The lower Cambrian Cranbrook Lagerstätte of British Columbia

Author:

Caron Jean-Bernard123ORCID,Webster Mark4ORCID,Briggs Derek E. G.5ORCID,Pari Giovanni6,Santucci Guy7,Mángano M. Gabriela8ORCID,Izquierdo-López Alejandro12ORCID,Streng Michael9ORCID,Gaines Robert R.10ORCID

Affiliation:

1. Department of Natural History, Royal Ontario Museum, 100 Queen's Park, Toronto, ON M5S 2C6, Canada

2. Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, ON M5S 3B2, Canada

3. Department of Earth Sciences, University of Toronto, 22 Ursula Franklin Street, Toronto, ON M5S 3B1, Canada

4. Department of the Geophysical Sciences, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, USA

5. Department of Earth and Planetary Sciences and Yale Peabody Museum, Yale University, PO Box 208109, New Haven, CT 06520-8109, USA

6. 44 Fairpark Drive, Ottawa, ON K2G 6X8, Canada

7. 217 11th Street South, Cranbrook, BC V1C 1T9, Canada

8. Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada

9. Department of Earth Sciences, Palaeobiology, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden

10. Geology Department, Pomona College, Claremont, CA 91711, USA

Abstract

Discovered over a century ago, the lower Cambrian (Series 2, Stage 4) Cranbrook Lagerstätte of southeastern British Columbia's Eager Formation is one of the oldest Burgess Shale-type deposits in North America. This Konservat-Lagerstätte is rich in olenelloid trilobites, but also yields a very low-diversity soft-bodied fossil assemblage including Tuzoia and Anomalocaris , and a low-diversity ichnofauna. Its scientific study, however, remains limited. A 2015 field-based investigation by the Royal Ontario Museum has revealed new information about the site's biota, depositional environment and taphonomic conditions. Not only is the Cranbrook Lagerstätte significant for early Cambrian biostratigraphy and comparisons with other Burgess Shale-type deposits, it also reveals some of the little-known diversity of life in a distal outer shelf environment during the Cambrian period. Supplementary material: Three supplementary figures (historical map, Tuzoia outlines, Anomalocaris specimens), supplementary material and methods, and a supplementary data file (generic presence/absence matrix) are available at https://doi.org/10.6084/m9.figshare.c.6850810

Funder

Royal Ontario Museum

Publisher

Geological Society of London

Subject

Geology

Reference86 articles.

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4. Hexactins in the ‘protomonaxonid’ sponge Choiaella and proposal of Ascospongiae (class nov.) asa formal replacement for the Protomonaxonida

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