Polycotylidae is a family of short-necked plesiosaurian marine reptiles within the clade Xenopsaria, characterized by elongated skulls, robust dentition, and limbs adapted as paddles for aquatic locomotion, which first appeared during the Early Cretaceous and persisted until the end of the Late Cretaceous.^[1] Derived from long-necked plesiosauroids, polycotylids evolved short necks convergently with the distantly related pliosaurids, marking a significant morphological shift toward more streamlined, predatory forms suited to open marine environments.^[1] Their fossils, including well-preserved skeletons with evidence of gastroliths and viviparity, indicate they were apex predators with global distributions across Laurasian and Gondwanan continents.^[2][3] The family's evolutionary history reveals an origin possibly as early as the Berriasian stage, with definitive records from the Albian, followed by a radiation during the Cenomanian–Turonian stages of the Early Late Cretaceous, when they achieved peak diversity and morphological disparity.^[1] Notable genera include the type genus Polycotylus, known for its large size and powerful jaws from Late Cretaceous North American deposits; Dolichorhynchops, a smaller, agile form with slender snouts; and Thililua, an atypical member with a longer neck comprising 30 cervical vertebrae and carinated teeth, highlighting intrafamilial variation.^[1] Other taxa, such as Mauriciosaurus and Plesiopleurodon, further illustrate their cosmopolitan presence, from Mexico to Antarctica.^[1] Phylogenetic analyses place Polycotylidae within a subclade including the Occultonectia group, closely related to cryptoclidids rather than Jurassic pliosaurs, underscoring homoplasy in short-necked adaptations.^[2] Polycotylids' anatomy features triradiate clavicles, curved ilia, and scapulae that ossify extensively in adulthood, adaptations enhancing pectoral girdle stability for propulsion.^[2] Evidence from specimens like a gravid Polycotylus latipinnis confirms viviparous reproduction, with embryos positioned head-first for birth, a trait shared with other marine reptiles.^[2] Despite their abundance in formations like the Pierre Shale, taxonomic challenges arise from ontogenetic changes and convergent traits, leading to ongoing revisions in genus-level classifications.^[2] Their decline coincided with the end-Cretaceous extinction, leaving no descendants.^[1]

Description

Cranial anatomy

The skulls of polycotylids are characterized by an elongated rostrum that typically comprises over 60% of the total skull length, forming a narrow, triangular shape adapted for streamlined pursuit of prey in marine environments.^[4] In Polycotylus latipinnis, for example, the preorbital region accounts for approximately 65% of the skull, contributing to a hydrodynamic profile that enhances predatory efficiency.^[1] This rostral elongation contrasts with the relatively short neck in these plesiosaurs, emphasizing a head-focused strategy for hunting.^[4] Dentition in polycotylids features numerous small, conical teeth with sharply pointed crowns suited for grasping slippery prey such as fish. The mandibular symphysis often bears 18–20 teeth, while the maxilla supports 20–25 alveoli, with teeth exhibiting fine striations and slight recurvature. Heterodonty is evident in genera like Dolichorhynchops, where anterior teeth are larger and more robust compared to posterior ones, facilitating initial capture and retention of prey. Adult skull lengths generally range from 40 to 80 cm, with P. latipinnis serving as a representative example at around 50–60 cm. The temporal region displays large temporal fenestrae and a prominent sagittal crest, which anchor powerful jaw adductor muscles for delivering rapid, forceful bites.^[4] In Dolichorhynchops, the fenestrae are short but broad, and the crest is high and sharply keeled, whereas in Polycotylus it is lower and more elongate, reflecting variations in bite mechanics across the family.^[4] Orbits are notably large and positioned to enable enhanced binocular vision, aiding in depth perception during hunts, while a pineal foramen on the parietal bone suggests potential sensitivity to light for environmental cues.^[4]

