Abstract
A predominantly fish-eating diet was envisioned for the sail-backed theropod dinosaur Spinosaurus aegyptiacus when its elongate jaws with subconical teeth were unearthed a century ago in Egypt. Recent discovery of the high-spined tail of that skeleton, however, led to a bolder conjecture that S. aegyptiacus was the first fully aquatic dinosaur. The ‘aquatic hypothesis’ posits that S. aegyptiacus was a slow quadruped on land but a capable pursuit predator in coastal waters, powered by an expanded tail. We test these functional claims with skeletal and flesh models of S. aegyptiacus. We assembled a CT-based skeletal reconstruction based on the fossils, to which we added internal air and muscle to create a posable flesh model. That model shows that on land S. aegyptiacus was bipedal and in deep water was an unstable, slow-surface swimmer (<1 m/s) too buoyant to dive. Living reptiles with similar spine-supported sails over trunk and tail are used for display rather than aquatic propulsion, and nearly all extant secondary swimmers have reduced limbs and fleshy tail flukes. New fossils also show that Spinosaurus ranged far inland. Two stages are clarified in the evolution of Spinosaurus, which is best understood as a semiaquatic bipedal ambush piscivore that frequented the margins of coastal and inland waterways.
Research organism: Other
Introduction
In 1915, Ernst von Stromer announced the discovery in Egypt’s Western Desert of the elongate jaws and partial skeleton of a large sail-backed predator Spinosaurus aegyptiacus (Stromer, 1915). Other bones found nearby (Stromer, 1934) contributed to his initial reconstruction of S. aegyptiacus as a sail-backed, piscivorous biped (Stromer, 1936), shortly before all of these bones were destroyed in World War II (Nothdurft et al., 2002; Smith et al., 2006). Over the last 30 years, additional skull and postcranial bones came to light in western Morocco in beds of similar age to those in Egypt (Russell, 1996; Dal Sasso et al., 2005; Smyth et al., 2020; Ibrahim et al., 2020a). Central among these finds was a partial skeleton (designated the neotype) that allowed a more complete reconstruction, confirming its interpretation as a semiaquatic piscivore (Ibrahim et al., 2014).
As skeletal information on the unusual predator improved, so has speculation as to whether S. aegyptiacus was better adapted to life in water as an aquatic predator, based on inferences from oxygen isotopes in enamel (Amiot et al., 2010), the dental rosette likened to the jaws of a conger eel (Vullo et al., 2016), the alleged elevated positioning of the orbits in the skull for visibility while largely submerged (Arden et al., 2019), the hypothetical underwater role of the trunk sail (Gimsa et al., 2016), and the infilling of the medullary cavities of hind limb bones that may have functioned as ballast (Ibrahim et al., 2014; Aureliano et al., 2018).
The aquatic hypothesis
Recent discovery of the tall-spined tail bones of the neotypic skeleton reinvigorated the interpretation of S. aegyptiacus as the first fully aquatic dinosaur (Ibrahim et al., 2020b), here dubbed the ‘aquatic hypothesis,’ which makes three basic propositions. Unlike any other theropod, according to the hypothesis, S. aegyptiacus:
reverted to a quadrupedal stance on land, as shown by a trunk-positioned center of mass (Ibrahim et al., 2014; Ibrahim et al., 2020b), ostensibly knuckle-walking with long-fingered, long-clawed forelimbs;
functioned in water as a capable, diving pursuit predator using an expanded tail as a ‘novel propulsor organ’ (Ibrahim et al., 2020b) or as a ‘subaqueous forager’ (Fabbri et al., 2022); and
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fossils would be found exclusively in coastal or deep-water marine habitats, like all large-bodied secondarily aquatic vertebrates, and would not be expected to be found in freshwater inland environments.
We test these three central propositions.
Critique of the aquatic hypothesis thus far has focused on an alternative functional explanation for the high-spined tail as a display structure and largely qualitative functional interpretations of its skeletal anatomy (Hone and Holtz, 2021). Biomechanical evaluation of the aquatic functionality of S. aegyptiacus remains rudimentary. The propulsive capacity of the tail in water was judged to be better than terrestrial counterparts by oscillating miniature plastic tail cutouts in water (Ibrahim et al., 2020b), a limited approximation of the biomechanical properties of an anguilliform tail (Lighthill, 1969; van Rees et al., 2013; Gutarra and Rahman, 2022) that failed to take account of the bizarre anterior half of the animal. The center of body mass, a critical functional parameter, has been estimated for S. aegyptiacus three times, each estimate pointing to a different location ranging from the middle of the trunk (Ibrahim et al., 2014; Ibrahim et al., 2020b) to a position over the hind limbs (Henderson, 2018). Quantitative comparisons have not been made regarding the size or surface area of the limbs, hind feet, and tail of S. aegyptiacus to counterparts in extant primary or secondary swimmers.
Thus, adequate evaluation of the aquatic hypothesis requires more realistic biomechanical tests, quantitative body, axial and limb comparisons between S. aegyptiacus and extant primary and secondary swimmers, and a survey of bone structure beyond the femur and shaft of a dorsal rib. Such tests and comparisons require an accurate 3D digital flesh model of S. aegyptiacus, which, in turn, requires an accurate skeletal model. Hence, we began this study by assembling a complete set of CT scans of the fossil bones for S. aegyptiacus and its African forerunner, Suchomimus tenerensis (Sereno et al., 1998).
Aquaphilic terminology
Aquatic status is central to the ‘aquatic hypothesis.’ The hypothesis holds that S. aegyptiacus is the first non-avian dinosaur bearing skeletal adaptations devoted to lifestyle and locomotion in water, some of which inhibited terrestrial function. The contention is that S. aegyptiacus was not only a diving pursuit predator in the open-water column, but also a quadruped on land with long-clawed forelimbs poorly adapted for weight support. A later publication seemed to downgrade that central claim by suggesting that any vertebrate with ‘aquatic habits,’ such as wading, submergence, or diving, had an ‘aquatic lifestyle’ (Fabbri et al., 2022). That broadened usage of ‘aquatic lifestyle,’ however, blurs the long-standing use of aquatic as applied to lifestyle (Pacini and Harper, 2008). We outline below the traditional usage of aquaphilic terms, which we follow.
The adjective ‘aquatic’ is used either as a broad categorization of lifestyle or, in more limited capacity, in reference to an adaptation of a species or group. In the former case, a vertebrate with an ‘aquatic lifestyle’ or ‘aquatic ecology’ is adapted for life primarily, or solely, in water with severely reduced functional capacity on land (Pacini and Harper, 2008). Aquatic vertebrates (e.g., bony fish, sea turtles, whales) live exclusively or primarily in water and exhibit profound cranial, axial, or appendicular modifications for life in water, especially at larger body sizes (Webb, 1984; Webb and De Buffrénil, 1990; Hood, 2020). For example, extant whales are secondarily aquatic mammals that spend all of their lives at sea and exhibit profound skeletal modifications for aquatic sensory and locomotor function. A marine turtle, similarly, is considered an aquatic reptile, regardless of whether it ventures ashore briefly to lay eggs, because the vast majority of its life is spent in water using profoundly modified limbs for aquatic locomotion (flippers) that function poorly on land.
An aquaphilic animal with less profound adaptations to an aqueous arena is said to be semiaquatic (or semi-aquatic), no matter the proportion of aquatic foodstuffs in its diet, the proportion of time spent in water, or the proficiency of swimming or diving. Nearly all semiaquatic vertebrates are secondarily aquaphilic, having acquired aquatic adaptations over time to enhance functional capacity in water without seriously compromising terrestrial function (Howell, 1930; Hood, 2020). Indeed, semiaquatic animals are also semiterrestrial (Fish, 2016). For example, freshwater turtles are regarded as semiaquatic reptiles because they frequent water rather than live exclusively within an aqueous habitat, are sometimes found in inland habitats, and exhibit an array of less profound modifications (e.g., interdigital webbing) for locomotion in water (Pacini and Harper, 2008). Likewise, extant crocodylians and many waterbirds are capable swimmers and divers but retain excellent functional capacity on land. Auks (Alcidae), among the most water-adapted of semiaquatic avians, are agile wing-propelled, pursuit divers with an awkward upright posture on land resembling penguins, but they retain the ability to fly and inhabit land for extended periods (Nettleship, 1996). On the other hand, the flightless penguins (Sphenisciformes) are considered aquatic due to their more profound skeletal modifications for swimming and deep diving and more limited terrestrial functionality, although still retaining the capacity to trek inland and stand for considerable durations while brooding. As nearly all semiaquatic vertebrates have an aquatic diet and the ability to swim or dive, more profound functional allegiance to water is requisite for an ‘aquatic’ appellation (Pacini and Harper, 2008).
An aquatic adaptation of an organism refers to the function of a particular feature, not the overall lifestyle of an organism. That feature should have current utility and primary function in water (Houssaye and Fish, 2016). Aquatic adaptations are presumed to have evolved their functionality in response to water and cannot also have special functional utility in a subaerial setting. For example, the downsized, retracted external nares in spinosaurids would inhibit water intake through the nostrils while feeding with the snout submerged (Sereno et al., 1998; Dal Sasso et al., 2005; Ibrahim et al., 2014; Hone and Holtz, 2021). There is at present no plausible alternative explanation involving terrestrial function for the downsizing and retraction of the external nares in spinosaurids, a unique condition among non-avian theropods. In contrast, the hypertrophied neural spines of the tail in S. aegyptiacus are ambiguous as an ‘aquatic adaptation’ because expanded tails can function both as aquatic propulsors and terrestrial display structures. For the expanded tail to be an ‘aquatic adaptation,’ its morphological construction and biomechanical function must unequivocally show primary utility and capability in water, as is the case with extant tail-powered primary or secondarily aquatic vertebrates (e.g., newts, crocodylians, beavers, otters; Fish et al., 2021). The same must be shown or inferred to be the case in extinct secondarily aquatic vertebrates (Gutarra and Rahman, 2022). Using various comparative and biomechanical approaches (below), we have not found such substantiating evidence to interpret the heightened tail in S. aegyptiacus or other spinosaurids as an aquatic adaptation, confirming similar conclusions reached recently by Hone and Holtz, 2021.
Our approach
To test the aquatic hypothesis for S. aegyptiacus, we began with CT scans of spinosaurid fossils from sites in Africa to build high-resolution 3D skeletal models of S. aegyptiacus (Figure 1A) and its forerunner, S. tenerensis (Figure 1F). Many vertebrae and long bones in both genera show significant internal pneumatic (air) or medullary (marrow) space, which has ramifications for buoyancy. When compared to the 2D silhouette drawing used in the aquatic hypothesis (Ibrahim et al., 2020b), our CT-based 3D skeletal model of S. aegyptiacus differs significantly in skeletal proportions.
We enveloped the skeletal model in flesh informed by CT scans revealing the muscle volume and air spaces in extant reptilian and avian analogs. To create a 3D flesh model for S. aegyptiacus (Figure 2A and B), internal air spaces (trachea, lungs, air sacs) were shaped and positioned as in extant analogs. We created three options for internal air volume based on extant squamate, crocodilian, and avian conditionsand assigned densities to body partitions based on local tissue types and air space. We calculated the surface area and volume of the flesh model as well as its component body parts.
We posed this integrated flesh model in bipedal, hybrid- and axial-powered poses, the latter two based on the swimming postures of extant semiaquatic reptiles (Grigg and Kirshner, 2015; Figure 2B). We calculated center of mass (CM) and center of buoyancy (CB) to evaluate the habitual two- or four-legged stance of S. aegyptiacus on land (Figure 1A), the depth of water at the point of flotation (Figure 2D), and the neutral position of the flesh model in deeper water (Figure 2A and B). Using biomechanical formulae (Lighthill, 1969) and data from extant alligators (Fish, 1984), we estimated the maximum force output of its tail, which was used to calculate maximum swimming velocity at the surface and underwater(Figure 3A). We also evaluated its stability, maneuverability, and diving potential in water (Figure 3B), with all of these functional capacities compared to extant large-bodied aquatic vertebrates.
We turned to extant analogs to consider the structure and function of similar spine-supported sails over the trunk and tail in lizards and the form of tail vertebrae in tail-powered secondary swimmers (Figure 4). We also considered the relative size (surface area) of appendages in a range of secondary swimmers (Figure 5), and how the surface area of foot paddles and tail scale in crocodylians (Figure 6).
Lastly, we turned to the spinosaurid fossil record to look at the habitats where spinosaurid fossils have been found. We reviewed their distributionto determine whether spinosaurids, and S. aegyptiacus in particular, were restricted to coastal, marine habitats like all large secondarily aquatic vertebrates. We updated spinosaurid phylogeny in order to discern major stages in the evolution of spinosaurid piscivorous adaptations and sail structures (Figure 8), incorporating the latest finds including new fossils of Spinosaurus from Niger.
