|Reconstructed skeleton of M. hoffmannii at the Maastricht Natural History Museum|
Species pending reassessment
List of synonyms
Mosasaurus (//; "lizard of the Meuse River") is the type genus (defining example) of the mosasaurs, an extinct group of aquatic squamate reptiles. It lived from about 82 to 66 million years ago during the Campanian and Maastrichtian stages of the Late Cretaceous. The earliest fossils of Mosasaurus known to science were found as skulls in a chalk quarry near the Dutch city of Maastricht in the late 18th century, which were initially thought to have been the bones of crocodiles or whales. One particular skull discovered around 1780, and which was seized by France during the French Revolutionary Wars for its scientific value, was famously nicknamed the "great animal of Maastricht". In 1808, naturalist Georges Cuvier concluded it belonged to a giant marine lizard with similarities to monitor lizards but otherwise unlike any known living animal. This concept was revolutionary at the time and helped support the then-developing ideas of extinction. However, Cuvier did not designate a scientific name for the new animal; this was done by William Daniel Conybeare in 1822 when he named it Mosasaurus in reference to its origin in fossil deposits near the Meuse River. The exact affinities of Mosasaurus as a squamate remain controversial, and scientists continue to debate whether its closest living relatives are monitor lizards or snakes.
Traditional interpretations have estimated the maximum length of the largest species, M. hoffmannii, to be up to 17.1 meters (56 ft), making it one of the largest mosasaurs. The skull of Mosasaurus was equipped with robust jaws capable of swinging back and forth and strong muscles capable of powerful bites using dozens of large teeth designed for cutting prey. Its four limbs were shaped into robust paddles to steer the animal underwater. Its tail was long and ended in a downward bend and a paddle-like fluke. Mosasaurus was a predator possessing excellent vision to compensate for its poor sense of smell, and a high metabolic rate suggesting it was endothermic ("warm-blooded"), an adaptation only found in mosasaurs among squamates. There is considerable morphological variability across the currently-recognized species in Mosasaurus—from the robustly-built M. hoffmannii to the slender and serpentine M. lemonnieri—but an unclear diagnosis (description of distinguishing features) of the types species M. hoffmannii led to a historically problematic classification. As a result, more than fifty different species have been attributed to the genus in the past. A redescription of the type specimen in 2017 helped resolve the taxonomy issue and confirmed at least five species to be within the genus. Another five species still nominally classified within Mosasaurus are planned to be reassessed in a future study.
Fossil evidence suggests Mosasaurus inhabited much of the Atlantic Ocean and the seaways adjacent to it. Continents where Mosasaurus fossils have been found include North America, South America, Europe, Africa, Western Asia, and Antarctica. This distribution encompassed a wide range of oceanic climates including tropical, subtropical, temperate, and subpolar climates. Mosasaurus was a common large predator in these oceans and was positioned at the top of the food chain. Paleontologists believe its diet would have included virtually any animal; it likely preyed on bony fish, sharks, cephalopods, birds, and other marine reptiles including sea turtles and other mosasaurs. It likely preferred to hunt in open water near the surface. From an ecological standpoint, Mosasaurus probably had a profound impact on the structuring of marine ecosystems; its arrival in some locations such as the Western Interior Seaway in North America coincides with a complete turnover of faunal assemblages and diversity. Mosasaurus faced competition with other large predatory mosasaurs such as Prognathodon and Tylosaurus—which were known to feed on similar prey—though they were able to coexist in the same ecosystems through niche partitioning. There were still conflicts among them, as an instance of Tylosaurus attacking a Mosasaurus has been documented. Several fossils document deliberate attacks on Mosasaurus individuals by members of the same species. Infighting likely took place in the form of snout grappling, similarly seen in modern crocodiles today.
Discovery and identification
The first Mosasaurus fossil known to science was discovered in 1764 in a chalk quarry near Maastricht, the Netherlands in the form of a skull, which was initially identified as a whale. Later around 1780,[a] the quarry produced a second skull that caught the particular attention of the physician Johann Leonard Hoffmann, who thought it was a crocodile. He contacted the prominent biologist Petrus Camper, and the skull gained international attention after Camper published a study identifing it as a whale. This caught the attention of French revolutionaries, who looted the fossil following the capture of Maastricht during the French Revolutionary Wars in 1794. In a 1798 narrative of this event by Barthélemy Faujas de Saint-Fond, the skull was allegedly retrieved by twelve grenadiers in exchange for an offer of 600 bottles of wine. This story helped elevate the fossil into cultural fame, but historians agree that the narrative was exaggerated.
After its seizure, the second skull was sent to the National Museum of Natural History, France in 1795 and later cataloged as MNHN AC 9648. By 1808, Camper's son Adriaan Gilles Camper and Georges Cuvier concluded that the fossil, which by then was nicknamed the "great animal of Maastricht," belonged to a marine lizard with affinities to monitor lizards, but otherwise unlike any modern animal. The skull became part of Cuvier's first speculations about the conception of extinction, which later led to his theory of catastrophism, a precursor to the theory of evolution. At the time, it was not believed that a species could go extinct, and fossils of animals were often interpreted as some form of an extant species. Cuvier's idea that there existed an animal unlike any today was revolutionary at the time, and in 1812 he proclaimed, "Above all, the precise determination of the famous animal from Maastricht seems to us as important for the theory of zoological laws, as for the history of the globe." William Daniel Conybeare coined the genus Mosasaurus in 1822, and Gideon Mantell added the specific epithet hoffmannii in 1829.[b] Cuvier later designated the second skull as the new species' holotype (defining example).
In 1804, the Lewis and Clark Expedition discovered a now-lost fossil skeleton alongside the Missouri River, which was identified as a 45-foot (14 m) long fish. Richard Ellis speculated in 2003 that this may have been the earliest discovery of the second species M. missouriensis, although competing speculations exist. In 1818, a fossil from Monmouth County, New Jersey became the first North American specimen to be correctly recognized as a Mosasaurus by scientists of the time.[c]
The type specimen of M. missouriensis was first described in 1834 by Richard Harlan based on a snout fragment found along the river's Big Bend. He coined the specific epithet and initially identified it as a species of Ichthyosaurus but later as an amphibian. The rest of the skull had been discovered earlier by a fur-trapper, and it eventually came under the possession of prince Maximilian of Weid-Neuwied between 1832 and 1834. The fossil was delivered to Georg August Goldfuss in Bonn for research, who published a study in 1845. The same year, Christian Erich Hermann von Meyer suspected that the skull and Harlan's snout were part of the same individual. This was eventually confirmed in 2004.
The third species was described in 1881 from fragmentary fossils in New Jersey by Edward Drinker Cope, who thought it was a giant species of Clidastes and named it Clidastes conodon. In 1966, it was reidentified as a species of Mosasaurus.
The fourth species M. lemonnieri was first detected by Camper Jr. based on fossils from his father's collections, which he discussed with Cuvier during their 1799 correspondence, but Cuvier rejected the idea of another Mosasaurus species. This species was re-introduced to science and formally described in 1889 by Louis Dollo based on a skull recovered from a phosphate quarry in Belgium. Further mining of the quarry in subsequent years uncovered many additional well-preserved fossils, including multiple partial skeletons which collectively represented nearly the entire skeleton of the species. They were described by Dollo in later papers. Despite being the best anatomically represented species, M. lemonnieri was largely ignored in scientific literature. Theagarten Lingham-Soliar suggested two reasons for this neglect. First, M. lemonnieri fossils are endemic to Belgium and the Netherlands, which despite the famous discovery of the M. hoffmannii holotype attracted little attention from mosasaur paleontologists. Second, the species was overshadowed by the more famous and history-rich type species.
M. lemonnieri is a controversial taxon, and there is debate on whether it is a distinct species or not. In 1967, Dale Russell argued that M. lemonnieri and M. conodon are the same species and designated the former as a junior synonym per the principle of priority. In a 2000 study, Lingham-Soliar refuted this based on a comprehensive study of existing M. lemonnieri specimens, which was corroborated by a study on the M. conodon skull by Ikejiri and Lucas in 2014. In 2004, Eric Mulder, Dirk Cornelissen, and Louis Verding suggested M. lemonnieri could be a juvenile form of M. hoffmannii based on the argument that significant differences could be explained by age-based variation. However, the need more research to confirm any hypotheses of synonymy was expressed.
Scientists during the early and mid-1800s initially imagined Mosasaurus as an amphibious marine reptile with webbed feet and limbs for walking. This was based on fossils like the M. missouriensis holotype, which indicated an elastic vertebral column that Goldfuss in 1845 saw as evidence of an ability to walk and interpretations of some phalanges as claws. In 1854, Hermann Schlegel proved how Mosasaurus actually had fully aquatic flippers. He clarified that earlier interpretations of claws were erroneous and demonstrated how the phalanges show no indication of muscle or tendon attachment, which would make walking impossible. They are also broad, flat, and form a paddle. Schlegel's hypothesis was largely ignored by contemporary scientists but became widely accepted by the 1870s when Othniel Charles Marsh and Cope uncovered more complete mosasaur remains in North America.
One of the earliest depictions of Mosasaurus in paleoart is a life-size concrete sculpture created by Benjamin Waterhouse Hawkins between 1852 and 1854 as part of the collection of sculptures of prehistoric animals on display at the Crystal Palace Park in London. The restoration was primarily informed by Richard Owen's interpretation of the M. hoffmannii holotype and the anatomy of monitor lizards, so Hawkins depicted the animal as essentially a water-going monitor lizard. It was given a boxy head, nostrils at the side of the skull, large volumes of soft tissue around the eyes, lips reminiscent of monitor lizards, scales consistent with those in large monitors like the Komodo dragon, and a flipper. The model was deliberately sculpted incomplete, which Mark Witton believed was likely to save time and money. Many elements of the sculpture can be considered inaccurate, even for the time. It did not take into account Golduss' 1845 study of M. missouriensis which instead called for a narrower skull, nostrils at the top of the skull, and amphibious terrestrial limbs (the latter being incorrect in modern standards).
Mosasaurus was a type of derived mosasaur, or a latecoming member with advanced evolutionary traits such as a fully aquatic lifestyle. As such, it had a streamlined body, an elongated tail ending with a downturn supporting a two-lobed fin, and two pairs of flippers. While in the past derived mosasaurs were depicted as akin to giant flippered sea snakes, it is now understood that they were more similar in build to other large marine vertebrates such as ichthyosaurs, marine crocodylomorphs, and archaeocete whales through convergent evolution.
The type species, M. hoffmannii, is one of the largest mosasaurs known, though knowledge of its skeleton remains incomplete as it is mainly known from skulls. Russell (1967) wrote that the length of the jaw equalled one tenth of the body length in the species. Based on this ratio, Grigoriev (2014) used the largest lower jaw attributed to M. hoffmannii (CCMGE 10/2469, also known as the Penza specimen; measuring 171 centimeters (67 in) in length) to estimate a maximum length of 17.1 meters (56 ft). Using a smaller partial jaw (NHMM 009002) measuring 90 centimeters (35 in) and "reliably estimated at" 160 centimeters (63 in) when complete, Lingham-Soliar (1995) estimated a larger maximum length of 17.6 meters (58 ft) via the same ratio.[d] No explicit justification for the 1:10 ratio was provided in Russell (1967). In 2014, Federico Fanti and colleagues alternatively argued that the total length of M. hoffmannii was more likely closer to seven times the length of the skull, which was based on a near-complete skeleton of the related species Prognathodon overtoni. The study estimated that an M. hoffmannii individual with a skull measuring 144 centimeters (57 in) would have measured 11 meters (36 ft) long or more.
Isolated bones suggest some M. hoffmannii may have exceeded the lengths of the Penza specimen. One such bone is a quadrate (NHMM 003892) which is 150% larger than the average size, which Everhart and colleagues in 2016 reported can be extrapolated to scale an individual around 18 meters (59 ft) in length. It was not stated whether they applied Russell's 1967 ratio.
