This research history of Tylosaurus documents the historical developments in the study of Tylosaurus , a genus of extinct aquatic squamate reptile that lived during the Late Cretaceous.
This research history of Tylosaurus documents the historical developments in the study of Tylosaurus , a genus of extinct aquatic squamate reptile that lived during the Late Cretaceous.
Tylosaurus was the third new genus of mosasaur to be described from North America behind Clidastes and Platecarpus and the first in Kansas. [1] The early history of the genus as a taxon was subject to complications spurred by the infamous rivalry between American paleontologists Edward Drinker Cope and Othniel Charles Marsh during the Bone Wars. [1] [2] The type specimen was described by Cope in 1869 based on a fragmentary skull measuring nearly 5 feet (1.5 m) in length and thirteen vertebrae lent to him by Louis Agassiz of the Harvard Museum of Comparative Zoology. [3] The fossil, which remains in the same museum under the catalog number MCZ 4374, was recovered from a deposit of the Niobrara Formation located in the vicinity of Monument Rocks [4] near the Union Pacific Railroad at Fort Hays, Kansas. [5] Cope's first publication of the fossil was very brief and was named Macrosaurus proriger, the genus being a preexisting European mosasaur taxon. [1] [3] The specific epithet proriger means "prow-bearing", which is in reference to the specimen's unique prow-like elongated rostrum [6] [7] and is derived from the Latin word prōra (prow) and suffix -gero (I bear). [8] In 1870, Cope published a more thorough description of MCZ 4374. Without explanation, he moved the species into another European genus Liodon and declared his original Macrosaurus proriger a synonym. [1] [5]
In 1871, Cope identified a second species of North American Liodon based on several vertebrae and limb fragments, which he named Liodon dyspelor. The fossils came to Cope under the label as having been collected by an army doctor named William B. Lyon at Fort McRae, New Mexico. [9] [10] However, a 1997 study led by David C. Parris of the New Jersey State Museum found that the chemical composition of the fossil did not match any known geological deposit in New Mexico and is instead identical to that of the Niobrara Formation; the study speculated from examinations of multiple letters between Lyon and the Smithsonian Institution that the Liodon dyspelor fossils were actually recovered from somewhere in Western Kansas and were mislabeled as being collected by Lyon in New Mexico (who was shipping a different fossil from Fort McRae around the same time) during transit. The type specimen of the taxon is split between two museums; some of the vertebrae went to Cope's American Museum of Natural History as AMNH 1580 while the rest were sent to the Smithsonian as USNM 41. [10]
In 1872, Marsh argued that Liodon proriger and Liodon dyspelor are taxonomically distinct from the European genus and must be assigned a new one. For this, he erected the genus Rhinosaurus, which means "nose lizard" and is a portmanteau derived from the Ancient Greek words ῥίς (rhī́s, meaning "nose") and σαῦρος (saûros, meaning "lizard"). Marsh also described a third species based on a partial skeleton he collected near the southern portion of the Smoky Hill River [11] that is now in the Yale Peabody Museum as YPM 1268, [12] [13] which Marsh named Rhinosaurus micromus. [11] [13] Cope responded by arguing that Rhinosaurus was already a preoccupied synonym of Liodon. He disagreed with Marsh's arguments but proposed that in case Marsh was indeed correct, the genus name Rhamphosaurus should be used. [14] Marsh later discovered that the taxon Rhamphosaurus was preoccupied as a genus of lizard named in 1843. As a result, he suggested a move to a newly erected genus named Tylosaurus. [15] This name means "knob lizard" in another reference to the elongated rostrum characteristic of the genus. It is derived from the Latin tylos (knob) and Ancient Greek σαῦρος. [7] Despite coining the new genus, Marsh never formally transferred the Rhinosaurus species to Tylosaurus; this was first done in 1873 by Joseph Leidy of the University of Pennsylvania by transferring Rhinosaurus proriger and Rhinosaurus dyspelor to Tylosaurus. [16] [17] Rhinosaurus micromus was formally transferred to the same genus in 1894 by John Campbell Merriam, a paleontologist of the University of Munich at the time. [18]
Tylosaurus subsequently became the near-universally accepted genus for T. proriger, T. dyspelor, and T. micromus. An exception to this adoption was Cope, [14] who refused to accept Marsh's new genus and continued to refer to its species as Liodon. Cope also insisted that Rhamphosaurus was not preoccupied, arguing that while it was indeed used as a genus of lizard, it was subsequently synonymized with other genera before 1872 and was thus a vacant taxon. [6] Cope's persistence can be seen in his 1874 description of the fourth described species of Tylosaurus, which he named Liodon nepaeolicus. This type specimen of this species consists of a right lower jaw, a partial upper jaw, a quadrate bone, and a dorsal vertebra and was discovered by geologist Benjamin Franklin Mudge in an unspecified deposit of Cretaceous grey shale about a half-mile south of the Solomon River. [19] The fossils are stored in the American Museum of Natural History under the catalog number AMNH 1565. The specific epithet nepaeolicus is in reference to the Nepaholla, the Native American name for the Solomon River. [16] Liodon nepaeolicus was formally transferred to the genus Tylosaurus in Merriam's 1894 publication. [18]
