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Stylimis Turtle Shell Fragment Fossil Oligocene South Dakota USA 30 Million Years

Original price was: £6.00.Current price is: £5.40.

Stylimis Turtle Shell Fragment – Oligocene Fossil (30 Million Years Old), South Dakota, USA

This authentic Stylimis turtle shell fragment is a genuine fossil specimen dating back approximately 30 million years to the Oligocene Epoch. Collected from the fossil-rich sediments of South Dakota, USA, this piece represents a remarkable glimpse into the diverse reptilian fauna that inhabited North America during the early Cenozoic era. The photographs show a representative example of the specimen you will receive, with individual pieces ranging from 5–45 mm. A 1 cm scale cube is included for accurate size comparison. All of our Fossils are 100% Genuine Specimens and come with a Certificate of Authenticity.

Geological Age and Formation

The fossil dates to the Oligocene Epoch (approx. 34–23 million years ago), a period of significant global cooling following the Eocene–Oligocene transition. During this time, the region now known as South Dakota formed part of a vast inland ecosystem of river systems, floodplains, and woodland environments inhabited by crocodilians, turtles, early horses, oreodonts, rhinos, canids, and diverse bird species.

Fossils from this region are typically preserved within:

  • Fluvial sandstones
  • Clay-rich floodplain deposits
  • Volcanic ash layers, which sometimes provide precise dating

These sediments created ideal conditions for the long-term preservation of reptile bone and shell material.

Fossil Type, Species, and Classification

Fossil Type

  • Shell fragment from a prehistoric turtle belonging to the genus Stylimis.

Taxonomy

  • Class: Reptilia
  • Order: Testudines
  • Family: Likely associated with Emydidae or closely related families typical of Oligocene North American turtles
  • Genus: Stylimis

While full classification of isolated fragments requires comparative analysis, Stylimis is known for its distinctive shell structure and widespread presence in Oligocene sediments across the Great Plains.

Morphological Features

Each fragment displays characteristic features of prehistoric turtle shell material, including:

  • Thick, durable bone plates (scutes) forming part of the carapace or plastron
  • Visible growth sutures, where neighbouring scutes once joined
  • Natural curvature, indicating whether the fragment originated from the dome-like carapace or the flatter plastron
  • Fine surface ornamentation such as ridges, grooves, or subtle polygonal patterns
  • Solid mineralised structure, resulting from millions of years of diagenesis

These details allow paleontologists and collectors to identify turtle fragments with confidence and appreciate the complexity of ancient reptile anatomy.

Depositional Environment

The Oligocene landscape of South Dakota belonged to the White River Group, one of the most important Cenozoic fossil deposits in the world. This region was defined by:

  • Seasonal rivers and braided channels
  • Wide open savanna–woodland habitats
  • Volcanic ashfalls that buried living environments and preserved remains
  • Sediment-rich flood basins, perfect for fossilisation

Turtles were abundant in these environments, inhabiting lakes, streams, and wetlands while leaving behind a wealth of fossil evidence.

Scientific Importance

Stylimis turtle fossils help researchers understand:

  • The spread and diversification of early North American turtles
  • Shell morphology and evolutionary transitions within Testudines
  • Paleoecology of Oligocene river and wetland ecosystems
  • Climatic changes following the Eocene–Oligocene boundary

Shell fragments are particularly valuable because they preserve surface patterns that provide insight into growth, age, and environmental adaptation.

Collector Grade and Display Appeal

This fossil fragment has been chosen for:

  • Strong, solid preservation
  • Clear bone texture and scute structure
  • Natural mineral tones typical of South Dakota Oligocene fossils
  • High scientific and educational value

Despite their small size (5–45 mm), these fragments make excellent reference pieces for fossil identification, collection building, and teaching.

Ideal for Collectors, Educators, and Fossil Enthusiasts

This Stylimis Turtle Shell Fragment from the Oligocene of South Dakota provides a fascinating link to the ancient reptile life that once flourished across prehistoric North America. Its preservation, provenance, and geological importance make it a meaningful addition to any fossil collection or natural history display.