M. missouriensis and M. lemonnieri are smaller than M. hoffmannii but are known from more complete fossils. Based on measurements of various Belgian skeletons, Dollo estimated M. lemonnieri grew to around 7 to 10 meters (23 to 33 ft) in length. He also measured the dimensions of IRSNB 3119 and recorded that the skull constituted approximately one-eleventh of the whole body. Polcyn et al. (2014) estimated that M. missouriensis may have measured up to 8–9 meters (26–30 ft) in length. Street (2016) noted that large M. missouriensis individuals typically had skulls exceeding lengths of 1 meter (3.3 ft). A particular near-complete skeleton of M. missouriensis is reportedly measured at 6.5 meters (21 ft) in total length; its skull approached 1 meter (3.3 ft) in length. Based on personal observations of various unpublished fossils from Morccoo, Nathalie Bardet estimated that M. beaugei grew to a total length of 8–10 meters (26–33 ft); their skulls typically measure around 1 meter (3.3 ft) in length. Valid explicit size estimates of M. conodon have not been recorded in the scientific literature, but with a skull measuring around 97.7 centimeters (38.5 in) in length, it has been regarded as a small to medium-sized representative of the genus.
The skull of Mosasaurus is conical and tapers off to a short snout which extends a little beyond the frontmost teeth. In M. hoffmannii, this snout is blunt, while in M. lemonnieri it is pointed. Above the gum line in both jaws, a single row of small pits known as foramina are lined parallel to the jawline; they are used to hold the terminal branches of jaw nerves. The foramina along the snout form a pattern similar to the foramina in Clidastes skulls. The upper jaws in most species are robustly built, broad, and deep except in M. conodon, where they are slender. The disparity is also reflected in the dentary, the lower jawbone, although all species share a long and straight dentary. In M. hoffmannii, the top margin of the dentary is slightly curved upwards; this is also the case with the largest specimens of M. lemonnieri, although more typical skulls of the species have a near-perfectly straight jawline. The premaxillary bar,[e] the long portion of the premaxillary bone extending behind the premaxillary teeth, is narrow and constricts near the middle in M. hoffmannii and M. lemonnieri like in typical mosasaurs. In M. missouriensis, the bar is robust and does not constrict. The external nares (nostril openings) are moderately sized and measure around 21–24% of the skull's length in M. hoffmannii. They are placed further toward the back of the skull than in nearly all other mosasaurs (exceeded only by Goronyosaurus), and begin above the fourth or fifth maxillary teeth. As a result, the rear portions of the maxilla (the main tooth-bearing bone of the upper jaw) lack the dorsal concavity that would fit the nostrils in typical mosasaurs.
The palate, which consists of the pterygoid bones, palatine bone, and nearby processes of other bones, is tightly packed to provide greater cranial stability. The neurocranium housed a brain which was narrow and relatively small compared to other mosasaurs. For example, the braincase of the mosasaur Plioplatecarpus marshi provided for a brain around twice the size of that in M. hoffmannii despite being only half the length of the latter. Spaces within the braincase for the occipital lobe and cerebral hemisphere are narrow and shallow, suggesting such brain parts were relatively small. The parietal foramen in Mosasaurus, which is associated with the parietal eye, is the smallest among mosasaurids. The quadrate bone, which connected the lower jaw to the rest of the skull and formed the jaw joint, is tall and somewhat rectangular in shape, differing from the rounder quadrates found in typical mosasaurs. The quadrate also housed the hearing structures, with the eardrum residing within a round and concave depression in the outer surface called the tympanic ala. The trachea likely stretched from the esophagus to below the back end of the lower jaw's coronoid process, where it split into smaller pairs of bronchi which extended parallel to each other.
The features of teeth in Mosasaurus vary across species, but unifying characteristics include a design specialized for cutting prey, highly prismatic surfaces (enamel circumference shaped by flat sides called prisms), and two opposite cutting edges. Mosasaurus teeth are large and robust except for those in M. conodon and M. lemonnieri, which instead have more slender teeth. The cutting edges of Mosasaurus differ by species. The cutting edges in M. hoffmannii and M. missouriensis are finely serrated, while in M. conodon and M. lemonnieri serrations do not exist.[f] The cutting edges of M. beaugei are neither serrated nor smooth, but instead possess minute wrinkles known as crenulations. The number of prisms in Mosasaurus teeth can slightly vary between tooth types and general patterns differ between species[g]—M. hoffmannii had two to three prisms on the labial side (the side facing outwards) and no prisms on the lingual side (the side facing the tongue), M. missouriensis had four to six labial prisms and eight lingual prisms, M. lemonnieri had eight to ten labial prisms, and M. beaugei had three to five labial prisms and eight to nine lingual prisms.
Like all mosasaurs, Mosasaurus had four types of teeth, classified based on the jaw bones they were located on. On the upper jaw, there were three types: the premaxillary teeth, maxillary teeth, and pterygoid teeth. On the lower jaw, only one type, the dentary teeth, were present. In each jaw row, from front to back, Mosasaurus had: two premaxillary teeth, twelve to sixteen maxillary teeth, and eight to sixteen pterygoid teeth on the upper jaw and fourteen to seventeen dentary teeth on the lower jaw. The teeth were largely consistent in size and shape with only minor differences throughout the jaws (homodont) except for the smaller pterygoid teeth. The number of teeth in the maxillae, pterygoids, and dentaries vary between species and sometimes even individuals—M. hoffmannii had fourteen to sixteen maxillary teeth, fourteen to fifteen dentary teeth, and eight pterygoid teeth; M. missouriensis had fourteen to fifteen maxillary teeth, fourteen to fifteen dentary teeth, and eight to nine pterygoid teeth; M. conodon had fourteen to fifteen maxillary teeth, sixteen to seventeen dentary teeth, and eight pterygoid teeth; M. lemonnieri had fifteen maxillary teeth, fourteen to seventeen dentary teeth, and eleven to twelve pterygoid teeth; and M. beaugei had twelve to thirteen maxillary teeth, fourteen to sixteen dentary teeth, and six or more pterygoid teeth. One indeterminate specimen of Mosasaurus similar to M. conodon from the Pembina Gorge State Recreation Area in North Dakota was found to have an unusual count of sixteen pterygoid teeth, far greater than in known species.
The dentition was thecodont (tooth roots deeply cemented within the jaw bone). Teeth were constantly shed through a process where the replacement tooth developed within the root of the original tooth and then pushed it out of the jaw. Chemical studies conducted on a M. hoffmannii maxillary tooth measured an average rate of deposition of odontoblasts, the cells responsible for the formation of dentin, at 10.9 micrometers (0.00043 in) per day. This was by observing the von Ebner lines, incremental marks in dentin that form daily. It was approximated that it took the odontoblasts 511 days and dentin 233 days to develop to the extent observed in the tooth.[h]
One of the most complete Mosasaurus skeletons in terms of vertebral representation (Mosasaurus sp.; SDSM 452) has seven cervical (neck) vertebrae, thirty-eight dorsal vertebrae (which includes thoracic and lumbar vertebrae) in the back, and eight pygal vertebrae (front tail vertebrae lacking haemal arches) followed by sixty-eight caudal vertebrae in the tail. All species of Mosasaurus have seven cervical vertebrae, but other vertebral counts vary among them. Various partial skeletons of M. conodon, M. hoffmannii, and M. missouriensis suggest M. conodon likely had up to thirty-six dorsal vertebrae and nine pygal vertebrae; M. hoffmannii had likely up to thirty-two dorsal vertebrae and ten pygal vertebrae;[i] and M. missouriensis around thirty-three dorsal vertebrae, eleven pygal vertebrae, and at least seventy-nine caudal vertebrae. M. lemmonieri had the most vertebrae in the genus, with up to around forty dorsal vertebrae, twenty-two pygal vertebrae, and ninety caudal vertebrae. Compared to other mosasaurs, the rib cage of Mosasaurus is unusually deep and forms an almost perfect semicircle, giving it a barrel-shaped chest. Rather than being fused together, extensive cartilage likely connected the ribs with the sternum, which would have facilitated breathing movements and compression when in deeper waters. The texture of the bones is virtually identical with in modern whales, which indicates Mosasaurus possessed a high range of aquatic adaptation and neutral buoyancy as seen in cetaceans.
The tail structure of Mosasaurus is similar to relatives like Prognathodon, in which soft tissue evidence for a two-lobed tail is known. The tail vertebrae gradually shorten around the center of the tail and lengthen behind the center, suggesting rigidness around the tail center and excellent flexibility behind it. Like most advanced mosasaurs, the tail bends slightly downwards as it approached the center, but this bend is offset from the dorsal plane at a small degree. Mosasaurus also has large haemal arches located at the bottom of each caudal vertebra which bend near the middle of the tail, which contrasts with the reduction of haemal arches in other marine reptiles such as ichthyosaurs. These and other features support a large and powerful paddle-like fluke in Mosasaurus.
The forelimbs of Mosasaurus are wide and robust. The scapula and humerus are fan-shaped and wider than tall. The radius and ulna are short, but the former is taller and larger than the latter. The ilium is rod-like and slender; in M. missouriensis, it is around 1.5 times longer than the femur. The femur itself is about twice as long as it is wide and ends at the distal side in a pair of distinct articular facets (of which one connects to the illium and the other to the paddle bones) that meet at an angle of approximately 120°. Five sets of metacarpals and phalanges (finger bones) were encased in and supported the paddles, with the fifth set being shorter and offset from the rest. The overall structure of the paddle is compressed, similar to in Plotosaurus, and was well-suited for faster swimming. In the hindlimbs, the paddle is supported by four sets of digits.
Interactive skeletal reconstruction of M. hoffmannii
(hover over or click on each skeletal component to identify the structure)
History of taxonomy
Because nomenclatural rules were not well-defined at the time, 19th century scientists did not give Mosasaurus a proper diagnosis during its initial descriptions, which led to ambiguity in how the genus is defined. This led Mosasaurus to become a wastebasket taxon containing as many as fifty different species. A 2017 study by Hallie Street and Michael Caldwell performed the first proper diagnosis and description of the M. hoffmannii holotype, which allowed a major taxonomic cleanup confirming five species as likely valid—M. hoffmannii, M. missouriensis, M. conodon, M. lemonnieri, and M. beaugei. The study also held four additional species from Pacific deposits—M. mokoroa, M. hobetsuensis, M. flemingi, and M. prismaticus—to be possibly valid, pending a future formal reassessment.[j] Street & Caldwell (2017) was derived from Street's 2016 doctoral thesis, which contained a phylogenetic study prosposing the constraining of Mosasaurus into four species—M. hoffmannii, M. missouriensis, M. lemonnieri, and a proposed new species 'M. glycys'—with M. conodon and the Pacific taxa belonging to different genera and M. beaugei being a synonym[k] of M. hoffmannii.[l]
Systematics and evolution
As the type genus of the family Mosasauridae and the subfamily Mosasaurinae, Mosasaurus is a member of the order Squamata (which comprises lizards and snakes). Relationships between mosasaurs and living squamates remain controversial as scientists still fiercely debate on whether the closest living relatives of mosasaurs are monitor lizards or snakes. Mosasaurus, along with mosasaur genera Eremiasaurus, Plotosaurus, and Moanasaurus[m] traditionally form a tribe within the Mosasaurinae variously called Mosasaurini or Plotosaurini.
Phylogeny and evolution of the genus
One of the earliest relevant attempts at an evolutionary study of Mosasaurus was done by Russell in 1967. He proposed that Mosasaurus evolved from a Clidastes-like mosasaur, and diverged into two lineages, one giving rise to M. conodon and another siring a chronospecies sequence which contained in order of succession M. ivoensis, M. missouriensis, and M. maximus-hoffmanni.[n][o] However, Russell used an early method of phylogenetics and did not use cladistics.
