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Pliosaurus

Pliosaurus is a of large, short-necked marine reptiles belonging to the family within the order Plesiosauria, known primarily from the period, specifically the stage approximately 157–152 million years ago. These apex predators were among the largest marine reptiles, with body lengths estimated at 10–13 meters and robust skulls reaching up to 2 meters in length, adapted for powerful bites with trihedral or subtrihedral teeth suited to macropredatory lifestyles targeting large prey such as other reptiles and fish. Fossils of Pliosaurus have been discovered in marine deposits across (including the , , and ) and Russia, with related pliosaurids known from and . The genus was first described by in 1841 based on material from the Formation in , and subsequent discoveries have revealed a diverse array of cranial and postcranial remains that highlight its ecological dominance in Jurassic marine ecosystems. In 2023, a nearly complete 2-meter-long pliosaur was discovered on the in Dorset, , offering further insights into these predators. Key anatomical features include a shortened neck with typically 4–5 , massive fore- and hind-limbs functioning as paddles for , and a deep, interlocking suture that enhanced bite force, estimated at 9,600–48,000 Newtons in large specimens. Dietary evidence from associated coprolites and stomach contents suggests a generalist feeding strategy, including cephalopods, , and even conspecifics, underscoring their role as top-tier carnivores. Taxonomically, Pliosaurus encompasses several valid species distinguished by variations in skull morphology, mandibular tooth counts (ranging from 50 to 70), and symphyseal length, with notable taxa including P. kevani (from Dorset, UK, with a 1.995-meter skull), P. carpenteri (from Wiltshire, UK), P. brachyspondylus, P. macromerus, and P. funkei. Recent phylogenetic analyses place Pliosaurus as a derived pliosaurid, closely related to other Late Jurassic giants like Liopleurodon, and emphasize the genus's evolutionary success before the decline of pliosaurids in the Early Cretaceous. Iconic specimens, such as the nearly complete P. funkei skull nicknamed "Predator X" from Norway, have provided insights into growth patterns and biomechanics, revealing a weakly constructed cranium relative to its size that relied on rapid, powerful strikes rather than sustained crushing.

Research History

Initial Discovery and Naming

The specimen of Pliosaurus, consisting of fragmentary remains including a partial skull, lower jaw fragments, , and limb elements such as an ilium, was collected by geologist near in , , during the early 1820s. These fossils originated from the Lower Formation, specifically the Rasenia cymodoce ammonite biozone of the Lower stage of the . In 1824, William Daniel Conybeare first referenced this material in his description of a complete skeleton, noting the Market Rasen finds as belonging to a large-bodied, short-necked variant of the genus, distinct from the long-necked P. dolichodeirus. This early observation highlighted the morphological differences, such as shortened , that set the specimen apart from typical plesiosaurs. The formal naming occurred in 1841 when anatomist described the specimen in detail within his work Odontography, erecting the Pleiosaurus under Plesiosaurus and designating it as the new Plesiosaurus (Pleiosaurus) brachydeirus. The generic name derives from plēios (more) and sauros (), emphasizing its perceived greater reptilian affinities compared to the more sauropterygian-like Plesiosaurus, while the specific epithet brachydeirus combines brachys (short) and deirē (neck), reflecting the abbreviated cervical region. Owen's diagnosis focused on distinctive features like trihedral teeth with fine striations and robust jaw architecture, distinguishing it from the Plesiosaurus, which at the time encompassed diverse marine reptiles. By 1842, Owen elevated Pleiosaurus to full generic rank as Pliosaurus brachydeirus in a report to the British Association for the Advancement of , solidifying its separation from Plesiosaurus and establishing Pliosaurus as the for the short-necked pliosaurid group. Early 19th-century paleontologists interpreted Pliosaurus as a variant of plesiosaurs adapted for a more predatory lifestyle, with its compact neck and powerful build suggesting enhanced aquatic agility over the elongated-necked forms like Plesiosaurus. This naming resolved initial taxonomic confusion, marking a key step in recognizing pliosaurs as a distinct lineage within Plesiosauria during the nascent field of paleontology.

