, did not increase drag force while swimming compared to shorter necked plesiosaurs. On the other hand, bending the neck sideways did increase drag force, more so in forms with very long necks.[59] Another study found the long necks of elasmosaurs would normally increase drag during forward swimming but this was cancelled out by their large torsos, and hence large body sizes may have facilitated the evolution of longer necks.[60]

Feeding

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Old picture of bones and stones on a black background
Gastroliths and bones (right) of an undetermined plesiosaur from Kansas

The flexion ranges of elasmosaurids necks would have allowed them to employ a number of hunting methods including "benthic grazing", which would have involved swimming close to the bottom and using the head and neck to dig for prey on the sea floor. Elasmosaurids may also have been active hunters in the pelagic zone, retracting their necks to launch a strike or using side-swipe motions to stun or kill prey with their laterally projected teeth (like sawsharks).[57] It has also been suggested that the predatory abilities of elasmosaurids have been underestimated; their large skulls, big jaw-muscles, strong jaws, and long teeth indicate they could prey on animals between 30 centimeters (12 in) and 2 meters (6.6 ft) long, as indicated by stomach contents including those of sharks, fish, mosasaurs, and cephalopods.[61]

It is possible that elasmosaurids stalked schools of fish, concealing themselves below and moving the head slowly up as they approached. The eyes of theses animals were at the top of the head and allowed them to see directly upward. This stereoscopic vision would have helped it to find small prey. Hunting from below would also have been possible, with prey silhouetted in the sunlight while concealed in the dark waters below. Elasmosaurids probably ate small bony fish and marine invertebrates, as their small, non-kinetic skulls would have limited the size of the prey they could eat. Also, with their long, slender teeth adapted for seizing prey and not tearing, elasmosaurids most certainly swallowed their prey whole.[49][57]

Elasmosaurids are commonly found with several gastroliths. A specimen of Styxosaurus contained fragmented fish bones and stones in the abdominal region behind the pectoral girdle. The fish remains were identified as Enchodus and other clupeomorph fish.[62] Several different functions have been proposed for gastroliths, including aiding in digestion, mixing food content, mineral supplementation, and storage and buoyancy control.[63]

Notes

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Elasmosauridae is an extinct family of plesiosaurian marine reptiles within the clade , renowned for their extraordinarily long necks comprising 50–76 , which often accounted for more than half of their body length, and they inhabited epicontinental and open marine environments across all continents during the period (145–66 million years ago). These long-necked predators evolved a streamlined with paddle-like limbs for , small triangular skulls featuring (typically 5 premaxillary, 14 maxillary, and 17–19 dentary teeth per side), and a short ending in a pygostyle-like structure, adaptations that facilitated agile swimming in diverse palaeoenvironments from equatorial to polar seas. Fossils of elasmosaurids are abundant in deposits, particularly from the of and the , reflecting their by the end of the period. Taxonomically, Elasmosauridae forms a monophyletic clade defined by synapomorphies such as a convex anterior margin of the orbit and a heart-shaped embayment between the intercoracoid vacuity, with origins in the Early Cretaceous around 130 million years ago. The family diversified significantly in the Late Cretaceous, giving rise to at least two major subfamilies: Styxosaurinae, characterized by extreme neck elongation (over 60 cervical vertebrae) and including genera like Styxosaurus, Albertonectes, Libonectes, and Elasmosaurus; and Aristonectinae, which exhibited relatively shorter necks, homodont dentition with more numerous teeth, and genera such as Aristonectes and Kaiwhekea. Phylogenetic analyses indicate multiple independent instances of cervical elongation within the family, with basal forms like Brancasaurus and Wapuskanectes appearing in the Early Cretaceous (Aptian–Albian stages), followed by a radiation that produced regionally distinct assemblages, such as those in the Cenomanian–Santonian Western Interior Seaway. In terms of , elasmosaurids were macropredatory swimmers that likely employed their elongated necks for stealthy hunting of schooling , cephalopods, and soft-bodied in the , supported by evidence of gastroliths in their stomachs for grinding ingested prey and aiding digestion. Some advanced forms, particularly within Aristonectinae, may have specialized in benthic or near-shore filter-feeding on small crustaceans and , inferred from their robust skulls and increased tooth counts, while others like attained lengths of 10–14 meters and served as apex predators in mid-Cretaceous seas. Recent discoveries, such as the 2025 identification of Traskasaura sandrae from , highlight ongoing revelations into their dietary adaptations, with robust teeth suggesting crushing predation on hard-shelled prey. Their persistence until the underscores their ecological success, though they faced predation from larger marine reptiles such as mosasaurs and pliosaurs.

