Dinosaurs, plesiosaurs, mosasaurs and more (2023)

By R Ewan Fordyce

The text below is modified slightly from an original review which appeared as:
Fordyce, R. E. 2006. New light on New Zealand Mesozoic reptiles.
Geological Society of New Zealand newsletter 140: 6-15.
Thanks to the President and Editor of the Geological Society for permission to post this review. You can get a pdf of the article.

Jeff Stilwell and coauthors recently (early 2006) published the first report of dinosaur bones from Chatham Island. The fossils include convincing material, and the occurrence promises more finds. Questions remain, however, about the stratigraphic setting. This commentary summarises the recent finds, considers earlier reports of New Zealand Mesozoic vertebrates, and reviews some broader issues of Mesozoic reptile paleobiology relevant to New Zealand.

The Chatham Island finds

A diverse team reports on the Chathams finds. Jeff Stilwell (fig. 1 here) is an invertebrate paleontologist with research interests on Gondwana breakup and Southern Hemisphere Cretaceous-early Cenozoic molluscs (e.g. Stilwell & Zinsmeister 1992), including Chatham Islands (1997). Several authors are vertebrate paleontologists – Chris Consoli, Tom Rich, Pat Vickers-Rich, Steven Salisbury, and Phil Currie – with diverse experience of dinosaurs. Rupert Sutherland and Graeme Wilson (GNS) are well-known for their research on tectonics and biostratigraphy.

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Dinosaurs, plesiosaurs, mosasaurs and more (1)
Fig 1 Jeff Stilwell in the field, Seymour Island,Antarctica photo E Fordyce

The Chathams article describes a range of isolated bones attributed to theropod (“beast-footed,” carnivorous) dinosaurs, including a centrum (main part or body of a vertebra), a pedal phalanx (toe bone), the proximal head of a tibia (lower leg bone, at the knee joint), a manual phalanx (finger bone) and a manual ungual (terminal “claw” of a finger). On names of groups, fig. 2 here gives a simple guide to dinosaur classification. Specimens are catalogued in the GNS collections. Those outside the field of vertebrate paleontology might be sceptical that isolated and sometimes incomplete bones can be identified as to position (e.g. vertebra, limb) or to species. However, this approach has been thoroughly tested since Georges Cuvier proposed the idea of “correlation of parts” – that, because organisms can be viewed as integrated whole entities, a species may be identified from only a fragment of a skeleton. In vertebrate paleontology, as in human forensic pathology, the identification of single bones is based on knowledge of more-complete specimens. There is a wealth of supporting information in the global literature (e.g. Weishampel et al. 2004, Farlow & Brett-Surmann 1997), and the technique is widely and successfully used. Of the Chathams bones, the phalanges are compellingly dinosaurian, although it is also possible that the ungual phalanx is from the foot of a large bird. The vertebral centrum does not seem to represent a marine reptile (plesiosaur, mosasaur). For this incomplete element, the authors state that position in the vertebral column and orientation are uncertain, but their conclusion that it was from a medium-sized theropod about 4 m long and 3 m high suggests far more confidence. The fragment of tibia (reportedly proximal, and thus figured upside down) cannot reasonably belong to other than dinosaur.

Dinosaurs, plesiosaurs, mosasaurs and more (2)
Fig 2 Simple cladogram of dinosaur relationships, based on Brochu 2001). Symbols indicate groups reported from the New Zealand Cretaceous

