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The
Walcott Quarry
Charles
Walcott's main collection site, enlarged by excavation of the Royal Ontario
Museum. View to the Northwest with Mount Wapta in the upper left corner.
The escarpment beyond the edge of the quarry on the left is formed by the
contact between dark shales and light-colored dolomites of the Stephen
Formation. Copyright
© 1995 by Andrew MacRae. |
The
fossiliferous strata of the Burgess Shale represent a so-called Lagerstatten
deposit, where shallow dwelling marine animals were swept to a deeper
site of the shelf and buried by slumps, rapidly and generally alive.
This rapid burial prevented from decay of the soft parts. It is thus responsible
for the preservation of the entire fauna whereas a usual fossil assemblage
presents only part of the original biota.
Today,
we know of about 125 different genera from the Burgess Shale - the most
comprehensive assemblage known from any Paleozoic locality. The spectrum
of organisms reaches from Cyanobacteria and green and red algae over sponges,
brachiopods, priapulids, annelids,
many different arthropod groups, echinoderms and problematic skleritome-bearing
animals to one of the first chordates. Famous examples of strange animals
are Opabinia,
Yohoia, Hallucigenia,
and Pikaia. Anomalocaris
was identified as one of the first great predators and perhaps the largest
animal in the Cambrian seas.
Charles
Walcott interpreted all of his findings as belonging to modern phyla. A
revival of the Burgess Shale studies by Harry Whittington and his research
group starting in the 1970s have radically changed this view. These studies
have shown that many of the organisms had strange and previously unknown
morphologies and lack modern analogues. They represent a large number of
higher taxa that are only known from the Cambrian fossil archives and probably
became extinct before the end of the Cambrian - early experiments of nature
that for unperceptible reasons failed to survive the tail of the Cambrian
Explosion. The insight won from the Burgess Shale fauna was a major argument
not only for a maximal initial proliferation of the metazoan animals (the
so-called Cambrian Explosion) but also for their pronounced decimation
after the outburst of so many anatomical designs.
The
Burgess Shale fauna has now become popular, particularly through S. J.
Gould's best-seller "Wonderful
Life",
a highly recommendable introduction. The locality has been declared a World
Heritage.
.
.
Andrew
MacRae kindly provided most of the photos on this side. Here is a link
to his
Burgess Shale page.
.
Links
to Burgess Shale information
(unordered
and of extremely differing scientific significance, but still worth to
browse)