adaptive radiation & extinction Flashcards
lecture 15 - Mark Briffa
views of life since Cambrian explosion
- ‘cone of increasing diversity’
- ‘decimation and diversification’
both show adaptive radiation (increasing diversity)
both show extinction (loss of diversity)
diversity is determined by the rate of each process
adaptive radiation
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
caused of adaptive radiation
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
evidence of extinction
direct observation
- recent extinctions with anthropogenic causes
fossil record
- presence of forms no longer living
- difficult to infer why it happened
small scale extinction
local and occur over a short period of time
loss of species with limited distribution; can accumulate to cause complete extinction
mass extinction
global or continental occur over long streches of time
loss of species and taxa
causes of small scale extinctions
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)
factors affecting chance of extinction
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
the ‘big five’ mass extinctions
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
the K-T mass extinction
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
asteroid-impact theory : the K-T mass extinction
- 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
evidence to support the asteroid-impact theory
- iridium anomaly (iridium in rock strata)
- chicxulub creter (impact crater, mexico)
- rock structures
- simultaneous extinction:
• amonites
• bivalves
• brachiopods
• vertebrates (dinos)
passive replacement
the replacing fauna took advantage of the lack of the replaced one and did not compete directly with it.
early mammals
- 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