"An Analysis of Stratigraphic, Paleoecologic, and Geochemical Variabili" by Ainsley Wiesner

Abstract

The “Squaw Bay Formation,” a middle Devonian mixed carbonate-clastic unit located in the Michigan Basin, was named almost 100 years ago by Warthin and Cooper (1935) for a single, poorly exposed outcrop of condensed strata. Since then, the stratigraphic term has been used inconsistently in the subsurface where the unit is stratigraphically expanded, but should also be revised because it is a derogatory term for Native American women. The goal of this study is to aid in the renaming process for this formation by determining its variability and defining boundaries. To accomplish this, the current research combines lithostratigraphy, paleoecology, and geochemical analyses of the Krocker 1-17, State Chester Welch 18, and Paxton Quarry cores to provide background information needed to revise the formation.

The “Squaw Bay Formation” in core is composed of dominantly argillaceous limestone and calcareous shale and is characterized by a crinoid and brachiopod fauna. Further lithologic analysis was helpful in locating the contact, which is primarily a pyritized hardground, between the “Squaw Bay” and the underlying Traverse Group. Lithologic analysis could not, however, indicate a definitive location for the overlying transitional contact with the Norwood Member. Lithostratigraphic data and pXRF analysis both indicated a potential subdivision of the “Squaw Bay Formation” into two units while magnetic susceptibility analysis suggests a three-member subdivision. Future research on this formation, especially in geochemical fields, would likely be beneficial in determining the upper contact and decisively subdividing the formation.

Advisor

Judge, Shelley

Department

Earth Sciences; Geology

Disciplines

Earth Sciences | Geochemistry | Geology | Paleontology | Physical Sciences and Mathematics | Stratigraphy

Publication Date

2024

Degree Granted

Bachelor of Arts

Document Type

Senior Independent Study Thesis

Share

COinS
 

© Copyright 2024 Ainsley Wiesner