Valid Species and Key Specimens

The genus Pliosaurus currently encompasses six valid species, recognized based on diagnostic cranial, dental, and postcranial features from Late Jurassic deposits primarily in Europe. These species are distinguished by variations in skull proportions, tooth morphology, and body size, with material ranging from isolated bones to partial skeletons. Taxonomic validity is supported by phylogenetic analyses emphasizing autapomorphies such as mandibular tooth counts and symphyseal length. Pliosaurus brachydeirus, the , was established by in 1841 based on fragmentary remains including a partial , lower fragments, , and limb elements ( OUMNH J.9245 and associated OUMNH J.9247–J.9301) from the Formation ( stage) at , , . Additional referred material includes vertebrae, ribs, and limb elements from the same formation in , indicating a small to medium-sized pliosaur with an estimated body length of 5–7 meters and a more gracile build compared to later species. Diagnostic features include a relatively short and approximately 70 mandibular teeth, though the 's fragmentary nature limits detailed comparisons. Pliosaurus carpenteri was named in from partial skeletons, including a nearly complete vertebral column and associated postcranial elements ( NHMUK PV R 3533), collected from the at Westbury Water Park, , . This exhibits a robust build with broad neural spines and strong limb girdles, suggesting enhanced propulsion in shallow marine environments, and an estimated body length of about 8 meters. It is diagnosed by a mandibular tooth count of around 60 and subtrihedral teeth with fine serrations. The type specimen, showing of like , was fully prepared and mounted for display at in 2017, where it remains a centerpiece for public education on marine reptiles. Pliosaurus funkei, described in 2012, represents one of the largest known pliosaurs, based on multiple specimens from the Agardhfjellet Formation (Middle Volgian, Tithonian stage) on Spitsbergen, Svalbard, Norway. The holotype (PM628, "Predator X") includes a partial skeleton with vertebrae, ribs, and a fragmentary skull exceeding 1.7 meters in length, yielding an estimated total body length of 10 meters and a mass of up to 45 tonnes. Key diagnostics include a long mandibular symphysis (about 25% of jaw length) and robust, trihedral teeth suited for crushing. Additional referred material, including a second partial skeleton (PM666), was excavated between 2006 and 2009; preparation involved advanced CT scanning for internal structures, and elements have been exhibited at the University of Oslo's Natural History Museum since 2012, with ongoing displays highlighting Arctic paleoenvironments as of 2025. Pliosaurus kevani was named in 2013 from a near-complete and ( NHMUK PV R 12552, Weymouth Bay specimen) discovered piecemeal between 2003 and 2012 from the at Weymouth Bay, Dorset, . The measures 1.995 meters long, with a preorbital region comprising 52% of its length and about 60 mandibular teeth, indicating similarity to P. funkei in size and predatory adaptations, with an estimated body length of 9–10 meters. It is diagnosed by a broad temporal region and pronounced for jaw muscle attachment. The specimen underwent meticulous preparation over five years, involving acid and consolidation; it entered permanent at Dorset County Museum in in 2013 and remains on display as of 2025. Pliosaurus rossicus was established in by N.I. Novozhilov based on a partial ( PIN 2440/1) and associated vertebrae from the Lower Volgian () deposits along the River, region, . This species is characterized by a mandibular count of approximately 50 and elongated vertebral centra, suggesting a body length of 8–9 meters, though its validity has been noted as tentative due to limited material. Diagnostics include a slender and conical , adapted for piercing prey in deeper settings. Pliosaurus westburyensis was formally named in 2013, drawing on fragments and partial cranium ( BRSMG Ck430) originally collected in 1910 from the at , , and later described in 1993. It features a short (15–20% of ) and around 70 teeth, with an estimated of 1.5 meters and body size of 7–8 meters, indicating a more compact form than other . The material highlights early 20th-century collecting efforts and has been referenced in studies of pliosaurid diversity without dedicated public exhibition. In 2023, a nearly complete 2-meter-long was discovered eroding from the at , Dorset, , representing one of the largest known pliosaurid crania. This specimen, potentially indicative of a new species, was the subject of the 2024 BBC documentary "Attenborough and the Giant Sea Monster" narrated by Sir , exploring its excavation and significance. It entered the in April 2024 as the largest known and is on display at the Etches Collection in Kimmeridge as of 2025, contributing to ongoing studies of pliosaurid diversity.
SpeciesHolotype SpecimenFormation & LocationKey DiagnosticsEstimated Size
P. brachydeirusOUMNH J.9245 (partial skull and associated elements), , , ~70 mandibular teeth; gracile build5–7 m
P. carpenteriNHMUK PV R 3533 (partial ), ~60 teeth; robust vertebrae~8 m
P. funkeiPM628 (partial )Agardhfjellet Fm., Long ; trihedral teeth~10 m
P. kevaniNHMUK PV R 12552 (skull & mandible), Broad temporal region; ~60 teeth9–10 m
P. rossicusPIN 2440/1 (mandible & vertebrae)Lower Volgian, ~50 teeth; slender 8–9 m
P. westburyensisBRSMG Ck430 (jaw fragments), Short ; ~70 teeth7–8 m