Description

Overall body plan

Elasmosaurids were large marine reptiles characterized by body lengths ranging from 4 to 14 meters, depending on the species and ontogenetic stage. Smaller forms, such as Kawanectes lafquenianum, measured around 4 meters, while larger taxa like vanderveldei and quiriquinensis approached or exceeded 11 meters in total length. Mass estimates vary accordingly, with intermediate-sized taxa like vanderveldei weighing approximately 4.8 metric tons and larger specimens, including cf. sp., reaching up to 13.5 metric tons based on volumetric reconstructions assuming a similar to that of modern aquatic reptiles. Their overall body plan was streamlined and , optimized for efficient aquatic locomotion, featuring a broad, robust torso supported by and single-headed dorsal that formed a wide, barrel-shaped midsection. The tail was relatively short, comprising typically 20–30 caudal vertebrae that tapered gradually without a prominent fluke, contributing to stability rather than . Four well-developed, paddle-like limbs, with expanded phalanges and hyperphalangy, served as primary propulsors, enabling underwater flight-like movements akin to those of modern sea turtles or . This integrated anatomy, including a notably elongated as a defining trait, underscored their to open-ocean predation. Preserved skin impressions from related plesiosaurians indicate a smooth, scaleless texture across the body, resembling that of modern cetaceans and facilitating reduced drag during swimming. Hypotheses of —darker dorsal surfaces and lighter ventral areas—for in marine environments have been proposed based on pigmentation patterns in contemporaneous aquatic reptiles, though for elasmosaurids remains elusive. Size variations among specimens have led to hypotheses of , potentially with females larger than males to support egg production, but these remain unconfirmed due to limited sample sizes and overlapping ontogenetic series.

Skull and dentition

The skulls of elasmosaurids are typically triangular and elongated, measuring approximately 40–60 cm in length in adult specimens, which is small relative to their overall body size. These crania feature a long, tapered rostrum comprising about 40% of the total length, often with a pronounced dorsomedian ridge, and reduced temporal fenestrae that occupy roughly 35–40% of the skull length. In most elasmosaurid genera, the is , consisting of robust conical fangs up to 5 cm long at the anterior margins of the jaws for grasping prey, grading posteriorly into smaller, needle-like teeth suited for retaining slippery aquatic organisms. Examples include enlarged fangs in the second maxillary position in Thalassomedon haningtoni and anisodont teeth with ridglets in Cardiocorax mukulu, where premaxillary alveoli number 5, maxillary 17, and dentary at least 20. An exception occurs in the subfamily Aristonectinae, where the dentition is homodont, featuring hundreds of tiny, uniform, needle-like teeth arranged in interlocking combs that form an oral battery suggestive of durophagous or filter-feeding habits. In taxa such as and , premaxillary teeth number 8–13, maxillary 38–50, and dentary 46–63, enabling sieving of small prey particles. Palatal structures in elasmosaurids include robust pterygoid bars that form the floor of the mouth, often separated medially by a , with possible interpterygoid vacuities or vomeronasal fenestrae analogous to housing for Jacobson's organ in related sauropterygians. The vomer extends posteriorly beyond the internal nares in some specimens, contributing to a reinforced .

