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Elasmosaurus platyurus
Cretaceous Piscivore

Elasmosaurus

Elasmosaurus platyurus

"Thin-plate flat-tailed reptile"

Period
Cretaceous · Campaniano
Lived
80.5–77 Ma
Length
up to 14 m
Estimated weight
2.2 t
Country of origin
United States
Described in
1868 by Edward Drinker Cope

Elasmosaurus platyurus was one of the largest and most distinctive plesiosaurs of the Late Cretaceous, famous for its extraordinarily long neck that accounted for more than half of its total length of approximately 14 meters. With 71 cervical vertebrae, it holds the record for the greatest number of neck vertebrae of any known vertebrate. It was not a dinosaur but a marine reptile of the group Sauropterygia. It lived in the Western Interior Seaway that covered central North America, feeding on fish and cephalopods with sharp teeth. It became famous for a historic error: when Edward Drinker Cope described it in 1868, he assembled the skeleton with the skull at the wrong end, placing it at the tip of the tail. The mistake was corrected in 1870 following the intervention of Joseph Leidy.

The Elasmosaurus platyurus holotype was collected from the Sharon Springs Member of the Pierre Shale Formation, in the lower Campanian (~80 Ma) of Logan County, Kansas. The Pierre Shale Formation is a sequence of marine shales deposited at the bottom of the Western Interior Seaway, rich in marine reptile fossils (mosasaurs, plesiosaurs), fish, ammonites, and invertebrates. The Smoky Hill Chalk, an equivalent formation to the west, preserved similar fauna including Styxosaurus, Tylosaurus, Platecarpus, and Pteranodon.

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Habitat

Elasmosaurus platyurus inhabited the Western Interior Seaway, a shallow epicontinental sea (50-150 m) that crossed North America during the Campanian. The waters were warm and productive, with high diversity of fish, cephalopods, and other marine reptiles. The environment was similar to a modern tropical sea, with normal salinity and surface temperatures above 25°C. The Pierre Shale formation, where the holotype was found, represents open-sea deposits far from the coast.

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Feeding

Elasmosaurus was piscivorous, feeding predominantly on teleost fish, squid, and other cephalopods available in the Western Interior Seaway. The sharp, pointed teeth were ideal for capturing slippery prey. The long neck was not used to strike like a snake, but probably to stealthily approach schools of fish from below or to sweep the water searching for prey. Gastroliths found in close relatives indicate the species swallowed polished stones, possibly as ballast or for grinding.

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Behavior and senses

Behavioral evidence for Elasmosaurus is scarce, but data from close relatives and biomechanical analyses provide some inferences. The neck rigidity suggests flipper-based swimming, not body undulation. Gastroliths indicate intentional rock-swallowing behavior. There is no evidence of gregarious behavior or parental care. Body shape suggests an efficient open-sea swimmer, probably covering large distances in search of fish schools.

Physiology and growth

Elasmosaurus was a warm-blooded (endothermic or mesothermic) reptile, as suggested by oxygen isotope analyses in plesiosaurs from the same group and by the need to sustain large muscle masses in four flippers. Growth was determinate, with animals reaching sexual maturity possibly between 10 and 15 years and final lengths of up to 14 meters. Bone histology from close relatives indicates rapid growth rates in the juvenile phase, slowing at maturity.

Continental configuration

Mapa paleogeográfico do Cretáceous (~90 Ma)

Ron Blakey · CC BY 3.0 · Cretáceous, ~90 Ma

During the Campaniano (~80.5–77 Ma), Elasmosaurus platyurus inhabited Laramidia, the western half of present-day North America, separated from the east by the Western Interior Seaway, a shallow sea dividing the continent. The continents were in very different positions: India was drifting toward Asia, Antarctica was still connected to Australia, and South America was an isolated island.

Estimated completeness 55%

The holotype ANSP 10081, collected in 1867 by Theophilus H. Turner in Kansas, is the only specimen definitively attributed to E. platyurus. It preserves a nearly complete vertebral column with 72 cervical vertebrae, dorsal, sacral, and caudal vertebrae, as well as cranial fragments, ribs, and elements of the pectoral and pelvic girdles. The flippers and most of the skull are missing. The 55% completeness reflects the excellent state of the vertebral column but the absence of complete appendicular elements.

