Evolution Part 2

1. Evolution Part 2

2. Vocabulary Adaptive value– the value to the population of an adaptation Common Descent – organisms have a common ancestor

3. Struggle for existence – every organism struggles to survive, but only the fittest survive Genetic equilibrium – situation in which allele frequencies remain constant Reproductive isolation – organisms become unable to breed and produce fertile offspring

4. Speciation – a new species is formed Genetic Drift – random change in allele frequencies that occurs in small populations Disruptive selection – Form of natural selection where the 2 ends of the distribution curve are favored

5. Geographic isolation – form of reproductive isolation where 2 populations are separated physically Behavioral isolation – form of reproductive isolation in which 2 populations have differences in courtship rituals that prevents interbreeding

6. EVOLUTION Part 2 • Darwin and DNA Darwindid not know how heredityworked. Two factors he couldn’t explain: 1. Source of variation 2. how inheritable traitswere passedfrom one generation to the next

7. II Gene Pools Combined genetic information of allthe Membersof a particularpopulation. Two main sources of genetic variation: 1. Mutations-- change in sequence of DNA 2. Genetic shuffling – sexual reproduction (crossing-over)

8. III Genetic Drift In small populations, an allelebecomes moreor Lesscommon simply by chance.

9. IV When will evolution NOT occur? When there is genetic equilibrium – allele Frequenciesremainconstant. * if the allele frequenciesdo notchange, the population will notevolve.

10. Hardy-Weinburg principle FIVE conditions to maintain genetic equilibrium: 1. random mating 2. large population 3. no movement in or out of population 4. no mutations 5. no natural selection

11. ORIGIN OF LIFE *Current scientific view of events on early Earth Primitive Earth 1. Surface- sea of molten rock 2. Atmosphere- gases such as: hydrogen cyanide, carbon dioxide,carbon monoxide, nitrogen, hydrogen sulfide, water NO OXYGEN

12. 3. Earth cooled enough to form crust ; violent volcanic activity 4. More cooling caused thunderstorms which created oceans.

13. How could organic molecules have evolved under these conditions? Stanley Miller and Harold Urey simulated conditions on early Earth in the laboratory.

14. Filled flask with hydrogen , methane ,ammonia, and water. • Passed electric sparks through mixture of gases to simulate lightning • Over a few days, several amino acids began to accumulate (organic compounds)

15. Sidney Fox demonstrated iteractionsamong these organic molecules. These experiments joined Miller’s organic compounds into aggregates, similar in form to “ cell-like ” structures.

16. These first aggregates were called heterotrophs and were similar to prokaryotic bacteria and had the ability to reproduce. These discoveries created the heteotroph hypothesis.

17. Heterotrophs -- anaerobic respiration -- CO2 given off Autotrophs -- O2given off – aerobic respiration

18. Excessive oxygen in the atmosphere produced an ozone layer which gave protection from ultraviolet radiation. Some anaerobic species became extinct, while others adapted to the environmental change.

19. PATTERNS of EVOLUTION 1. Punctuated equilibrium • long, stable periods of no change interrupted by brief periods of more rapid change which produced many new species

21. 2. Gradualism evolution occurs gradually, slowly and continuously

23. Divergent Speciation