Institutional abbreviations
BSPG, Bayerische Staatssammlung für Paläontologie und Geologie, Munich, Germany; FMNH, Field Museum of Natural History, Chicago, IL, USA; FSAC, Faculté des Sciences Aïn Chock, University of Casablanca, Casablanca, Morocco; KU, The University of Kansas, Natural History Museum, Lawrence, KS, USA; MNBH, Musée National de Boubou Hama, Niamey, Niger; MNHN, Muséum national d’Histoire naturelle, Paris, France; NMC, Canadian Museum of Nature, Ottawa, Canada; UCMP, University of California, Museum of Paleontology, Berkeley, CA, USA; UCRC, University of Chicago Research Collection, Chicago, IL, USA; UF, University of Florida, University of Florida Collections, Gainesville, FL, USA; UMMZ, University of Michigan, Museum of Zoology, Ann Arbor, MI, USA; WDC, Wildlife Discovery Center, Lake Forest, IL, USA.
Results
Spinosaurid skeletal models
Our skeletal reconstruction of an adult S. aegyptiacus is just under 14 m long (Figure 1A), which is more than 1 m shorter than previously reported (Ibrahim et al., 2014). Major differences are apparent when compared to the 2D graphical reconstruction of the aquatic hypothesis (Ibrahim et al., 2020b). The length of the presacral column, depth of the ribcage, and length of the forelimb in that reconstruction were overestimated by ~10, 25, and 30%, respectively, over dimensions based on CT-scanned fossils. When translated to a flesh model, all of these proportional overestimates (heavier neck, trunk, forelimb) shift the center of mass anteriorly (see ‘Materials and methods’).
The hind limb long bones (femur, tibia, fibula, metatarsals) in S. aegyptiacus lack the medullary cavity common to most dinosaurs and theropods in particular. When first discovered, the infilled hind limb bones in S. aegyptiacus were interpreted as ballast for swimming (Ibrahim et al., 2014). However, the infilled condition is variable as shown by the narrow medullary cavity in a femur of another individual slightly larger than the neotype (Russell, 1996; NMC 41869). Furthermore, the bone infilling is fibrolamellar and cancellous, similar to the infilled medullary cavities of other large-bodied terrestrial dinosaurs (Vanderven et al., 2014) and mammals (Houssaye et al., 2016). In contrast, dense pachystotic bone composes the solid and sometimes swollen bones of many secondarily aquatic vertebrates that use increased skeletal density as ballast (Houssaye, 2009).
Medullary space is present in most forelimb bones in both S. aegyptiacus and S. tenerensis (Figure 1D and H). The centra of anterior caudal vertebrae are occupied by a large medullary space (Figure 1C and J), and large air-filled pneumatic spaces are present in the centra and neural arches of cervical vertebrae (Evers et al., 2015; Figure 1B). Collectively, these less dense, internal marrow- and air-filled spaces in S. aegyptiacus more than offset the added density of infilled medullary space in the relatively reduced hind limb long bones (Figure 1A). Hind limb bone infilling is better explained as compensation for the reduced size of the hind limb long bones that must support a body mass at the upper end of the range for theropods. Bending strength increases by as much as 35% when the medullary cavity is infilled (see Appendix 1).
S. aegyptiacus flesh model form and function
We added flesh to the adult skeletal model and divided the flesh model into body partitions adjusted for density. Muscle volume was guided by CT cross-sections from extant lizards, crocodylians, and birds (Figure 2B), and internal air space (pharynx-trachea, lungs, paraxial air sacs) was modeled on lizard, crocodilian, and avian conditions (Figure 2C; see ‘Materials and methods,’ Appendix 2). Whole-body and body part surface area and volume were calculated, and body partitions were assigned density comparable to that in extant analogs (see ‘Materials and methods’). For biomechanical analysis, we positioned the integrated flesh model in bipedal stance (Figure 1A) as well as hybrid- and axial-powered swimming poses (Grigg and Kirshner, 2015; Figure 2A and B).
The CM and CB of the flesh model were determined to evaluate habitual stance on land and in shallow water (Figure 1A), the water depth at the point of flotation (Figure 2D), and its swimming velocity, stability, maneuverability, and diving potential in deeper water (Figure 3). No matter the included volume of internal air space, CM is positioned over the ground contact of symmetrically positioned hind feet (Figure 1A, red cross). Thus, S. aegyptiacus had a bipedal stance on land as previously suggested (Henderson, 2018), contrary to trunk-centered CM of the aquatic hypothesis (Ibrahim et al., 2020b). Consistent with a bipedal stance, the manus is adapted for prey capture and manipulation (elongate hollow phalanges, scythe-shaped unguals) rather than weight support (Figure 1A and D).
Adult S. aegyptiacus can feed while standing in water with flotation occurring in water deeper than ~2.6 m (Figure 2D). In hybrid or axial swimming poses, trunk air space tilts the anterior end of the model upward (Figure 2A and B). With density-adjusted body partitions and avian-like internal air space, the flesh model of S. aegyptiacus has a body mass of 7390 kg and an average density of 833 kg/m3 (see ‘Materials and methods’), which is considerably less than the density of freshwater (1000 kg/m3) and saltwater (1026 kg/m3) or the average density of living crocodylians (1080 kg/m3; Grigg and Kirshner, 2015).
Swimming velocity at the surface and underwater in extant lizards and crocodylians is powered by foot paddling and axial undulation (hybrid swimming; Frey and Salisbury, 2001) and at moderate to maximum (critical) speeds by axial undulation alone (axial swimming) (Fish, 1984; Grigg and Kirshner, 2015). We used Lighthill’s bulk momentum formula to estimate maximum surface and underwater swimming velocity for the flesh model of S. aegyptiacus (Lighthill, 1969). Assuming a fully compliant Alligator-like tail (tail amplitude 0.24/body length, tail wavelength 0.57/body length, and tailbeat frequency 0.25 Hz; Fish, 1984; Sato et al., 2007), tail thrust (Pt) and maximum velocity (U) can be determined (Pt = –164.93 + 1899.1U – 896.35U2). Assuming turbulent conditions, a body drag coefficient of 0.0035 was estimated for a Reynolds number of 752,400 at a swimming speed of 1.0 m/s. The total power from estimates of drag increased three- to fivefold to account for undulation of the tail, near-surface wave formation, and increased sail drag when underwater (Figure 3A). The addition of the sail increases the drag on the body of S. aegyptiacus by 33.4%. The intersection of the thrust power curve and drag power curves, where the animal would be swimming at a constant velocity, indicates slow maximum velocity at the surface (~0.8 m/s) and only slightly greater when submerged (~1.4 m/s) (Figure 3A). Maximum tail thrust in S. aegyptiacus is 820 Watts (683 N or 154 lbs), a relatively low value for the considerable caudal muscle mass in this large theropod (Snively and Russell, 2007; Mallison et al., 2015). Only a minor amount of caudal muscle power, however, is imparted to the water as thrust during undulation. As a result, maximum velocity is only 1.2 m/s, an order of magnitude less than extant large-bodied (>1 m) pursuit predators. These species (mackerel sharks, billfish, dolphins, and killer whales) are capable of maximum velocities of 10–33 m/s (Tinsley, 1984; Fish, 1998; Fish and Rohr, 1999; Iosilevskii and Weihs, 2008).
Stability and the capacity to right are important in water. When positioned upright in water, the trunk sail of S. aegyptiacus is emergent (Figure 3B, position 1). The flesh model, however, is particularly susceptible to long-axis rotation given the proximity of CM and CB, with stable equilibrium attained when floating on its side (Figure 3B, position 3). Righting requires substantial torque (~5000 Nm) that is impossible to generate with vertical limbs and a tail with far less maximum force output (~700 N). This stability predicament remains even with the smallest internal air space. The absence of vertical stability and righting potential in water stands in stark contrast to the condition in extant crocodylians and marine mammals (Fish, 1998; Grigg and Kirshner, 2015).
Maneuverability in water (acceleration, turning radius, and speed) wanes as body length increases (Domenici, 2001; Parson et al., 2011; Domenici et al., 2014; Hirt et al., 2017; Gutarra and Rahman, 2022), which is further compromised in S. aegyptiacus by its rigid trunk (see below) and expansive, unretractable sail. In contrast, large-bodied secondary swimmers capable of pursuit predation in open water have fusiform body forms with a narrow caudal peduncle for efficient tail propulsion (ichthyosaurs, cetaceans; Motani, 2009), control surfaces for reorientation, and narrow extensions (bills) to enhance velocity in close encounters with smaller more maneuverable prey (Maresh et al., 2004; Domenici et al., 2014). Besides some waterbirds, semiaquatic pursuit predators are rare and include only the small-bodied (<2 m), exceptionally maneuverable otters that employ undulatory swimming (Fish, 1994).
Diving with an incompressible trunk requires a propulsive force (Fg) greater than buoyancy. For S. aegyptiacus, in addition, a depth of ~10 m is needed to avoid wave drag (Figure 3A, bottom). The propulsive force required to dive is ~17,000 N: ; 8.94 m3 [1026–833 kg/m3] 9.8 m/s = 16,909 N), or ~25 times the maximum force output of the tail. Even with lizard-like internal air space, diving still requires ~15 times maximum force output of the tail. To initiate a dive, furthermore, the tail would be lifted into the air as the body rotates about CB (Figure 2D), significantly reducing tail thrust. The now common depictions of S. aegyptiacus as a diving underwater pursuit predator contradict a range of physical parameters and calculations, which collectively characterize this dinosaur as a slow, unstable, and awkward surface swimmer incapable of submergence.
Axial comparisons to aquatic vertebrates and sail-backed reptiles
Axial flexibility is requisite for axial-propulsion in primary or secondary swimmers. However, in S. aegyptiacus, trunk and sacral vertebrae are immobilized by interlocking articulations (hyposphene-hypantrum), an expansive rigid dorsal sail composed of closely spaced neural spines, and fused sacral centra (Figure 1A).
The caudal neural spines in S. aegyptiacus stiffen a bone-supported tail sail by an echelon of neural spines that cross several vertebral segments, which effectively resist bending at vertebral joints (Figure 4A). The caudal centra in S. aegyptiacus have nearly uniform subquadrate proportions along the majority of the tail in lateral view, rather than narrowing, spool-shaped centra in crocodylians and other secondarily aquatic squamates (Figure 4D), which increases distal flexibility during tail undulation. These salient structural features of the tail suggest that it functioned more as a pliant billboard than flexible fluke.
No primary or secondary vertebrate swimmer has a comparable drag-magnifying, rigid dorsal sail including sailfish, the dorsal fin of which is fully retractable and composed of pliable spines in membrane (Domenici et al., 2014). In contrast, the distal tail of secondary swimmers such as crocodylians (Grigg and Kirshner, 2015), mosasaurs (Lindgren et al., 2013) and cetaceans (Fish, 1998) is expanded with pliable soft tissues free of bone to form a flexible caudal paddle or fluke (Figure 4C).
Spine-supported, torso-to-caudal sails aligned with median cranial crests, in contrast, have evolved multiple times for intraspecific display rather than aquatic propulsion among extant lizard (agamids, iguanians, chameleons). Semiaquatic sailfin and basilisk lizards (Figure 4B), for example, do not use their sails while swimming, spend very little time submerged, and are not aquatic pursuit predators (Hone and Holtz, 2021).
Caudal centra proportions in most secondary swimmers, as mentioned above, grade from subquadrate to spool-shaped in the distal half of the tail to increase flexibility and undulatory amplitude (Figure 4D), whereas those in S. aegyptiacus maintain relatively uniform proportions along the tail. This uniformity of subquadrate proportions in S. aegyptiacus should not be confused with a more derived piscine pattern of uniform, short, disc-shaped centra that has evolved in parallel in mosasaurs (Lindgren et al., 2013; Figure 4D, Appendix 2).
Appendicular comparisons to vertebrate secondary swimmers
Appendage (fore and hind limb) surface area in secondary swimmers is minimized to reduce drag because terrestrial limbs are inefficient aquatic propulsors. Appendage surface area in S. aegyptiacus, in contrast, is substantially greater than in reptilian and mammalian secondary swimmers and even exceeds that of the terrestrial predators Allosaurus and Tyrannosaurus (Figure 5).
Interdigital webbing is used by some secondary swimmers to increase the area of the foot paddle (Fish, 2004). Extant crocodylians use their limbs in paddling only at launch and slow speed before tucking them against the body (Grigg and Kirshner, 2015). Crocodylian interdigital webbing, which is better developed and always present in the hind foot (Figure 6C and D), only modestly increases surface area (<20%). Across a range of body size, we show that crocodylian paddle area scales isometrically (Figure 6F; see Appendix 3). The crocodylian foot paddle, thus, becomes even less effective as a propulsor with increasing body size. A crocodylian of spinosaurid size, nonetheless, would have a foot paddle area an order of magnitude greater than is possible in S. aegyptiacus (Figure 6E). Even a fully webbed hind foot in S. aegyptiacus (Figure 6A), for which there is no hard evidence to establish as likely, is far too small to have functioned either for significant aquatic propulsion or for stabilizing control.
Paleohabitats and evolution
Most Spinosaurus fossils come from marginal basins along northern Africa in deltaic sediment laid down during an early Late Cretaceous transgression (Figure 7A, sites 1, 2). These deposits, however, also include the majority of non-spinosaurid dinosaur remains, all of which may have been transported to some degree from inland habitats to coastal delta deposits. Because fossil transport is one way (downstream), documenting the inland fossil record is key to understanding true habitat range. We recently discovered fossils pertaining to Spinosaurus in two inland basins in Niger far from a marine coastline (Figure 7A, site 3). They were buried in fluvial overbank deposits alongside terrestrial herbivores (rebbachisaurid and titanosaurian sauropods) (see Appendix 4).
