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Prognathodon

Prognathodon is an extinct genus of large marine squamate reptiles belonging to the family Mosasauridae, subfamily Mosasaurinae, and the tribe Globidensini, that inhabited the world's oceans during the Late Cretaceous period from the early Campanian to the late Maastrichtian stages, approximately 83 to 66 million years ago.^[1] Fossils of the genus have been discovered on multiple continents, including North America, Europe, Africa, the Middle East, and even as far as New Zealand, indicating a widespread distribution across the Western Interior Seaway and Tethys Sea regions.^[1] Characterized by a robust skull with massive jaws, short premaxillary-maxillary suture, and conical teeth featuring carinae and crenulations, Prognathodon species exhibited adaptations for durophagous feeding, capable of crushing hard-shelled prey such as turtles, fish, cephalopods, and possibly ammonites.^[1] The genus encompasses several valid species, including P. overtoni, P. currii, P. giganteus, P. solvayi, P. saturator, P. sectorius, P. rapax, P. waiparaensis, and P. kianda, with body lengths ranging from about 5 to 10 meters, the largest exemplified by P. currii with a skull exceeding 1.4 meters in length.^[1]^[2] As apex predators, Prognathodon species occupied an opportunistic ecological niche, blending traits of both "cut" and "crunch" feeding guilds to exploit diverse prey in marine environments.^[1] Evidence from associated gut contents, such as turtle remains (Nichollsemys baieri) and fish in P. overtoni specimens, supports their role as versatile hunters rather than strict specialists.^[1] The genus's postcranial skeleton was relatively lightly built, similar to that of Clidastes, suggesting efficient swimming capabilities suited to open-water pursuits.^[1] Despite their global presence, Prognathodon species went extinct during the Cretaceous-Paleogene mass extinction event, alongside other mosasaurs, likely due to environmental upheavals including asteroid impact and volcanic activity.^[1] The systematics of Prognathodon have evolved with new discoveries, with earlier classifications sometimes placing it in Plioplatecarpinae, but modern analyses firmly root it within Mosasaurinae based on shared derived traits like the triangular frontal bone and specialized dentition.^[3]^[1] Ongoing research continues to refine species boundaries and phylogenetic relationships, particularly through exceptional specimens from sites like the phosphates of Morocco and Angola, which reveal variations in tooth morphology and jaw strength across taxa.^[2]

Discovery and research

Etymology

The genus name Prognathodon was coined by Belgian paleontologist Louis Dollo in 1889 for the type species P. solvayi, based on fragmentary remains recovered from the Maastrichtian phosphorite deposits near Mesvin, Belgium.^[4] The name derives from the Greek roots pro- (forward), gnathos (jaw), and odous (tooth), highlighting the distinctive forward-projecting anterior teeth in the massively built lower jaw.^[5] This nomenclature captures Dollo's initial impressions of the taxon's robust cranial architecture and protruding dentition, which set it apart from contemporary mosasaur genera known at the time.^[6]

Initial discovery and naming

The genus Prognathodon was established based on fossils recovered from Upper Cretaceous (Maastrichtian) phosphorite deposits in Belgium during the late 19th century. The type species, P. solvayi, was discovered in 1887 at the Solvay phosphate quarry near Mesvin in the Mons Basin, yielding a nearly complete skull and partial postcranial skeleton (holotype IRSNB R33). This material was formally described and named by Louis Dollo in 1889, who initially proposed the generic name Prognathosaurus due to a perceived preoccupation of Prognathodon, though the latter was later validated as the correct name.^[6] Early 20th-century discoveries broadened the geographic scope of Prognathodon to North America and additional European sites. In 1898, Samuel W. Williston identified and described P. overtoni from fragmentary postcranial remains, including vertebrae and limb elements, collected from the Pierre Shale Formation in western Kansas; this material had been initially collected in the 1870s and tentatively assigned to other mosasaur genera such as Liodon or Platecarpus by Edward Drinker Cope. In Europe, Dollo named P. giganteus in 1904 from isolated cranial and vertebral fragments unearthed at the Solvay quarry in Spiennes, Belgium.^[6] The fragmentary nature of these early specimens posed significant classification challenges, leading to initial misassignments of Prognathodon material to genera like Mosasaurus based on superficial dental or vertebral similarities. Such taxonomic uncertainties persisted until more complete skeletons were recovered in subsequent decades, allowing for clearer distinctions within Mosasauridae.^[6]

