Evolution of Life Chapter 13. Origin of Life Age of Planet Earth - 4.6 billion years Oldest fossils...

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Evolution of Life Chapter 13

Transcript of Evolution of Life Chapter 13. Origin of Life Age of Planet Earth - 4.6 billion years Oldest fossils...

Page 1: Evolution of Life Chapter 13. Origin of Life Age of Planet Earth - 4.6 billion years Oldest fossils - 3.5 billion years Possible Formation of the First.

Evolution of Life

Chapter 13

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Origin of Life

• Age of Planet Earth - 4.6 billion years

• Oldest fossils - 3.5 billion years

• Possible Formation of the First Cells– Inorganic molecules reacted to

form organic molecules– Organic molecules polymerized

to become macromolecules– Plasma membrane formed– Protocells formed

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Evidence of Evolution

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Evidence of Evolution

• Evolution– All the changes that have occurred in living

things since the beginning of life• Due to differential reproductive success

• 4 main areas of evidence that lead us to believe in “some” evolution:

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Evidence of Evolution

• Fossil Evidence

• Biogeographical evidence

• Anatomical evidence

• Biochemical evidence

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1. Fossil Evidence • Fossils

– The remains and traces of past life or any other direct evidence of past life

• Deposited in layers called strata– Each stratum is older than

the one above and younger than the one below

• Transitional fossils– Especially significant– Represent evolutionary

links

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Fossil Evidence - Geological Timescale

• Based on dating of fossil evidence– Relative Dating Method

• Determines the relative order of fossils and strata but not the actual date

– Absolute Method-• Radioactive dating techniques • Assign an actual date to a fossil• Technique based on the half-life of radioactive

isotopes

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Absolute Method

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Fossil Evidence - Mass Extinctions

• Large numbers of species become

extinct in a short period of time

– Remaining species may spread out

and fill habitats left vacant

• Five Major Extinctions have occurred

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2. Biogeographical Evidence

• Biogeography – Study of the distribution of species throughout the

world

• Earth has six biogeographical regions– Each has its own distinctive mix of species

• Barriers prevented evolving species from migrating to other regions

• Continental Drift-– The positions of continents and oceans has shifted

through time– The distribution of fossils and existing species allows

us to determine approximate timeline

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3. Anatomical Evidence• Common descent offers explanation

for anatomical similarities– Homologous Structures

• Same function and same basic structure, indicating a common ancestor

• Ex: human arm and whale forelimb

– Analogous Structures • Same basic function but different

origins• Ex: wing of bird and wing of an insect

– Vestigial Structures• Anatomical structures fully functional

in one group and reduced, nonfunctional in another

• Ex: Modern whales have a pelvic girdle and hind leg bones

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4. Biochemical Evidence

• All organisms use same basic biochemical molecules– DNA– ATP– Identical or nearly identical enzymes

• Many developmental genes are shared• Degree of similarity between DNA base

sequences and amino acid sequences indicates the degree of relatedness

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Process of Evolution

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Process of Evolution

• Occurs at the population level• Evolution – genetic changes within

population – more generations – phenotypic changes

• Microevolution - evolution on a small scale– Gene pool of a population

• All the alleles in all the individuals making up the population

– When the allele frequencies for a population change, microevolution has occurred

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Evolutionary Change

• Mutations

• Genetic drift

• Gene flow

• Nonrandom mating

• Natural selection

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1. Mutations

• Genetic changes that provide the materials for evolutionary change

• Can cause allele frequencies to change in a gene pool – microevolution to occur

• Has the ability to create new alleles in a population

• Happen randomly • Does not have an adverse effect on the

individual’s reproductive state

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2. Genetic Drift

• Changes in the allele frequencies of a gene pool due to chance

• Greater effects on smaller populations

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2. Genetic Drift

• Two main mechanisms– Founder Effect

• Few individuals found a colony

• Their collective genes represent only fraction of the original gene pool

– Bottleneck Effect: • Population is subjected to

near extinction by a disaster

• Only a few genotypes contribute to next generation

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3. Gene Flow

• Movement of alleles between populations

• Occurs when individuals migrate from one population to another

• Keeps gene pools similar

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4. Nonrandom Mating

• Occurs when individuals pair up according to phenotype or genotype

• Inbreeding is an example

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5. Natural Selection

• Natural Selection

– Process by which populations adapt to their environment

– Charles Darwin explained evolution through natural selection

– Why does this happen????

