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Spinosaurus

Genus of spinosaurid dinosaur

  • 38 min read
  • 6 chapters
Cast of FSAC-KK-11888, currently classified as Spinosaurus , displayed in a swimming posture at the Field Museum of Natural History in Chicago, Illinois. The skeleton reflects the known fossil materia
3blindMies · CC BY-SA 4.0

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Through World War II, Carnivore and Buoyancy

Spinosaurus is among the largest known terrestrial carnivores; other large carnivores comparable to Spinosaurus include theropods such as Tyrannosaurus, Giganotosaurus and the contemporary Carcharodontosaurus. A 2022 study suggests that S. aegyptiacus could have reached 14 m (46 ft) in length and 7.4 t (8.2 short tons) in body mass. The skull of Spinosaurus was long, low, and narrow, similar to that of a modern crocodilian, and bore straight conical teeth with few to no serrations. It would have had large, robust forelimbs bearing three-fingered hands, with an enlarged claw on the first digit. The distinctive neural spines of Spinosaurus, which were long extensions of the vertebrae, grew to at least 1.65 m (5.4 ft) long and were likely to have had skin connecting them, forming a sail-like structure. The hip bones of Spinosaurus were reduced, and the legs were very short in proportion to the body. Its long and narrow tail was deepened by tall, thin neural spines and elongated chevrons, forming a paddle-like structure.

Spinosaurus is known to have eaten both aquatic and terrestrial prey. Evidence suggests that it was semiaquatic, although the extent of its swimming capability has been strongly contested. Spinosaurus's leg bones had a high bone density, allowing for better buoyancy control. Multiple functions have been put forward for the dorsal sail, including thermoregulation and display; either to intimidate rivals or attract mates. It lived in a humid environment of tidal flats and mangrove forests alongside many other dinosaurs as well as fish, crocodylomorphs, squamates, turtles, pterosaurs, and plesiosaurs.

Discovery and naming

Initial finds

The first discovery of Spinosaurus may have been in October 1898, when French geologist Fernand Foureau unearthed two unusual teeth in Cenomanian-aged sediments of the Djoua Escarpment in what is now southern Algeria, then French Algeria. Foreau found the specimens while on the Foureau-Lamy Expedition of 1898-1900, which traveled across the Sahara from Algeria to Lake Chad. In 1905, French geologist Emile Haug described the fossils unearthed while on the expedition, including the two teeth which he assigned to the fish Saurocephalus. However, in 1915 German paleontologist and describer of Spinosaurus Ernst Stromer reassigned the teeth to Spinosaurus. Later studies have agreed with this assessment, however the teeth themselves has since been lost.

The first confidently referable remains of Spinosaurus were discovered in the autumn of 1912 by Austro-Hungarian paleontologist Richard Markgraf, a fossil collector who was financed by Stromer and the Bavarian Academy of Sciences, in deposits of the Bahariya Formation in the Bahariya Oasis of western Egypt. The sediments of the Bahariya Formation come from the Cenomanian stage of the Late Cretaceous period, one of many Cretaceous-aged formations of North Africa. In 1915, Stromer described these remains as belonging to a new genus and species of dinosaur, Spinosaurus aegyptiacus. The generic name Spinosaurus comes from the Latin spina, meaning "spine", and the Greek sauros, meaning "lizard", and thus "spine lizard". The specific name aegyptiacus derives from Egypt, where the fossils were unearthed. Spinosaurus aegyptiacus' type specimen (BSP 1912 VIII 19) consists of elements of the mandible (lower jaw), a maxilla (upper jaw) fragment, cervical (neck), caudal (tail), and dorsal (back) vertebrae, including much of the neural spines, ribs, teeth, and some gastralia (belly ribs).

In April 1914, another expedition to the Bahariya Oasis by Markgraf unearthed an incomplete skeleton (BSP 1922 X45) of a spinosaurid. This skeleton was poorly preserved and, as a result of illegal unpacking and insufficient repacking by Anglo-Egyptians during World War I, was greatly damaged. After much deliberation due to the war and poor Anglo-German relations, the skeleton arrived in Germany in 1922 where it was described by Stromer in 1934. Stromer assigned the skeleton to Spinosaurus, but considered it different enough from S. aegyptiacus that it would belong to its own Spinosaurus species, "Spinosaurus B".

