Stromatolites are primarily formed by the activity of cyanobacteria, which are photosynthetic microorganisms. These bacteria create layered structures by trapping sediments and precipitating calcium carbonate, leading to the formation of these ancient rock-like formations. While stromatolites are associated with microbial life, they can also host a diverse range of other microorganisms and small invertebrates in their ecosystems.
Microbial mats and sediment layers are typically found on the outer surfaces of stromatolites. These structures are formed by the trapping and binding of sediment particles by microbial communities, resulting in layered structures visible on the surface.
The oldest fossils in Australia are 3.5 billion year old stromatolites. Stromatolites are layered accretions of prokaryotic microbes, most often made up of photosynthetic organisms. Stromatolites still live in Australia today.
The are examples of stromatolites still living. They are not extinct.
The stromatolites are the layered mounds, columns, and the sheet-like sedimentary rocks.
Stromatolites were much more abundant on the planet in Precambrian times which means that fossils found around stromatolites are typically from the Precambrian era.
Stromatolites form in shallow, saline or hypersaline environments such as coastal lagoons, estuaries, and hypersaline lakes. They are also found in some marine environments where conditions are suitable for their growth, such as in the Bahamas and Shark Bay in Australia.
Stromatolites are typically found in shallow marine environments within a cave, such as near the cave entrance where light can penetrate for photosynthesis to occur. These microbial mats form layers of sediment and minerals over time, creating structures that can be observed in cave environments.
Stromatolites.
Stromatolites
The oldest known fossils are from Greenland and date back to 3850 million years ago. They are of stromatolites which are clumps of a fungus like form that dominated the early shallow seas
Stromatolites are layered structures formed by the activity of microbial mats, primarily cyanobacteria, which trap and bind sediment over time. They are some of the oldest known fossils, providing crucial evidence of early life on Earth, dating back over 3.5 billion years. Stromatolites are typically found in shallow aquatic environments and are important for understanding the evolution of life and Earth's ancient ecosystems. Today, they are rare and primarily found in a few locations, such as Shark Bay in Australia.
Stromatolites