Found (8)
Inferred (8)
Esqueleto de dinossauro — other
Slate Weasel, domínio público CC0 / domínio público

Found elements

skulllower_jawvertebraeribspelvisscapulahumerusfemur

Inferred elements

radiusulnahandtibiafibulafootsoft_tissueskin_coloration

15 papers in chronological order — from the original description to recent research.

1868

Remarks on a new enaliosaurian, Elasmosaurus platyurus

Cope, E.D. · Proceedings of the Academy of Natural Sciences of Philadelphia

Original description of Elasmosaurus platyurus by Edward Drinker Cope, based on the holotype collected in Kansas in 1867 by Theophilus H. Turner. Cope presented the animal as a new enaliosaurian from the Upper Cretaceous, attributing it a short neck and long tail because he reversed the orientation of the skeleton. The error would be pointed out two years later by Joseph Leidy, becoming one of the most famous episodes in American paleontology history and fueling the rivalry between Cope and Marsh in the Bone Wars.

Cope's corrected 1870 reconstruction showing Elasmosaurus platyurus with the skull at the correct (anterior) end, above the holotype ANSP 10081 elements. The original 1868 version had the skull inverted at the tail tip.

Cope's corrected 1870 reconstruction showing Elasmosaurus platyurus with the skull at the correct (anterior) end, above the holotype ANSP 10081 elements. The original 1868 version had the skull inverted at the tail tip.

Dorsal vertebrae of Elasmosaurus, illustrated by T. Sinclair in 1870. The dorsal vertebrae are significantly shorter than the cervicals, a feature that Cope initially confused when orienting the skeleton.

Dorsal vertebrae of Elasmosaurus, illustrated by T. Sinclair in 1870. The dorsal vertebrae are significantly shorter than the cervicals, a feature that Cope initially confused when orienting the skeleton.

1906

North American plesiosaurs: Elasmosaurus, Cimoliasaurus, and Polycotylus

Williston, S.W. · American Journal of Science

Comprehensive review by Samuel Wendell Williston on North American plesiosaurs, including Elasmosaurus, Cimoliasaurus, and Polycotylus. Williston reassesses the known material, clarifies taxonomic relationships between genera, and consolidates the basic anatomy of Elasmosaurus from the holotype. The work establishes Elasmosauridae as a distinct family and describes the diagnostic features separating elasmosaurids from other plesiosaur groups from the Cretaceous of North America.

Gastroliths (stomach stones) and bones of a plesiosaur from the Lower Cretaceous of Kansas, illustrated by Williston (1914). Elasmosaurus and relatives swallowed polished stones as ballast or to help digest prey.

Gastroliths (stomach stones) and bones of a plesiosaur from the Lower Cretaceous of Kansas, illustrated by Williston (1914). Elasmosaurus and relatives swallowed polished stones as ballast or to help digest prey.

Size comparison chart of the main members of Plesiosauroidea, including Elasmosaurus platyurus. The chart illustrates the extreme proportions of the neck relative to the body in elasmosaurids.

Size comparison chart of the main members of Plesiosauroidea, including Elasmosaurus platyurus. The chart illustrates the extreme proportions of the neck relative to the body in elasmosaurids.

1999

Revision of North American elasmosaurids (Reptilia, Plesiosauria) from the Cretaceous of the Western Interior

Carpenter, K. · Paludicola

Systematic revision by Ken Carpenter on North American elasmosaurids from the Cretaceous of the Western Interior. Carpenter concluded that only Elasmosaurus platyurus is a valid species within the genus, invalidating all other previously assigned species or transferring them to other genera. The work redefined the limits of the genus Elasmosaurus and established clear criteria for identifying the taxon, essential for all subsequent revisions of North American elasmosaurids.

Size diagram of Elasmosaurus platyurus compared with a human diver. Unknown regions were restored based on Albertonectes and Styxosaurus, close relatives studied by Carpenter (1999).

Size diagram of Elasmosaurus platyurus compared with a human diver. Unknown regions were restored based on Albertonectes and Styxosaurus, close relatives studied by Carpenter (1999).

Skull of the holotype (KUVP 1301) of Styxosaurus snowii, an elasmosaurid relative of Elasmosaurus from the Smoky Hill Chalk of Kansas. Carpenter (1999) redefined the relationships between these genera in his systematic revision.

