Ecology
Populations, communities and ecosystems, from growth models to biomes
About this course
Ecology from population models to the biosphere — growth, life tables and regulation, species interactions, community structure and succession, energy flow and nutrient cycles, and climate and human forcing.
What you will be able to do
- Model population growth with exponential, logistic and life-table methods
- Analyse predator–prey and competitive interactions and relate them to the niche
- Explain how community structure changes on islands and during succession
- Trace energy flow and nutrient cycling through an ecosystem
- Relate the distribution of biomes to climate and assess human forcing of ecosystems
What this course covers
- Sun to plant: the one-percent ceiling
- Why one percent is a theorem, not a failure
- The trophic pyramid and the ten-percent rule
- Transfer efficiency as a product of three fractions
- The ten-percent rule as a log-scale geometric mean
- Chain length and the inverted biomass pyramid
- Worked example: forest production to wolf territory
- Exponential population growth and doubling time
- R as rate per head: meaning and limits
- K as rate reaching zero, not a physical wall
- Logistic growth model
- Human population curve and demographic transition
- Sustainable harvest and the collapse cliff
- Worked deer-herd example: four ecological conversions
- Lotka-Volterra predator-prey equations
- Neutral cycles versus limit cycles
- Holling's functional response
- Dual regulation of the hare cycle
- Rosenzweig-MacArthur isoclines and the paradox of enrichment
- Fitting the lynx–hare cycle to the model
- Worked example: voles and weasels
- Solar insolation by latitude and season
- Hadley cell and the 30-degree desert belt
- Global circulation belts and continental modifiers
- Whittaker's biome plane
- Limits of mean annual temperature as a classifier
- Thornthwaite water balance
- Mountain as a folded latitude and the tree line isotherm
- Species–area power law and loss rate
- Diversity indices: Shannon and Simpson
- Extinction debt and law limitations
- Keystone species and trophic cascades
- May vs. Tilman: stability of parts vs. steadiness of whole
- Food webs and May's stability criterion
- Worked example: applying S = CA^Z and diversity indices
- Lotka-Volterra Competition Equations and Four Outcomes
- Alpha as a Summary Coefficient: Strengths and Limits
- Gause's Competitive Exclusion Principle
- Tilman's R* Rule and Resource Competition
- The Niche: Fundamental, Realized, and Limiting Similarity
- Synthesis: Five-Line Master Summary
- Worked Example: Two Grasses
- Biogeochemical cycles: boxes, arrows, and residence time
- Exchange time vs. perturbation lifetime of CO₂
- Why the airborne fraction is near one-half
- The Keeling curve and the two-box model
- Nitrogen cycle doubled by human fixation
- Phosphorus: a one-way cycle with no gaseous reservoir
- Hubbard Brook: forest nitrogen held by uptake, not storage
- Worked example: emissions to ppm, date of 500 ppm, and two timescales
- The Life Table: Survivorship, Mortality, and Expectancy
- Cohort vs. Period Life Tables
- Net Reproductive Rate R₀, Generation Time T, and Intrinsic Rate r
- Effect of Breeding Timing on r (Cole's Result)
- The Leslie Matrix and Stable Age Structure
- Population Momentum
- Gompertz's Law and the Human Lifespan
- Elasticity and the Juvenile Survival Lever
- Extinction rate and species-area debt
- Limits of the vertebrate extinction count
- Logistic harvest, maximum sustainable yield, and fixed-catch collapse
- Why the Grand Banks collapsed despite effort-based fishing
- Climate velocity and the species-climate race
- Mechanism vs. trend: why these numbers are not Malthusian projections
- Human appropriation of net primary production and the Living Planet Index
- Island Equilibrium Theory: Two Lines and a Crossing
- Why the Two Lines Curve: Distance and Area Parameters
- Tests of the Theory: Simberloff's Islets and Krakatau
- Conservation Implications: Turnover, Relaxation, and Reserve Design
- Succession and Nitrogen Fixation at Glacier Bay
- The Climax as a Matrix's Stationary Vector
- Intermediate Disturbance and the Landscape Mosaic
- Olson's exponential decay of litter
- Soil carbon pools and their residence times
- Steady-state store: input over K
- Carbon-to-nitrogen ratio and the line at 20
- Two-pool soil feedback and the permafrost
- Meentemeyer's regression: K from climate and lignin
- Worked example: warming a woodland floor
- SIR model and epidemic threshold
- Final size equation
- R₀ as a ratio of rates and intervention logic
- Herd immunity threshold and endemic dynamics
- Anderson–May host regulation by pathogens
- Aggregated worm burdens and negative binomial distribution
- Mutualism as Lotka-Volterra with reversed signs
- Daisyworld: feedback without foresight
- Earth's energy balance and the greenhouse
- Ice-albedo feedback and snowball hysteresis
- Lake phosphorus: two states and hysteresis
- Self-reinforcing feedbacks and the fold as a theorem
- Carbon budget: cumulative warming and time paths
- Worked example: planet arithmetic on one page
- Ricker Map: Discrete-Generation Dynamics
- Why the Ricker Map Overshoots the Logistic
- Regulation vs. Stability: Not the Same Word
- Delayed Logistic and the π/2 Threshold
- Distinguishing Cycles, Chaos, and Weather Noise
- Allee Effect: Threshold and the Harvest Cliff
- Killing-Power Accounting: Key Factor vs. Regulating Factor
Syllabus
Population Dynamics
- L1 · Exponential and Logistic Growth
- L2 · Life Tables and Age Structure
- L3 · Density Dependence and Regulation
Species Interactions
- L4 · Predator-Prey
- L5 · Competition and the Niche
- L6 · Parasites, Pathogens and Mutualists
Communities
- L7 · Community Structure
- L8 · Islands and Succession
Ecosystems
- L9 · Energy Flow
- L10 · Nutrient Cycles
- L11 · Decomposition and Soil
Climate, Humans and the Biosphere
- L12 · Climate and Biomes
- L13 · Humans as a Forcing
- L14 · The Integrated Biosphere