L7 - Evolution and Early Diversification Flashcards

1
Q

Assessing descent… how do we compare phenotypic traits?

A
  • Observation and measurement suffice
  • Evaluate degrees of similarity and account for patterns of change in time to reconstruct relationships and lines of descent
  • Fossil sequences test inferred patterns of change
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2
Q

Problems with these techniques?

A
  • Environmental influence on phenotypes
  • Ontogenetic (development of an organism usually from the time of fertilization of the egg to adult) changes
  • Identifying “derived traits”
  • Insufficient data from living and fossil organisms to unambiguously trace changes in time
  • Lack of universal traits
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3
Q

What are the chances of finding a fossil?

A
  • Chance of dying in one piece
  • Chance of being fossilized
  • Chance of remaining undisturbed
  • Chance of being exposed
  • Chance of being found
  • Chance of being recognized
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4
Q

Advantages of comparisons involving molecular traits?

A
  • Nucleotide sequences provide a direct record of all information stored in the genome
  • Issues like plasticity or environmental influences that affect phenotypic trait, don’t affect the genetic record
  • If all of life came ultimately from one ancestor: potential for universal traits
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5
Q

Difficulties of comparisons involving molecular traits?

A
  • Difficulties in the use of sophisticated technology
  • Inferring patterns of change in time not intuitive
  • Back mutation at a site in the sequence is possible and COMPLICATES ANALYSIS
  • Assuming constant molecular clock: if you’re trying to relate the number of differences to an amount of time that has passed, you are making assumptions that may not be true
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6
Q

How do we reconstruct phylogeny (lines of descent)?

A
  1. Acquire nucleotide sequence data
    - Different portions of the genome relate to periods of time
  2. Align the mostly like pairings of those sequences sequences from different organisms
    - Allow for mismatches due to point mutations, insertions, and deletions
  3. Reconstruct most likely lines of descent
    - Assess the minimal number of steps required to change from one sequence to another and use this as a measure of relatedness across all the organisms in the analysis
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7
Q

Characteristics of Early Marine Plankton (single-cell)?

A

A diverse community of photosynthetic eukaryotes in marine waters.
- Why are there so many different physical structures of plankton? Which one is optimal?
- Interplay between abiotic-biotic and biotic-biotic
- Stochasticity: Depends on random chance
- Depends on your evolutionary history

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8
Q

What are “Acritarchs”?

A
  • A group of eukaryote fossils probably including algae, ciliates, dinoflagellates, radiolarians, foraminiferans
  • Many acritarchs had tests (shells)
    • An example of increasing structural complexity
    • Also made for a better source of fossil material
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9
Q

Why did diversity increase?

A
  • Changing environmental conditions
  • Changing biotic conditions
  • Interactions between these changes resulting in higher diversity
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10
Q

Processes involved in the increase of Eukaryote diversity?

A
  • Increase in size of genome: more proteins, and enzymes coded for, more opportunities for mutations to arise
  • Sexual reproduction: meiosis increases possible variation/mixing
  • Increase in structural complexity: locomotion (transport), protection
  • Ecological changes: great oxidation event, energy sources, physical/biological landscape, photosynthesis in shallow water.
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11
Q

How do we get from a diverse community of unicellular eukaryotes to multicellular organisms? Why?

A
  • Random chance?
  • Colonial hypothesis
    • Dividing cells do not separate after division
    • Mutation in cell membranes or walls?
  • Greater surface area for photosynthesis?
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12
Q

How do colonial photosynthetic protists work?

A
  • Protist: any eukaryotic organism that is not an animal, plant, or fungus
  • Colonial protists and algae illustrate the intermediate stage of complexity
  • Specialization of cells: colonial life allows evolution of separate functions for individual cells
    • Feeding, reproduction, locomotion…
    • Different metabolic pathways turned on and off
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13
Q

What are Ediacaran Fossils?