Dubious Species and Taxonomic Revisions

Several species originally assigned to Pliosaurus have been re-evaluated as dubious or synonymous due to inadequate diagnostic material or taxonomic overlap. Pliosaurus brachyspondylus, described by Owen in 1841 based on vertebrae from the Formation in , has its lost, rendering it a under ICZN rules, as the neotype (CAMSM J.29564) lacks species-level diagnostic features. Subsequent analyses, including a 2013 study on a large pliosaurid , reinforced this status, noting uncertainty in its distinction from P. brachydeirus without clarifying mandibular or dental traits. Pliosaurus macromerus, erected by Seeley in from fragmentary postcranial remains including a femur from the of , was initially considered poorly diagnostic. Although Knutsen (2012) proposed a neotype (NHMUK 39362) to validate it based on mandibular tooth count and retroarticular process , later assessments have suggested it may represent a junior synonym of P. brachyspondylus or P. rossicus due to overlapping vertebral proportions and stratigraphic similarity, though this remains unresolved without additional cranial material. Pliosaurus irgisensis, named by Novozhilov in 1948 from a fragmentary (PIN 426) in the Upper of , is regarded as a and reassigned to indeterminate, as the specimen lacks autapomorphies distinguishing it from other pliosaurids and may pertain to P. rossicus based on size and age. Southern Hemisphere taxa present additional uncertainties. Pliosaurus patagonicus, described in 2014 from isolated teeth in the middle Vaca Muerta Formation of , was proposed based on conical crown morphology with fine striations, but its generic assignment remains unconfirmed due to the absence of associated skeletal elements for comparison with . Similarly, Pliosaurus almanzaensis, named in 2018 from a partial (MOZ 3728P) in the upper of , exhibits autapomorphies such as angular participation in the and a notched occipital condyle, yet its validity within Pliosaurus is debated, with some suggesting it warrants a new genus given deviations in symphyseal alveoli count (nine or more) from northern counterparts. The 2012 taxonomic revision by Knutsen et al. reduced the number of valid Pliosaurus species to four (including P. brachydeirus, P. brachyspondylus, P. macromerus, and P. funkei) by emphasizing cranial and dental characters, while reclassifying others as invalid or indeterminate, a framework that has influenced subsequent work but prompted ongoing refinements. Recent studies from 2023 highlight mandibular symphyseal morphology as key to resolving referrals, noting potential but lacking consensus on integration with Laurasian taxa. As of 2025, discussions continue on whether P. almanzaensis aligns with Pliosaurus or represents a distinct lineage, pending phylogenetic analyses incorporating new Patagonian finds.

