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Orthosuchus
Fossil range: Early Jurassic

Scientific classification

Kingdom:

Animalia

Phylum:

Chordata

Class:

Sauropsida

Infraclass:

Archosauromorpha

Superorder:

Crocodylomorpha

Genus:

Orthosuchus

Orthosuchus is an extinct genus of protosuchian that lived during the Early Jurassic.[1]

Description[]

Orthosuchus has a body proportion similar to lizards, with a body length about 0.6 meters, and a flattened skull, a typical skull of crocodilian.

The external skull surface is covered randomly with small pits. The orbits are huge, with a complete dorsal roof made by the paired supraorbitals. The maxilla has sharp edge, which extends forward and covers some part of the lateral notch. The ears are protected by earflaps, which prevent water inflow to the otic recess when this animal is in water. The fossil resembles some features of a primitive crocodilian, one of them is the reduced antorbital fenestra. The quadratojugal is the backbone of the skull, which connects to the jugal and quadrate. The flattened head shape of Orthosuchus is made by the posterior quadrate contact, which is below the rear end of the squamosal. This form is a typical archosaurian characteristic that had lost in modern crocodiles, and also absent in teleosaurs. It developed a short secondary bony palate, with crocodilian featuring pterygoids. The elongated choana is located behind the secondary palate, which is made by the premaxilla and maxilla. In modern crocodiles, the choana is between the vomers and the anterior processes of pterygoids. The dentary forms the largest part of the lower jaw with some shallow pits, which indicated that the animal probably has 15-18 teeth, fewer teeth in the far back. The teeth are equal in size and similar in shape.

Orthosuchus has 24 vertebrae, and 8 of them are believed to be in the cervical region. All vertebrae appear to be amphicoelous. It does not have tall neural spine but the height of them decrease from head to tail. The vertebrae in the neck region are tightly bonded together. The ribs start at the twelfth vertebra, which supports the ilium. The tail consists of 8 vertebrae of different size and shape. The first one is in contact with the sacral ribs, three vertebrae at the far end of the tail are tiny in size, and the other four vertebrae form the middle of the tail. The ribs form antero-ventral and postero-dorsal flanges, which are for the muscle attachments.

Orthosuchus has similar pectoral girdles and pelvic girdles compare to living crocodiles, with a long scapula and a shorter coracoid. The interclavicle is hypothesized to be cartilaginous. As for the forelimb, the fossil records showed that Orthosuchus has similar humerus, but the distal and proximal expansions does not lay on the same plane as the modern crocodiles. Also, not like the living crocodiles, the ulna and radius of Orthosuchus, or other typical archosaurs, are around 88% of the length of the humerus, while the radius and ulna in modern crocodiles are the shortest elements in the forelimb. It has two non-elongated carpals, with one of the elliptical shape. Orthosuchus appeared to have 5 digits. The first digit is the shortest and the fifth digit is the weakest. Although some of the phalanges are missing, it is believed that the phalanges formula is 2, 3, 4, 5, 3, 3. The femur is thought to be the longest bone. The tibia is more developed than the fibula, and they are 94% of the length of the femur. Taking all the bones into account, the forelimb is 91% the length of the hind limb. Orthosuchus has similar astragalus and calcaneum. Compared to the astragalus, the rectangular shaped calcaneum is small in size and forms a prominent tuber.

Discovery[]

The first fossil materials were collected by an expedition of South African Museum in April 1963 led by Alfred W. Crompton. The materials were collected from the Lower Jurassic Red Bed Formation (= Upper Elliot Formation) of the Stormberg, so that as soon as they found out that the fossils belongs to a new crocodilian species, they named the species Orthosuchus Stormbergi in a paper published by Nash 1968. They also found a smaller skull that also belongs to Orthosuchus Stormbergi at the same horizon but in a different place at the same site. The main part of the skull and the law jaw was well preserved, but some of the phalanges, ribs, and one side of the pelvic girdle with its hind limb were missing. Since the specimens had some distortions, major issues were fix at the site before it was X-rayed.

In 1931, a new primitive form of crocodilian was found in the Dinosaur Canyon Beds of northern Arizona, United States. The beds are at the top of the Upper Triassic Formation and below the Lower Jurassic sediments. The crocodilian found is about 1 meter long, with flattened head and large frontals. Its more advanced transverse process indicates that it is a new crocodilian species. In 1933 Barnum Brown named it Archaeosuchus, and then changed it to Protosuchus in 1934 and form the family of Protosuchidae. The classification of Protosuchidae is debatable, however, since Orthosuchus resemble some of the characteristics of Protosuchidae, it is believed to be in the part of this family.

Classification[]

Modern crocodiles are considered within the group archosaurs, which also include birds, dinosaurs, and crocodilians. However, from appearance, archosaurs resemble more of crocodiles than of birds. Orthosuchus resembles a primitive form of crocodilian by some of its traits: the fusion midline together at the parietal, the form of the secondary palate, the fusion of pterygoid and quadrate, the extension of coracoid, radius, and ulna, and the form of tuber on the calcaneum. Orthosuchus is closely related to Protosuchus, Notochampsa, Erythrochampsa, and probably other crocodilian families. Although Orthosuchus could be grouped into Notochampsa, more people want to keep the family Protosuchidae because it is widely accepted.

Paleobiology[]

References[]

  1. ^ Pol D, Ji S, Clark JM, Chiappe LM. 2004. Basal crocodyliforms from the Lower Cretaceous Tugulu Group (Xinjiang, China), and the phylogenetic position of Edentosuchus. Cretaceous Research 25(4): 603-622.