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Rare Mazon Creek Fossil Fern Mariopteris Carboniferous Plant Fossil Illinois USA COA

£60.00

Authentic Mazon Creek Fossil Fern – Mariopteris

This specimen is a beautifully preserved Mazon Creek fossil fern of the genus Mariopteris, encased in its natural siderite nodule and split to reveal the fossil impression inside. Dating back to the Carboniferous Period, approximately 307–309 million years ago, this fossil comes from the world-renowned Mazon Creek Lagerstätte in Illinois, USA. Famous for its exceptional preservation, Mazon Creek offers collectors a rare glimpse into ancient swamp ecosystems. The fossil shown is the exact piece you will receive, and it is accompanied by a Certificate of Authenticity, guaranteeing that it is a 100% genuine specimen.

Geological Context

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

The Francis Creek Shale was deposited in a deltaic swamp environment, where rapid burial in fine sediments created ideal conditions for the preservation of plants and animals. Fossils from this site are often found in siderite nodules, which protected delicate organic structures from decay and compression, leaving us with exquisitely detailed impressions.

Scientific Classification

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

Mariopteris was part of the seed ferns, a now-extinct group of plants that dominated the lush Carboniferous forests. Although resembling modern ferns in appearance, these plants reproduced by seeds, making them more advanced than true ferns of the period.

Morphological Features

The fossil captures the diagnostic features of Mariopteris:

  • Fronds: Pinnate fronds with regularly arranged pinnules.
  • Leaf Shape: Characteristically lobed pinnules with distinct outlines.
  • Venation: Well-developed veins radiating from a central midrib.
  • Surface Detail: Preserved textures show fine leaf architecture.

These features distinguish Mariopteris from other Carboniferous plants such as Neuropteris or Pecopteris, making it a particularly desirable fossil for collectors who want variety in their Mazon Creek specimens.

Paleoenvironment and Significance

During the Carboniferous, Illinois lay close to the equator and was covered by dense swamp forests dominated by seed ferns, lycopsids, horsetails, and tree ferns. These plants contributed to the vast peat deposits that later formed coal seams.

The Mazon Creek Lagerstätte is unique for its ability to preserve both plant and animal life in such fine detail. Fossils like this Mariopteris specimen provide vital information about the ecology of ancient swamp forests, highlighting the role of seed ferns in shaping the Carboniferous landscape. Their evolutionary significance lies in the transition toward more advanced seed-bearing plants that would eventually dominate terrestrial ecosystems.

Key Details

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

Collectability and Display Value

Mazon Creek fossils are prized worldwide for their rarity and beauty. Mariopteris is a sought-after genus among fossil plant collectors because of its striking frond patterns and distinct venation. This specimen offers both scientific value and aesthetic appeal, making it ideal for display in a collection, study, or educational setting.

Owning this fossil means holding a piece of Earth’s deep history—an ancient seed fern that once thrived in the coal swamps of the Carboniferous. It is a natural work of art and a scientifically important relic of prehistoric plant life.

(Actual as seen)

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Description

Authentic Mazon Creek Fossil Fern – Mariopteris

This specimen is a beautifully preserved Mazon Creek fossil fern of the genus Mariopteris, encased in its natural siderite nodule and split to reveal the fossil impression inside. Dating back to the Carboniferous Period, approximately 307–309 million years ago, this fossil comes from the world-renowned Mazon Creek Lagerstätte in Illinois, USA. Famous for its exceptional preservation, Mazon Creek offers collectors a rare glimpse into ancient swamp ecosystems. The fossil shown is the exact piece you will receive, and it is accompanied by a Certificate of Authenticity, guaranteeing that it is a 100% genuine specimen.

Geological Context

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

The Francis Creek Shale was deposited in a deltaic swamp environment, where rapid burial in fine sediments created ideal conditions for the preservation of plants and animals. Fossils from this site are often found in siderite nodules, which protected delicate organic structures from decay and compression, leaving us with exquisitely detailed impressions.

Scientific Classification

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

Mariopteris was part of the seed ferns, a now-extinct group of plants that dominated the lush Carboniferous forests. Although resembling modern ferns in appearance, these plants reproduced by seeds, making them more advanced than true ferns of the period.

Morphological Features

The fossil captures the diagnostic features of Mariopteris:

  • Fronds: Pinnate fronds with regularly arranged pinnules.
  • Leaf Shape: Characteristically lobed pinnules with distinct outlines.
  • Venation: Well-developed veins radiating from a central midrib.
  • Surface Detail: Preserved textures show fine leaf architecture.

These features distinguish Mariopteris from other Carboniferous plants such as Neuropteris or Pecopteris, making it a particularly desirable fossil for collectors who want variety in their Mazon Creek specimens.

Paleoenvironment and Significance

During the Carboniferous, Illinois lay close to the equator and was covered by dense swamp forests dominated by seed ferns, lycopsids, horsetails, and tree ferns. These plants contributed to the vast peat deposits that later formed coal seams.

The Mazon Creek Lagerstätte is unique for its ability to preserve both plant and animal life in such fine detail. Fossils like this Mariopteris specimen provide vital information about the ecology of ancient swamp forests, highlighting the role of seed ferns in shaping the Carboniferous landscape. Their evolutionary significance lies in the transition toward more advanced seed-bearing plants that would eventually dominate terrestrial ecosystems.

Key Details

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

Collectability and Display Value

Mazon Creek fossils are prized worldwide for their rarity and beauty. Mariopteris is a sought-after genus among fossil plant collectors because of its striking frond patterns and distinct venation. This specimen offers both scientific value and aesthetic appeal, making it ideal for display in a collection, study, or educational setting.

Owning this fossil means holding a piece of Earth’s deep history—an ancient seed fern that once thrived in the coal swamps of the Carboniferous. It is a natural work of art and a scientifically important relic of prehistoric plant life.

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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