In 1936, Stromer worked with Dr. Erhardt (the first name is unknown) to create a skeletal reconstruction of Spinosaurus based on fossils of the holotype, "Spinosaurus B", and related taxa. Although Stromer was hesistant about the lack of known remains, he and Erhardt produced a restoration that filled in missing elements of Spinosaurus' skeleton with the tyrannosaurid theropods Tyrannosaurus and Gorgosaurus. Unfortunately, during the night of April 24/25, 1944, the building of the Paläontologisches Museum München (Bavarian State Collection of Paleontology) of the Bavarian Academy of Sciences was severely damaged during the British Bombing of Munich. Due to personal and political tensions between Stromer and the museum's director Karl Beurlen, who was a fervent Nazi, the Spinosaurus fossils held there were not rehoused and subsequently destroyed as a result of the bombing. Stromer's finds, including Spinosaurus, received little academic or public attention. In 1995, Stromer's son donated his father's archives to the Paläontologische Staatssammlung München, leading to a 2006 study by American researcher Joshua Smith and colleagues of the photographs, two of which were of Spinosaurus' holotype. Based on these photographs of the mandible and the entire specimen as mounted, Smith concluded that Stromer's original 1915 drawings were slightly inaccurate. No more spinosaurid material would be described from Africa until the latter half of the 20th century, with Spinosaurus remaining an enigmatic and mysterious theropod.

Additional finds

Beginning in the 1980s, Spinosaurus material began being described from sites in Algeria, Morocco, and Tunisia, although these fossils were often isolated and fragmentary. In 1986, a paper referred several teeth found in Cretaceous deposits in Tunisia to Spinosaurus, being the first evidence of the taxon's existence in the country. In 1989, French paleontologist Eric Buffetaut assigned two jaw fragments and a tooth that had been unearthed in a deposit of the Kem Kem Beds in Taouz, Morocco to Spinosaurus sp., expanding the known distribution of the genus to Morocco. In the 1990s, a wealth of spinosaurid remains were described from South America, Asia, Africa, and Europe, strengthening the understanding of Spinosaurus and Spinosauridae. However, much of the anatomy of Spinosaurus still remained obscure and many studies proposed that fossils previously assigned to the genus or Sigilmassasaurus were actually from iguanodont ornithischians, megaraptorans, carcharodontosaurids, or other forms of theropod.

Additional fossils of Spinosaurus were recovered from the Kem Kem Beds in the Tafilalt Oasis of Morocco, near the site of the ancient city of Sigilmassa. In 1996, Canadian paleontologist Dale Russell described these fossils, consisting of three cervical vertebrae, two mandible fragments, and the neural spine of a dorsal vertebra, as belonging to a new species of Spinosaurus, S. maroccanus. The specific name, maroccanus, derives from royaume du Maroc ("Kingdom of Morocco"), where the fossils were unearthed. The site where S. maroccanus' fossils were found is located in the south of the country and made up of red sandstone, known by various names, including the Grès rouges infracénomaniens, Continental Red Beds, and lower Kem Kem Beds. Of these fossils, one cervical vertebra (cataloged at the Canadian Museum of Nature as NMC 50791), was selected as the holotype of S. maroccanus.

S. maroccanus was differentiated from S. aegyptiacus based on the length of its neck vertebrae. Specifically, Russell claimed that the ratio of the length of the centrum (body of vertebra) to the height of the posterior articular facet was 1.1 in S. aegyptiacus and 1.5 in S. maroccanus. Later authors have been split on this topic, with some authors noting that the length of the vertebrae can vary from individual to individual, that the holotype specimen was destroyed and thus cannot be compared directly with the S. maroccanus specimen, and that it is unknown which cervical vertebrae the S. maroccanus specimens represent. Therefore, though some have retained the species as valid without much comment, most researchers regard S. maroccanus as a nomen dubium (dubious name), a junior synonym of S. aegyptiacus, or a junior synonym of Sigilmassasaurus brevicollis. Some studies have referred to the holotype and other referred specimens of S. maroccanus (NMC 50791 and MNHN SAM 124–128) as S. cf. aegyptiacus. The specimens previously ascribed as paratypes of S. maroccanus (NMC 41768 and NMC 50790) were reidentified as spinosaurid specimens that are currently not identifiable at the generic level.

In 1996, a study by American paleontologist Paul Sereno and colleagues assigned cervical vertebrae referred to "Spinosaurus B" and the spinosaurid Sigilmassasaurus (a possible synonym of Spinosaurus) to the carcharodontosaurid Carcharodontosaurus. This was based on the erroneous belief that a cervical vertebra (SGM Din-3) found nearby a skull of Carcharodontosaurus (SGM Din-1) belonged to the same individual. Sereno and colleagues also reasoned that stout cervicals like those of Sigilmassasaurus would be needed to carry the skulls of carcharodontosaurids, however later analyses have proven that "Spinosaurus B" and Sigilmassasaurus are not synonyms or contain fossils from Carcharodontosaurus. Some studies have continued to refer "Spinosaurus B" to Sigilmassasaurus, although this is still debated. In 2003, Oliver Rauhut suggested that Stromer's Spinosaurus holotype (name-bearing) specimen was a chimera, composed of vertebrae and neural spines from a carcharodontosaurid similar to Acrocanthosaurus and a mandible from Baryonyx or Suchomimus, an analysis that was rejected in at least one subsequent paper.