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Charles Darwin and The Origin of Species

• Charles Darwin’s On the Origin of Species by Means of Natural Selection– Published on November 24, 1859

• Argued that contemporary species arose from ancestors– Through a process of “descent with

modification,” with natural selection as the mechanism

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• Darwin made two main points in The Origin of Species:– Organisms inhabiting Earth today

descended from ancestral species– Natural selection was the mechanism

for descent with modification• Basic idea of natural selection is

that:– Organisms can change over

generations– Individuals with certain heritable

traits leave more offspring than others• The result of natural selection is

evolutionary adaptation

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Natural Selection• Evolution by natural selection requires the

following– Variation

• members of a population differ

– Inheritance• differences are inheritable

– Overproduction• populations produce more offspring than the environment

can support (struggle for existence)

– Differential Reproductive Success• better adapted individuals survive to reproduce more

offspring

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Natural Selection

• Fitness– Measured by the number of fertile

offspring produced by an individual

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Natural Selection

• Three Main Types of Natural Selection:

– Stabilizing Selection

– Directional Selection

– Disruptive Selection

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Natural Selection

• Stabilizing Selection

– Occurs when an

intermediate, or

average, phenotype is

favored

– Improves adaptation of

population to a stable

environment

– Extreme phenotypes

are selected against

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Stabilizing Selection

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Natural Selection

• Directional Selection

– One extreme phenotype is favored

– Distribution curve shifts in that

direction

– Can occur when population is

adjusting to a changing

environment

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Directional Selection

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Natural Selection

• Disruptive Selection

– Two or more extreme phenotypes are selected

– Two different habitats result in two different

phenotypes in a population

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Disruptive Selection

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Speciation

Chapter 14

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What is a species?

• biological species

• All individuals of 1 species can interbreed

• Offspring are fertileSterile zebra-horse cross: not a

new species

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Speciation

• Macroevolution

– observed best within the fossil record

• Speciation

– Splitting of one species into two or more

– the transformation of one species into a new species over time

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Hybrid Animals

• Breeding of two closely related but distinct species

• Human activities

• Unnatural conditions

• Usually sterile

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Reproductive Barriers between Species

• Prezygotic isolating mechanisms

• Postzygotic isolating mechanisms

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Reproductive isolating mechanisms

• Prezygotic isolating mechanisms– Habitat isolation

– Temporal isolation

– Behavioral isolation

– Mechanical isolation

– Gamete isolation

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Reproductive isolating mechanisms

• Postzygotic isolating mechanisms– Zygote mortality

– Hybrid sterility

– F2 fitness

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Process of Speciation

• Allopatric Speciation– Geographical barriers separate a

population into two groups

• Sympatric Speciation– Occurs without geographical barriers– Ex: Plants

• Self-reproduction can maintain a new species

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Pace of Speciation

• How FAST does evolution occur?

• 2 main mechanisms to explain:– Phyletic Gradualism– Punctuated Equilibrium

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Pace of Speciation• 1. Phyletic Gradualism

– Change is slow but steady before and after a divergence

– Proposes that speciation occurs after populations become isolated

• Reproductive isolation cannot be detected in fossils

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Pace of Speciation

• 2. Punctuated Equilibrium– Some think species appear

suddenly• Remain essentially unchanged

phenotypically until they undergo extinction

– Long periods of stasis followed by rapid speciation

• Occurs relatively rapidly

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Extinction…• Inevitable • Occurs all the time

– rates have not been steady

• Extinctions typically eliminate various species of organisms– followed by

explosive diversifications of organisms