C1.5 - History of Life and Modern Additions to Evolution

PART I: History of Life

The Early Earth

Illustration of early Earth

  • Characterized by extreme heat, high UV, radio and electrical activity
  • Primitive atmosphere contained nitrogen (N2), carbon dioxide (CO2), carbon monoxide (CO), ammonia (NH3), methane (CH3)
  • Asteroid impacts common
  • Surface gradually cools, water vapour condenses forming oceans

Miller-Urey Experiment

Diagram of Miller-Urey experiment

  • First life forms arose by primary abiogenesis theory
  • primary abiogenesis theory: theory where life arose from no life
  • Complex organic molecules form spontaneously
  • organic molecules: molecules that contain carbon
  • Miller-Urey experiment recreated early atmosphere
  • Sugars, amino acids, and nitrogenous bases created (building blocks of life)
  • Thermal proteinoids: protein-like molecules formed abiotically from amino acids

The Oldest Fossils

  • 400 my after Earth’s formation: Earth’s crust begins to cool and solidify
  • 3.5 bya: life on Earth confirmed
  • stromatolites: layered rocks that form when certain prokaryotes bind thin layers of sediment together
  • perhaps life in simpler forms began 3.9 bya

Protocells

Protocell

  • All living things composed of cells
  • Compartmentalization necessary
  • liposomes: lipid membrane
  • Lipid membranes form spontaneously
  • Membranes may act as semi-permeable barriers

Early Life

  • RNA world? No DNA?
  • Oldest fossils 3.5B yrs. old
  • Oldest life perhaps may have formed in deep sea hydrothermal vents
  • Cyanobacteria-like organisms (blue-green)
  • Anaerobic and chemoautotrophs
  • anaerobic: can break down glucose to energy w/o oxygen
  • chemoautotroph: makes own energy through chemical reactions
    • believed that oldest fossilzed prokaryotes evovled from them
  • Eukaryotic cells (complex cells w/ nucleus) arise through endosymbiosis
  • endosymbiosis: organism that lives within body/cells of another organism

Endosymbiotic Theory

  • eukaryotes: cells w/ membrane-bound organelles, nuclei, and complex organelles like mitochondria
  • Infolding of membrane formed endoplasmic reticulum and nucleus
  • heterotroph: organism that ingests organic carbon to produce energy
  • Consumption of heterotrophic cell formed mitochondria
  • Consumption of photosynthetic cell formed chloroplasts in plants

Formation of eukaryotes

The Cambrian Explosion

  • Multicellular organisms arise 750 mya
  • 565 mya: Animal kingdom undergoes dramatic increase in diversity
  • All major animal groups arise in Cambrian explosion
  • Early animals preserved in Burgess Shale

Cambrian Explosion illustration

Cambrian explosion illustration

Burgess Shale

Burgess Shale

Extinction Events

Geological time map
  • Geological time divided into 5 eras, subdivided into periods and epochs
  • mass extinction: brief episodes of great species loss
  • 5 major extinction events
  • 65 mya: Cretaceous extinction ends the age of dinosaurs and gives rise to mammals
    • meteor strike near land mass that became Yucatan Peninsula, Mexico
    • polluted sky w/ debris for months
    • dinosaurs thrived on Earth for 150 my
    • all dinos gone, except those that evolved into birds
  • end of Permian period
    • 90% of marine animals lost
  • pseudoextinction: the species never went extinct, they just evolved
  • positive side: adaptive radiation of survivors forming new biodiversity
  • 6th great extinction?

Fossil Record and Geologic Time Scale

  • geologic time scale: scale that organizes Earth’s geological history into distinct blocks of time
  • era: block of time
  • period: block formed by dividing era

Geologic time scale

Continental Drift

  • Earth’s continents move on plates floating on hot mantle
  • continental drift: movement of continents
    • N.A. and Europe currently drifting apart ~2 cm/yr.
  • solution to many biological puzzles
    • i.e. matching Mesozoic fossils in W. Africa and Brazil
    • same fossil in parts of world separated by 3,000 km of ocean?
    • evidence makes sense if part of one land mass during that time
    • explains why life on Australia is so diff. from rest of world

Formation and Breakup of Pangaea

  • 250 million years ago, continents formed one landmass called Pangaea (“all land”)
  • shorelines reduced, sea levels dropped, shallow seas drained
  • many marine habitats destroyed
  • inland areas became drier with extreme climates
  • species that evolved separately were forced to compete
  • led to mass extinctions
  • 180 million years ago, Pangaea began breaking apart
  • continents drifted and became isolated
  • species evolved separately on different land masses
  • marsupials survived in isolated Australia
  • placental mammals dominated other continents
  • explains Australia’s unique marsupial diversity
Breakup of Pangaea

Phylogeny

Please see Diversity of Life

Human Disruption — Bison Skull Hunting and Processing

Bisons hunted w/ rifles which are accurate and have fairly fast reloads

Bison skulls

PART II: Modern Additions to the Evolutionary Theory

Rate of Evolution

Rate of evolution morphology
  • gradualism: evolution of species by gradual accumulation of small genetic changes over a long period of time
    • asserts slow, gradual change
    • small changes accumulate in species over time
    • first developed by Charles Darwin
    • limitation: in fossil record, species would arise abruptly, persist in rock for thousands/mil. of years, then disappear suddenly
  • punctuated equilibrium: species often diverge in sudden bursts of rapid evolutionary change
    • developed in 1972 by paleontologists Niles Eldridge and Stephen Jay Gould
    • large changes occur rapidly followed by little change
    • term comes from idea that long periods of little evolutionary changes (equilibrium) are broken (punctuated) by shorter bursts of speciation

FUN FACT: Okapis and giraffes share the same evolutionary common ancestor

Gradualism vs. punctuated equilibrium

Divergent and Convergent Evolution

  • divergent evolution: evolution that creates species diverging in similarity
  • adaptive radiation: when one species gives rise to many distinct species
    • caused by small founding group colonzing new environment and adapting to its environment over generations
    • the new group changes and loses compatibility with original group
  • convergent evolution: distantly-related species develop similar adaptations, “analogous structures”
Adaptive radiation Convergent evolution

Co-Evolution and Mimicry

  • co-evolution: one species evolves in response to another species’ evolutionary changes
  • mutualism: when two species support each other in order to survive
    • i.e. flowers and insects have a mutual relationship w/ each other; insects get food and flowers get pollinated
  • Plants evolved toxins to prevent insects from eating them, but insects also evolved to resist these toxins to eat them again
    • i.e. milkweed plants produce toxins, but monarch caterpillar can handle toxins and store them so that they aren’t eaten
  • mimicry: one species evolves to represent another species to gain a survival advantage
    • i.e. hoverfly looks like a wasp, and predators avoid both to avoid a poisonous sting

Sources

  • Mr. C. Jones
  • BiologySource 11