The stratigraphic setting is intriguing. The bones are from a coastal outcrop of Takatika Grit on the northern part of Chatham Island (see also Campbell et al. 1993: 60). This unit is a thin (~10 m) marine unit, with abundant phosphorite nodules, greensand and volcanogenic debris, resting unconformably on basement schist. Stilwell et al. (2006: fig. 2) divide the unit into 14 beds, of which 8 contain bone (although p 249 states 3 bone horizons). The article title will be taken widely to mean that the KT boundary is present in this sequence, will ensure wide citation, and will likely smooth the path to more research funding. Note, though, that the authors actually state: “The grit may represent, in part, an allochthonous accumulation of reworked uppermost Cretaceous sediments and fossils that were deposited post K–T boundary, in the Danian. However, the mixed latest Cretaceous–earliest Tertiary age of associated microfossils indicate that the K–T boundary may be present below the exposed bone-rich beds…” It’s interesting to read “may be present,” given the lack of a firm Haumurian (late Cretaceous) or older age for the grit. Later (p 248), it is stated that the Takatika Grit is significant for allowing reconstruction of paleoenvironment and biota from just before the KT boundary, hinting at a Cretaceous age after all. Readers would have been served better had ages been indicated directly on the stratigraphic column of Stilwell et al.: fig. 2. I await a more-conclusive statement on age.

For now, we can assume that Cretaceous terrestrial bones were reworked into Paleocene shallow marine sediments. Is that really possible? Yes; dinosaur bones and remains of other terrestrial organisms have been collected many times from shallow marine strata. Consider, for example, Late Cretaceous dinosaurs from shallow marine Tahora Formation of Mangahouanga Stream, Hawkes Bay (Molnar and Wiffen 1994), and Late Eocene terrestrial mammal bones from shallow marine La Meseta Formation of Seymour Island, Antarctica (Reguero et al. 2002).

(Video) Plesiosaurs 101 | National Geographic

As with many good stories, there is an earlier history. Campbell et al. (1993: 62-64) mentioned the presence of reptile bones, possibly dinosaurian (see their fig. 4.30), in the Takatika Grit, but didn’t offer a firm identification. Before that, in 1991, University of Canterbury Geosciences student Evan Meek reported bone associated with phosphorite horizons in the Grit, and collected several fragments of presumed plesiosaur bone now held in the Geology Museum at University of Otago.

Some points made by Stilwell et al. don’t stand close scrutiny. For example, it is implied twice in the introduction to the paper that the dinosaurs are from an oceanic island, and on p 249 the authors emphasise that the dinosaurs are from an isolated setting nearly 1000 km east of New Zealand. These statements miss the point. “Oceanic” is correct in the sense that Chatham Island is now distant from mainland New Zealand, but in the geological sense and especially in the paleobiogeographic sense it is misleading, and the authors should know better: Chatham Island is based on New Zealand continental crust, not oceanic crust. Some dinosaur afficionados likely to read Stilwell et al. without knowledge of New Zealand geology could be confused needlessly by such wording. Stilwell et al. (their fig. 4) indeed show Chatham Island as continuous with what is now South Island, as also indicated in Fig. 3 of this review (based in turn on reconstructions by King).

Mesozoic terrestrial reptiles

The article on the Chathams dinosaurs is one of many on Mesozoic, mainly Cretaceous, reptiles from New Zealand. Our record of marine reptiles is highly informative, yet the more fragmentary record of dinosaurs – perhaps a shoe-box full of bones in contrast to a shipping-container full of marine reptiles – arouses interest because of implications to ecology and paleogeography. Early geologists hinted inconclusively at the presence of terrestrial reptiles. For example, Haast (1870: 189) commented, about Cretaceous reptiles at Waipara, “There was also, what I consider to be, the distal or lower portion of the femur, which, judging from the articulation, evidently had some affinities with terrestrial remains, such as the Iguanodon a herbivorous terrestrial reptile, of enormous size, and living in the Northern Hemisphere, in the wealden and greensand (Cretaceous) period” [original spellings and capitals retained]. Later, an anonymous author, most likely Hector (in McKay 1877: 41), referred to the tooth of a "megalosauroid . . . land saurian", apparently also from Waipara. The identity of these specimens was not elaborated on and, by 1900, there was still no firm evidence of dinosaurs in New Zealand. In following decades, many people assumed that those reptiles had never actually been here, and the absence of evidence was taken as evidence of absence. Fleming (1962: 93), however, cautioned in generalising about the absence of fossil land vertebrates, particularly as some living forms, such as tuatara, must have had a long Tertiary record in spite of a lack of fossils.

