L14 - Mass Extinctions Flashcards
What is the background rate of extinction?
- This is calculated by using the fossil record to first count how many distinct species existed in a given time and place, and then to identify which ones went extinct
- From here, we back-calculate an extinction rate
What are the limitations of using the fossil record?
- Fossil record does not accurately represent past species diversity
- Fossil formation is not possible in all environments/habitats
- Shallow seas are the most conducive environment for fossil formation
- Soft-bodied organisms do not preserve well (jellyfish, worms)
- Fossils of land animals are scarcer than those of plants
- Hard to tell distinctions between species in the fossil record
- If we find only small fragments of the species…
What conditions are required for a fossil to form?
- Fossils can form through freezing, drying or encasement in tar or resin (rare)
- Most are formed when a plant or animal dies in a watery environment and is buried in mud and silt
Other issues with using the fossil record to estimate the background rate of extinction…?
- Chronospecies: a single species, changing morphologically, genetically, or ecologically over a long time scale
- Changes occur to such an extent that the original species, and its descendants, are identified as separate species
- Pseudoextinction: when a species is presumed to have gone extinct, but has instead become a different species
- Incomplete fossil record can lead us to believe a species has gone extinct, when it simply evolved into a different species over time.
Other issues with using the fossil record to estimate the background rate of extinction…?
- Extinction rates are generally measured at the taxonomic level of family (relative high)
- Not specific enough to differentiate between species
- Some families are bigger than others: one extinction of a family of 8 species is not as severe as one extinction of a family of 2 species =
What are biotic mechanisms of extinction?
- A species can be competitively excluded by a closely related species
- The organisms that a species feeds on may come up with an unbeatable defense
- A new predator may expand its territory
- A species can be wiped out by a disease
What are abiotic mechanisms of extinction?
- The niche or habitat the species occupied can no longer support the species due to…
- Temperature or climate fluctuations
- Extreme sea level changes
- Impact events (meteorites)
- Volcanism
What is a mass extinction?
- Extinction of a large number of unrelated species over a short period of geological time
- Background rates of extinction are substantially higher
- Extinctions are globally distributed
What are the five mass extinctions in history?
- Late Ordovician
- Late Devonian
- Late Permian
- Late Triassic
- Late Cretaceous
How do mass extinctions affect the evolution of life?
- Very rapid period of speciation among the few species that do survive
- More room for surviving species to spread out and so many niches in the environment that need to be filled
Late Ordovician ~ 440 MYA
- At this time, most complex multicellular organisms lived in the sea
- Almost all major taxonomic groups were affected during this extinction event
- Marine organisms suffered the most
- 49-60% of marine genera and nearly 85% of marine species were eliminated.
What were the causes of the late-Ordovician extinction?
- Global temperatures cooled and the sea levels fell
- Considering that much of the plant and animal diversity of the time had adapted to shallow warm waters, this was devastating
- Species could not survive in colder, deeper oceans and many died out
- Land moved to the south pole due to place tectonics
- Allowing for the formation of glaciers
- Removed water from oceans leading to rapid fall in sea levels
- Many shallow seas were drained completely
Late-Devonian (Age of the Fishes) Extinction ~ 375 MYA
- Land: been colonized by plants and insects
- Oceans: massive reefs built by corals
- Late-Devonian extinction lasted over 20 M years whereas most extinction last 100 000 to 5 M years
- Consisted of extinction pulses – no single cause has been identified
Theories behind the Devonian extinction
- During the Devonian, the Earth experienced super greenhouse climate conditions.
- Very warm and lots of CO2 in atmosphere
- As plants expanded onto land to form first forests, they depleted CO2 in the atmosphere (PHOTOSYNTHESIS)
- Rapid reduction in atmospheric CO2 that led to the earth cooling and the extinction of many organisms?
- Glacial deposits in northern Brazil (near the Devonian South Pole) suggests widespread glaciation at the end of the Devonian
Late-Permian Extinction ~ 250 MYA (Largest of all known mass extinctions)
- “The Great Dying”
- 70% of terrestrial vertebrates and 96% of marine species went extinct
- All life today is descended from the few survivors of The Great Dying