The Burgess Shale is famous for the exceptional preservation of the fossils found within it, in which the soft parts are preserved. A Cambrian black shale formation, it crops out in the Canadian Rockies of British Columbia, Canada. It is in Yoho National Park, near the town of Field and is named after Burgess Pass.
With Parks Canada and UNESCO recognising the significance of the Burgess Shale, collecting fossils became politically more difficult from the mid 1970s. Collections continued to be made by the Royal Ontario Museum. The curator of invertebrate palaeontology, Desmond Collins, identified a number of additional outcrops, stratigraphically higher and lower than the original Walcott quarry. These localities continue yield new organisms faster than they can be studied.
Stephen J Gould's book Wonderful Life, published in 1989, brought the Burgess Shale fossils to the public's attention. Gould suggests that the extraordinary diversity of the fossils indicate that life forms at the time were much more diverse than those that survive today, and that many of the unique lineages were evolutionary experiments that became extinct. He suggests that this interpretation supports his hypothesis of evolution by punctuated equilibrium. Gould's interpretation of the diversity of Cambrian fauna relied heavily on Simon Conway Morris' reinterpretation of Charles Walcott's original publications. Conway Morris strongly disagreed with Gould's conclusions, arguing that almost all the Cambrian fauna could be classified into modern day phyla.
The fossiliferous deposits of the Burgess Shale belong to the Stephen formation, a collection of sightly calcareous dark mudstones, about 505 million years old. The beds were deposited at the base of a cliff about 160m tall. This vertical cliff was composed of the calcareous reefs of the Cathedral formation, which probably formed shortly before the deposition of the Burgess shale. The precise formation mechanism is not known for certain, but the most widely accepted hypothesis suggests that the edge of the Cathedral formation reef became detached from the rest of the reef, slumping and being transported some distance – perhaps kilometers – away from the reef edge. This would have left a steep cliff, the bottom of which would be protected from both general oceanic circulation – producing anoxic conditions – and later, because the limestone of the Cathedral formation is difficult to compress, from tectonic decompression. This latter protection explains why fossils preserved further from the Cathedral formation are impossible to work with – tectonic squeezing of the beds has produced a vertical cleavage which fractures the rocks, so they split perpendicular to the fossils. The Walcott quarry produced such spectacular fossils because it was so close the the Stephen formation – indeed the quarry has now been excavated to the very edge of the Cambrian cliff.
The anoxic setting not only protected the newly dead organisms from decay, but it also created chemical conditions allowing the preservation of the soft parts of the organisms. Further, it reduced the abundance of burrowing organisms – burrows and trackways are found in beds containing soft-bodied organisms, but they are rare and generally of limited vertical extent.
Please expand this section
There are many other comparable Cambrian lagerstatten; indeed such assemblages are far more common in the Cambrian than in any other period. This is mainly due to the limited extent of burrowing activity; as such bioturbation became more prevalent throughout the Cambrian, environments capable of preserving organisms' soft parts became much rarer.
The biota of the Burgess Shale appears to be typical of Middle Cambrian deposits. Although the hard-part bearing organisms make up as little as 14% of the community, these same organisms are found in similar proportions in other Cambrian localities. This means that there is no reason to assume that the organisms without hard parts are exceptional in any way; indeed, many appear in other Lagerstatten of different age and locations.
The biota consists of a range of organisms. Free-swimming organisms are relatively rare, with the majority of organisms being bottom dwelling (benthic) - either moving about (vagrant) or permanently attached to the sea floor (sessile). About two-thirds of the Burgess Shale organisms lived by feeding on the organic content in the muddy sea floor, while almost a third filtered out fine particles from the water column. Under 10% of organisms were predators or scavengers, although since these organisms were larger, the biomass was split equally between each of the filter feeding, deposit feeding, predatory and scavenging organisms.