In 1997, Bell published the first cladistical study of North American mosasaurs. Incorporating the species M. missouriensis, M. conodon, M. maximus, and an indeterminate specimen (UNSM 77040), some of his findings agreed with Russell (1967), such as Mosasaurus descending from an ancestral group containing Clidastes and M. conodon being the most basal of the genus. Contrary to Russell (1967), Bell also recovered Mosasaurus in a sister relationship with another group which included Globidens and Prognathodon, and M. maximus as a sister species to Plotosaurus. The latter rendered Mosasaurus paraphyletic (an unnatural grouping), but Bell (1997) nevertheless recognized Plotosaurus as a distinct genus.
Bell's study served as a precedent for later studies that mostly left the systematics of Mosasaurus unchanged, although some later studies have recovered the sister group to Mosasaurus and Plotosaurus to instead be Eremiasaurus or Plesiotylosaurus depending on the method of data interpretation used, with at least one study also recovering M. missouriensis to be the most basal species of the genus instead of M. conodon. In 2014, Konishi and colleagues expressed a number of concerns with the reliance on Bell's study. First, the genus was severely underrepresented by incorporating only the three North American species M. hoffmannii/M. maximus, M. missouriensis, and M. conodon; by doing so, others like M. lemonnieri, which is one of the most completely known species in the genus, were neglected, which affected phylogenetic results. Second, the studies relied on an unclean and shaky taxonomy of the Mosasaurus genus due to the lack of a clear holotype diagnosis, which may have been behind the genus's paraphyletic status. Third, there was still a lack of comparative studies of the skeletal anatomy of large mosasaurines at the time. These problems were addressed in Street's 2016 thesis in an updated phylogenetic analysis.
Conrad uniquely used only M. hoffmannii and M. lemonnieri in his 2008 phylogenetic analysis, which recovered M. hoffmannii as basal to a multitude of descendant clades containing (in order of most to least basal) Globidens, M. lemonnieri, Goronyosaurus, and Plotosaurus. This result indicated that M. hoffmannii and M. lemonnieri are not in the same genus. However, the study used a method unorthodox to traditional phylogenetic studies on mosasaur species because its focus was on the relationships of entire squamate groups rather than mosasaur classification. As a result, some paleontologists caution that lower-order classification results from Conrad's 2008 study such as the specific placement of Mosasaurus may contain technical problems, making them inaccurate.
The following cladogram on the left (Topology A) is modified from a maximum clade credibility tree inferred by a Bayesian analysis in the most recent major phylogenetic analysis of the Mosasaurinae subfamily by Madzia & Cau (2017), which was self-described as a refinement of a larger study by Simões et al. (2017). The cladogram on the right (Topology B) is modified from Street's 2016 doctoral thesis proposing a revision to the Mosasaurinae, with proposed new taxa and renamings in single quotations.
|Maximum clade credibility tree by Madzia & Cau (2017)|
Positions of groups
Nominal Pacific species
Positions of individual taxa
Species traditionally referred as Mosasaurus conodon
Species traditionally referred as Plotosaurus bennisoni
|Proposed revision by Street (2016)|
Head musculature and mechanics
In 1995, Lingham-Soliar studied the head musculature of M. hoffmannii. Because soft tissue like muscles do not easily fossilize, reconstruction of the musculature was largely based on the structure of the skull, muscle scarring on the skull, and the musculature in extant monitor lizards.
In modern lizards, the mechanical build of the skull is characterized by a four-pivot geometric structure in the cranium that allows flexible movement of the jaws, possibly to allow the animals to better position them and prevent prey escape when hunting. In contrast, the frontal and parietal bones, which in modern lizards connect to form a flexible pivot point, overlap in the skull of M. hoffmannii. This creates a rigid three-pivot geometric cranial structure. These cranial structures are united by strong interlocking sutures formed to resist compression and shear forces caused by a downward thrust of the lower jaw muscles or an upward thrust of prey. This rigid but highly shock-absorbent structure of the cranium likely allowed a powerful bite force.
Like all mosasaurs, the lower jaws of Mosasaurus could swing forward and backward. In many mosasaurs like Prognathodon and M. lemonnieri, this function mainly served to allow ratchet feeding, in which the pterygoid and jaws would "walk" captured prey into the mouth like a conveyor belt. But especially compared to those in M. lemonnieri, the pterygoid teeth in M. hoffmannii are relatively small, which indicates ratchet feeding was relatively unimportant to its hunting and feeding. Rather, M. hoffmannii likely employed inertial feeding (in which the animal thrusts its head and neck backward to release a held prey item and immediately thrust the head and neck forward to close the jaws around the item) and used jaw adduction to assist in biting during prey seizure. The magnus adductor muscles, which attach to the lower jaws to the cranium and have a major role in biting function, are massive, indicating M. hoffmannii was capable of enormous bite forces. The long, narrow, and heavy nature of the lower jaws and attachment of tendons at the coronoid process would have allowed quick opening and closing of the mouth with little energy input underwater, which also contributed to the powerful bite force of M. hoffmannii and suggests it would not have needed the strong magnus depressor muscles (jaw-opening muscles) seen in some plesiosaurs.
Mobility and thermoregulation
Mosasaurus swam using its tail. The swimming style was likely sub-carangiform, which is exemplified today by mackerels. Its elongated paddle-like limbs functioned as hydrofoils for maneuvering the animal. The paddles' steering function was enabled by large muscle attachments from the outwards-facing side of the humerus to the radius and ulna and modified joints allowed an enhanced ability of rotating the flippers. The powerful forces resulting from utilization of the paddles may have sometimes resulted in bone damage, as evidenced by a M. hoffmannii ilium with significant separation of the bone's head from the rest of the bone likely caused by frequent shearing forces at the articulation joint.
The tissue structure of Mosasaurus' bones suggests it had a metabolic rate much higher than modern squamates and its resting metabolic rate was between that of the leatherback sea turtle and that of ichthyosaurs and plesiosaurs. Mosasaurus was likely endothermic and maintained a constant body temperature independent of the external environment. Although there is no direct evidence specific to the genus, studies on the biochemistry of related mosasaur genera such as Clidastes[p] suggests that endothermy was likely present in all mosasaurs. Such a trait is unique among squamates, the only known exception being the Argentine black and white tegu, which can maintain partial endothermy. This adaptation would have given several advantages to Mosasaurus, including increased stamina when foraging across larger areas and pursuing prey. It may have also been a factor that allowed Mosasaurus to thrive in the colder climates of locations such as Antarctica.
Mosasaurus had relatively large eye sockets with large sclerotic rings occupying much of the sockets' diameter; the latter is correlated with eye size and suggests it had good vision. The eye sockets were located at the sides of the skull, which created a narrow field of binocular vision at around 28.5° but alternatively allowed excellent processing of a two-dimensional environment, such as the near-surface waters inhabited by Mosasaurus.
Brain casts made from fossils of Mosasaurus show that the olfactory bulb and vomeronasal organ, which both control the function of smell, are poorly developed and lack some structures in M. hoffmannii; this indicates the species had a poor sense of smell. In M. lemonnieri, these olfactory organs, although still small, are better developed and have some components lacking in M. hoffmannii. The lack of a strong sense of smell suggests that olfaction was not particularly important in Mosasaurus; instead, other senses like vision may have been more useful.
Paleontologists generally agree that Mosasaurus was likely an active predator of a variety of marine animals. Fauna likely preyed upon by the genus include bony fish, sharks, cephalopods, birds, and marine reptiles such as other mosasaurs and turtles. It is unlikely Mosasaurus was a scavenger as it had a poor sense of smell. Mosasaurus was among the largest marine animals of its time, and with its large, robust cutting teeth, scientists believe larger members of the genus would have been able to handle virtually any animal. Lingham-Soliar (1995) suggested that Mosasaurus had a rather "savage" feeding behavior as demonstrated by large tooth marks on scutes of the giant sea turtle Allopleuron hoffmanni and fossils of re-healed fractured jaws in M. hoffmannii. The species likely hunted near the ocean surface as an ambush predator, using its large two-dimensionally adapted eyes to more effectively spot and capture prey. Chemical and structural data in the fossils of M. lemonnieri and M. conodon suggests they may have also hunted in deeper waters.
Carbon isotope studies on fossils of multiple M. hoffmannii individuals have found extremely low values of δ13C, the lowest in all mosasaurs for the largest individuals. Mosasaurs with lower δ13C values tended to occupy higher trophic levels, and one factor for this was dietary: a diet of prey rich in lipids such as sea turtles and other large marine reptiles can lower δ13C values. M. hoffmannii's low δ13C levels reinforces its likely position as an apex predator.
Currently, there is only one known example of a Mosasaurus preserved with stomach contents: a well-preserved partial skeleton of a small M. missouriensis dated about 75 million years old with dismembered and punctured remains of a 1 meter (3.3 ft) long fish in its gut. This fish was much longer than the length of the mosasaur's skull, which measured 66 centimeters (26 in) in length, confirming that M. missouriensis consumed prey larger than its head by dismembering and consuming bits at a time. Due coexistence with other large mosasaurs like Prognathodon, which specialized in robust prey, M. missouriensis likely specialized more on prey best consumed using cutting-adapted teeth in an example of niche partitioning.
Mosasaurus may have taught their offspring how to hunt, as supported by a fossil nautiloid Argonautilus catarinae with bite marks from two conspecific mosasaurs, one being from a juvenile and the other being from an adult. Analysis of the tooth marks by a 2014 study by Kauffman concluded that the mosasaurs were either Mosasaurus or Platecarpus. The positioning of both bite marks are at the direction the nautiloid's head would have been facing, indicating it was incapable of escaping and was thus already sick or dead during the attacks; it is possible this phenomenon was from a parent mosasaur teaching its offspring about cephalopods as an alternate source of prey and how to hunt one. An alternate explanation postulates the bite marks as from one individual mosasaur that lightly bit the nautiloid at first, then proceeded to bite again with greater force. However, there are differences in tooth spacing between both bites which indicate different jaw sizes.
Behavior and paleopathology
There is fossil evidence that Mosasaurus engaged in aggressive and lethal combat with other individuals of its kind. One particular fossil is of a partial M. conodon skeleton bearing multiple cuts, breaks, and punctures on various bones, particularly in the rear portions of the skull and neck, and a tooth from another M. conodon individual piercing through the quadrate bone. No injuries on the fossil show signs of healing, signifying that the mosasaur was killed by its attacker through a fatal blow in the skull. Another example is of a M. missouriensis skeleton with a tooth from another M. missouriensis embedded in the lower jaw underneath the eye. In this case, there were signs of healing around the wound, implying a survival of the incident. Takuya Konishi suggested an alternative cause of this example being head-biting behavior during courtship as seen in modern lizards.
Attacks by another Mosasaurus are a possible cause of physical pathologies in other skulls, but they could have instead arisen from other incidents like attempted biting on hard turtle shells. In 2004, Lingham-Soliar observed that if these injuries were indeed the result of an intraspecific attack, then there is a pattern of them concentrating in the skull region. Modern crocodiles commonly attack other crocodiles by grappling their opponent's head using their jaws, and Lingham-Soliar hypothesized that Mosasaurus employed similar head-grappling behavior during intraspecific combat. Many of the fossils with injuries possibly attributable to intraspecific combat are of juvenile or sub-adult Mosasaurus, leading to the possibility that attacks on smaller, weaker individuals may have been more common. However, the attacking mosasaurs of the M. conodon and M. missouriensis specimens were likely similar in size to the victims. In 2006, Schulp and colleagues speculated that Mosasaurus may have even occasionally engaged in cannibalism as a result of intraspecific aggression.
