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Paleozoic Seas
in The Early Cambrian
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More than 1/2 BILLION years old, the fossils of the Burgess Shale fauna preserve for us an intriguing glimpse of early animal life on Earth. These fossils are named after a Cambrian rock formation (the Burgess Shale) that is located in the western Canadian Rockies. This is our first sight of modern multicelled creatures. Most of the animals have few hard parts and not normally create fossils.
update 01/05/05
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Opabinia with its five eyes is a strange looking one indeed. Wielding a long flexible proboscis tipped with grasping spines. It was about 3 inches long. It may be related to
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Many of members of the Burgess Shale do not fit into any existing families.
Wiwaxia looks like a slug
armored with spines called sclerites. The longer spines project in two rows along the back, and evidently provided some protection from predators. The rest of the upper (dorsal) surface is covered with small, flat, overlapping hard plates, termed sclerites. Each of these little scales was attached with a root-like base and we assume
Wiwaxia grew by molting these plates from time to time. Since there are none on the bottom (ventral) surface, the animal partly resembles the slug, a member of the mollusk family. However, mollusks do not have any sclerite armor so the animal's affinity to present day species is unsettled. It did have an anterior jaw with two rows of teeth on the ventral surface, suggesting it was another bottom feeder. Fossil sizes range from 1/8 to 2 inches.
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Anomalocaris form the UHA Kaiyodo series
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Olenoides is decribed by Stephen Gould in his
book 'Its a Wonderful Life' as a standard trilobite The long, curved
antennae were well preserved in the Burgess Shale. The middle legs, near their
base, bore a series of spines that could be used to grasp the soft-bodied
animals it preyed on and then to move them forward toward the mouth. The thin
limbs tell us that this was not a swimmer. Instead, it was an active predator
and scavenger moving about the muddy seafloor.
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Originally the Hallucigenia was thought to have stood on its spines, with the tentacles upward.
It is still displayed spines down at the Smithsonian Natural History Museum. Later studies have shown that the "tentacles" are actually feet,
It is less than three millimeters long, making it one of the smaller creatures in the Burgess Shale. At one end there is a bulbous "head" which is a round
mass. This connects to the cylindrical trunk of the
Hallucigenia, which, on
the top has seven pairs of spines pointing upward and outward. These conical spines
are embedded into the trunk, and are fairly long when compared to the rest of the
Hallucigenia. Below each pair of spines there is a tentacle except that the last
tentacle is offset from the pair of spines. Behind these tentacles there are three pairs of
much shorted tentacles, and then the trunk narrows and curves upward. The tentacles
have pincers at their tips, and there is a hollow tube in each one which is connected
to the gut. It is now thought to be related to the velvet worms an obscure phylum
of caterpillarish looking animals found in South Africa.
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Pleurocystites is a good example of the sedentary filter feeders that dominate Paleozoic seas. Sea Lilies belong to the same family as starfish and sea urchins. They decline sharply at the end of the Paleozoic.
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