The earliest depictions of Tylosaurus can be traced back to Cope's 1870 description of MCZ 4374. He suggested that Tylosaurus was an "excessively elongate reptile" because four of the back tail vertebrae of the specimen were less than a fifth in diameter than one more proximal, or closer to, the base of the tail, and there was little dimensional variation between the four back tail vertebrae. To Cope, this indicated that the enormous decrease in the size of the tail vertebrae from the base to the tip of the tail was minimal between vertebrae; thus, in order for the vertebrae in the column to approach the size of the tail vertebrae based on the observed rate of size decrease per vertebrae, plentiful amounts of vertebrae would have been needed. By measuring the proportions of the change in dimensions between the vertebrae, Cope estimated that Tylosaurus had at minimum over sixty vertebrae between the described proximal tail vertebra and a hypothetical vertebra measuring half the diameter of the four back tail vertebrae. Cope speculated that there were even more tail vertebrae ahead of the proximal vertebra, justified by the small transverse process it possessed, which would increase the vertebral count in the tail to an unknown but monstrous amount. [5] The resulting animal became that akin to an enormous sea serpent-like reptile reaching lengths rivaling that of the largest whales. [20] [21] [22] In an 1872 publication, Cope described in detail his imagination of the appearance of Tylosaurus. He depicted the head as akin to a giant flat cone supporting eyes directed partially upwards that is capable of swallowing entire prey whole like a snake, with a loose and baggy pelican-like throat to allow entry of such prey. Like a whale, one pair of paddle-like flippers was described to be present in the animal [20] and functional hind limbs were thought to be absent. [23] [20] The tail was imagined as long and flat, propelling Tylosaurus forward via an anguilliform locomotion. Cope estimated that T. proriger measured at minimum 50 feet (15 m) in length. T. dyspelor was the largest species of the genus was also described as the longest of all reptiles. Its maximum length was estimated to equal that of the blue whale, [a] [20] which reaches lengths of up to nearly 30 meters (98 ft) or more. [26] One T. dyspelor specimen with fossils relatively smaller than that of the taxon's type specimen had a skull measuring about 5 feet (1.5 m) in length; the whole animal was estimated to measure 75 feet (23 m) in total length. [20] In 1874, Cope estimated that T. nepaeolicus was around one-third the length of T. proriger, [19] which would translate to around 5.08 meters (16.7 ft) when using his 1872 estimates. [16] [20]
One of the earliest restorations of Tylosaurus comes from an illustration by a popular artist named Henry Worrall for paleontologist William E. Webb's 1872 fictional book Buffalo Land. This illustration, which is titled The sea which once covered the plains, represents one of the first paleoart of marine reptiles and pterosaurs from the Niobrara Formation. At the center of the illustration rises a giant Tylosaurus (identified as Liodon proriger). The appearance of this mosasaur was influenced by Cope, who was an acquaintance of Webb, as evidenced by its excessively elongated tail and serpentine appearance. [27] Additionally, the Tylosaurus was given a rather long neck. Although not as long as those of plesiosaurs like Elasmosaurus , this detail would influence subsequent depictions of Tylosaurus in art. An example of this can be seen in the famous fossil collector Charles Hazelius Sternberg's 1889 fictional narrative The Young Fossil Hunters: A True Story of Western Exploration and Adventure, which contains a scene where a giant Tylosaurus skeleton measuring 80 feet (24 m) in total length with a long and slender neck that is 20 feet (6.1 m) long is uncovered. [22]
Paleontologists began to understand Tylosaurus as scientists do today beginning with Samuel Wendell Williston's 1898 publication of a comprehensive study of the skeletal anatomy of Kansas mosasaurs, which among many things corrected many of the erroneous beliefs held by earlier paleontologists about Tylosaurus. A central component of the publication was a rigorous skeletal reconstruction of T. proriger, [28] [29] which was drawn by paleoartist Sydney Prentice under Williston's instructions. This reconstruction was almost entirely informed by three specimens in the collections of the University of Kansas Natural History Museum, but they nevertheless provided enough material to represent nearly an entire skeleton. [29] These three specimens include one consisting of a posterior fragment of the skull and an "absolute complete series of vertebrae, connected from head to tip of tail" collected in an unspecified date by a fossil collector named Elias Putnam West (KUVP 1048); one containing a complete skull and cervical vertebrae collected in 1898 by colleague Handel T. Martin (KUVP 28705); and one collected in 1877 by university