The inland location of these fossils completely undermines the interpretation of S. aegyptiacus as a ‘highly specialized aquatic predator that pursued and caught its prey in the water column’ (Ibrahim et al., 2020b). All large-bodied secondarily aquatic vertebrates are marine—both extant (e.g., sea turtles, sirenians, seals, whales) and extinct (e.g., protostegid turtles, ichthyosaurs, metriorhynchoid crocodylomorphs, plesiosaurs). None of these diverse water dwellers live in both saltwater and freshwater habitats (Evers et al., 2019; Motani and Vermeij, 2021). Secondarily aquatic vertebrates that live in freshwater habitats have marine antecedents and are all small-bodied, such as river dolphins (<2.5 m length; Hamilton et al., 2001), small lake-bound seals (<2 m; Fulton and Strobeck, 2010), the river-bound Amazonian manatee (<2.5 m; Guterres-Pazin, 2014), and a few mosasaurs and plesiosaurs of modest body size (Gao et al., 2019).
Large-bodied semiaquatic reptiles, in contrast, frequent coastal and inland locales today and in the past. Sarcosuchus imperator, among the largest of semiaquatic reptiles (~12 m length; Sereno et al., 2001), lived in the same inland basin as S. tenerensis. The fossil record supports our interpretation of Spinosaurus as a semiaquatic bipedal ambush predator that frequented the margins of both coastal and inland waterways.
The large body size of S. aegyptiacus and older related species such as S. tenerensis also mitigates against an aquatic interpretation for the former as it would constitute the only instance among vertebrates where the evolution of a secondarily aquatic species occurred at body size greater than 2–3 m. The profound changes involved in fully reentering the aquatic realm from a land-based lifestyle seem more likely to occur at relatively small body size. All other large-bodied secondarily aquatic vertebrates (e.g., ichthyosaurs, plesiosaurs, metriorhynchoid crocodylomorphs, protostegid turtles, mosasaurs, sirenians, whales) evolved the adaptations requisite for an aquatic lifestyle at small body size, increasing in body size once fully established within the marine realm (Domning, 2000; Thewissen et al., 2009; Polcyn et al., 2014; Moon and Stubbs, 2020; Motani and Vermeij, 2021).
Phylogenetic analysis of an enlarged dataset for spinosaurids clarifies piscivorous adaptations in the earliest spinosaurids (stage 1, ~130 Ma) that enhance prey capture in shallow water and heighten visual display (Figure 8; Appendix 5). In the skull, these include an elongate snout tipped with a dental rosette for snaring fish, retracted external nares to inhibit water intake, and a prominent nasal crest (Charig and Milner, 1997; Sereno et al., 1998). The ornamental crest over the snout is accompanied by the evolution of a postcranial sail of varying height supported by neural spines of the posterior dorsal, sacral and caudal vertebrae (Stromer, 1915; Sereno et al., 1998; Allain et al., 2012; Barker et al., 2021).
The earliest spinosaurids, in addition, have ‘cervicalized’ anterior trunk vertebrae to enhance ventroflexion and the effective length of the neck, presumably as an adaptation to feeding in water (Hone and Holtz, 2021). Using the second dorsal vertebrae of the terrestrial predator Allosaurus for comparison, the homologous vertebra in spinosaurids shows marked modification (anterior face is convex, prominent ventral keel for muscular attachment, neural spine is reduced, zygapophyses large and planar). Giraffids, for a similar purpose, have ‘cervicalized’ the first thoracic vertebra to facilitate dorsiflexion and effective neck length (Lankester, 1908; Danowitz et al., 2015; Müller et al., 2021). Neural spines over the trunk and tail are heightened to varying degrees in all spinosaurids including baryonychines (Figure 1F and I). The features cited above to enhance piscivory and display appear to be shared by all currently known spinosaurids and comprise the adaptations we identify as Stage 1 (Figure 8).
Baryonychines (e.g., Suchomimus, Baryonyx, Ceratosuchops) have a low, cruciate nasal crest and swollen brow ridges over the orbits for display or agonistic purposes. These may comprise features unique to this subclade of spinosaurids. Spinosaurines, on the other hand, exhibit further specializations for piscivory and display (Figures 1A and 8, stage 2). Piscivorous adaptations include spaced teeth with smooth carinae for puncturing efficiency, smaller, more retracted external nares to inhibit water intake, more prominent muscle attachments on the ventral aspect of cervicodorsal vertebrae for ventral lunging, and scythe-shaped manual unguals for slicing (Sues et al., 2002; Dal Sasso et al., 2005; Ibrahim et al., 2014). Adaptations for enhanced display include a heightened cranial crest, low cervical sail, and a hypertrophied torso-to-caudal sail.
Discussion
In 1915 Ernst Stromer highlighted the remarkable adaptations in the jaws and neural spines of S. aegyptiacus for piscivory and ostentatious display, respectively, citing modern analogs for both (Stromer, 1915). Nothing close to this morphology had ever been described among nonavian dinosaurs at that time. More recently, a sequence of investigators have gone further, attempting to fathom the manner in which the lifestyle of this large predatory dinosaur engaged coastal waters. All have been hamstrung by the scarcity and fragmentary nature of the specimens, as all of Stromer’s Egyptian fossils were destroyed in World War II. Indeed, the unveiling of a new partial skeleton from Morocco (Ibrahim et al., 2014) and its tail 6 years later (Ibrahim et al., 2020b) generated hypotheses for semiaquatic and aquatic interpretations, respectively.
The superficially eel-like morphology of the tail, viewed as a ‘novel propulsor organ,’ provided the inspiration for the ‘aquatic hypothesis,’ which envisioned S. aegyptiacus as a tail-propelled, diving predator ‘that pursued and caught its prey in the water column’ (Ibrahim et al., 2020b). Conversely, as would be requisite for status as a secondarily aquatic reptile, its terrestrial capabilities were regarded as seriously diminished by a trunk-positioned center of body mass (Ibrahim et al., 2014; Ibrahim et al., 2020b) that would require a quadrupedal stance on land and the use of long-clawed forelimbs not at all designed for weight support. Presented as support for the aquatic hypothesis, Fabbri et al used bone compactness to assert that S. aegyptiacus was a ‘subaqueous forager’ with diving bona fides (Fabbri et al., 2022).
The aquatic hypothesis, nonetheless, requires far more than proving its tail was a high-powered source of propulsion or its bones a bit more compact. In order to conclude that S. aegyptiacus was an aquatic diver and pursuit predator, one also must understand its buoyancy, stability, velocity, maneuverability, and diving performance in water. Those calculations require an accurate flesh rendering, which in turn is built over an accurate skeletal model.
Therefore, we began with CT scans of the fossils to piece together an accurate skeletal model, discovering major discrepancies with the original 3D skeletal model (Ibrahim et al., 2014) and the 2D skeletal silhouette used by the aquatic hypothesis (Fabbri et al., 2022). Comparisons to the 2D model with the more accurate tail show that skeletal regions anterior to the hips are enlarged in length and depth beyond the dimensions of our CT-based reconstruction, shifting the CM in the resulting flesh model forward from the hips to the trunk. Trunk length was increased in both previous models of S. aegyptiacus due to unnatural ventroflexion of the dorsal column that also spread further the neural spines of the sail (Figure 9). When neotype (CT-scanned) or rebuilt holotype dorsal vertebrae of S. aegyptiacus are rearticulatd in an osteological neutral pose, the shorter torso has a straighter column with less spread neural spines. The ribcage, in addition, is not as deep, based on the preserved rib pieces of the holotype and neotype and the nearly complete ribcage known for S. tenerensis (Figures 1F and 9). These proportions effectively reduce the volume of the trunk in our flesh model (Figure 2). The flesh model used by the aquatic hypothesis, likewise, underestimated the muscle mass at the base of the tail, judging from our study of CT scans of crocodylians and a range of other reptiles (Díez Díaz et al., 2020). These differences are far from trivial when considering centers of mass and buoyancy in S. aegyptiacus. The dinosaur, in fact, stood back up on its hind legs like all other theropods.
With a more accurate flesh model in hand, we embarked on a range of biomechanical tests of its performance in water, determining that it fell short in all critical measures by huge margins. S. aegyptiacus failed spectacularly by factors from four- to tenfold for maximum swimming speed on the surface or underwater (Figure 3A), for the capacity to right and remain stable or maneuver underwater (Figure 3B), and for generating the force needed to overcome buoyancy and fully submerge. S. aegyptiacus was an unstable, slow swimmer without the capacity to submerge. These are stiff biomechanical hurdles for the aquatic hypothesis to overcome.
We thought of other comparative means to test the aquatic hypothesis, plotting S. aegyptiacus against various extant and extinct secondarily aquatic amniotes to consider appendage area (Figure 5), the size of foot and tail paddles in crocodylians (Figure 6), tail structure (Figure 4C and D), and the habitats occupied by large-bodied secondarily aquatic vertebrates (Figure 7A). S. aegyptiacus fails all of these comparative tests as well because it resembles other theropod dinosaurs in limb size, other reptiles that use midline sails for display, and semiaquatic reptiles in the diversity of coastal and inland habitats occupied.
Although additional fossils of S. aegyptiacus and other spinosaurids will surely come to light, the overall skeletal proportions and form of S. aegyptiacus are largely known. Although many fine points on the structure and function of this interesting clade of predators will surely continue to engender controversy. The aquatic hypothesis, for that reason, is unlikely to survive as a plausible lifestyle interpretation. What then is our lifestyle interpretation for S. aegyptiacus? Our study and that of Hone and Holtz, 2021 envision S. aegyptiacus as a bipedal, semiaquatic dinosaur using ambush predation of large fish while wading into shallow coastal and riverine waters.
Thirteen principal conclusions can be drawn from this study, all of which may be tested:
Adult S. aegyptiacus had a body length of under 14 m with the axial column in neutral pose.
The reduced hind limb long bones in neotypic skeleton of S. aegyptiacus are infilled likely as an adaptation to weight support on land rather than functioning as ballast to increase density in water.
The segment-crossing caudal neural spines in S. aegyptiacus suggest that its tail functioned more as a pliant billboard than flexible fluke.
S. aegyptiacus, like S. tenerensis and other spinosaurids, was bipedal on land with its CM positioned over its hind feet. The long-clawed forelimbs of S. aegyptiacus were not used in weight support on land.
S. aegyptiacus could wade into shallow water for feeding with flotation occurring at water depth greater than ~2.6 m.
An adult flesh model of S. aegyptiacus has a body mass of ~7400 kg and average density of ~830 kg/m3, which is considerably less than the density of saltwater (1026 kg/m3).
S. aegyptiacus was incapable of diving, given its buoyancy and incompressible trunk. Full submergence would require 15–25 times the maximum force output of its tail, depending on estimated lung volume.
S. aegyptiacus was unstable in deeper water with little ability to right itself, swim, or maneuver underwater. Maximum power from its tail, assuming it could undulate as in Alligator, is less than 700 N, which would generate a top speed of ~1 m/s, an order of magnitude slower than extant large-bodied pursuit predators.
All extant and extinct large-bodied (>2 m long) secondarily aquatic vertebrates are strictly marine, whereas fossils pertaining to Spinosaurus have been found in inland basins distant from a marine coast.
Transition to a semiaquatic lifestyle, as occurred in the evolution of spinosaurid theropods, can occur at any body size. Transition to an aquatic lifestyle among tetrapods, in contrast, has only occurred at relatively small body size (<3 m) with subsequent radiation once in the marine realm into larger body sizes.
S. aegyptiacus is interpreted as a semiaquatic shoreline ambush predator more closely tied to waterways than baryonychine spinosaurids.
Spinosaurids flourished over a relatively brief Cretaceous interval (~35 My) in circum-Tethyan habitats with minimal impact on aquatic habitats globally.
Two phases are apparent in evolution of aquatic adaptations among spinosaurids, the second distinguishing spinosaurines as the most semiaquatic of non-avian dinosaurs.
Materials and methods
Skeletal reconstruction
The composite skeletal reconstruction of S. aegyptiacus is based principally on bones of holotypic and neotypic specimens supplemented by associated and isolated bones from Cenomanian-age formations in Egypt, Morocco, and Niger (Figure 1A). The two most important specimens include the subadult partial skeleton composing the holotype (BSP 9012 VIII 19) from the Western Desert of Egypt (Stromer, 1915; Smith et al., 2006) and a subadult partial skeleton designated as the neotype from the Kem Kem Group in Morocco (FSAC-KK 11888; Ibrahim et al., 2014; Ibrahim et al., 2020b). A third referred specimen from Egypt was also considered (BSPG 1922 X45, ‘Spinosaurus B’; Stromer, 1934). These are the only associated specimens known for S. aegyptiacus on which to base the skeletal reconstruction, the relative size calculated from overlapping bones (Table 1). Of these three specimens, only the bones of the neotype are preserved, all of which have been CT-scanned except for recently discovered bones of the tail (Ibrahim et al., 2020b). Noteworthy isolated specimens have been recovered from the Kem Kem Group in Morocco, including a large snout and manual phalanx used to gauge maximum adult body size.
Table 1. Relative size of specimens in the skeletal reconstruction of S. aegyptiacus.