Postcranial anatomy

Polycotylids exhibit a short neck relative to long-necked plesiosauroids such as elasmosaurids, typically comprising 19–26 cervical vertebrae.^[5] For example, Dolichorhynchops species possess 21 cervical vertebrae, while Polycotylus latipinnis has 26.^[6] The axial skeleton is robust, with 17–20 dorsal vertebrae characterized by broad neural spines that served as attachment points for axial musculature.^[6] In Occultonectia, the dorsal count ranges from 17 to 19 vertebrae.^[6] The limbs are modified into four large, hydrofoil-shaped flippers, with hyperphalangy evident in both the manus and pes due to an increased number of phalanges beyond the ancestral condition.^[7] The propodials are elongated and flattened to form paddle-like structures.^[8] The pelvic girdle features robust ilia and ischia that articulate to form a rigid basin enclosing the pelvic cavity and supporting the hindlimb flippers.^[9] In Polycotylus latipinnis, the ilia exhibit distinctive morphology, including variability potentially linked to ontogeny or dimorphism.^[8] Evidence of viviparity is preserved in a specimen of Polycotylus latipinnis containing a single large embryo (approximately 1.5 m long) positioned head-first within the maternal body cavity, consistent with the expanded pelvic outlet morphology permitting live birth.^[2] The tail is moderately elongate, consisting of 15–20 caudal vertebrae with low neural spines and chevrons that taper posteriorly.^[5] In one Albian polycotylid specimen, at least 18 caudal vertebrae are documented.^[5]

History of research

Discovery and naming

The genus Polycotylus was first established by American paleontologist Edward Drinker Cope in 1869, based on a partial skeleton comprising vertebrae, an ilium, metapodials, and phalanges recovered from the Late Cretaceous Pierre Shale of western Kansas, United States.^[10] The type species, P. latipinnis, was named from this fragmentary material, which represented postcranial elements collected during early explorations of the Western Interior Seaway deposits.^[11] The type locality lies within the Sharon Springs Member of the Pierre Shale, a marine depositional environment characterized by chalky shales indicative of shallow epicontinental seas during the Campanian stage.^[12] Early discoveries of polycotylid material occurred primarily in North America between the 1870s and 1900s, led by Cope and contemporaries such as Othniel Charles Marsh amid the "Bone Wars" rivalry, with specimens unearthed from the Western Interior Seaway's Niobrara and Pierre formations in Kansas and surrounding states.^[13] A notable referred specimen, SMNS 10958, consists of a well-preserved skull and partial skeleton of Polycotylus from the Pierre Shale, providing early insights into cranial morphology despite initial fragmentary evidence.^[14] These finds highlighted the short-necked anatomy of the group, leading to initial taxonomic confusion with pliosaurs, as the reduced cervical count mimicked Jurassic pliosauromorphs rather than typical long-necked plesiosaurs.^[15] The family Polycotylidae was formally erected by Samuel Wendell Williston in 1908 to accommodate Polycotylus and the related genus Trinacromerum as core taxa, distinguishing them from other plesiosauroids based on shared features like elongate snouts and robust limb girdles adapted for marine propulsion.^[16] Williston's diagnosis emphasized the group's distinctiveness within Cretaceous marine reptiles.^[17] In Europe, 19th-century reports of possible polycotylid fragments, such as isolated teeth from the Chalk Group of England attributed to forms like Polyptychodon, were later reassigned to other plesiosaur groups or deemed indeterminate due to morphological overlaps with local taxa.^[18]