Anatomy and Description

Skull and Jaws

The skull of Pliosaurus is characteristically elongate and robust, reaching lengths of up to 2 meters in large species such as P. kevani and specimens from Weymouth Bay, Dorset. This longirostrine form features a preorbital region comprising approximately 57% of the total length, with a transversely broad temporal region measuring around 730 mm in width and supporting extensive adductor muscle chambers via large temporal fenestrae. The high temporal region, often with a smooth parietal crest up to 85 mm tall, accommodated powerful musculature, including the M. adductor mandibulae externus and M. pterygoideus, contributing to the genus's predatory adaptations. The of Pliosaurus exhibits a long , extending anteriorly to accommodate 9–17 alveoli depending on the and specimen, as seen in P. brachyspondylus (up to the 8th–9th alveolus) and P. kevani (14–15 symphysial alveoli). Total mandibular length can exceed 2 meters, with the being proportionally robust yet shorter in some reconstructions to reduce stress concentrations during feeding. In certain , the bone contributes significantly to the and posterior ventral margin, forming a spearhead-shaped process that extends from the 14th alveolus to the retroarticular process, enhancing structural integrity. Key palatal and articular elements include the quadrate and pterygoid bones, which underpin the powerful bite mechanics. The quadrate is stout with a double condyle—shallow laterally and deep medially—articulating firmly with the squamosal to resist torsional forces. The triradiate pterygoid features anterior, lateral, posterior, and quadrate rami, forming a ventral and serving as an origin for adductor muscles; it is partially preserved in many specimens but digitally reconstructed to span the posterior . These structures supported estimated bite forces of up to approximately 49,000 N in large specimens, based on biomechanical analyses from a 2014 study. Sensory adaptations in the Pliosaurus skull include large external nares, measuring 116–118 mm anteroposteriorly and 24–38.5 mm mediolaterally, positioned for enhanced underwater olfaction. A prominent suboval pineal , up to 57 mm long and 23 mm wide with a raised rim, lies posterior to the orbits, potentially aiding in environmental sensing. The orbits are large and anterodorsally oriented, bordered by an embayed prefrontal margin, facilitating acute essential for hunting.

Dentition and Bite Force

The teeth of Pliosaurus are monocuspid and conical, featuring trihedral or sub-trihedral cross-sections with fine, apicobasal ridges on the lingual surface and smooth labial faces, adaptations suited for puncturing and gripping prey. These teeth exhibit fine serrations along the cutting edges in some , enhancing their predatory function. Crowns are robust and recurved in anterior positions, becoming stouter and more hooked posteriorly, with lengths reaching up to 13 cm in large specimens. Dental arrangement in Pliosaurus includes 8–9 pairs of teeth (16–18 total) in the , with the upper jaw featuring approximately 6 premaxillary teeth and 7–8 maxillary teeth per side, potentially totaling up to 30 teeth along the maxillary margin. Tooth replacement follows a patterned , with showing symmetrical resorption and longer intervals (period 4), while posterior teeth display asymmetrical patterns and faster replacement (periods 2–3), indicative of continuous use in active predation. Wear patterns on crowns, including apical and longitudinal striations, further suggest frequent engagement with resistant prey tissues. The enamel cap on Pliosaurus teeth is thick relative to the dentine core, providing durability for piercing tough-skinned or armored prey, as evidenced by the low proportion of exposed dentine even in worn specimens. This structure is supported by the robust cranial architecture, including a short and wide , which distributes occlusal loads effectively. Biomechanical analyses of Pliosaurus feeding mechanics employ lever models and finite element analysis (FEA) to assess bite performance. A 2014 study on P. kevani used the "dry skull" method with a 1.5× correction, estimating bite forces ranging from 9,617 N at anterior positions to a maximum of 48,728 N posteriorly, comparable to those of large crocodylians. FEA of the same specimen revealed high stress concentrations at the maxillary-premaxillary suture and caudal during simulated bites, indicating a trade-off between size and structural optimization for powerful, but potentially risky, predation. For P. funkei, lever-based models estimate peak bite forces around 33,000 N, reflecting its larger proportions. Species variations in dentition include more robust, deeply rooted teeth in P. funkei compared to the relatively gracile crowns in P. kevani, correlating with greater overall body size and presumed prey-handling demands.

