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Rare Mazon Creek Split Fossil Fern Nodule Pecopteris Leaves Carboniferous Illinois USA with Certificate of Authenticity

£84.00

Genuine Mazon Creek Fossil Fern – Pecopteris Leaves

This listing is for an authentic Mazon Creek split fossil fern nodule featuring beautifully preserved Pecopteris leaves from the Carboniferous Period. Found in the world-famous Mazon Creek deposits of Illinois, USA, this fossil dates back around 307 million years and provides an exceptional glimpse into the lush tropical forests that once dominated Earth. The specimen comes from a siderite nodule carefully split to reveal delicate plant impressions, showing remarkable natural detail. The photos display the actual specimen you will receive, with a 1 cm scale cube included for accurate sizing. As with all of our specimens, this piece comes with a Certificate of Authenticity.

Geological Context

  • Geological Period: Carboniferous (Pennsylvanian Subperiod)
  • Age: Approx. 307 million years old
  • Formation: Francis Creek Shale, Carbondale Formation
  • Locality: Mazon Creek, Illinois, USA

The Mazon Creek fossil beds are renowned worldwide for their extraordinary preservation of both flora and fauna. Encased within ironstone concretions, these fossils were sealed quickly after burial in deltaic muds, preserving fine detail rarely seen in plant fossils.

Scientific Classification

  • Kingdom: Plantae
  • Order: Marattiales
  • Genus: Pecopteris

Pecopteris was one of the most abundant fern types in Carboniferous coal forests. The name refers to the characteristic fern fronds with pinnate leaves, which often resemble the foliage of modern ferns, although the group represents seed ferns (pteridosperms) rather than true ferns.

Morphological Features

This specimen displays the classic features of Pecopteris:

  • Frond Structure: Pinnately arranged leaflets with a central rachis.
  • Venation: Clear central midrib in each leaflet with fine, regular side veins.
  • Preservation: Crisp impressions capturing the leaf outlines and textures in exquisite detail.

These features made Pecopteris one of the most easily recognisable plants of the Carboniferous swamps. The broad fronds allowed these plants to thrive in the low-light, dense forest environments of equatorial coal swamps.

Paleoenvironment and Significance

During the Carboniferous, Illinois was located near the equator, covered in vast wetlands and tropical forests. These swampy environments supported an incredible diversity of plants, from giant lycopsid trees to horsetails, seed ferns, and early conifers. Fossils such as this Pecopteris leaf help reconstruct the biodiversity of these ecosystems, which ultimately formed much of the world’s coal reserves.

The Mazon Creek deposits are particularly significant because they preserve both the flora and fauna of the Carboniferous, providing a complete ecological snapshot of these ancient forests.

Key Details

  • Fossil Type: Split siderite nodule with Pecopteris fern leaves
  • Age: Carboniferous (~307 million years)
  • Location: Mazon Creek, Illinois, USA
  • Authenticity: 100% genuine specimen with Certificate of Authenticity
  • Size: Please see photos with 1 cm scale cube

Collectability and Display

Mazon Creek fossils are highly sought after by collectors and institutions alike for their outstanding preservation and scientific importance. This Pecopteris specimen is not only a fascinating scientific relic but also a natural work of art, showcasing the fine detail of ancient plant life. Its well-defined frond structure makes it a desirable display piece, while its historical and geological significance makes it an excellent addition to any collection.

Owning a Mazon Creek Pecopteris fossil allows you to hold in your hands a genuine piece of Earth’s prehistoric past, beautifully preserved for over 300 million years. This fossil is both a collectible treasure and a stunning educational specimen, perfect for collectors, enthusiasts, or as a unique natural history gift.

(Actual as seen)

Out of stock

SKU: UF0792 Category:

Description

Genuine Mazon Creek Fossil Fern – Pecopteris Leaves

This listing is for an authentic Mazon Creek split fossil fern nodule featuring beautifully preserved Pecopteris leaves from the Carboniferous Period. Found in the world-famous Mazon Creek deposits of Illinois, USA, this fossil dates back around 307 million years and provides an exceptional glimpse into the lush tropical forests that once dominated Earth. The specimen comes from a siderite nodule carefully split to reveal delicate plant impressions, showing remarkable natural detail. The photos display the actual specimen you will receive, with a 1 cm scale cube included for accurate sizing. As with all of our specimens, this piece comes with a Certificate of Authenticity.

Geological Context

  • Geological Period: Carboniferous (Pennsylvanian Subperiod)
  • Age: Approx. 307 million years old
  • Formation: Francis Creek Shale, Carbondale Formation
  • Locality: Mazon Creek, Illinois, USA

The Mazon Creek fossil beds are renowned worldwide for their extraordinary preservation of both flora and fauna. Encased within ironstone concretions, these fossils were sealed quickly after burial in deltaic muds, preserving fine detail rarely seen in plant fossils.

Scientific Classification

  • Kingdom: Plantae
  • Order: Marattiales
  • Genus: Pecopteris

Pecopteris was one of the most abundant fern types in Carboniferous coal forests. The name refers to the characteristic fern fronds with pinnate leaves, which often resemble the foliage of modern ferns, although the group represents seed ferns (pteridosperms) rather than true ferns.

Morphological Features

This specimen displays the classic features of Pecopteris:

  • Frond Structure: Pinnately arranged leaflets with a central rachis.
  • Venation: Clear central midrib in each leaflet with fine, regular side veins.
  • Preservation: Crisp impressions capturing the leaf outlines and textures in exquisite detail.

These features made Pecopteris one of the most easily recognisable plants of the Carboniferous swamps. The broad fronds allowed these plants to thrive in the low-light, dense forest environments of equatorial coal swamps.

Paleoenvironment and Significance

During the Carboniferous, Illinois was located near the equator, covered in vast wetlands and tropical forests. These swampy environments supported an incredible diversity of plants, from giant lycopsid trees to horsetails, seed ferns, and early conifers. Fossils such as this Pecopteris leaf help reconstruct the biodiversity of these ecosystems, which ultimately formed much of the world’s coal reserves.

The Mazon Creek deposits are particularly significant because they preserve both the flora and fauna of the Carboniferous, providing a complete ecological snapshot of these ancient forests.

Key Details

  • Fossil Type: Split siderite nodule with Pecopteris fern leaves
  • Age: Carboniferous (~307 million years)
  • Location: Mazon Creek, Illinois, USA
  • Authenticity: 100% genuine specimen with Certificate of Authenticity
  • Size: Please see photos with 1 cm scale cube

Collectability and Display

Mazon Creek fossils are highly sought after by collectors and institutions alike for their outstanding preservation and scientific importance. This Pecopteris specimen is not only a fascinating scientific relic but also a natural work of art, showcasing the fine detail of ancient plant life. Its well-defined frond structure makes it a desirable display piece, while its historical and geological significance makes it an excellent addition to any collection.

Owning a Mazon Creek Pecopteris fossil allows you to hold in your hands a genuine piece of Earth’s prehistoric past, beautifully preserved for over 300 million years. This fossil is both a collectible treasure and a stunning educational specimen, perfect for collectors, enthusiasts, or as a unique natural history gift.

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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