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Silesauridae

life science Maturity 11-13 Next article →

Silesauridae is an extinct family of early dinosauriforms from the Triassic Period. These animals are crucial for understanding the early evolution of dinosaurs.

Silesaurid distribution
Silesaurid distribution

Scientists still debate their exact place in the family tree of life. Some studies suggest they are a sister group to dinosaurs. This means they shared a common ancestor but evolved separately from the Dinosauria group. Other researchers argue they belong inside Dinosauria. Specifically, they may be early representatives of the ornithischian dinosaurs.

Lewisuchus skeletal
Lewisuchus skeletal

Silesaurids had a consistent, lightly-built body plan. They possessed fairly long necks and long legs. Their forelimbs were notably long and slender compared to other Triassic dinosauriforms.

Kwanasaurus skeletal reconstruction
Kwanasaurus skeletal reconstruction

This anatomy suggests many species were primarily quadrupedal, or walked on all fours. In contrast, most early dinosaurs like theropods were bipedal. Some silesaurids might have practiced facultative bipedalism. This means they could walk on two legs during specific moments, such as fleeing a predator.

Silesaurus opolensis by Szymon Górnicki
Silesaurus opolensis by Szymon Górnicki

Their diets changed significantly across different species and time periods. Early examples like Lewisuchus were small carnivores. They had ziphodont teeth, which are sharp, knife-like teeth used for rending flesh.

Silesaurid left dentaries
Silesaurid left dentaries

Other species, such as Silesaurus, may have been insectivorous. Fossilized dung, known as coprolites, suggests they ate small beetles and other arthropods. Later taxa like Kwanasaurus became specialized herbivores. They developed leaf-shaped teeth and a beak at the tip of the lower jaw.

Kwanasaurus life restoration
Kwanasaurus life restoration

Silesaurid teeth were unique due to a process called ankylothecodonty. This means the teeth were set in deep sockets, known as thecodonty. Over time, the ligaments within these sockets hardened into bone, a process called ankylosis.

Amanasaurus fossil material
Amanasaurus fossil material

While many Triassic reptiles had deep sockets, this specific hardening of ligaments is not found in traditional ornithischians. Their skull structure also included weight-saving holes. These holes are found on the snout, the jaw, and the back of the skull. These openings are called the antorbital, mandibular, and temporal fenestrae.

Their hip structure was also quite distinct from most dinosaurs. Silesaurids possessed a pillar-erect hip joint.

Sprawling and erect hip joints - horizontal
Sprawling and erect hip joints - horizontal

In this arrangement, the femur supports the thickened upper lip of the hip socket. This allowed for a narrow, mammal-like gait. This differs from the ball-and-socket joints found in most dinosaurs. Most dinosaurs have a rounded femur head that is deeply embedded in the socket. Additionally, silesaurids were propubic. This means their pubis, the front lower bone of the pelvis, pointed down and forward.

Lutungutali
Lutungutali

Silesaurids varied greatly in size throughout the Triassic. Many species were quite small. For instance, Silesaurus opolensis reached a total length of about one meter.

Sacisaurus skeletal
Sacisaurus skeletal

However, some silesaurids were the largest dinosauriforms of their era. Isolated femur bones from Tanzania and Zambia belong to silesaurids up to 2 meters in length. These African fossils date back to the Middle Triassic. Large fossils have also been found in South America from the same period. By the late Carnian, the carnivore Herrerasaurus reached a similar size.

Understanding silesaurids helps scientists track major biological shifts. The transition from the Triassic to the Jurassic involved a mass extinction event. Evidence suggests a miniaturization event occurred during this time. Early Jurassic ornithischians were generally smaller than most silesaurids. This change in size provides clues about how animals survived environmental shifts. By studying these fossils, paleontologists can better map the complex transition from early dinosauriforms to the massive dinosaurs of the later Mesozoic Era.

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🖼️ Images & Media (20)
File:Silesauridae.png
Silesauridae.png
File:Lewisuchus skeletal.png
Lewisuchus skeletal.png
File:Silesaurid left dentaries.png
Silesaurid left dentaries.png
File:Kwanasaurus skeletal reconstruction.png
Kwanasaurus skeletal reconstruction.png
File:Sacisaurus skeletal.png
Sacisaurus skeletal.png
File:Lutungutali.png
Lutungutali.png
File:Sprawling and erect hip joints - horizontal.svg
Sprawling and erect hip joints - horizontal.svg
File:Amanasaurus fossil material.png
Amanasaurus fossil material.png
File:Silesaurid distribution.png
Silesaurid distribution.png
File:Marasuchus.jpg
Marasuchus.jpg
File:Lewisuchus NT, white background.jpg
Lewisuchus NT, white background.jpg
File:Asilisaurus.jpg
Asilisaurus.jpg

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