Skull of the holotype (KUVP 1301) of Styxosaurus snowii, an elasmosaurid relative of Elasmosaurus from the Smoky Hill Chalk of Kansas. Carpenter (1999) redefined the relationships between these genera in his systematic revision.

2002

Terminonatator ponteixensis, a new elasmosaurid (Reptilia; Plesiosauria) from the Upper Cretaceous of Saskatchewan

Sato, T. · Journal of Vertebrate Paleontology

Sato describes Terminonatator ponteixensis, a new elasmosaurid from the Upper Cretaceous of Saskatchewan, Canada. The accompanying phylogenetic analysis places Terminonatator as sister taxon to Elasmosaurus within the subfamily Styxosaurinae. This work was fundamental in defining the phylogenetic relationships of Elasmosaurus within Elasmosauridae, demonstrating that extremely long-necked elasmosaurids form a coherent clade within the family.

Articulated neck and skull of the Styxosaurus snowii holotype (KUVP 1301), an elasmosaurid relative of Elasmosaurus and Terminonatator. Sato's (2002) analysis demonstrated that these three genera form an ultra-long-necked clade (Styxosaurinae).

Articulated neck and skull of the Styxosaurus snowii holotype (KUVP 1301), an elasmosaurid relative of Elasmosaurus and Terminonatator. Sato's (2002) analysis demonstrated that these three genera form an ultra-long-necked clade (Styxosaurinae).

Paleogeography of North America during the Campanian (~75 Ma). The Western Interior Seaway, where Elasmosaurus and Terminonatator lived, covered much of the continental center, with Kansas, Saskatchewan, and other states and provinces submerged.

Paleogeography of North America during the Campanian (~75 Ma). The Western Interior Seaway, where Elasmosaurus and Terminonatator lived, covered much of the continental center, with Kansas, Saskatchewan, and other states and provinces submerged.

2005

Redescription of Elasmosaurus platyurus Cope, 1868 (Plesiosauria: Elasmosauridae) from the Upper Cretaceous (Lower Campanian) of Kansas, U.S.A.

Sachs, S. · Paludicola

First comprehensive modern redescription of the holotype ANSP 10081 by Sven Sachs. The work defines E. platyurus by two unambiguous autapomorphies: presence of six premaxillary teeth and the high number of 71 cervical vertebrae. Sachs systematically documents all preserved material, corrects previous interpretations of vertebral morphology, and establishes the diagnostic characters distinguishing E. platyurus from all other elasmosaurids, becoming the standard anatomical reference for the species.

Artistic reconstruction of Elasmosaurus platyurus capturing a juvenile Tylosaurus, with Hesperornis in the background. Sachs's (2005) redescription confirmed that E. platyurus was the largest elasmosaurid in its environment, capable of attacking considerably sized prey.

Artistic reconstruction of Elasmosaurus platyurus capturing a juvenile Tylosaurus, with Hesperornis in the background. Sachs's (2005) redescription confirmed that E. platyurus was the largest elasmosaurid in its environment, capable of attacking considerably sized prey.

Life reconstruction of Elasmosaurus platyurus by Nobu Tamura, showing the animal with neck extended horizontally, a posture considered more plausible by modern biomechanics than S-shaped or swan-like poses.

Life reconstruction of Elasmosaurus platyurus by Nobu Tamura, showing the animal with neck extended horizontally, a posture considered more plausible by modern biomechanics than S-shaped or swan-like poses.

2013

Revised vertebral count in the 'longest-necked vertebrate' Elasmosaurus platyurus Cope 1868, and clarification of the cervical-dorsal transition in Plesiosauria

Sachs, S., Kear, B.P. & Everhart, M.J. · PLOS ONE

Sachs, Kear, and Everhart revisit the vertebral count of Elasmosaurus platyurus, correcting it to 72 cervical vertebrae rather than the previously accepted 71. The study clarifies the criteria for distinguishing cervical from dorsal vertebrae in plesiosaurs, based on morphological features of the ribs and zygapophyseal facets. Published as an open-access article in PLOS ONE, the work became the primary reference for elasmosaurid vertebral anatomy and confirmed E. platyurus as the vertebrate with the most known cervical vertebrae.

