Our website is made possible by displaying online advertisements to our visitors.
Please consider supporting us by disabling your ad blocker.
Cambrian explosion
Opabinia made a big contribution to interest in the Cambrian explosion. This Marrella specimen shows how clear and detailed the fossils are from the Burgess Shalelagerstätte.An Ediacaran trace fossil, made when an organism burrowed below a microbial mat.Dickinsonia, an Ediacaran animal with a quilted appearance. A fossilized trilobite. This specimen of Olenoides serratus, from the Burgess shale, preserves 'soft parts' – the antennae and legs.
The Cambrian explosion is when many animal phyla first appeared in the fossil record. It happened 541 million years ago (mya).[1][2][3] Probably most had evolved before then, but that was their first appearance as fossils.[4]
Before about 580 mya it seems that most organisms were simple. They were made of individual cells, occasionally organized into colonies. Over the following 70 or 80 million years the rate of evolution seemed to accelerate.[5] By the end of the Cambrian most phyla we know today existed.
The Cambrian explosion has caused much scientific debate. The seemingly rapid appearance of fossils in the 'primordial strata' was noted as early as the mid 19th century,[6] and Charles Darwin saw it as one of the main objections that could be made against his theory of evolution by natural selection.[7]
↑Bambach, Richard K.; Bush, Andrew M.; Erwin, Douglas H. (2007). "Autecology and the filling of ecospace: key metazoan radiations". Palæontology. 50 (1): 1–22. doi:10.1111/j.1475-4983.2006.00611.x. S2CID84142740.