Snowy Pass Stromatolite WY [133gm ~ 2.1 Ga]
Brand : Sciencemall-USA
- SKU:
- JPT-15291
- Condition:
- New
- Availability:
- Usually ships in 24 hours.
- Weight:
- 1.00 LBS
- Minimum Purchase:
- 1 unit
- Maximum Purchase:
- 1 unit
- Shipping:
- Calculated at Checkout
Snowy Pass Stromatolite: Glaciation and the Great Oxidation Event
This Snowy Pass Stromatolite is an extraordinary specimen from the Paleoproterozoic Era, approximately 2.1 billion years old. Stromatolites provide tangible connections to a transformative period in Earth's history, in the aftermath of the Huronian Glaciation and the rise of the Great Oxidation Event.
Geological Context
Formed during the Orosirian Period (2.05–1.8 Ga), Paleoproterozoic Era, the Snowy Pass Stromatolites emerged in the aftermath of the Huronian Glaciation. As the glaciers receded, shallow marine environments flourished. It was the ideal time and conditions for microbial life as cyanobacteria to flourish. Cyanobacteria in these habitats constructed stromatolites by trapping and binding sediment, creating a layered record of life adapting to variations in climatic events.
Stromatolites: Nature’s Ancient Builders
Stromatolites are layered sedimentary structures created by microbial communities, predominantly cyanobacteria. These early photosynthesizers played a critical role in oxygenating Earth’s atmosphere. This Snowy Pass stromatolite displays characteristic banded layers, showing growth influenced by environmental cycles. Each layer tells an interesting story about early microbial life's resilience and its contribution to shaping Earth’s biosphere.
Specimen Details:
- Size: 60mm L X 52mm W X 28mm D
- Weight: 166 grams
- Finish: Smooth face, rough back
- What is Included: Certificate of Authenticity, tag, tag stand, and information about the Snowy Pass stromatolites and scientific paper "The Early Earth's Atmosphere, the Huronian Glaciation and the Rise of Stromatolites" (Note: The display stand and sizing cube are not included.)
Significance of the Orosirian Period
- Post-Huronian Recovery: Microbial life thrived as Earth’s climate stabilized, creating productive shallow marine ecosystems.
- Great Oxidation Event (GOE): Cyanobacteria drove oxygen production, transforming Earth’s atmosphere and enabling aerobic life.
- Banded Iron Formations (BIFs): Oxygen reacted with oceanic iron, forming distinctive geological features.
- Impact Events: Asteroid impacts, such as those forming the Vredefort Crater and Sudbury Impact Structure, highlight the dynamic nature of Earth’s early meteorite and asteroid bombardment history.
- Supercontinent Activity: Tectonic movements fostered ocean circulation and nutrient distribution, supporting microbial growth.
Scientific and Educational Value
The Snowy Pass Stromatolite offers invaluable insights into:
- Early Life at the Beginning of the Great Oxygen Event: Demonstrates life’s adaptability and early evolution
- Atmospheric Evolution: Showcases microbial contributions to oxygenation and the rise of new atmospheric conditions
- Geological Processes: great example of sedimentation and environmental cycles from billions of years ago.
This specimen is ideal for researchers, educators, and collectors, providing a window into Earth's ancient history and the interaction of life and environment during the Paleoproterozoic Era.
Physical Characteristics
- Age: Approximately 2.1 billion years old
- Composition: Carbonate minerals with fine-grained sediments
- Appearance: Banded layers formed by microbial growth and sediment trapping
Applications
This specimen is versatile, with applications in:
- Education: Perfect for teaching about early life, the Great Oxidation Event, and atmospheric evolution.
- Research: Provides a tangible resource for studying ancient microbial ecosystems.
- Collections: A scientifically significant addition to private and institutional collections.
- Display: A great centerpiece for geology collections, museums, classrooms, or personal exhibits.
Conclusion
This Snowy Pass Stromatolite is a great specimen for studying, Snowball Earth, Glaciers, the Great Oxidation Event. It is an example of the exceptional transformative power of one of the first microbial mat ecosystems, the stromatolites.