A widely distributed sedimentary structure consisting of laminated carbonate or silicate rocks, produced over geologic time by the trapping, binding, or precipitating of sediment by groups of microorganisms, primarily cyanobacteria.
very little, there are stromatolites, domed mates of microscopic algae that are aged as precambrian. No other fossils in the precambrian
The earliest fossils known are in the form of stromatolites formed by cyanobacteria about 3.5 billion years ago. To say however that these are the first life forms is not likely to be correct. Cyanobacteria are already a relatively complex single celled organism. It is likely that simpler forms preceded them but so far no evidence of this has been found.
There isn't, of course, a gap in time. There are, however, very few fossils intermediate between simple stromatolites (the first more or less multicellular organisms) and the first complex organisms found just before the Cambrian Explosion. This gap most likely exists because while predation already existed (organisms consuming other organisms), no organisms had yet developed an internal or external skeleton that could have been preserved at death. The very few organisms from that era that were preserved despite of this, were preserved in the form of molds and casts.
Well, it is either a turtle or an alligator because they are very wise and I think they were living at the time of the dinosaurs. Thank You!P.S. I think more of the Turtle because I saw it on a documentary!That is of course if you are ruling out zooplankton.
Wolves have changed some over the past 20 million years, but not by a huge amount. There are fossils of mosquitoes in amber that are remarkably similar to modern mosquitoes, though they are over 200 million years old. Coelacanth is a variety of fish for which modern specimens are somewhat similar to species that lived at the close of the Cretaceous, 65 million years ago. So there are a few creatures that have not changed a whole lot over vast stretches. Horseshoe crabs are yet another example, for which there are specimens over 440 million years old.
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.
Stromatolites
Stromatolites
stromatolites
The prokaryotic cells that built stromatolites are classified as cyanobacteria. Cyanobacteria are photosynthetic bacteria that played a crucial role in the formation of stromatolites, which are layered structures formed by the trapping and binding of sediment by microbial communities.
stromatolites
they are aerobically anaerobic
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 most common Precambrian fossils are stromatolites. These are layered structures formed by the growth of cyanobacteria, also known as blue-green algae, in shallow water environments. Stromatolites are important in understanding early life on Earth.
Stromatolites were much more abundant on the planet in Precambrian times which means that fossils found around stromatolites are typically from the Precambrian era.