Diagram illustrating five hypotheses on neck flexibility in elasmosaurids using Elasmosaurus as a model: vertical S-curve (A), horizontal (B), downward curve (C), wide lateral curve (D), and serpentine undulation (E). Sachs et al. (2013) contributed to understanding vertebral limitations.

Diagram illustrating five hypotheses on neck flexibility in elasmosaurids using Elasmosaurus as a model: vertical S-curve (A), horizontal (B), downward curve (C), wide lateral curve (D), and serpentine undulation (E). Sachs et al. (2013) contributed to understanding vertebral limitations.

Scientific reconstruction of Elasmosaurus platyurus by Dmitry Bogdanov, showing the body proportions verified by Sachs et al.'s (2013) vertebral revision. With 72 confirmed cervical vertebrae, E. platyurus's neck made up more than 55% of total body length.

Scientific reconstruction of Elasmosaurus platyurus by Dmitry Bogdanov, showing the body proportions verified by Sachs et al.'s (2013) vertebral revision. With 72 confirmed cervical vertebrae, E. platyurus's neck made up more than 55% of total body length.

Figure 1. Cervical vertebra fragment from the ANSP collection.

Figure 1. Cervical vertebra fragment from the ANSP collection.

Figure 2. Craniad cervical vertebra of Elasmosaurus platyurus (ANSP 10081).

Figure 2. Craniad cervical vertebra of Elasmosaurus platyurus (ANSP 10081).

Figure 3. Pectoral series.

Figure 3. Pectoral series.

2016

Taxonomic reassessment of Hydralmosaurus as Styxosaurus: new insights on the elasmosaurid neck evolution throughout the Cretaceous

Otero, R.A. · PeerJ

Rodrigo Otero performs a taxonomic reassessment of Hydralmosaurus as Styxosaurus, with a detailed phylogenetic analysis placing Elasmosaurus as the closest relative of Albertonectes within Styxosaurinae. The work provides new data on neck evolution in elasmosaurids throughout the Cretaceous, demonstrating a trend of progressive increase in the number of cervical vertebrae. Otero's analysis became a reference point for Elasmosauridae phylogeny.

Size diagram of Elasmosaurus platyurus with Russian labels, compared with a human diver. Otero's (2016) analysis confirmed the extreme neck proportions of Elasmosaurus within Styxosaurinae: more than 55% of total body length.

Size diagram of Elasmosaurus platyurus with Russian labels, compared with a human diver. Otero's (2016) analysis confirmed the extreme neck proportions of Elasmosaurus within Styxosaurinae: more than 55% of total body length.

Life reconstruction of Elasmosaurus platyurus by Connor Ashbridge. Otero's (2016) phylogeny confirmed the position of Elasmosaurus as one of the most derived elasmosaurids, with a proportionally longer neck than its relatives Styxosaurus and Terminonatator.

Life reconstruction of Elasmosaurus platyurus by Connor Ashbridge. Otero's (2016) phylogeny confirmed the position of Elasmosaurus as one of the most derived elasmosaurids, with a proportionally longer neck than its relatives Styxosaurus and Terminonatator.

Figure 1: Macaque faces. (A) An example illustrating how fWHR was calculated from images (Barbary macaque). Bizygomatic width was measured as the horizontal distance between the left and right zygion (vertical lines); upper-face height as the vertical distance between the highest point of the eyelids and the highest point of the upper lip (horizontal lines). The fWHR was calculated as width divided by height. (B) A male rhesus macaque (dominance style 1). Photo by Lauren Brent (modified). (C) A

Figure 1: Macaque faces. (A) An example illustrating how fWHR was calculated from images (Barbary macaque). Bizygomatic width was measured as the horizontal distance between the left and right zygion (vertical lines); upper-face height as the vertical distance between the highest point of the eyelids and the highest point of the upper lip (horizontal lines). The fWHR was calculated as width divided by height. (B) A male rhesus macaque (dominance style 1). Photo by Lauren Brent (modified). (C) A

Figure 2: Relationship between female dominance style and fWHR (data averaged per species). Scatter plot and line of best fit for the relationship between dominance style ( y axis) and fWHR ( x axis) in female (A) and male (B); grade 1 defines despotic species and grade 4 tolerant species ( Thierry, 2000 ). Download full-size image DOI: 10.7717/peerj.1775/fig-2

