
Location: 2.5hours drive south of Carnarvon between Cape Leeuwin and Cape Naturaliste Western Australia.
10 things about Hamelin Pool Stromatolites
- The Hamelin Pool cyanobacteria dominated Earth for over 2 billion years
- The original stromatolite colonies were responsible for raising the oxygen level to 20% of atmospheric gases.
- When the sea receded approximately a thousand years ago, many of the stromatolite died due to prolonged exposure to Earth's atmosphere.
- Tidal movement, waves and swirling sand allow the stromatolites to form unique shapes however stromatolites below the water surface tend to form a club like shape.
- 60 years ago, the locals banned wagons carrying wool from nearby ships. Deep ruts made from the wagon's wheels are still visible today on living stromatolite mats near the boardwalk.
- It can take 30 years for stromatolites to grow 1cm.
- Depending on the stromatolites location, they may grow as mats instead of sculptures.
- The red pigment capping the stromatolite stopped growing between 500-1,000 years ago when the sea level receded.
- Stromatolite layers grow in an outward fashion, similar to the growth rings of a tree. Their outer layer is a thin strip of active life with a sticky film to trap drifting shells and sand.
- Scientists believe growth rings provide information about environmental transformations including changes in duration of light, angle of the sun, even the earth rotation rate!
If you are a budding scientist, or have a quirky interest in bacteria like me, visiting Hamelin Pools is something to put on your bucket list!
Watch and share the video about Hamelin Pool Stromatolites below:
If you would like further information head to:
Department of Parks and Wildlife
Hamelin Pool
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