Course GEOSC 897A:
Earth's History: Interactions Between Life and the Environment
(Both Part 1 and Part 2 offered summer 2009)
For Educators Grades 6-12
June 28 - July 2, 2009
This workshop will begin at NOON on Sunday, June 28th and will conclude at 4:00pm on July 2nd, to accomodate the 4th of July holiday.
- How did the rise of oxygen affect the evolution of animals and the Earth’s climate?
- Were all mass extinctions caused by the same type of environmental trigger?
- Is modern global warming happening faster than did previous climate changes in earth history?
Educators will develop an appreciation for the rate of climate change and biodiversity loss today through a study of the coevolution of Earth and life through geologic time. Investigate the current scientific understanding of Earth history through interactions with leading experts in geochemistry, geology, and paleobiology. Participants will learn how Earth scientists determine the ages of rocks using state-of-the-art methods in geochronology and gain hands-on experience applying these methods in a local geologic setting. Astrobiology themes will be woven throughout this workshop.
Given this foundational perspective of Earth science through deep time, teachers will then work with the Earth and Mineral Sciences Museum at Penn State to assist in developing a museum exhibit based upon the research being conducted by Dr. Mark Patzkowsky and others. During the school year, with support from PSU faculty and graduate students, teachers will implement the workshop content into the classroom.
Returning teachers will complete the museum exhibit, share their implementation strategies and producsts from the 2008-2009 school year with the new participants, and learn additional astrobiology content information from our NASA Astrobiology Institute science team. Teachers attending the workshop for the first time will receive content and related hands-on activities to incorporate into their classroom instruction, in addition to collaborations with the returning students.
Tentative Schedule
Sunday: Orientation
Monday: Age of the earth, geologic time
Tuesday: Origin of earth and life, early earth environment
Wednesday: Rise of oxygen, molecular clocks and the origin of major groups
Thursday: Geologic history of biodiversity; mass extinction
Friday: Global warming and the biodiversity crisis
Facilitators: Mark Patzkowsky and James Kasting
PSU Researchers: Mark Patzkowsky and James Kasting
National Science Education Standards
•Life Science
• Diversity and Adaptations of Organisms
4–8 Grade:
- Millions of species of animals, plants, and microorganisms are alive today. Although different species might look dissimilar, the unity among organisms becomes apparent from an analysis of internal structures, the similarity of their chemical processes, and the evidence of common ancestry.
- Biological evolution accounts for the diversity of species developed through gradual processes over many generations. Species acquire many of their unique characteristics through biological adaptation, which involves the selection of naturally occurring variations in populations. Biological adaptations include changes in structures, behaviors, or physiology that enhance survival and reproductive success in a particular environment.3. Extinction of a species occurs when the environment changes and the adaptive characteristics of a species are insufficient to allow its survival.
- Fossils indicate that many organisms that lived long ago are extinct. Extinction of species is common; most of the species that have lived on the earth no longer exist.
• Biological evolution
9–12 Grade:
- Species evolve over time. Evolution is the consequence of the interactions of (1) the potential for a species to increase its numbers, (2) the genetic variability of offspring due to mutation and recombination of genes, (3) a finite supply of the resources required for life, and (4) the ensuing selection by the environment of those offspring better able to survive and leave offspring. [See Unifying Concepts and Processes]
- The great diversity of organisms is the result of more than 3.5 billion years of evolution that has filled every available niche with life forms.
- Natural selection and its evolutionary consequences provide a scientific explanation for the fossil record of ancient life forms, as well as for the striking molecular similarities observed among the diverse species of living organisms.
- The millions of different species of plants, animals, and microorganisms that live on earth today are related by descent from common ancestors.
- Biological classifications are based on how organisms are related. Organisms are classified into a hierarchy of groups and subgroups based on similarities which reflect their evolutionary relationships. Species is the most fundamental unit of classification.
• Earth and Space Science
• Origin and Evolution of the Earth System
4–8 Grade:
- Geologic time can be estimated by observing rock sequences and using fossils to correlate the sequences at various locations. Current methods include using the known decay rates of radioactive isotopes present in rocks to measure the time since the rock was formed.
• Earth's History
9–12 Grade:
- The earth processes we see today, including erosion, movement of lithospheric plates, and changes in atmospheric composition, are similar to those that occurred in the past. earth history is also influenced by occasional catastrophes, such as the impact of an asteroid or comet.
- Fossils provide important evidence of how life and environmental conditions have changed.
Pennsylvania Academic Standards for Science and Technology with Assessment Anchors
Grade 10:
Geologic History; Correlate rock units with general geological time periods in the history of the earth; evaluate and interpret geologic history using geological maps; interpret topographic maps to identify and describe significant geological history/structures in PA; Describe the processes that formed PA geologic structures and resources including mountains, glacial, water gaps, and ridges; examine and describe recurring patterns that form the basis of ...geological order: Explain the mechanisms of the theory of evolution;
Grade 12:
Interpret Geological Evidence Supporting Evolution; Analyze how models, systems...changed over time (evolution); Critically evaluate the status of existing theories (evolution); Analyze and evaluate earth features and processes that change the earth - Interpret geological evidence supporting evolution;
Lead Instructors
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Mark Patzkowsky is an associate professor of geosciences in the College of Earth and Mineral Sciences at Penn State. He uses field observations and large databases to understand the physical and biologic factors that govern the distribution and abundance of organisms over geologic time. Most recently, he and his students have begun investigating the major mass extinctions in earth history. Mark has led field trips and conducted his own research in many geologically interesting areas across the United States. He is currently working in the Bighorn Mountains, Wyoming. He has also been a contributor to the Paleobiology Database since its inception and he has served on the advisory board since 2000. Mark has published on a wide range of topics in earth history and is currently working on a book on stratigraphic paleobiology. |
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James Kasting is a professor at Penn State University, where he holds joint appointments in the Departments of Geosciences and Meteorology. He received his undergraduate degree from Harvard University in Chemistry and Physics and did his Ph.D. at the University of Michigan in Atmospheric Sciences. Prior to coming to Penn State in
1988, he spent 7 years in the Space Science Division at NASA Ames Research Center. His research focuses on the evolution of planetary atmospheres, particularly the question of why the atmospheres of Mars and Venus are so different from that of Earth. He is also interested in the question of whether habitable planets exist around other stars and how we might look for signatures of life by doing spectroscopy on their atmospheres. |