No. | Specimen | Maturity | Relative size (%) | Linearupsizing | Description |
---|---|---|---|---|---|
1 | BSPG 1912 VIII 19 |
Subadult | 76 | 1.32 | Holotype (destroyed) preserving dentaries, presacral, sacral and caudal vertebrae including the dorsal sail (Stromer, 1915) |
2 | FSAC-KK 11888 | Subadult | 76 | 1.32 | Neotype preserving skull bones, partial limbs, dorsal sail and most of the tail (Ibrahim et al., 2014) |
3 | BSPG 1922X45 |
Subadult | 66 | 1.51 | ‘Spinosaurus B’ (destroyed) fragmentary specimen with five partial dorsals (~D1 centrum, mid dorsal centrum, partial ~D13 vertebra), seven partial caudal vertebrae, and both tibiae (Stromer, 1934) |
4 | MSMN V4047 | Adult | 100 | — | Isolated snout with broken teeth (Dal Sasso et al., 2005); large size and coossified sutures indicate maturity |
5 | UCRC PV8 | Adult | 80 | 1.25 | Large manual phalanx I-1 (28.0 cm length) of an adult within reach but still smaller than the 35 cm length estimated on the basis of the proportions in the manus of Angaturama (?=Irritator) scaled to the adult snout (Aureliano et al., 2018) |
6 | UCRC PV24 | Adult | 75 | 1.33 | Large Kem Kem vertebra, ~C9, from Gara Sbaa (centrum length 11.6 cm, centrum width 14.0 cm) |
We incorporated all CT-scanned bones of the neotype and reconstructions (based on lithographic plates and photographs) of bones of the holotype and referred specimen from Egypt. For unknown bones without sequential adjacency as a guide, other spinosaurids were consulted for shape and proportion. All digital bones were articulated in osteologically neutral pose (Stevens and Parrish, 1999), a standardizing criterion for comparing vertebrate skeletons (Mallison, 2010; Vidal et al., 2020). In the case of overlapping bones, priority was given to the neotype (blue) followed by the holotype (red) and referred specimens (yellow). Bones without representation among specimens attributed to S. aegyptiacus are shaded gray (Figure 1A).
Skeletal reconstructions compared
We compared our digital skeletal model of S. aegyptiacus to the recently published 2D silhouette skeletal reconstruction in the aquatic hypothesis (Ibrahim et al., 2020b), both of which are based primarily on holotypic and neotypic specimens (Figure 9). We registered the reconstructions to each other by superimposing the four longest complete bones of the neotype (femur, tibia, ilium, ischium). Significant differences are apparent in several dimensions with major implications for the calculation of CM and CB.
When aligned at the hip, sacral and caudal columns have nearly identical length, but the presacral column is significantly longer (~10%) in the reconstruction of the aquatic hypothesis. The extra length of the presacral column is located in the neck between C2-10 and torso between D4-13. The trunk in our digital skeletal model is also not as deep as that in skeletal silhouette drawing, as can be seen by aligning the skeletons along the dorsal column (Figure 9C). The contour of the belly marked by the gastral basket and the coracoids of the pectoral girdle extend farther ventrally (~25%) than the ends of the pubes, unlike our digital reconstruction or that of most other silhouette reconstructions for non-avian theropods. The length of the ribcage in our model is consistent with the only well-preserved spinosaurid ribcage known to date (S. tenerensis, MNBH GAD70).
Finally, the forelimb in the skeletal silhouette drawing is ~30% longer than that in our digital reconstruction (Figure 9A). The neotype is the only associated specimen of S. aegyptiacus preserving bones from the forelimb (partial manual digit II). The preserved manual phalanges are slender with deeply cleft distal condyles, which allows reference of additional phalanges of similar form from the Kem Kem Group (Figure 1D). Our reconstruction of the manus is based on a recently described forelimb of the close relative Irritator (=Angaturama; Machado and Kellner, 2009; Aureliano et al., 2018). The proportions of more proximal forelimb segments and the pectoral girdle are based on the holotypic specimens of Baryonyx and Suchomimus. The forelimb in S. aegyptiacus is robust and long relative to other non-avian theropods, although considerably shorter than in some previous reconstructions (Ibrahim et al., 2014).
The longer presacral proportions, deeper torso, and longer forelimb of the skeletal reconstruction and flesh model used by the aquatic hypothesis cantilever show significant additional body mass anterior to the hip joint. That additional front-loading appears to be the main factor generating their mid trunk location for CM (Ibrahim et al., 2020b), which constitutes the basis for regarding S. aegyptiacus as a quadruped on land (Ibrahim et al., 2014).
Flesh reconstruction of axial musculature
To estimate the volume of axial musculature in S. aegyptiacus (Figure 10), we referenced CT-based studies on the ostrich (Struthio; Wedel, 2003; Snively and Russell, 2007; Persons et al., 2020) and alligator (Alligator; Cong et al., 1998; Mallison et al., 2015). To estimate caudal muscle mass, we used CT scans of various reptiles including the sail-backed basilisk lizard, Basiliscus plumifrons (Figure 11, Tables 2–5).
Table 2. Axial muscle area in the crested basilisk.
Location | Total area | Epaxial area | Hypaxial area | ||
---|---|---|---|---|---|
mm2 | mm2 | % total | mm2 | % total | |
Anterior neck (C2) | 180.4 | 83.9 | 46.5 | 96.5 | 53.5 |
Mid neck (C3) | 139.7 | 54.9 | 39.3 | 84.8 | 60.7 |
Posterior neck (C4-D1) | 202.1 | 69.8 | 34.7 | 132.3 | 65.3 |
Mid dorsal (D12) | 212.0 | 60.0 | 28.3 | 152.0 | 71.7 |
Basal tail (CA4) | 434.0 | 153.8 | 35.4 | 280.2 | 64.6 |
Anterior tail (CA10, last transverse process) | 221.7 | 63.5 | 28.6 | 158.2 | 71.4 |
Mid tail (CA15) | 97.8 | 29.8 | 29.8 | 68.0 | 70.2 |
Table 3. Axial muscle and transverse process length in the tail of the crested basilisk.
Location | Measurement | Total(mm) | % bone and muscle | % muscle only |
---|---|---|---|---|
CA4 | Transverse process width | 16.8 | 62.9 | 37.1 |
Total width | 26.7 | |||
CA10 | Transverse process width | 8.1 | 57 | 43.0 |
Total width | 14.2 | |||
CA15 | Centrum width | 3.5 | 36.8 | 63.2 |
Total width | 9.5 |
Table 4. Epaxial muscle height and neural spine height in the tail of the crested basilisk.
Location | Measurement | Total(mm) | % neural spine adjacent to muscle | % neural spine above muscle |
---|---|---|---|---|
CA4 | Neural spine height | 18.4 | 70.7 | 29.3 |
Epaxial mm height | 13.0 | |||
CA10 | Neural spine height | 33.6 | 32.1 | 67.9 |
Epaxial mm height | 10.8 | |||
CA15 | Neural spine height | 34.5 | 23.2 | 76.8 |
Epaxial mm height | 8.0 |
Table 5. Hypaxial muscle depth and chevron length in the tail of the crested basilisk.
Location | Measurement | Total(mm) | % chevron length | % muscle below chevron |
---|---|---|---|---|
CA4 | Chevron depth | 9.0 | 52.6 | 47.4 |
Hypaxial depth | 17.1 | |||
CA10 | Chevron depth | 7.1 | 67.0 | 33.0 |
Hypaxial depth | 10.6 | |||
CA15 | Chevron depth | 4.8 | 67.6 | 32.4 |
Hypaxial depth | 7.1 |
For epaxial muscle mass in S. aegyptiacus, we estimated its vertical extent as twice centrum height, measuring upward from the base of the neural spine. The transverse width of epaxial musculature was estimated to be a little less than that of the hypaxial muscles, widest ventrally and tapering to the midline dorsally. For hypaxial muscle mass in S. aegyptiacus, we estimated its vertical depth at approximately twice chevron length in the anterior tail and 1.5 times chevron length in mid and posterior portions of the tail. We estimated the transverse width of hypaxial muscles as twice the length of the transverse processes. CT cross-sections of extant reptiles show that considerable muscle mass is present beyond the distal end of caudal transverse processes in anterior and middle portions of the tail (Figure 10).
Several cross-sections from Basiliscus plumifrons (crested basilisk) provided valuable insights on the distribution of axial muscles in a lizard with a dorsal-to-caudal sail (Figure 11, Tables 2–5). Epaxial musculature in the trunk and tail comprises less than one-third of total axial muscle volume (Table 2). Caudal neural spines project beyond the epaxial musculature to support the sail to a greater extent in mid and distal portions of the tail. At the base of the tail (CA4), approximately one-third (29.3%) of the neural spine projects dorsally supporting the sail. At mid tail (CA15), approximately three-quarters (76.8%) of the neural spine projects dorsally supporting the sail. The hypaxial musculature extends well below the distal end of the chevrons. At the base of the tail (CA4), the chevron lies internal to approximately one-half (52.6%) of hypaxial muscle depth, with the remainder (47.4%) distal to the end of the chevon. Farther along the tail (CA10-15), the chevrons are proportionately longer, supporting approximately two-thirds (67%) of hypaxial muscle depth with approximately one-third of hypaxial musculature beyond the distal end of the chevron. These cross-sections confirm the presence of considerable muscle mass ventral to the distal end of the chevrons in anterior through mid portions of the tail (Figures 10 and 11).
Flesh model density partitions, dimensions, and properties
The digital skeletal model was wrapped in flesh (using ZBrush) guided by recent documentation of muscle mass in CT scans of various modern analogs (Wedel, 2003; Snively and Russell, 2007; Mallison et al., 2015; Persons et al., 2020; Díez Díaz et al., 2020). We inserted anatomically shaped and -positioned air spaces (pharynx-trachea, paraxial air sacs, lungs) of optional volumes (minimum-lizard, medium-crocodylian, maximum-avian) within the head, neck, and torso (Figure 2C). For additional measurements, we added a ‘mesh’ over the flesh model (Henderson, 1999; Figure 2D).
We divided the flesh model into six parts (axial body-presacral, axial-caudal, dorsal-to-caudal sail, forelimbs, hindlimbs, lungs) in order to assign appropriate densities (Table 6). Densities were assigned to body parts based on their estimated composition, using values for tissues ranging from fat (900 g/l) to compact bone (2000 g/l). The average whole-body density for S. aegyptiacus, 833 g/l (Table 6) compares favorably to whole-body density estimates for various non-avian dinosaurs (800–900 g/l). We have compiled various functional dimensions of the adult flesh model (Table 7), and we divided the flesh model into 10 body parts, for which we list volumes and external surface areas (excluding cut surfaces) (Table 8).
Table 6. Density, volume, and mass in the flesh model of S. aegyptiacus.
No. | Body partition | Average density(kg/m3) | % of axial volume without sail | Mass(kg) |
---|---|---|---|---|
1 | Whole body | 833 | — | 7390 |
2 | Axial body (excluding lung/sail) |
788 | 100.0 | 5794 |
3 | Axial head-trunk (not lung/sail/tail) |
850 | 64.8 | 3209 |
4 | Axial tail (not sail) |
1000 | 35.2 | 2585 |
5 | Forelimb (paired) | 1050 | 3.8 | 108 |
6 | Hind limb (paired) | 1050 | 11.1 | 590 |
7 | Dorsocaudal sail | 1196 | 8.5 | 441 |
8 | Lungs | 0 | 12.5 | 0 |
Table 7. Flesh model functional dimensions in S. aegyptiacus.
No. | Dimension | Measure (m) |
---|---|---|
1 | Total body length (sculling pose) | 13.53 |
2 | Body length minus tail (sculling pose) | 6.92 |
3 | Head length | 1.57 |
4 | Neck length (sculling pose) | 2.18 |
5 | Trunk depth (mid trunk, without sail) | 1.28 |
6 | Trunk sail depth (mid trunk) | 1.93 |
7 | Trunk sail length (maximum at base) | 3.53 |
8 | Tail length | 6.61 |
9 | Tail depth at base | 1.38 |
10 | Tail depth at midpoint | 0.97 |
11 | Tail depth at distal end | 0.87 |
12 | Tail depth average | 1.08 |
13 | Forelimb length (straightened) | 1.85 |
14 | Hind limb length (straightened) | 2.88 |
Table 8. Flesh model volume and surface area in S. aegyptiacus.
