Ecology through time Flashcards

1
Q

The creation of the Atlantic

A
  • Isolation: the biota of the Americas and Africa become isolated, creation of new mountain ranges split continents
  • New shallow seas - hotspot for diversification (centres of biodiversity)
  • New ocean seaways and terrestrial land bridges: Biotic exchange
  • Subduction creates oceanic islands; dispersal and isolated evolution
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2
Q

Tectonic and mass extinctions

A
  • Mass extinction events linked to multiple drivers - bolide impacts
  • But all 5 mass extinctions linked to marine regression/transgression events
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3
Q

Biotic interchange

A

Biotic interchange: large-scale exchange of species from two distinct and isolated biota
- Barriers to species dispersal are reduced :
- Usually bc two continents come together
- Or a seaway opens to connect previously separated oceans

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4
Q

Great American Biotic Interchange (GABI)

A
  • GABI triggered by the formation of a land bridge between N and S America
    -The combination or dispersal, species interactions, extinction and revelation had dramatic effects on biodiversity of two continents
  • Focus on mammals - the best fossil record
  • Mammals evolved 220 million year ago
  • Pangaea - S America becomes isolated 140-75 million years ago and mammal families evolved in isolation
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5
Q

GABI

A
  • Isolation not continuous, later land bridges and long distance dispersal events added primates
  • Added diversity upon arrival and all the groups diversified
  • By 3.5 million years ago S America had developed unique mammal biota - a small pool of species but diversification and adaptive radiation
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6
Q

Adaptive Radiation

A
  • It is a rapid increase in the number of species with a common ancestor, characterised by great ecological and morphological diversity
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7
Q

Why is there such an unbalanced interchange?

A
  1. Nothern species have a high greater dispersal ability - NA contained more savanna specialists so greater migration over the land bridge (filter effects)
  2. Nothern species had higher survival and speciation rates - a higher proportion of SA species that arrived in NA subsequently went extinct
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8
Q

Biodiversity on islands

A
  • Tectonics create new landmass + control isolation of existing landmasses
  • Dispersal, speciation and extinction
  • Species richness tends to increase with increasing area
  • Increase in species slows with increasing island size
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9
Q

Species-isolation relationship

A
  • Islands far away from continents have fewer species
  • Species richness declines with isolation
  • Most islands have 0 species and they are added by dispersal and colonisation
  • Once arrived species can only be lost by local extinction
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10
Q

Equilibrium Theory of Island Biogeography

A
  • McArthur and Wilson 1967
  • Species richness on the island will result from immigration on the island and extinction of species on the island
    Extinction rate = Extinction risk * number of species
  • Extinction rate increases as SR increase in the island bc number of species at risk increases
  • Also increasing extinction risk bc fewer resources per species
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11
Q

Equilibrium Theory of Island Biogeography

A
  • Number of new species arriving on the island is
    matched by the number of species going extinct
  • Equilibrium species richness is lower
  • Dispersal is more unlike to more isolated areas
  • Immigration rate is lower of new species
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12
Q

Endemism: Global scale patterns

A
  • Endemic species: a species restricted to a particular area like an area
  • Islands have fewer species than the continents but have far more endemic species
  • Remote oceanic islands are hotspots of endemism
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13
Q

Why do islands have more endemics?

A
  • Few founding events
  • Low gene flow from the continents
  • New unexploited niches
  • Larger islands = lower extinction
  • Greater resources
  • Larger population sizes
  • Greater range of niches
  • Larger islands = higher probability of vicariance
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14
Q

How and why are islands dynamic?

A
  1. Uplift and weathering e.g atoll life cycle
  2. Successional processes e.g. the development of soil + change in topography
  3. Long-term climate changes (and sea level)
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15
Q

How isolated are oceanic islands?

A
  • Modern Hawaiian islands contain many species that initially colonised on now submerged islands
  • Exposed seamounts exposed during low sea levels act as stepping stones for dispersal
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16
Q

Volcanic archipelagos - island hopping?

A
  • Species can disperse in both directions
  • Each island provides opportunity for divergence
  • Colonisatiion along the chain
  • Islands in a chan influence each other