Biofilms of microorganisms, especially cyanobacteria, are found on the outter surfaces of stromatolites.
Stromatolites were much more abundant on the planet in Precambrian times which means that fossils found around stromatolites are typically from the Precambrian era.
The inner planets (Mercury, Venus, Earth, Mars) have rocky surfaces composed of silicate minerals and metals. The outer planets (Jupiter, Saturn, Uranus, Neptune) have gas surfaces, primarily composed of hydrogen and helium. Additionally, outer planets may have icy surfaces due to the presence of water and other ices.
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.
They have rocky surfaces.
The inner planets are closer to the Sun compared to the outer planets, have solid rocky surfaces, and are smaller in size compared to the outer planets.
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.
receptors
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.
The inner planets (Mercury, Venus, Earth, Mars) have rocky surfaces composed of silicate minerals and metals. The outer planets (Jupiter, Saturn, Uranus, Neptune) have gas surfaces, primarily composed of hydrogen and helium. Additionally, outer planets may have icy surfaces due to the presence of water and other ices.
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 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.
They have rocky surfaces.
Yes because the four outer planets,Jupiter, Saturn, Uranus, and Neptune are gas planets. They are known for their gas. The outer planets (closer to the sun) have rocky surfaces. So the outer planets have gas surfaces
The inner planets are closer to the Sun compared to the outer planets, have solid rocky surfaces, and are smaller in size compared to the outer planets.