Neck anatomy

Elasmosaurids are distinguished by their exceptionally elongated necks, formed by a high number of ranging from 50 to 76. For instance, platyurus possesses 72 , while Albertonectes vanderveldei exhibits the record of 76, the highest known in any . These vertebrae constitute over 70% of the presacral vertebral column length, emphasizing the neck's dominance in the overall and contributing to the animal's streamlined . The feature elongated that are typically longer than tall, with low neural spines that decrease in height posteriorly and often exhibit a semi-circular outline by the mid-neck region. Articulation occurs via ball-and-socket-like zygapophyses, where the prezygapophyses project anteriorly and postzygapophyses posteriorly, facilitating some lateral flexion while restricting dorsoventral bending due to the overlapping and attachments. Muscle scars on the and neural spines indicate robust ligamentary attachments, supporting a semi-rigid that maintained stability during movement. Inferred ligamentary systems include a strong, elastin-rich dorsal anchored along the neural spines and a midline pit on the , which together provided tensile support to counteract gravitational and hydrodynamic forces. These features suggest the was held in a predominantly horizontal orientation during locomotion, with limited flexibility for precise adjustments rather than broad undulations. Ontogenetic development reveals shorter relative lengths in juveniles, achieved through meristic addition of vertebrae and positive allometric growth of during maturation. In adults, this results in a fusiform profile, with the longest concentrated in the mid-cervical , enhancing elongation without proportional increases at the ends.

Limbs and tail

The limbs of elasmosaurids were highly modified into paddle-like flippers adapted for aquatic propulsion, featuring extensive hyperphalangy in the autopodia, with some digits containing up to 17 phalanges, far exceeding the ancestral pentadactyl condition and contributing to elongated, flexible paddles. The propodials, including the and , possessed robust, rectangular shafts that supported powerful muscular attachments for stroke generation, with the humerus typically broader and more robust than the femur, reflecting differences in load-bearing during swimming. Epipodials and mesopodials were shortened relative to the propodials, tapering distally to form streamlined flippers, while hyperphalangy elongated the distal segments, enhancing hydrodynamic efficiency. Forelimbs in elasmosaurids were significantly larger than hindlimbs, often exceeding them in length and breadth by 20-50%, indicating a primary role in generation through alternating or synchronized paddling motions. This disparity is evident in specimens like those of Libonectes, where humeri measure up to 30 cm in length compared to femora of about 20 cm, with corresponding differences in patterns that suggest greater mechanical stress on the forelimbs. Hindlimbs, though smaller, retained similar paddle morphology but with reduced hyperphalangy, likely serving auxiliary roles in maneuvering. The of elasmosaurids was short and robust, comprising 20-30 caudal vertebrae that did not exceed the trunk length in proportion, tapering rapidly to a terminal pygostyle-like fusion of the last few vertebrae. Caudal neural spines were low and variably oriented, with chevrons numbering approximately one per caudal centrum (20-30 total), providing attachment for hypaxial musculature that enabled limited lateral undulation for steering rather than primary . This contrasts with the more flexible tails of other marine reptiles, emphasizing the reliance on limb-based locomotion. Many skeletal elements, particularly in the flippers, show evidence of extensive inferred from incomplete patterns, such as retained calcified cores in the medullary regions of long bones like the . These patterns suggest greater flexibility in the flippers than indicated by remains alone, comparable to the reinforcements in modern flippers that allow for dynamic underwater "flight." Such inferences are supported by histological analyses of specimens like perinatal aristonectines, where was immature, implying soft-tissue extensions beyond preserved bones.