Key studies and recent findings

One of the foundational studies on Prognathodon was Dale A. Russell's 1967 monograph, Systematics and Morphology of American Mosasaurs, which systematically reviewed North American mosasaur fossils and established Prognathodon as a distinct genus separate from Mosasaurus based on cranial and dental differences observed in specimens from the Western Interior Seaway.^[7] In 1989, Theagarten Lingham-Soliar and Dirk Nolf published a detailed analysis of European Prognathodon material from the Upper Cretaceous of Belgium, emphasizing intraspecific skull variations such as differences in quadrate morphology and maxilla shape among specimens, which helped refine the genus's diagnostic features beyond North American forms.^[6] Recent post-2020 research has further advanced Prognathodon systematics through reexaminations of global specimens. Woolley et al. (2022) conducted a comprehensive taxonomic review of South African mosasaurids, reclassifying the holotype of Tylosaurus capensis—previously assigned to Tylosaurus and later Taniwhasaurus—as a composite specimen (chimera) incorporating elements from Prognathodon and another indeterminate mosasaur, based on mismatched vertebral and cranial proportions.^[8] Additionally, Abu El-Kheir et al. (2023) reported a new prognathodontin mosasaur specimen from the Maastrichtian Dakhla Formation in Egypt's Western Desert, consisting of associated teeth and postcranial elements that exhibit conical, carinate dentition typical of Prognathodon, providing evidence of the tribe's diversity in North African marine ecosystems near the Cretaceous-Paleogene boundary.^[9] Notable individual specimens have also driven recent insights. The "Carlo" specimen, a partial Prognathodon skull discovered in 2012 from the Maastrichtian Gulpen Formation in the Netherlands, was analyzed for pathology in 2020 by Bastiaans et al., revealing healed fractures and abnormal bone growth on the snout suggestive of traumatic injury during life, offering rare evidence of non-lethal predatory interactions or environmental hazards in late Maastrichtian mosasaurs.^[10] In 2025, Polcyn et al. described a Prognathodon cf. P. overtoni tooth from the Maastrichtian of Louisiana, one of the few pre-extinction mosasaur remains from the Gulf Coastal Plain, indicating the genus's persistence in shallow epicontinental seas immediately prior to the Cretaceous-Paleogene mass extinction event.^[11]

Taxonomy

Phylogenetic position

Prognathodon is placed within the subfamily Mosasaurinae of Mosasauridae, as a derived mosasaurine closely related to the tribe Globidensini, which encompasses genera such as Globidens and Carinodens.^[12] This positioning is supported by cladistic analyses utilizing cranial characters, which recover Prognathodon species as basal to or nested within Globidensini, sharing features like inflated tooth bases indicative of specialized feeding.^[13] Phylogenetic studies, including those employing parsimony, maximum likelihood, and Bayesian inference methods, consistently demonstrate that Prognathodon is paraphyletic within Mosasaurinae.^[14] This paraphyly arises from convergent evolution of durophagous adaptations, such as robust, blunt dentition for crushing hard-shelled prey, which developed independently across multiple mosasaurine lineages including Prognathodon, Globidens, and Carinodens.^[15] Such convergence complicates generic boundaries and highlights homoplasy in late mosasaur evolution.^[14] The temporal range of Prognathodon extends from the Campanian to the Maastrichtian stages of the Late Cretaceous, spanning approximately 83.6 to 66 million years ago, with the earliest known forms appearing in the early Campanian.^[5]