As it happens, in 1958, Don Haw had already discovered reptile bones in Cretaceous shallow marine strata of Mangahouanga Stream, Hawkes Bay (Haw 2002), stimulating the now widely-recognised field programme of Joan and Pont Wiffen and associates including Crabtree, McKee, and Moisley. The first formal report of a New Zealand dinosaur was by Ralph Molnar (1981), who described an isolated vertebra recovered by the Wiffen group from Mangahouanga. The bone did not match any of the marine reptiles already known from New Zealand. Molnar, a Brisbane-based dinosaur paleontologist trained in USA, convincingly argued that the vertebra recovered by Wiffen was from the tail of a theropod dinosaur. Later finds, reviewed by Molnar and Wiffen (1994) and Wiffen (1996), include fragments of other dinosaurs: the partial rib from a sauropod (large quadrupedal plant-eating saurischian), the pelvis of a hypsilophodontid (an small bipedal ornithopod), a fragment of ankylosaur (armoured ornithopod), and the phalanx of a probable theropod (but possibly a large bird). Reptiles other than dinosaurs are known from Mangahouanga, including a protostegid marine turtle (Wiffen 1981), and a fragment of pterosaur (Wiffen and Molnar 1988). Beyond the primary literature, these discoveries are well-covered in popular books (e.g. Stace and Eagle 2001).

What of New Zealand localities other than Chatham Island and Mangahouanga Stream? The only other described putative dinosaur is an isolated manual phalanx (finger bone) from the Huriwai Measures (Puraroan, Late Jurassic), south of the Waikato River mouth. This single small bone was identified as probable theropod (Molnar et al. 1998); it represents the first tetrapod vertebrate described from the New Zealand Jurassic.

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There are hints of other tetrapod fossils from our Mesozoic, although these are not necessarily dinosaurian and some may actually represent marine groups. Fleming et al. (1971) mentioned the "teeth having Labyrinthodont characters" earlier reported by Hector (1880, 1886) and Worley (1894) from unspecified formations (probably Triassic) at Nugget Point, South Otago, and Wairoa district, Nelson. These could represent ichthyosaurs or, alternatively, an amphibian. Fordyce et al. (2003) recently reported a bone fragment from a large “labyrinthodont” amphibian (strictly, a sterospondyl) from the basal Triassic south of Mataura.

Mesozoic marine reptiles

The New Zealand record of marine reptiles, particularly Piripauan-Haumurian (Late Cretaceous), is significant at a global level, thanks to some rather complete and informative specimens. The key groups are plesiosaurs and mosasaurs, while the main localities are Mangahouanga Stream, Haumuri Bluff-Conway, Waipara, and Shag Point. For a historical overview, and details of some of the important species, one starts with the monograph of Welles & Gregg (1971). That document arose from Welles’ visit to New Zealand in the late 1960s (Gregg 1997) to start a new phase of study on Cretaceous reptiles after a break of about 70 years since the days of Hutton. Welles and Gregg reviewed the early contributions of Owen, Haast, Hector (especially 1874), and Hutton, and the productive field work of the indefatigable Alexander McKay. The monograph also gave details of unpublished early research, and discussed the tragic loss of fossils collected by McKay and sent overseas for study. A notable contribution of Welles and Gregg was to name and describe a new species of mosasaur (sea-lizard), Prognathodon waiparaensis, based on a partial skull recovered from just below the KT boundary in the Waipara River section at Laidmore-Claremont. The taxonomy in the Welles and Gregg monograph is specialised, and when I read the article as a graduate student seeking an introduction to reptile anatomy and classification, I found it not very helpful; other sources, such as books by A.S. Romer, were more rewarding. (For more recent works, see Callaway & Nicolls 1997, and many articles in Journal of Vertebrate Paleontology.)

