The final exam is approaching (Friday, December 16th, 12:45 to 3 pm in our classroom), covering new material taught since the Midterm, and drawing on the earlier material (time scale, any general evolutionary trends - e.g., convergence, adaptive radiation, those sorts of big concepts) as needed to discuss the significance of the new material. This is an in-class, closed-book and closed/notes exam, designed to be completed in 1.5-2 hours. Here is a sample final exam to help you prepare for the kind of questions that will be asked. This is not the final I will be giving you, but is typical of the format and is drawn from the same material. Total 100 points.
I. Definitions
1. Please write out the geologic
periods
in the time scale in order (oldest on the bottom, youngest at the top), including
dates for the boundaries between
the Archean Era and Proterozoic Era of the Precambrian, the Proterozoic
Era of the Precambrian and the Paleozoic Era of the Phanerozoic Eon,
between
the Paleozoic and the Mesozoic Era, and between the Mesozoic and the
Cenozoic
Era. Spelling Counts! 20 points
2. Please give brief definitions (one to two sentences) of any 3 of the following terms (5 points ea.): (15 total) (Note: this means, you choose 3, not more)
tiering
18O/16O
lignin
13C/12C
Paleocene Eocene Thermal Maximum (PETM)
Siberian Traps
II. Short Answer: Please choose any 3 of these 5 questions and answer with a short (1 paragraph) response. Based on class lectures and assigned readings, explain: 15 points ea. (45 total)
1. One of our questions from book discussion days on Lane's "Life Ascending" will be asked.
2. What are the major working
hypotheses for the cause(s) of the Permian-Triassic extinction event?
3. What are the major working hypotheses for the cause(s) of the Cretaceous-Tertiary (Paleogene) extinction event?
4. The
Jurassic Ocean was marked by OAE's (Ocean Anoxia Events) apparent as black
shales. One
outcome of these events was a diversification in types of reef structures.
How did reef communities respond to the dysoxic and anoxic conditions of
Jurassic seas?
5. The PETM and early Eocene Warmth are distinctly tracked with the
fossil record. Discuss two lines of fossil evidence that indicate the
onset, rise and end of this global warming event of the early Eocene.
III. Essay Answer: Please choose 1 of these 3 questions and answer with a one page essay response. 20 points ea. (20 total) Based on your readings and class lectures:
Note: Refer to the isotope curve for the Cenozoic (Zachos et al., 2001 listed on class web page under Useful Links) when reading questions 1 and 2:
1. Here is the oxygen isotope curve from marine benthic foraminifera for the Cenozoic Era. Why is this kind of curve an important part of the argument that Earth moves from a “hothouse” to an “ice house” mode by mid-Cenozoic time? (e.g., Why does a record from forams tell us anything about past climate?)
2. Here is the oxygen isotope curve from marine benthic foraminifera for the Cenozoic Era. Discuss the important tectonic events that affected global climate at approximately 30 -35 m.y.a. and 3-4 m.y.a. What has been the effect on climate and the biosphere of these events?
3. How do these two equations link activity in the terrestrial biosphere to the changes in atmospheric oxygen concentration in the late Paleozoic (Devonian through Permian)?
2Fe2O3 + 8SO42- + 16H ↔ 15O2 + 4FeS2 + 8H2O
CO2 + H2O ↔ CH2O + O2