Valid species

The genus Prognathodon encompasses several valid species, primarily known from the Late Cretaceous (Campanian to Maastrichtian stages) across multiple paleobiogeographic regions. These species are distinguished by variations in skull robustness, dentition, and overall size, reflecting adaptations to marine predation in epicontinental seas and open oceans. Fossils of Prognathodon have been recovered from the Western Interior Seaway of North America, the Tethys Sea encompassing Europe and the Middle East, and the Indo-Pacific region including New Zealand.^[16] The type species, Prognathodon solvayi Dollo, 1889, is from the Maastrichtian of Belgium in Europe, with referred material also known from North America; it is characterized by a robust skull and conical teeth adapted for grasping prey.^[3] This species represents the baseline morphology for the genus, with a body length estimated at around 5-6 meters.^[16] Prognathodon currii Christiansen and Bonde, 2002, hails from the Maastrichtian of Israel in the Middle East and features the largest known skull in the genus, exceeding 1.4 meters in length, with an estimated total body length of up to 10 meters; its massive jaws suggest it was a top predator capable of exerting immense bite forces.^[17] Prognathodon giganteus Dollo, 1904, occurs in Campanian-Maastrichtian deposits of North America and Europe, noted for its large body size (up to 10 meters) and dentition suited for consuming fish and softer prey.^[16] Prognathodon lutugini (Yakovlev, 1901) Grigoriev, 2013, is recorded from the Maastrichtian of Russia, exhibiting similarities to P. giganteus in overall proportions but with regional variations in dental morphology, such as slightly more elongated crowns, and a body length approaching 8 meters.^[18] Prognathodon overtoni is known from the Upper Campanian Bearpaw Formation of Alberta, Canada, with new exceptional specimens described as of 2025 confirming its distinction through dental characters such as anastomosed enamel and cranial proportions; body length estimated around 10 meters.^[5] Prognathodon kianda is a valid species from the Maastrichtian of Angola, described in 2010 as the sister taxon to other Prognathodon species, characterized by unique jugal morphology.^[19] Prognathodon saturator and Prognathodon sectorius are known from the Maastrichtian type area in the Netherlands, distinguished by dental and vertebral features.^[20]

Disputed and synonymized species

Several species originally assigned to Prognathodon have been re-evaluated and either synonymized with other taxa or reassigned to different genera due to insufficient diagnostic material, overlapping morphological traits, and phylogenetic analyses revealing paraphyly within the genus. These revisions highlight the challenges in mosasaur taxonomy, where fragmentary fossils often lead to initial misclassifications, and ontogenetic changes or convergent adaptations with other mosasaurines like Globidens or Tylosaurus can obscure species boundaries. The species P. rapax from the Maastrichtian of North America has been considered a junior synonym of P. giganteus owing to shared traits like robust, conical teeth with weak serrations and similar vertebral proportions. This synonymy stems from comprehensive reviews of mosasaurine dentition and postcrania. Prognathodon waiparaensis, known from the Late Cretaceous of New Zealand, is based on limited material—a partial skull and vertebrae—but is considered valid based on unique frontal morphology, though additional specimens are needed to further confirm its placement within Prognathodon.^[15] Prognathodon hudae, described from Jordanian Maastrichtian deposits in 2009, remains a valid species within the genus, characterized by unique autapomorphies including blunt teeth and atypical sclerotic ring structure.^[21] Similarly, P. primus from the same deposits is recognized under Prognathodon.

