92 Clastic Sediments: Precambrian to Recent, Experimental to Applied Studies

Monday, 28 October 2013
8:00 AM - 12:00 PM
Room 504

SUSPECT MICROBIAL-INDUCED SEDIMENTARY STRUCTURES (MISS) IN FURONGIAN (UPPER CAMBRIAN; JIANGSHANIAN, SUNWAPTAN) STRATA OF THE UPPER MISSISSIPPI VALLEY

Paper number: 92-3
Program: Technical Sessions
Time: 8:30 AM – 8:45 AM

Authors

Abstract

Sedimentary structures mediated by microbial activity—microbial-induced sedimentary structures (MISS)—have received attention in the last decade as researchers recognized the vital role microbes played in siliciclastic sedimentation throughout the geological column. In the absence of early cementation that characterizes some carbonates, most of the evidence for biostabilization of clastic sediment are proxy structures resulting from the interaction of microbes with the sediment. MISS provide unique signals of biological-physical processes that physical structures alone cannot mimic. Much remains to be learned, particularly for ancient examples lacking modern analogs.

The Furongian (upper Cambrian; Jiangshanian and Sunwaptan stages) Tunnel City Group (Lone Rock and Mazomanie formations), exposed in west-central Wisconsin and southeastern Minnesota, represents a shallow-marine clastic environment during a time of exceptionally high sea level. Lithofacies, from shoreface to transitional-offshore settings, document deposition in a wave- and storm-dominated epicontinental sea. During deposition of a condensed section in the lower part of the Tunnel City Group, eustatic flooding was associated with development and preservation of microbial-mat textures or associated sedimentary structures. Possible fragments of microbial mats similar to “roll-up” structures, wrinkle structures, and syneresis cracks are present in sandstones of the Birkmose and Tomah members of the Lone Rock Formation.

In the Lone Rock Formation, MISS are associated with a trilobite extinction event in the Steptoean–Sunwaptan boundary interval. This conforms to recent predictions that Phanerozoic microbial mats were disaster forms that flourished during extinction intervals. Further investigation of stratigraphic, taphonomic, and other potential biases, however, is needed to fully test this hypothesis.