A-Grade Stromatolite Fossil, Algae Bacteria, Cotham Marble, triassic

Description

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: Stromatolite Section

Age: Cotham Marble, Triassic

Location: Bristol, UK

Scale cube=1cm:Full sizing please see photo

**The photo shows the ACTUAL specimen you will receive**

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.