Much research on marine reptiles has been reported since 1971, and only a brief summary is given here. Material from Mangahouanga Stream (Wiffen and Moisley 1986) includes the new plesiosaur Tuarangisaurus and more material attributed to Mauisaurus, plus mosasaurs (Wiffen 1981a, 1990) including a Prognathodon and 3 new species: Moanasaurus mangahouangae, Rikisaurus tehoensis, and Mosasaurus flemingi. It would be surprising to find a diversity of closely related species (in this case, mosasaurs) of similar size in one assemblage, and whether all the latter mosasaurs are distinct is moot.

To consider fossils from northern South Island, Caldwell et al. (2005) reported new material of the mosasaur Taniwhasaurus oweni (including T. haumuriensis of previous authors) from Haumuri Bluff. Norton Hiller and Al Mannering at Canterbury Museum have made notable advances. Hiller et al. (2005) described rather complete and highly informative new material of the plesiosaur Mauisaurus haasti from Ngaroma, Conway River, clarifying the concept of a species named by James Hector, and confirming M. haasti as an elasmosaur (extreme long-necked plesiosaur). Because Tuarangisaurus keyesi and Mauisaurus haasti are not known from comparable material (the first is based on a skull, the latter on postcranial skeleton), it is not clear whether the 2 species are truly distinct. A possible third elasmosaur species may be represented by an indeterminate fragmentary elasmosaur (Hiller & Mannering 2004) from the classical locality of Claremont-Laidmore at Waipara. Yet more material is known from Waipara: most recently, Hiller & Mannering (2005) described a cluster of postcranial remains from a large concretion, apparently representing another elasmosaur distinct from Mauisaurus haasti. The species was not named because it lacks a skull – probably the single most important element on which to base a new species. The most-recently recovered Waipara reptile is a mosasaur, apparently a new Prognathodon, which includes the skull and jaws. The fossil is under preparation (see www.otago.ac.nz/geology/features/paleontology/).

From the south, the large plesiosaur Kaiwhekea katiki (Shag Point) was described by Cruickshank & Fordyce (2002) as a new genus in the mainly Jurassic family Cryptoclididae - a group in which the neck is significantly shorter than in elasmosaurs. Kaiwhekea is notable as (currently) being the only New Zealand Mesozoic reptile represented by an articulated and nearly complete skeleton, albeit with many bones represented by natural moulds. Kaiwhekea was compared with 2 other Gondwanan plesiosaurs, Aristonectes and Morturneria, also thought to be cryptoclidids. Later, Gasparini et al. (2003) showed that Aristonectes is probably a specialised elasmosaur. Where does Kaiwhekea belong? It is not an elasmosaur in the usual sense of the term. O’Keefe (2004) used cladistic analysis to show that Kaiwhekea might not belong in the Cryptoclididae, but rather in the specialised cryptocleidoid family Cimoliasauridae. It is trite but true to say that more research is needed.

(Video) Jurassic World - All Mosasaurus Scenes

Dinosaurs, plesiosaurs, mosasaurs and more (3)
Figure 3. New Zealand Cretaceous reptile localities and paleogeography, based on Cruickshank and Fordyce (2002) with map simplified from King (1998).

Beyond mosasaurs and plesiosaurs, a third marine reptile group is known from the New Zealand Mesozoic, the dolphin-like Ichthyosauria. Fleming et al. (1971) reviewed the specimens, most of which were reported first in the 19th century. Probably the most tantalising fossil known by 1971 was the Late Triassic partial rostrum reported by Campbell (1965) from the Murihiku Supergroup. More Murihiku specimens have been found since, but they are too incomplete to identify (Fordyce 2003). Sachs & Grant-Mackie (2003) recently reported a fragment of snout of a presumed Cretaceous (and thus geologically young) ichthyosaur from Northland, giving hope of finding other more-complete material.