Proposed neotype

In 2008, a Moroccan fossil collector based in Erfoud presented a few fragmentary dinosaur fossils to Italian paleontologist Nizar Ibrahim, who suspected they may belong to Spinosaurus. The next year, several other fossils, constituting a partial skeleton, were acquired by the Museo di Storia Naturale di Milano (MSNM) from an Italian fossil dealer who had purchased them from the same who showed the remains to Ibrahim the previous year. Later, Ibrahim visited the MSNM and was presented the material by Italian paleontologists Cristiano Dal Sasso and Simone Maganuco. Ibrahim recognized that the MSNM fossils and the ones he had seen in 2008 were from a similar sandstone matrix and that the neural spines of the MSNM fossils were similar to those depicted by Stromer in 1915, leading him to think that they may be from the same individual and belonged to Spinosaurus.

Following this, an international collaboration began between Ibrahim and other paleontologists to study the bones and visit the original site, with fossils from the MSNM getting sent to the University of Chicago for study. In 2013, Ibrahim, Moroccan paleontologist Samir Zouhri, and British paleontologist David Martill ventured to Casablanca in search of the original fossil dealer, who they were able to track down. Subsequently, the dealer took them back to the site where the fossils had been found. Over the course of several years, a skeleton of a subadult individual consisting of skull fragments, some cervical, dorsal, and caudal vertebrae, neural spines, a complete sacrum, much of the hindlimbs, several pedal phalanges, and several dorsal ribs was unearthed. This skeleton comes from a locality of the Douria Formation of the Kem Kem Beds in Zrigat, Morocco, dated to the Cenomanian stage of the mid-Cretaceous period. It was deposited at the Casablanca Museum under specimen number FSAC-KK-11888.

In 2014, Ibrahim and colleagues assigned the fossils to S. aegyptiacus, proposed it the neotype (replacement holotype), and stated that all North African Cenomanian spinosaurid material belongs to S. aegyptiacus. The description of these remains were met with intrigue, surprise, and controversy, as the authors claimed that Spinosaurus was a possibly quadrupedal, semiaquatic, short-limbed spinosaurid. The body proportions of the specimen have been debated, as the hind limbs are disproportionately shorter in the specimen than in previous reconstructions. However, it has been demonstrated by multiple paleontologists that the specimen is not a chimera, and is indeed a specimen of Spinosaurus that suggests that the animal had much smaller hind limbs than previously thought.

In 2015, British paleontologist Serjoscha Evers and colleagues rejected the neotype proposal for FSAC-KK-11888 on the basis of the lack of association or locality information for FSAC-KK-11888, the geographical separation between the holotype and FSAC-KK-11888 localities, and anatomical differences between FSAC-KK-11888 and the holotype. Evers and colleagues argue for the validity of both S. marrocanus and S. aegyptiacus, stating that FSAC-KK-11888 likely belongs to the former. Additionally, they state that the geographical separation of FSAC-KK-11888 and the holotype as well as the detailed description of the holotype by Stromer are evidence that FSAC-KK-11888 does not meet the ICZN (International Code of Zoological Nomenclature)'s requirements for a neotype and that the creation of a neotype is unnecessary for S. aegyptiacus. Additionally, some paleontologists have suggested that the proportions of the dorsal vertebrae compared to the legs of FSAC-KK-11888 when compared to the proportions of "Spinosaurus B" illustrate that either the former is a composite (a specimen composed of multiple individuals of the same species)/chimera (a specimen composed of material from two or more species) between an individual known from dorsal vertebrae and an individual known from limb, pelvic, and tail material or that FSAC-KK-11888 is not from Spinosaurus.

Between 2015 and 2019, several additional expeditions to the site unearthed additional fossils of FSAC-KK-11888 including many caudal vertebrae, composing about 80% of the tail with a preserved length of 4 m (13 ft), elements of the pes and hindlimbs, skull fragments, and more. Around 90% of this new material was found in late 2018, whereas some fragments including cranial material were found in debris of previous expeditions. In 2020, Ibrahim and colleagues described the tail of FSAC-KK-11888, which they stated closely compares to the caudal vertebrae of the holotype and "Spinosaurus B". The material found on these expeditions perfectly matches elements of the FSAC-KK-11888, proving that they come from a single individual. The body length of the proposed neotype excluding the tail portion, from the anterior tip of the skull to the posterior region of the pelvic girdle, is estimated up to 5.88 m (19.3 ft),Table S1 and the total length of the tail is estimated up to 5.3 m (17 ft).

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