chancellor Francis H. Snow that contains a near-complete set of front paddles along with some ribs, vertebrae, and shoulder girdles (KUVP 1075). [29] [30] Various additional Tylosaurus specimens informed minor missing body parts such as the hind limbs. The resulting animal was correctly depicted as a four-flipper reptile with a short neck and a tail making up around half the body length. [29] Rather unrealistically, the vertebral column was drawn straight and lacking in structural curves that Tylosaurus would have possessed in life. Commentating on this issue, Everhart noted that Williston was already aware of the curvature of a mosasaur's spinal column and suggested that he had a straight spine drawn to save space on the plate the reconstruction was published on. Nevertheless, apart from the straight spine, Williston's century-old skeletal reconstruction of T. proriger is still considered accurate by modern standards, and adaptations of the skeleton remain in use by paleontologists and museum workers. [31] In his own interpretation of the available fossil evidence, Williston proposed that Tylosaurus grew no larger than 35 feet (11 m) in length and lived as a highly mobile predator "at the expense of strength" that was best adapted for preying on small fish and occasionally an "animal of their own kind". In a review of the taxonomy of the Tylosaurus genus, Williston (1898) expressed doubt regarding the validity of T. micromus and T. nepaeolicus and went as far as to suggest the latter species was merely a juvenile representative of T. proriger. He also remarked that there exist little anatomical differences between T. proriger and T. dyspelor; the only real distinction between the two species being in size. [29]
In 1899, Henry Fairfield Osborn described the first complete skeleton of Tylosaurus, a specimen measuring 8.83 meters (29.0 ft) long that resides in the American Museum of Natural History as AMNH FR 221. Discovered in Kansas by a local named W. O. Bourne and initially identified as T. dyspelor, the fossil has been considered remarkable in that it contained not only every bone apart from a few in the tail's tip, but also had exceptional preservation of the animal's soft tissue, including the larynx, trachea, bronchi, and cartilage in the throat, chest, and shoulders. This was due to calcification, a condition in a calcium-rich environment like the Kansas chalk that causes soft tissue to harden, allowing it to better fossilize. [32] The completeness of AMNH FR 221 allowed Osborn to accurately measure the proportions of each body part; [32] these ratios remain in use by modern paleontologists when extrapolating Tylosaurus fossils. [16] [33] Osborn (1899) included a life impression of AMNH FR 221 by paleoartist Charles R. Knight. [32] The restoration carried a number of erroneous features, such as a baggy throat, bloated belly, and inaccurate paddles and dorsal fin. [34] But a seminal feature was the addition of a dorsal crest (known as a fringe) lining the mosasaur's back. This was based on another 1898 description of a mosasaur fossil by Williston that erroneously identified tracheal rings as remains of a dorsal fringe, which he corrected in 1902. Knight updated his Tylosaurus restorations with the dorsal fringes removed to reflect this correction. However, his original depiction of a fringe was picked up as a meme, and many subsequent illustrations of the mosasaur continued to portray this inaccuracy. [35]
Additional largely complete skeletons of T. proriger and T. dyspelor were uncovered from the Niobrara Formation between the 1900s to 1920s by Charles Sternberg and his son George, which were sold to museums in the United States and Germany. [36] A particular find was a T. proriger skeleton collected by C. Sternberg from Smoky Hill Chalk deposits in Logan County, Kansas, in 1917, which contained digested remains of a plesiosaur within its ribcage. The specimen was sold the following year to the Smithsonian, and the mosasaur has been permanently displayed as USNM 8898. [37] [38] The plesiosaur remains, despite their significance, were stashed as a separate specimen and promptly forgotten until their redescription by Everhart in 2004. This rediscovery formed the basis for the plot of the 2007 National Geographic film Sea Monsters: A Prehistoric Adventure . [38] George Sternberg attempted to sell another complete T. proriger skeleton he found to the Smithsonian 1926, but the museum was satisfied with his father's earlier specimen and declined the offer. This skeleton was ultimately transferred to the Sternberg Museum as FHSM VP-3. [39]
In his landmark 1967 work Systematics and Morphology of American Mosasaurs, Dale Russell performed a complete review and redescription of Tylosaurus. In a taxonomic examination, Russell found little justification for recognizing the validity of T. dyspelor and declared it a nomem vanum , [9] along with recognizing T. micromus as a junior synonym of T. proriger. [14] Many of the complete skeletons formerly assigned to the former taxon were reassigned to the type species. [12] T. nepaeolicus was affirmed as a distinct species. [40] Russell (1967) provided extensive diagnoses of Tylosaurus that are still used by scientists today, and Everhart remarked that the work "remains the single best reference regarding the skeletons of the various mosasaur genera" like Tylosaurus. [41]