Postcranial Skeleton

The postcranial skeleton of Pliosaurus is characterized by a robust axial column adapted for stability in a fully , with a notably short consisting of a reduced number of (fewer than in long-necked plesiosaurs). These vertebrae are massive and abbreviated anteroposteriorly relative to their height and width, featuring flattened, subcircular to slightly oval centra and prominent ventral subcentral foramina for neurovascular passage. Recent discoveries, such as large from the Formation near Abingdon, (described in 2023), further illustrate the robust . Neural arches are robust, with tall, anteroposteriorly oriented spines that supported strong epaxial musculature, as evidenced in specimens like the Westbury pliosaur where at least 17 vertebrae preserve associated neural processes. Dorsal vertebrae transition smoothly, maintaining similar robust proportions to reinforce the compact torso. The pectoral and pelvic girdles are enlarged and plate-like, forming broad ventral platforms that anchored powerful swimming muscles and stabilized the body against hydrodynamic forces. In P. carpenteri and related , the scapulae and coracoids expand laterally to create a deep , while the pubis and form a similarly expansive pelvic , with the ilium articulating via sacral . The limbs are modified into four hydrofoil-like flippers, with elongate propodials (humeri and femora up to 1 m in large individuals) and shortened, robust epipodials; hyperphalangy is pronounced, adding extra phalanges to elongate the paddles, which could span up to 3 m in the largest specimens like P. funkei. Caudal vertebrae number around 30–40, tapering progressively in size to form a flexible tail fin base, with haemal spines (chevrons) and reduced caudal ribs supporting a deep, muscular caudal region for propulsion. Gastralia form a rigid ventral basket between the girdles, consisting of overlapping, boomerang-shaped elements that provided structural support and protected internal organs. Dorsal ribs are robust and double-headed, articulating with centra and transverse processes to encase the thoracic cavity, while preserved elements in Westbury specimens include at least seven large ribs. These features align with pliosaurid trends seen in Liopleurodon, where similar short cervical counts and enlarged girdles emphasize a streamlined, powerful body plan, though Pliosaurus exhibits proportionally more robust neural spines. Larger body sizes in Pliosaurus amplify skeletal robustness, scaling vertebral and girdle dimensions accordingly.

Size and Morphology

Body Dimensions and Proportions

Pliosaurus species displayed considerable variation in body size, with total lengths generally estimated at 6 to 10 meters based on comparisons of skeletal elements from multiple specimens. Smaller species such as P. carpenteri reached ~8 m, while the largest, including P. funkei and P. kevani, attained lengths up to 10 to 12 meters, derived from 2023 scaling analyses that extrapolated from dimensions and vertebral proportions. These estimates highlight the genus's for predation through substantial overall mass, often exceeding 10 tonnes in the biggest individuals. The typically comprised about 1:5 to 1:6 of the total body length, emphasizing the disproportionate size of the head relative to the postcranial in this short-necked pliosauromorph . The neck, formed by typically 4–5 , accounted for approximately 10 to 15% of the overall length, contributing to a compact anterior region optimized for rapid head movements. Limb proportions exhibited clear , with foreflippers longer and more robust than hindflippers, facilitating primary and during underwater locomotion. A notable example is the Abingdon specimen from the Formation, initially estimated in 2023 at 9.8 to 14.4 meters using cervical scaling against related pliosaurids like . However, 2024 revisions incorporating refined body reconstruction models reduced this to 10.7 to 11.8 meters, correcting the prior overestimation by accounting for more accurate intervertebral and trunk proportions.

