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Precambrian |
| The Precambrian, with a duration of approx. 4 billion years, covers the longest part of earth's history. Despite the very early occurence of evidence for primitive single-celled organisms, remains of more complex lifeforms are limited to the latest Precambrian (Proterozoic). Those early eumetazoans didn't have hard endo- or exeskeletons, so fossil evidence is quite rare. The famous proterozoic Ediacara fauna dates back to the Vendian, about 650 Ma ago. Ediacara fossils can be found in late proterozoic sediments all over the world, but are always only preserved as casts. Interpretation and systematic position still raise controversal discussions. While some paleontologists believe them to be primitive ancestors of all the phylums that finally appeared on the beginning of the Cambrian, some others presume that they were a separate branch of the tree of life that died out without successors.
Macroscopic animals were mainly filterers or surface and sediment feeders. Base of the food chain were planctonic organisms and algal mats which were filtered out of the sea water or directly fed from the ground by larger animals. Teeth for hunting or armour plates for defense against predators were unknown. The Precambrian ends with the first occurence of shelly organisms. The vast majority of all known classes of animals suddenly appeared at the beginning of the Cambrian. Before scientists recognized that it's more a matter of the sudden appearance of preservable exoskeletons, there was a long discussion about the "Cambrian Explosion". According to this theory, the ancestors of all known organisms have evolved from a few groups of organisms within an astonishingly short time. Today it seems much more simple: It is now believed that those ancestors have evolved much earlier and underwent a far longer evolutionary process than presumed, but they didn't have had any hard body parts and therefore could not be fossilized. |
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Stratigraphy of the Precambrian
(after FAUPL 2000, abbreviated) |
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Nemiana simplex PALEJ
The casts have probably been caused by protomeduses that packed sand into their body orifices to achieve a more stable position on the sedimentary surface. Unlike fossils of later successors from the Cambrian they don't show any structures of the soft body. Vendian, Mogilev Region (Ukraine) |
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| Scale length, if not otherwise stated: 1 cm | |