(Regular, will differ to photo)

Only 5 left in stock

SKU: FS7722 Category:

Description

Stylimis Turtle Shell Fragment – Oligocene Fossil (30 Million Years Old), South Dakota, USA

This authentic Stylimis turtle shell fragment is a genuine fossil specimen dating back approximately 30 million years to the Oligocene Epoch. Collected from the fossil-rich sediments of South Dakota, USA, this piece represents a remarkable glimpse into the diverse reptilian fauna that inhabited North America during the early Cenozoic era. The photographs show a representative example of the specimen you will receive, with individual pieces ranging from 5–45 mm. A 1 cm scale cube is included for accurate size comparison. All of our Fossils are 100% Genuine Specimens and come with a Certificate of Authenticity.

Geological Age and Formation

The fossil dates to the Oligocene Epoch (approx. 34–23 million years ago), a period of significant global cooling following the Eocene–Oligocene transition. During this time, the region now known as South Dakota formed part of a vast inland ecosystem of river systems, floodplains, and woodland environments inhabited by crocodilians, turtles, early horses, oreodonts, rhinos, canids, and diverse bird species.

Fossils from this region are typically preserved within:

  • Fluvial sandstones
  • Clay-rich floodplain deposits
  • Volcanic ash layers, which sometimes provide precise dating

These sediments created ideal conditions for the long-term preservation of reptile bone and shell material.

Fossil Type, Species, and Classification

Fossil Type

  • Shell fragment from a prehistoric turtle belonging to the genus Stylimis.

Taxonomy

  • Class: Reptilia
  • Order: Testudines
  • Family: Likely associated with Emydidae or closely related families typical of Oligocene North American turtles
  • Genus: Stylimis

While full classification of isolated fragments requires comparative analysis, Stylimis is known for its distinctive shell structure and widespread presence in Oligocene sediments across the Great Plains.

Morphological Features

Each fragment displays characteristic features of prehistoric turtle shell material, including:

  • Thick, durable bone plates (scutes) forming part of the carapace or plastron
  • Visible growth sutures, where neighbouring scutes once joined
  • Natural curvature, indicating whether the fragment originated from the dome-like carapace or the flatter plastron
  • Fine surface ornamentation such as ridges, grooves, or subtle polygonal patterns
  • Solid mineralised structure, resulting from millions of years of diagenesis

These details allow paleontologists and collectors to identify turtle fragments with confidence and appreciate the complexity of ancient reptile anatomy.

Depositional Environment

The Oligocene landscape of South Dakota belonged to the White River Group, one of the most important Cenozoic fossil deposits in the world. This region was defined by:

  • Seasonal rivers and braided channels
  • Wide open savanna–woodland habitats
  • Volcanic ashfalls that buried living environments and preserved remains
  • Sediment-rich flood basins, perfect for fossilisation

Turtles were abundant in these environments, inhabiting lakes, streams, and wetlands while leaving behind a wealth of fossil evidence.

Scientific Importance

Stylimis turtle fossils help researchers understand:

  • The spread and diversification of early North American turtles
  • Shell morphology and evolutionary transitions within Testudines
  • Paleoecology of Oligocene river and wetland ecosystems
  • Climatic changes following the Eocene–Oligocene boundary

Shell fragments are particularly valuable because they preserve surface patterns that provide insight into growth, age, and environmental adaptation.

Collector Grade and Display Appeal

This fossil fragment has been chosen for:

  • Strong, solid preservation
  • Clear bone texture and scute structure
  • Natural mineral tones typical of South Dakota Oligocene fossils
  • High scientific and educational value

Despite their small size (5–45 mm), these fragments make excellent reference pieces for fossil identification, collection building, and teaching.

Ideal for Collectors, Educators, and Fossil Enthusiasts

This Stylimis Turtle Shell Fragment from the Oligocene of South Dakota provides a fascinating link to the ancient reptile life that once flourished across prehistoric North America. Its preservation, provenance, and geological importance make it a meaningful addition to any fossil collection or natural history display.

Additional information

Era

Oligocene

Origin

USA

Oligocene Information

The Oligocene Epoch (33.9–23 million years ago) was a time of cooling climates and the transition to more modern ecosystems. Following the warm Eocene, global temperatures dropped, leading to the expansion of grasslands and the first permanent Antarctic ice sheets. Forests shrank, and grazing mammals like early horses, deer, and rhinos thrived in open landscapes. Primates evolved, with the ancestors of monkeys and apes appearing. In the oceans, whales diversified, and the first seals emerged. The Oligocene also saw the formation of major ocean currents, which further shaped Earth's climate. This period set the stage for the Miocene, with continued cooling and the rise of more modern mammal species.

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