Mesozoic New Zealand – isolated in a high latitude setting

For the Jurassic and much of the Cretaceous, New Zealand was probably within or close to the polar circle (e.g. Lawver et al. 1992, Pole 1999, McLoughlin 2001, Schellart et al. 2006), implying significant seasonal variation in light and climate, and thus in biological productivity (plant growth). Further, by about 85 Ma (Piripauan; Cooper 2004), the Tasman Sea was opening, and the New Zealand landmass was presumably physically isolated from other parts of Gondwana. There are implications for dinosaur (and marine reptile) biology, as noted by Molnar and Wiffen (1994) for New Zealand, and by Rich et al. (2002) for southern Australia. In summary, in a high latitude setting, dinosaurs on an “island continent” would have had limited ability to migrate during winter cold and darkness. Marine reptiles would likely be affected by fluctuations in food caused by great seasonal variation in productivity. How many dinosaurs lived on Late Cretaceous New Zealand after separation from the Gondwana margin? Molnar (1981) noted that a small landmass would support only a small population of any one dinosaur species, and citing small population numbers that might barely be self-sustaining. His discussion, however, did not consider that home ranges of many organisms are not exclusive but may overlap; there may have been more dinosaurs on New Zealand than suggested by Molnar. It is intriguing also that some reptiles may represent late occurrences of groups otherwise reported earlier in the Northern Hemisphere fossils. Consider, for example, the Late Cretaceous plesiosaur Kaiwhekea, which apparently represents an otherwise mainly Jurassic lineage known from Europe, or the Early Cretaceous report of an Allosaurus-like dinosaur, presumably close to Jurassic forms from North America. Another “out of time” record is that of a supposed ceratopsian dinosaur from Victoria, which is older than the start of the great ceratopsian radiation of the northern Hemisphere. (Ceratopsians were “horned” herbivores, such as Triceratops.) Admittedly, those specimens known from nearly complete skeletons (Kaiwhekea) are more convincing than those based on single bones (the Australian Allosaurus and ceratopsian). Some of these issues were discussed further by Long (1998) and Rich and Rich (2000).


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The author - R.Ewan Fordyce, Associate Professor at Otago University with the jaw of a fossil mosasaur from the Waipara River area


How are plesiosaurs related to dinosaurs? ›

Marine reptiles, such as ichthyosaurs, plesiosaurs and mosasaurs are not dinosaurs. Nor is Dimetrodon or other reptiles in the same group (previously called 'mammal-like reptiles' and now called synapsids). None of these other extinct groups shared the characteristic upright stance of dinosaurs.

Why are mosasaurs dinosaurs? ›

Mosasaurs, meanwhile, were actually giant lizards, close relatives of the monitor lizards of today, including Komodo Dragons. A good basic rule is: If it flew in the air (and didn't have feathers) or lived entirely in the sea, it's not a dinosaur.

What killed mosasaurs? ›

What happened to Mosasaurs? The mosasaurs disappeared from the fossil record alongside non-avian dinosaurs 65.5 million years ago, after a giant asteroid crashed into Earth at the end of the Cretaceous period.

Is a plesiosaur a mosasaur? ›

Many of the so-called 'dinosaur' remains found on New Zealand are actually mosasaurs and plesiosaurs, both being Mesozoic predatory marine reptiles.

What killed the plesiosaurs? ›

During the Late Cretaceous, the elasmosaurids still had many species. All plesiosaurs became extinct as a result of the K-T event at the end of the Cretaceous period, approximately 66 million years ago.

What did a plesiosaur eat? ›

All plesiosaurs – so far as we know – were predators, the shapes of their teeth and jaws indicating that they preyed variously on swimming and benthic invertebrates, on fish, and also on other aquatic reptiles.

Is Mosasaurus real or fake? ›

mosasaur, (family Mosasauridae), extinct group of aquatic lizards that attained a high degree of adaptation to the marine environment and were distributed worldwide during the Cretaceous Period (145.5 million to 66 million years ago).

