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1
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2
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- Life on earth began about 3.5 to 4.0 Billion years ago.
- Stromatolites
- Fossil prokaryotes - 3.4 billion years ago
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3
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4
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5
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6
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7
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- The earth's crust began to solidify about 4.1 billion years ago.
- by 3.5 billion years ago there were bacteria advanced enough to form
stomatolites
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8
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- therefore the early earth environment must have allowed life to arise
through spontaneous generation.
- CHEMICAL EVOLUTION HYPOTHESIS
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9
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- Abiotic synthesis of small organic molecules (monomers ie. amino acids,
simple sugars, nucleotides etc.)
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10
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- postulated that the reducing atmosphere (no O2) and high UV
radiation would enhance the reactions that could have produced organic
molecules.
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11
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12
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13
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14
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- The Urey-Miller experiments produced all 20 amino acids, ATP, some
sugars, lipids, and the purine and pyrimidine bases of RNA and DNA.
- These building blocks must have been joined into long chains or
“polymers”.
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15
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- Proteinoids - are abiotically synthesised polypeptides
- Sidney Fox
- amino acid polymers can be made by dripping amino acids (monomers) onto
hot sand, rock, or clay.
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16
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- Protobionts are aggregates of abiotically produced molecules able to
maintain an internal environment, and exhibit some life properties.
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17
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- Protobionts
- Liposomes - spheres made from phospholipids mixed with water (bilayers
like cell membranes)
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18
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19
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- selfreplication requires a genetic mechanism
- RNA may have been the first genetic molecule “Riboszymes”
- short polymers of RNA have been formed with zinc as a catalyst (no
enzymes)
- RNA is autocatalytic - RNA acts like an enzyme to make mRNA, tRNA, and
rRNA.
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20
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21
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- Panspermia - organic compounds may have reached earth in meteorites or
comets
- First organisms may have originated on the deep ocean floor - “Deep
Ocean Vent communities”
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22
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23
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24
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- Relative Dating
- Older sediments below , younger sediments on top
- Absolute Dating
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25
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26
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27
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28
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29
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30
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31
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32
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- Early prokaryotes evolved all of the common metabolic pathways seen
today.
- Photosynthesis and the “Oxygen Revolution”.
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33
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- Oldest eukaryote fossils are about 2.1 billion years old.
- Endosymbioyic origin of Mitochondria and Chloroplasts
- Genetic annealing
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34
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- The oldest multicellular fossils are found about 1.2 billion years ago.
- Larger organisms don’t appear until about 570 million years ago.
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35
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- First multicellular organisms were colonies.
- Some cells in the colony became specialized for specific functions.
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36
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- Most of the major animal phyla appeared suddenly in the fossil record
during the first 20 million years of the Cambrian period. (542 – 500
million years ago).
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37
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- The colonization of the land was one of the pivotal milestone in the
history of Life.
- Plants , fungi and animals colonized the land during the late Paleozoic
era, about 500 million years ago.
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38
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39
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40
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- “Heterochrony”
- Differential growth rates and timing of development
- Allometric growth
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41
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- Heterochrony in salamander foot growth
- Longer developmental time
- Shorter developmental time
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42
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- Sexually mature stage still retains some juvenile structures.
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43
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44
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- Homeotic genes control spatial organization of body parts
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45
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46
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47
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