By Russell (1967), the only recognized valid species of Tylosaurus were T. proriger and T. nepaeolicus. However, throughout the 19th and 20th centuries, numerous species of mosasaurs were described from around the world that are now recognized within the genus Tylosaurus. These additional species were identified as different genera during their times of discovery and it was not until the early 21st century when they were reclassified as Tylosaurus. [42]
In 1885, Louis Dollo described the genus Hainosaurus from a near-complete but poorly preserved skeleton excavated from a phosphate quarry in the Ciply Basin near the town of Mesvin, Belgium. [43] [44] The fossil was initially discovered as eight vertebrae by a worker in the January of the same year, who sold them to the Royal Belgian Institute of Natural Sciences. Based on information about the circumstances and locality of the discovery given the museum, it was recognized that the rest of the skeleton may have remained intact. In February, excavations were made under the authorization of an industrialist named Leopold Bernard, who managed the quarry the fossil resided in. The rest of the skeleton was recovered after a month of excavating between 500–600 cubic meters (650–780 cu yd) of phosphate, although a section of the tail was found to have been destroyed by erosion from an overlying deposit. The skeleton went to the museum, which was subsequently studied by Dollo, who recognized that it belonged to a new type of mosasaur. By instruction of the museum, he named it Hainosaurus bernardi. The prefix Haino- in the generic name refers to the Haine, a river located nearby the Ciply Basin, and thus combined with σαῦρος means "lizard from the Haine"; Dollo wrote that this was erected specifically to complement the etymology of Mosasaurus , which was similarly named in reference to a river near its type locality. The specific epithet bernardi was in recognition of Bernard, who made the excavation of the skeleton possible. [43] The skeleton is now on display at the Royal Belgian Institute under the catalog number IRSNB R23. [44]
A second species historically pertained to Hainosaurus was described by in 1988 by Elizabeth Nicholls based on a partial skeleton consisting of a partial skull, lower jaw, a near-complete vertebral column, and some limb bones recovered from the Pembina Member of the Pierre Shale in Manitoba, Canada. This skeleton resides in the Miami Museum in Miami, Manitoba cataloged as MT 2. Although Hainosaurus was previously only known in Europe, Nicholls (1988) argued that the new species differed from the more locally known Tylosaurus based on a higher count of pygal vertebrae, longer external nares, and femur longer than the humerus. The species was named H. pembinensis, the specific epithet referring to the Pembina Member the skeleton was found in. [45]
In 2005, paleontologist Johan Lindgren suspected that H. pembinensis was actually a species of Tylosaurus but stated that a better description of MT 2 was needed to be certain. [46] In 2010, paleontologists Timon Bullard and Michael Caldwell redescribed such specimen. They argued that the pygal vertebrae reported by Nicholls (1988) actually belonged to another individual mosasaur, reducing the vertebral count in MT 2 to one that was indistinguishable with Tylosaurus. They also noted that the length of the external nares was within the known range of Tylosaurus and additionally argued that the femur being longer than the humerus was an insufficient characteristic to diagnose the species at the generic level. Based on these and other characteristics, the study found that the species cannot be referred to Hainosaurus and renamed it to T. pembinensis. With this rediagnosis, the study also noted that the only confirmed characteristic that distinguished Hainosaurus from Tylosaurus at the time was a higher count of pygal vertebrae. It was doubted as to if this would be sufficient for Hainosaurus to be a distinct genus but acknowledged that further research may provide additional characteristics. [47] This further research was done in 2016 by Paulina Jimenez-Huidobro and Caldwell, which reexamined H. bernardi. They found that the unique characteristics of the type species are indeed insufficient to warrant a distinction between Hainosaurus and Tylosaurus and declared the former as a junior synonym of the latter, thus renaming H. bernardi to T. bernardi. [48] However, some scientists argue that Hainosaurus should remain a distinct genus, justified by differences in tooth morphology unexplored by Jimenez-Huidobro & Caldwell (2016) such as the presence of an advanced cutting-based dentition in T. bernardi as opposed to a more general smashing-based dentition seen in other Tylosaurus species. [49] [50]