Taxonomy

Historical development

The family Elasmosauridae was erected by Edward Drinker Cope in 1869 to accommodate the newly described genus Elasmosaurus, based on the type specimen E. platyurus from the Upper Cretaceous Pierre Shale of Kansas. This taxon was characterized by an exceptionally long neck, with Cope initially estimating around 72 cervical vertebrae, though he noted some elements might be missing from the incomplete skeleton. However, in his preliminary reconstruction published in 1868, Cope famously misplaced the skull at the end of the tail rather than the neck, an error stemming from the disarticulated nature of the fossils and his haste amid competitive paleontological discoveries. Joseph Leidy first publicly corrected this mistake in 1870, highlighting the elongated neck as the defining feature of Elasmosaurus. , Cope's rival during the of the 1870s, subsequently used the blunder to mock Cope's anatomical interpretation. This incident underscored the intense rivalry between the two paleontologists, which accelerated discoveries but also led to rushed publications and occasional inaccuracies in early plesiosaurian . By 1875, Cope revised his count to 71 cervical vertebrae, solidifying Elasmosaurus as the eponymous long-necked form within Elasmosauridae. Modern re-examination confirms 72 cervical vertebrae. In 1874, Harry Govier Seeley formalized a three-family classification for Plesiosauria, recognizing for long-necked forms like Elasmosaurus, alongside Plesiosauridae for moderate-necked plesiosaurs and for short-necked, large-headed taxa. This system emphasized neck length as a primary taxonomic criterion and grouped elasmosaurids with other sauropterygian marine reptiles based on vertebral morphology. Twentieth-century refinements included Samuel P. Welles' 1943 monograph, which synonymized the family Cimoliasauridae (erected by Harry Seeley in 1879 for Cimoliasaurus) with Elasmosauridae, arguing that differences in vertebral proportions were insufficient to warrant separation and that Cimoliasaurus represented an early elasmosaurid. Welles also addressed ongoing debates, such as whether polycotylids—short-necked plesiosaurs like Polycotylus—should be classified as aberrant, short-necked elasmosaurids, ultimately distinguishing them based on cranial and limb features while restricting Elasmosauridae to taxa with more than 50 . These revisions laid the groundwork for later cladistic analyses, though pre-1960s classifications remained largely phenetic.

Phylogenetic position

Elasmosauridae is positioned within the superfamily , as part of the derived clade Xenopsaria, which also encompasses and Cimoliosauridae, according to a comprehensive phylogenetic analysis of 66 plesiosaurian taxa. This placement reflects the monophyletic nature of , excluding more basal plesiosauroids, and highlights Elasmosauridae's role in the diversification of long-necked plesiosaurs. Within Xenopsaria, Elasmosauridae forms a to the polycotylids and cimoliosaurs, supported by shared derived traits adapted to marine predation. Recent analyses as of 2025 continue to support this positioning while refining intra-family relationships, with new basal taxa like Traskasaura sandrae indicating early divergences. Key synapomorphies diagnosing Elasmosauridae include the exclusion of from the transverse processes via a distinct notch, which facilitates greater flexibility, and markedly elongated cervical vertebral centra exceeding three times their height, contributing to the extreme lengths characteristic of the family (up to 75 vertebrae in some taxa). These features distinguish elasmosaurids from closely related plesiosauroids like those in Elasmosauridae's outgroup, Plesiosauridae, which exhibit shorter and different rib articulation patterns. Updated 2024–2025 phylogenies affirm , with elongated cervical centra lacking a lateral ridge as a basal condition, and introduce clades like Euelasmosaurida for derived forms. The of Elasmosauridae has been debated in cladistic analyses, with some earlier matrices recovering paraphyletic arrangements due to incomplete sampling, but recent studies affirm its validity as a cohesive family that persisted until the Cretaceous–Paleogene (K–Pg) boundary. For instance, a 2020 analysis incorporating 42 elasmosaurid taxa and 128 characters placed Elasmosauridae as monophyletic within , with strong support against Plesiosauridae (bootstrap values exceeding 70%), emphasizing evolutionary stability through the . Subsequent 2024–2025 studies, including those resolving basal positions for new taxa like Marambionectes molinai, reinforce this with updated matrices confirming and multiple instances of neck elongation. This positioning underscores Elasmosauridae's distinct lineage amid broader plesiosaurian radiations.