There are a number of M. hoffmannii jaws with evidence of infectious diseases as a result of physical injuries. Two examples include IRSNB R25 and IRSNB R27, both having fractures and other pathologies in their dentaries. IRSNB R25 preserves a complete fracture near the sixth tooth socket. Extensive amounts of bony callus almost overgrowing the tooth socket are present around the fracture along with various osteolytic cavities, abscess canals, damages to the trigeminal nerve, and inflamed erosions signifying severe bacterial infection. There are two finely ulcerated scratches on the bone callus, which may have developed as part of the healing process. IRSNB R27 has two fractures: one had almost fully healed and the other is an open fracture with nearby teeth broken off as a result. The fracture is covered with a nonunion formation of bony callus with shallow scratch marks and a large pit connected to an abscess canal. Lingham-Soliar described this pit as resembling a tooth mark from a possible attacking mosasaur. Both specimens show signs of deep bacterial infection alongside the fractures; some bacteria may have spread to nearby damaged teeth and caused tooth decay, which may have entered deeper tissue from prior post-traumatic or secondary infections. However, the dentaries ahead of the fractures in both specimens are in good condition, indicating that the arteries and trigeminal nerves had not been damaged; if they were, those areas would have necrotized due to a lack of blood. The dentaries' condition suggests that the species may have had an efficient process of immobilizing the fracture during healing, which likely helped prevent damage to vital blood vessels and nerves. This, along with signs of healing, also signifies that the fractures were not imminently fatal.
In 2006, Schulp and colleagues published a study describing a quadrate of M. hoffmannii with multiple unnatural openings and an estimated 0.5 liters (0.13 U.S. gal) of tissue destroyed. This was likely a severe bone infection initiated by septic arthritis, which progressed to the point where a large portion of the quadrate was reduced to abscess. Extensive amounts of bone reparative tissue were also present, suggesting the infection and subsequent healing process may have progressed for a few months. This level of bone infection would have been tremendously painful and severely hampered the mosasaur's ability to use its jaws. The location of the infection may have also interfered with respiration. Considering how the individual was able to survive such conditions for an extended period of time, Schulp and colleagues speculated it switched to a foraging-type diet of soft-bodied prey like squid that could be swallowed whole to minimize jaw usage. The cause of the infection remains unknown, but if it were a result of an intraspecific attack then it is possible one of the openings on the quadrate may have been the point of entry for an attacker's tooth from which the infection entered.
Avascular necrosis has been reported by many studies to be present in every examined specimen of M. lemonnieri and M. conodon. In examinations of M. conodon fossils from Alabama and New Jersey and M. lemonnieri fossils from Belgium, Rothschild and Martin in 2005 observed the condition affected between 3-17% of the vertebrae in the mosasaurs' spines. Avascular necrosis is a common result of decompression illness, caused by bone damage from the formation of gaseous nitrogen bubbles within inhaled air decompressed during frequent deep-diving trips or by intervals of repetitive diving and short breathing. This indicates both Mosasaurus species may have either been habitual deep-divers or repetitive divers. Agnete Weinreich Carlsen considered it the simplest explanation that such conditions were a product of inadequate anatomical adaptation. Nevertheless, fossils of other mosasaurs with invariable avascular necrosis still exhibit substantial adaptations like developed eardrums that were well-protected from rapid changes in pressure.
Unnatural fusion of tail vertebrae has been documented in Mosasaurus, which occurs when the bones remodel themselves after damage from trauma or disease. A 2015 study by Rothschild and Everhart surveyed 15 Mosasaurus specimens from North America and Belgium and found cases of fused tail vertebrae in three of them.[q] Two of these cases displayed irregular surface deformities around the fusion site caused by drainage of the vertebral sinuses, which is indicative of a bone infection. The causes of such infections are uncertain, but records of fused vertebrae in other mosasaurs suggest attacks by sharks and other predators as a possible candidate. The third case was determined to be caused by a form of arthritis based on the formation of smooth bridging between fused vertebrae.
It is likely that Mosasaurus was viviparous (giving live birth) like most modern mammals today. There is no evidence for live birth in Mosasaurus itself, but it is known in a number of other mosasaurs; examples include a skeleton of a pregnant Carsosaurus, a Plioplatecarpus fossil associated with fossils of two mosasaur embryos, and fossils of newborn Clidastes from pelagic (open ocean) deposits. Such fossil records, along with a total absence of any evidence suggesting external egg-based reproduction, indicates the likeliness of viviparity in Mosasaurus. Microanatomical studies on bones of juvenile Mosasaurus and related genera have found their bone structures to be comparable to adults and do not exhibit the bone mass increase found in juvenile primitive mosasauroids to support buoyancy and associated with a lifestyle in shallow water, signifying that Mosasaurus was precocial: they were already efficient swimmers and lived fully functional lifestyles in open water at a very young age, and did not require nursery areas to raise their young. However, a number of localities in Europe and South Dakota have yielded concentrated assemblages of juvenile M. hoffmannii, M. missouriensis and/or M. lemonnieri. These localities are all shallow ocean deposits, suggesting that juvenile Mosasaurus may have still lived in shallow waters.
Distribution, ecosystem, and ecological impact
Mosasaurus had a transatlantic distribution, with its fossils having been found in marine deposits on both sides of the Atlantic Ocean. These localities include the Midwestern and East Coast of the United States of the United States, Canada, Europe, Turkey, Russia, the Levant, the African coastline from Morocco to South Africa, Brazil, Argentina, and Antarctica. During the Late Cretaceous, the aforementioned regions made up the three seaways inhabited by Mosasaurus: the Atlantic Ocean, the Western Interior Seaway, and the Mediterranean Tethys. Multiple oceanic climate zones encompassed the seaways, including tropical, subtropical, temperate, and subpolar climates. The wide range of oceanic climates yielded a large diversity of fauna that coexisted with Mosasaurus.
The Mediterranean Tethys during the Maastrichtian stage was located in what is now Europe, Africa, and the Middle East. In recent studies, the confirmation of paleogeographical affinities extended this range to areas across the Atlantic including Brazil and the East Coast state of New Jersey. It is geographically subdivided into two biogeographic provinces that respectively include the northern and southern Tethyan margins. The two mosasaurs Mosasaurus and Prognathodon appear to have been the dominant taxa, being widespread and ecologically diversified throughout the seaway.
The northern Tethyan margin was located around the paleolatitudes of 30–40°N, consisting of what is now the European continent, Turkey, and New Jersey. At the time, Europe was a scattering of islands with most of the modern continental landmass being underwater. The margin provided a warm-temperate climate with habitats dominated by mosasaurs and sea turtles. M. hoffmannii and Prognathodon sectorius were the dominant species in the northern province. In certain areas such a Belgium, other Mosasaurus species like M. lemonnieri were instead the dominant species, where it's occurrences greatly outnumber those of other large mosasaurs.  Other mosasaurs found in the European side of the northern Tethyan margin include smaller genera such as Halisaurus, Plioplatecarpus, and Platecarpus; the shell-crusher Carinodens; and larger mosasaurs of similar trophic levels including Tylosaurus bernardi and four other species of Prognathodon. Sea turtles such as Allopleurodon hoffmanni and Glyptochelone suickerbuycki were also prevalent in the area and other marine reptiles including indeterminate elasmosaurs have been occasionally found. Marine reptile assemblages in the New Jersey region of the province are generally equivalent with those in Europe; the mosasaur faunae are quite similar but exclude M. lemonnieri, Carinodens, Tylosaurus, and certain species of Halisaurus and Prognathodon. In addition, they exclusively feature M. conodon, Halisaurus platyspondylus and Prognathodon rapax. Many types of sharks such as Squalicorax, Cretalamna, Serratolamna, and sand sharks, as well as bony fish such as Cimolichthys, the saber-toothed herring Enchodus, and the swordfish-like Protosphyraena are represented in the northern Tethyan margin.
The southern Tethyan margin was located along the equator between 20°N and 20°S, resulting in warmer tropical climates. Seabeds bordering the cratons in Africa and Arabia and extending to the Levant and Brazil provided vast shallow marine environments. These environments were dominated by mosasaurs and marine side-necked turtles. Of the mosasaurs, Globidens phosphaticus is the characteristic species of the southern province; in the African and Arabian domain, Halisaurus arambourgi and 'Platecarpus ptychodon'[r] were also common mosasaurs alongside Globidens. Mosasaurus was not well-represented: the distribution of M. beaugei was restricted to Morocco and Brazil and isolated teeth from Syria suggested a possible presence of M. lemonnieri, although M. hoffmannii also had some presence throughout the province. Other mosasaurs from the southern Tethyan margin include the enigmatic Goronyosaurus, the shell-crushers Igdamanosaurus and Carinodens, Eremiasaurus, four other species of Prognathodon, and various other species of Halisaurus. Other marine reptiles such as the marine monitor lizard Pachyvaranus and the sea snake Palaeophis are known there. Aside from Zarafasaura in Morocco, plesiosaurs were scarce. As a tropical area, bony fish such as Enchodus and Stratodus and various sharks were common throughout the southern Tethyan margin.
Western Interior Seaway
Many of the earliest fossils of Mosasaurus were found in Campanian stage deposits in North America, including what was once the Western Interior Seaway, an inland sea which flowed through what is now the central United States and Canada and connected the Arctic Ocean to the modern-day Gulf of Mexico. The region was rather shallow for a seaway, reaching a maximum depth of about 800–900 meters (2,600–3,000 ft). Extensive drainage from the neighboring continents, Appalachia and Laramidia, brought in vast amounts of sediment. Together with the formation of a nutrient-rich deepwater mass from the mixing of continental freshwater, Arctic waters from the north, and warmer saline Tethyan waters from the south, this created a warm and highly-productive seaway that supported a rich diversity of marine life.
The biogeography of the region has been generally subdivided into two Interior Subprovinces characterized by different climates and faunal structures, and their borders are separated in modern-day Kansas. The oceanic climate of the Northern Interior Subprovince was likely a cool temperate one, while the Southern Interior Subprovince had warm temperate to subtropical climates. The fossil assemblages throughout these regions suggest a complete faunal turnover when M. missouriensis and M. conodon appeared at 79.5 Ma, indicating that the presence of Mosasaurus in the Western Interior Seaway had a profound impact on the restructuring of marine ecosystems. The faunal structure of both provinces was generally much more diverse prior to the appearance of Mosasaurus, during a faunal stage known as the Niobraran Age, than it was during the following Navesinkan Age.
In what is now modern-day Alabama within the Southern Interior Subprovince, most of the key genera including sharks like Cretoxyrhina and the mosasaurs Clidastes, Tylosaurus, Globidens, Halisaurus, and Platecarpus disappeared and were replaced by Mosasaurus. During the Navesinkan Age, Mosasaurus dominated the entirety of the region, accounting for around two-thirds of all mosasaur diversity with Plioplatecarpus and Prognathodon sharing the remaining third. The Northern Interior Subprovince also saw a restructuring of mosasaur assemblages, characterized by the disappearance of mosasaurs like Platecarpus and their replacement by Mosasaurus and Plioplatecarpus. Some Niobraran genera such as Tylosaurus, Cretoxyrhina, hesperornithids, and plesiosaurs including elasmosaurs such as Terminonatator and polycotylids like Dolichorhynchops maintained their presence until around the end of the Campanian, during which the entire Western Interior Seaway started receding from the north. Mosasaurus continued to be the dominant genus in the seaway until the end of the Navesinkan Age at the end of the Cretaceous. Contemporaneous fauna included sea turtles such as Protostega and Archelon; many species of sea birds including Baptornis, Ichthyornis, and Halimornis; sharks such as the mackerel sharks Cretalamna, Squalicorax, Pseudocorax, and Serratolamna, the goblin shark Scapanorhynchus, the sand tiger Odontaspis, and the sawfish-like Ischyrhiza; and bony fish such as Enchodus, Protosphyraena, Stratodus, and the ichthyodectids Xiphactinus and Saurodon.
