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Barasaurus besairiei Fossil Reptile Skeleton Upper Permian Madagascar Morondava Basin Authentic Specimen

£360.00

Barasaurus besairiei Early Reptile Skeleton Fossil from the Upper Permian of Madagascar

This remarkable Barasaurus besairiei fossil reptile skeleton originates from the Sakamena Group of the Morondava Basin in the Fianarantsoa region of Madagascar, dating to the Lopingian Stage of the Upper Permian Period. Fossils from this time interval are exceptionally important in understanding the evolution of early reptiles and the ecosystems that existed shortly before the largest mass extinction event in Earth’s history at the end of the Permian.

The specimen represents an articulated or partial skeleton of Barasaurus besairiei, an early reptile belonging to a group of primitive diapsid reptiles that lived approximately 259–252 million years ago. Fossils of Barasaurus are considered uncommon and highly significant because they provide insight into reptile diversification during the late Paleozoic.

This fossil has been carefully selected for its preservation and scientific interest, with the listing photographs showing the exact specimen you will receive. Full sizing is visible in the listing images.

The fossil is a genuine specimen and includes a fully hand-signed Premium Certificate of Authenticity, confirming its authenticity and geological origin.

Fossil Identification and Scientific Classification

Barasaurus besairiei is an early reptile that belongs to a lineage of primitive diapsids that played an important role in reptile evolution during the late Permian.

Scientific classification includes:

  • Kingdom: Animalia
  • Phylum: Chordata
  • Class: Reptilia
  • Clade: Diapsida
  • Family: Araeoscelididae
  • Genus: Barasaurus
  • Species: Barasaurus besairiei

The species Barasaurus besairiei was first described by the French palaeontologist Jean Piveteau in 1955 based on fossils discovered within the Sakamena Formation of Madagascar.

Araeoscelidid reptiles such as Barasaurus are among the earliest known diapsid reptiles, a group that would eventually give rise to major reptilian lineages including lizards, crocodiles, dinosaurs, and birds.

Geological Formation and Age

This fossil originates from the Sakamena Group, a well-known sedimentary sequence within the Morondava Basin of southwestern Madagascar. These deposits date to the Lopingian Stage of the Upper Permian, representing one of the final chapters of the Paleozoic Era.

The Upper Permian period occurred roughly 259 to 252 million years ago, immediately preceding the Permian–Triassic extinction event, the most severe mass extinction in Earth’s history.

The Sakamena Group consists primarily of:

  • Red and grey shales
  • Fine-grained sandstones
  • Lacustrine and floodplain sediments

These deposits represent ancient continental environments that preserved a variety of terrestrial vertebrates, including early reptiles, amphibians, and other vertebrate fauna.

Morphology of Barasaurus besairiei

Barasaurus was a relatively small reptile characterised by a slender body and elongated skeletal proportions typical of early diapsids.

Key anatomical features include:

  • Elongated vertebral column
  • Slender limb bones suited for terrestrial locomotion
  • Long tail providing balance and mobility
  • Light skeletal structure typical of early reptilian lineages

One of the defining features of diapsid reptiles is the presence of two temporal openings in the skull, which allowed for stronger jaw muscles and more efficient feeding adaptations.

Although the skull may not always be preserved in every specimen, the postcranial skeleton provides valuable information about locomotion and body structure.

Depositional Environment of the Sakamena Group

During the Late Permian, the Morondava Basin formed part of a large continental interior basin located within the southern supercontinent Gondwana.

The sediments in which Barasaurus fossils are found were deposited in:

  • Freshwater lake environments
  • Floodplains and river channels
  • Low-energy sedimentary basins

Fine mud and silt accumulated in these environments, allowing delicate skeletal remains to become buried and preserved within the sediment.

The fossil-bearing layers often contain remains of other early terrestrial vertebrates, indicating that the region supported a diverse ecosystem of reptiles and amphibians during the Late Permian.

Fossil Preservation and Formation

The skeletons of Barasaurus were preserved when individuals died near lakes or floodplain environments and were rapidly buried by sediment. Over millions of years, the bones became mineralised as groundwater introduced dissolved minerals into the skeletal material.

This fossilisation process preserved the anatomical structure of the reptile skeleton within fine sedimentary rock.

