Midterm 2 Study Guide Flashcards
How has the movement of continents contributed to the distribution pattern of organisms?
- Movement of continents has been the most important factor in long term changes in organism distribution
- Movement along latitude bands= different land masses lying in different climatic regions
- Formation of mountain chains and volcanic islands
- *formation/ destruction of epeiric/ epicontinental seas
–> Acted as barriers to terrestrial organisms (land subdivided into smaller pieces)
–> Diverse marine life could thrive
Briefly outline the major changes in the positions of the continents over time.
- At first: 1 supercontinent called Rodinia (formed over a billion years ago)
- Early Cambrian: 3 fragments broke away from Rodinia
- During Carboniferous & Permian periods (Paleozoic era): consolidation of the ancient continents → formed mountain ranges
- Eventually, supercontinent Pangaea formed & the global Panthalassic Ocean
–> Supercontinent + global ocean= great connectivity - Mesozoic Era: Laurasian and Gondwanan continents separated (began as a rift valley & expansion of the Atlantic Sea
–> This separation led to opening of the circum-equatorial seaway - Early Cenozoic: chicxulub asteroid + mass extinctions
–> Continents continued to drift apart, sometimes colliding with once isolated landmasses
=rapid northward drifting of india→ eventually it hit Asia which resulted in the uplift of Himalayas
Neogene & Quaternary periods: continents continued drifting, most landmasses ended up north of the equator = climatic instability + glacial cycle in pleistocene
Explain how continental drift occurs.
Mechanism of continental drift= plate tectonics
- New sea floor created at mid-ocean ridges, where it moves outward by seafloor spreading & gets destroyed by subduction into ocean trenches
- Ocean floor= “conveyor belt” being continuously formed at mid-ocean ridges & then destroyed at trenches → continents passively ride along the conveyor belt
Provide evidence for the following events: first prokaryotic cells, increase in atmospheric oxygen, Cambrian explosion.
1st Prokaryotic Cells Evidence:
- Resemble modern photosynthetic algae?
- Stromatolites in limestone built by photosynthetic cyanobacteria
Increase in Atmospheric Oxygen Evidence:
- Deposition of iron oxide sediments on marine continental shelves
- Stromatolites in limestone built by photosynthetic cyanobacteria
- Extensive banded iron formations
Cambrian Explosion Evidence:
Burgess Shale! In Field, BC: very rich fossil record of the Cambrian Explosion
List the drivers of change (9).
Changing solar output
Evolving atmosphere
Tectonic/ volcanic activity
Asteroid impacts
Methane clathrate releases
Orbital patterns (Milankovitch cycles)
Changing ocean circulation
Changing sea levels
Humans!
Explain the three concepts of change.
- Predictable rules govern climate change and results in gradual change
Eg solar luminosity, continental drift, CO2/ O2 concentrations
- High CO2 associated with warmer conditions → found on multiple timescales (El Nino oscillations to geological timescales) - Random, abrupt, catastrophic events cause climate change
Eg asteroid impacts, volcanic eruptions, methane clathrate releases - The Climate alternates between alternate stable states
Eg glacial/ interglacial periods (ice-house vs hot-house)
- Called “metastable models”
Describe what life was like in the Phanerozoic eon.
Showed all 3 patterns of change (gradual, abrupt, periodic)
Both catastrophe and recovery
–> Mass extinctions and rebounds (adaptive radiation)
Diversity gradually increased during phanerozoic, but was punctuated by major extinctions
Explain the concept of extinction.
= the permanent loss of a species, population, etc
Often followed by adaptive radiation
Explain the cause behind many of the mass extinctions.
Tectonically-driven cycles of regression and transgression of marine waters across continental inland seas
- Regression → vast decreases in area of shallow water enviros
- Transgressions → brings masses of anoxic waters across expanses of shallow seas
- Each of these events could = mass extinctions (could have also been in conjunction with other factors like asteroids)
Describe the Permian-Triassic extinction event.
The most disastrous extinction ever!
Occurred 250 mya, and spanned 60,000 years
Massive scale and scope. Extinctions:
90%+ of marine invertebrates
75%+ of land tetrapods (mostly amphibians)
Majority of land plants
Explain the cause of the P-T extinction event.
There was likely more than one cause over the massive time span. Possibilities:
- Continental drift
- Ocean salinity changes
- Anoxic, acidic, and sulfidic oceanic conditions
- Possible meteorite impact
- Extensive volcanism, causing cooling
–> Sulfur dioxide from eruption goes into atmosphere, combines with water → forms sulfuric acid aerosols which reflect incoming solar radiation (cooling effect)
Describe the Cretaceous-Tertiary extinction event.
The mass extinction between the cretaceous and tertiary
~65 mya
Well-known because it caused the dinosaurs to go extinct
Explain the cause of the K-T extinction event.
Most likely cause= meteorite impact
Initial evidence= Italy: thin clay layer with very high iridium concentrations at the K-T boundary (later found around the world)
*Note Iridium suggests extraterrestrial origin
Additional evidence: Yucatan impact crater in Mexico (10km wide!)
What are the mechanisms for species formation (5)?
- Mutations (changes in DNA sequences) → substitution, insertion, deletion, or inversion of at least 1 nucleotide
- Genetic drift: occurrence of random changes in allele frequency b/w generations
- Natural Selection: change in a population b/c individuals express genetic traits that alter their interactions w/ their environment so that their survival & reproduction are enhanced relative to other individuals in the population
- Gene flow: movement of alleles within or between populations b/c of the dispersal of gametes or offspring
- Endosymbiosis: a symbiotic relationship where one organism lives inside the other
What is the difference between allopatric and sympatric speciation?
Allopatric:
Geographic isolation cuts off gene flow
Vicariance due to enviro barriers
Peripheral isolates due to founder events/ jump dispersal
Sympatric:
No geographic isolation
Includes sympatric and parapatric
Describe the two processes under which allopatric speciation occurs.
- Allopatric speciation due to vicariance
Each species arises from an isolation event (geographic barrier) → populations diverge into separate species (can happen again and again) - Allopatric speciation due to peripheral isolates and founder events
Random dispersal= new, geographically isolated populations that diverge into separate species (also can happen again and again- many levels)
What is the difference between sympatric and parapatric speciation?
- In sympatric, the populations are overlapping extensively and maintain contact throughout the speciation process
- In parapatric, there is only slight overlap in populations (narrow zone of contact b/w ancestral population and new population)