Title: What causes extinction?
1What causes extinction?
- Old explanations
- Maladaptation - organisms evolved poorly-adapted
features - Racial senescence - species became weak over
time - Discuss the likelihood of these explanations with
your table
2Adaptation, not maladaptation
- No mechanism for maladaptation
- Natural selection increases, not decreases,
fitness - Species arent organisms - no programmed species
death and no mechanism for weak genes
3Is everyone equally vulnerable to extinction?
- Generalists v. specialists
- Relationship between extinction and speciation
rates - Organisms that speciate readily also tend to have
short species duration - high speciation and high
extinction rates go together - Talk at your table about what would cause high
speciation rates
4Examples
- High extinction and speciation
- Mammals (E0.71/my, S0.93/my)
- Also trilobites, ammonites, graptolites
- Low extinction and speciation
- Clams (E0.09/my, S0.15/my)
- Nautiloids
5Mass Extinction Causes
- Coincidence lots of organisms happened to die at
the same time. Can be ruled out statistically. - Need to be especially cautious if the species
that go extinct are unstable groups - More persuasive if stable groups also suffer
extinction
6Mass Extinction Causes
- Coincidence
- Physical causes
- changes in climate
- Salinity
- living space reduction in continental shelf
space due to plate motions or regression
7Mass Extinction Causes
- Coincidence
- Physical causes
- Biological causes competition, predation
8Mass Extinction Causes
- Coincidence
- Physical causes
- Biological causes
- Catastrophe impact, volcanoes
9Permo-Triassic extinction
- Coincidence? Over 90 of life dies, so
definitely real
10Permo-Triassic extinction
- Coincidence? No
- Physical Continental configuration and
regression - Reduced continental shelf space
- Glaciation
- Severe climate
11Permo-Triassic extinction
- Coincidence? No
- Physical
- Continental configuration and regression
- Biological Appearance of biological
bulldozers - Shallow burrowers
- Earlier life was immobile bottom dwellers
(brachiopods, bryozoans, crinoids, etc.)
12Permo-Triassic extinction
- Coincidence? No
- Physical Continental configuration and
regression - Biological Appearance of biological bulldozers
- Catastrophe
- Impact? Probably not
- Lack of tektites, shocked quartz
- Some iridium, but not enough
13Permo-Triassic extinction
- Coincidence No
- Physical Continental configuration and
regression - Biological Appearance of biological bulldozers
- Catastrophe
- Impact? Probably not
- Volcanoes (Methane hydrates)
14Flood Basalt effects
- Increased carbon dioxide and global warming
- Acid rain from sulphur
- Release of methane hydrates from ocean floor
15Testing the volcanic hypothesis
- For volcanic hypothesis to be credible
- Eruptions must predate the extinction
- Extinctions must not be instantaneous
- Expect to see pulses of extinction as disaster
intensifies
16Permian
- Sooo
- Its complicated - plenty of instability
physical, biological and disaster - Insufficient evidence yet to point to a single
cause
17Cretaceous-Tertiary Extinction
- Coincidence85 species extinction, so its real
- No big physical changes - many small continents
with lots of shelf space, mild climate - No big biological changes preceding the
extinction, no big change in ecological structure
of the oceans after the extinction - That only leaves catastrophe
18K/T Catastrophe
- Impact hypothesis
- Volcanic hypothesis
19Impact scenario
- Asteroid about 10 km (6 mi.) struck, probably in
Yucatan at Chicxulub
20Impact scenario
- Asteroid about 10 km (6 mi.) struck, probably in
Yucatan at Chicxulub - Immediate heat shock and wildfires near impact
site
21Impact scenario
- Asteroid about 10 km (6 mi.) struck, probably in
Yucatan at Chicxulub - Immediate heat shock and wildfires near impact
site - Particulates of gypsum (Ca2SO4) cause acid rain,
killing plankton
22Impact scenario
- Asteroid about 10 km (6 mi.) struck, probably in
Yucatan at Chicxulub - Immediate heat shock and wildfires near impact
site - Particulates of gypsum (Ca2SO4) cause acid rain,
killing plankton - Particulates create clouds, block sun, killing
plants
23Impact scenario
- Asteroid about 10 km (6 mi.) struck, probably in
Yucatan at Chicxulub - Immediate heat shock and wildfires near impact
site - Particulates of gypsum (Ca2SO4) cause acid rain,
killing plankton - Particulates create clouds, block sun, killing
plants - Temperature drops, killing organisms with no
tolerance for cold
24Evidence
25Evidence
- Crater at Chicxulub
- Iridium spike
Asteroids have higher iridium abundance than
Earths crust. Iridium of Earth is mostly in the
mantle and core.
26Evidence
- Crater at Chicxulub
- Iridium spike
- Shocked quartz
Two directions of lamellae typical of impacts
27Evidence
- Crater at Chicxulub
- Iridium spike
- Shocked quartz
- Tektites
Glass globules from melting of surface and
striking object
28Evidence
- Crater at Chicxulub
- Iridium spike
- Shocked quartz
- Tektites
- Soot
Carbon in boundary clay from wildfires
29Evidence
- Crater at Chicxulub
- Iridium spike
- Shocked quartz
- Tektites
- Soot
- C-13 indicates catastrophic extinction
30Biological effects predictions
- Who dies?
- Planktonic orgs.
- Ocean surface ecosystem
- Orgs. with poor thermoregulation
31Biological effects predictions
- Who dies?
- Planktonic orgs.
- Ocean surface ecosystem
- Orgs. with poor thermoregulation
- Who lives?
- Bottom dwellers who eat dead things
- Orgs. with dormancy capability
32Biological effects
- Who actually dies?
- Planktonic forams
- Marine reptiles
- Ammonites
- Dinosaurs
- Birds
- Non-flowering plants
- Marsupials
33Biological effects
- Who actually lives?
- Bottom communities clams, snails, crustaceans,
etc. - Placental mammals
- Angiosperms
- Amphibians
- Turtles
- Insects
34Volcanic hypothesis
- Huge volcanic eruption produces climatic change,
acid rain - Volcanoes bring up iridium
- BUT
- Problems demonstrating that the eruption is the
right age - Basaltic eruptions usually produce little ash, so
little climate change