UNDER THE SCOPE: INVESTIGATING THE IDLEWILD MEMBER OF THE LITHOGRAPH CITY FORMATION, DEVONIAN (FRASNIAN), IOWA BASIN
Within the Devonian sea that existed in the Iowa Basin during this time, stromatoporoids, ostracodes, brachiopods, corals, and bryozoans, mollusks, and conodonts proliferated. Sea level continued rising during this part of the Devonian (Frasnian). The fossils found in the Idlewild Member of the Lithograph City Formation represent a vibrant and diverse seafloor community. A paleoecological reconstruction including a tiering scheme has been undertaken to describe the seafloor community present at the time.
As part of this investigation, allochems have been identified in order to classify the type of carbonate according to Folk (1959). These carbonate classifications are compared to those made solely from field investigations at this site, as well as, petrographic investigations of the unit in other locations (Day, Witzke, and Lundy, 2013; Groves, Walters, and Day, 2008).