Is Mosasaurus the biggest dinosaur? ›

Even at 40 meters long, this would make the Jurassic World Mosasaurus by far the largest animal to have ever lived.

What eats a Mosasaurus? ›

Mosasaurs would have been prey, as well. They were eaten by sharks, a detail established with the discovery of shark teeth fixed into mosasaur bone. A fossil Mosasaur tooth from Morocco. Like a snake, the jaws of a mosasaur were double-hinged.

Who would win Mosasaurus or Megalodon? ›

While a similar length, the Megalodon had a much more robust body and huge jaws built for devouring whales and other large marine mammals. A Mosasaurus would not have been able to get its jaws around the much thicker body of the Megalodon. It would just take one catastrophic bite for the Megalodon to end the battle.

Is the Indominus Rex a girl? ›

If you've seen Jurassic World, you know that the fearsome antagonist, a hybrid beast called Indominus Rex, is female. All the dinosaurs are female, we're told in the Jurassic Park series of movies, to prevent breeding.

Did anything eat the Mosasaurus? ›

There's not much that could have preyed upon this gigantic creature, but bite marks and mangled paddles of fossil mosasaurs suggest that mosasaurs often fought (and ate) each other. Young mosasaurs also had to avoid predators like sharks and giant predatory fish.

Is a mosasaur a Mosasaurus? ›

Mosasaurus (/ˌmoʊzəˈsɔːrəs/; "lizard of the Meuse River") is the type genus (defining example) of the mosasaurs, an extinct group of aquatic squamate reptiles. It lived from about 82 to 66 million years ago during the Campanian and Maastrichtian stages of the Late Cretaceous.

How fast can a plesiosaur swim? ›

“Studies have shown an optimal swimming speed for plesiosaurs of about 0.4 m/s (1.44 km/h) to a maximum sustained speed of about 2.5 m/s (9 km/h) (like today's dolphins), depending on joint movement of the limbs and specific species.

What is the plesiosaur known for? ›

It is known by nearly complete skeletons from the Lias of England. It is distinguishable by its small head, long and slender neck, broad turtle-like body, a short tail, and two pairs of large, elongated paddles. It lends its name to the order Plesiosauria, of which it is an early, but fairly typical member.

How did plesiosaurs born? ›

Other extinct marine reptiles, such as ichthyosaurs, mosasaurs and choristoderans, were known to give birth to live young, a strategy called viviparity. This is the first evidence that plesiosaurs did the same, rather than hatching their offspring from eggs on land.

How long were plesiosaurs alive for? ›

plesiosaur, (clade Plesiosauria), any of a group of long-necked marine reptiles found as fossils from the late Triassic Period into the late Cretaceous Period (215 million to 66 million years ago).

Can plesiosaurs survive today? ›

There has been no evidence to prove the existence of surviving plesiosaurs has ever been found or provided. Adam S. Smith, a plesiosaur palaeontologist and curator of Natural Sciences at Nottingham Natural History Museum, concluded that "Unfortunately, living- plesiosaurs almost certainly do not exist today".

How big is a plesiosaur? ›

How did plesiosaurs swim? ›

Plesiosaurs were paraxial swimmers – they used their limbs to swim. In this regard they are like turtles and penguins, but different to fish, whales, mosasaurs, and ichthyosaurs, which are paraxial swimmers – they undulate their body and tail for propulsion.

What hunted plesiosaurs? ›

Antarctica was once home to a 10-metre long sea monster that hunted the reptilian equivalent of whales at the end of the dinosaur age, scientists have discovered.

Is Mosasaurus a girl or boy? ›

In Jurassic World, while not explicitly stated, it seems to hold true, given that all the mentioned "character" dinosaurs — the raptor pack, the Indominous, the Rex, the mosasaurus — are referred to as female.

What is the biggest dinosaur in water? ›

Shonisaurus sikanniensis is believed to be the largest sea dinosaur at 85 ft. The largest sea animal to exist during the age of the dinosaurs was an incredible 85 feet long and is believed to be Shonisaurus sikanniensis.

