adaptive radiation & extinction Flashcards

lecture 15 - Mark Briffa

1
Q

views of life since Cambrian explosion

A
  1. ‘cone of increasing diversity’
  2. ‘decimation and diversification’

both show adaptive radiation (increasing diversity)
both show extinction (loss of diversity)
diversity is determined by the rate of each process

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2
Q

adaptive radiation

A

a small number of ancestoral species increaes to giver a large number

radiations are very clear when observed in a small taxonomic group

e.g galapagos finches

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3
Q

caused of adaptive radiation

A

colonization of a new area free of competators : adaptations to exploit new resources

adaptive breakthrough : adaptations to exploit new resources

extinction of competitors : adaptations to explot previously used resources

replacement of competators : superior adaptation or environmental change

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4
Q

evidence of extinction

A

direct observation
- recent extinctions with anthropogenic causes

fossil record

  • presence of forms no longer living
  • difficult to infer why it happened
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5
Q

small scale extinction

A

local and occur over a short period of time

loss of species with limited distribution; can accumulate to cause complete extinction

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6
Q

mass extinction

A

global or continental occur over long streches of time

loss of species and taxa

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7
Q

causes of small scale extinctions

A

biotic
- parasite, pathogens, competitors - losing an evolutionary arms race

physical
- change in climate

developmental constarints prevent adaptations to change

(extinction happens because environmental changes happen faster than the rate of adaptation)

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8
Q

factors affecting chance of extinction

A

population size
- small or isolated population more likely to become extinct that large connected ones

longevity
- short lifespan more susceptible than long lived species

rate of increase
- few young and reproduce irregularly more susceptible than species with high reproductive outputs

stability of environment

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9
Q

the ‘big five’ mass extinctions

A
late ordovivian - 400 mya 
late devonian - 350 mya 
end permian - 250 mya 
late truassic - 210 mya 
end cretaceous - 80 mya 

the average ate of extinction appears to have declined

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10
Q

the K-T mass extinction

A

60-75% of species lost
seperates the Cretaceous - Tertiary boundary
affected every group of animals and plants
best evidence given by microfossils - Foraminfera
- dinosaurs and ammonites went extinct (allowed adaptive radiation of mammals)
- crocs survived

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11
Q

asteroid-impact theory : the K-T mass extinction

A
  • 7.5 - 9 miles in diametre
  • 108 megatos blast
  • concurrent impact s as an even larger asteroid broke up
  • global dust blocks sunlight for several years:
    • global warming
    • acid rain
    • vulcanisation
    • global fires
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12
Q

evidence to support the asteroid-impact theory

A
  • iridium anomaly (iridium in rock strata)
  • chicxulub creter (impact crater, mexico)
  • rock structures
  • simultaneous extinction:
    • amonites
    • bivalves
    • brachiopods
    • vertebrates (dinos)
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13
Q

passive replacement

A

the replacing fauna took advantage of the lack of the replaced one and did not compete directly with it.

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14
Q

early mammals

A
  • early mammals small, low abundance
  • arboreal
  • mammals lay low for 40 myr until extinxtion of dinos : allow for adaptive radiation
  • modern orders adapted into vacated niches
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