Burgess Shale

Fossil Sites
 

Fossils from the Burgess Shale of the Stephen Formation

British Columbia, Canada

Cambrian Period about 505 million years ago

Also see:
Cambrian Explosion
Laggerstatten
Chengjiang Biota

Guanshan Fauna

 


First Glimpse of the Cambrian Explosion

MarellaThe Burgess Shale is a very famous fossil Lagerstätte named after the nearby Burgess Pass. This site is high in the Canadian Rockies within Yoho National Park near the town of Field, British Columbia, Canada. The Burgess Shale was discovered in 1909 by famed paleontologist Charles Doolittle Walcott, who returned time and again to extensively study its fossils. Walcott described a large diversity of previously unknown arthropods, and most importantly many forms of previously unknown phyla as well as many forms that remain enigmatic today. The fossils were particularly important at the time to understand Cambrian paleobiology because of their often Walcott Quary of Burgess Sahleexquisite preservation that included soft body parts. Many such Cambrian sites have since been discovered, most notably the Chengjiang Maotianshan Shales, which are collectively called sites with Burgess Shale-like preservation.

The Burgess Shale fossils are about 505 million years old, some 20 million years younger than those from Chengjiang. In fact, the Burgess Shale and Chengjiang have considerable overlap in faunal forms. Less well known is that Cambrian formations in the House Range of Utah yield many fossils like the Burgess Shale, though the soft tissue preservation is usually not as good. The Burgess Shale Formation comprises 10 separate members, the most famous being the Walcott Quarry Shale Member comprising the greater phyllopod bed.

Satellite image of Burgess Shale areaThe Burgess Shale comprises shale, limestone and siltstone and extends in a large area in outcrops of the Stephen Formation that exhibite different faunal mixes. The fossils of the Burgess Shale are preserved as black carbon films on black shales. Scientists long believed the deposits were formed when areas of muddy ocean floor slid into a lower place creating an anoxic (oxygen-starved) environment that was particularly favorable to fossilization because decay was inhibited. More recent research that oxygen was continually present in the sediment

While there are older Cambrian Lagerstatten, the Burgess Shale was science's first glimpse of the Cambrian Explosion in the fossil record. The extensive diverse fauna generally new to science and their often exquisite soft-bodied preservation, caused Walcott him to return repeatedly to the fossil site until 1924. By age 74 he had amassed more than 65,000 specimens. Describing the fossils was a vast task the Walcott continued until his death in 1927. Walcott, influenced by the opinion of scientific peers, tried to associate the fossils with living taxa, which delayed the scientific significant of them to be delayed by serveral decades. Three decades of study commencing in the 1960's led to the Burgess Shale ultimately attaining the recognition of today as a remarkable rock record of early Cambrian life and its early diversification.

Burgess Shale Fossils

Partial List of Burgess Shale Fauna

Phylum Annelida
Canadia
Phylum Arthropoda
Burgessia
Canadaspis
Elrathina (trilobite)
Leanchoilia
Marella
Naraoia
Olenoides (trilobite)
Perspicaris
Ptychagnostus (trilobite)
Sidneyia
Waptia
Yohoia
Phylum Brachiopoda
Micromitra
Phylum Chordata
Pikaia
Phylum Ctenophora
Ctenorhabdotus
Fasciculus
Xanioascus

Phylum Hyolitha
Haplophrentis
Phylum Mollusca
Scenella
Phylum Onychophora
Aysheaia
Hallucigenia
Phylum Porifera
Choia
Phylum Priapulida
Ottoia
Phylum Incertae sedis
Amiskwia
Anomalocaris
Dinomischus
Nectocaris
Odontogriphus
Opabinia
Orthrozanclus
Wiwaxia
Leanchoilia superlata
Naraoia compacta
Leanchoilia superlata
Phylum Arthropoda
Stephen Formation
Burgess Pass
Naraoia compacta
Phylum Arthropoda
Stephen Formation
Burgess Pass
Ottoia
Marella splendens
Phylum Arthropoda
Order Marrellomorpha
Stephen Formation
Burgess Pass
Micromitra burgessensis
Phylum Brachiopoda
Family Paterinatidae
Stephen Formation
Burgess Pass
Ottoia prolifica
Phylum Priapulida
Family Ottoidae
Stephen Formation
Burgess Pass
Canadaspis perfecta
Burgessia bella
Phylum Arthropoda
Family Bugessiidae
Stephen Formation
Burgess Pass
Elrathina (= Ptychoparella) cordillerae Mass Mortality
Class Trilobita
Order Ptychopariida
Family Alokistocaridae

Walcott Quarry Shale Member
Scenella amii
Phylum Mollusca (?)
Family Scenellidae
Stephen Formation
Burgess Pass
Canadaspis perfecta
Phylum Arthropoda
Family Canadaspididae
Stephen Formation
Burgess Pass

 


Burgess Shale References