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Fossil Algal Mounds Stromatolites Conophyton Lower Cambrian Ougnet Morocco Authentic Specimen

Original price was: £180.00.Current price is: £162.00.

Fossil Stromatolites – Ancient Algal Mounds

This listing is for an exceptional fossil specimen of stromatolites (Conophyton), preserved as algal mound structures from the Lower Cambrian deposits of Ougnet, Morocco. Stromatolites are among the most significant fossils in Earth’s history, representing layered biosedimentary structures created by the activity of cyanobacteria and other microbial mats. This carefully chosen piece comes exactly as shown in the photographs, with a scale cube of 1 cm included for reference. You will receive this precise specimen, a genuine and unique piece of early life history, supplied with a Certificate of Authenticity.

Geological Context and Age

The fossil originates from the Lower Cambrian strata of Ougnet, Morocco, a region known for yielding important fossils that shed light on the early diversification of marine ecosystems. The Cambrian Period (approximately 541–485 million years ago) is famous for the “Cambrian Explosion,” a time of rapid evolutionary development when complex organisms began to flourish. Stromatolites such as this specimen predate and extend into this period, representing some of the earliest large-scale evidence of microbial life shaping the Earth’s geology. The Ougnet locality provides excellent preservation conditions, making these stromatolites particularly desirable to collectors and researchers alike.

Stromatolite Morphology – Conophyton

This specimen belongs to the genus Conophyton, characterised by its distinctive conical or mound-like layered growth patterns. These structures were formed by successive layers of cyanobacterial mats trapping and binding sediment, combined with the precipitation of calcium carbonate. Over time, this growth created laminated mounds with clear internal banding. The concentric or wavy layering visible in this fossil is a hallmark of stromatolite growth, recording both the biological activity of microbial communities and the environmental conditions of ancient shallow seas.

Scientific and Historical Importance

Stromatolites are some of the earliest known macroscopic evidence of life, with records extending back more than 3.5 billion years. By the Cambrian, stromatolites such as Conophyton were already well-established in shallow marine environments. These fossils provide crucial insight into early ecosystems, atmospheric oxygen production, and the co-evolution of microbial communities with developing marine fauna. They represent a vital link between biology and geology, showing how life and Earth’s environments have shaped one another across geological time.

Depositional Environment

The stromatolites of Ougnet formed in warm, shallow, sunlit marine waters, where photosynthetic cyanobacteria thrived. Periodic sedimentation events and mineral precipitation played an important role in their preservation, creating robust, layered carbonate mounds. The presence of stromatolites in these deposits indicates stable, shallow-water platforms with low levels of grazing organisms compared to later geological periods. The Cambrian seas of Morocco were dynamic, but they provided ideal conditions for microbial mats to flourish and leave behind these enduring stone records of early life.

A Carefully Chosen Collector’s Piece

This fossil has been selected for its scientific value, aesthetic qualities, and rarity. The well-preserved laminated structures of the stromatolite mounds make it not only a piece of natural art but also a tangible example of life’s earliest builders. Whether displayed as a striking natural specimen, used as an educational aid, or cherished in a private collection, this stromatolite block is a fascinating addition for anyone with an interest in Earth history.

Authenticity and Guarantee

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity. The photographs show the exact piece you will receive, ensuring transparency and trust. Unlike casts or reproductions, this is a natural fossil formed through biological and geological processes more than half a billion years ago.

A Unique Fossil from Deep Time

This Conophyton stromatolite from the Lower Cambrian of Morocco is not just a fossil but a direct connection to the earliest microbial ecosystems that shaped our planet. Its rarity, scientific importance, and natural beauty make it a truly remarkable specimen for collectors, educators, and enthusiasts of palaeontology and deep-time geology.