In 1896, paleontologist Armand Thevenin published a formal description of a poorly preserved skull consisting of the majority of the maxilla, premaxilla, and dentary bones that was found in a phosphate deposit in Eclusier-Vaux, France during an earlier unspecified date. Thevenin wrote that the skull was first described by Jean Albert Gaudry, who initially thought that it belonged to a species of Liodon. However, Dollo thought that the characteristics of skull supported an alternative placement as a species of Mosasaurus. Through correspondence with Dollo and a reexamination of the skull, Thevenin noted that the rostrum was more elongated than those found in typical Mosasaurus skulls but not as long as those in the skulls of Tylosaurus or Hainosaurus. He suggested that this represented an intermediate trait for a new species, which he subsequently named Mosasaurus gaudryi; the specific epithet recognizing Gaudry's previous work on the fossil skull. [51] The skull is now on display at the French National Museum of Natural History as MNHN 1896–15. In 1990, paleontologist Theagarten Lingham-Soliar proposed reassignment of M. gaudryi to a possible specimen of H. bernardi based on the discovery of a double buttress supporting the suture between the premaxilla and maxilla in MNHN 1896–15, a trait he claimed that was unique to the latter species, and estimations that the rostrum may have been more elongated than preserved. This was elaborated on a publication of the same year by Nathalie Bardet of the Natural History Museum, who concluded that MNHN 1896-15 belongs to the genus Hainosaurus but as a separate species, thus changing the skull's scientific name to Hainosaurus gaudryi. This was agreed on by Lingham-Soliar in a 1992 publication. [44] In 2005, Lindgren pointed out that the characteristics used to justify the placement in Hainosaurus, such as the double buttress, can also be found in Tylosaurus. He also noted that the dentition of MNHN 1896-15 morphologically overlaps more with T. ivoensis and T. pembinensis than H. bernardi. With these characteristics, Lindgren concluded that H. gaudryi is most certainly a species of Tylosaurus, renaming it to Tylosaurus gaudryi. [46]
In 1963, paleontologist Per Ove Persson identified a new taxon of mosasaur based on isolated teeth from a deposit located in an area called Ivö Klack near Ivö Lake in the Kristianstad Basin in Scania, Sweden. Such teeth and various other teeth pertaining to the same taxon were recovered and described from this area numerous times in the past since 1836, but they have always been misidentified as either an ichthyosaur or Mosasaurus hoffmannii. Persson proposed that the teeth belonged to a new subspecies of M. hoffmannii and gave it the name Mosasaurus hoffmannii ivoensis, the prefix ivo- in the species name referring to Ivö Klack. Russell (1967) amended this identification by elevating the taxon to a distinct species. He also identified a mosasaur fossil from the Niobrara Formation in Kansas consisting of a partial skull, some vertebrae, and a coracoid bone as being of Mosasaurus ivoensis. In an abstract presented in 1998, Lindgren doubted if M. ivoensis was a species of Mosasaurus. He instead proposed that the species was actually of Hainosaurus. The next year in 1999, Lindgren amended this in another abstract and instead suggested that the species should be moved to Tylosaurus. In 2002, he co-authored a study with paleontologist Mikael Siversson which examined the fossils referred to the species as well as new material consisting of pterygoid teeth, partial jawbones, and some vertebrae. It was found that the Niobrara fossil identified as M. ivoensis by Russell (1967) is actually of a different species. Examinations of the Swedish teeth found possible similarities with that of Taniwhasaurus , but due to the poor representation of the genus and the sheer distance between the two taxa (Taniwhasaurus was primarily known from New Zealand at the time), it was expressed that it is unlikely that M. ivoensis belongs to it. Instead, the study concluded that the species should belong to Tylosaurus and thus renamed it Tylosaurus ivoensis. [52] However, a 2008 study led by Caldwell discovered Taniwhasaurus in northern Japan, which was of similar latitude with Ivö Klack during the Cretaceous, and reasserted dental similarities between T. ivoensis and the genus. This opened the possibility that the species could be reassigned to Taniwhasaurus, but the authors considered this to be a topic for a different study. [53]
In 1964, Miguel Telles Antunes described Mosasaurus iembeensis from a partial skull excavated from the Itombe Formation near the town of Iembe, Angola. [54] The deposit was initially dated to the Turonian age [55] but this was later revised to about 88 mya during the later Coniacian. [56] In 1992, Lingham-Soliar argued that the features of the skull disagreed with those of Mosasaurus and were instead characteristic of Tylosaurus. He subsequently moved the species into the genus, becoming T. iembeensis. However, Lingham-Soliar did not figure the holotype skull, which he identified as residing in the collections of NOVA University Lisbon without a catalog number, [44] and it was later reported in 2006 that the specimen may have been lost during a fire. [55] [57] In a 2012 multi-author study led by Octávio Mateus, it was reported that an additional T. iembeensis fossil consisting of fragmentary skull elements was recovered during an expedition to the lost holotype's locality, although the specimen was not figured or formally described. [57]
