The fossils here are from the Cambrian period of Earth's history, which began over 540 million years ago and lasted more than 55 million years.
More than half a billion years old, these fossils are incredibly diverse and well-preserved, providing a glimpse into the Earth's early life forms.
The fossils were preserved after, animals that lived on a muddy sea floor, were sent into deeper, oxygen-poor water by submarine landslides. Those with hard shells were preserved, but so too were soft-bodied forms.
About a dozen of the phyla that still exist today can be found in the fossil collection. But, the shale also preserves sea-dwelling invertebrates unlike anything alive today.
Stanleycaris hirpex, a 20-centimetre-long distant relative of today's arthropods, had two protruding eyes on the side of its head and a larger eye in the centre.
The Anomalocaris (“abnormal shrimp”) that grew up to six feet long, is the largest animal among the Burgess Shale fossils. It propelled itself through the water by undulating the flexible flaps on the sides of its body.
Anomalocaris canadensis grasping claw (Burgess Shale Formation, Middle Cambrian; Walcott Quarry, above Field, British Columbia, Canada) James St. John |
The Pikaia fossil from the Royal Ontario Museum's collection. |
Ogygopsis klotzi fossil trilobite tail (Burgess Shale Formation, Middle Cambrian; Mt. Stephen, British Columbia, southwestern Canada) https://www.flickr.com/photos/jsjgeology/ |
Diorama of the Burgess Shale Biota (Middle Cambrian) - anomalocaridid, sponges 1 https://www.flickr.com/photos/jsjgeology/ |