The Evolution Of Life From The
Anaerobic To The Aerobic World
Principal Instructor: David Catling, Rm. 422, ATG Building, dcatling@u
T,Th 10.30-11.50am, F 10.30-11.20am, Rm. 406, ATG Building
The
most significant era in Earth's biological and geological history is the
Paleoproterozoic (2.5-1.6 billion years ago). It is marked by the appearance of
the first fossils visible to the naked eye, the diversification of aerobic
eukaryotes, the possible loss of anaerobic lineages of microbes, a world-wide
spread of intracontinental rifts, dramatic climate change with putative
"Snowball Earth" glaciations, the formation of an oxygenated
atmosphere, the development of the most significant positive 13C/12C
shift of sedimentary carbonates in Earth's history, a vast accumulation of 13C-depleted
organic material, and a flood of sulfate to the ocean. Yet all these events
remain poorly understood. We will review current research on the transition
from the anaerobic to aerobic world. We will conclude by moving from microbial
metabolism to global-scale thermodynamics. We will examine the global
bioenergetic change with the rise of oxygen, which allowed life to exist in
states of lower entropy.
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Week |
Session |
|
Faculty
lead |
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1 |
Geological and Biogeochemical Change
in the Paleoproterozoic |
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|
I |
Geologic
Indicators of the Rise of Oxygen |
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|
II |
|||
|
III |
Research Paper Discussion: Student debate on the Rise of Oxygen |
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|
2 |
I |
Paleoproterozoic
Biology
|
|
|
II |
|||
|
III |
Research Paper Discussion: Earliest
Evidence of Cyanobacteria?
|
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3 |
I |
Isotopes
& Global Change
|
|
|
Atmospheric Change and “Snowball
Earth” at 2.4-2.2 Ga |
|||
|
II |
The Archean-Proterozoic Atmosphere |
||
|
III |
Research Paper Discussion: A deeply
sulfidic Proterozoic ocean?
|
||
|
4 |
I |
Mass-Independent
Isotope Fractionation (MIF) in Sulfur
|
|
|
II |
The
Rise of Oxygen: Why and How Did It Happen? |
||
|
III |
Research Paper Discussion: How does
MIF work?
|
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|
5 |
I |
Paleoproterozoic
Snowball Earth: Theory
and Evidence |
|
|
II |
|||
|
III |
Research Paper Discussion: Snowball
Earth or hailstorm of hype?
|
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|
6 |
Evolution of Microbial Metabolism: From Anaerobes to
Aerobes
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|
|
|
I |
Anaerobic
Metabolism I: Methanogens
|
||
|
II |
Anaerobic
Metabolism II: Sulfate reduction |
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|
III |
Research
Paper Discussion
|
All |
|
|
7 |
I |
No Class: Veteran’s Day Holiday
|
N/A |
|
II |
Anaerobic
Metabolism III: Anaerobic Photosynthesis
|
||
|
III |
Research
Paper Discussion
|
All |
|
|
8 |
Bioenergetics and Entropy in an
Anerobic vs. Aerobic World |
|
|
|
I |
From Anaerobic to Oxygenic Photosynthesis |
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|
II |
Energy and Metabolism Thermodynamics |
David
Catling |
|
|
III |
Research
Paper Discussion
|
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9 |
I |
Oxygen,
Metabolism, and the Size of Life |
|
|
II,III |
No Class: Thanksgiving Holiday |
N/A |
|
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10 |
I |
Entropy
in Physics vs. Entropy in Information Theory
|
David
Catling |
|
II |
Linking
it all together: Life and Entropy
|
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|
III |
Research
Paper Discussion
|
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11 |
Student Paper Presentations |
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Students
should select a topic to review for a term paper by the end of week 5. This
written paper will be marked and will also be presented orally by the student
in Week 11.
During
research paper discussion sessions, students will be asked to present at least
one research paper. This part of the course is graded to ensure well-prepared
presentations.
Finally,
the instructor will give out one homework problem set in Week 9 on metabolism
thermodynamics, life and entropy.
Research
Paper Discussion: 15%
Written
term paper: 60%
Presentation
of term paper: 15%
Homework: 10%
Back to Class webpage.