Subfamilies and genera

Elasmosauridae is traditionally divided into two primary subfamilies: Elasmosaurinae and Aristonectinae, though some classifications recognize additional clades such as Styxosaurinae within Elasmosaurinae. Elasmosaurinae encompasses the majority of long-necked elasmosaurids, characterized by heterodont dentition with differentiated anterior and posterior teeth, and notably elongated necks comprising 60–76 cervical vertebrae. Representative genera include , the type genus named from the Late Cretaceous of with the type species E. platyurus (etymology: "flat-tailed thin-plate lizard," referring to its vertebral plates and tail structure); Libonectes from the ; with up to 76 cervicals in S. snowii; from the ; and Terminonatator from the . Aristonectinae features more robust builds, homodont dentition with numerous slender, pin-like teeth adapted for filter-feeding, and relatively shorter necks with around 32 or more . Key genera include from the of and , Kaiwhekea from , and Jucha from the of , the latter representing an early, basal form with primitive elongation patterns. Some analyses, such as O'Keefe and Street (2009), elevate Aristonectinae to family status (Aristonectidae) due to distinct cranial and postcranial features, though most recent phylogenies retain it as a within Elasmosauridae. Approximately 18–20 valid genera are currently recognized within Elasmosauridae as of 2025, reflecting diverse morphologies from the Early to and incorporating recent discoveries. These include Hydrotherosaurus from the of with a well-preserved complete , Cardiocorax from the of , a basal form with a broad lacking extreme cervical elongation, Traskasaura sandrae (2025) from the Santonian of as a basal , and Marambionectes molinai (2024) from . Dubious or invalid taxa include Aphrosaurus, originally described from but considered a due to insufficient diagnostic material, and Hydralmosaurus, synonymized with Styxosaurus.

Distribution and timeline

Geological occurrence

Elasmosauridae first appeared during the stage of the , approximately 130 million years ago, and persisted until the stage of the , ending at 66 million years ago. The group's temporal range is supported by fragmentary remains from European deposits in the Hauterivian, with more definitive records emerging by the and stages. Although possible pre-Cretaceous affinities have been suggested based on basal plesiosauromorphs, confirmed elasmosaurids are restricted to the , with early examples including the Albian Wapuskanectes from the Clearwater Formation in . The family exhibited increasing diversity through the mid-Cretaceous, achieving peak generic and morphological diversity during the and stages of the . Late-occurring genera such as from the Pierre Shale (late –early ) represent some of the youngest records, co-occurring with advanced assemblages in North American deposits. Elasmosaurids did not survive the (K–Pg) , with all post-boundary reports refuted by stratigraphic re-evaluations confirming ages for purported specimens. In biostratigraphic terms, elasmosaurid fossils from the are commonly associated with inoceramid bivalves such as and occur within defined biozones, including those dominated by and in the upper .

Geographic distribution

Elasmosaurids achieved a nearly cosmopolitan distribution across marine environments, with the majority of well-documented occurrences concentrated in Laurasian landmasses. In , the represents the primary region of abundance, spanning present-day and , where epicontinental seas facilitated widespread deposition of fossil-bearing sediments. Notable genera from this area include , recovered from the -Missourian Niobrara Formation in , exemplifying the group's prevalence in mid-continental shallow seas, and , known from the in , highlighting persistence into the latest . A new genus, Traskasaura sandrae, described in 2025 from the Haslam Formation, further underscores North American diversity. South American records underscore a significant Gondwanan presence, particularly , where elasmosaurids inhabited high-latitude margins. The genus , including species such as A. parvidens and A. quiriquinensis, is documented from strata of the López de Bertodano Formation in and , indicating adaptation to cooler, polar-influenced waters of the proto-South Atlantic. A new aristonectine, Wunyelfia maulensis, from the early Quiriquina Formation in (described 2021), adds to this southern record. Similarly, Kaiwhekea katiki from the Haumurian Stage of New Zealand's region further evidences this southern distribution, linking Pacific Gondwanan basins. These finds suggest faunal continuity across the Weddellian Biogeographic Province, encompassing southern , the , and . Scattered European discoveries reveal a more peripheral Laurasian footprint, with isolated remains from the , , and southern pointing to Tethyan Sea connections. For instance, indeterminate elasmosaurid vertebrae from sediments in southern Sweden represent rare northern European records, while fragmentary material from the in the UK suggests episodic incursions into epicontinental shelf seas. localities, such as Vega Island's (), yield taxa like Vegasaurus molyi, reinforcing high-latitude Gondwanan ties and trans- dispersal. Recent discoveries extend the range to the Tethyan region, including the first elasmosaurid remains from the Coniacian-Santonian of (Palmyrides chain, described 2024), indicating broader Middle Eastern distribution. Overall, this global pattern implies vicariance following the mid-Mesozoic breakup of , though active migration via the widening and proto-Pacific currents likely contributed to the observed cosmopolitanism during the -.

