WK12: Geographic or Global Ecology - Part 1

Geographic and Global Ecology

Origins of Geographic and Global Ecology

  • Emerged from natural history observations.
  • Early origins linked to natural historians of the late 1700s and 1800s:
    • Joseph Banks (Australia).
    • Von Humboldt and Von Plante (South America).
    • Charles Darwin (South America and Australia).
    • Alfred Russell Wallace (Indonesia).
  • Wallace's Line: A biogeographic boundary distinguishing between Asian and Australian fauna in the Indonesian archipelago.
    • North and west: predominantly Asian fauna.
    • South and east: predominantly Austro-Papuan fauna.
    • The underlying land areas in the Pleistocene were more connected due to lower sea levels.
    • Land bridges facilitated fauna movement. For example, Borneo, Sumatra, and Java were linked to Southeast Asia, and Papua New Guinea was linked to Australia via the Sahul Shelf.
    • The deep water straight now known as Wallace's Line acted as a barrier, preventing fauna exchange between Southeast Asia and the Austro-Papuan region.

Key Theories

  • Species-area relationships.
  • Equilibrium theory of island biogeography.

Species-Area Relationships

  • Possibly the most consistent generalization in ecology.
  • Species richness varies with the total area available.
    • Applies to continents, islands, remnant habitats, and aquatic systems like lakes.
    • Positive relationship between land area and the number of mammal species (log scales).
Examples
  • Number of mammal species vs. area of continents and large islands.
  • Number of plant species vs. area of islands in the Galapagos (log scale).
  • Jim Brown's study using mountain peaks as habitat patches:
    • Mountain peaks treated as islands due to isolation by intervening valleys.
    • Positive relationship found between land area and the number of mammal species on mountain peaks (log scale).
Species-Area Function
  • S=cAzS = cA^z
    • S = species richness.
    • A = area.
    • c = constant.
    • z = constant (slope of the line when the equation is logged).
  • Solving the equation by logging:
    • log(S)=log(c)+zlog(A)log(S) = log(c) + z * log(A)
  • A plot of species richness vs. log area yields a straight line.
  • The slope of the line (z) measures how quickly richness increases with area.
  • If z=0.3z = 0.3, species richness doubles for every tenfold increase in area.
Empirical Evidence
  • Jim Brown's work on mountain peaks:
    • Compared birds and mammals.
    • Found a steeper slope (higher z value) for mammals (0.326) than for birds (0.165).
    • Explanation: Birds' higher mobility allows them to move between mountain peaks more easily, reducing the influence of isolation on species richness changes.

Equilibrium Theory of Island Biogeography

  • Developed by MacArthur and Wilson.
  • Species richness on islands is determined by an equilibrium between colonization and local extinction events.
  • Colonization: Arrival and persistence of a species on an island.
  • Extinction: Loss of a species from a single patch or island (not necessarily global extinction).
Model Explanation
  • Consider a large continental landmass as a source for a smaller island patch.
  • Colonization rate decreases as the number of species on the island increases.
  • Extinction rate increases as the number of species on the island increases.
Graphical Representation
  • Number of species present (x-axis) vs. rate of immigration or extinction (y-axis).
  • Immigration rate decreases as the number of species increases.
  • Extinction rate increases as the number of species increases.
  • The intersection of the immigration and extinction curves indicates the equilibrium number of species.
Distance and Area Effects
  • Distance and area affect the equilibrium species richness.
  • Empirical evidence from bird colonization of satellite islands around New Guinea:
    • Species-area relationship observed.
    • Distance effect: Colonization curve is shifted upwards for near islands due to higher dispersal ability.
    • Extinction curve is shifted upwards for smaller islands due to increased susceptibility to stochastic events and less area to support species.
Dynamic Equilibrium
  • The theory postulates a dynamic equilibrium, not a static response.
  • Species richness fluctuates around a mean due to ongoing species colonizations and extinctions.
Evidence for Dynamic Equilibrium
  • Jared Diamond's work on Californian islands:
    • Compared species lists of birds from 50 years prior to his study.
    • Found that species richness was broadly the same, but species composition had changed.
    • Evidence of species extinctions and colonizations occurred, demonstrating a dynamic interaction.