The Morondava Basin is known for producing well-preserved vertebrate fossils due to the fine-grained nature of the sediment and relatively low-energy depositional conditions.

Scientific Importance of Barasaurus Fossils

Barasaurus besairiei fossils are scientifically important because they represent early members of the diapsid reptile lineage, a group that would eventually dominate terrestrial vertebrate ecosystems throughout the Mesozoic Era.

The study of these fossils helps palaeontologists understand:

  • Early reptile diversification
  • Evolutionary relationships among primitive diapsids
  • Late Permian terrestrial ecosystems
  • Vertebrate evolution prior to the end-Permian extinction

Because fossils from the Late Permian terrestrial environments are relatively rare compared to marine fossils of the same age, specimens such as Barasaurus are particularly valuable for scientific research and fossil collections.

Authentic Fossil Specimen

This specimen is a genuine Barasaurus besairiei early reptile skeleton fossil from the Sakamena Group of the Morondava Basin in the Fianarantsoa region of Madagascar.

Key details include:

  • Authentic Barasaurus besairiei fossil reptile skeleton
  • Geological Age: Lopingian Stage, Upper Permian Period
  • Formation: Sakamena Group
  • Locality: Morondava Basin, Fianarantsoa, Madagascar
  • Age: Approximately 259–252 million years old
  • Early diapsid reptile fossil
  • Exact specimen shown in listing photographs
  • Full sizing visible in listing images
  • Includes fully hand-signed Premium Certificate of Authenticity

This fossil represents an extraordinary example of Late Permian terrestrial life preserved from one of the most significant evolutionary periods in Earth’s history, making it a rare and scientifically important addition to fossil collections and natural history displays.

 

(Actual as seen)

Includes a fully hand-signed Premium Certificate of Authenticity.

Only 1 left in stock

SKU: P00343 Category:

Description

Barasaurus besairiei Early Reptile Skeleton Fossil from the Upper Permian of Madagascar

This remarkable Barasaurus besairiei fossil reptile skeleton originates from the Sakamena Group of the Morondava Basin in the Fianarantsoa region of Madagascar, dating to the Lopingian Stage of the Upper Permian Period. Fossils from this time interval are exceptionally important in understanding the evolution of early reptiles and the ecosystems that existed shortly before the largest mass extinction event in Earth’s history at the end of the Permian.

The specimen represents an articulated or partial skeleton of Barasaurus besairiei, an early reptile belonging to a group of primitive diapsid reptiles that lived approximately 259–252 million years ago. Fossils of Barasaurus are considered uncommon and highly significant because they provide insight into reptile diversification during the late Paleozoic.

This fossil has been carefully selected for its preservation and scientific interest, with the listing photographs showing the exact specimen you will receive. Full sizing is visible in the listing images.

The fossil is a genuine specimen and includes a fully hand-signed Premium Certificate of Authenticity, confirming its authenticity and geological origin.

Fossil Identification and Scientific Classification

Barasaurus besairiei is an early reptile that belongs to a lineage of primitive diapsids that played an important role in reptile evolution during the late Permian.

Scientific classification includes:

  • Kingdom: Animalia
  • Phylum: Chordata
  • Class: Reptilia
  • Clade: Diapsida
  • Family: Araeoscelididae
  • Genus: Barasaurus
  • Species: Barasaurus besairiei

The species Barasaurus besairiei was first described by the French palaeontologist Jean Piveteau in 1955 based on fossils discovered within the Sakamena Formation of Madagascar.

Araeoscelidid reptiles such as Barasaurus are among the earliest known diapsid reptiles, a group that would eventually give rise to major reptilian lineages including lizards, crocodiles, dinosaurs, and birds.

Geological Formation and Age

This fossil originates from the Sakamena Group, a well-known sedimentary sequence within the Morondava Basin of southwestern Madagascar. These deposits date to the Lopingian Stage of the Upper Permian, representing one of the final chapters of the Paleozoic Era.

The Upper Permian period occurred roughly 259 to 252 million years ago, immediately preceding the Permian–Triassic extinction event, the most severe mass extinction in Earth’s history.