Figure 2: Relationship between female dominance style and fWHR (data averaged per species). Scatter plot and line of best fit for the relationship between dominance style ( y axis) and fWHR ( x axis) in female (A) and male (B); grade 1 defines despotic species and grade 4 tolerant species ( Thierry, 2000 ). Download full-size image DOI: 10.7717/peerj.1775/fig-2

Figure 3: Relationship between female dominance style and fWHR (data points represent each image in the dataset). Scatter plot and line of best fit for the relationship between dominance style ( y axis) and fWHR ( x axis) in female (A) and male (B); grade 1 defines despotic species and grade 4 tolerant species ( Thierry, 2000 ). Download full-size image DOI: 10.7717/peerj.1775/fig-3

Figure 3: Relationship between female dominance style and fWHR (data points represent each image in the dataset). Scatter plot and line of best fit for the relationship between dominance style ( y axis) and fWHR ( x axis) in female (A) and male (B); grade 1 defines despotic species and grade 4 tolerant species ( Thierry, 2000 ). Download full-size image DOI: 10.7717/peerj.1775/fig-3

2017

A new elasmosaurid (Sauropterygia, Plesiosauria) from the Bearpaw Shale (Late Cretaceous, Maastrichtian) of Montana with information on the phylogenetics and ecology of latest Cretaceous elasmosaurids

Serratos, D.J., Druckenmiller, P.S. & Bhullar, B.A.S. · Journal of Vertebrate Paleontology

Serratos and colleagues describe a new elasmosaurid from the Maastrichtian of Montana, with a comprehensive phylogenetic analysis including Elasmosaurus platyurus. The study also incorporates stable isotope analysis to infer the ecology and feeding habits of latest Cretaceous elasmosaurids. The work provides valuable data on the ecological diversity and biogeography of North American elasmosaurids at the end of the Cretaceous.

Reconstruction of Elasmosaurus platyurus by Dmitry Bogdanov on transparent background, showing the general anatomy of the animal. Serratos et al.'s (2017) analysis expanded knowledge of late Cretaceous elasmosaurid ecology using stable isotopes.

Reconstruction of Elasmosaurus platyurus by Dmitry Bogdanov on transparent background, showing the general anatomy of the animal. Serratos et al.'s (2017) analysis expanded knowledge of late Cretaceous elasmosaurid ecology using stable isotopes.

Reconstruction of Albertonectes vanderveldei, a Canadian elasmosaurid and close relative of Elasmosaurus. Serratos et al. (2017) included Albertonectes in the phylogenetic analysis to contextualize Elasmosaurus's position within Styxosaurinae.

Reconstruction of Albertonectes vanderveldei, a Canadian elasmosaurid and close relative of Elasmosaurus. Serratos et al. (2017) included Albertonectes in the phylogenetic analysis to contextualize Elasmosaurus's position within Styxosaurinae.

1999

Gastroliths and diet in plesiosaurs

Wahl, W.R. · Tate Museum Publications

Wahl examines gastroliths (stomach stones) associated with plesiosaurs from the Sundance and Morrison formations, discussing their physiological and dietary function. The study is relevant for Elasmosaurus because members of the family were found with similar accumulations of polished stones, suggesting that these marine reptiles intentionally swallowed rocks as ballast for buoyancy control or as an aid in crushing hard-to-digest food.

Chalk and impure chalk from the Smoky Hill Chalk Member of the Niobrara Formation, Upper Cretaceous, Monument Rocks, Kansas. This is precisely the lithology of the environment where close relatives of Elasmosaurus like Styxosaurus lived.

Chalk and impure chalk from the Smoky Hill Chalk Member of the Niobrara Formation, Upper Cretaceous, Monument Rocks, Kansas. This is precisely the lithology of the environment where close relatives of Elasmosaurus like Styxosaurus lived.

Detail of the Smoky Hill Chalk Member at Monument Rocks, Kansas. Elasmosaurus was found in the chronological equivalent of this formation (Pierre Shale), demonstrating that these animals inhabited the shallow, productive waters of the Western Interior Seaway.

Detail of the Smoky Hill Chalk Member at Monument Rocks, Kansas. Elasmosaurus was found in the chronological equivalent of this formation (Pierre Shale), demonstrating that these animals inhabited the shallow, productive waters of the Western Interior Seaway.

