

Time Frame – 40 minutes
Materials
Advanced Preparation In order to complete this activity, the student should have a concept of the foraminifera and how different benthic foraminifera prefer a particular environment, which may be associated with water depth. The student should also have had an introduction to the concept of geologic time and feel comfortable working with a map. Familiarity with the concepts of petroleum reservoir rock and source rock from studies of earth sciences is useful. Introduce the concept that benthic foraminifera live in a preferred environment; but after their death their shells may be transported to a different environment. Transportation occurs downslope due to gravity processes. Therefore, in a sample the students will find a mixture of foraminifera, specifically a death assemblage, representing foraminifera living at one time in that environment and foraminifera transported from shallower water depths into that environment. Guide the students to initiate the mental leap of understanding that in order to interpret the water depth in which the foraminifera were deposited and later buried, the deepest dwelling forms represent the true water depth. Specifically, at a present water depth of 1,000m, foraminifera will be found there which preferred to live in that environment as well as foraminifera that were brought in from shallower water by downslope processes (i.e. the Amazon Fan moves sediment, including foraminifera, in a downslope direction off of Brazil). Foraminifera preferring parameters characteristic of water depths greater than 1,000m would not be found at this sight. The students should interpret past water depth based on the deepest dwelling form found in the sample.
Procedure
Formative Assessment Make an interpretation for water depth for the various samples you have analyzed. Notice that each box displays the various foraminiferal species found in the sample. Compare each sample in Figure 3 with the key to Miocene environments in Figure 1. In the blank for paleo-water depth interpretation under each sample, put a water depth range inferred from your analysis. Notice that Sample 2 has been interpreted for you. What would cause the lack of foraminifera in Sample 9? Look at the sample’s position to other samples on the map in Figure 2. After you have made an interpretation for each sample, mark these paleo-water depth numbers on your map (Figure 2). Notice that the interpretation for Sample 2 has been done for you. Look at the distribution of water depths on your map. Based on this information could you give an estimate of where the beach was located during Miocene time in the study area? Using a colored pencil, highlight and label the potential trend of the beach (shoreline) and its location. Do you see potential for source rocks in the study area during this time? If you do, highlight and label the potential source rock area with a different colored pencil. State your recommendation to Earthquest Inc. as to the description of the general environment of this area during Miocene time and the potential for reservoir and source rock in the area. Make a specific recommendation to your company as to whether they should continue looking in this general area for hydrocarbon prospects based on your research. Summative Assessment Instructor will lead students through the visualization
module on the Ice Age. The CD is included at the back of the workbook. This
CD-ROM visualization module was developed at the University of Minnesota, by
the Department of Geology and Geophysics. The module was funded in part by the
National Science Foundation. This material requires the installation of Quicktime
version 3.0 or greater. To install this go into the folder called Quicktime
on the CD and click on the installer icon. Once Quicktime is installed, begin
the module by clicking on the TheIceAge.htm file. (If the movies are not working
correctly, try reinstalling the Quicktime on this CD.)
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