Mosasaurus is known from late Maastrichtian deposits in the Antarctic Peninsula, specifically the López de Bertodano Formation in Seymour Island. Located within the Antarctic polar circle at around ~65°S latitude, temperatures at medium to large water depths would have been around 6 °C (43 °F) on average, while sea surface temperatures may have dropped below freezing and sea ice may have formed at times. At least two species of Mosasaurus have been described, but the true number of species is unknown as remains are often fragmentary and specimens are described in open nomenclature. These species include one comparable with M. lemonnieri and another that appears to be closely related to M. hoffmannii. Mosasaurus appears to be the most diverse mosasaur in the Maastrichtian Antarctica. At least four other mosasaur genera have been reported in Antarctica, including Plioplatecarpus, the mosasaurines Moanasaurus and Liodon, and Kaikaifilu. However, the validity of some of these genera is disputed as they are primarily based on isolated teeth. Prognathodon and Globidens are also expected to be present based on distribution trends of both genera, although conclusive fossils have yet to be found. Other Antarctic marine reptiles included elasmosaurid plesiosaurs like Aristonectes and another indeterminate elasmosaurid. The fish assemblage of the López de Bertodano Formation was dominated by Enchodus and ichthyodectiformes.
Known fossils of Mosasaurus have typically been recovered from deposits representing nearshore habitats during the Cretaceous period, with some fossils coming from deeper-water deposits. Lingham-Soliar (1995) elaborated on this, finding that Maastrichtian deposits in the Netherlands with M. hoffmannii occurrences represented nearshore waters around 40–50 meters (130–160 ft) deep. Changing temperatures and an abundance in marine life were characteristic of these localities. The morphological build of M. hoffmannii, nevertheless, was best adapted for a pelagic surface lifestyle.
δ13C is also correlated with a marine animal's feeding habitat as isotope levels deplete when habitat is farther from the shoreline, so some scientists interpreted isotope levels as a proxy for habitat preference. Separate studies involving multiple Mosasaurus specimens have yielded consistently low δ13C levels of tooth enamel, indicating that Mosasaurus fed in more offshore or open waters. It has been pointed out how δ13C can be influenced by other factors in an animal's lifestyle, such as diet and diving behavior. To account for this, a 2014 study by T. Lynn Harrell Jr. and Alberto Perez-Huerta examined the concentration ratios of neodymium, gadolinium, and ytterbium in M. hoffmannii and Mosasaurus sp. fossils from Alabama, the Demopolis Chalk, and the Hornerstown Formation. Previous studies demonstrated that ratios of these three elements can act as a proxy for relative ocean depth of a fossil during early diagenesis without interference from biological processes, with each of the three elements signifying either shallow, deep, or fresh waters. The rare earth element ratios were very consistent throughout most of the examined Mosasaurus fossils, indicating consistent habitat preference, and clustered towards a ratio representing offshore habitats with ocean depths between or deeper than 50–150 meters (160–490 ft).
Mosasaurus lived alongside other large predatory mosasaurs also considered apex predators, most prominent among them being the tylosaurines and Prognathodon. Tylosaurus bernardi, the only surviving species of the genus during the Maastrichtian, measured up to 12.2 meters (40 ft) in length while the largest coexisting species of Prognathodon like P. saturator exceeded 12 meters (39 ft). These three mosasaurs preyed on similar animals such as marine reptiles.
A study published in 2013 by Schulp and colleagues specifically tested how mosasaurs such as M. hoffmannii and P. saturator were able to coexist in the same localities through δ13C analysis. The scientists utilized an interpretation that differences in isotope values can help explain the level of resource partitioning because it is influenced by multiple environmental factors such as lifestyle, diet, and habitat preference. Comparisons between the δ13C levels in multiple teeth of M. hoffmannii and P. saturator from the Maastrichtian-age Maastricht Formation showed that while there was some convergence between certain specimens, the average δ13C values between the two species were on average different. This is one indication of niche partitioning, where the two mosasaur genera likely foraged in different habitats or had different specific diets to coexist without direct competitive conflict. The teeth of P. saturator are much more robust than those of M. hoffmannii and were specifically equipped for preying on robust prey like turtles. While M. hoffmannii also preyed on turtles, its teeth were built to handle a wider range of prey less suited for P. saturator.
Another case of presumed niche partitioning between Mosasaurus and Prognathodon from the Bearpaw Formation in Alberta was documented in a 2014 study by Konishi and colleagues. The study found a dietary divide between M. missouriensis and Prognathodon overtoni based on stomach contents. Stomach contents of P. overtoni included turtles and ammonites, providing another example of a diet specialized for harder prey. In contrast, M. missouriensis had stomach contents consisting of fish, indicative of a diet specialized in softer prey. It was hypothesized that these adaptations helped maintain resource partitioning between the two mosasaurs.
Nevertheless, competitive engagement evidently could not be entirely avoided. There is also evidence of aggressive interspecific combat between Mosasaurus and other large mosasaur species. This is shown from a fossil skull of a subadult M. hoffmannii with fractures caused by a massive concentrated blow to the braincase; Lingham-Soliar (1998) argued that this blow was dealt by a ramming attack by Tylosaurus bernardi, as the formation of the fractures were characteristic of a coordinated strike (and not an accident or fossilization damage), and T. bernardi was the only known coexisting animal likely capable of causing such damage, using its robust arrow-like elongated snout. This sort of attack has been compared to the defensive behavior of bottlenose dolphins using their beaks to kill or repel lemon sharks, and it has been speculated that T. bernardi dealt the offensive attack via an ambush on an unsuspecting Mosasaurus.
By the end of the Cretaceous, mosasaurs like Mosasaurus were at the height of their evolutionary radiation, and their extinction was a sudden event. During the late Maastrichtian, global sea levels dropped, which drained the continents of their nutrient-rich seaways and altered circulation and nutrient patterns, reducing the number of available habitats for Mosasaurus. The genus endured by accessing new habitats in more open waters. The geologically youngest fossils of Mosasaurus, which include those of M. hoffmannii and indeterminate species, occur up to the Cretaceous-Paleogene boundary (K-Pg boundary). The demise of the genus was likely a result of the Cretaceous-Paleogene extinction event which also wiped out the non-avian dinosaurs. Localities where Mosasaurus fossils have been found less than 15 meters (49 ft) below the boundary include the Maastricht Formation, the Davutlar Formation in Turkey, the Jagüel Formation in Argentina, Stevns Klint in Denmark, Seymour Island, and Missouri.
M. hoffmannii fossils have been found within the K-Pg boundary itself in southeastern Missouri between the Paleocene Clayton Formation and Cretaceous Owl Creek Formation. Fossil vertebrae from the layer were found with fractures formed after death. The layer itself was likely deposited as a tsunamite, alternatively nicknamed the "Cretaceous cocktail deposit". This means it formed through a combination of catastrophic seismic and geological disturbances, mega-hurricanes, and giant tsunamis as direct consequences of the impact of the Chicxulub asteroid that catalyzed the K-Pg extinction event. Aside from the physical destruction of these events, the impact also had subsequent environmental reverberations like blocking out sunlight leading to a collapse of marine food webs. Any Mosasaurus surviving the immediate cataclysms by taking refuge in deeper waters would have eventually died out due to starvation from a total loss of prey.
One enigmatic occurrence of Mosasaurus sp. fossils is in the Hornerstown Formation, a deposit typically dated to be from the Paleocene Danian age, which was immediately after the Maastrichtian age. The fossils were found in association with fossils of Squalicorax, Enchodus, and various ammonites within a uniquely fossil-rich bed at the base of the Hornerstown Formation known as the Main Fossiliferous Layer. This does not mean Mosasaurus and its associated fauna survived the K-Pg extinction. According to one hypothesis, the fossils may actually have originated from an earlier Cretaceous deposit and were reworked into the Paleocene formation during its early deposition. Evidence of reworking typically comes from fossils worn down due to further erosion during their exposure at the time of redeposition. Many of the Mosasaurus fossils from the Main Fossiliferous Layer consist of isolated bones commonly abraded and worn; however, the layer also yielded better-preserved Mosasaurus remains. Another explanation suggests the Main Fossiliferous Layer is a Maastrichtian time-averaged remanié deposit, which means it originated from a Cretaceous deposit with winnowed low-sediment conditions. A third hypothesis proposes that the layer is a lag deposit of Cretaceous sediments forced out by a strong impact by a tsunami, and what remained was subsequently refilled with Cenozoic fossils.
- The exact year is not fully certain due to multiple contradicting claims. An examination of existing historical evidence by Pieters et al., (2012) suggested the most accurate date would be on or around 1780. More recently, Limburg newspapers reported in 2015 that Ernst Homburg discovered a Liège magazine issued in the October 1778 reporting in detail a recent discovery of the second skull.
- hoffmannii was the original spelling used by Mantell, ending with -ii. Later authors began to drop the final letter and spelled it as hoffmanni, as became the trend for specific epithets of similar structure in later years. Recent scientists argue that the special etymological makeup of hoffmannii cannot be subjected to International Code of Zoological Nomenclature Articles 32.5, 33.4, or 34, which would normally protect similar respellings. This makes hoffmannii the valid spelling, although hoffmanni continues to be incorrectly used by many authors.
- Because the genus Mosasaurus was not coined at the time, the original identifier, Samuel L. Mitchill, described the fossil as a lizard monster or saurian animal resembling the famous fossil reptile of Maestricht [sic]." Cuvier doubted whether the two specimens were related. The congeneric relationship was eventually confirmed by James Ellsworth De Kay in 1830, and the New Jersey fossil was named Mosasaurus dekayi in his honor. The taxon was declared a nomen dubium in 2005, and other fossils attributed to it were reidentified as M. hoffmannii.
- Lingham-Soliar may have misapplied the ratio. His calculations interpreted "body length" as the length of the postcranial body, not the total length of the animal as demonstrated in Russell (1967), This erroneously inflated the estimate by 10%.
- Also known as the internarial bar
- One specimen traditionally attributed to M. lemonnieri has serration-like features in its cutting edges. Scientists believe this specimen likely belongs to a different species.
- The number of prisms in M. conodon and number of lingual prisms in M. lemonnieri are uncertain.
- This study was conducted on only one tooth and may not represent the exact durations of dentinogenesis in all Mosasaurus teeth.
- The number of caudal vertebrae is not fully certain for M. conodon and M. hoffmannii. At least ten have been documented in M. conodon, while the count is completely unknown in M. hoffmannii.
- Street & Caldwell (2017) also included M. dekayi as a potentially valid species without addressing it's dubious status.
- Street & Caldwell (2017) revised this assessment of M. beaugei and found it to be a distinct species based on additional anatomical distinctions.
- As the proposal remains restricted to a PhD thesis, it is defined as an unpublished work per Article 8 of the ICZN and therefore is not yet formally valid.
- Some studies such as Madzia & Cau (2017) also recover Prognathodon and Plesiotylosaurus within the Mosasaurini.
- M. maximus is a North American taxon Russell (1967) recognized as a distinct species. It is now generally recognized as a junior synonym of M. hoffmannii, although some scientists maintain the taxon is a distinct species.
- maximus-hoffmannii was the wording used in Russell (1967); this is in recognition of the belief of a close relationship between the two species.
- The 2018 MS thesis of Cyrus Green disputes the notion that Clidastes was an endotherm based on the skeletochronology of the genus, finding its growth rates to be too low to be endothermic and instead similar to ectotherms. The dissertation argued that the high body temperatures calculated in pro-endoterm studies were a result of gigantothermy. However, only four specimens were studied.
- Two of the 15 surveyed fossils were reported from the Niobrara Formation, a deposit that Mosasaurus was previously thought but is no longer recognized to be present in.
- A dubious taxon that may represent various mosasaurs such as Gavialimimus or Platecarpus somenensis
- James G. Ogg; Linda A. Hinnov (2012). Cretaceous. The Geologic Time Scale 2012. pp. 793–853. doi:10.1016/B978-0-444-59425-9.00027-5. ISBN 9780444594259.
