Transcript Chap22
Geographic Ecology
Chapter 22
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Outline
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Introduction
Island Area, Isolation, and Species Richness
Terrestrial
Aquatic
Equilibrium Model of Island Biogeography
Latitudinal Gradients in Species Richness
Historical and Regional Influences
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Introduction
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MacArthur defined geographic ecology as
the search for patterns of plant and animal
life that can be put on a map.
Above level of landscape ecology.
Vast breadth
Chapter only focuses on a few aspects.
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Island Area, Isolation, and Species
Richness
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Preston found fewest bird species live on
smallest islands and most species on largest
islands.
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Nilsson et al. found island area was best
single predictor of species richness among
woody plants, carabid beetles, and land
snails.
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Island Area, Isolation, and Species
Richness
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Habitat Patches on Continents: Mountain
Islands
As Pleistocene ended and climate warmed,
forest and alpine habitats contracted to the
tops of high mountains across American
Southwest.
Woodlands, grasslands, and desert scrub,
invaded lower elevations.
Once continuous forest converted to
series of island-like fragments associated
with mountains: Montane.
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Lakes as Islands
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Lakes can be considered as habitat islands.
Differ widely by degree of isolation.
Tonn and Magnuson found the number
of species increases with the area of an
insular environment.
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Marine Islands
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MacArthur and Wilson found isolation
reduces bird diversity on Pacific Islands.
Island area and species richness in Azore
Islands:
Birds show clear influence of isolation on
diversity, pteridophytes do not.
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Marine Islands
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Isolation and Habitat Islands on Continents
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Lomolino et al. found a strong negative
relationship between isolation and the
number of montane mammal species living
on mountaintops across the American
Southwest.
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Equilibrium Model of Island Biogeography
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MacArthur and Wilson: Model explaining
species diversity on islands = immigration
and extinction rates.
Rates of immigration highest on new
island with no organisms.
As species accumulate, rate of
immigration declines since fewer
arrivals arenew species.
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Equilibrium Model of Island Biogeography
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Equilibrium Model of Island Biogeography
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Rate of extinction rises with increasing
number of species on an island for three
reasons:
More species creates larger pool of
potential extinctions
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Equilibrium Model of Island Biogeography
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Rate of extinction rises with increasing
number of species on an island for three
reasons:
More species creates larger pool of
potential extinctions
As number of species increases,
population size of each must diminish
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Equilibrium Model of Island Biogeography
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Rate of extinction rises with increasing
number of species on an island for three
reasons:
More species creates larger pool of
potential extinctions
As number of species increases,
population size of each must diminish
As number of species increases,
competitive interactions between species
will increase
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Equilibrium Model of Island Biogeography
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Point where two lines cross predicts the
number of species on island
Rates of extinction determined mainly by
island size:
Large near islands = highest S
Small far islands = lowest S
Small near and Large = intermediate S
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Equilibrium Model of Island Biogeography
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Species Turnover on Islands
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Equilibrium model predicts species
composition on islands is dynamic
Change = species turnover
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Diamond: birds on 9 CA Channel Islands in
stable equilibrium
Species turnover result of equal levels of
immigration and extinction
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Species Turnover on Islands
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Experimental Island Biogeography
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Simberloff and Wilson studied insect
recolonization in Florida Keys
Chose 2 stands of mangroves as control
islands; 6 others as experimental islands
Defaunated islands
Followed recolonization for 1 yr
– Species number constant, but
composition changed considerably
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Spray insecticide on 2 islands, 6 no spray
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Experimental Island Biogeography
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Manipulating Island Area
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Simberloff tested effect of island area on
species richness = cut mangroves out
area reduced, S decreased
control island S increased slightly
reduced area < species
Area has positive influence on S
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Simberloff (1976) Manipulating Island Area
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Latitudinal Gradients in Species Richness
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Latitudinal Gradients in Species Richness
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Most groups of organisms are more speciesrich in tropics
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Brown grouped hypotheses into six
categories:
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1. Time Since Perturbation
More species in the tropics because
tropics are older and disturbed less
frequently
More time for speciation, less
frequent disturbance reduces
extinction rate
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2. Productivity
High productivity = high species
richness (coral reefs, rainforests)
More energy to divide among
population
3. Environmental Heterogeneity
More heterogeneity, more potential
habitat areas and niches
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4. Favorableness
Tropics more favorable environments
No extremes to limit diversity
5. Niche Breadth and Interspecific
Interactions
Various themes
Brown: biological processes play
secondary role
– Ultimate causes are physical
differences
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6. Speciation rates and extinction rates
Tropics have increased speciation
Tropics have decreased extinction
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Area and Latitudinal Gradients
in Species Richness
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Rosenzweig: immigration can be largely
discounted at broad scales, thus speciation
is primary source of new species
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Area and Latitudinal Gradients
in Species Richness
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Rosenzweig: immigration can be largely
discounted at broad scales, thus speciation
is primary source of new species
Species removal via extinction
Tropics richness is greater due to higher
rates of speciation and / or lower rates
of extinction
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Continental Area and Species Richness
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Rosenzweig - strong positive relationship
between area and species diversity
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Map with real projection
Tropics have higher area
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Historical and Regional Influences
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Latham and Ricklefs: diversity of temperate
zone trees cannot be explained by area
effect
Temperate forest biome in Europe,
Eastern Asia, and Eastern North America
all have ~ similar area, but different levels
of biological diversity
Eastern Asia: 3x NA and 6x Europe.
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Diversity of Temperate Trees
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Latham and Ricklefs: Must examine
conditions in these regions during last glacial
period
Mountains in Europe form east-west
oriented barriers
During last ice age, temperate trees had
southward retreat largely cut-off
Lower species richness as
consequence of higher extinction rate
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Diversity of Temperate Trees
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Latham and Ricklefs: Must examine
conditions in these regions during last glacial
period
Mountains in Europe form east-west
oriented barriers
During last ice age, temperate trees had
southward retreat largely cut-off
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Historical and Regional Influences
Appalachian Mountains in N.A. run northsouth
temperate trees had retreat path as
temperatures cooled
Also no mountain barriers in Asia
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Historical and Regional Influences
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Appalachian Mountains in N.A. run northsouth; temperate trees had retreat path as
temperatures cooled.
Also no mountain barriers in Asia.
Most temperate tree taxa originated in
Eastern Asia - dispersed to Europe and N.A.
After dispersal lines were cut, speciation
continued in Asia
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Review
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Introduction
Island Area, Isolation, and Species Richness
Terrestrial
Aquatic
Equilibrium Model of Island Biogeography
Latitudinal Gradients in Species Richness
Historical and Regional Influences
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