Anatomy

Skull morphology

The skull of Prognathodon is characterized by its robust and deep construction, adapted for powerful biting forces, with overall proportions that are typically wider than long. In the species P. currii, the skull reaches an exceptional length of 1,422 mm, making it one of the largest known among mosasaurs, while smaller species like P. solvayi exhibit skulls around 600 mm in length with widths of 240–270 mm across the posterior regions.^[22]^[6] This deep profile distinguishes Prognathodon from related genera like Mosasaurus, which possess a relatively shallower cranial outline. The rostrum is notably shortened and obtuse-angled, terminating in a blunt premaxillary apex without a prominent median ridge, which contrasts with the more elongate rostra in some other mosasaurs. Large temporal fenestrae, including long and broad supratemporal openings, accommodate expansive jaw adductor muscles, enhancing bite strength; the upper temporal bar is formed by the postorbitofrontal and squamosal bones and is slightly bowed dorsally.^[6] The frontal bone is short and triangular, often with a marked anterior constriction, contributing to the skull's compact anterior proportions. Variations in the quadrate bone reflect ecological adaptations, particularly in durophagous forms like P. currii, where it is robust with a broad, sub-ovoid shape, a circular conch rim, and fused suprastapedial and infrastapedial processes that broaden dorsally to support increased mechanical loads during hard-prey consumption.^[6]^[22] Sclerotic rings, composed of overlapping ossicles (typically five per ring), encircle large eyes, with a dorsoventrally compressed aperture indicating enhanced visual capabilities suited to marine predation.^[6] Compared to Mosasaurus hoffmannii, Prognathodon features a straighter fronto-parietal suture and more robust ectopterygoid and jugal elements, further emphasizing its specialized cranial architecture for forceful occlusion.^[6]

Dentition

The dentition of Prognathodon is characterized by robust, conical teeth that vary in form across species, reflecting specialized adaptations in crown shape and attachment. Marginal teeth are typically bicarinate with fine striae or smooth enamel, featuring minimal to moderate recurvature and basal inflation that increases posteriorly. Anterior teeth often exhibit a single unserrated carina, while posterior teeth may develop finer serrations along the carinae. Pterygoid teeth are generally smaller and less recurved than marginal ones, contributing to a heterodont arrangement. Tooth attachment follows a thecodont pattern, with deep sockets and subdental crypts facilitating replacement, as observed in multiple specimens.^[19]^[3] In most species, such as P. giganteus, the teeth are large, triangular, and posteriorly recurved, with smooth to finely striated surfaces suited for piercing and holding prey; these forms lack pronounced bulbosity and emphasize a conical profile. Tooth counts typically range from 10 to 14 per side on the maxilla and dentary, with P. overtoni reaching 14 dentary teeth and P. kianda exhibiting a higher count of 15 dentary and 13 maxillary teeth. Premaxillary teeth project forward at a slight angle, enhancing anterior grasp, as evidenced by socket orientations in P. giganteus and P. overtoni.^[3]^[19]^[3] Durophagous variants, such as P. solvayi, display low-crowned, bulbous teeth with moderate inflation and pronounced striae, featuring 12 maxillary and 13 dentary teeth; these crowns are broader and less recurved than in piercing forms, with highly procumbent anterior premaxillary teeth oriented nearly horizontal for enhanced leverage. Jaw mechanics in Prognathodon support substantial occlusal forces, with a high coronoid process and robust temporal arcade providing large muscle attachment areas.^[3]

Postcranial skeleton

The postcranial skeleton of Prognathodon is adapted for an aquatic lifestyle, featuring an elongated axial column and reduced, flipper-like appendages that provided stability and maneuverability in marine environments. The axial skeleton consists of approximately 50–52 presacral vertebrae, including seven cervical, 33 dorsal, and 11–12 pygal vertebrae, as preserved in articulated specimens of P. overtoni from the Bearpaw Formation.^[16] Neural spines on the dorsal vertebrae vary in orientation, becoming more recumbent posteriorly, which supported the attachment of epaxial musculature for undulatory swimming.^[16] Pygal vertebrae are notably short and robust compared to the preceding dorsals, marking the transition to the caudal series and contributing to the flexibility of the posterior body.^[16] Recent analyses of gut contents in related specimens suggest robust thoracic adaptations for handling large prey.^[23] The appendicular skeleton exhibits significant reduction, with both forelimbs and hindlimbs modified into broad, paddle-like structures suited for hydrodynamic efficiency rather than terrestrial locomotion. In P. overtoni, the hindlimb phalangeal formula is 4-5-5-3-1, with flat and elongate phalanges but without pronounced hyperphalangy, differing from more extreme conditions in other mosasaurines.^[16] The pectoral girdle, including semi-equal scapula and coracoid, anchors these flippers, while the hindlimbs are proportionally longer, aiding in steering.^[16] Overall body length in Prognathodon species ranges from 7 to 12 meters, with P. saturator estimated at up to 13 meters based on a partial skeleton including a 1.6-meter lower jaw.^[24] Robust, curved ribs articulate with the anterior 10 dorsal vertebrae, forming a reinforced thoracic cage that indicates powerful swimming musculature.^[16] In some specimens, such as P. saturator, cervical and dorsal ribs bear bite marks suggestive of post-mortem scavenging, but the skeletal robustness underscores adaptations for predatory bursts in open water.