The Sakamena Group consists primarily of:

  • Red and grey shales
  • Fine-grained sandstones
  • Lacustrine and floodplain sediments

These deposits represent ancient continental environments that preserved a variety of terrestrial vertebrates, including early reptiles, amphibians, and other vertebrate fauna.

Morphology of Barasaurus besairiei

Barasaurus was a relatively small reptile characterised by a slender body and elongated skeletal proportions typical of early diapsids.

Key anatomical features include:

  • Elongated vertebral column
  • Slender limb bones suited for terrestrial locomotion
  • Long tail providing balance and mobility
  • Light skeletal structure typical of early reptilian lineages

One of the defining features of diapsid reptiles is the presence of two temporal openings in the skull, which allowed for stronger jaw muscles and more efficient feeding adaptations.

Although the skull may not always be preserved in every specimen, the postcranial skeleton provides valuable information about locomotion and body structure.

Depositional Environment of the Sakamena Group

During the Late Permian, the Morondava Basin formed part of a large continental interior basin located within the southern supercontinent Gondwana.

The sediments in which Barasaurus fossils are found were deposited in:

  • Freshwater lake environments
  • Floodplains and river channels
  • Low-energy sedimentary basins

Fine mud and silt accumulated in these environments, allowing delicate skeletal remains to become buried and preserved within the sediment.

The fossil-bearing layers often contain remains of other early terrestrial vertebrates, indicating that the region supported a diverse ecosystem of reptiles and amphibians during the Late Permian.

Fossil Preservation and Formation

The skeletons of Barasaurus were preserved when individuals died near lakes or floodplain environments and were rapidly buried by sediment. Over millions of years, the bones became mineralised as groundwater introduced dissolved minerals into the skeletal material.

This fossilisation process preserved the anatomical structure of the reptile skeleton within fine sedimentary rock.

The Morondava Basin is known for producing well-preserved vertebrate fossils due to the fine-grained nature of the sediment and relatively low-energy depositional conditions.

Scientific Importance of Barasaurus Fossils

Barasaurus besairiei fossils are scientifically important because they represent early members of the diapsid reptile lineage, a group that would eventually dominate terrestrial vertebrate ecosystems throughout the Mesozoic Era.

The study of these fossils helps palaeontologists understand:

  • Early reptile diversification
  • Evolutionary relationships among primitive diapsids
  • Late Permian terrestrial ecosystems
  • Vertebrate evolution prior to the end-Permian extinction

Because fossils from the Late Permian terrestrial environments are relatively rare compared to marine fossils of the same age, specimens such as Barasaurus are particularly valuable for scientific research and fossil collections.

Authentic Fossil Specimen

This specimen is a genuine Barasaurus besairiei early reptile skeleton fossil from the Sakamena Group of the Morondava Basin in the Fianarantsoa region of Madagascar.

Key details include:

  • Authentic Barasaurus besairiei fossil reptile skeleton
  • Geological Age: Lopingian Stage, Upper Permian Period
  • Formation: Sakamena Group
  • Locality: Morondava Basin, Fianarantsoa, Madagascar
  • Age: Approximately 259–252 million years old
  • Early diapsid reptile fossil
  • Exact specimen shown in listing photographs
  • Full sizing visible in listing images
  • Includes fully hand-signed Premium Certificate of Authenticity

This fossil represents an extraordinary example of Late Permian terrestrial life preserved from one of the most significant evolutionary periods in Earth’s history, making it a rare and scientifically important addition to fossil collections and natural history displays.

 

Additional information

Era

Permian

Origin

Madagascar

Permian Information

The Permian Period (299–252 million years ago) was a time of dramatic climate shifts and evolutionary advancements, marking the end of the Paleozoic Era. Initially, the climate was warm and humid, supporting vast conifer forests and swampy environments, but it gradually became drier as the supercontinent Pangaea fully formed. This led to the expansion of early reptiles, including synapsids like Dimetrodon, which were distant ancestors of mammals. Amphibians thrived in wetlands, while the first conifer trees became dominant. In the oceans, ammonites, brachiopods, and early sharks flourished. However, the Permian ended with the largest mass extinction in Earth’s history, the Permian-Triassic Extinction, wiping out nearly 90% of marine species and 70% of land species, paving the way for the rise of dinosaurs in the Triassic.

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