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Permanent link (DOI): https://doi.org/10.7939/R3PK0778T

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The Ecology, Neoichnology and Sedimentology of Siliciclastic Hardground Communities: Implications for Trypanites Assemblages in the Rock Record Open Access

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Other title
Subject/Keyword
Neoichnology
Gastrochaenolites
Ecology
Sedimentology
Siliciclastic Hardground
Trypanites Ichnofacies
Type of item
Thesis
Degree grantor
University of Alberta
Author or creator
Furlong, Carolyn Marie
Supervisor and department
Gingras, Murray (Department of Earth and Atmospheric Sciences)
Zonneveld, John Paul (Department of Earth and Atmospheric Sciences)
Examining committee member and department
Duane Froese (Department of Earth and Atmospheric Sciences)
Gingras, Murray (Department of Earth and Atmospheric Sciences)
John Acorn (Department of Renewable Resources)
Zonneveld, John Paul (Department of Earth and Atmospheric Sciences)
Department
Department of Earth and Atmospheric Sciences
Specialization

Date accepted
2014-05-02T13:17:06Z
Graduation date
2014-11
Degree
Master of Science
Degree level
Master's
Abstract
The paleoecology of rocky substrates in the rock record is commonly interpreted based on ichnology (the Trypanites ichnofacies) and is frequently associated with a biotic assemblage with low diversity. However, analyses of two modern, siliclastic, intertidal hardground community at Lion Rock, located at Arcadia Beach State Park, Oregon, and Thomas Cove at Upper Economy, Nova Scotia (Bay of Fundy), reveal diverse communities of boring, encrusting and squatting/clinging organisms. Through observations and descriptions of organism distribution and abundance, up to 45 species of flora and fauna are reported to inhabit the study areas. At Lion Rock, organisms reside within five littoral zones (supra-, upper-, middle-, and lower littoral zones, and a newly established sublittoral zone) on the sea stack. Borings are produced by Adula californiensis, Hiatella arctica, Penitella penita, and Zirfaea pilsbryi and are identified as Gastrochaenolites-type traces. At Thomas Cove, organisms inhabit eleven depositional sub-environments and borings are formed by Petricola pholadiformis and Zirfaea pilsbryi, and are also identified as Gastrochaenolites-type traces. Within the two studied localities, substrate, sediment type and thickness, water presence during low tide and water velocity control boring location and abundance. It is likely that ancient Trypanites communities had considerably higher diversity and faunal abundance than their ichnological record indicates. Comparisons with modern assemblages are thus crucial in assessing these environments in ancient successions.
Language
English
DOI
doi:10.7939/R3PK0778T
Rights
Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission.
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