EF

Bio- The Origin of Life, Universe, and Everything

The Big Bang Theory

  • about 13.8 billion years ago all energy and matter were at the same spot in the universe

  • it exploded

  • very small particles went flying away from the point of singularity

    • point of SINGULARITY because it only happened once

  • After the big boom

    • as universe cools atoms form

    • then clouds of atoms come together to form the first galaxies and stars

    • in these stars heavier elements were formed

      • including carbon, oxygen, nitrogen

      • things that stuff is made of

    • first generation of galaxies died and formed second set of galaxies including the milky way

  • 4.7 billion years ago the sun is formed

  • 4.5 billion years ago the earth formed

Early environment

  • water

    • shallow oceans

    • lots of rain

  • lots of energy

    • heat

    • lightning

    • UV

    • radiation

    • volcanoes

  • Gasses

    • nitrogen

    • carbon dioxide

    • hydrogen

    • carbon monoxide

    • methane

    • ammonia

    • no oxygen or ozone

  • contains things that can lead to the creation of life

Organic Molecules

  • Oparin, Haldane hypothesis

    • energy acting on the gasses in the early atmosphere resulted in the formation of organic molecules

  • Miller and Urey Experiment

    • simulated the atmosphere

    • found amino acids

    • repeated and found nucleic acids formed in the same way as amino acids

  • meteorites and comets contain organic matter

First Living molecules

  • probably RNA

    • simpler than DNA- simpler things come before complicated ones

    • self replicate

    • store info

    • direct synthesis of proteins

    • act as a catalyst

First cells

  • iron sulfide

    • columns contain spaces that can concentrate organic molecules

  • liposomes

    • fat bubbles can contain organic molecules

Oldest fossils

  • stromatolites

    • prokaryotic

    • lack a nucleus or other organelles

Early cells and energy

  • heterotroph hypothesis

  • first cells were heterotrophs- eating energy rich molecules in the early oceans

  • once they had eaten most of the food available autotrophs became abundant

  • Autotrophs produce oxygen

    • oxygen is reactive and toxic to many early organisms

    • organisms either became extinct or adapted with aerobic respiration

Eukaryotes

  • cells with nucleus and organelles

  • 1.4 billion years ago

Margulis

  • endosymbiont hypothesis

  • explains the formation of the nucleus and membrane bound organelles

  • mitochondria/chloroplast- once individual organisms that got engulfed in the membrane

    • one membrane from being a prokaryote

    • another from engulfment

  • first multicellular organisms


Speciation

Species

  • group of individuals that can breed with one another to produce fertile offspring in nature

  • evolution acts on species not individuals

Background

  • niche- ecological role of an organism

    • what it does and where it lives

    • no 2 species can occupy the same niche at the same time

  • Reproductive Isolation- part of the population is separated so that they can’t breed with the rest

    • leads to evolutionary change

Isolating mechanisms

  • morphological- things have to match

  • behavioral- mating rituals

  • geographic- change in geography

  • temporal- time

The Process- Darwin’s Finches

  1. founding fathers and mothers

  2. separation of populations

  3. changes in the gene pool

  4. reproductive isolation

  5. sharing the same space- ecological competition

Patterns of Evolution

  • divergent evolution- adaptive radiation

    • one original species fives rise to many diverse forms

    • Homologous structures- similar origin but a different appearance/function

  • Convergent evolution

    • evolution produces species that are similar in form or function

    • analogous structures- similar in appearance/function but a different origin

Rate of evolutionary change

  • gradualism- evolution occurring by a slow steady change

  • punctuated equilibria- long stable periods with short periods of fast change

    • often associated with mass extinction