In 1968, a well-preserved mosasaur skull, now cataloged in the Sternberg Museum as FHSM VP-2295, was discovered in an outcrop of the Niobrara Formation in the northwestern part of Ellis County, Kansas. During the 1990s, this specimen was recognized by multiple authors as possibly coming from a new species of Tylosaurus. Despite such recognition, however, no paleontologist investigated this further and the fossil remained undescribed during the remainder of the 20th century. In a 2004 meeting, Everhart suggested that the new species should finally be given a scientific name and formal description, to which paleontologist Louis L. Jacobs responded with "Well, get it done." [58] In 2005, Everhart published a formal description of the new species represented by FHSM VP-2295. Thirteen different Tylosaurus specimens also from Kansas were identified as conspecific with FHSM VP-2295, and in reference to their shared localities the new species was given the name Tylosaurus kansasensis. [59] However, during a 2007 meeting, Caldwell approached Everhart and suggested that his description of T. kansasensis was not adequate enough and should be readdressed in a followup paper. [58] In 2013, Caldwell and Jiménez-Huidobro presented an abstract at the annual Society of Vertebrate Paleontology meeting casting doubt on the distinction of the species from T. nepaeolicus [58] and in 2016 the two and paleontologist Tiago Simões published a study arguing that T. kansasensis was merely a juvenile form of T. nepaeolicus, thus making the former a junior synonym of the latter. [60] This was criticized by Everhart, who in his 2017 book Oceans of Kansas claimed that the study was "poorly researched and written". However, he did not provide any comments on the topic, claiming that such would merely be considered "sour grapes". Nevertheless, Everhart maintained that T. kansasensis remains a distinct species "until proven otherwise". [58] A 2018 study by Robert F. Stewart and Jordan Mallon also rejected the synonymy based on inconsistencies when comparing the ontogenetic trends of T. kansasensis and T. nepaeolicus between the better-understood T. proriger. [61] Another ontogenetic study published in 2020 by Amelia R. Zietlow came in support of the synonymy based on results from ontograms constructed from a cladistical analysis. [62]
In 1995, the Royal Saskatchewan Museum excavated a partial skeleton first discovered a year prior by a local farmer from a hill located northwest of Herbert Ferry, Saskatchewan. [63] [64] The skeleton was found articulated and consists of a "moderately complete" skull, a largely complete vertebral column, limb bones, and bones of a smaller mosasaur as stomach content; [65] [63] it was curated into the museum as RSM P2588.1 and nicknamed "Omācīw" (meaning "hunter" in Cree). [63] In 2006, Timon Bullard of the University of Alberta studied the specimen in his Master of Science thesis. At the time, the Omācīw fossil was still in preparation and Bullard was only able to examine the right side of the skull. However, he identified that the fossil represented a new species of Tylosaurus and suggested that it be named Tylosaurus saskatchewanensis in reference to the original province of its discovery. [65] [66] Bullard's thesis was never published but subsequently published studies recognized T. saskatchewanensis as a valid species despite technically never having been formally described. [48] [53] In 2018, Bullard co-authored a multi-author study led by Jiménez-Huidobro which formally described Omācīw, which by then was more fully prepared, and confirmed its identity as a distinct species. [65]
In 2020, the MS thesis of Samuel Garvey of the University of Cincinnati was published. The thesis focused on TMP 2014.011.0001, a Tylosaurus fossil in the collections of the Royal Tyrrell Museum consisting of a partial snout and a fragment of the right mandible. The specimen was found around 55 kilometers (34 mi) northeast of Grande Prairie, Alberta; during the Cretaceous this locality was located at around 62° N, making the fossil the northernmost known occurrence of Tylosaurus and one of the few known occasions of a mosasaur existing in boreal climates. Moreover, the morphology of TMP 2014.011.0001 was recognized as very distinct from other Tylosaurus species. For example, it exhibited paedomorphosis in its teeth, which were slender and designed for piercing prey (contrary to the more robust cutting-specialized teeth of typical Tylosaurus species), a trait likely retained from juveniles. The uniqueness of the specimen led to the conclusion that it was a new species, which Garvey subsequently proposed that it be named Tylosaurus borealis in reference to its northernly occurrence. [33]
Mosasaurs are an extinct group of large aquatic reptiles within the family Mosasauridae that lived during the Late Cretaceous. Their first fossil remains were discovered in a limestone quarry at Maastricht on the Meuse in 1764. They belong to the order Squamata, which includes lizards and snakes.
Cretoxyrhina is an extinct genus of large mackerel shark that lived about 107 to 73 million years ago during the late Albian to late Campanian of the Late Cretaceous. The type species, C. mantelli, is more commonly referred to as the Ginsu shark, first popularized in reference to the Ginsu knife, as its theoretical feeding mechanism is often compared with the "slicing and dicing" when one uses the knife. Cretoxyrhina is traditionally classified as the likely sole member of the family Cretoxyrhinidae but other taxonomic placements have been proposed, such as within the Alopiidae and Lamnidae.