Soft tissue preservation

Soft tissue preservation in Prognathodon fossils is exceptionally rare, but documented cases offer valuable insights into the external anatomy of these marine squamates. One of the most significant examples is the juvenile specimen ERMNH HFV 197 from the Maastrichtian Muwaqqar Chalk Marl Formation in Harrana, Jordan, which preserves a bilobed tail fluke as a thin buff-whitish calcium carbonate film representing the original soft tissues. This hypocercal structure features an enlarged ventral lobe aligned with the downturned terminal vertebrae and a smaller, wing-like dorsal lobe, confirming scyphocraniate-style propulsion akin to that in sharks. Chemical analyses, including time-of-flight secondary ion mass spectrometry (ToF-SIMS), identified organic signatures consistent with eumelanin-based pigments, supporting the fidelity of the preserved morphology.^[25] Associated skin impressions on this specimen reveal small, rhomboidal, non-overlapping scales measuring 1.0–1.5 mm in height and 1.5–2.0 mm in length, distributed across the dorsal and ventral fin lobes. These scales, similar to those observed in other mosasaaurines, likely contributed to hydrodynamic efficiency by providing a smooth integument without the drag of overlapping structures.^[25] The "Carlo" specimen (NHMM 2012.072), a partial skeleton of Prognathodon cf. sectorius from the Maastrichtian of the southeastern Netherlands, includes preserved sclerotic rings and impressions suggestive of muscle attachments around the orbital region. The robust sclerotic rings, comprising multiple overlapping ossicles, indicate an unusually large eye diameter relative to skull size—estimated at over 20% of the orbital length—adapted for enhanced vision in dimly lit, deep-water habitats.^[26]^[10]

Paleobiology

Diet and predation

Prognathodon species displayed opportunistic carnivory, preying on a range of marine organisms as indicated by fossilized gut contents and bite traces. In specimens of P. overtoni from the upper Campanian of Alberta, Canada, preserved abdominal remains include scales and fragments from a large fish (approximately 1.6 m long), a smaller fish, a sea turtle carapace, and possibly cephalopod beaks, suggesting these mosasaurs ambushed diverse prey in open marine environments.^[16] Certain species exhibited durophagous adaptations for processing hard-shelled prey, while others leaned toward piscivory. For instance, P. solvayi featured a stout dentary and robust, striated teeth suited for gripping and piercing tough but soft-bodied prey such as belemnites, as inferred from jaw morphology.^[3] In contrast, P. currii possessed robust, conical teeth with blunt apices suited for crushing hard-shelled prey such as turtles and ammonites, aligning with durophagous habits.^[27] The diverse prey profiles from these fossils highlight Prognathodon as a versatile apex predator, capable of shifting between tearing flesh from fish and turtles and pulverizing tougher invertebrate shells depending on species-specific morphology and local availability.^[16] A 2023 study on a P. kianda specimen from the Maastrichtian of Angola documented gut contents including partial skeletons of three other mosasaurs (two cf. Prognathodon and one Mosasaurus sp.), indicating multispecies intrafamilial predation and cannibalism.^[23]