2000

Gastroliths associated with plesiosaur remains in the Smoky Hill Chalk (Upper Cretaceous) of western Kansas

Everhart, M.J. · Transactions of the Kansas Academy of Science

Everhart documents gastroliths found in association with elasmosaurid plesiosaur remains in the Smoky Hill Chalk of Kansas. The study records the precise location, quantity, and type of rocks found, inferring ballast functions for buoyancy control or a role in digestion. The work is especially relevant for Elasmosaurus because the Smoky Hill Chalk is the lateral contemporaneous environment to the Pierre Shale where the E. platyurus holotype was found.

Chalk sample from the Smoky Hill Chalk Member, Niobrara Formation, Kansas. The chalk and limestone formations of this region exceptionally preserved plesiosaur, mosasaur, and fish fossils from the Western Interior Seaway.

Chalk sample from the Smoky Hill Chalk Member, Niobrara Formation, Kansas. The chalk and limestone formations of this region exceptionally preserved plesiosaur, mosasaur, and fish fossils from the Western Interior Seaway.

Current landscape of the Smoky Hills, Kansas, where the Upper Cretaceous rocks that preserved the fossils of Elasmosaurus and other marine reptiles of the Western Interior Seaway outcrop. Erosion continuously exposes new material.

Current landscape of the Smoky Hills, Kansas, where the Upper Cretaceous rocks that preserved the fossils of Elasmosaurus and other marine reptiles of the Western Interior Seaway outcrop. Erosion continuously exposes new material.

2001

A cladistic analysis and taxonomic revision of the Plesiosauria (Reptilia: Sauropterygia)

O'Keefe, F.R. · Acta Zoologica Fennica

Comprehensive cladistic analysis by Frank Robin O'Keefe establishing the major clades of plesiosaurs and revising their taxonomy. The work placed Elasmosaurus within Elasmosauridae and established the fundamental phylogenetic relationships of the order Plesiosauria. O'Keefe's analysis provided the taxonomic framework that would be refined by subsequent work by Sato, Otero, and others, becoming a mandatory reference in plesiosaur literature.

Historical reconstruction of Trinacromerum, a polycotylid from the Cretaceous that shared the Western Interior Seaway with Elasmosaurus. O'Keefe's (2001) analysis clarified the phylogenetic differences between polycotylids and elasmosaurids.

Historical reconstruction of Trinacromerum, a polycotylid from the Cretaceous that shared the Western Interior Seaway with Elasmosaurus. O'Keefe's (2001) analysis clarified the phylogenetic differences between polycotylids and elasmosaurids.

Skeleton of Trinacromerum osborni, a Cretaceous plesiosaur mounted at the University of Kansas. O'Keefe (2001) used comparative skeletons of polycotylids and elasmosaurids, including Kansas specimens, in his phylogenetic analysis.

Skeleton of Trinacromerum osborni, a Cretaceous plesiosaur mounted at the University of Kansas. O'Keefe (2001) used comparative skeletons of polycotylids and elasmosaurids, including Kansas specimens, in his phylogenetic analysis.

2021

Revision of Nectosaurus and Megacephalosaurus, polycotylid-grade (Reptilia, Plesiosauria) taxa from the Cretaceous of North America

Zverkov, N.G. & Jacobs, M.L. · Journal of Paleontology

Zverkov and Jacobs revise the polycotylids Nectosaurus and Megacephalosaurus from the Cretaceous of North America, with a new phylogenetic analysis including Elasmosauridae. The work brings comparative data on plesiosaur diversity in the Western Interior Seaway and reinforces understanding of the relationships between different plesiosaroid families that coexisted with Elasmosaurus in the same environment during the Campanian.

Skeleton of Trinacromerum osborni mounted at the University of Kansas museum, from Williston (1925). The Western Interior Seaway during the Campanian was inhabited by a diversity of plesiosaurs, including Elasmosaurus and polycotylids like Trinacromerum.

Skeleton of Trinacromerum osborni mounted at the University of Kansas museum, from Williston (1925). The Western Interior Seaway during the Campanian was inhabited by a diversity of plesiosaurs, including Elasmosaurus and polycotylids like Trinacromerum.

Map of the Western Interior Seaway during the Cretaceous (~95 Ma). In more recent times like the Campanian (~80 Ma), the sea was less extensive but still covered Kansas, where the Elasmosaurus holotype was found.