Systematic revisions

During the early 20th century, polycotylids were initially classified within Pliosauridae due to their short necks and large skulls, but this assignment was revised in the 1920s through the 1980s as evidence from vertebral counts—typically 19–26 cervical vertebrae in polycotylids, more than the 10–15 in pliosauroids—along with other postcranial features supported their reassignment to Plesiosauroidea. Andrews (1922) contributed to this shift by describing related short-necked forms like Leptocleidus, highlighting morphological affinities with plesiosauroids rather than pliosauroids. Welles (1962) further solidified this reassignment in his comprehensive review of Cretaceous plesiosaurs, proposing the family Dolichorhynchopidae (later reverted to Polycotylidae) and emphasizing vertebral and cranial features that aligned polycotylids firmly within Plesiosauroidea. From the 1990s onward, polycotylids gained recognition as a distinct group of short-necked plesiosauroids, with cladistic analyses refining their position outside the elasmosaurid radiation. O'Keefe (2001) conducted a seminal phylogenetic study that proposed the clade Xenopsaria, encompassing polycotylids alongside leptocleidids and other short-necked forms, based on shared synapomorphies such as reduced cervical counts and specialized cranial kinesis. This framework highlighted polycotylids' derivation within Plesiosauroidea, distinct from long-necked plesiosauroids. Key taxonomic revisions in the 2000s addressed synonymies and generic boundaries within Polycotylidae. Albright et al. (2007) examined new material from the Tropic Shale, addressing nomenclatural issues by providing replacement names for preoccupied genera such as Palmula (renamed Palmulasaurus) and streamlining diagnoses, thereby reducing the number of valid genera based on overlapping postcranial and dental traits. Ketchum and Benson (2010) confirmed the plesiosauroid affinity of Polycotylidae through an expanded cladistic analysis incorporating 137 characters across 50 plesiosaur taxa, recovering polycotylids as a monophyletic sister group to elasmosaurids within Plesiosauroidea and rejecting earlier pliosauroid placements.^[19] Recent additions to the family have challenged assumptions of uniformity in neck length and body plan. The description of Serpentisuchops pfisterae in 2022 revealed a long-necked polycotylid, with approximately 25 cervical vertebrae contrasting the typical short-necked condition, prompting reevaluation of morphological diversity within the clade.^[20] Ongoing debates surround genera like Rarosaurus (described in 2019), with recent analyses (as of 2024) suggesting crocodylomorph affinities based on atypical cranial proportions and limb structure, rather than retention within Polycotylidae pending further material. More recent discoveries, such as the small-bodied Unktaheela specta from the Campanian of North America (Sato et al., 2024), and revisions to South American taxa like Sulcusuchus erraini (O'Gorman et al., 2023), continue to expand understanding of polycotylid diversity and circum-Pacific distribution.^[21][22] Methodological advances, including CT scans, have informed revisions by revealing ontogenetic changes relevant to taxonomy. O'Keefe and Byrd (2012) applied CT imaging to Polycotylus latipinnus specimens, documenting scapular and girdle remodeling during growth that supports viviparity evidence and clarifies diagnostic characters for distinguishing juvenile forms from separate genera.^[2]

Classification

Included genera

Polycotylidae encompasses approximately 13 to 18 valid genera, comprising around 19 recognized species, primarily known from Cretaceous marine deposits worldwide, with body lengths ranging from about 3 to 9 meters.^[23] The family exhibits considerable morphological diversity, including variations in neck length, skull elongation, and vertebral counts, though most genera share short necks and elongated snouts adapted for piscivory.^[24]

Valid Genera

• Polycotylus: The type genus of the family, known from the Late Cretaceous (Turonian to Campanian) of North America, particularly the Western Interior Seaway; the type species P. latipinnis reaches approximately 3.5–4 meters in length, with a short neck of 26 cervical vertebrae and a robust skull featuring a broad temporal fenestra. Additional species include P. sopozkoi from the Campanian of Russia, distinguished by protruding basioccipital tubera.^[24][23]
• Dolichorhynchops: A diverse genus from the Late Cretaceous (Turonian to Campanian) of North America, especially Kansas; known from multiple species such as D. bonneri, D. tropicensis, and D. herschelensis, with specimens often representing juveniles; features a notably elongated snout, short neck of 21 cervical vertebrae, and overall length of 2–4 meters; exhibits paraphyletic tendencies in some analyses.^[24]
• Trinacromerum: Restricted to the Turonian of North America; the type species T. bentonianum possesses a short neck with 21 cervical vertebrae and a single jugal foramen, attaining lengths of about 4–5 meters.^[24]
• Eopolycotylus: The earliest known polycotylid, from the early Turonian (Early–Late Cretaceous boundary) of Utah, USA; the species E. rankini is characterized by a short neck and represents an early diversification of the family.^[24]
• Manemergus: From the Cenomanian of Canada; M. anguirostris is a small, possibly juvenile form with 25 cervical vertebrae, potentially congeneric with more derived taxa, though retained as valid pending further material.^[24]
• Edgarosaurus: Known from the Turonian of Texas, USA; E. muddi has a short neck with 26 cervical vertebrae and two small jugal foramina, estimated at 4–5 meters long.^[24]
• Mauriciosaurus: From the Early Turonian of Mexico; M. fernandezi is notable for a pregnant specimen preserving embryos, with 21 cervical vertebrae, an extensive splenial bone, and a body length of approximately 4.5 meters; neck-to-skull ratio of 0.92.^[24]
• Thililua: Middle Turonian of Morocco; T. longicollis stands out with an unusually long neck of 30 cervical vertebrae (among the highest in the family), carinated teeth, and foramina-bearing jugal; skull length 665 mm, neck 2.17 m, total estimated over 6 meters.^[24]
• Plesiopleurodon: Cenomanian of North America; P. wellesi features a short neck and a long maxillary groove, with a compact build around 3–4 meters.^[24]
• Sulcusuchus: Late Campanian to Early Maastrichtian of Patagonia, Argentina; S. erraini is a small-bodied form (under 3 meters) with a short neck and elongated maxillary groove, representing one of the youngest valid polycotylids.^[24]
• Pahasapasaurus: Cenomanian of North America; P. haasi is diagnosed by a short neck and limited cranial material, estimated at 3–4 meters.^[24]
• Palmulasaurus: Turonian; P. quadratus exhibits a short neck and is known from fragmentary remains, with body size around 4 meters.^[24]
• Georgiasaurus: Late Cretaceous; G. penzensis from Russia features a short neck, though details remain sparse; approximately 4 meters long.^[24]
• Serpentisuchops: Campanian (Pierre Shale) of Wyoming, USA; S. pfisterae is distinguished by a long neck (32 cervical vertebrae) combined with an elongated crocodile-like snout, reaching up to 7 meters, highlighting morphological convergence within the family.^[25]

