Title: Lecture%2022:%20Coevolution
1Lecture 22 Coevolution
- reciprocally induced evolutionary ?s in 2 spp.
or popns - Mutualistic vs. Antagonistic
type species 1 species 2
commensalism 0
competition - -
predation -
parasitism -
mutualism
2Mutualism
- e.g. C. Am. Acacias Ants
- Herbivory ? growth permits competition from
fast growing spp. - 90 acacia spp bitter alkaloids ? prevent
insect/mammal browsing - 10 spp lack alkaloids have symbiotic ants
3Acacias Ants
- swollen thorns
- (nest sites)
- petioles (nectaries)
- Beltian bodies (protein)
- attack herbivores
- remove fungal spores
- attack shading plants
4Competition
- Anolis spp.
- spp. turnover (Caribbean islands) due to coevoln
- carrying capacity of island is a function of body
size
best body size for invading spp
5After Invasion - invader selected for smaller
body size - competition displaces residents
body size ?
frequency
body size
- Later
- invader evolves to
- optimum body size
- - eventually, resident
- driven to extinction
frequency
X
body size
6Sequential Evolution
- tit for tat
- e.g. plants herbivorous insects (predation)
- plants 2 metabolites to repel insects
- insects detoxification (mixed function oxidases)
- e.g. nicotine from a.a. or sugar pathway
7Erlich Raven (1964)
- 2 metabolites ? new adaptive zones
- MFOs ? new adaptive zones
- leads to cycle of adaptive radiations
- ? diversity
8- speciation of plant ? speciation of insect
- OR
- speciation of insect ? speciation of plant
- Phylogenetic analysis of sequential evolution
- e.g. pinworm parasites of primates
- congruent phylogenies
- divergence in host ? divergence of parasite
- not the other way around
- parasite/host interactionshost evolves defenses
- should parasite ? or ? virulence?
- depends!
9Virulence
- Transmission
- Correlated w repro rate NS ? virulence
- Requires live host NS ? virulence (trade-off)
- e.g. Myxoma virus of rabbits
- 2) Coinfection
- 1 parasite all offspring related
- kin selection ? ? virulence
- multiple infection competition
- selection for ? repro rate ? ? virulence
10- 3) Type of Transmission
- Horizontal ? virulence
- Vertical ? virulence
- Arms Race adaptive advances must be countered
or face extinction!
11e.g. Brain Size Race b/w Ungulates
Carnivores
- Ungulate
- Carnivore
12Conclusions
- Relative brain size ? through time
- Carnivores are smarter than ungulates
- Evidence for coevolution?
- Less evidence for coevoln of running speed
- Why? costs of adaptation
- resistance to 1 pred. may ? vulnerability to
others - e.g. Cucurbitacinsprotect from mites attract
beetles
13Generally
- Specialist predator Single prey ? coevoln
probable - Multiple Interactions ? coevoln slow sporadic
- How important is coevolution to pattern of
diversity? - taxonomic survival curves used to determine if
survival of taxon is age-independent
14Taxonomic Survival Curves
- Does mortality (extinction) depend on age ?
age species 1 species 2 1 1000 1000 2
900 740 3 810 600 4 729 580 5
656 570 6 590 560 7 531 550 8
478 540 9 430 460
Sp. 1 10 die yearly, regardless of age Sp. 2
mortality high for young old mortality low in
middle age
15Log - linear analysis Age - independent
mortality is linear
16Taxonomic Survival Curves
- log ( of taxa surviving) vs. age of taxon
- for most taxa linear ? age - independent
- 2 interpretations
time
time
a) constant rate of extinction b) variable
rate of extinction independent of age
17Extinction
- Probability of Extinction New Taxa Old Taxa
- What causes extinctions?
- Biotic factors antagonistic interactions
- (predn, parasitism, competn)
lag load L
Diffn b/w mean optimum genotype L ? rate of
evolution ? Why? selection coefficient ? L ?
probability of extinction ? Why? falling behind
in the arms race
18Lag-Load Models
- 1. Contractionary
- sp. w ? L falls behind, goes extinct
- 2. Expansionary
- sp. w ? L outcompetes increases
- these 2 models are unstable
- may fluctuate between 1 2
19- 3. Stationary
- all spp. L 0
- no change no extinction
- perturbations back to equilibrium
- extinctions not due to biotic factors
- 4. Dynamic Equilibrium Red Queen hypothesis
- all spp. have ? L
- Envt constantly deteriorating
- due to arms race
- running as fast as they can
- to stay in the same place!
20Implications of Red Queen to TSCs
- older taxa same prob. of extinction as newer taxa
- log - linear survival curves are evidence for RQ
- Why? zero - sum game means L stays constant
- 2 versions of RQ
- 1. Strong
- Abiotic factors negligible
- Extinctions due to spp. interns
- improbable, but testable
- 2. Weak
- Abiotic Biotic factors imp.
- likely true, but untestable
21Testing RQ using TSCs
- Evidence for Strong RQ
- constant chance of going
- extinct b/c of spp.
- interactions
- - extinctions even in
- constant physical envt !
- Evidence for weak RQ?
- other mechanisms b/c
- extinction rates fluctuate
- over time
22Lecture 23 Mass Extinctions
- Biodiversity balance b/w specn extinction
- gt 99 of all species are extinct
- Because of
- Background extinctions
- genlly due to biotic factors
- e.g. competition, predation etc.
23Background Rate
- marine families ? relatively constant
- 5 - 10 families / my
mass extinctions
e.g. Sepkoski Raup (1982)
24Ecological Significance of Mass Extinctions
- Open up vast niche spaces
- Lead to adaptive radiations
- e.g. mammals diversify after extinction of
dinosaurs - 3. Taxa can recover
- e.g. ammonites decimated in Permian extinction
came back diversified in Triassic
25Mass Extinctions of the Phanerozoic The Big 5
- 1.) Cambrian (540 - 510 mya)
- Explosion of diversification
- Marine soft-bodied (few fossils)
- Evidence for 4 separate events
- Trilobites, conodonts, brachiopods hit hard
- Cause Glaciation
- - sea level ? (locked in ice)
- - cold H2O upwelling spread
- - ? O2 levels?
262.) Ordovician (510 - 438 mya)
- 2nd most devastating to marine organisms
- Echinoderms, nautiloids, trilobites, reef -
building corals - Causes Glaciation of Gondwanaland
- evidence in Saharan deposits
- drifted over N. pole (cooling)
- sea level ?
- losses correspond to start retreat of glaciers
273.) Devonian (408 - 360 mya)
- Terrestrial life starts diversifies
- Extinctions over 0.5 - 15 my (peak 365 mya)
- Marine more than terrestrial
- Brachiopods, ammonites, placoderms
- Causes Glaciation of Gondwanaland
- evidence in Brazil
- Meteor impact?
284.) Permian (286 - 245 mya)
- formation of Pangea continental area gt oceanic
- Devastation (245 mya)
- 96 marine spp 75 terrestrial spp
- Causes
- a) formation of Pangea?
- b) vulcanism? - basaltic flows in Siberia
- - sulphates in atmosphere ? ash clouds
- c) glaciation at both poles major climatic flux
- d) ? salinity of oceans?