- William B. Gallagher (2005). "Recent mosasaur discoveries from New Jersey and Delaware, USA: stratigraphy, taphonomy and implications for mosasaur extinction". Netherlands Journal of Geosciences. 84 (3): 241–245. doi:10.1017/S0016774600021028.
- William B. Gallagher (1984). "Paleoecology of the Delaware Valley region, Part II: Cretaceous to Quaternary". The Mosasaur. 2 (1): 9–43.
- Christian C. Obasi; Dennis O. Terry Jr.; George H. Myer; David E. Grandstaff (2011). "Glauconite Composition and Morphology, Shocked Quartz, and the Origin of the Cretaceous(?) Main Fossiliferous Layer (MFL) in Southern New Jersey, U.S.A.". Journal of Sedimentary Research. 81 (1): 479–494. Bibcode:2011JSedR..81..479O. doi:10.2110/jsr.2011.42.
- Hallie P. Street; Michael W. Caldwell (2017). "Rediagnosis and redescription of Mosasaurus hoffmannii (Squamata: Mosasauridae) and an assessment of species assigned to the genus Mosasaurus". Geological Magazine. 154 (3): 521–557. Bibcode:2017GeoM..154..521S. doi:10.1017/S0016756816000236. S2CID 88324947.
- Joseph Leidy (1864). Cretaceous Reptiles of the United States. 14. Smithsonian Contributions to Knowledge. pp. 30–120.
- Hallie P. Street (2016). A re-assessment of the genus Mosasaurus (Squamata: Mosasauridae) (PDF) (PhD). University of Alberta. doi:10.7939/R31N7XZ1K.
- T. Lynn Harrell Jr.; James E. Martin (2014). "A mosasaur from the Maastrichtian Fox Hills Formation of the northern Western Interior Seaway of the United States and the synonymy of Mosasaurus maximus with Mosasaurus hoffmanni (Reptilia: Mosasauridae)". Netherlands Journal of Geosciences. 94 (1): 23–37. doi:10.1017/njg.2014.27. S2CID 131617632.
- Takuya Konishi; Michael Newbrey; Michael Caldwell (2014). "A small, exquisitely preserved specimen of Mosasaurus missouriensis (Squamata, Mosasauridae) from the upper Campanian of the Bearpaw Formation, western Canada, and the first stomach contents for the genus". Journal of Vertebrate Paleontology. 34 (4): 802–819. doi:10.1080/02724634.2014.838573. S2CID 86325001.
- Michael W. Caldwell; Gorden L. Bell Jr. (2005). "Of German princes and North American rivers: Harlan's lost mosasaur snout rediscovered". Netherlands Journal of Geosciences. 84 (3): 207–211. doi:10.1017/S0016774600020989.
- Takehito Ikejiri; Spencer G. Lucas (2014). "Osteology and taxonomy of Mosasaurus conodon Cope 1881 from the Late Cretaceous of North America". Netherlands Journal of Geosciences. 94 (1): 39–54. doi:10.1017/njg.2014.28. S2CID 73707936.
- Martinus van Marum (1790). Beschrijving der beenderen van den kop van eenen visch, gevonden in den St Pietersberg bij Maastricht, en geplaatst in Teylers Museum (in Dutch). 9. Verhandelingen Teylers Tweede Genootschap. pp. 383–389.
- Florence Pieters; Peggy G. W. Rompen; John W. M. Jagt; Nathalie Bardet (2012). "A new look at Faujas de Saint-Fond's fantastic story on the provenance and acquisition of the type specimen of Mosasaurus hoffmanni MANTELL, 1829". Bulletin de la Société Géologique de France. 183 (1): 55–65. doi:10.2113/gssgfbull.183.1.55.
- Vikkie Bartholomeus (September 21, 2015). "Datum vondst mosasaurus ontdekt: in oktober 1778". 1Limburg (in Dutch). Archived from the original on March 7, 2020.
- Eric Mulder (2004). Maastricht Cretaceous finds and Dutch pioneers in vertebrate palaeontology. Royal Netherlands Academy of Arts and Sciences. pp. 165–176.
- Petrus Camper (1786). "Conjectures relative to the petrifactions found in St. Peter's Mountain near Maestricht". Philosophical Transactions of the Royal Society of London. 76 (2): 443–456. doi:10.1098/rstl.1786.0026. ISSN 2053-9223.
- Florence F. J. M. Pieters (2009). "Natural history spoils in the Low Countries in 1794/95: the looting of the fossil Mosasaurus from Maastricht and the removal of the cabinet and menagerie of stadholder William V". Napoleon's legacy: the rise of national museums in Europe, 1794–1830 (PDF). 27. Berlin: G+H Verlag. pp. 55–72. ISBN 9783940939111.
- Mike Everhart (May 14, 2010). "Mosasaurus hoffmanni-The First Discovery of a Mosasaur?". Oceans of Kansas. Archived from the original on September 4, 2019. Retrieved November 6, 2019.
- Mark Evans (2010). "The roles played by museums, collections and collectors in the early history of reptile palaeontology". Geological Society, London, Special Publications. 343 (1): 5–29. Bibcode:2010GSLSP.343....5E. doi:10.1144/SP343.2. S2CID 84158087.
- Mike Everhart (October 21, 2013). "The Goldfuss Mosasaur". Oceans of Kansas. Archived from the original on June 2, 2019. Retrieved November 10, 2019.
- Richard Ellis (2003). Sea Dragons: Predators of the Prehistoric Oceans. University Press of Kansas. p. 216. ISBN 978-0700613946.
- Robert W. Meredith; James E. Martin; Paul N. Wegleitner (2007). The largest mosasaur (Squamata: Mosasauridae) from the Missouri River area (Late Cretaceous; Pierre Shale Group) of South Dakota and its relationship to Lewis and Clark (PDF). The Geological Society of America. pp. 209–214.
- James Ellsworth De Kay (1830). "On the Remains of Extinct Reptiles of the genera Mosasaurus and Geosaurus found in the secondary formation of New-Jersey; and on the occurrence of the substance recently named Coprolite by Dr. Buckland, in the same locality". Annals of the Lyceum of Natural History of New York. 3: 134–141.
- Heinrich Georg Bronn (1838). Lethaea Geognostica Oder Abbildungen und Beschreibungen Der für die Gebirgs-Formationen bezeichnendsten Versteinerungen (in German). 2. Stuttgart. p. 760. doi:10.5962/bhl.title.59080.
- Eric W. A. Mulder (1999). "Transatlantic latest Cretaceous mosasaurs (Reptilia, Lacertilia) from the Maastrichtian type area and New Jersey". Geologie en Mijnbouw. 78 (3/4): 281–300. doi:10.1023/a:1003838929257. S2CID 126956543.
- Richard Harlan (1834). "Notice of the Discovery of the Remains of the Ichthyosaurus in Missouri, N. A.". Transactions of the American Philosophical Society. 4: 405–408. JSTOR 1004839.
- Richard Harlan (1839). "Notice of the discovery of Basilosaurus and Batrachiotherium". Proceedings of the Geological Society of London. 3: 23–24.
- Edward Drinker Cope (1881). "A new species of Clidastes from New Jersey". American Naturalist. 15: 587–588.
- Donald Baird; Gerard R. Case (1966). "Rare marine reptiles from the Cretaceous of New Jersey". Journal of Paleontology. 40 (5): 1211–1215. JSTOR 1301995.
- Adriaan Gilles Camper (1812). "Mémoire sur quelques parties moins connues du squelette des sauriens fossiles de Maestricht". Annales du Muséum d'histoire naturelle (in French). 19: 215–241.
- Louis Dollo (1889). "Première note sur les Mosasauriens de Mesvin". Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie (in French). 3: 271–304. ISSN 0037-8909.
- Theagarten Lingham-Soliar (2000). "The Mosasaur Mosasaurus lemonnieri (Lepidosauromorpha, Squamata) from the Upper Cretaceous of Belgium and The Netherlands". Paleontological Journal. 34 (suppl. 2): S225–S237.
- Pablo Gonzalez Ruiz; Marta S. Fernandez; Marianella Talevi; Juan M. Leardi; Marcelo A. Reguero (2019). "A new Plotosaurini mosasaur skull from the upper Maastrichtian of Antarctica. Plotosaurini paleogeographic occurrences". Cretaceous Research. 103 (2019): 104166. doi:10.1016/j.cretres.2019.06.012. hdl:11336/125124.
- Dale A. Russell (1967). Systematics and morphology of American mosasaurs (PDF). 23. Bulletin of the Peabody Museum of Natural History. pp. 1–124.
- Daniel Madzia (2019). "Dental variability and distinguishability in Mosasaurus lemonnieri (Mosasauridae) from the Campanian and Maastrichtian of Belgium, and implications for taxonomic assessments of mosasaurid dentitions". Historical Biology. 32 (10): 1–15. doi:10.1080/08912963.2019.1588892. S2CID 108526638.
- Nathalie Bardet; Xabier Pereda Suberbiola; Mohamed Iarochene; Fatima Bouyahyaoui; Baadi Bouya; Mbarek Amaghzaz (2004). "Mosasaurus beaugei Arambourg, 1952 (Squamata, Mosasauridae) from the Late Cretaceous phosphates of Morocco". Geobios. 37 (2004): 315–324. doi:10.1016/j.geobios.2003.02.006.
- Eric Mulder; Bert Theunissen (1986). "Hermann Schlegel's investigation of the Maastricht mosasaurs". Archives of Natural History. 13 (1): 1–6. doi:10.3366/anh.1918.104.22.168.
- Mark Witton (May 17, 2019). "The science of the Crystal Palace Dinosaurs, part 2: Teleosaurus, pterosaurs and Mosasaurus". Mark Witton.com. Archived from the original on June 3, 2019.
- Emily Osterloff. "The world's first dinosaur park: what the Victorians got right and wrong". Archived from the original on April 18, 2021.
- Dimitry V. Grigoriev (2014). "Giant Mosasaurus hoffmanni (Squamata, Mosasauridae) from the Late Cretaceous (Maastrichtian) of Penza, Russia" (PDF). Proceedings of the Zoological Institute RAS. 318 (2): 148–167.
- Johan Lindgren; Michael W. Caldwell; Takuya Konishi; Luis M. Chiappe (2010). "Convergent Evolution in Aquatic Tetrapods: Insights from an Exceptional Fossil Mosasaur". PLOS ONE. 5 (8): e11998. Bibcode:2010PLoSO...511998L. doi:10.1371/journal.pone.0011998. PMC 2918493. PMID 20711249.
- Michael W. Caldwell (2012). "A challenge to categories: "What, if anything, is a mosasaur?"". Bulletin de la Société Géologique de France. 183 (1): 17–34. doi:10.2113/gssgfbull.183.1.7.
- Johan Lindgren; Michael J. Polcyn; Bruce A. Young (2011). "Landlubbers to leviathans: evolution of swimming in mosasaurine mosasaurs". Paleobiology. 37 (3): 445–469. doi:10.1666/09023.1. S2CID 85165085.
- Theagarten Lingham-Soliar (1995). "Anatomy and functional morphology of the largest marine reptile known, Mosasaurus hoffmanni (Mosasauridae, Reptilia) from the Upper Cretaceous, Upper Maastrichtian of The Netherlands". Philosophical Transactions of the Royal Society B. 347 (1320): 155–172. Bibcode:1995RSPTB.347..155L. doi:10.1098/rstb.1995.0019.
- Fedrico Fanti; Andrea Cau; Alessandra Negri (2014). "A giant mosasaur (Reptilia, Squamata) with an unusually twisted dentition from the Argille Scagliose Complex (late Campanian) of Northern Italy". Cretaceous Research. 49 (2014): 91–104. doi:10.1016/j.cretres.2014.01.003.
- Michael Everhart; John W. M. Jagt; Eric W. A. Mulder; Anne S. Schulp (2016). Mosasaurs—how large did they really get?. 5th Triennial Mosasaur Meeting—A Global Perspective on Mesozoic Marine Amniotes.