Mosasaurus is the type genus 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 genus was one of the first Mesozoic marine reptiles known to science—the first fossils of Mosasaurus were found as skulls in a chalk quarry near the Dutch city of Maastricht in the late 18th century, and were initially thought to be crocodiles or whales. One skull discovered around 1780 was famously nicknamed the "great animal of Maastricht". In 1808, naturalist Georges Cuvier concluded that 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. Cuvier did not designate a scientific name for the 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.
Tylosaurus is a genus of russellosaurine mosasaur that lived about 92 to 66 million years ago during the Turonian to Maastrichtian stages of the Late Cretaceous. Its fossils have been found primarily around North Atlantic Ocean including in North America, Europe, and Africa.
Selmasaurus is an extinct genus of marine lizard belonging to the mosasaur family. It is classified as part of the Plioplatecarpinae subfamily alongside genera like Angolasaurus and Platecarpus. Two species are known, S. russelli and S. johnsoni; both are exclusively known from Santonian deposits in the United States.
The Tylosaurinae are a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates. Members of the subfamily are informally and collectively known as "tylosaurines" and have been recovered from every continent except for South America. The subfamily includes the genera Tylosaurus, Taniwhasaurus, and Kaikaifilu, although some scientists argue that only Tylosaurus and Taniwhasaurus should be included.
The Halisaurinae are a subfamily of mosasaurs, a group of Late Cretaceous marine lizards. They were small to medium-sized, ranging from just under 3 meters in Eonatator sternbergi to as much as 8 or 9 meters in Pluridens serpentis. They tended to have relatively slender jaws and small, numerous teeth, suggesting a diet of small fish and other prey. Although the skeleton is primitive compared to other Mosasauridae in many respects, halisaurines had the distinctive hypocercal tail of other mosasaurids suggesting good swimming ability, and they persisted alongside other mosasaurs until the end of the Cretaceous. The earliest known remains of halisaurines occur in rocks of Santonian age and the subfamily persists until the latest Maastrichtian. Halisaurines are known from North and South America, Europe, Asia and Africa, indicating a more or less global distribution in the Late Cretaceous. Four genera are currently recognized: Eonatator, Halisaurus, Phosphorosaurus and Pluridens.
Eonatator is an extinct genus of marine lizard belonging to the mosasaur family. It is a close relative of Halisaurus, and part of the same subfamily, the Halisaurinae. It is known from the Late Cretaceous of North America, Colombia and Sweden. Originally, this taxon was included within Halisaurus, but was placed in its own genus, which also led to the subfamily Halisaurinae being created for the two genera.
Protosphyraena is a fossil genus of swordfish-like marine fish, that thrived worldwide during the Cretaceous period (Albian-Maastrichtian). Fossil remains of this taxon are mainly discovered in North America and Europe, and potential specimens are also known from Asia, Africa and Australia. Its fossils are best known from the Smoky Hill Member of the Niobrara Chalk Formation of Kansas.
Platecarpus is an extinct genus of aquatic lizards belonging to the mosasaur family, living around 84–81 million years ago during the middle Santonian to early Campanian, of the Late Cretaceous period. Fossils have been found in the United States and possible specimens in Belgium and Africa. A well-preserved specimen of Platecarpus shows that it fed on moderate-sized fish, and it has been hypothesized to have fed on squid, and ammonites as well. Like other mosasaurs, it was initially thought to have swum in an eel-like fashion, although another study suggests that it swam more like modern sharks. An exceptionally well-preserved specimen of P. tympaniticus known as LACM 128319 shows skin impressions, pigments around the nostrils, bronchial tubes, and the presence of a high-profile tail fluke, showing that it and other mosasaurs did not necessarily have an eel-like swimming method, but were more powerful, fast swimmers. It is held in the Natural History Museum of Los Angeles County. Isotopic analysis on teeth specimens has suggested that this genus and Clidastes may have entered freshwater occasionally, just like modern sea snakes.
Plotosaurus is an extinct genus of mosasaurs who lived during the Upper Cretaceous (Maastrichtian) in what is now North America. Only one species is recognized, P. bennisoni, described by Berkeley paleontologist Charles Lewis Camp in 1942 from fossils discovered in California. Originally named Kolposaurus, it was changed to Plotosaurus in 1951 when Camp discovered that the name had already been assigned to a type of nothosaur. Unlike other mosasaurids, Plotosaurus possesses a morphology converging with those of ichthyosaurs, suggesting a much more advanced swimming adaptation than some of its close relatives.
Prognathodon is an extinct genus of marine lizard belonging to the mosasaur family. It is classified as part of the Mosasaurinae subfamily, alongside genera like Mosasaurus and Clidastes. Prognathodon has been recovered from deposits ranging in age from the Campanian to the Maastrichtian in the Middle East, Europe, New Zealand, and North America.
Plioplatecarpus is a genus of mosasaur lizard. Like all mosasaurs, it lived in the late Cretaceous period, about 73-68 million years ago.
