Evolution 35 |
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The most famous site for animal fossils must be the Burgess
Shale in the mountains of British Columbia, Canada. The strata date
from the Middle Cambrian, about 520 million year ago. Thus they are only
'slightly' younger than the oldest-known fossils. From 543 million years
ago on, at the beginning of the Cambrian, fossils are frequent. The Burgess
Shale is very special because the fossils from that place are exceptionally
well preserved. Even the soft parts are preserved. In by far most places
only hard parts like shells and bones are fossilized. In the layers
of the Burgess Shale numerous very strange animal have been found, which
are often unknown from other places. Only in China (Chengjiang) comparable
finds have recently been made, which are even somewhat older. It appears from the fossils that in the beginning of the Cambrian many life forms were existing which later on have apparently died out. The huge radiation of life forms in this period is often called the Cambrian explosion.
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Here you can see a couple of these very peculiar animals. Like the
Anomalocaris, a predator sized up to 2 m, with eyes on short stalks,
a mouth with the shape of a pineapple ring and a pair of dangerous claws.
This was by far the biggest animal in the Burgess Shale. The Sidneyia was an arthropodal predator with a length of about 10 cm which could be the ancestor of the spiders, the trilobites and the scorpions. The Leanchoilia was a blind arthropod with long appendages on the head each ending in three whip-like tentacles. These are only three of the more than 120 species of animals found in the Burgess Shale.
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Evolution 35 |