Stratiotosuchus Temporal range: Late Cretaceous, | |
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Life restoration of Stratiotosuchus maxhechti | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Reptilia |
Clade: | Archosauria |
Clade: | Pseudosuchia |
Clade: | Crocodylomorpha |
Clade: | Crocodyliformes |
Suborder: | † Notosuchia |
Clade: | † Sebecosuchia |
Family: | † Baurusuchidae |
Subfamily: | † Baurusuchinae |
Genus: | † Stratiotosuchus Campos et al., 2001 |
Type species | |
†Stratiotosuchus maxhechti Campos et al., 2001 |
Stratiotosuchus (from Greek, στρατιώτης (stratiōtēs, "soldier") and σοῦχος (suchos, "crocodile")) is an extinct genus of baurusuchid mesoeucrocodylian from the Adamantina Formation in Brazil. It lived during the Late Cretaceous. [1] [2] The first fossils were found in the 1980s, and the type species Stratiotosuchus maxhechti was named in 2001. [1] A hyperpredator, [2] it and other baurusuchids may have filled niches occupied elsewhere by theropod dinosaurs. [3] [4]
Stratiotosuchus has a deep, laterally compressed skull 47 centimetres (19 in) long. Based on that skull size, Stratiotosuchus is estimated up to 4 metres (13 ft) in total length (including tail), [5] although later study mentioned that head and total length ratio of Stratiotosuchus being about 1:6. [6] The teeth are ziphodont, meaning that they are laterally compressed, curved, and serrated. Like other baurusuchids, Stratiotosuchus has a reduced number of teeth: three in its premaxilla and five in its maxilla. When the jaw is closed, the teeth of the upper jaw overlie those of the lower jaw and shear closely together. Stratiotosuchus has one large caniniform tooth in its premaxilla, and several large maxillary teeth behind it. An enlarged fourth dentary tooth in the lower jaw also forms a canine, and is visible when the jaw is closed. [5]
Like all crocodyliforms, Stratiotosuchus was quadrupedal. Unlike the sprawling gait of crocodilians living today, Stratiotosuchus is thought to have been a fully erect quadruped. The transition from a sprawling, low to the ground posture in the ancestors of Stratiotosuchus to an erect, elevated posture involved a significant transformation of the limbs, hips, and shoulders. [5]
Large crests are present over the acetabulum, or hip socket, stabilizing the hip in what is known as a pillar-erect stance (the acetabular crest lies like a shelf on top of the femur to form a pillar). The ischium bone, which extends backward from the hip, has a large projection that in life would serve as a strong attachment site for the puboischiotibialis muscle. The puboischiotibialis is also present in living crocodilians and is used primarily to keep the legs upright in what is known as a high walk, in which they hold their legs underneath them while walking. The puboischiotibialis is very weak in living crocodilians, so they cannot sustain a high walk for very long. Stratiotosuchus is thought to have had a much stronger puboischiotibialis, allowing it to have a permanent upright stance. [5]
Stratiotosuchus also has a relatively straight femur bone; while the bone is somewhat twisted along its length, the degree of torsion is not as high as that of other crocodyliforms. The shape of the femur is more similar to that of rauisuchids and poposaurids, which were early crocodile relatives that are known to have had erect gaits. The femur even shares similarities with those of early theropod dinosaurs, which were fully bipedal. When compared to crocodilians, the top of the femur of Stratiotosuchus is rotated toward the front, so that the femoral head faces backward rather than medially inward. This position restricts the movement of the hindlimbs along a forward-backward or parasagittal axis. Muscles that attach to the side of the leg in crocodilians would have attached to the back of the leg in Stratiotosuchus, enabling a powerful backward extension of the hind leg. [5]
The arm socket faces backwards and downwards from a bone in the shoulder girdle called the coracoid, suggesting that the arms were held beneath the body. The large articular surface on the head of the humerus implies that the arms had a wide range of movement, but restricted to a parasagittal axis. The deltopectoral crest on the front of the humerus would have anchored large arm muscles to bring the arm forward while walking. Modern crocodilians also have a deltopectoral crest, but it is positioned laterally and anchors to muscles that pull the arms up to the sides, not forward. The muscle thought to have facilitated forward movement in Stratiotosuchus is called the deltoideus clavicularis; it is also present in modern crocodilians, which use it for high walking. [5]
Other features that suggest an erect posture are tightly clustered metacarpals forming narrow hands well-suited for walking and a backward-projecting calcaneal tuberosity in the ankle, which would have attached to muscles that fixed the lower limb in a parasagittal axis. A backward-projecting calcaneal tuberosity is present in most early crocodilian relatives, including those that are thought have sprawling gaits, yet modern crocodilians have more laterally projected tuberosities impeding a parasagittal orientation of the hind foot. [5]