Associated environments

Elasmosaurids predominantly inhabited epicontinental seas and shallow continental shelves, typically at depths ranging from 50 to 200 meters, where sedimentary records indicate stable, near-shore marine conditions favorable for long-necked plesiosaurs. A prime example is the warm-temperate of during the , characterized by salinity gradients influenced by freshwater influx from surrounding landmasses and periodic connections to open ocean basins. These environments featured varying water masses, with lower salinities in northern and coastal regions transitioning to more normal marine conditions southward, supporting diverse benthic and nektonic communities. In these settings, elasmosaurids co-occurred with apex predators such as mosasaurs, large-bodied sharks (e.g., ), and abundant fishes, reflecting a complex with niche partitioning that positioned elasmosaurids as mid-trophic level piscivores and hunters. Stable isotope analyses of elasmosaurid remains suggest they foraged primarily in coastal or near-shore areas, distinct from the more offshore habits of many mosasaurs, allowing coexistence through spatial and dietary separation. assemblages from the , spanning the to , consistently document this faunal overlap, underscoring elasmosaurids' role in mid-level trophic dynamics. Elasmosaurids demonstrated tolerance for dysoxic to suboxic conditions prevalent in deeper basinal parts of their habitats, as evidenced by their preservation in fine-grained sedimentary such as dark shales and chalks that accumulated under low-oxygen bottom waters. The Pierre Shale Formation, a key depositional basin in the , exemplifies these environments with its organic-rich, stagnant indicative of restricted oxygenation, yet elasmosaurid skeletons are frequently recovered intact, implying physiological adaptations to periodic hypoxia. As global climates cooled during the , particularly from the onward, elasmosaurids persisted in temperate to cool high-latitude seas, with distributions suggesting adaptability to shifting thermal regimes across epicontinental systems. Their presence in both northern Boreal-connected waters and southern extensions of the aligns with broader cooling trends, potentially involving seasonal movements between warmer equatorial margins and cooler shelves to optimize foraging opportunities.

Paleobiology

Locomotion

Elasmosaurids achieved locomotion primarily through paddling, employing a subaqueous flying motion that generated via oscillatory movements of their enlarged, wing-like flippers, while the hindlimbs functioned mainly for and stability. This four-flipper propulsion system, where hind flippers operated in phase with fore flippers, enhanced overall by up to 60% and efficiency by 40% compared to forelimb-only , allowing effective cruising at estimated speeds of 1–2 m/s. Burst speeds could reach up to 5 m/s during short accelerations, though sustained high velocities were limited by their body plan. Their lightweight , characterized by reduced bone density and trabecular infilling, combined with an extensible structure, provided that minimized the need for constant propulsion and enabled prolonged with infrequent surfacing. Gastroliths, often present in specimens, further aided control by counteracting the positive buoyancy of the inflated lungs, particularly in stabilizing the long . During swimming, elasmosaurids maintained a horizontal body axis with the extended straight forward, which reduced hydrodynamic drag and optimized flow over the streamlined form; the played a minimal role in , serving instead for fine adjustments. This posture, informed by vertebral joint morphology, allowed efficient transit without the energy penalty of curved configurations. Energy efficiency models indicate that elasmosaurid locomotion incurred a lower metabolic cost than that of ichthyosaurs, owing to flipper aspect ratios of approximately 4–6, which favored sustained, low-speed cruising over rapid pursuits. These ratios, derived from limb elements, reflect adaptations for oscillatory lift-based rather than drag-based rowing.

