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AP BIOLOGY THE HISTORY of EARTH CHAPTER 25 CAMPBELL and REECE

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Page 1: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

AP BIOLOGYTHE HISTORY of EARTH

CHAPTER 25CAMPBELL and REECE

Page 2: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Conditions on early Earth made the Origin of Life possibleMacroevolution : evolutionary change

above the species levelexamples:1. emergence of terrestrial vertebrates2. mass extinctions impact on diversity of

life3. origin of key adaptations like flight in

birds

Page 3: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Where did 1st cell come from?4 main stages could have produced very

simple cells:1. The abiotic synthesis of small organic

molecules2. Joining of these small molecules into

macromolecules (proteins, nucleic acids)3. Packaging of these macromolecules into

protocells, droplets with membranes that maintained internal chemistry different from their surroundings

4. Origin of self-replicating molecules that eventually made inheritance possible

Page 8: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Primordial SoupHaldane had hypothesized the early seas

site of 1st organic compounds 1st cellsMiller & Urey (Univ. of Chicago) in

1950’s Tested Oparin & Haldane ‘s premiseCreated a reducing atmosphereAdded compounds considered to have been

found existing on early earth (hydrogen gas – H2, ammonia – NH3, methane – CH4, and H2O vapor)

Page 9: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Miller & UreyExperiment: In 1953, Stanley Miller set up a closed system to

simulate conditions thought to have existed on early Earth1. Water mixture in “sea” flask was heated; vapor entered atmosphere

flask2. “Atmosphere” flask contained mix of hydrogen gas, methane, ammonia,

and water vapor (believed to mimic early Earth’s atmosphere)3. Sparks were discharged to mimic lightning 4. Condenser cooled the “atmosphere”, “raining” water and any

dissolved molecules down into sea flask5. As material cycled through apparatus, Miller periodically collected

samples for analysisResults: Miller identified variety of organic molecules common

in organisms (including simple molecules like formaldehyde (CH2O) and hydrogen cyanide (HCN) and more complex molecules (like amino acids and hydrocarbons)

Conclusion: Organic molecules (a 1st step in the origin of life) may have been synthesized abiotically on early Earth

Page 11: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Miller & Urey’s Results

Page 13: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Miller & Urey’s ResultsHave been repeated using same or

similar ingredients, different recipes for the atmosphere and they also produced organic compounds

Still ?s about amounts of methane, ammonia (was there really enough to make it a reducing environment?)

Some repeated experiment in non-reducing, non-oxidizing conditions & still produce organic compounds

Page 19: CHAPTER 25 CAMPBELL and REECE. Conditions on early Earth made the Origin of Life possible Macroevolution : evolutionary change above the species level

Vesicles as 1st step?When lipids & other organic molecules added

to water vesicles spontaneously formlipid bilayer (separation of hydrophilic & hydrophobic molecules)

These abiotically produced vesicles “reproduce” and grow on their own.

Clay, like from early Earth will be absorbed into the vesicles

some vesicles demonstrate semi-permeability