Other genera such as Unktaheela (a small form from the Upper Cretaceous Western Interior Seaway, ~2 meters) further expand the known diversity. Synonymies include historical referrals like Plesiopleurodon material occasionally lumped with Polycotylus, though currently treated as distinct.^[24]

Dubious or Excluded Genera

Several taxa originally assigned to Polycotylidae have been reclassified or deemed invalid due to insufficient diagnostic material:

• Rarosaurus: From the late Maastrichtian of Jordan; R. singularis was initially considered a polycotylid but is now regarded as likely a crocodylomorph based on cranial features.^[24]
• Piratosaurus: Late Cretaceous (Santonian) of North America; P. plicatus is a nomen dubium, known only from fragmentary vertebrae lacking unique apomorphies.
• Umoonasaurus: Early Cretaceous (Albian) of Australia; U. demoscyllus has been reassigned to Leptocleididae due to its crested skull and coastal adaptations, distinct from polycotylid traits.

Phylogenetic relationships

Polycotylidae represents a derived clade within Plesiosauroidea, specifically nested in the larger Xenopsaria radiation of Cretaceous plesiosaurs, which diverged from Jurassic lineages during the Early Cretaceous.^[26] This positioning places Polycotylidae distal to short-necked pliosauroids such as Rhomaleosauridae and Pliosauridae, emphasizing their evolutionary shift toward more specialized aquatic adaptations within long-necked plesiosauroid stock.^[24] Phylogenetic analyses consistently recover Polycotylidae as the sister group to Leptocleididae, forming a clade of short-necked forms that contrasts with the long-necked Elasmosauridae, though some earlier studies suggested a more basal position relative to Elasmosauridae + Polycotylidae.^[26][24] Key synapomorphies defining Polycotylidae include a reduced cervical count (typically 19–32 vertebrae, fewer than in long-necked plesiosaurs), an elongated premaxilla contributing to a long rostrum, and reduced coracoids with limited scapular articulation, features that support their monophyly and adaptation for agile swimming.^[24] Cladistic datasets, such as those modified from Benson and Druckenmiller (2014), position early stem taxa like Eopolycotylus rankini (Turonian) as basal polycotylines, marking an Early Cretaceous origin before a Late Cretaceous diversification.^[26] This radiation peaked in the Cenomanian–Turonian, with the crown group Polycotylinae—encompassing monophyletic assemblages like Dolichorhynchops + Polycotylus—dominating Campanian assemblages through enhanced cranial elongation and dental specialization.^[24] Outgroup comparisons highlight Polycotylidae's affinity to other xenopsarians, with occasional analyses placing them near Aristonectes (an aristonectine elasmosaurid) due to shared rostral proportions, though this remains debated.^[24] Monophyly is robustly supported in recent phylogenies, resolving prior uncertainties about paraphyly with pliosauroids.^[24] Forms like Serpentisuchops pfisterae, with retained long necks (32 cervicals), represent primitive retentions rather than reversals, underscoring secondary shortening as the derived trend within the family.^[25]