No. | Body part | Volume (m3) | Surface area (m2) |
---|---|---|---|
1 | Whole body | 8.94 | 54.06 |
2 | Body above waterline (floating) | 1.65 | 22.58 |
3 | Body below waterline (floating) | 7.27 | 31.38 |
4 | Head | 0.21 | 2.23 |
5 | Neck | 0.78 | 4.37 |
6 | Trunk | 4.01 | 11.44 |
7 | Trunk sail (both sides, external edge) | 0.40 | 10.06 |
8 | Forelimb (both) | 0.24 | 3.86 |
9 | Hind limb (both) | 0.45 | 5.29 |
10 | Tail | 2.81 | 16.56 |
11 | Tail with axial muscle | 2.71 | 13.27 |
12 | Tail sail only | 0.10 | 3.17 |
13 | Airspace-minimum (~4% body volume) |
0.37 | 4.86 |
14 | Airspace-medium (~8% body volume) |
0.67 | 6.63 |
15 | Airspace-maximum (~12% body volume) |
1.08 | 8.66 |
We registered CM as the horizontal distance from the apex of the acetabulum (x-coordinate) and the vertical distance from the ground surface under the sole of the foot (y-coordinate) (Table 9, no. 4). This is the fourth estimation of CM for S. aegyptiacus, and we argue here the most accurate. We prefer a measure from the acetabulum rather than the distal tail tip, which as in S. aegyptiacus is often a matter of speculation given the rarity of completely preserved caudal columns (Hone, 2012). For the acetabulum, we recommend using its ‘apex’ rather than its ‘cranial end’ (Ibrahim et al., 2020b) for three reasons. First, the apex of the acetabulum is a more easily recognized landmark than the poorly defined anterior edge (or rim) of the acetabulum. Second, the apex rather than the ‘cranial end’ of the acetabulum is a more functionally intuitive point from which to measure CM, given its proximity to the rotational point for body mass centered over the hind limbs. And third, the dorsal (proximal) articular end of the femoral head is close to the apex of the acetabulum, and so the length of the femur and the distance that CM lies farther forward can be directly compared (CM located anteriorly beyond femoral length excludes stable bipedal posture with a relatively horizontal dorsosacral column).
Table 9. Center of mass (CM) calculations for S. aegyptiacus.
No. | Author/result | x-origin | x | y | Notes |
---|---|---|---|---|---|
1 | Ibrahim et al., 2014; quadruped | Hip joint | >81 | – | Based on an adult flesh model, no coordinates given, CM shown graphically under D10 and said to be anterior to hip/knee joints at a distance greater than femur length (MeshLab calculation error) |
2 | Henderson, 2018; biped | Tip of tail | 8,850 | 100 | Based on an 3D mesh model based on the adult skeletal model of Ibrahim et al., 2014 with estimated length 16 m long; y-coordinate origin is ‘lowest point of axial body’ |
3 | Ibrahim et al., 2020b; quadruped | ‘Cranial rim’ of acetabulum | 72.5–82.5 (adult = 95.7–108.9) |
–81 (adult: 106.9) |
Based on a flesh model of the subadult neotype with femur length of 62.5 cm (actual 61.0 cm); y-coordinate measures to substrate |
4 | This paper; biped | Apex of the acetabulum | 15.3 | –240 | Based on an adult flesh model with avian-style internal air spaces and femur length of 81.0 cm; y-coordinate measures to substrate |
With avian-like air space (‘maximum’), CM is positioned only 15.3 cm anterior to the apex of the acetabulum and clearly over the pedal phalanges of the foot for a bipedal stance (Table 10). The smallest air space option modeled on lizards (‘minimum,’ only 4% of body volume) generates the heaviest torso and displaces CM anteriorly 13.2 cm to a distance of 28.5 cm from the apex of the acetabulum (Table 10). In this location, CM is still ~12 cm short of the midpoint along the length of the femur (~40 cm; femoral length is 81 cm in adult S. aegyptiacus). In this worst-case scenario regarding internal air volume, CM is still positioned over the pedal phalanges of the hind limb. Our flesh model does not support an obligatory quadrupedal pose on land for S. aegyptiacus.
Table 10. Estimated internal air space in S. aegyptiacus.
No. | Air space option | Part of whole-body volume (%) | Mean whole-body density(g/l) | BM(kg) | CM x-coordinate(cm) |
---|---|---|---|---|---|
1 | Minimum (lizard-like) |
4.0 | 909 | 8013 | 28.5 |
2 | Medium (croc-like) |
8.0 | 875 | 7716 | 23.2 |
3 | Maximum (bird-like) |
12.5 | 833 | 7390 | 15.3 |
Acknowledgements
We thank A Resetar, J Mata, and D Coldren of The Field Museum, R Carmichael of the Wildlife Center and R Bavrisha of the Chicago Herpetological Society for access to recent preserved and live reptile specimens, MorphoSource, FMNH, UMMZ, UF, and KU for access to and archiving of CT scans, R Shonk and A Schulte for digital modeling, E Fitzgerald for fossil preparation, J Mallon for photography, and J Schwartz, E Saitta, E Johnson-Ransom, DB Dutheil, SW Evers, E Snively, D Hone, and T Holtz for comments on the manuscript. This research was supported by Bob and Ellen Vladem and SC Johnson.
Appendix 1
Long bone infilling in S. aegyptiacus
In S. aegyptiacus, the medullary cavities in the long bones of the hind limb are reduced in diameter or infilled altogether by non-pachystotic bone. This condition is unusual among non-avian dinosaurs and was initially thought to be an adaptation for decreasing buoyancy (Ibrahim et al., 2014; Fabbri et al., 2022). Enhanced bone strength is an alternative explanation for solid hind limb long bones in S. aegyptiacus, a very large bipedal theropod with reduced hind limbs. Similar long bone infilling occurs in other large-bodied bipedal and quadrupedal dinosaurs and mammals (Vanderven et al., 2014; Houssaye et al., 2016).
To better understand this alternative explanation, we compare the increase in strength of a femur with a solid shaft compared to one of identical size with a hollow shaft using the section modulus (SM) as an indicator of the resistance to bending (Farlow et al., 1995). For a solid circular cross-section, the SM is given by , where R is the outer radius. When R has a value 1.0, SM is , or 0.785 m3. The SM for a cylinder with a hollow core is calculated by subtracting the SM of an inner cylinder comprising the hollowed space from that of the outer cylinder.
An inner radius of 0.5 generates a hollow cylinder that decreases the solid cylinder volume with 25% and generates an SM of = . This is a reduction of ~13% of SM. However, many theropods have hollow cores within long bones that comprise 50% or more of the volume of the long bone. For a hollow core equal to 50% of outer cylinder volume, the inner radius is 0.707. The SM, calculated by subtracting SM for a cylinder of radius 0.707 from the full cylinder of radius 1.0, is , or , a reduction of ~35% of the SM of a solid cylinder.
Thus, infilling of hind limb bones in S. aegyptiacus may have increased bending strength by as much as 35%. The femur in S. aegyptiacus, in particular, may have been subjected to substantial bending forces. The hypertrophied attachment flange for the caudofemoralis muscle occupies almost one-third of the length of the femoral shaft.
Appendix 2
Extant and extinct comparative materials
We used references in the literature, extant amphibian and reptile specimens, and a mosasaur to estimate muscle mass in the flesh reconstruction of S. aegyptiacus and to measure caudal centrum proportions along the tail (Figures 2 and 4D, Appendix 2—table 1 and Appendix 2—table 2).
Appendix 2—table 1. Extant newt and squamate specimens used for muscle mass estimation and for logging centrum proportions along the tail.
Specimen no. | Taxon | Sex | Type | Purpose |
---|---|---|---|---|
FMNH 84926 | Triturus cristatus | Male | Wet | Caudal centrum ratios, muscle mass estimation |
FMNH 57512 | Intellagama lesueurii | Male | Wet | Muscle mass estimation |
FMNH 22389 | Intellagama lesueurii | Male | Skeleton | Caudal centrum ratios, muscle mass estimation |
KU 314941 | Hydrosaurus amboinensis | Unknown; low neural spines (female/ immature male) | Wet | Caudal centrum ratios |
FMNH 52698 | Hydrosaurus pustulatus | Male | Wet | Muscle mass estimation |
FMNH 236131 | Hydrosaurus pustulatus | Unknown; low neural spines (female/ immature male) | Skeleton | Muscle mass estimation |
FMNH 112993 | Basiliscus plumifrons | Male | Wet | Muscle mass estimation |
FMNH 257162 | Basiliscus plumifrons | Male | Skeleton | Additional high-resolution visualization |
UMMZ 121461 | Basiliscus basiliscus | Male | Wet | Caudal centrum ratios |
UF 41558 | Amblyrhynchus cristatus | Unknown | Wet | Caudal centrum ratios |
FMNH 22042 | Amblyrhynchus cristatus | Unknown;?male (tallest caudal neural spines in FMNH collection) | Skeleton | Muscle mass estimation |
UF 21461 | Alligator mississippiensis | Unknown; juvenile | Wet | X-ray image of caudal centra in tail; caudal centrum ratios |
Appendix 2—table 2. Caudal centrum ratios along the tail in S. aegyptiacus, Mosasaurus, and extant semiaquatic amphibians and reptiles (Figure 4D).
L-H ratios | Relative distance (caudal #/total # of caudals) | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
CA # | Spino. | Mosa. | Ambly. | Alli. | Basil. | Hydro. | Trit. | Intel. | Spino. | Mosa. | Ambly. | Alli. | Basil. | Hydro. | Trit. | Intel. |
1 | 0.73 | 1.40 | 1.14 | 1.52 | 1.25 | 3.26 | 1.60 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 | 0.02 | |
2 | 1.56 | 1.11 | 1.92 | 1.50 | 3.78 | 2.21 | 0.04 | 0.03 | 0.04 | 0.05 | 0.04 | 0.04 | 0.05 | 0.04 | ||
3 | 1.55 | 1.05 | 2.05 | 1.97 | 3.18 | 2.48 | 0.06 | 0.04 | 0.06 | 0.07 | 0.06 | 0.05 | 0.08 | 0.06 | ||
4 | 0.84 | 1.88 | 1.18 | 2.30 | 2.05 | 3.20 | 2.73 | 0.08 | 0.05 | 0.09 | 0.10 | 0.08 | 0.07 | 0.11 | 0.08 | |
5 | 1.86 | 1.22 | 2.44 | 2.14 | 2.88 | 2.78 | 0.10 | 0.07 | 0.11 | 0.12 | 0.10 | 0.09 | 0.14 | 0.10 | ||
6 | 1.96 | 1.33 | 2.50 | 2.14 | 3.08 | 2.83 | 0.12 | 0.08 | 0.13 | 0.15 | 0.12 | 0.11 | 0.16 | 0.13 | ||
7 | 1.12 | 1.06 | 2.06 | 1.38 | 2.55 | 2.26 | 3.05 | 2.98 | 0.14 | 0.09 | 0.15 | 0.17 | 0.14 | 0.13 | 0.19 | 0.15 |