Growth Patterns and Ontogeny

Histological analyses of plesiosaur bones, including those from pliosaurids, reveal fibrolamellar bone tissue indicative of rapid rates during early , comparable to those observed in modern crocodilians but potentially elevated due to denser vascularization and parallel-fibered matrix deposition. marks such as annuli and lines of arrested (LAGs) in limb s suggest periodic slowdowns in deposition, with early formation of the first LAG occurring after substantial body size is achieved, implying accelerated juvenile followed by sustained but decelerating into adulthood. These features point to indeterminate patterns, akin to those in extant reptiles like crocodilians, where individuals continue adding layers throughout without a fixed cessation point. In Pliosauridae, ontogenetic changes are evident in dental development, where juvenile specimens exhibit recumbent replacement teeth initiating in shallow crypts, transitioning to vertical orientation and deeper alveolar embedding in adults, reflecting maturation of the feeding apparatus. Symphyseal regions in derived species show symmetrical tooth replacement in anterior jaws during early stages, shifting to asymmetrical patterns posteriorly as the animal grows, potentially correlating with increased robusticity in the for handling larger prey. The subadult of kevani (specimen DORCM G.13,675), with a length of approximately 2 and unfinished sutures such as the non-co-ossified , exemplifies intermediate ontogenetic features, indicating ongoing cranial fusion despite near-adult proportions.

Taxonomy and Phylogeny

Historical Taxonomy

The genus Pliosaurus was established by in 1841, based on isolated jaw elements from the Formation of , which he placed within the order Plesiosauria as a short-necked form distinct from typical long-necked plesiosaurs. The , P. brachydeirus, was diagnosed by its robust and trihedral teeth featuring fine longitudinal ridges, with the consisting of a partial lower (OUMNH J.9245) measuring about 1.2 meters long. emphasized the genus's lizard-like dental morphology, contrasting it with the conical teeth of other plesiosaurs, and he formally included it in his newly proposed superorder in 1860, recognizing marine reptiles as a cohesive group beyond terrestrial saurians. By the early 20th century, taxonomic practices often lumped Pliosaurus species with the genus Liopleurodon (erected by Sauvage in 1873), particularly due to overlapping features like proportions and tooth counts, leading to synonymies such as Pliosaurus ferox being reassigned to Liopleurodon ferox. This lumping was influenced by limited complete specimens and a focus on isolated cranial elements, with European finds from the and dominating interpretations and blurring distinctions between and Kimmeridgian-Tithonian forms. In the mid-20th century, L.B. Tarlo provided the first comprehensive revision of Upper pliosaurs in 1960, subgrouping taxa within Pliosaurus based on mandibular tooth counts—distinguishing forms with 30–38 teeth per mandibular ramus (60–76 total) and 10–12 pairs in the from those with shorter (fewer than 10 pairs)—and recognizing at least five valid including P. brachydeirus, P. brachyspondylus, and P. andrewsi. Tarlo's work separated "true" short-necked pliosaurs from longer-necked relatives like rhomaleosaurs, emphasizing vertebral and cranial metrics from specimens. During the 1970s and 1980s, further revisions by researchers like L. Beverly Halstead and D.S. Brown refined these separations, explicitly distinguishing pliosaurs (characterized by highly reduced necks of 4–6 and massive skulls) from rhomaleosaurs (with 11–13 cervicals and more elongated snouts), based on postcranial proportions from European and emerging material. Halstead's 1971 analysis, for example, reassigned P. rossicus (Novozhilov, 1948) to due to its abbreviated symphysis, while Brown's 1981 review of plesiosauroids upheld Tarlo's subgroups but incorporated new finds to validate additional species like P. macromerus. By the late , over 10 species names had proliferated within Pliosaurus, driven by isolated bones from European sites (e.g., P. westburyensis from the ) and Volga River deposits (e.g., P. irgisensis by Novozhilov in 1964), reflecting regional biases in fossil recovery and variable diagnostic criteria like dental ornamentation and jaw robusticity.

