Litho- and biofacies analysis of postglacial marine mud using CT-Scanning

• Published in: Engineering geology Vol. 103; no. 3; pp. 106 - 111
• Main Authors: Gagnoud, Marie, Lajeunesse, Patrick, Desrosiers, Gaston, Long, Bernard, Dufour, Suzanne, Labrie, Jacques, Mermillod-Blondin, Florian, Stora, Georges
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 10.02.2009; Elsevier
• Subjects: Biofacies; Brackish; CT-Scan; Lithofacies; Macoma balthica; Ocean, Atmosphere; Postglacial marine sediments; Sciences of the Universe; Sedimentary structures; ANW, Canada, Quebec; CT-Scan; Biofacies; Postglacial marine sediments; Sedimentary structures; Lithofacies
• ISSN: 0013-7952; 1872-6917
• DOI: 10.1016/j.enggeo.2008.06.010

Marine silty clay deposited during the Late-Wisconsinian postglacial marine transgression of eastern Québec (Goldthwait Sea) is ubiquitous in the sedimentary column of intertidal zones of the St-Lawrence Estuary. This mud is very compact and limits the penetration of organisms composing the modern Macoma balthica community. In order to describe the characteristics of intertidal sediments containing Goldthwait Sea mud, axial tomography (CT-Scan) is used. CT-Scan is a non-destructive method that can be used to describe sediment characteristics (grain size, mineralogy, primary and secondary sedimentary structures, fabric, shape and roundness, bedding contact), and to obtain high resolution, 3D representations of structures within sediment cores. Based on differences in the densities of analysed materials, the different lithologies, lithofacies, and organisms within the core can be discriminated, and a quantification of the volume occupied by the different components of the material can be made. Here, CT-Scan images provide information on the distribution, orientation and interweaving of thanatocœnosis shell beds that alternate with massive or faintly laminated postglacial marine mud beds, as well as on ichnofacies characteristics. In addition, we show 3D images of bioturbation structures within the recent sediment layer, which is distinguished from the underlying Goldthwait Sea mud. When coupled with conventional sedimentary (grain size statistics) and radiochronological ( 14C) analyses, these data provide information which is valuable for identifying depositional processes within sedimentary environments.