Is Mosasaurus bigger than Megalodon? ›

So It was around 14.2-15.3 meters long, and possibly weighing 30 tons. Mosasaurus was longer than Megalodon so yeah.

What is the 2nd biggest dinosaur? ›


Who is bigger T Rex or Mosasaurus? ›

Either way, this was a big animal and an apex predator in its habitat. Prognathodon has been estimated to reach lengths in excess of 33 feet, and the biggest Mosasaurus species got to be even larger—around 59 feet, or nearly 20 feet longer than the biggest T. rex.

What dinosaur can defeat Mosasaurus? ›

Fight with Spinosaurus

However, Spinosaurus uses the icicles above to kill Mosasaurus and was successful, thus killing Mosasaurus.

What did T Rex eat? ›

T. rex was a huge carnivore and primarily ate herbivorous dinosaurs, including Edmontosaurus and Triceratops. The predator acquired its food through scavenging and hunting, grew incredibly fast and ate hundreds of pounds at a time, said University of Kansas paleontologist David Burnham.

What ate Indominus Rex? ›

The Indominus rex left a legacy on the campers, they found the remains of the battle of main street realizing the Tyrannosaurus fought the Indominus and that the Mosasaurus had recently eaten it.

How smart is a Mosasaurus? ›

Base Stats. Mosasaurus has the maximum power available which gave it an extreme edge in the old meta. It has average intelligence but at the time not many animals had worked too much into the stats and at the time, it was actually pretty high which is great considering how op this build was.

Is megalodon bigger than Godzilla? ›

Legendary Godzilla was 108.20 meters tall, Shin Godzilla was 118.5 meters, and the new anime Godzilla is 300 meters tall! Estimates for the Megalodon's maximum size fall into the 18.288- 21.336 meter range. Therefore, Godzilla is bigger.

Who is stronger Mosasaurus or blue whale? ›

That's why, with everything in mind, the blue whale would win in a fight against the Mosasaurus. However, it would be a difficult battle, given the Mosasaurus' speed, agility, and high intelligence.

Who would win in a fight T rex or Spinosaurus? ›

Yet, the T-Rex had a massive neck that the Spinosaurus wasn't going to break with its bite power. The T-Rex could thrash free and clamp down on the Spinosaurus. With all that power and the 12-inch teeth, the most likely outcome is that the T-Rex kills Spinosaurus.

Is Rexy a hero? ›

In Jurassic Park, Rexy was showcased as more of an anti-hero. She never protected the survivors on purpose but saw a threat in the raptors that needed to be eliminated instead.

Is Blue friendly? ›

Blue force tracking is a United States military term for a GPS-enabled capability that provides military commanders and forces with location information about friendly (and despite its name, also hostile) military forces. In NATO military symbology, blue typically denotes friendly forces.

Who killed Indominus? ›

The Indominus Rex is killed while fighting the T-Rex and Blue the raptor. She is backed up during the battle the edge of the park's lagoon and is snatched and dragged in by the jaws of the Mosasaurus and was devoured off-screen.

How big is a Mosasaurus tooth? ›

Most of the fossils from the Mosasaurus were found in Europe and North America. The powerful carnivores that reached lengths of up to 56 feet roamed the oceans near the surface where they would hunt their prey of ammonites, birds, fish and turtles. Mosasaurus Tooth will measure between 25mm and up to 30mm in length.

Is Mosasaurus a monster? ›

It swam through Cretaceous seas 80 million years ago. About 80 million years ago, when dinosaurs walked the Earth, an 18-foot-long (5 meters) sea monster called a mosasaur cruised the ancient ocean that once covered western Kansas, snagging prey with its slender, tooth-lined snout.

How did Mosasaurus escape? ›

The Mosasaurus then ate the sub, along with a mercenary trying to escape on a helicopter, and when the gates were left open, it escaped the lagoon and swam into the ocean.