The first known fossil of Stratiotosuchus was a nearly complete skeleton, cataloged as DGM 1477-R. It was found by paleontologist José Martin Suárez in the town of Irapuru in São Paulo State in 1988. This skeleton and all other specimens of Stratiotosuchus come from the Adamantina Formation, which is either Turonian-Santonian in age (about 85 million years old) or Campanian-Maastrichtian in age (about 70 million years old). DGM 1477-R includes a nearly complete skull, partial lower jaw, vertebral column, and limb bones. The skeleton was identified as that of a baurusuchid, closely related but distinct from Baurusuchus pachechoi , which had been known since 1945. Stratiotosuchus maxhechti was named in 2001 on the basis of this skeleton, designated the holotype of the species. The generic name, Stratiotosuchus, means "soldier crocodile" in Greek, and the specific name, maxhechti, honors paleontologist Max Knobler Hetch (1925–2002). [1] [7]
Further preparation of DGM 1477-R revealed that two individuals were present in the same block of sandstone, as indicated by two extra leg bones, an extra fragment of the hip, and extra metatarsals. They are the same size as the other bones, suggesting that the second individual was equal in body size to the first. [5]
Stratiotosuchus has been recognized as a baurusuchid since it was first described in 1988. [8] In 2004, Baurusuchidae was even defined as the most recent common ancestor of Baurusuchus and Stratiotosuchus and all of its descendants; thus, the definition of Baurusuchidae relies on the inclusion of Stratiotosuchus. [9] Stratiotosuchus and Baurusuchus both belong to a large clade called Metasuchia, which includes living crocodilians and many extinct relatives extending back into the Jurassic. However, the exact position of Stratiotosuchus and Baurusuchus within Metasuchia is still uncertain. Below are several possibilities that have been uncovered in various phylogenetic analyses:
Montefeltro et al. (2011) found support for baurusuchids as advanced notosuchians, and divided the family into two subfamilies, Baurusuchinae and Pissarrachampsinae. Stratiotosuchus belonged to Baurusuchinae along with Baurusuchus. Below is the cladogram from Montefeltro et al. (2011): [10]
Another phylogenetic analysis of baurusuchids was conducted by Riff and Kellner (2011). Their analysis placed Stratiotosuchus and Baurusuchus deep within Notosuchia, as the sister taxon of the family Sphagesauridae. Below is the cladogram from that study: [5]
Based on the types of deposits in the Adamantina Formation, Stratiotosuchus most likely lived alongside a river system with many small ephemeral lakes. [5]
With a fully erect stance, Stratiotosuchus has many features convergent with theropod dinosaurs, which are fully bipedal. In Stratiotosuchus, a roughly surfaced region on the upper part of the femur is analogous to the accessory trochanter common to tetanuran theropods. These projections are thought to have anchored the same muscle, called the puboischiofemoralis internus pars dorsalis. A crest on the forward edge of the tibia is similar to those seen in early theropod dinosaurs. The articular surface of the tibia that attaches to the femur is laterally compressed, which is unlike the more circular surface in living crocodilians and more like that of a theropod dinosaur. On the hip of Stratiotosuchus, a depression on the ilium is convergent with the brevis fossa of dinosaurs, and the small bump anchoring the puboischiotibialis muscle is convergent with the obturator tubercle of maniraptoriform theropods. [5]
Along with anatomical similarities, Stratiotosuchus and other baurusuchids are thought to have had lifestyles very similar to those of theropod dinosaurs. While many small carnivorous crocodyliforms are known from the Adamantina Formation, Stratiotosuchus and Baurusuchus are believed to have been the only large carnivores the Adamantina ecosystem. Decades of paleontological exploration in these deposits have uncovered only a few theropod dinosaur bones, so it appears that baurusuchids like Stratiotosuchus occupied the niche of top predators in the absence of these dinosaurs. A nearby Cretaceous deposit in Argentina called the Neuquén Group also contains baurusuchids, but they are much smaller than Stratiotosuchus and were likely out-competed by the wide range of theropod dinosaurs known from these deposits. In the absence of large theropods, carnivores like Stratiotosuchus may have fed on large herbivorous titanosaurs, including Adamantisaurus , Arrudatitan , Gondwanatitan , and Maxakalisaurus . [5]
Pseudosuchians superficially resembling Stratiotosuchus were the top predators of the Triassic period, until they were decimated by the Triassic–Jurassic extinction event and replaced by large theropods. [11] [12] The appearance of Stratiotosuchus and other baurusuchids marks a brief recovery of this top position during the Late Cretaceous. [5] Niche partitioning existed between large theropods and baurusuchids where they overlapped in range. [13]
Razanandrongobe is a genus of carnivorous ziphosuchian crocodyliform from the Middle Jurassic of Madagascar. It contains the type and only species Razanandrongobe sakalavae, named in 2004 by Simone Maganuco and colleagues based on isolated bones found in 2003. The remains, which included a fragment of maxilla and teeth, originated from the Bathonian-aged Sakaraha Formation of Mahajanga, Madagascar. While they clearly belonged to a member of the Archosauria, Maganuco and colleagues refrained from assigning the genus to a specific group because the fragmentary remains resembled lineages among both the theropod dinosaurs and crocodylomorphs.