Feeding ecology

Elasmosaurids were primarily piscivorous predators, consuming small schooling fish such as Enchodus and clupeomorphs, along with cephalopods like squid and belemnites, and occasionally ammonites. Direct evidence comes from preserved stomach contents in specimens from the Late Cretaceous Pierre Shale, where disarticulated fish bones and scales indicate ingestion of nektonic prey less than 50 cm in length. In related plesiosauroids, coprolites and gastric residues further support a diet incorporating ammonite jaws and soft-bodied cephalopods, suggesting opportunistic predation on abundant marine invertebrates. Hunting strategies likely involved ambush tactics, utilizing the elongated for lateral sweeps to intercept schools in open water or probing seabeds for demersal prey. Gastroliths, polished stones accumulated in the , aided gastric processing through of soft-bodied prey, with specimens preserving up to 95 stones totaling 6.8 kg in a single individual. Other elasmosaurid examples document hundreds of gastroliths, such as 253 stones weighing 8.3 kg or 2,626 stones at 3.0 kg, though their mass rarely exceeded 0.2% of estimated body weight, supporting a role in mechanical rather than significant . Stable carbon isotope (δ¹³C) analyses of elasmosaurid reveal values around -10.2‰ to -12.5‰, positioning them as mid-level predators in offshore marine food webs, with depleted signatures indicating in open oceanic environments rather than coastal zones. These values overlap with those of mosasaurs, suggesting shared trophic niches as secondary to apex consumers preying on and . Within Elasmosauridae, the subfamily Aristonectinae exhibited specialized benthic filter feeding on small crustaceans and plankton, in contrast to the pelagic piscivory of elasmosaurines. Their robust crania, numerous small triangular teeth forming an interlocking sieve, and restricted gape (<20°) facilitated engulfment and filtration of sediment-laden water to capture prey, marking a derived adaptation for near-bottom foraging in shallow marine settings.

Sensory and behavioral inferences

Elasmosaurids possessed large orbits positioned laterally but with some anterior orientation, enabling a wide and potentially limited for underwater prey detection.023%5B0883:TPANES%5D2.0.CO;2.short) This adaptation likely supported acute in marine environments, where light penetration was limited, allowing individuals to track schooling or navigate complex habitats. Olfactory capabilities were enhanced by elongated external nares and internal palatal grooves that channeled water flow toward the olfactory chambers, facilitating hydrodynamically driven underwater olfaction. Brain endocasts from specimens like Terminonatator ponteixensis reveal expanded olfactory bulbs and tracts, indicating a keen for locating prey or mates over distances.023%5B0883:TPANES%5D2.0.CO;2.short) No direct evidence exists for electroreceptive organs in elasmosaurids, unlike in some ichthyosaurs, suggesting reliance on other sensory modalities for close-range detection. Vibration sensitivity may have been mediated by skin structures analogous to the system in fishes, inferred from the smooth, scaleless integument preserved in related plesiosaurs. Reproductive behavior likely involved , as evidenced by the narrow pelvic girdle restricting egg passage and direct documentation of intrauterine embryos in closely related plesiosaurs, implying live birth in a single, large offspring to minimize predation risk in open marine settings. histology reveals rapid early growth rates, with local apposition rates of approximately 94 μm/day in elasmosaur specimens, supporting sustained linear increases of around 10 cm per year during and indicating elevated metabolic rates consistent with endothermy. High is suggested by the abundance of juvenile remains in some assemblages, potentially reflecting environmental pressures in coastal or shelf habitats. Ontogenetic changes in neck proportions enhanced maneuverability in juveniles, where cervical centra exhibited lower vertebral length indices (VLI ≈ 90–100) and relatively shorter, more robust for agile swimming and prey capture in shallow waters. In adults, positive allometric growth elongated mid-cervical centra (VLI >135), resulting in up to 7 meters long suited for slow, cruising foraging strategies over broader oceanic ranges, with increased variability in centrum length reflecting adaptive flexibility. This shift underscores a life history transition from high-mobility youth to energy-efficient patrolling.

