An unusual sponge-microbe-synsedimentary cement framework in a Late Ordovician reef, Southampton Island (Nunavut, Canada)
A large, resistant buildup at the top of the Upper Ordovician (Hirnantian?) Red Head Rapids Formation (RHR) on Southampton Island (Nunavut, Arctic Canada) is dominated by massive boundstone and cementstone facies. These massive facies have more in common with the spongeâ microbial reefs that dominat...
| Main Authors: | , , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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NRC Research Press (a division of Canadian Science Publishing)
2016
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| Subjects: | |
| Online Access: | http://hdl.handle.net/1807/72670 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2015-0244 |
| Summary: | A large, resistant buildup at the top of the Upper Ordovician (Hirnantian?) Red Head Rapids Formation (RHR) on Southampton Island (Nunavut, Arctic Canada) is dominated by massive boundstone and cementstone facies. These massive facies have more in common with the spongeâ microbial reefs that dominated worldwide in the Early Ordovician including the following primary components: early calcified sponge material, microbial elements, and synsedimentary cement. A close spatial relationship between sponge and microbial framework elements suggests that a poorly preserved decaying sponge framework provided substrates for the attachment and development of microbes, and that the microbes played essential roles as reef consolidators. Centimetre-scale colonial metazoans are present and locally intergrown with the sponge and microbial components. Other dwelling invertebrates or calcareous algae are rare. Although altered now to calcite, cement fabrics suggest that aragonite was ubiquitous as sea-floor precipitate. Prior to its subaerial exposure in the latest Ordovician, the RHR buildup developed on the margin of a shallow-marine evaporative epicratonic basin where a diverse community of reef-building metazoans was unable to flourish. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. |
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