Baurusuchus is an extinct genus of baurusuchid mesoeucrocodylian, which lived in Brazil from 90 to 83.5 million years ago, in the Late Cretaceous period. It was a terrestrial predator and scavenger, estimated to reach up to 113.4 kilograms (250 lb) in weight. Baurusuchus lived during the Turonian to Santonian stages of the Late Cretaceous Period, in Adamantina Formation, Brazil. It gets its name from the Brazilian Bauru Group. It was related to the earlier-named Cynodontosuchus rothi, which was smaller, with weaker dentition. The three species are B. pachechoi, named after Eng Joviano Pacheco, its discoverer, B. salgadoensis and B. albertoi. The latter species is disputed. Its relatives include the similarly sized Stratiotosuchus from the Adamantina Formation, and Pabweshi, from the Pakistani Pab Formation.
Notosuchia is a suborder of primarily Gondwanan mesoeucrocodylian crocodylomorphs that lived during the Jurassic and Cretaceous. Some phylogenies recover Sebecosuchia as a clade within Notosuchia, others as a sister group ; if Sebecosuchia is included within Notosuchia its existence is pushed into the Middle Miocene, about 11 million years ago. Fossils have been found from South America, Africa, Asia, and Europe. Notosuchia was a clade of terrestrial crocodilians that evolved a range of feeding behaviours, including herbivory (Chimaerasuchus), omnivory (Simosuchus), and terrestrial hypercarnivory (Baurusuchus). It included many members with highly derived traits unusual for crocodylomorphs, including mammal-like teeth, flexible bands of shield-like body armor similar to those of armadillos (Armadillosuchus), and possibly fleshy cheeks and pig-like snouts (Notosuchus). The suborder was first named in 1971 by Zulma Gasparini and has since undergone many phylogenetic revisions.
Baurusuchidae is a Gondwanan family of mesoeucrocodylians that lived during the Late Cretaceous. It is a group of terrestrial hypercarnivorous crocodilians from South America and possibly Pakistan. Baurusuchidae has been, in accordance with the PhyloCode, officially defined as the least inclusive clade containing Cynodontosuchus rothi, Pissarrachampsa sera, and Baurusuchus pachecoi. Baurusuchids have been placed in the suborder Baurusuchia, and two subfamilies have been proposed: Baurusuchinae and Pissarrachampsinae.
The Adamantina Formation is a geological formation in the Bauru Basin of western São Paulo state, in southeastern Brazil.
Pabwehshi is an extinct genus of mesoeucrocodylian. It is based on GSP-UM 2000, a partial snout and corresponding lower jaw elements, with another snout assigned to it. These specimens were found in Maastrichtian-age Upper Cretaceous rocks of the Vitakri and Pab Formations in Balochistan, Pakistan, and represent the first diagnostic crocodyliform fossils from Cretaceous rocks of South Asia. Pabwehshi had serrated interlocking teeth in its snout that formed a "zig-zag" cutting edge. Pabwehshi was named in 2001 by Jeffrey A. Wilson and colleagues. The type species is P. pakistanensis, in reference to the nation where it was found. It was traditionally classified as a baurusuchid closely related to Cynodontosuchus and Baurusuchus. Larsson and Sues (2007) found close affinity between Pabwehshi and the Peirosauridae within Sebecia. Montefeltro et al.Pabwehshi has a sagittal torus on its maxillary palatal shelves – a character that is absent in baurusuchids – but they did not include Pabwehshi in their phylogenetic analysis.
Bergisuchus is an extinct genus of small sebecosuchian mesoeucrocodylian known primarily from the Eocene Messel Pit in Germany. Few fossils of Bergisuchus have been discovered, only a single incomplete snout, a few partial lower jaws and some teeth. Despite being fragmentary, the jaw bones are enough to indicate that Bergisuchus had a short, deep, narrow snout and serrated teeth, quite unlike the broad flat snouts of modern crocodylians.
Metasuchia is a major clade within the superorder Crocodylomorpha. It is split into two main groups, Notosuchia and Neosuchia. Notosuchia is an extinct group that contains primarily small-bodied Cretaceous taxa with heterodont dentition. Neosuchia includes the extant crocodylians and basal taxa, such as peirosaurids and pholidosaurids. It is phylogenetically defined by Sereno et al. (2001) as a clade containing Notosuchus terrestris, Crocodylus niloticus, and all descendants of their common ancestor.