A
  • Cryptic soft-bodied organisms (570 MYA) found in Australia in 1946
  • Late Precambrian era
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14
Q

How to evaluate Ediacaran diversity?

A
  • Variety of forms: “Vendian animals”
    • leaflike fronds, round pads, worms
  • Some resemble jellyfish, sponges
  • Most are unique and unlike known animals
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15
Q

What does the Ediacran seascape look like ~ 570 MYA?

A
  • Small shelly fossils in ocean sediments
  • Soft parts not preserved - hard to tell if the soft Ediacarans were much less present at the time or if their fossils are just much less preserved
  • No idea what organism constructed the shells
    • What are the costs/advantages of shells and hard body parts?
      • Energy costs with producing more different and unique traits
      • More specific conditions required to produce said traits (climate, resources (Ca needed for shells), location)
      • New opportunities for locomotion and protection
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16
Q

What is the Burgess Shale Assemblage

A
  • A fossil (mid-Cambrian) marine community ~ 515 Ma
    • Yoho National Park, BC found in 1909
  • Fossils include ancestors of many modern groups (Arthropods, worms, jelly fish)
  • Also many mystery organisms…
    • Failed lines of evolution: offspring were not well adapted or simply victims of chance
17
Q

What is the “Pikaia”?

A
  • What is believed to be the predecessor of humans
    • Ancestor of chordates, and therefore the ancestor of vertebrates; mammals and humans
18
Q

What is the Cambrian Explosion ~ 570-540Ma?

A
  • Rapid onset of diversification in the animal kingdom
  • All modern animal body plans established
19
Q

How did the Cambrian explosion occur?

A
  • Biological factors in the Cambrian explosion
  • Interplay between different organisms
  • Increase in genetic complexity?
    • Enough DNA to code for a much greater range of structural and metabolic proteins
  • Increase in structural complexity?
    • More body parts for variation and selection to act on?
    • More structures that were adapted to multiple functions?
  • Change in the environment?
  • Change in ecological relationships?
20
Q

Explain the concept of “fitness landscape”.

A
  • “Roughening” the landscape
  • If organisms mutate a little bit: some will be better than others
    • High fitness = more likely to survive
    • Low fitness = less likely to survive
  • The species that survive will end up in specific geographic locations and diversity will increase = roughening
21
Q

Examples of ecological processes

A
  • Burrowing priapulid worms
    • Predators of small molluscs with spines
    • Swallowed prey all face the same way
    • Well developed feeding behaviour
22
Q

Predator-prey “arms race”

A
  • Predator-prey start to change one another over evolutionary time
  • However, this is not a result of “purposeful” responses to the other organism
  • But rather, the result of random chance (EVOLUTION DOESN’T HAVE A GOAL)
23
Q

What is the purpose of evolution?

A
  • none!!!
  • Variations arise through chance mutations
  • Some mutations are positive, some negative, many neutral
  • Selection, not the organisms, decides which variations will survive/success
  • Always interpret evolution in terms of chance variations, selection, probabilities of survival and not, purpose and progress towards an objective
24
Q

What is co-evolution?

A

Selection of favourable mutations in a biotic interaction between different organisms

25
Q

How do predator-prey interactions increase diversity?

A

Many possible variations at each step in the process

26
Q

What were the physical factors that occurred in the Cambrian explosion?

A
  • Much new diversity was apparently in shallow water marine environments
    • Increase in number and complexity of those habitats
    • Increase in availability of nutrients for metabolism and growth
    • Change in chemistry of environment
27
Q

Other considerable mechanisms for explosion?

A
  • Heating and melting, ending of most recent “Snowball Earth”
  • With melting, new elements become available and have complex changes and interactions
  • Tectonic activity
  • CO2 degassing rate
  • Increased photosynthesis
  • Increased pO2 by 50-75% during Ediacaran period/beginning of Cambrian
  • Enough to support energy requirements for larger predators