Is a sarcosuchus a dinosaur? ›

Sarcosuchus was a giant crocodilian and was a close relative to Deinosuchus . It was much larger than a modern crocodile, ranging around 8 tons. The fossils have been found around in Africa & lived during the Early Cretaceous era.

What did plesiosaurs evolve from? ›

Plesiosaurs were a group of marine reptiles that evolved from land-living reptiles in the Triassic period about 210 million years ago. They too, like ichthyosaurs had four flippers, a remnant of their terrestrial ancestors.

How closely related are crocodiles to dinosaurs? ›

Well, crocodiles share a heritage with dinosaurs as part of a group known as archosaurs (“ruling reptiles”), who date back to the Early Triassic period (250 million years ago). The earliest crocodilian, meanwhile, evolved around 95 million years ago, in the Late Cretaceous period.

What is the closest living relative to a plesiosaur? ›

Latest studies suggested that plesiosaurs' closest living relatives are turtles, and clump them together as Pantestudines—a sister group of Archosauria.

What made dinosaurs so big? ›

They had hollow bones, didn't chew their food, they had incredibly long necks, and likely possessed huge stomachs. These traits are theorized to be key in how they attained their enormous size.

Do crocodiles eat dinosaurs? ›

In August 2020, researchers discovered the fossils of "terror crocodiles" that could take down large dinosaurs with teeth "the size of bananas." "It is likely dinosaurs constituted an important resource in the Cretaceous ecological food web," White said.

What is the name of a dinosaur? ›

List of dinosaur names
Dinosaur NamesMeaning of Name
TriceratopsThree horned Face
TroodonWounded tooth
TyrannosaurusTyrant lizard
74 more rows

How did the plesiosaur protect itself? ›

Its primary form of defense was probably its very large size. The plesiosaur probably didn't have to defend itself often, but it may have used its strong jaws to attack other large predators.

How long were plesiosaurs alive for? ›

plesiosaur, (clade Plesiosauria), any of a group of long-necked marine reptiles found as fossils from the late Triassic Period into the late Cretaceous Period (215 million to 66 million years ago).

What hunted plesiosaurs? ›

Antarctica was once home to a 10-metre long sea monster that hunted the reptilian equivalent of whales at the end of the dinosaur age, scientists have discovered.

What was on Earth before dinosaurs? ›

At the time all Earth's land made up a single continent, Pangea. The age immediately prior to the dinosaurs was called the Permian. Although there were amphibious reptiles, early versions of the dinosaurs, the dominant life form was the trilobite, visually somewhere between a wood louse and an armadillo.

Why did sharks survive when dinosaurs didn t? ›

Having a skeleton made of lightweight cartilage allows sharks to conserve energy and swim long distances. Because shark skeletons are made of soft cartilage, which doesn't fossilize well, most of what scientists know about ancient sharks comes from teeth, scales and fin spine fossils.

What came before the dinosaurs? ›

The Permian is a geological record that began nearly 300 million years ago, almost 50 million years before the Age of the Dinosaurs. During the Permian the first large herbivores and carnivores became widespread on land. The Permian ended with the largest mass extinction in the history of the Earth.

What is unique about the plesiosaur? ›

Swimming with wing-like paddles, flippers or fins is not, in itself, especially remarkable: among modern animals, there are otariids (sea lions and fur seals), sea turtles, penguins and assorted fish that fly with enlarged pectoral fins. But what makes plesiosaurs remarkable is that they had two pairs of such flippers.

Can a plesiosaur walk on land? ›

"Scientists have long known that the bodies of plesiosaurs were not well suited to climbing onto land and laying eggs in a nest [like dinosaurs]. So the lack of evidence of live birth in plesiosaurs has been puzzling," O'Keefe, a plesiosaur expert at West Virginia's Marshall University, said in a statement.

Did plesiosaurs lay eggs? ›

Plesiosaurs were reptiles, which as a group tend to lay eggs rather than giving birth.


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