- Louis Dollo (1892). "Nouvelle note sur l'osteologie des mosasauriens". Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie (in French). 6: 219=259. ISSN 0037-8909.
- Michael J. Polcyn; Louis L. Jacobs; Ricardo Araújo; Anne S.Schulp; Octávio Mateus (2014). "Physical drivers of mosasaur evolution" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 400 (15): 17–27. Bibcode:2014PPP...400...17P. doi:10.1016/j.palaeo.2013.05.018.
- Michael D. D'Emic; Kathlyn M. Smith; Zachary T. Ansley (2015). "Unusual histology and morphology of the ribs of mosasaurs (Squamata)". Palaeontology. 58 (3): 511–520. doi:10.1111/pala.12157.
- Carolyn Gramling (October 26, 2016). "Ancient sea monster battle revealed in unusual fossil". Science. doi:10.1126/science.aal0310.
- Nathalie Bardet; Alexandra Houssaye; Peggy Vincent; Xabier Pereda Suberbiola; M'barek Amaghzaz; Essaid Jourani; Saïd Meslouh (2015). "Mosasaurids (Squamata) from the Maastrichtian Phosphates of Morocco: Biodiversity, palaeobiogeography and palaeoecology based on tooth morphoguilds". Gondwana Research. 27 (3): 1068–1078. Bibcode:2015GondR..27.1068B. doi:10.1016/j.gr.2014.08.014.
- Michael J. Everhart (January 1, 2010). "Mosasaur brain". Oceans of Kansas. Archived from the original on November 6, 2020.
- Anne S. Schulp; Hubert B. Vonhof; Jeroen van der Lubbe; Renée Janssen; Remy R. van Baal (2013). "On diving and diet: resource partitioning in type-Maastrichtian mosasaurs". Netherlands Journal of Geosciences. 92 (2–3): 165–170. doi:10.1017/S001677460000010X. S2CID 131884448.
- Anne S. Schulp; Michael J. Polcyn; Octavio Mateus; Louis L. Jacobs; Maria Lusia Morais; Tatiana da Silva Tavares (2006). "New mosasaur material from the Maastrichtian of Angola, with notes on the phylogeny, distribution, and paleoecology of the genus Prognathodon" (PDF). Publicaties van Het Natuurhistorisch Genootschap in Limburg. 45 (1): 57–67. ISSN 0374-955X.
- Clint A. Boyd (2017). "A New Addition to the Cretaceous Seaway of North Dakota" (PDF). Geo News. Vol. 44 no. 1. North Dakota Geological Society. pp. 20–23.
- Mike Everhart (March 26, 2009). "Samuel Wilson's Mosasaurus horridus". Oceans of Kansas. Archived from the original on June 2, 2021.
- Michael W. Caldwell (2007). "Ontogeny, anatomy and attachment of the dentition in mosasaurs (Mosasauridae: Squamata)". Zoological Journal of the Linnean Society. 149 (4): 687–700. doi:10.1111/j.1096-3642.2007.00280.x.
- Anusuya Chinsamy; Cemal Tunoǧlu; Daniel B. Thomas (2012). "Dental microstructure and geochemistry of Mosasaurus hoffmanni (Squamata: Mosasauridae) from the Late Cretaceous of Turkey". Bulletin de la Société Géologique de France. 183 (2): 85–92. doi:10.2113/gssgfbull.183.2.85.
- Johan Lindgren; Hani F. Kaddumi; Michael J. Polcyn (2013). "Soft tissue preservation in a fossil marine lizard with a bilobed tail fin". Nature Communications. 4 (2423): 2423. Bibcode:2013NatCo...4.2423L. doi:10.1038/ncomms3423. PMID 24022259.
- International Commission on Zoological Nomenclature (2012). "Article 8. What constitutes published work". International Code of Zoological Nomenclature (4th ed.). Retrieved July 16, 2021.
- Mike Taylor (June 8, 2010). "Notes on Early Mesozoic Theropods and the future of zoological nomenclature". Sauropod Vertebra Picture of the Week. Archived from the original on March 9, 2021.
- Natalia B. Ananjeva (2019). "Current State of the Problems in the Phylogeny of Squamate Reptiles (Squamata, Reptilia)". Biology Bulletin Reviews. 9 (2): 119–128. doi:10.1134/s2079086419020026. S2CID 162184418.
- Aaron R. H. LeBlanc; Michael W. Caldwell; Nathalie Bardet (2012). "A new mosasaurine from the Maastrichtian (Upper Cretaceous) phosphates of Morocco and its implications for mosasaurine systematics". Journal of Vertebrate Paleontology. 32 (1): 82–104. doi:10.1080/02724634.2012.624145. S2CID 130559113.
- Daniel Madzia; Andrea Cau (2017). "Inferring 'weak spots' in phylogenetic trees: application to mosasauroid nomenclature". PeerJ. 5: e3782. doi:10.7717/peerj.3782. PMC 5602675. PMID 28929018.
- Hallie P. Street (2017). "Reassessing Mosasaurini based on a systematic revision of Mosasaurus". Vertebrate Anatomy Morphology Palaeontology. 4: 42. ISSN 2292-1389.
- Gorden L. Bell Jr. (1997). "A Phylogenetic Revision of North American and Adriatic Mosasauroidea". Ancient Marine Reptiles. Academic Press. pp. 293–332. doi:10.1016/b978-012155210-7/50017-x. ISBN 978-0-12-155210-7.
- Tiago R. Simões; Oksana Vernygora; Ilaria Paparella; Paulina Jimenez-Huidobro; Michael W. Caldwell (2017). "Mosasauroid phylogeny under multiple phylogenetic methods provides new insights on the evolution of aquatic adaptations in the group". PLOS ONE. 12 (5): e0176773. Bibcode:2017PLoSO..1276773S. doi:10.1371/journal.pone.0176773. PMC 5415187. PMID 28467456.
- Dimitry V. Grigoriev (2013). "Redescription of Prognathodon lutugini (Squamata, Mosasauridae)" (PDF). Proceedings of the Zoological Institute RAS. 317 (3): 246–261.
- Jack L. Conrad (2008). "Phylogeny And Systematics Of Squamata (Reptilia) Based On Morphology". Bulletin of the American Museum of Natural History. 310: 1–182. doi:10.1206/310.1. S2CID 85271610.
- Keith A. Metzger; Anthony Herrel (2002). "Inertial feeding in reptiles: the role of skull mass reduction". Archived from the original on June 10, 2021.
- Theagarten Lingham-Soliar (1991). "Locomotion in mosasaurs". Modern Geology. 16: 229–248.
- Alexandra Houssaye; Johan Lindgren; Rodrigo Pellegrini; Andrew H. Lee; Damien Germain; Michael J. Polcyn (2013). "Microanatomical and Histological Features in the Long Bones of Mosasaurine Mosasaurs (Reptilia, Squamata) – Implications for Aquatic Adaptation and Growth Rates". PLOS ONE. 8 (10): e76741. Bibcode:2013PLoSO...876741H. doi:10.1371/journal.pone.0076741. PMC 3797777. PMID 24146919.
- Cyrus C. Greene (2018). Osteohistology And Skeletochronology Of an Ontogenetic Series Of Clidastes (Squamata: Mosasauridae): Growth And Metabolism In Basal Mosasaurids (MS). Fort Hays State University.
- Glenn J. Tattersall; Cleo A. C. Leite; Colin E. Sanders; Viviana Cadena; Denis V. Andrade; Augusto S. Abe; William K. Milsom (2016). "Seasonal reproductive endothermy in tegu lizards". Science Advances. 2 (1): e1500951. Bibcode:2016SciA....2E0951T. doi:10.1126/sciadv.1500951. PMC 4737272. PMID 26844295.
- T. Lynn Harrell Jr.; Alberto Pérez-Huerta; Celina A. Suarez (2016). "Endothermic mosasaurs? Possible thermoregulation of Late Cretaceous mosasaurs (Reptilia, Squamata) indicated by stable oxygen isotopes in fossil bioapatite in comparison with coeval marine fish and pelagic seabirds". Palaeontology. 59 (3): 351–363. doi:10.1111/pala.12240.
- Vanessa C. Bowman; Jane E. Francis; James B. Riding (2013). "Late Cretaceous winter sea ice in Antarctica?" (PDF). Geology. 41 (12): 1227–1230. Bibcode:2013Geo....41.1227B. doi:10.1130/G34891.1.
- James E. Martin (2006). "Biostratigraphy of the Mosasauridae (Reptilia) from the Cretaceous of Antarctica". Geological Society, London, Special Publications. 258 (1): 101–108. Bibcode:2006GSLSP.258..101M. doi:10.1144/gsl.sp.2006.258.01.07. S2CID 128604544.
- Martin S. Fernandez; Zulma Gasparini (2012). "Campanian and Maastrichtian mosasaurs from Antarctic Peninsula and Patagonia, Argentina". Bulletin de la Société Géologique de France. 183 (2): 93–102. doi:10.2113/gssgfbull.183.2.93.
- Takuya Konishi; Michael W. Caldwell; Tomohiro Nishimura; Kazuhiko Sakurai; Kyo Tanoue (2015). "A new halisaurine mosasaur (Squamata: Halisaurinae) from Japan: the first record in the western Pacific realm and the first documented insights into binocular vision in mosasaurs". Journal of Systematic Palaeontology. 14 (10): 809–839. doi:10.1080/14772019.2015.1113447. S2CID 130644927.
- John A. Robbins (2010). Investigating Holocene climate change on the northern Channel Islands and Cretaceous mosasaur ecology using stable isotopes (PhD). Southern Methodist University. ISBN 978-1-124-43286-1. Archived from the original on June 21, 2021.
- Erle G. Kauffman (2004). "Mosasaur Predation on Upper Cretaceous Nautiloids and Ammonites from the United States Pacific Coast". PALAIOS. 19 (1): 96–100. Bibcode:2004Palai..19...96K. doi:10.1669/0883-1351(2004)019<0096:MPOUCN>2.0.CO;2.
- Gorden L. Bell Jr.; James E. Martin (1995). "Direct evidence of aggressive intraspecific competition in Mosasaurus conodon (Mosasauridae:Squamata)". Journal of Vertebrate Paleontology. 15 (suppl. to 3): 18A. doi:10.1080/02724634.1995.10011277.
- Takuya Konishi. "Anything Mosasaur". Takuya Konishi, PhD. Archived from the original on March 24, 2021.
- Theagarten Lingham-Soliar (2004). "Palaeopathology and injury in the extinct mosasaurs (Lepidosauromorpha, Squamata) and implications for modern reptiles". Lethaia. 37 (3): 255–262. doi:10.1080/00241160410006519.
- Anne S. Schulp; Geert H. I. M. Walenkamp; Paul A. M. Hofman; Yvonne Stuip; Bruce M. Rothschild (2006). "Chronic bone infection in the jaw of Mosasaurus hoffmanni (Squamata)" (PDF). Oryctos. 6 (2006): 41–52. ISSN 1290-4805.
- Bruce M. Rothschild; Larry D. Martin (2005). "Mosasaur ascending: the phytogeny of bends". Netherlands Journal of Geosciences. 84 (Special Issue 3): 341–344. doi:10.1017/S0016774600021120.
- Agnete Weinreich Carlsen (2017). "Frequency of decompression illness among recent and extinct mammals and "reptiles": a review". The Science of Nature. 104 (7–8): 56. Bibcode:2017SciNa.104...56C. doi:10.1007/s00114-017-1477-1. PMID 28656350. S2CID 23194069.
- Bruce Rothschild; Michael J. Everhart (2015). "Co-Ossification of Vertebrae in Mosasaurs (Squamata, Mosasauridae); Evidence of Habitat Interactions and Susceptibility to Bone Disease". Transactions of the Kansas Academy of Science. 118 (3–4): 265–275. doi:10.1660/062.118.0309. S2CID 83690496.