8 | 1.15 | 1.03 | 2.10 | 1.43 | 2.72 | 2.17 | 3.11 | 2.99 | 0.16 | 0.11 | 0.17 | 0.20 | 0.16 | 0.14 | 0.22 | 0.17 |
9 | 0.95 | 2.13 | 1.49 | 2.87 | 2.41 | 3.07 | 3.22 | 0.18 | 0.12 | 0.19 | 0.22 | 0.18 | 0.16 | 0.24 | 0.19 | |
10 | 0.97 | 2.19 | 1.52 | 2.89 | 2.45 | 2.90 | 3.26 | 0.20 | 0.14 | 0.21 | 0.24 | 0.20 | 0.18 | 0.27 | 0.21 | |
11 | 0.98 | 2.29 | 1.53 | 3.14 | 2.34 | 2.95 | 3.17 | 0.22 | 0.15 | 0.23 | 0.27 | 0.22 | 0.20 | 0.30 | 0.23 | |
12 | 0.93 | 2.37 | 1.67 | 2.94 | 2.50 | 3.17 | 3.28 | 0.24 | 0.16 | 0.26 | 0.29 | 0.24 | 0.21 | 0.32 | 0.25 | |
13 | 1.24 | 1.07 | 2.57 | 1.62 | 3.27 | 2.48 | 2.73 | 3.34 | 0.26 | 0.18 | 0.28 | 0.32 | 0.25 | 0.23 | 0.35 | 0.27 |
14 | 1.21 | 1.04 | 2.52 | 1.65 | 3.35 | 2.43 | 2.77 | 3.21 | 0.28 | 0.19 | 0.30 | 0.34 | 0.27 | 0.25 | 0.38 | 0.29 |
15 | 1.06 | 2.59 | 1.74 | 3.49 | 2.64 | 2.85 | 3.51 | 0.30 | 0.20 | 0.32 | 0.37 | 0.29 | 0.27 | 0.41 | 0.31 | |
16 | 0.91 | 2.67 | 1.72 | 3.46 | 2.52 | 2.95 | 3.64 | 0.32 | 0.22 | 0.34 | 0.39 | 0.31 | 0.29 | 0.43 | 0.33 | |
17 | 1.43 | 0.92 | 2.74 | 1.91 | 3.55 | 2.94 | 2.65 | 3.52 | 0.34 | 0.23 | 0.36 | 0.41 | 0.33 | 0.30 | 0.46 | 0.35 |
18 | 1.33 | 0.95 | 2.80 | 1.81 | 3.66 | 2.82 | 3.29 | 3.73 | 0.36 | 0.24 | 0.38 | 0.44 | 0.35 | 0.32 | 0.49 | 0.38 |
19 | 0.99 | 2.91 | 1.89 | 3.73 | 3.03 | 3.14 | 3.61 | 0.38 | 0.26 | 0.40 | 0.46 | 0.37 | 0.34 | 0.51 | 0.40 | |
20 | 1.37 | 0.98 | 2.77 | 1.97 | 3.89 | 2.85 | 2.70 | 3.50 | 0.40 | 0.27 | 0.43 | 0.49 | 0.39 | 0.36 | 0.54 | 0.42 |
21 | 0.97 | 0.99 | 2.94 | 1.89 | 3.91 | 2.89 | 2.82 | 3.73 | 0.42 | 0.28 | 0.45 | 0.51 | 0.41 | 0.38 | 0.57 | 0.44 |
22 | 1.40 | 0.98 | 2.99 | 1.95 | 3.99 | 2.87 | 3.16 | 3.69 | 0.44 | 0.30 | 0.47 | 0.54 | 0.43 | 0.39 | 0.59 | 0.46 |
23 | 1.38 | 1.02 | 2.99 | 2.12 | 4.01 | 2.82 | 3.27 | 3.93 | 0.46 | 0.31 | 0.49 | 0.56 | 0.45 | 0.41 | 0.62 | 0.48 |
24 | 1.32 | 0.92 | 3.00 | 2.21 | 3.74 | 2.96 | 2.92 | 3.90 | 0.48 | 0.32 | 0.51 | 0.59 | 0.47 | 0.43 | 0.65 | 0.50 |
25 | 1.41 | 0.88 | 3.05 | 2.25 | 4.40 | 3.29 | 3.22 | 3.96 | 0.50 | 0.34 | 0.53 | 0.61 | 0.49 | 0.45 | 0.68 | 0.52 |
26 | 1.36 | 0.90 | 3.05 | 2.49 | 4.14 | 3.12 | 3.63 | 3.72 | 0.52 | 0.35 | 0.55 | 0.63 | 0.51 | 0.46 | 0.70 | 0.54 |
27 | 1.35 | 0.93 | 3.02 | 2.63 | 4.25 | 3.31 | 3.45 | 3.99 | 0.54 | 0.36 | 0.57 | 0.66 | 0.53 | 0.48 | 0.73 | 0.56 |
28 | 1.15 | 0.90 | 3.24 | 2.79 | 3.69 | 3.13 | 3.36 | 4.03 | 0.56 | 0.38 | 0.60 | 0.68 | 0.55 | 0.50 | 0.76 | 0.58 |
29 | 1.44 | 0.83 | 3.27 | 2.70 | 4.37 | 3.25 | 3.03 | 4.14 | 0.58 | 0.39 | 0.62 | 0.71 | 0.57 | 0.52 | 0.78 | 0.60 |
30 | 1.29 | 0.89 | 3.31 | 2.99 | 3.97 | 3.18 | 3.11 | 4.06 | 0.60 | 0.41 | 0.64 | 0.73 | 0.59 | 0.54 | 0.81 | 0.63 |
31 | 1.34 | 0.97 | 3.22 | 3.10 | 3.82 | 3.37 | 3.23 | 3.77 | 0.62 | 0.42 | 0.66 | 0.76 | 0.61 | 0.55 | 0.84 | 0.65 |
32 | 1.42 | 0.82 | 3.54 | 3.21 | 4.56 | 3.48 | 3.27 | 4.22 | 0.64 | 0.43 | 0.68 | 0.78 | 0.63 | 0.57 | 0.86 | 0.67 |
33 | 1.36 | 0.94 | 3.44 | 3.32 | 4.76 | 3.46 | 2.19 | 3.86 | 0.66 | 0.45 | 0.70 | 0.80 | 0.65 | 0.59 | 0.89 | 0.69 |
34 | 1.45 | 0.88 | 3.31 | 3.45 | 4.87 | 3.48 | 1.75 | 4.25 | 0.68 | 0.46 | 0.72 | 0.83 | 0.67 | 0.61 | 0.92 | 0.71 |
35 | 0.89 | 3.07 | 3.92 | 5.09 | 3.59 | 1.89 | 4.11 | 0.70 | 0.47 | 0.74 | 0.85 | 0.69 | 0.63 | 0.95 | 0.73 | |
36 | 0.89 | 3.25 | 3.72 | 5.19 | 3.68 | 2.70 | 4.00 | 0.72 | 0.49 | 0.77 | 0.88 | 0.71 | 0.64 | 0.97 | 0.75 | |
37 | 1.96 | 0.82 | 3.50 | 3.90 | 5.54 | 3.71 | 1.98 | 4.21 | 0.74 | 0.50 | 0.79 | 0.90 | 0.73 | 0.66 | 1.00 | 0.77 |
38 | 0.82 | 3.31 | 2.96 | 5.50 | 3.65 | 4.17 | 0.76 | 0.51 | 0.81 | 0.93 | 0.75 | 0.68 | 0.79 | |||
39 | 0.82 | 3.22 | 3.19 | 5.94 | 3.82 | 4.13 | 0.78 | 0.53 | 0.83 | 0.95 | 0.76 | 0.70 | 0.81 | |||
40 | 0.82 | 3.19 | 3.54 | 5.93 | 3.71 | 3.95 | 0.80 | 0.54 | 0.85 | 0.98 | 0.78 | 0.71 | 0.83 | |||
41 | 1.74 | 0.77 | 3.07 | 3.06 | 5.95 | 3.91 | 4.45 | 0.82 | 0.55 | 0.87 | 1.00 | 0.80 | 0.73 | 0.85 | ||
42 | 0.79 | 3.25 | 5.99 | 4.06 | 4.31 | 0.84 | 0.57 | 0.89 | 0.82 | 0.75 | 0.88 | |||||
43 | 0.72 | 3.42 | 6.22 | 3.99 | 4.67 | 0.86 | 0.58 | 0.91 | 0.84 | 0.77 | 0.90 | |||||
44 | 0.75 | 3.29 | 6.73 | 4.32 | 4.80 | 0.88 | 0.59 | 0.94 | 0.86 | 0.79 | 0.92 | |||||
45 | 0.74 | 3.16 | 6.64 | 4.24 | 4.59 | 0.90 | 0.61 | 0.96 | 0.88 | 0.80 | 0.94 | |||||
46 | 0.80 | 2.63 | 6.00 | 4.33 | 4.56 | 0.92 | 0.62 | 0.98 | 0.90 | 0.82 | 0.96 | |||||
47 | 0.83 | 2.53 | 5.82 | 4.42 | 5.31 | 0.94 | 0.64 | 1.00 | 0.92 | 0.84 | 0.98 | |||||
48 | 0.90 | 6.61 | 4.66 | 3.27 | 0.96 | 0.65 | 0.94 | 0.86 | 1.00 | |||||||
49 | 0.88 | 6.16 | 4.61 | 0.98 | 0.66 | 0.96 | 0.88 | |||||||||
50 | 0.98 | 6.49 | 4.39 | 1.00 | 0.68 | 0.98 | 0.89 | |||||||||
51 | 0.95 | 5.49 | 4.29 | 0.69 | 1.00 | 0.91 | ||||||||||
52 | 0.83 | 4.39 | 0.70 | 0.93 | ||||||||||||
53 | 0.91 | 4.52 | 0.72 | 0.95 | ||||||||||||
54 | 0.91 | 4.53 | 0.73 | 0.96 | ||||||||||||
55 | 0.88 | 4.18 | 0.74 | 0.98 | ||||||||||||
56 | 0.96 | 3.97 | 0.76 | 1.00 | ||||||||||||
57 | 0.89 | 0.77 | ||||||||||||||
58 | 1.04 | 0.78 | ||||||||||||||
59 | 0.96 | 0.80 | ||||||||||||||
60 | 0.94 | 0.81 | ||||||||||||||
61 | 1.08 | 0.82 | ||||||||||||||
62 | 0.99 | 0.84 | ||||||||||||||
63 | 0.86 | 0.85 | ||||||||||||||
64 | 0.88 | 0.86 | ||||||||||||||
65 | 1.06 | 0.88 | ||||||||||||||
66 | 1.03 | 0.89 | ||||||||||||||
67 | 0.96 | 0.91 | ||||||||||||||
68 | 1.02 | 0.92 | ||||||||||||||
69 | 1.01 | 0.93 | ||||||||||||||
70 | 0.99 | 0.95 | ||||||||||||||
71 | 1.00 | 0.96 | ||||||||||||||
72 | 1.01 | 0.97 | ||||||||||||||
73 | 1.01 | 0.99 | ||||||||||||||
74 | 0.98 | 1.00 |
Appendix 3
Crocodylian foot paddle size and scaling
We measured forefoot, hind foot, and tail areas in five species of extant crocodylians by photographing appendages of individuals in captivity (Appendix 3—table 1).
Appendix 3—table 1. Forefoot, hind foot, and tail area and other data in five species of extant crocodylians.
No. | Total length (cm) | Snout-vent length(cm) | Skull length(cm) | Post skull width (cm) | Tail length(cm) | Mass (kg) | Sex(m, f) | Age est.(year) | Hand(cm) | Foot(cm) | Tail(cm) |
---|---|---|---|---|---|---|---|---|---|---|---|
1 | 65.0 | 32.0 | 9.0 | 5.5 | 35.5 | 1.15 | f | 2 | 5.7 | 9.8 | 90.9 |
2 | 69.0 | 36.0 | 9.8 | 5.6 | 35.0 | 1.05 | f | 12 | 7.0 | 13.2 | 102.8 |
3 | 85.0 | 42.5 | 11.5 | 6.8 | 43.0 | 1.95 | f | 3 | 10.9 | 23.6 | 114.1 |
4 | 105.4 | 52.2 | 14.0 | 8.5 | 54.5 | 3.65 | f | 4 | 18.3 | 39.9 | 267.7 |
5 | 154.0 | 78.0 | 22.0 | 14.3 | 77.5 | 15.45 | m | 12 | 46.2 | 93.3 | 655.2 |
6 | 167.0 | 85.0 | 21.8 | 15.5 | 86.8 | 22.95 | m | ? | 51.4 | 96.0 | 717.9 |
7 | 211.5 | 104.5 | 25.3 | 18.5 | 108.0 | 39.10 | m | 23 | 69.5 | 146.5 | 1372.5 |
8 | 86.3 | 47.6 | 12.6 | 8.5 | 37.0 | 2.85 | f | 5 | 8.4 | 19.8 | 172.1 |
9 | 75.5 | 38.0 | 8.6 | 6.3 | 38.0 | 1.55 | f | 3 | 5.8 | 18.3 | 141.6 |
10 | 108.8 | 55.5 | 14.0 | 10.0 | 55.5 | 4.95 | f | 5 | 12.1 | 29.6 | 272.1 |
11 | 68.2 | 33.3 | 9.4 | 6.2 | 32.4 | 1.15 | f | 4 | 6.3 | 17.1 | 99.0 |
Appendix 4
Inland fossils referable to Spinosaurus
Inland fossils referable to Spinosaurus sp. were discovered in 1970 at the locality Gara Samani in the Béchar Basin of Algeria (Appendix 4—table 1). The most complete specimen is a snout (MNHN SAM 124) comparable in size to subadult S. aegyptiacus and eventually described as S. maroccanus (Taquet and Russell, 1998). We consider its specific status in doubt. S. maroccanus is based on isolated vertebrae from the Kem Kem Group in Morocco (Russell, 1996) and has recently been reduced to a junior synonym of S. aegyptiacus (Ibrahim et al., 2020a).
Appendix 4—table 1. Fossil material referable to Spinosaurus from inland basins in Algeria and Niger. D, dorsal.
Specimens | Description |
---|---|
MNHN SAM 124 | Snout with preserved length of 62 cm (Gara Samani, Béchar Basin, Algeria) compared to ~1 m for adult snout MSNM V4047 |
MNHN SAM 125 | Premaxilla fragment (Gara Samani, Béchar Basin, Algeria) |
MNHN SAM 125–8 | Two cervical vertebra, one dorsal vertebra (Gara Samani, Béchar Basin, Algeria) |
MNBH IGU11 | ~D1 short, very low oval centrum with low parapophysis, very strong ventral keel (In Abangharit, Iullumeden Basin, Niger) |
MNBH EGA1 | Both maxillae and a portion of the alveolar edge of the right dentary with tooth roots within alveoli (Égaro North, Chad Basin, Niger) |
MNBH EGA2 | Isolated tooth with root (Égaro North, Chad Basin, Niger) |
Inland fossils referable to Spinosaurus sp. come from two areas of outcrop of the Cenomanian-age Echkar Formation in Niger (Appendix 4—table 1). The first locality is near In Abangharit, which is northeast of Agadez and yielded isolated teeth and an anterior dorsal centrum initially referred to Carcharodontosaurus iguidensis (Appendix 4—figure 1). Reassigned to Spinosaurus sp., this vertebra is very close in form to the first dorsal centrum of S. aegyptiacus from Morocco (Ibrahim et al., 2020a: Fig. 128A–D) and Egypt (Stromer, 1934: pl. 1, Fig. 2), although differences suggest it may pertain to a distinct species. For the time being, reference is made only to the genus Spinosaurus.
In 2019, a fragmentary snout preserving most of the right and left maxillae of Spinosaurus sp. was recovered from a second locality southeast of Agadez also in the Echkar Formation (Figure 7B). The material also includes a partial right dentary (MNBH EGA1) and subconical crowns and long tapering roots (MNBH EGA2). The jaw bones, which closely resemble S. aegyptiacus although possibly a new species, are comparable in size to the subadult holotypic and neotypic skeletons, or about 75% of the size of the large snout recovered in Morocco (Dal Sasso et al., 2005). They were found in overbank deposits near the remains of rebbachisaurid and titanosaurian sauropods and evidence of a vertebrate fauna common to Cenomanian sites across northern Africa (including Carcharodontosaurus, lungfish tooth plates, sawfish rostral teeth, etc.).