Map of the Western Interior Seaway during the Cretaceous (~95 Ma). In more recent times like the Campanian (~80 Ma), the sea was less extensive but still covered Kansas, where the Elasmosaurus holotype was found.

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2005

A stratigraphic and taxonomic review of plesiosaurs from the old 'Fort Benton Group' of central Kansas: a new assessment of old records

Schumacher, B.A. & Everhart, M.J. · Paludicola

Schumacher and Everhart stratigraphically and taxonomically review the plesiosaur records from the old Fort Benton Group of central Kansas, including material relevant to Elasmosaurus. The work updates the identifications of historical specimens collected in the 19th and early 20th centuries, contextualizing them within modern stratigraphic units. The revision is essential for understanding the temporal and geographic distribution of E. platyurus and its relatives in the Western Interior Seaway.

Monument Rocks, Kansas, Upper Cretaceous limestone formation. The exposed rocks in this landscape are contemporaneous with the Pierre Shale where Elasmosaurus was found and preserved a rich marine fauna from the Western Interior Seaway.

Monument Rocks, Kansas, Upper Cretaceous limestone formation. The exposed rocks in this landscape are contemporaneous with the Pierre Shale where Elasmosaurus was found and preserved a rich marine fauna from the Western Interior Seaway.

Panoramic view of Monument Rocks, Kansas. The central Kansas region has been one of the most productive sites for collecting Cretaceous marine reptile fossils in North America since the time of Cope and Marsh.

Panoramic view of Monument Rocks, Kansas. The central Kansas region has been one of the most productive sites for collecting Cretaceous marine reptile fossils in North America since the time of Cope and Marsh.

2014

Faunal turnover of marine tetrapods during the Jurassic-Cretaceous transition

Benson, R.B.J. & Druckenmiller, P.S. · Biological Reviews

Benson and Druckenmiller present a comprehensive phylogenetic analysis of marine tetrapods including a revised topology for Elasmosauridae. The study analyzes faunal turnover during the Jurassic-Cretaceous transition, demonstrating that Elasmosauridae emerged and diversified during this period. The work establishes the position of Elasmosaurus within a global plesiosaur phylogeny and contextualizes the group's evolution within the broader framework of Mesozoic marine reptile radiations.

Paleogeographic map of the Western Interior Seaway with ancient continents visible (~95 Ma). Benson and Druckenmiller (2014) analyzed how marine tetrapods, including elasmosaurids, colonized these epicontinental marine environments throughout the Cretaceous.

Paleogeographic map of the Western Interior Seaway with ancient continents visible (~95 Ma). Benson and Druckenmiller (2014) analyzed how marine tetrapods, including elasmosaurids, colonized these epicontinental marine environments throughout the Cretaceous.

Map of North America with the Western Interior Seaway during the Campanian (Upper Cretaceous, ~75 Ma). Elasmosaurus platyurus lived in this epicontinental sea during the lower Campanian, exactly in the region that is now Kansas.

Map of North America with the Western Interior Seaway during the Campanian (Upper Cretaceous, ~75 Ma). Elasmosaurus platyurus lived in this epicontinental sea during the lower Campanian, exactly in the region that is now Kansas.

2024

How elongated? The pattern of elongation of cervical centra of Elasmosaurus platyurus with comments on cervical elongation patterns among plesiosauromorphs

O'Gorman, J.P. · Diversity

O'Gorman performs a detailed quantitative analysis of the cervical vertebrae elongation pattern in Elasmosaurus platyurus, comparing it with other plesiosauromorphs. The study demonstrates a unique distribution pattern of elongation along the neck, with more elongated central vertebrae and a gradual decrease toward the skull and trunk. This is the most recent and comprehensive work on the vertebral anatomy of E. platyurus, providing precise morphometric data on the holotype ANSP 10081.

Skull and scale diagram of Styxosaurus browni, a close relative of Elasmosaurus. O'Gorman (2024) compared the vertebral elongation pattern of E. platyurus with Styxosaurus and other elasmosaurids to identify unique features of E. platyurus's neck.

Skull and scale diagram of Styxosaurus browni, a close relative of Elasmosaurus. O'Gorman (2024) compared the vertebral elongation pattern of E. platyurus with Styxosaurus and other elasmosaurids to identify unique features of E. platyurus's neck.

