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Evolution Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

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Page 1: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Fossil Records Remains or traces of organisms

that lived in the past Usually found in sedimentary

rocks

Page 2: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Organism buried soon after death and the hard parts become fossilized

Fossils indicate a great deal about the actual structure of the organisms and their environment

Page 3: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Types of Fossils petrified bones imprints molds preserved in tar, amber, or ice

Page 4: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Dating of fossils Layering of fossils

Older fossils are found in the lower levels of sediment

Carbon-14 Dating Carbon-14 is a radioactive isotope in

all living organisms. It decays at a known rate Carbon-12 does not decay Compare ratio of C-12 to C-14 to

determine age

Page 5: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Contemporary changes DDT resistance in insects Antibiotic resistance in bacteria

Indirect Evidences Evidences of common ancestry Parts of the body with similar

(homologous) structures

Page 6: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Evolution

Indirect Evidences Similar patterns of inheritance Biochemical Similarities (protein and

DNA) Vestigial organs

Page 7: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

Lamarck’s Theory – 1809 “Inner need” to change Inheritance of acquired

characteristics (based on use and disuse)

Disproved

Page 8: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

Charles Darwin and Natural Selection - (1859) Naturalist on HMS Beagle Exploration of South America (3 ½ years) Visited the Galapagos Islands

Page 9: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

Natural Selection Living things increase in number

geometrically - (overproduction) There is no net increase in the

number of individuals over a long period of time

A “struggle for existence” exists since not all individuals can survive

Page 10: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

Natural Selection No two individuals are exactly alike

(variation) In the struggle for existence those

variations which are better adapted to their environment leave behind them proportionately more offspring than those less adapted - (Survival of the Fittest)

Page 11: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

A Modern Perspective Mutation

A sudden change in the genetic material (A source of variation)

Recombination of genes within a population Provides new combinations for natural

selection Shows how the percentage of genes in

a population can change

Page 12: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

The Methods of Change

A Modern Perspective Isolation

Separation of a population from others of the same kind

Natural Selection Certain traits give an adaptive

advantage to organisms and they leave more offspring

Page 13: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Species

A group of individuals that LOOK similar and are capable of producing FERTILE offspring in the natural environment.

Page 14: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Population

All of the members of the same SPECIES that live in particular AREA at the same TIME.

Page 15: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Variation in a population

Bell Curve The distribution of traits (Average is the

middle.)

Mode The number that occurs most often (High pt.)

Range The lowest number to the highest number

Page 16: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks
Page 17: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Gene Pool

The collection of GENES for all of the traits in a POPULATION

Page 18: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Hardy-Weinberg Principle

Genetic Equilibrium No CHANGE in the gene pool

Page 19: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Conditions that must exist for genetic equilibrium

1. No MUTATION 2. No MIGRATION3. Large POPULATION 4. Random MATING 5. No NATURAL SELECTION

Page 20: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Natural Selection

Four types of selection1. Stabilizing Selection2. Directional Selection3. Disruptive Selection4. Sexual Selection

Page 21: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Stabilizing Selection

Individuals with the AVERAGE form have the ADVANTAGE

Page 22: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks
Page 23: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Directional Selection

Individuals with one of the EXTREME forms have the ADVANTAGE

Page 24: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks
Page 25: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Disruptive Selection

Individuals with either of the EXTREME forms have the ADVANTAGE

Page 26: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks
Page 27: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Sexual Selection

Preferential choice of a MATE based on the presence of a specific trait

Page 28: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Speciation

The formation of new SPECIES

Page 29: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Isolation

Separation of a formerly successful BREEDING population

Page 30: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Geographic Isolation

Separated PHYSICALLY from each other

Page 31: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Reproductive Isolation

Can no longer produce FERTILE offspring

Page 32: Evolution  Fossil Records Remains or traces of organisms that lived in the past Usually found in sedimentary rocks

Extinction

When an entire SPECIES dies off.