Appendix 5
Phylogenetic analysis of Spinosauridae
Phylogenetic analysis of Spinosauroidea
We conducted a phylogenetic analysis within Spinosauroidea to better understand the distribution and evolution of putative display and semiaquatic features. The analysis includes 15 terminal taxa (9 spinosaurids) scored for 120 characters (49% cranial, 51% postcranial), 25 of which are newly introduced (marked NEW). Using the phylogenetic analysis program TNT (Goloboff et al., 2008), we used a heuristic search using 1000 Wagner tree replicates with 10 tree bisection reconnections per replicate. This generated a single most-parsimonious tree of 129 steps with consistency and retention indices of 0.806 and 0.854, respectively (Appendix 5—figure 1).
Camarillasaurus cirugedae, originally described as a ceratosaur (Sánchez-Hernández and Benton, 2012), has been reinterpreted as a megalosauroid or possibly a spinosaurid (Rauhut et al., 2019; Malafaia et al., 2020; Samathi et al., 2021). Our analysis tentatively positions Camarillasaurus as the most basal spinosaurid, although additional remains of this fragmentary taxon are needed.
Recently, baryonychine material from the Wessex Formation on the Isle of Wight was described as two new genera, Ceratosuchops inferodios and Riperovenator milnerae (Barker et al., 2021). Both are close in form to S. tenerensis and differ from each other only in minor ways, with these disparities limited to overlapping bones (premaxillae, portions of the braincase). Some doubt remains regarding their association as single specimens as neither were found in association at single sites. The distinguishing features in the premaxillae (low narial tuberosity in one, not preserved in the other) and in the shape or depth of braincase fossae, the relative thickness of laminae and other minutiae of the braincase could well be due to individual variation (for Allosaurus fragilis, see Chure and Madsen, 1996). Several of these supposedly distinguishing features seem to occur on one or the other side of a well-preserved braincase of S. tenerensis (MNBH GAD43). The configuration of the orbital margin and form of the swollen postorbital brow in S. tenerensis (Appendix 5—figure 2) is similar to that in Riparovenator (it was cited as a distinguishing feature). We tentatively score the Wessex baryonychine material as a single taxon, C. inferodios, which resolves as the sister taxon to S. tenerensis (Appendix 5—figure 1).
With more spinosaurid remains coming to light in the decades before 2000, Sereno et al., 1998 split the group into sister clades, Baryonychinae and Spinosaurinae. Nearly all subsequent analyses including the current effort resolve this basal split (Allain et al., 2012; Carrano et al., 2012; Arden et al., 2019; Malafaia et al., 2020; Barker et al., 2021), with one outlier showing Baryonyx, Suchomimus, and Spinosaurinae as an unresolved polytomy (Sales and Schultz, 2017). Larger-scale analyses that incorporate theropods farther afield have not added any resolution or insights to an understanding of spinosauroid interrelationships. Although we use some of the relevant characters in those analyses (e.g., Carrano et al., 2012).
The holotypic specimen of Irritator shares important cranial apomorphies with Spinosaurus (an oval quadrate head, fewer and more spaced maxillary teeth, straight tooth crowns). Spinosaurid postcranial remains from the same formation yielding Irritator, in addition, share additional apomorphies with Spinosaurus (posterior dorsal neural spines anteroposteriorly shorter than centrum length, a proportionately lower iliac blade, and a ventrally directed iliac pubic peduncle). Ichthyovenator (Allain et al., 2012) and the recently published Vallibonavenatrix (Malafaia et al., 2020) are also recovered as spinosaurines on the basis of a few unambiguous postcranial synapomorphies (see below).
Character list
Skull
Snout (preorbital region of skull), length relative to antorbital fenestra length: less (0) or more (1) than three times. (Sereno et al., 1998, char. 7)
Jaws (premaxillae and dentary), anterior end, form: convergent (0); expanded into a premaxillary/ dentary rosette (1). (Sereno et al., 1998, char. 6)
Premaxilla, form of premaxilla-nasal suture: V-shaped (0); W-shaped (1). (Carrano et al., 2012, char. 5)
Premaxilla, external nares, proportions and position: shorter than premaxilla ventral to nares, angle between anterior and alveolar margins >75° (0); longer than body ventral to nares (1). (Carrano et al., 2012, char. 6)
Premaxillae, inter-premaxillary suture at maturity, form: open (0); fused (1). (Sereno et al., 1998, char. 10)
Premaxilla-maxilla articulation, form: scarf or butt joint (0); interlocking (1). (Sereno et al., 1998, char. 11)
Premaxilla-maxilla suture, lateral surface, subnarial foramen, shape: foramen (0); dorsoventrally directed channel (1). (Carrano et al., 2012, char. 10)
Premaxilla, ventral margin, shape in lateral view: straight to convex (0); concave (1). (Cau, 2018, char. 1485)
Premaxilla, lateral and dorsal surface, extensive pitting of neurovascular foramina: absent (0); present (1). (Barker et al., 2021, char. 1796)
Maxilla, anterior ramus, length relative to maximum depth: 70% (0); 100% or more (1). (Sereno et al., 1998, char. 1)
Maxilla, contribution to the narial fossa: no contribution (0); contributes partially or totally (1). (Modified from Longrich and Currie, 2009, char. 7)
Maxilla, antorbital fossa, width of ventral margin relative to depth of posterior ramus of maxilla: more (0) or less (1) than 30%. (Sereno et al., 1998, char. 40)
Maxilla, antorbital fossa, anterior margin: rounded (0); squared (1). (Carrano et al., 2012, char. 23)
Maxilla, subcircular depression in the anterior corner of the antorbital fossa: absent (0); present (1). (Sereno et al., 1998, char. 41)
Maxilla, anteromedial process, shape: fluted prong (0); plate (1). (Sereno et al., 1998, char. 12)
Maxilla, anteromedial process, anterior extension: as far as (0) or far anterior to (1) the anterior margin of the maxilla. (Sereno et al., 1998, char. 13)
Maxilla, antorbital fossa, size relative to orbit: larger (0); smaller (1). (Sereno et al., 1998, char. 9)
Maxilla, anteroventral margin, curvature: not curved (0); dorsomedially curved (1). (Modified from Cau, 2018, char. 731; Tykoski, 2005)
Nasal, posterior process, overlap of frontal in articulation: absent or limited (0); extensive, in particular medially, on almost or all the process dorsal surface (1). (Modified from Cau, 2018, char. 1500)
Jugal, posterior ramus, depth relative to orbital ramus: less (0); more (1). (Sereno et al., 1998, char. 43)
Lacrimal, anterior and ventral rami, angle of divergence: 75° to 90° (0); 30° to 45° (1). (Sereno et al., 1998, char. 15)
Lacrimal foramen, position relative to ventral process: near the base (0); at mid-height (1). (Sereno et al., 1998, char. 42)
Lacrimal, anterior ramus, length relative to ventral ramus: more (0) or less (1) than 65%. (Sereno et al., 1998, char. 2)
Postorbital, ventral process, cross section of distal half: subcircular (0); U-shaped (1). (Sereno et al., 1998, char. 44)
Postorbital, supraorbital shelf (boss) formed mostly by palpebral: absent (0); present (1). (Modified from Carrano et al., 2012, char. 61)
Frontal, postorbital facet, anterior depth: less than 2/5 facet length (0); more than 2/5 facet length (1). (Barker et al., 2021, Source data 2)
Frontal, shape of the lateral margin in dorsal view: describes a smooth transition between the anterior half and the postorbital process (0); an abrupt transition between the anterior half and the postorbital process (1). (Senter et al., 2010, char. 44)
Prefrontal, boss-like process: absent (0); present (1). (Barker et al., 2021, Source data 2)
Parietal, length: less than 3/4 of the frontal (0); subequal or more than 3/4 of the frontal (1). (Cau, 2018, char. 78)
Quadrate, head, shape: oval (0); subquadrate (1). (Sereno et al., 1998, char. 27)
Quadrate, foramen, size: foramen (0); broad fenestra (1). (Sereno et al., 1998, char. 28)
Quadrate, medial foramina adjacent to condyles: absent (0); present (1). (Carrano et al., 2012, char. 84)
Quadrate, foramen margin, placement: at mid-height or dorsal (0); ventral, close to mandibular condyles (1). (Modified from Loewen et al., 2013, char. 158)
Basisphenoid, width of the interbasipterygoidal web: thin; 40% of occipital condyle width or less (0); thick, more than 40% occipital condyle width (1). (Modified from Barker et al., 2021, Source data 1)
Basisphenoid, basipterygoid process, exposure of the ventral surface in lateral view: thick (0); reduced (1). (Barker et al., 2021, Source data 2)
Basisphenoid, basipterygoid process, shape of lateral margin in ventral view: flat or slightly concave (0); convex (1). (Barker et al., 2021, Source data 2)
Basioccipital, position of subcondylar recess: dorsoventrally tall, recess reaches the occipital condyle neck (0); ventrally restricted, surface directly below condyle convex (1). (Barker et al., 2021, Source data 2)
Basioccipital, width of subcondylar recess relative to occipital condyle width: narrow, 0.5 times or less (0); wide, greater than 0.5 times (1). (Modified from Barker et al., 2021, Source data 2)
Basioccipital, thick crests bordering subcondylar recess laterally: present (0); absent (1). (Barker et al., 2021, Source data 2)
Basioccipital, contribution to foramen magnum: large, exoccipitals widely separated (0); reduced, exoccipitals closely placed (1). (Barker et al., 2021, Source data 2)
Basioccipital, proportions relative to basisphenoid (measured along midline ventral to occipital condyle to interbasipterygoidal web), in posterior view: shorter (0); longer (1). (Barker et al., 2021, Source data 2)
Otoccipitals, angle of projection of paroccipital processes: posterolaterally (0); laterally or subhorizontal (1). (Barker et al., 2021, Source data 2)
Splenial foramen, size: small (0); large (1). (Sereno et al., 1998, char. 16)
Dentary, shape of anterior end in lateral view: blunt and unexpanded (0); dorsoventrally expanded, rounded and slightly upturned (1); squared off in lateral view via anteroventral process (2). (Carrano et al., 2012, char. 120)
Premaxilla and anterior dentary, interdental septa spacing: regular (0); alternate (alveoli result paired) (1). (Modified from Cau, 2018, char. 1614)
Dental
Teeth, distal, curvature: present, marked (0); reduced or non-curved (1). (Sereno et al., 1998, char. 35; modified after Hendrickx et al., 2019)
Teeth, maxillary and dentary, serrations: present (0); absent (1). (Sereno et al., 1998, char. 17)
Teeth, distal, midcrown cross-section: elliptical (0); circular (1). (Sereno et al., 1998, char. 36; modified after Hendrickx et al., 2019)
Teeth, distal, crown striations (flutes/apicobasal ridges): absent (0); present (1). (Sereno et al., 1998, char. 18; modified after Hendrickx et al., 2019)
Teeth, enamel ornamentation: absent (0); present (1). (Modified from Carrano et al., 2012, char. 143)
Teeth, enamel ornamentation type: extending as bands across labial and lingual tooth surfaces (0); pronounced marginal enamel wrinkles (1); pronounced deeply veined/anastomous texture (2). (Modified from Carrano et al., 2012, char. 143)
Teeth, basalmost root shape: broad (0); strongly tapered (1). (Sereno et al., 1998, char. 21)
Premaxilla, tooth count: 3–4 (0); 6–7 (1). (Sereno et al., 1998, char. 19)
Premaxillary tooth 1, size: slightly smaller (0) or much smaller (1) than crowns 2 and 3. (Sereno et al., 1998, char. 38)
Premaxilla, diastemata within the premaxillary rosette: narrow (0); broad (1). (Sereno et al., 1998, char. 39)
Maxillary teeth, mid-tooth spacing: adjacent (0); with intervening space/diastemata (1). (Sereno et al., 1998, char. 20)
Dentary, tooth count: up to 15 (0); ≥15 (1). (Sereno et al., 1998, char. 26)
Dentary teeth, spacing: adjacent (0); with intervening space (1). (Sereno et al., 1998, char. 37)
Paradental laminae: present (0); absent (1). (Sereno et al., 1998, char. 14)
Axial
Cervical vertebrae, middle, shape of anterior pneumatic foramina: round (0); anteroposteriorly elongate (1). (Carrano et al., 2012, char. 169)
Cervical vertebrae, posteriormost, ventral keel: absent or developed as a weak ridge (0); pronounced, around 1/3 the height of centrum and inset from lateral surfaces (1). NEW
Cervical vertebrae, prezygapophyseal facets, elongation related to width: as long as wide (0); longer than wide (1); wider than longer (2). NEW
Cervical vertebrae, middle and posterior centra width relative to centra height: taller than wide or round (0); wider than tall (1). NEW