Skull (with partial cross section) and scale diagram of Styxosaurus snowii, an elasmosaurid from the Smoky Hill Chalk of Kansas. O'Gorman (2024) included Styxosaurus in his quantitative comparisons with Elasmosaurus platyurus.

Skull (with partial cross section) and scale diagram of Styxosaurus snowii, an elasmosaurid from the Smoky Hill Chalk of Kansas. O'Gorman (2024) included Styxosaurus in his quantitative comparisons with Elasmosaurus platyurus.

Holótipo ANSP 10081 — Academy of Natural Sciences of Drexel University, Filadélfia, Estados Unidos

Slate Weasel, domínio público

Holótipo ANSP 10081

Academy of Natural Sciences of Drexel University, Filadélfia, Estados Unidos

Completeness: ~55% (coluna vertebral quase completa)
Found in: 1867
By: Theophilus H. Turner

The only specimen definitively attributed to E. platyurus. Collected near Fort Wallace, Logan County, Kansas, from Pierre Shale rocks (lower Campanian). Preserves 72 cervical vertebrae, part of the skull, ribs, and elements of the pectoral and pelvic girdles. It was the specimen used by Cope in his erroneous and later famous 1868 scheme.

KUVP 1301 (Styxosaurus snowii, parente próximo) — University of Kansas Natural History Museum, Lawrence, Estados Unidos

Neil Pezzoni (NGPezz), CC BY 4.0

KUVP 1301 (Styxosaurus snowii, parente próximo)

University of Kansas Natural History Museum, Lawrence, Estados Unidos

Completeness: ~80%
Found in: 1895
By: H.T. Martin

Although it is Styxosaurus snowii (not E. platyurus), this specimen is the most complete of an elasmosaurid from Elasmosaurus's sister genus, collected from the Smoky Hill Chalk of Kansas. It preserves the skull, nearly complete neck, and part of the body. Fundamental for understanding E. platyurus anatomy by comparison, since the Elasmosaurus holotype lacks a complete skull.

Elasmosaurus held a special place in cultural imagination long before modern cinema. Its long, sinuous neck became the visual basis for the Loch Ness monster and other aquatic monsters of 20th-century folklore. In film, it appeared as early as King Kong (1933) as a terrifying lake creature. The most notable production was Chased by Sea Monsters (BBC, 2003), a documentary narrated by Nigel Marven that dedicated an entire episode to the Campanian Western Interior Seaway, depicting Elasmosaurus with relative scientific accuracy for the time. Sea Monsters: A Prehistoric Adventure (2007) brought the species to IMAX in 3D, making it accessible to new audiences. In animation, Elsie in The Land Before Time V (1997) popularized elasmosaurids with young audiences. The long, sinuous neck of Elasmosaurus remains one of the most recognizable silhouettes in paleontology, frequently mistaken for a dinosaur by the general public, despite the animal belonging to a completely different group of marine reptiles.

Animatrônico do T-rex da franquia Jurassic Park com o Jeep característico da série

Full-size T-rex animatronic from the Jurassic Park franchise, with the iconic red Jeep — Amaury Laporte · CC BY 2.0

1933 🎞️ King Kong — Merian C. Cooper, Ernest B. Schoedsack Wikipedia →
1997 🎨 The Land Before Time V: The Mysterious Island — Charles Grosvenor Wikipedia →
2003 📹 Chased by Sea Monsters — Nigel Paterson Wikipedia →
2007 📹 Sea Monsters: A Prehistoric Adventure — Sean MacLeod Phillips Wikipedia →
2009 🎨 Dinosaur Train (série TV) — Craig Bartlett Wikipedia →
Sauropterygia
Plesiosauria
Plesiosauroidea
Elasmosauridae
Styxosaurinae
First fossil
1867
Discoverer
Theophilus H. Turner
Formal description
1868
Described by
Edward Drinker Cope
Formation
Pierre Shale (Sharon Springs Member)
Region
Kansas
Country
United States
Cope, E.D. (1868) — Proceedings of the Academy of Natural Sciences of Philadelphia

Fun fact

Edward Drinker Cope's 1868 mistake, placing Elasmosaurus's skull at the tip of the tail instead of the head, was so embarrassing that the paleontologist reportedly tried to buy and destroy all copies of the original paper to erase the record of the blunder.