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Refining 2 km of Ordovician chronostratigraphy beneath Anticosti Island utilizing integrated chemostratigraphy
Journal article   Peer reviewed

Refining 2 km of Ordovician chronostratigraphy beneath Anticosti Island utilizing integrated chemostratigraphy

Patrick I. McLaughlin, Poul Emsbo, Andre Desrochers, Alyssa Bancroft, Carlton E. Brett, John F. Riva, Wayne Premo, Leonid Neymark, Aicha Achab, Esther Asselin, …
Canadian journal of earth sciences, Vol.53(8), pp.865-874
08/01/2016
DOI: 10.1139/cjes-2015-0242
url
https://utoronto.scholaris.ca/bitstreams/66bdec84-559d-4f29-80b5-da251341e945/downloadView
Open Access

Abstract

New high-resolution chemostratigraphy, in combination with updated biostratigraphy, refines the chronostratigraphic resolution of the nearly 2 km thick Ordovician section below Anticosti Island. A total of 1414 horizons, spaced at 1.0-1.5 m intervals, were sampled from the New Associated Consolidated Paper (NACP) drill core and analyzed for major and trace elemental composition by portable X-ray fluorescence analyzer (pXRF). Select micrite and calcareous shale powders were then analyzed for delta C-13(carb) (number of samples, N = 364) and Sr-87/Sr-86 (N = 25). Our results indicate a Floian to early Darriwilian (F3-Dw1) age for the Romaine Formation, a middle Darriwilian to Sandbian (Dw2-Sa1) age for the Mingan Formation, a lower to mid-Katian (Ka1-Ka2) age for the Macasty Formation, an upper Katian (Ka3) age for the lower Vaureal Formation, an uppermost Katian (Ka4) age for the upper Vaureal, and a Hirnantian (H1) age for the Ellis Bay Formation. This integrated chemostratigraphic and biostratigraphic synthesis establishes the position of numerous unconformities, the duration of the intervening depositional sequences, and rates of sedimentation.
Geology Geosciences, Multidisciplinary Physical Sciences Science & Technology

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