Paleobiology

Locomotion and ecology

Polycotylids utilized a quadrupedal swimming style characterized by subaqueous flight, employing all four flippers in semi-synchronous up-and-down motions to generate thrust and lift, with foreflippers serving as the primary propulsors and hindflippers aiding in steering. This locomotion was efficient for short-necked forms like polycotylids, whose streamlined bodies and hydrofoil-like flippers—detailed in postcranial anatomy—minimized drag during maneuvers.^[27] Bone microstructure analyses reveal high vascularization and rapid deposition of fibrolamellar bone, indicating sustained growth rates consistent with an energetically demanding aquatic lifestyle, though direct speed estimates from preserved soft tissues suggest cruising velocities exceeding 1.9 m/s in species such as Mauriciosaurus.^[28][29] These plesiosaurs inhabited pelagic environments within epicontinental seas, particularly the shallow to mid-depth waters of the Western Interior Seaway during the Late Cretaceous, where they acted as ambush predators capable of rapid lateral strikes on schooling prey. Ontogenetic shifts in bone histology and body proportions, as seen in Dolichorhynchops, suggest juveniles possessed relatively more agile swimming capabilities suited to evasive pursuits, while adults adopted a more stable cruising mode for energy-efficient patrolling of open waters.^[28] Polycotylids filled a mid-trophic level carnivorous niche, preying on mid-sized marine organisms while coexisting alongside larger predators such as mosasaurs and sharks, as inferred from faunal assemblages in deposits like the Niobrara Chalk.^[30][11] Evidence for viviparity in Polycotylus latipinnis, based on a fossilized adult containing a large, well-developed embryo positioned head-first for birth, supports live parturition in fully pelagic settings, eliminating any reliance on terrestrial nesting sites.^[31]

Diet and reproduction

Polycotylids exhibited a piscivorous and teuthophagous diet, primarily consisting of small fish, squid, and other soft-bodied prey that could be grasped and swallowed whole. Their conical, recurved, and narrow teeth were well-suited for piercing and holding elusive, agile prey in the water column, rather than for crushing hard-shelled organisms. Direct evidence of ichthyophagy comes from stomach contents preserved in a polycotylid specimen, which include remains of small fish, confirming predatory interactions with teleost prey. Although coprolites attributable to polycotylids are rare, general patterns in plesiosaur coprolites from similar Cretaceous marine deposits support a diet dominated by fish scales, bones, and cephalopod fragments. Gastroliths preserved in some polycotylid specimens further indicate a diet requiring mechanical aid for digestion of fish and cephalopods.^[32] The elongated snout and mandibular symphysis of polycotylids facilitated rapid jaw closure during pursuit predation in open water, with jaw mechanics emphasizing speed over sustained force. The bite was adapted for initial piercing to immobilize prey, generating sufficient force to penetrate soft tissues without the robust crushing capabilities seen in durophagous reptiles. Tooth and jaw structures, including the arrangement of conical dentition, underscore this strategy for capturing evasive, mid-water prey. Reproduction in polycotylids was viviparous, with females giving birth to live young rather than laying eggs, as demonstrated by a well-preserved specimen of Polycotylus latipinnis (cataloged as LACM 129639) from the Pierre Shale Formation in Kansas, which contains a single embryo positioned within the mother's uterus.^[31] The embryo, measuring approximately 1.5 meters in length compared to the adult's 5-meter body, represents a large offspring at birth—about 30% of maternal size—indicative of a K-selected reproductive strategy focused on few, well-developed young to maximize survival in marine environments. This viviparity likely evolved to avoid the challenges of egg-laying on land or in shallow waters for fully aquatic reptiles. Sexual dimorphism may have been present in the pelvic girdle, with variations in ilium width and morphology potentially reflecting differences between males and females, though direct confirmation remains elusive due to limited associated skeletal data. Individuals reached sexual maturity at lengths of 4–5 meters, based on ontogenetic changes in bone microstructure. Growth was rapid during juvenility, characterized by woven-fibered bone tissue indicative of high metabolic rates, before transitioning to slower lamellar-zonal bone deposition in adults.

