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Rare Mazon Creek Fossil Fern Macroneuropteris Carboniferous Illinois USA with COA Authentic

£60.00

Authentic Mazon Creek Fossil Fern – Macroneuropteris

This beautifully preserved Mazon Creek fossil fern nodule features clear impressions of Macroneuropteris, one of the most iconic seed ferns of the late Carboniferous Period. Dating back approximately 307–309 million years, this specimen originates from the world-renowned Mazon Creek fossil beds in Illinois, USA. Split open to reveal the fossil impression within the ironstone concretion, this piece offers a rare and detailed glimpse into the dense tropical coal swamp forests that once dominated Earth’s equatorial regions. The fossil shown is the exact specimen you will receive, and it comes complete with a Certificate of Authenticity.

Geological Context

  • Geological Period: Carboniferous (Pennsylvanian Subperiod)
  • Age: ~307–309 million years old
  • Formation: Francis Creek Shale, Mazon Creek Lagerstätte
  • Location: Mazon Creek, Illinois, USA

The Mazon Creek Lagerstätte is celebrated worldwide for its exceptional preservation of plants and animals within siderite nodules. Rapid burial and mineralisation created fossils of extraordinary detail, making this site one of the most significant paleontological locations for studying late Paleozoic ecosystems.

Scientific Classification

  • Kingdom: Plantae
  • Division: Pteridospermatophyta (Seed Ferns)
  • Order: Medullosales
  • Genus: Macroneuropteris

Unlike modern ferns, seed ferns like Macroneuropteris reproduced by seeds rather than spores, making them an important evolutionary step between primitive vascular plants and more advanced seed-bearing flora.

Morphological Features

This specimen shows the distinctive features of Macroneuropteris:

  • Large Leaflets (Pinnae): Broad, lance-shaped fronds with gently tapering ends.
  • Vein Structure: Prominent midrib with fine lateral veins branching outward.
  • Surface Texture: Fine details of the leaf surface, occasionally with faint venation preserved.

The large size of Macroneuropteris fronds made them a dominant component of Carboniferous swamp forests, often forming dense canopies that shaded the forest floor.

Paleoenvironment and Significance

During the Carboniferous, the region that is now Illinois was positioned near the equator and covered in humid, swampy lowlands. These ecosystems were rich in giant lycopsids, horsetails, ferns, and seed ferns such as Macroneuropteris. Over millions of years, the accumulation of plant matter created the vast coal deposits that the period is famous for.

The Mazon Creek fossil site is particularly valued because it preserves a wide range of organisms, from delicate plants like ferns to rare soft-bodied animals, all trapped in siderite nodules. The fossilisation process at this site captured remarkable details, allowing scientists and collectors alike to study Carboniferous biodiversity with unmatched clarity.

Key Details

  • Specimen: Macroneuropteris fossil fern
  • Type: Split siderite nodule fossil
  • Age: Carboniferous (~307–309 million years)
  • Location: Mazon Creek, Illinois, USA
  • Authenticity: 100% genuine fossil with Certificate of Authenticity
  • Sizing: Shown with 1cm scale cube in photos

Collectability and Display Value

Fossils from Mazon Creek are globally sought after for both their scientific importance and aesthetic appeal. This Macroneuropteris specimen offers exceptional display value, highlighting the beauty of ancient plant life. Its historical significance makes it an ideal acquisition for collectors, educators, or anyone fascinated by the origins of Earth’s coal forests.

Owning this fossil means owning a genuine piece of Carboniferous history—an elegant reminder of the prehistoric tropical landscapes that shaped our planet’s natural heritage.