Goronyosaurus is an extinct genus of marine lizard belonging to the mosasaur family. Fossils of Goronyosaurus are exclusively known from the Late Maastrichtian of the Iullemmeden Basin in West Africa, specifically the Dukamaje Formation of Niger and Nigeria and Farin Doutchi Formation of Niger. The type specimen was first described in 1930 as Mosasaurus nigeriensis, but subsequent remains revealed a highly unique set of adaptations that prompted the species to be reclassified as the only species of the new genus Goronyosaurus in 1972. These unique adaptations have made Goronyosaurus notoriously difficult to classify within the Mosasauridae and it is often left out of phylogenetic analyses, although most authors agree that Goronyosaurus belonged to Mosasauridae.
Taniwhasaurus is an extinct genus of mosasaurs that lived during the Campanian stage of the Late Cretaceous. It is a member of the subfamily Tylosaurinae, a lineage of mosasaurs characterized by a long toothless conical rostrum. Two valid species are attached to the genus, T. oweni and T. antarcticus, known respectively from the fossil record of present-day New Zealand and Antarctica. Two other species have been nominally classified within the genus, T. 'capensis' and T. 'mikasaensis', recorded in present-day South Africa and Japan, but their attribution remains problematic due to the fragmentary state of their fossils. The generic name literally means "taniwha lizard", referring to a supernatural aquatic creature from Māori mythology.
Liodon is a dubious genus of mosasaur from the Late Cretaceous, known from fragmentary fossils discovered in St James' Pit, England and possibly also the Ouled Abdoun Basin of Morocco. Though dubious and of uncertain phylogenetic affinities, Liodon was historically a highly important taxon in mosasaur systematics, being one of the genera on which the family Mosasauridae was based.
Angolasaurus is an extinct genus of mosasaur. Definite remains from this genus have been recovered from the Turonian and Coniacian of Angola, and possibly the Coniacian of the United States, the Turonian of Brazil, and the Maastrichtian of Niger. While at one point considered a species of Platecarpus, recent phylogenetic analyses have placed it between the (then) plioplatecarpines Ectenosaurus and Selmasaurus, maintaining a basal position within the plioplatecarpinae.
During the time of the deposition of the Niobrara Chalk, much life inhabited the seas of the Western Interior Seaway. By this time in the Late Cretaceous many new lifeforms appeared such as mosasaurs, which were to be some of the last of the aquatic lifeforms to evolve before the end of the Mesozoic. Life of the Niobrara Chalk is comparable to that of the Dakota Formation, although the Dakota Formation, which was deposited during the Cenomanian, predates the chalk by about 10 million years.
This timeline of mosasaur research is a chronologically ordered list of important fossil discoveries, controversies of interpretation, and taxonomic revisions of mosasaurs, a group of giant marine lizards that lived during the Late Cretaceous Epoch. Although mosasaurs went extinct millions of years before humans evolved, humans have coexisted with mosasaur fossils for millennia. Before the development of paleontology as a formal science, these remains would have been interpreted through a mythological lens. Myths about warfare between serpentine water monsters and aerial thunderbirds told by the Native Americans of the modern western United States may have been influenced by observations of mosasaur fossils and their co-occurrence with creatures like Pteranodon and Hesperornis.
Mosasaurus is the type genus of the mosasaurs, an extinct group of aquatic squamate reptiles that lived during the Late Cretaceous. The first fossils of Mosasaurus were skulls found in a chalk quarry near the Dutch city of Maastricht in the late 18th century, and were initially thought to be crocodiles or whales. While the first skull discovered has always resided in the Netherlands, the second was looted in 1794 by French soldiers led by Jean-Baptiste Kléber after the siege of Maastricht, in the context of the French Revolutionary Wars. The second skull was then transferred the following year to the French National Museum of Natural History in Paris. In 1808, naturalist Georges Cuvier concluded that it belonged to a giant marine reptile with similarities to monitor lizards but otherwise unlike any known living animal. In 1822, William Daniel Conybeare proposed naming the animal Mosasaurus in reference to its origin in fossil deposits near the Meuse River. The genus name, although later approved by Cuvier himself, remained without specific epithets until 1829, from which a certain number of proposed names appeared. Later consensus, however, suggests the use of the name M. hoffmannii as first proposed by Gideon Mantell, as well the designation of the second skull as the type specimen of this species. Being one of the first Mesozoic marine reptiles known to science, its research history is therefore very broad and has great importance in the field of paleontology, since the second skull of M. hoffmannii helped Cuvier to conceptualize the notion of extinction.
{{cite book}}: CS1 maint: ref duplicates default (link){{cite book}}: CS1 maint: ref duplicates default (link){{cite book}}: CS1 maint: ref duplicates default (link)