Distribution and timeline

Temporal range

Polycotylidae possibly originated during the Aptian stage of the Early Cretaceous, with the earliest potential records from fragmentary remains in Australia; definitive records appear during the Albian stage, approximately 113–100 million years ago (Ma). The oldest known specimens come from the Clearwater Formation in Alberta, Canada, dating to around 110 Ma, representing a partial postcranial skeleton, including articulated cervical vertebrae, dorsal vertebrae, ribs, a partial pelvis, and elements of all four limbs, that confirms the presence of basal polycotylids in North American marine deposits at this time.^[33] Additional early occurrences are documented from the Eagle Ford Group in Texas, which spans the late Albian to early Cenomanian, providing evidence of an initial radiation in shallow epicontinental seas. The family underwent significant diversification during the Cenomanian–Turonian stages of the Late Cretaceous, roughly 100–90 Ma, coinciding with expanding ocean anoxic events and global marine ecosystem shifts that favored short-necked plesiosaurs, marked by a burst in morphological disparity. This interval saw multiple genera emerging across Laurasian and Gondwanan localities, including the Goulmima Formation in Morocco, with maximal disparity achieved in the Cenomanian. High taxic diversity occurred later in the Campanian stage, particularly within the Western Interior Seaway of North America, where polycotylids formed a prominent component of marine reptile assemblages in formations like the Niobrara Chalk (Santonian–Campanian). Following this peak, Polycotylidae experienced a decline starting in the Campanian stage (83–72 Ma), characterized by reduced generic diversity and ecomorphological disparity amid faunal turnovers in epicontinental seas. Possible holdouts persisted into the early Maastrichtian (around 70 Ma), as evidenced by Sulcusuchus erraini from the Allen and La Colonia formations in Patagonia, Argentina, representing one of the geologically youngest named members of the family. However, no records extend beyond the Cretaceous–Paleogene boundary at 66 Ma, with the group succumbing to the end-Cretaceous mass extinction event. Throughout their temporal span, basal polycotylid forms were relatively short-lived, confined primarily to the Early Cretaceous, while derived members of the subfamily Polycotylinae dominated the final approximately 20 million years of the group's history, from the Turonian onward, adapting to diverse pelagic niches before the terminal decline.

Geographic distribution

The fossil record of Polycotylidae is predominantly concentrated in North America, where the majority of known specimens derive from deposits associated with the Western Interior Seaway, a vast epicontinental sea that spanned the continent during the Late Cretaceous.^[6] Key localities include the Niobrara Chalk Formation in Kansas, particularly Sternberg Quarry in Logan County, which has yielded multiple well-preserved skeletons of Dolichorhynchops osborni, including articulated specimens exceeding 3 meters in length.^[34] Other significant U.S. sites encompass the Pierre Shale in Wyoming and South Dakota, the Tropic Shale in Utah, and the Greenhorn Limestone in South Dakota, all representing warm, shallow marine environments of Cenomanian to Campanian age.^[6] In Canada, notable occurrences are from the Albian Clearwater Formation in Alberta and the Campanian Bearpaw Formation in Saskatchewan and Manitoba, highlighting an early Laurasian dominance in the family's distribution.^[35] Beyond North America, polycotylid remains are reported from several Gondwanan and other Laurasian regions, reflecting a later expansion into southern high latitudes. In Mexico, the Early Turonian laminated limestones of Vallecillo in Nuevo León have produced the nearly complete, pregnant specimen of Mauriciosaurus fernandezi, preserving soft tissues and embryos in a shallow lagoonal setting.^[29] South American records include the Late Campanian to Early Maastrichtian Sulcusuchus erraini from Patagonian deposits in Argentina, associated with nearshore marine paleoenvironments.^[6] In Africa, the Middle Turonian Goulmima Formation in Morocco's Er-Rachidia Province has yielded Thililua longicollis and Manemergus anguirostris, from tropical, open marine conditions.^[6] Antarctic finds are limited but significant, with an indeterminate polycotylid skeleton from the upper Coniacian to lower Campanian Alpha Member of the Santa Marta Formation on James Ross Island, indicating presence in high-latitude, cool-temperate seas. European evidence consists of fragmentary material from the Albian of England, such as isolated elements from the Vectis Formation on the Isle of Wight, suggesting marginal occurrences in early shallow-shelf habitats.^[6] In Asia, a Turonian polycotylid is known from the Upper Cretaceous of Hokkaido, Japan, while possible Russian records include Campanian large-toothed forms from the European part of the country, both from epicontinental marine settings. Australasian localities feature an Upper Albian polycotylid (Richmond pliosaur) from southeastern Australia, all in warm, coastal environments; no freshwater deposits are associated with the family.^[6] Overall, the distribution exhibits an initial Laurasian bias in the Early Cretaceous, shifting toward Gondwanan regions later, consistent with global marine connectivity.^[6]