Phylogenetic Relationships

Pliosaurus is classified within the family , specifically as a member of the clade , a group of advanced pliosaurids characterized by large skulls and short necks that dominated marine predator guilds from the to the early . This placement is supported by cladistic analyses using morphological datasets, where Pliosaurus forms part of the derived thalassophonean radiation, often positioned near the base of Brachaucheninae in recent matrices. Within , Pliosaurus shares synapomorphies such as a relatively long and subtrihedral tooth cross-sections with well-developed labial and lingual carinae, features that distinguish it from earlier pliosaurids like . Phylogenetic matrices from 2012 to 2023 consistently recover Pliosaurus as monophyletic, though internal relationships remain partially unresolved due to limited postcranial data for some species. Recent analyses (up to 2023) continue to support this placement, with no significant changes as of 2025. For instance, analyses using modified datasets from Ketchum and Benson (2010) show varying topologies within the genus, with low bootstrap values (under 50%) for deeper pliosaurid nodes but higher consistency for genus-level synapomorphies. Recent weighted parsimony approaches in 2023 datasets further affirm this topology, with Pliosaurus forming a clade with Simolestes exhibiting moderate Bremer support (2-3 steps) for shared mandibular features like a mediolaterally thick surangular. Debates persist regarding the of Pliosaurus, particularly the inclusion of taxa such as P. almanzaensis from , which some 2023-2024 analyses suggest may warrant separation into a distinct due to divergent symphyseal and geographic isolation, potentially indicating rather than close affinity with European species. Bootstrap support for the Pliosaurus + Simolestes varies (40-60% in unweighted analyses), highlighting sensitivity to character scoring in mandibular and dental traits, though most trees uphold monophyly when excluding fragmentary Southern material. In broader context, Pliosaurus exemplifies the radiation of thalassophoneans following the (post-Toarcian) bottleneck, where diversity rebounded after the reduced early plesiosauroid lineages, enabling pliosaurids to diversify into macropredatory niches by the Oxfordian-Kimmeridgian.

Paleobiology

Locomotion and Buoyancy

Pliosaurus utilized a four-flipper system characteristic of plesiosaurs, generating primary through powerful strokes of the enlarged hind flippers while employing the fore flippers primarily for steering, stability, and fine maneuverability. This underwater flight-style , involving dorso-ventral oscillations of the flippers, enabled efficient cruising. Skeletal features such as robust pelvic girdles and elongated hind limb elements facilitated this hindlimb-dominant , distinguishing pliosauroids from long-necked plesiosauroids. Buoyancy in Pliosaurus was regulated through a multi-layered system involving adjustable lung volume for dynamic control and skeletal for static stability. The limb bones exhibit high with solid cortices and no open medullary cavities, functioning as to offset the positive provided by air-filled lungs and achieve near- during submersion. This is further inferred from the robust, amphicoelous vertebral structure, which supported a streamlined adapted for prolonged aquatic life without excessive energy expenditure on depth regulation. Hydrodynamic modeling has highlighted adaptations in Pliosaurus for minimizing resistance in water. The short neck reduced overall drag by streamlining the anterior body profile, facilitating smoother flow over the torso and flippers during . This configuration parallels that of extant sea turtles, where compact necks contribute to low-drag hydrodynamics during flipper-driven , allowing Pliosaurus to maintain efficiency at moderate speeds despite its massive size.

Feeding Ecology and Prey

Pliosaurs of the genus Pliosaurus occupied the role of apex predators in ecosystems, targeting a diverse array of prey including ichthyosaurs, s, , teleost fishes, hybodont sharks, and cephalopods. Direct evidence of predation comes from bite marks on remains, such as triangular scars on the of an indeterminate ophthalmosaurid ichthyosaur (specimen SGM 1566), attributed to a medium-sized pliosaur based on cross-section and spacing; these marks, measuring 12–15 mm in length and lacking signs of healing, suggest a fatal attack. Similar bite traces appear on plesiosaur propodials and the of Eromangasaurus armstrongi, confirming Pliosaurus as a top-tier capable of subduing large reptiles up to half its body length. Feeding strategies emphasized predation, leveraging the streamlined, hydrodynamic for rapid and inertial strikes to impale prey with robust, trihedral teeth positioned for crushing. Biomechanical modeling of Pliosaurus kevani (specimen NHMUK PV R12626) estimates bite forces reaching 48,000 N at the rear dentary teeth, far exceeding those of modern crocodilians and enabling penetration and dismemberment of tough tissues; this supports brief reference to optimized for prey capture rather than sustained tearing. Although lateral head shaking has been hypothesized in pliosaurids for prey manipulation, finite element analysis indicates the snout's structure was poorly suited for such torsional loads, favoring instead powerful, direct clamping. Inferred diet from preserved stomach contents in a pliosaurid from the includes abundant hooklets, fish scales and bones, and isolated reptilian teeth, pointing to an opportunistic, feeding habit that incorporated both soft-bodied and armored prey. Niche partitioning is evident among pliosaurids, with larger species like P. kevani ( ~2 m long) specializing in high-bite-force predation on sizable marine reptiles, while smaller congeners (e.g., P. westburyensis) likely focused on fishes and , as indicated by comparative cranial robusticity and adductor muscle leverage across sympatric taxa. This differentiation minimized in resource-rich epicontinental seas.

