Sedimentological and ichnological variations in fluvio‐tidal translating point bars, McMurray Formation, Alberta, Canada

• Published in: Sedimentology Vol. 71; no. 3; pp. 974 - 1022
• Main Authors: Fietz, Susanne W., MacEachern, James A., Gingras, Murray K., Ranger, Michael, Dashtgard, Shahin E.
• Format: Journal Article
• Language: English
• Published: Madrid Wiley Subscription Services, Inc 01.04.2024
• Subjects: Bioturbation; Brackish‐water; Chemical reactions; concave‐bank bench; counter‐point bar; Cretaceous; Deformation; Deposition; Descriptions; Dewatering; Dunes; Flow velocity; fluid mud; Fluvial deposits; fluvio‐tidal; Fossils; inclined heterolithic stratification; mesofacies; Mud; River discharge; River flow; Rivers; Sand; Sediment; Sediment concentration; Sediment deposits; Sedimentary facies; Stratification; Substrates; Temporal variations; Tidal currents; Tidal flow; Trace fossils; translating point bar; Turbidity; Water discharge; Alberta Canada; Canada
• ISSN: 0037-0746; 1365-3091
• DOI: 10.1111/sed.13164

ABSTRACT Sedimentological and ichnological descriptions of fluvio‐tidal translating point bars are rare, and complex physico‐chemical processes make highly detailed but concise facies descriptions challenging. Herein, mesofacies are defined to describe and interpret three ancient translating point bars from the Lower Cretaceous McMurray Formation, Alberta, Canada. Twenty‐three mesofacies are defined, based on their recurring sedimentological and ichnological characteristics. These mesofacies form the building blocks of beds and bedsets that make up three depositional facies. Facies 1 reflects sand dune migration at the channel base, which grades into inclined heterolithic stratification of Facies 2 and 3. Facies 2 occurs in the centre and seaward portions of the translating point bars and records tide‐dominated deposition of sand and muddy sand during periods of reduced river discharge. Ichnological suites and bioturbation intensities in these beds reflect persistent but variable brackish‐water conditions, fluctuating deposition rates and the deposition of mud. Mud beds are derived from flows with high suspended‐sediment concentrations. Tidally derived mud beds are typically bioturbated with trace fossil suites indicative of slow deposition rates and brackish‐water conditions. Mud deposited during elevated river discharge is burrowed after the dewatering of the bed. Facies 3 occurs at the landward apex of the translating point bar and is marked by sand‐rich and mud‐rich dune deposits with abundant soft‐sediment deformation, indicative of elevated flow velocities and deposition rates. Bioturbation is rare and sporadically distributed owing to unstable substrates. The distribution of the facies reflect the hydrodynamic variations that occurred vertically and laterally across the bar in response to temporal variations in fluvial and tidal flow interaction, as recorded by their mesofacies. The detailed facies analysis strongly suggests that deposition of the three McMurray Formation translating point bars occurred in proximity to the turbidity maximum zone of a fluvio‐tidal channel system.