(Actual as seen)

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Description

Fossil Stromatolites – Ancient Algal Mounds

This listing is for an exceptional fossil specimen of stromatolites (Conophyton), preserved as algal mound structures from the Lower Cambrian deposits of Ougnet, Morocco. Stromatolites are among the most significant fossils in Earth’s history, representing layered biosedimentary structures created by the activity of cyanobacteria and other microbial mats. This carefully chosen piece comes exactly as shown in the photographs, with a scale cube of 1 cm included for reference. You will receive this precise specimen, a genuine and unique piece of early life history, supplied with a Certificate of Authenticity.

Geological Context and Age

The fossil originates from the Lower Cambrian strata of Ougnet, Morocco, a region known for yielding important fossils that shed light on the early diversification of marine ecosystems. The Cambrian Period (approximately 541–485 million years ago) is famous for the “Cambrian Explosion,” a time of rapid evolutionary development when complex organisms began to flourish. Stromatolites such as this specimen predate and extend into this period, representing some of the earliest large-scale evidence of microbial life shaping the Earth’s geology. The Ougnet locality provides excellent preservation conditions, making these stromatolites particularly desirable to collectors and researchers alike.

Stromatolite Morphology – Conophyton

This specimen belongs to the genus Conophyton, characterised by its distinctive conical or mound-like layered growth patterns. These structures were formed by successive layers of cyanobacterial mats trapping and binding sediment, combined with the precipitation of calcium carbonate. Over time, this growth created laminated mounds with clear internal banding. The concentric or wavy layering visible in this fossil is a hallmark of stromatolite growth, recording both the biological activity of microbial communities and the environmental conditions of ancient shallow seas.

Scientific and Historical Importance

Stromatolites are some of the earliest known macroscopic evidence of life, with records extending back more than 3.5 billion years. By the Cambrian, stromatolites such as Conophyton were already well-established in shallow marine environments. These fossils provide crucial insight into early ecosystems, atmospheric oxygen production, and the co-evolution of microbial communities with developing marine fauna. They represent a vital link between biology and geology, showing how life and Earth’s environments have shaped one another across geological time.

Depositional Environment

The stromatolites of Ougnet formed in warm, shallow, sunlit marine waters, where photosynthetic cyanobacteria thrived. Periodic sedimentation events and mineral precipitation played an important role in their preservation, creating robust, layered carbonate mounds. The presence of stromatolites in these deposits indicates stable, shallow-water platforms with low levels of grazing organisms compared to later geological periods. The Cambrian seas of Morocco were dynamic, but they provided ideal conditions for microbial mats to flourish and leave behind these enduring stone records of early life.

A Carefully Chosen Collector’s Piece

This fossil has been selected for its scientific value, aesthetic qualities, and rarity. The well-preserved laminated structures of the stromatolite mounds make it not only a piece of natural art but also a tangible example of life’s earliest builders. Whether displayed as a striking natural specimen, used as an educational aid, or cherished in a private collection, this stromatolite block is a fascinating addition for anyone with an interest in Earth history.

Authenticity and Guarantee

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity. The photographs show the exact piece you will receive, ensuring transparency and trust. Unlike casts or reproductions, this is a natural fossil formed through biological and geological processes more than half a billion years ago.

A Unique Fossil from Deep Time

This Conophyton stromatolite from the Lower Cambrian of Morocco is not just a fossil but a direct connection to the earliest microbial ecosystems that shaped our planet. Its rarity, scientific importance, and natural beauty make it a truly remarkable specimen for collectors, educators, and enthusiasts of palaeontology and deep-time geology.

Additional information

Era

Cambrian

Origin

Morocco

Cambrian Information

The Cambrian Period (541–485 million years ago) was the first period of the Paleozoic Era, marking a dramatic explosion of life known as the Cambrian Explosion. During this time, complex multicellular organisms rapidly diversified, giving rise to the first arthropods, mollusks, echinoderms, and chordates—early ancestors of vertebrates. The climate was generally warm, with high sea levels covering much of the continents, creating vast shallow seas where life thrived. Iconic creatures such as Trilobites, Anomalocaris, and Opabinia dominated the oceans, while the first primitive reefs formed. The Cambrian set the stage for the evolution of modern animal groups and the complexity of marine ecosystems.

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