Sebecus is an extinct genus of sebecid crocodylomorph from Eocene of South America. Like other sebecosuchians, it was entirely terrestrial and carnivorous. The genus is currently represented by two species, the type S. icaeorhinus and S. ayrampu. Several other species have been referred to Sebecus, but were later reclassified as their own genera.
Sebecia is an extinct clade of mesoeucrocodylian crocodyliforms that includes peirosaurids and sebecids. It was first constructed in 2007 to include Hamadasuchus, Peirosauridae, and Sebecus. It was initially considered to be the sister taxon of the clade Neosuchia, which includes living crocodilians, although some later studies have placed it within Neosuchia as a basal clade. Sebecians were terrestrial crocodyliforms characterized by their deep snouts and ziphodont dentition. They first appeared in the Late Cretaceous, survived the Cretaceous–Paleogene extinction event, and became extinct in the Miocene epoch.
Sebecosuchia is an extinct group of mesoeucrocodylian crocodyliforms that includes the families Sebecidae and Baurusuchidae. The group was long thought to have first appeared in the Late Cretaceous with the baurusuchids and become extinct in the Miocene with the last sebecids, but Razanandrongobe pushes the origin of Sebecosuchia to the Middle Jurassic. Fossils have been found primarily from South America but have also been found in Europe, North Africa, Madagascar, and the Indian subcontinent.
Susisuchus is an extinct genus of neosuchian mesoeucrocodylian crocodyliform from the Early Cretaceous of Brazil. Fossils have been found from the Nova Olinda Member of the Aptian-age Crato Formation in the Araripe and Lima Campos Basins of northeastern Brazil. Named in 2003, Susisuchus is the sole member of the family Susisuchidae, and is closely related to the clade Eusuchia, which includes living crocodilians. The type species is S. anatoceps, known from a single partial articulated skeleton that preserves some soft tissue. A second species, S. jaguaribensis, was named in 2009 from fragmentary remains.
Pepesuchus is an extinct genus of carnivorous metasuchian from the Late Cretaceous period. It is a peirosaurid which lived during the Campanian and Maastrichtian stages of the Late Cretaceous in what is now state of São Paulo, Brazil. It was a semiaquatic crocodylomorph.
Campinasuchus is an extinct genus of baurusuchid mesoeucrocodylian from Minas Gerais State of Brazil.
Pissarrachampsa is an extinct genus of baurusuchid mesoeucrocodylian from the Late Cretaceous of Brazil. It is based on a nearly complete skull and a referred partial skull and lower jaw from the ?Campanian - ?Maastrichtian-age Vale do Rio do Peixe Formation of the Bauru Group, found in the vicinity of Gurinhatã, Brazil.
Pissarrachampsinae is a subfamily of baurusuchid crocodyliforms from the Late Cretaceous of Brazil and Argentina. It was named in 2011 with the description of Pissarrachampsa sera and includes P. sera from Brazil and the related Wargosuchus australis from Argentina. Pissarrachampsinae is one of two subfamilies of Baurusuchidae, the other being Baurusuchinae.
Baurusuchinae is a subfamily of baurusuchid crocodyliforms from the Late Cretaceous of Brazil. Named in 2011, it contains the baurusuchids Aphaurosuchus, Aplestosuchus, Baurusuchus and Stratiotosuchus. Baurusuchinae is one of two subfamilies of Baurusuchidae, the other being Pissarrachampsinae.
Aplestosuchus is an extinct genus of baurusuchid mesoeucrocodylian known from the Late Cretaceous Adamantina Formation of São Paulo, southern Brazil. It contains a single species, Aplestosuchus sordidus. A. sordidus is represented by a single articulated and nearly complete skeleton, preserving the remains of an unidentified sphagesaurid crocodyliform in its abdominal cavity. The specimen represents direct evidence of predation between different taxa of crocodyliforms in the fossil record.
Aphaurosuchus is an extinct genus of baurusuchid mesoeucrocodylian known from the Late Cretaceous Bauru Basin of São Paulo, southern Brazil. It contains two species, Aphaurosuchus escharafacies and Aphaurosuchus kaiju.
Titanochampsa is a genus of large mesoeucrocodylian from the Maastrichtian Marilia Formation of Brazil. Although only known from a single skull roof, the material shows that Titanochampsa was not a member of Notosuchia, which were previously believed to have been the only crocodyliforms present in the strata of the Bauru Group. Body size estimates vary greatly and range between 2.98–5.88 m due to the incomplete nature of the holotype fossil. The overall anatomy of the skull roof, alongside its size and possible affinities with Neosuchians, may suggest that it was a semi-aquatic ambush hunter similar to modern crocodilians.
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