Locomotion and physiology

Prognathodon, as a derived mosasaur, utilized undulatory swimming propelled primarily by contractions of its axial musculature and a bilobed, hypocercal tail fluke for locomotion in marine environments.^[25] The tail fluke featured an asymmetrical structure with a prominent ventral lobe aligned with the downturned vertebral column and a smaller dorsal lobe, enabling efficient thrust generation through lateral oscillations of the caudal fin, akin to modern sharks.^[25] This propulsion system supported sustained cruising speeds but offered relatively limited maneuverability compared to the more agile, pectoral-fin-dominated swimming of ichthyosaurs.^[28] Stable oxygen isotope (δ¹⁸O) analysis of tooth apatite in Late Cretaceous mosasaurs, including taxa closely related to Prognathodon, reveals elevated body temperatures averaging 33–36°C, significantly higher than those inferred for contemporaneous poikilothermic marine fish (around 28°C) and approaching values for endothermic seabirds (around 39°C).^[29] These data indicate that Prognathodon likely possessed a high metabolic rate consistent with endothermy or effective thermoregulation, facilitating active predation in diverse oceanic conditions without reliance on environmental heat.^[29] Such physiology aligns with regional endothermy observed in some modern lamniform sharks, supporting extended foraging in cooler waters.^[30] Sensory adaptations in Prognathodon included large sclerotic rings encircling the eyes, composed of multiple scleral ossicles that supported corneal shape and accommodated underwater vision in low-light conditions.^[6] In the species P. solvayi, partial preservation shows at least five ossicles per ring, a configuration typical of squamates with enhanced visual acuity for detecting prey at depth.^[6] Additionally, numerous cranial nerve foramina, particularly those associated with the trigeminal nerve, suggest the possible presence of electroreceptive capabilities, as inferred from similar neurovascular patterns in other mosasaurs that may have enabled detection of bioelectric fields from hidden prey.^[31]

Distribution and paleoecology

Prognathodon exhibited a broad global distribution across the Late Cretaceous, primarily during the Maastrichtian stage, with fossils documented in the Tethyan realms of Europe (e.g., Netherlands, Belgium, Denmark), the Middle East (e.g., Syria, Israel, Jordan), and North Africa (e.g., Morocco, Egypt, Angola).^[12]^[9] Records also extend to the Western Interior Seaway of North America (e.g., USA, Canada) and the Southern Ocean region near New Zealand, spanning paleolatitudes from approximately 50°N to 60°S.^[32]^[33] Isolated occurrences appear in Brazil and Indonesia, though South American records remain sparse and Australia lacks any documented fossils.^[12] The genus inhabited shallow epicontinental seas, such as the Western Interior Seaway and the Danish Basin, typically at depths of 100–200 m in nearshore to offshore marine settings.^[34] These environments featured warm-temperate waters, as inferred from oxygen isotope (δ¹⁸O) analyses of mosasaur teeth, which indicate ambient seawater temperatures consistent with subtropical to temperate paleoclimates during the Maastrichtian.^[34] In New Zealand, fossils from formations like those at Waipara suggest occupation of extensive shallow seas surrounding low-lying landmasses.^[33] Ecologically, Prognathodon served as an apex predator in these Late Cretaceous marine ecosystems, coexisting with other large mosasaurs such as Tylosaurus and occupying top trophic levels.^[12]^[35] Its diverse tooth morphologies enabled niche partitioning, with durophagous forms adapted for crushing hard-shelled prey like ammonites and turtles, contrasting with piercing-toothed variants suited for softer-bodied fish and smaller reptiles.^[9]^[35] Carbon isotope data (δ¹³C) further support offshore foraging preferences, distinguishing it from more nearshore taxa.^[34] Fossil records show limited representation in early Campanian strata, with most occurrences concentrated in the late Campanian to Maastrichtian, suggesting a diversification pulse in the later Late Cretaceous.^[32] Additionally, potential Indo-Pacific endemism is hinted at by Indonesian finds, though the genus's overall cosmopolitan distribution indicates high adaptability rather than strict regional isolation.^[12]