(Actual as seen)

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SKU: UF0767 Category:

Description

Authentic Mazon Creek Fossil Fern – Macroneuropteris

This beautifully preserved Mazon Creek fossil fern nodule features clear impressions of Macroneuropteris, one of the most iconic seed ferns of the late Carboniferous Period. Dating back approximately 307–309 million years, this specimen originates from the world-renowned Mazon Creek fossil beds in Illinois, USA. Split open to reveal the fossil impression within the ironstone concretion, this piece offers a rare and detailed glimpse into the dense tropical coal swamp forests that once dominated Earth’s equatorial regions. The fossil shown is the exact specimen you will receive, and it comes complete with a Certificate of Authenticity.

Geological Context

  • Geological Period: Carboniferous (Pennsylvanian Subperiod)
  • Age: ~307–309 million years old
  • Formation: Francis Creek Shale, Mazon Creek Lagerstätte
  • Location: Mazon Creek, Illinois, USA

The Mazon Creek Lagerstätte is celebrated worldwide for its exceptional preservation of plants and animals within siderite nodules. Rapid burial and mineralisation created fossils of extraordinary detail, making this site one of the most significant paleontological locations for studying late Paleozoic ecosystems.

Scientific Classification

  • Kingdom: Plantae
  • Division: Pteridospermatophyta (Seed Ferns)
  • Order: Medullosales
  • Genus: Macroneuropteris

Unlike modern ferns, seed ferns like Macroneuropteris reproduced by seeds rather than spores, making them an important evolutionary step between primitive vascular plants and more advanced seed-bearing flora.

Morphological Features

This specimen shows the distinctive features of Macroneuropteris:

  • Large Leaflets (Pinnae): Broad, lance-shaped fronds with gently tapering ends.
  • Vein Structure: Prominent midrib with fine lateral veins branching outward.
  • Surface Texture: Fine details of the leaf surface, occasionally with faint venation preserved.

The large size of Macroneuropteris fronds made them a dominant component of Carboniferous swamp forests, often forming dense canopies that shaded the forest floor.

Paleoenvironment and Significance

During the Carboniferous, the region that is now Illinois was positioned near the equator and covered in humid, swampy lowlands. These ecosystems were rich in giant lycopsids, horsetails, ferns, and seed ferns such as Macroneuropteris. Over millions of years, the accumulation of plant matter created the vast coal deposits that the period is famous for.

The Mazon Creek fossil site is particularly valued because it preserves a wide range of organisms, from delicate plants like ferns to rare soft-bodied animals, all trapped in siderite nodules. The fossilisation process at this site captured remarkable details, allowing scientists and collectors alike to study Carboniferous biodiversity with unmatched clarity.

Key Details

  • Specimen: Macroneuropteris fossil fern
  • Type: Split siderite nodule fossil
  • Age: Carboniferous (~307–309 million years)
  • Location: Mazon Creek, Illinois, USA
  • Authenticity: 100% genuine fossil with Certificate of Authenticity
  • Sizing: Shown with 1cm scale cube in photos

Collectability and Display Value

Fossils from Mazon Creek are globally sought after for both their scientific importance and aesthetic appeal. This Macroneuropteris specimen offers exceptional display value, highlighting the beauty of ancient plant life. Its historical significance makes it an ideal acquisition for collectors, educators, or anyone fascinated by the origins of Earth’s coal forests.

Owning this fossil means owning a genuine piece of Carboniferous history—an elegant reminder of the prehistoric tropical landscapes that shaped our planet’s natural heritage.

Additional information

Era

Carboniferous

Origin

USA

Carboniferous Information

The Carboniferous Period (359–299 million years ago) was a time of vast forests, giant insects, and the first reptiles. Named for its extensive coal deposits, this period saw lush swamps filled with towering lycophyte trees, ferns, and horsetails, which would later become today’s coal reserves. The climate was warm and humid, with high oxygen levels fueling the growth of giant arthropods like the dragonfly-like Meganeura and the massive millipede Arthropleura. Amphibians thrived in swampy environments, while the first reptiles evolved, laying eggs on land. In the oceans, sharks and early bony fish dominated, and corals flourished in warm, shallow seas. The period ended with a cooling climate and glaciation, leading to the drying of swamps and the decline of many species.

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