Phyllopod bed

The Phyllopod bed, designated by USNM locality number 35k, is the most famous fossil-bearing member of the Burgess shale fossil Lagerstätte. It was quarried by Charles Walcott from 1911–1917, and was the source of 95% of the fossils he collected during this time; tens of thousands of soft-bodied fossils representing over 150 genera have been recovered from the Phyllopod bed alone.

The phyllopod bed is a 2.31 m thick layer of the 7 m thick Greater Phyllopod Bed, found in the Walcott Quarry on Fossil ridge, between Mount Wapta and Mount Field, at an elevation of around 2,300 metres (7,500 ft), around 5 kilometres (3.1 mi) north of the railway town of Field, in the Canadian Rocky Mountains in British Columbia, Canada.

Walcott divided the bed into twelve units based on the rock type and fossil content. Certain fossil beds provide reference levels and can be recognized by the superabundance of a particular type of fossil: for instance, the Great Marrella layer and Great Eldonia layer.

After locating soft-bodied fossils in loose fragments of rock in 1907, the Phyllopod bed was located in a source for the fragments' origins by the Walcotts in 1910. Extensive quarrying was performed in field seasons until 1913, and Walcott considered the ton of shale he collected in his next visit, in 1917, to have practically exhausted the productive potential of the bed.

Most of the organisms within the Phyllopod bed had been transported minimal distances before they were buried, and decayed in place until they were buried (at which time decay and disarticulation was halted). Mineralization of tissues occurred shortly afterwards. The community of organisms preserved is a good representation of the (preservable) community; the biasing effects of time-averaging and preferential decay seem to be minimal. A great deal of compaction occurred after the deposition of the fossils.

The unit consists of mudstones that intergrade into coarser shelly sandstones that sometimes form small nodules. There are (very rare) turbidite layers, but on the whole the unit was deposited in large events that dumped tens of centimetres of sediment at a time as a slurry of mud was washed over the site by a density current, sweeping up and entombing any organisms in its path.

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