Pathology and taphonomy

The "Carlo" specimen (NHMM 2012 072), a partial skull of Prognathodon cf. sectorius from the Maastrichtian of the Netherlands, exhibits multiple cranial pathologies indicative of a traumatic encounter with another large mosasaur. Healed bite wounds are evident on the premaxilla and maxilla, including partial amputation of the premaxillary rostrum, with associated callus formation suggesting the individual survived the injury for weeks to months.^[36] Chronic osteomyelitis is present in the left maxilla, characterized by bone resorption, proliferative periosteal reactions, and tubular drainage canals, likely secondary to the initial trauma and indicative of a persistent infection that may have compromised feeding efficiency.^[36] Bone remodeling in this specimen shows rapid healing processes, with extensive callus development comparable to mammalian responses, highlighting the physiological resilience of mosasaurs to severe injury.^[36] Additional pathological evidence in Prognathodon includes tooth wear patterns consistent with durophagous feeding in certain species. In P. overtoni specimens from the Campanian of Alberta, Canada, marginal teeth display enamel thickening at the apex with visible abrasion facets, attributed to crushing hard-shelled prey such as ammonites or turtles, which caused uneven wear across the dentition. Possible intraspecific combat scars are suggested by stress fractures on ribs of the P. saturator holotype (NHMM 1998 141-44) from the Maastrichtian of the Netherlands, featuring callus-covered bumps with clefts and radiolucent lines on radiographs, interpreted as healed traumatic injuries from agonistic interactions rather than infection or neoplasm.80[1065:RFRIPS]2.0.CO;2) Taphonomic patterns of Prognathodon fossils reveal a prevalence of disarticulated skeletons in Upper Cretaceous phosphorite deposits, particularly from the Maastrichtian of Belgium and Egypt. In Belgian sites like the L'Ecaussinnes and Ciply formations, isolated bones and partial skeletons occur in condensed phosphorite layers, reflecting rapid burial in oxygen-depleted basin environments that minimized scavenging and disarticulation by currents. Similarly, Egyptian phosphorites of the Duwi Formation yield fragmented Prognathodon remains, preserved through phosphate precipitation in anoxic, upwelling-influenced nearshore settings that concentrated vertebrate debris. This taphonomic mode introduces a bias toward coastal and marginal marine discoveries, as offshore open-ocean skeletons are less likely to be preserved due to greater exposure to dissolution and dispersal. The documented pathologies imply high survival rates from severe injuries in Prognathodon, underscoring a robust physiology capable of withstanding trauma and infection, which likely contributed to the genus's ecological success as an apex predator.^[36]

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[27]
Endothermic physiology of extinct megatooth sharks - PNAS
Jun 26, 2023 · Shark teeth from various Miocene (triangle) and Pliocene (circle) localities provide phosphate oxygen isotope compositions (δ18Op) that reveal ...Missing: Prognathodon | Show results with:Prognathodon
[28]
[PDF] A rostral neurovascular system in the mosasaur Taniwhasaurus ...
Apr 3, 2020 · These nerves send sensitive information from the skin of the snout to the brain and have only two exit foramina at the tip of the premaxilla in ...
[29]
The northernmost occurrence of Prognathodon (Squamata
Jul 18, 2012 · The marine reptile Prognathodon (Squamata: Mosasauridae), a mosasaurine mosasaur exhibiting a characteristically robust skull and dentition, ...Missing: sources | Show results with:sources
[30]
Prognathodon: A new mosasaur fossil from North Canterbury
A recently-discovered fossil from the Waipara area of North Canterbury represents the skull and associated remains of a mosasaur – a large extinct marine lizard ...
[31]
[PDF] Carbon isotope trends in north-west European mosasaurs (Squamata
May 31, 2021 · Consequently, larger-sized mosasaurs such as Prognathodon that preferred more offshore habitats would have lower δ13C values than taxa that were ...
[32]
(PDF) Carbon isotope trends in north-west European mosasaurs ...
May 16, 2025 · A number of publications used phosphate-derived oxygen isotopes (δ 18 O P ) to analyze body temperature in marine reptiles, including ...
[33]
https://www.otago.ac.nz/geology/research/paleontology/mosasaur-prognathodon-a-new-mosasaur-fossil-from-north-canterbury