Cervical vertebrae, anterior post-axial neural spines in lateral view: longer than tall (0); taller than long (1). (Cau, 2018, char. 212)
Dorsal vertebrae, anterior centra, depth of ventral keel relative to total centrum height: absent or less than ¼ (0); blade-shaped, more than ¼ (1). (Sereno et al., 1998, char. 22)
Dorsal vertebrae, anterior centra, ventral processes anterior to the keel (hypapophysis): poorly developed (0); strongly developed (1). (Modified by Cau, 2018, char. 225; from Rauhut, 2003)
Dorsal vertebrae, middle, centra length relative to height: 1.4 < times centrum height (0); ≥1.4 times centrum height (1). NEW
Dorsal vertebrae, anterior parapophyses, size: less (0) or more (1) than half-depth of anterior facet of centrum. (Cau, 2018, char. 1740)
Dorsal vertebrae, anterior centra, pneumatic foramen, size relative to parapophysis: larger or equal (0); smaller (1). NEW
Dorsal vertebrae, anterior, prezygapophyseal facets, elongation related to width: as long as wide (0); longer than wide (1); wider than longer (2). NEW
Dorsal vertebrae, mid-posterior, excavated prezygo-para-diapophyseal fossa (prpadf) delimited by the paradiapophyseal lamina (ppdl): absent (0); present (1). NEW (after Malafaia et al., 2020)
Dorsal vertebrae, middle and posterior centra, pneumatic foramina: absent (0); present (1). (Modified from Cau, 2018, char. 1350)
Dorsal vertebrae, height of neural spines relative to centrum height: low,<1.3× (0); moderate, 1.3–1.8× (1); tall, <1.8× (2). (Modified from Carrano et al., 2012, char. 193)
Dorsal vertebrae, posterior neural spines, basal webbing: absent (0); present (1). (Sereno et al., 1998, char. 24)
Dorsal vertebrae, posterior neural spines, accessory centrodiapophyseal lamina: absent (0); present (1). (Sereno et al., 1998, char. 25)
Dorsal vertebrae, middle and posterior, neural spine anteroposterior length at base relative to centrum length: subequal (0); shorter (1). NEW
Dorsal vertebrae, middle-posterior parapophyses, development: distinct elevated process (0); reduced, knob-shaped (1). NEW
Dorsal vertebrae, accessory centrodiapophyseal lamina: absent (0); present (1). (Modified from Benson et al., 2010, char. 2015)
Sacrum, centrum pneumaticity: absent (0); present (1). (Modified from Carrano et al., 2012, char. 196)
Sacrum, centrum pneumaticity type: pleurocoelous fossae (0); pneumatic foramina (1). (Modified from Carrano et al., 2012, char. 196)
Sacrum, neural spines: without distal anteroposterior expansion (0); with distal expansion contacting adjacent spines (1). NEW
Caudal vertebrae, anterior, morphology of ventral surface: flat (0); groove (1); ridge (2). (Carrano et al., 2012, char. 202)
Caudal vertebrae, anterior, well-marked spino-diapophyseal lamina: absent (0); present (1). NEW
Caudal vertebrae, anterior neural arches, ventral rib laminae: absent (0); present (1). (Cau, 2018, char. 358)
Caudal vertebrae, anterior neural arches, anterolateral surface, deep triangular prezygocostal fossa delimited by two laminae: absent (0); present (1). (Cau, 2018, char. 1605; modified from Brusatte et al., 2010)
Caudal vertebrae, anterior neural arches, hyposphene: absent (0); present (1). (Cau, 2018, char. 359)
Caudal vertebrae, position of transition point (caudofemoralis and ilio-ischiocaudalis mm. correlates): at or beyond CA20 (0); around CA15-19 (1). NEW
Caudal vertebrae, middle, height of neural spines relative to centrum height: low, ≥1.3× (0); moderate, 1.3–2.0× (1); tall, 2.0–4.0× (2); extreme elongation >4× (3). NEW
Caudal vertebrae, distal, height of neural spines relative to centrum height: low, ≥1.3× (0); moderate, 1.3–2.0× (1); tall, 2.0–4.0× (2); extreme elongation >4× (3). NEW
Caudal vertebrae, middle, morphology of neural spines: rod-like and posteriorly inclined (0); subrectangular and sheet-like (1); rod-like and vertical (2). (Carrano et al., 2012, char. 207)
Caudal vertebrae, middle, centrum elongation relative to centrum height: elongated >1.6× (0); not elongated ≤1.6× (1). NEW
Caudal vertebrae, middle and posterior, prezygapophyses: elongated, projected beyond the anterior rim of the centrum (0); shortened, barely reaching the anterior rim of the centrum (1). NEW (after observations in Samathi et al., 2021)
Chevrons, anterior and posterior longitudinal groove: absent (0); present (1). NEW
Chevrons, anterior and posterior surfaces: without distinctive features (0); with longitudinal groove widened as a fossa (1). NEW
Chevrons, posterior elongation compared with anterior and middle ones: shorter (0); as elongated (1). NEW
Chevrons, anterior process: absent (0); present (1). (Carrano et al., 2012, char. 217)
Appendicular
Coracoid, posterior process, shape: low and rounded (0); crescentic (1). (Sereno et al., 1998, char. 29)
Appendicular bones, marrow cavity: present (0); reduced to barely present (1). NEW
Humerus, deltopectoral crest, length relative to humeral length: less (0) or more (1) than 45%. (Sereno et al., 1998, char. 3)
Humerus, deltopectoral crest, orientation of apex: anterior (0), lateral (1). (Sereno et al., 1998, char. 31)
Humerus, trochanters, size: low and rounded (0); hypertrophied and pointy (1). (Sereno et al., 1998, char. 30)
Humerus, internal tuberosity, size: low and rounded (0); hypertrophied (1). (Sereno et al., 1998, char. 32)
Radius (forearm), length relative to humeral length: more (0) or less (1) than 50%. (Sereno et al., 1998, char. 4)
Radius, external tuberosity and ulnar internal tuberosity, size: low and rounded (0); hypertrophied (1). (Sereno et al., 1998, char. 33)
Manual digit I–ungual, length relative to the depth of proximal end: 2.5 (0) or 3 (1) times. (Sereno et al., 1998, char. 5)
Ilium, ventrolateral development of supraacetabular crest: large/pendant ‘hood’ (0); reduced shelf (1). (Carrano et al., 2012, char. 267)
Ilium, lateral vertical crest dorsal to the acetabulum: absent (0); present (1). (Rauhut, 2003, char. 6)
Ilium, shape of posterior margin of postacetabular process: convex (0); concave (1); straight (2); with prominent posterodorsal process but lacking posteroventral process (3). (Carrano et al., 2012, char. 280)
Ilium, orientation of pubic peduncle: mostly ventral (0); mostly anterior or ‘kinked’ double facet with anterior and ventral components (1). (Carrano et al., 2012, char. 268)
Ilium, pubic peduncle length to width ratio: ≤1 (0); 1–2 (1); >2 (2). (Modified from Carrano et al., 2012, char. 272)
Ilium, brevis fossa, lateral and medial margins, orientation in ventral view and development of fossa: subparallel, narrow fossa (0); posteriorly diverging, expanded fossa (1). (Modified by Cau, 2018, char. 592; Holtz, 2000; Rauhut, 2003)
Puboischiadic plate, foramina/notches: closed along midline, 3 fenestrae (0); open along midline, 1 fenestra (obturator foramen of pubis) and 1–2 notches (1); open along midline, 0 fenestrae, 1–2 notches (2). (Carrano et al., 2012, char. 281)
Pubis, distal pubic foot, size: moderate to large (0); reduced to a small flange (1). (Modified from Sereno et al., 1998, char. 34)
Pubis, length relative to ischium: longer (0); subequal or shorter (1). NEW
Ischium, distal half, cross section: laminar, strongly mediolaterally compressed (0); robust, rod-like (1). (Cau, 2018, char. 425)
Femur, fourth trochanter position of distalmost end: proximal most 1/3 (0); almost at the half of the femur (1). NEW
Femur, oblique ligament groove on posterior surface of head: shallow, groove bounding lip does not extend past posterior surface of head (0); deep, bound medially by well-developed posterior lip (1). (Carrano et al., 2012, char. 304)
Tibia and/or femur, length compared to posterior dorsal centra length: more (0) or less (1) than five times. (Cau, 2018, char. 245)
Tibia, proximal diaphysis, length-width ratio: smaller than 2 (0); greater than 2 (1). NEW (after Samathi et al., 2021)
Pedal ungual phalanges, ventral side: concave (0); flat (1). NEW
Character-taxon matrix
See Source data 1 and Source data 2.
Spinosauridae (with Camarillasaurus)
Ch. 48: 0 →1 Maxillary lateral teeth with circular midcrown cross section.
Ch. 92: 0 →1 Middle and posterior caudal vertebrae with short prezygapophyses.
Ch. 119: 0 →1 Tibia with a proximal diaphysis with length + width ratio greater than 2.
Spinosauridae (minus Camarillasaurus)
Ch. 49: 0 →1 Maxillary lateral teeth with fluting (apico-basal ridges).
Ch. 94: 0 → 1 Anterior chevrons with longitudinal groove widened as a fossa.
Baryonychinae
Ch. 3: 0 → 1 V-shaped premaxilla-nasal suture.
Ch. 30: 0 →1 Square-shaped quadrate head.
Ch. 57: 0 →1 30 dentary teeth.
Ch. 64: 1 →0 Middle cervical vertebrae with neural spines longer than tall.
Ch. 74: 0 →1 Dorsal vertebrae, posterior neural spines with basal webbing.
Ch. 78: 0 →1 Dorsal vertebrae with accessory centrodiapophyseal lamina.
Ch. 97: 0 →1 Coracoid with crescentic posterior process.
Ceratosuchopsini (Suchomimus + Ceratosuchops)
Ch. 26: 0 →1 Frontal, postorbital facet depth more than 2/5 facet length.
Ch. 27: 0→1 Frontal with abrupt transition between the anterior half and the postorbital process.
Ch. 40: 0 →1 Basioccipital contribution to foramen magnum reduced, with exoccipitals closely placed.
Spinosaurinae
Ch. 63: 0 →1 Middle and posterior cervical vertebrae with centra wider than tall.
Ch. 66: 0 →1 Anterior dorsal vertebrae with strongly developed hypapophysis.
Ch. 69: 0→1 Anterior dorsal vertebrae with pneumatic foramen smaller than parapophysis.
Ch. 71: 0 →1 Middle and posterior dorsal vertebrae with deeply excavated prezygopara-diapophyseal fossa (prpadf).
Ch. 76: 0 →1 Posterior dorsal vertebrae with neural spine base shorter than centrum.
Ch. 77: 0→1 Middle and posterior dorsal vertebrae with reduced, knob-like parapophyses.
Ch. 84: 0 →1 Anterior caudal vertebrae with centro-costal laminae.
Ch. 85: 0 →1 Anterior caudal vertebrae with prezygo-costal fossa delimited by two laminae.
Vallibonavenatrix + (Spinosaurus + Irritator)
Ch. 67: 0 →1 Mid-dorsal vertebrae centra longer than 1.4 times centrum height.
Ch. 72: 0 →1 Middle and posterior dorsal centra with large pneumatic foramina.
Ch. 83: 0 →1 Anterior caudal vertebrae with well-marked spino-diapophyseal lamina.
Ch. 91: 0 →1 Shorter middle caudal centra.
Spinosaurus + Irritator
Ch. 109: 0 →1 Ilium, orientation of pubic peduncle mostly anterior or ‘kinked’ double facet with anterior and ventral components.
Funding Statement
The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.
Contributor Information
Paul C Sereno, Email: dinosaur@uchicago.edu.
Min Zhu, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, China.
Christian Rutz, University of St Andrews, United Kingdom.
Funding Information
This paper was supported by the following grants:
Bob and Ellen Vladem Gift to Paul C Sereno.
SC Johnson Gift to Paul C Sereno.
Chicago Herpetological Society to Paul C Sereno.
Additional information
Competing interests
No competing interests declared.
No competing interests declared.
Author contributions
Conceptualization, Resources, Formal analysis, Supervision, Funding acquisition, Validation, Investigation, Visualization, Writing - original draft, Project administration, Writing – review and editing.
Formal analysis, Validation, Investigation, Visualization, Methodology, Writing – review and editing.
Conceptualization, Formal analysis, Investigation, Visualization, Methodology, Writing – review and editing.
Conceptualization, Formal analysis, Investigation, Visualization, Methodology, Writing – review and editing.
Conceptualization, Formal analysis, Investigation, Visualization, Methodology, Writing – review and editing, phylogenetic analysis.
Conceptualization, Formal analysis, Investigation, Visualization, Methodology, Writing – review and editing, CT data on recent organisms.
Data curation, Formal analysis, Visualization, Methodology, Writing – review and editing, CT-based model reconstruction.
Conceptualization, Investigation, Visualization, Methodology, Writing – review and editing.
Data curation, Investigation, Visualization, Visualisations.
Additional files
Data availability
All data generated or analysed during this study are included in the manuscript and appendices. Data has been deposited to MorphoSource and provided as Source datas 1 and 2.
The following previously published dataset was used:
Sereno PC, Myrhvold N, Henderson DM, Fish FE, Vidal D, Baumgart SL, Keillor TM, Formoso KK, Conroy LL. 2020. Spinosaurus was not an aquatic dinosaur. MorphoSource. 000460619
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