Fossil record

History of discovery

The discovery of Elasmosauridae began in the late with the unearthing of the type specimen of platyurus by U.S. Army surgeon Theophilus H. Turner in spring 1867, near Fort Wallace in western , from the Sharon Springs Member of the Pierre Shale Formation (). Turner collected the nearly complete skeleton, which included over 130 vertebrae, and shipped it to paleontologist in . Cope formally described the in 1869, naming it Elasmosaurus platyurus and initially reconstructing it with the head on the tail due to assembly errors, amid the intense "" rivalry with that spurred rapid fossil prospecting in North American deposits. The late 19th and early 20th centuries saw a boom in elasmosaurid discoveries from North American chalk beds, particularly the Niobrara and formations, as quarrying and scientific expeditions intensified. Specimens from these sites revealed additional diversity, including material later assigned to snowii, which Samuel P. Welles named in 1943 based on a well-preserved from the Niobrara Chalk Formation (Smoky Hill Chalk Member) in western , notable for its 72 and complete . Further North American finds contributed to the recognition of Libonectes, with Jacobs and Stinmark describing Libonectes from the Eagle Ford Formation in in 1992, building on earlier Turonian-stage specimens that highlighted transatlantic distributions. Expansions in the extended elasmosaurid records beyond , with significant South American discoveries from the Allen and López de Bertodano formations. For instance, Gasparini, Salgado, and Casadio (2003) redescribed and analyzed Aristonectes material from , , confirming its elasmosaurid affinities and age through new specimens that refined the family's Gondwanan presence. In the , yielded Kaiwhekea katiki in 2002, described by Cruickshank and Fordyce from the Katiki Formation (), representing a high-latitude elasmosaurid and expanding the family's geographic range. Recent milestones include the 2012 description of Albertonectes vanderveldei by Kubo et al. from the in , , based on a nearly complete skeleton with a record 76 , underscoring ongoing discoveries in Western Interior deposits and solidifying Elasmosauridae's morphological extremes. Subsequent discoveries include Alexandronectes sarahae from the in 2021 and a new elasmosaurid from the in 2023, further highlighting post-Campanian diversity in and .

Key specimens and localities

The of Elasmosaurus platyurus (ANSP 10081) consists of a nearly complete , including fragments of the (premaxillae, parts of maxillae and dentaries, and the occipital condyle), 71 (forming the atlas-axis complex and postaxial series), and additional postcervical elements such as dorsal, sacral, and caudal vertebrae, along with fragments of the limb girdles (though the latter were lost due to historical mishandling during reconstruction). This specimen, exhibiting lateral compression in the mid- and dorsoventral crushing in the , was collected from the lower Pierre Shale near McAllaster in Logan County, Kansas, and is currently housed at the Academy of Natural Sciences in . A notable specimen of vanderveldei (holotype TMP 2007.011.0001), representing an almost complete postcranial skeleton with 76 cervical vertebrae—the highest count known among plesiosaurs—was recovered from the upper in , . This well-preserved individual, lacking the but featuring articulated vertebrae and partial limb elements, underscores the extreme neck elongation characteristic of advanced elasmosaurids and is housed at the Royal Tyrrell Museum of Palaeontology. The partial skull of parvidens (holotype MACN 6518) from the upper Campanian-lower Allen Formation in Patagonia, , preserves key cranial elements including the , braincase, and , revealing conical, peg-like teeth adapted for grasping soft-bodied prey. This specimen, collected from marine shales in , highlights the morphological diversity within aristonectine elasmosaurids and is stored at the Museo Argentino de Ciencias Naturales Bernardino Rivadavia in . The majority of Elasmosauridae fossils, including over two dozen described specimens, originate from Campanian-Maastrichtian marine shales of the North American , such as the Pierre Shale in and the in and , where exceptional preservation in fine-grained sediments has yielded articulated skeletons with associated gastroliths. Antarctic localities, including the on Vega Island, have produced several partial to complete elasmosaurid skeletons, such as a juvenile specimen (MLP 04-X-1-21-3) with preserved gastroliths, offering evidence of high-latitude habitation during the late . A recent discovery is the holotype of Traskasaura sandrae (RBCM.P2000.0001.001), a partial skeleton including a nearly complete skull, 42 cervical vertebrae, dorsal vertebrae, ribs, and partial limb elements, measuring approximately 12 meters in length, from the Santonian-stage Haslam Formation (~85 million years ago) on Vancouver Island, British Columbia, Canada. First unearthed in 1988, this basal elasmosaurid specimen, formally described in May 2025 by Druckenmiller et al., exhibits mosaic features bridging early and advanced elasmosaurids and suggests adaptations for diving to hunt ammonites; it is housed at the Royal BC Museum in Victoria, Canada, and represents one of the northernmost elasmosaurid finds, expanding knowledge of Santonian diversity in the Northeastern Pacific.

References

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