Paleoecology and Distribution

Temporal and Stratigraphic Range

Pliosaurus encompasses a stratigraphic range primarily within the , spanning the to stages, approximately 157 to 145 million years ago. The radiation of macropredatory pliosaurids, including the genus Pliosaurus, correlates to the Middle- boundary, with Pliosaurus first appearing in the stage and subsequent expansion into marine deposits of the and Tethyan realms. Fossils of Pliosaurus are most abundantly preserved in several key Upper Jurassic formations, reflecting peak generic diversity during the late stage. In , the Kimmeridge Clay Formation yields multiple species, including P. kevani and P. portentificus, from its lower to upper members, which span the late to earliest . The Slottsmøya Member of the Agardhfjellet Formation, dated to the middle (regional Volgian stage), has produced well-preserved specimens such as P. funkei, highlighting the persistence of the genus into the latest . In , the Formation contains -aged remains, including two species of Pliosaurus (P. patagonicus and P. almanzaensis), indicating broader hemispheric distribution during this interval. Stratigraphic correlations across these units reveal a pattern of increasing morphological disparity from the onward, with the late representing a zenith in before a decline in the , possibly linked to environmental shifts in epicontinental seas. Associated faunas in these strata, such as ophthalmosaurid ichthyosaurs and cryptoclidid plesiosaurs, provide for Pliosaurus as a dominant in shallow to deep-water settings.

Geographic Occurrences and Environments

Fossils of Pliosaurus are primarily known from deposits across , reflecting its dominance in marine ecosystems during this interval. In , numerous well-preserved specimens, including the holotype skull of P. kevani, have been recovered from the Formation along the of Dorset, representing outer shelf to basinal environments. In , particularly the Arctic archipelago of , large partial skeletons assignable to P. funkei occur in the Slottsmøya Member of the Agardhfjellet Formation, providing evidence of the genus's extension into high-latitude settings. Secondary occurrences outside Europe are rarer but significant for understanding Pliosaurus's broader distribution. In South America, two species, P. patagonicus and P. almanzaensis, are based on material from the Upper Jurassic Vaca Muerta Formation in Neuquén Province, Patagonia, Argentina, indicating trans-hemispheric dispersal via ancient seaways. These finds, though fragmentary, highlight the genus's presence in southern high-latitude basins during the Tithonian stage. The paleoenvironments inhabited by Pliosaurus were predominantly shallow epicontinental seas within the Jurassic Sub-Boreal Seaway, a northward extension of the that spanned from subtropical to polar latitudes. This seaway featured warm, tropical waters, with surface temperatures supporting diverse ectothermic , and exhibited high biological productivity driven by nutrient influx from enhanced and riverine input under a monsoonal regime influenced by dynamics. Black shale deposits in the seaway, such as those in the , attest to periods of elevated organic carbon accumulation linked to this nutrient-rich setting. Recent analyses of specimens from underscore the polar extensions of Pliosaurus's range, with the Slottsmøya yielding articulated pliosaurid remains that reveal fine anatomical details otherwise obscured by taphonomic processes. Preservation in this region is biased by congelifraction from freeze-thaw cycles, climatic due to sparse vegetation cover, and selective mineralization in carbonates, leading to underrepresentation of smaller or more fragile elements and favoring larger, robust macro-predators like Pliosaurus. These biases, compounded by limited outcrop exposure and collection efforts in remote polar areas, suggest the genus's true diversity and abundance in high latitudes may be underestimated.

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