T134 Clear as Mud: Stratigraphic, Diagenetic, Sedimentologic, Geomechanical Analyses, and Modern Analogs of Ancient Mudrock Systems

Monday, 23 October 2017
1:30 PM - 5:30 PM
Ballroom 6C


IMPLICATIONS OF LITHOLOGY, GEOCHEMISTRY AND MICROFACIES FOR CAMBRIAN PALEOENVIRONMENTS, PALEOCLIMATE, AND PALEOGEOGRAPHY OF EASTERN NEWFOUNDLAND, CANADA

Paper number: T134-11
Program: Technical Sessions
Time: 4:05 PM – 4:20 PM


Authors


Abstract

The outcrops in the Manuels River area, Avalon Peninsula, Newfoundland, are classic localities for Cambrian research. The rocks comprise a concordant sedimentary succession deposited on the former microcontinent Avalonia. The upper Series 2 to Furongian succession is represented by the Brigus, Chamberlain’s Brook, Manuels River and Elliot Cove formations and consists predominantly of green, grey, and black mudstones and siltstones, in part highly fossiliferous, with minor limestone intercalations and volcanic ash layers. The succession rests on Neoproterozoic magmatic rocks and is conformably overlain by Ordovician sedimentary rocks.

According to widely accepted concepts, the succession was deposited in a cold-water shelf to outer-marine environment. However, microfacies analysis indicates a sedimentary environment influenced by sea-level changes in a setting shallower than outer-shelf. Varying amounts of organic carbon in the succession suggest deposition under fluctuating levels of oxygenation, probably related to sea-level changes.

The Cambrian paleogeography and movements of Avalonia are subject to controversial interpretations. Due to an only moderate diagenetic overprint, analysis of detrital clay minerals enables paleoclimatic interpretations, which, in combination with interpretation of the depositional environments and the fossil record, challenges previous reconstructions of the palaeogeographic position of Avalonia and Cambrian climate.

Financial support by the Klaus Tschira Foundation (KTS 00.195.2011 and 00.272.2015) is gratefully acknowledged.


Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-299984

© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.