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Great Strategies for Teaching Paleontology: Paleobotany – 200,000 Years of Pollen and Environmental Change Christopher L. Hill Boise State University, Boise, Idaho; chill2@boisestate.edu On the Cutting Edge - Teaching Paleontology in the 21st Century Cornell University and the Paleontological Research Institute, Ithaca, NY
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Outline of Presentation Introduction: What is this activity? Context Goals Activity Description Adaptations
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Introduction: What is this activity? This is a “virtual lab” homework asignment Students experience the scientific process by: ◦Observation, identification ◦Data organization and analysis ◦Final product is a report Students use online resources ◦Identification key ◦Pollen slides to count ◦Basic table format and isotope curve provided
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Context Designed for upper-division undergraduate course in Quaternary Paleontology Majors in geosciences, geoarchaeology, environmental studies, anthropology
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Goals Introduction to Palynology; Students will… ◦Identify different fossil forms (pollen taxa) ◦Link pollen to vegetation/climate ◦Recognize changing patterns over time ◦Compare local pollen change to global isotope record Skills: “Scientific Process/Critical Thinking” ◦Observation, identification, counting ◦Organizing data ◦Analysis of data ◦Interpretations and Write-up
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Description Pre-activity introduction to paleobotany Provided online via BLACKBOARD: ◦Pollen key ◦Pollen slides ◦Step-by-step instructions for data organization and analysis ◦Stable isotope curve for last 300,000 years ◦Guide for report
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A Pollen Key for Quaternary Paleontology
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Ambrosia - Spherical - Exine: Echinate (short spines) - Favors warm, temperate climates Ragweeds (Ambrosia), also called bitterweeds and bloodweeds, are a genus of flowering plants from the sunflower family (Asteraceae)
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Picea - Vesiculate - Reticulum Bladders -The cap exine is a verrucate texture - Favors cold climates A spruce is a tree of the genus Picea, a genus of about 35 species of coniferous evergreen coniferous trees in the Family Pinaceae, found in the northern temperate or boreal regions.
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Paleobotany Project In this exercise you will 1) study a set of samples collected from the western North America, 2) compare your result to the global isotope climate record. The samples are from a sediment core from a lake basin. There are 8 samples. The top of the core dates to today, the bottom of the core extends to about 220,000 years ago. Sample 1 Today (or Recent) Sample 2 Sample 3 20,000 years ago Sample 4 Sample 5 130,000 years ago Sample 6 Sample 7 Sample 8 220,00 years ago
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Paleobotany Project Make a chart with the raw counts. Convert these into relative frequencies (percentages) for each slide (time level). Here is an example of a count sheet: Pollen Type 1 Pollen Type 2 Pollen Type 3 Total Sample 1 Sample 2 Sample 3 Sample 4 Sample 5
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Paleobotany Project Climate Set 1 Climate Set 2 Sample 1 Sample 2 Sample 3 Sample 4 Sample 5 Sample 6 Sample 7 Sample 8 Can they be grouped into sets based on what kinds of environments or climates they might indicate?
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Paleobotany Project Stable Isotope Curve to Compare with Pollen Diagram
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Paleobotany Project Written Report: “Guide to Paleobotany (Pollen) Assignment Report for Quaternary Paleontology” 1. Title 2. Introduction 3. Materials and Methods 4. Results 5. Interpretations/Discussion/Conclusion 6. Bibliography
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Adaptations Most students used EXCEL although this wasn’t part of the required assignment Some students presented data in an unconventional manner ◦Emphasize “standard” pollen chart? Different regions or timescales Links to other paleo-proxy data
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