- Daniel J. Field; Aaron LeBlanc; Adrienne Gau; Adam D. Behlke (2015). "Pelagic neonatal fossils support viviparity and precocial life history of Cretaceous mosasaurs". Palaeontology. 58 (3): 401–407. doi:10.1111/pala.12165.
- Gorden L. Bell Jr.; M. Amy Sheldon; James P. Lamb; James E. Martin (1996). "The first direct evidence of live birth in Mosasauridae (Squamata): Exceptional preservation in Cretaceous Pierre Shale of South Dakota". Journal of Vertebrate Paleontology. 16 (suppl. to 3): 21A. doi:10.1080/02724634.1996.10011371.
- Alexandra Houssaye; Paul Tafforeau (2012). "What vertebral microanatomy reveals about the ecology of juvenile mosasaurs (Reptilia, Squamata)". Journal of Vertebrate Paleontology. 32 (5): 1042–1048. doi:10.1080/02724634.2012.680999. S2CID 84662320.
- James E. Martin (2002). "Juvenile marine reptiles from the Late Cretaceous of the Antarctic peninsula and their relationships to other such occurrences in central South Dakota and Belgium" (PDF). Proceedings of the South Dakota Academy of Science. 81: 53–57.
- Nathalie Bardet (2012). "Maastrichtian marine reptiles of the Mediterranean Tethys: a palaeobiogeographical approach". Bulletin de la Société Géologique de France. 183 (6): 573–596. doi:10.2113/gssgfbull.183.6.573.
- Elizabeth L. Nicholls and Anthony P. Russell (1990). "Paleobiogeography of the Cretaceous Western Interior Seaway of North America: the vertebrate evidence". Palaeogeography, Palaeoclimatology, Palaeoecology. 79 (1–2): 149–169. Bibcode:1990PPP....79..149N. doi:10.1016/0031-0182(90)90110-S.
- David B. Kemp; Stuart A. Robinson; J. Alistair Crame; Jane E. Francis; Jon Ineson; Rowan J. Whittle; Vanessa Bowman; Charlotte O'Brien (2014). "A cool temperate climate on the Antarctic Peninsula through the latest Cretaceous to early Paleogene". Geology. 42 (7): 583–586. Bibcode:2014Geo....42..583K. doi:10.1130/g35512.1.
- Jose-Carmelo Corral; Ana Berreteaga; Henri Cappetta (2016). "Upper Maastrichtian shallow marine environments and neoselachian assemblages in North Iberian palaeomargin (Castilian Ramp, Spain)". Cretaceous Research. 57: 639–661. doi:10.1016/j.cretres.2015.08.001.
- Matt Friedman (2012). "Ray-finned fishes (Osteichthyes, Actinopterygii) from the type Maastrichtian, the Netherlands and Belgium". Scripta Geologica (8): 113–142.
- Catherine R. C. Strong; Michael W. Caldwell; Takuya Konishi; Alessandro Palci (2020). "A new species of longirostrine plioplatecarpine mosasaur (Squamata: Mosasauridae) from the Late Cretaceous of Morocco, with a re-evaluation of the problematic taxon 'Platecarpus' ptychodon". Journal of Systematic Palaeontology. 18 (21): 1769–1804. doi:10.1080/14772019.2020.1818322.
- Steven M. Stanley (1999). Earth System History. New York: W.H. Freeman and Company. pp. 487–489. ISBN 978-0-7167-2882-5.
- Michael J. Everhart (2017). Oceans of Kansas. Indiana University Press. pp. 24–263. ISBN 978-0253026323.
- Shaoneng He; T. Kurtis Kyser; William G. E. Caldwell (2005). "Paleoenvironment of the Western Interior Seaway inferred from δ18O and δ13C values of molluscs from the Cretaceous Bearpaw marine cyclothem". Palaeogeography, Palaeoclimatology, Palaeoecology. 217 (1–2): 67–85. Bibcode:2005PPP...217...67H. doi:10.1016/j.palaeo.2004.11.016.
- Cynthia G. Fisher; Michael A. Arthur (2002). "Water mass characteristics in the Cenomanian US Western Interior seaway as indicated by stable isotopes of calcareous organisms". Palaeogeography, Palaeoclimatology, Palaeoecology. 188 (3–4): 89–213. Bibcode:2002PPP...188..189F. doi:10.1016/S0031-0182(02)00552-7.
- Caitlin R. Kiernan (2002). "Stratigraphic distribution and habitat segregation of mosasaurs in the Upper Cretaceous of western and central Alabama, with a historical review of Alabama mosasaur discoveries". Journal of Vertebrate Paleontology. 22 (1): 91–103. doi:10.1671/0272-4634(2002)022[0091:sdahso]2.0.co;2.
- Andrew D. Gentry; James F. Parham; Dana J. Ehret; Jun A. Ebersole (2018). "A new species of Peritresius Leidy, 1856 (Testudines: Pan-Cheloniidae) from the Late Cretaceous (Campanian) of Alabama, USA, and the occurrence of the genus within the Mississippi Embayment of North America". PLOS ONE. 13 (4): e0195651. Bibcode:2018PLoSO..1395651G. doi:10.1371/journal.pone.0195651. PMC 5906092. PMID 29668704.
- Jun Ebersole; Takehito Ikejiri; Harry Lyon Blewitt; Sandy Ebersole (2013). "An Overview of Late Cretaceous Vertebrates from Alabama". Bulletin of the Alabama Museum of Natural History. 31 (1): 46–70.
- Paulina Jiménez-Huidobro; Michael W. Caldwell (2019). "A New Hypothesis of the Phylogenetic Relationships of the Tylosaurinae (Squamata: Mosasauroidea)". Frontiers in Earth Science. 7 (47): 47. Bibcode:2019FrEaS...7...47J. doi:10.3389/feart.2019.00047.
- Todd Cook, Eric Brown, Patricia E. Ralrick, and Takuya Konishi (2017). "A late Campanian euselachian assemblage from the Bearpaw Formation of Alberta, Canada: some notable range extensions". Canadian Journal of Earth Sciences. 54 (9): 973–980. Bibcode:2017CaJES..54..973C. doi:10.1139/cjes-2016-0233. hdl:1807/77762.CS1 maint: multiple names: authors list (link)
- Tim T. Tokaryk; C. R. Harington (1992). "Baptornis sp. (Aves: Hesperornithiformes) from the Judith River Formation (Campanian) of Saskatchewan, Canada". Journal of Paleontology. 66 (6): 1010–1012. doi:10.1017/S002233600002093X.
- Tamaki Sato (2003). "Terminonatator ponteixensis, a new elasmosaur (Reptilia; Sauropterygia) from the Upper Cretaceous of Saskatchewan". Journal of Vertebrate Paleontology. 23 (1): 89–103. doi:10.1671/0272-4634(2003)23[89:tpanes]2.0.co;2.
- Tamaki Sato (2005). "A new polycotylid plesiosaur (Reptilia: Sauropterygia) from the Upper Cretaceous Bearpaw Formation in Saskatchewan, Canada". Journal of Paleontology. 79 (5): 969–980. doi:10.1666/0022-3360(2005)079[0969:anpprs]2.0.co;2.
- John W. Hoganson; Brett Woodward (2004). "Skeleton of the Rare Giant Sea Turtle, Archelon, Recovered from the Cretaceous DeGrey Member of the Pierre Shale near Cooperstown, Griggs County, North Dakota" (PDF). North Dakota Geological Society Newsletter. 32 (1): 1–4. Archived from the original (PDF) on June 3, 2020.
- David J. Cicimurri; Gorden L. Bell, Jr.; Philip W. Stoffer (1999). "Vertebrate Paleontology of the Pierre Shale and Fox Hills Formations (Late Campanian-Late Maastrichtian) of Badlands National Park, South Dakota" (PDF). National Park Service Paleontological Research. 4: 1–7.
- Thomas S. Tobin; Peter D. Ward; Eric J. Steig; Eduardo B. Olivero; Isaac A. Hilburn; Ross N. Mitchell; Matthew R. Diamond; Timothy D. Raub; Joseph L. Kirschvink (2012). "Extinction patterns, δ18 O trends, and magnetostratigraphy from a southern high-latitude Cretaceous–Paleogene section: Links with Deccan volcanism". Palaeogeography, Palaeoclimatology, Palaeoecology. 350–352: 180–188. Bibcode:2012PPP...350..180T. doi:10.1016/j.palaeo.2012.06.029.
- Rodrigo A. Oteroa; Sergio Soto-Acuña; David Rubilar-Rogers; Carolina S. Gutstein (2017). "Kaikaifilu hervei gen. et sp. nov., a new large mosasaur (Squamata, Mosasauridae) from the upper Maastrichtian of Antarctica". Cretaceous Research. 70: 209–225. doi:10.1016/j.cretres.2016.11.002.
- José P. O'Gorman; Karen M. Panzeri; Marta S. Fernández; Sergio Santillana; Juan J. Moly; Marcelo Reguero (2018). "A new elasmosaurid from the upper Maastrichtian López de Bertodano Formation: new data on weddellonectian diversity". Alcheringa: An Australasian Journal of Palaeontology. 42 (4): 575–586. doi:10.1080/03115518.2017.1339233. S2CID 134265841.
- Alberto L. Cione; Sergio Santillana; Soledad Gouiric-Cavalli; Carolina Acosta Hospitaleche; Javier N. Gelfo; Guillermo M. Lopez; Marcelo Reguero (2018). "Before and after the K/Pg extinction in West Antarctica: New marine fish records from Marambio (Seymour) Island". Cretaceous Research. 85: 250–265. doi:10.1016/j.cretres.2018.01.004.
- T. Lynn Harrell Jr.; Alberto Pérez-Huerta (2014). "Habitat preference of mosasaurs indicated by rare earth element (REE) content of fossils from the Upper Cretaceous marine deposits of Alabama, New Jersey, and South Dakota (USA)". Netherlands Journal of Geosciences. 94 (1): 145–154. doi:10.1017/njg.2014.29. S2CID 128587386.
- Johan Lindgren (2005). "The first record of Hainosaurus (Reptilia: Mosasauridae) from Sweden". Journal of Paleontology. 79 (6): 1157–1165. doi:10.1111/j.1502-3931.1998.tb00520.x.
- Theagarten Lingham-Soliar (1998). "Unusual death of a Cretaceous giant". Lethaia. 31 (4): 308–310. doi:10.1111/j.1502-3931.1998.tb00520.x.
- William B. Gallagher; Carl E. Campbell; John W. M. Jagt; Eric W. A. Mulder (2005). "Mosasaur (Reptilia, Squamata) material from the Cretaceous-Tertiary boundary interval in Missouri". Journal of Vertebrate Paleontology. 25 (22): 473–475. doi:10.1671/0272-4634(2005)025[0473:mrsmft]2.0.co;2.
- Thomas R. Holtz (2006). "GEOL 104 Lecture 38: The Cretaceous-Tertiary Extinction III: Not With a Bang, But a Whimper". University of Maryland Department of Geology. Archived from the original on March 13, 2012.
- John W. Jagt; Dirk Cornelissen; Eric W. Mulder; Anne S. Schulp; Jacques Severinjns; Louis Verding (2008). "The youngest in situ record to date of Mosasaurus hoffmannii (Squamata, Mosasauridae) from the Maastrichtian type area, The Netherlands". Proceedings of the Second Mosasaur Meeting: 73–80.
- Kunio Kaiho; Naga Oshima; Kouji Adachi; Yukimasa Adachi; Takuya Mizukami; Megumu Fujibayashi; Ryosuke Saito (2016). "Global climate change driven by soot at the K-Pg boundary as the cause of the mass extinction". Scientific Reports. 6 (1): 1–13. Bibcode:2016NatSR...628427K. doi:10.1038/srep28427. PMC 4944614. PMID 27414998.
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