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Ordovician Fossil Bioturbated Hypersaline Microbial Lagoonal Mat, Richmond Group, Wisconsin USA

Original price was: £144.00.Current price is: £115.20.

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity

 

**Please note: Some fossils maybe propped up for photo purposes**

 

Specimen: Marbleized Stromatolite (Fossil Algae)

Age: Lower Cambrian

Location: Norway

Scale cube=1cm:Full sizing please see photo

 

A fossil stromatolite is a layered, sedimentary formation created by the activity of ancient microbial communities, particularly cyanobacteria (blue-green algae). These structures are among the oldest evidence of life on Earth, dating back to over 3.5 billion years ago.

Key Features of Fossil Stromatolites:

  1. Layered Structure: Stromatolites are characterized by their distinct, layered appearance. These layers are formed by the trapping, binding, and cementation of sedimentary grains by microbial mats.
  2. Microbial Activity: Cyanobacteria play a crucial role in the formation of stromatolites. These microorganisms photosynthesize, producing oxygen as a byproduct, which contributed to the oxygenation of Earth’s atmosphere.
  3. Sedimentation: The microorganisms in the mats trap and bind sediments from the water, creating a layered structure over time. These layers can become fossilized, preserving the stromatolite as a rock.
  4. Ancient Records: Fossil stromatolites provide valuable records of early life and environmental conditions on Earth. They offer insights into the evolution of life and the early biosphere.
  5. Locations: Fossil stromatolites are found in various locations worldwide, including Australia (e.g., the Pilbara region), Canada, and parts of Africa. Modern stromatolites can still be found in places like Shark Bay in Australia and certain hot spring environments.

Formation Process:

  1. Microbial Mats: Cyanobacteria form mats on the surface of sediments in shallow water.
  2. Sediment Trapping: These mats trap and bind sediment particles from the water.
  3. Layer Formation: Over time, additional layers of sediment are trapped, and the process repeats, creating a laminated structure.
  4. Mineral Precipitation: Minerals precipitate from the water, further cementing the layers together.
  5. Fossilization: Over geological time, the layers harden and become fossilized, preserving the stromatolite structure in rock.

Significance:

  • Oxygen Production: Stromatolites played a significant role in the Great Oxidation Event by producing oxygen through photosynthesis.
  • Early Life Evidence: They provide some of the earliest and most compelling evidence of life on Earth, helping scientists understand the origins and evolution of life.
  • Geological Insights: Studying stromatolites helps geologists understand ancient environments, including changes in Earth’s atmosphere and hydrosphere.

In summary, fossil stromatolites are layered structures created by ancient microbial life, providing critical insights into the early history of life and the Earth’s environment.

 

ACTUAL AS SEEN: The image shows the EXACT specimen you will receive. The specimen has been carefully hand selected and photographed. Measurements are as accurate as possible, though be aware measuring precise dimensions can be difficult from irregular shaped items. Whilst we portray colours as close to life-like as we can, colours will vary if taken in sunlight, indoors, from monitor to monitor and device to device. Once this specimen is sold, we will update this listing with new similar selected item, with a new photo and dimensions.

(Actual as seen)

Only 1 left in stock

SKU: FSR370 Category:

Description

Ordovician Fossil Identification

This geological specimen is identified as a bioturbated, hypersaline, microbial lagoonal mat associated with the Richmond Group of the Ordovician and recorded from Wisconsin, USA. It is an excellent choice for fossil collectors, geology enthusiasts, educators and anyone interested in ancient sedimentary environments preserved in the rock record.

Geological Context

The Ordovician Period is well known for significant marine diversification and for the preservation of varied shallow-water and coastal sedimentary environments. The Richmond Group represents Ordovician strata, and material associated with this interval can provide an appealing connection to the marine landscapes and depositional settings of deep geological time.

A lagoonal environment is a relatively restricted coastal setting where water chemistry, circulation and sediment accumulation can differ from those of the open sea. In a hypersaline lagoon, elevated salinity can influence which organisms and microbial communities are able to thrive. Microbial mats may develop as layered, surface-bound communities that trap sediment, bind particles and contribute to the formation or preservation of distinctive sedimentary textures.

Bioturbation and Microbial Mat Features

The identification of this material combines two important geological concepts. Bioturbation refers to the disturbance or reworking of sediment by living organisms. Burrowing, feeding and movement can disrupt originally deposited layers and create textural variations within sedimentary material. These traces are valuable to collectors because they reflect biological activity in an ancient depositional environment rather than representing purely inorganic sedimentary structure.

Microbial lagoonal mats are also significant in sedimentary geology because microbial communities can stabilize sediment surfaces and encourage the development of laminated or textured deposits. When such features are preserved, they offer a visual record of interactions between microorganisms, sediment and water chemistry. The hypersaline setting adds further geological interest by indicating an environment where salinity was an important influence on deposition and preservation.

Collector and Display Appeal

This Ordovician Richmond Group specimen is suited to fossil collections focused on ancient environments, sedimentology, trace structures and microbialite-related textures. It can be displayed as an educational example of how biological activity and environmental conditions may be recorded together in geological material. Its subject matter also makes it a useful conversation piece for collections organized by geological period, depositional environment or fossil formation process.

Location and Sizing

The specimen is associated with Wisconsin, USA. Full sizing is shown in the photographs. The photograph shows a representative example; the specimen supplied may vary naturally in colour, shape, size and detail.

Certificate of Authenticity

This Fossil is a genuine specimen and Includes a Certificate of Authenticity lifetime guarantee generic card.

Additional information

Weight 10 g

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