Exam 3 Flashcards
(27 cards)
Describe the Ordovician extinction:
- Common theories for cause
- Life forms wiped out
- Characteristics of climate
- Characteristics of atmosphere
- How long ago, what % lost
- Caused by two pulses:
- First pulse due glaciation with associated CO2 levels dropping, likely due to silicate sequestering or plant colonization.
- Second pulse due to regression of glaciation.
- Life forms affected: invertebrates living in shallow seas; nautiloids, corals, graptolites, to name a few.
- Severely impacted trilobites (90+ %)
- Climate a warm greenhouse in beginning/majority.
- Extensive glaciation occured at end of period.
- Carbon levels were high during most part of period, and dropped during glaciation event, and rose again when glaciers receded.
- 450-440 Ma, ~75% species lost; second biggest extinction.
Describe the Devonian extinction:
- Common theories for cause
- Life forms wiped out
- Characteristics of climate
- Characteristics of atmosphere
- How long ago, what % lost
- Possibly caused by anoxia in ocean, global cooling, and rising sea levels;
- Promoted weathering of rock releasing nutrients into oceans causuing algal blooms decreasing O2 content
- Photosynthesis/ silicate sequestering absorbs CO2
- Largest impact on marine groups; armoured fish vanish completely
- Plants/ insects suffered little
- Shallow tropical oceans suffered, reefs ceased to exist.
- Climate warm, dry.
- Atmosphere high O2/ low CO2
- 375-360 Ma; ~70% of all species lost.
Describe the Permian extinction:
- Common theories for cause
- Life forms wiped out
- Characteristics of climate
- Characteristics of atmosphere
- How long ago, what % lost
- Volcanism (Siberian Traips) and platonic activity causing greenhouse affect, temperature increase, ozone layer destroyed, acid rain, dramatically increased temperatures
- Single worst extinction event (“The Great Dying”): 70% land species, 95% marine species lost.
- Climate was hot, dry (desert) in northern hemisphere/ cold in southern hemisphere with dramatic seasonal changes
- O2 levels dropped from high point, while CO2 levels increased
- 250 Ma; 95% of all species lost
Describe the Triassic extinction:
- Common theories for cause
- Life forms wiped out
- Characteristics of climate
- Characteristics of atmosphere
- How long ago, what % lost
- Maybe least understood cause: falling sea levels, extreme temperatures, due to volcanic rift forming betweeen America/ Africa & Europe (Central Atlantic Magmatic Province)
- Many dinosaur groups, reptiles, and amphibians disappeared
- Reef ecosystems and other invertebrates badly affected
- Climate was hot and dry, and received heavy rainfall on a seasonal basis.
- Greenhouse atmosphere caused by CAMP
- 200 Ma; 70-75% species lost
Describe the Cretaceous extinction:
- Common theories for cause
- Life forms wiped out
- Characteristics of climate
- Characteristics of atmosphere
- How long ago, what % lost
- Cause undecided; best idea is asteroid impact shooting dust/sulfer/CO2 into atmosphere blocking sunlight
- Or maybe incerased volcanism, or both?
- Sea levels dropped/ ocean acidification
- Increased temperatures
- Dinosaurs previously dominated land/oceans; large dinosaurs wiped out
- Small dinosaurs left behind, evolved into birds
- Climate was humid, high sea levels with many inland seas
- 66 Ma; 75% species
List the stable isotopes of oxygen - “sizes” and abundance
Oxygen-16: “light” 8 protons, 8 neutrons
Oxygen-18: “heavy” - 8 protons, 10 neutrons
Oxygen-16 most naturally abundant
Why is oxygen-18 important?
Ratios of oxygen-18 and oxygen-16 vary based on climate - can infer past climate based on ratios in sediments, ice cores, fossils.
High oxygen-18 concentratoins infer ice age b/c oxygen-16 is evaporated and deposited in ice sheets first - leaving behind oxygen-18.
Describe the Yougner Dryas event.
~12,900 years ago very cold period, due to…
Cold, fresh water concentrations from melting glaciers interrupts thermohaline conveyor:
- Slowing down movement of warm water
- Result in cooler temperatures, because temperatures all stay constant
Describe the Holocene Max
Warm period, due to… Milankovitch cycles
List some greenhouse gases
- Water vapor
- CO2
- Methane
- Nitrous oxide
- Ozone
Describe the greenhouse effect.
Greenhouse gases reflect heat (infrared photons/ long-wave) back onto surface, holding heat onto planet.
What is obliquity?
The tilt of the Earth’s axis; changes every 41,000 years.
What is precession?
Changes in direction of tilt of rotation axis; changes very 23,000 years
What is eccentricity?
Changes in shape of orbit due to magnetic attraction of planets; changes every 100,000 years
What is current state of Milankovitch cycle?
- Northern hemisphere pointed toward sun (~23.5 degrees)
- Southern hemisphere pointed away from sun
- Results in mild winters/ cool summers for northern hemisphere
- Cooler winters/ warm summers for southern hemisphere
How do tectonic plates form?
Cracks on Earth surface formed by cooling of Earth
These cracks form Earth’s tectonic plates
Why are tectonic plates moving?
Warm, semi-liquid layer moves the plates on top (“rafting”)
Describe ridge push.
Rising warm liquids creates pressure on crust (convection)
Applies pressure, and causes crust to rise (ridge)
Rising of crust causes tension, with slopes on either side
Cracks result
Magma injected into crust through cracks, can create magma chambers
Lava erupts through top of ridge, rolls down sides of slope
Solidifying magma adds weight to the system
Describe slab pull.
Denser/ older material will subduct underneath younger/ less dense material.
Describe pieces of evidence for support of Plate Tectonic Theory:
- Seafloor rock dating shows youngest rocks at ridges in middle of oceans, oldest rocks furthest away from ridges
- Similar fossil record found on different continents
- Magnetism (sea floor)
- Hot spots (Hawaii islands)
- Observation of actual movement via GPS
List 3 possible outcomes of plate interactions:
- Divergent plate boundaries have magma creating new crust (North Atlantic Ridge)
- Subduction boundaries have oceanic crust sinking underneath continental; or oceanic crust sinks under other oceanic crust (denser rock subducts)
- Transform boundaries have plates that just slide past one another
Describe the relationship between accretion and orogeny
- Accretion occurs when loose sediments are scraped onto plate above the plate subducting
- More accreted terrain results in more mountain building (orogeny)
- Entire “mountains” can be accreted onto plates as well
Describe how the earth and moon formed
- Earth:
- Material strike together growing Earth
- Iron melts and begins to sink
- Lighter materials concentrate closer to surface
- Layers evolve
- Moon:
- Mars-sized impactor strikes early Earth
- Blows off material that will collect to form moon
Describe the rock cyle:
- Igneous rock cools/forms
- Weathers to form regolith
- Erodes to form sediment
- Deposited to form loess, till, alluvium
- Buried to become strata
- Lithifies to become sedimentary rock
- Metamorphosesis to become metamorphic rock
- Melts to form magma
- Crystallizes to form igneous rock