Biology Chapters 13-15
Galápagos Islands observations
The Galápagos Islands are volcanic, ~900 km off South America.
Darwin observed unique animals:
Blue-footed boobies
Giant tortoises (called galápagos in Spanish)
Marine iguanas
Many species of finches
Finches had different beak shapes, adapted to different foods:
Seeds
Cactus flowers
Insects
Some finches even eat parasites off tortoises.
These observations helped Darwin think about adaptation and evolution.
Early ideas about species
The ancient Greeks believed life could change over time.
Aristotle believed species were perfect and unchanging.
Judeo-Christian beliefs supported the idea that:
God created species
Earth was only ~6,000 years old
Fossils showed organisms different from living species → suggested a change over time.
Lamarck’s idea (early evolution theory)
Proposed that organisms change during life and pass traits to offspring.
Example: giraffes stretched necks → longer necks in offspring.
This idea is wrong (acquired traits are not inherited).
But Lamarck helped introduce the idea that species evolve.
Darwin’s voyage on the HMS Beagle
Born in 1809, loved nature.
Studied medicine → quit → studied to become clergy.
At age 22, I joined the HMS Beagle voyage (1831).
Collected plants, animals, and fossils around the world.
Noticed:
Fossils similar to living species in the same region
Different environments → different adaptations
Galápagos species similar to South American species
Influence of Charles Lyell
Lyell’s geology showed that Earth changes slowly over time.
Earth must be very old.
This helped Darwin realize evolution could take millions of years.
Darwin’s theory of evolution
Published On the Origin of Species (1859).
Proposed:
Species change over time
All species share ancestors
Called this descent with modification
Artificial selection
Humans breed organisms for traits.
Example:
Dog breeds
Crop plants
Shows big changes can happen over generations.
Natural selection
Key ideas:
Organisms produce more offspring than survive.
Individuals vary.
Some traits help survival.
Those with helpful traits reproduce more.
Result:
Helpful traits become common.
Populations change over time.
Important points:
Populations evolve, not individuals.
Only heritable traits evolve.
Evolution has no goal.
Adaptations depend on the environment.
Examples of natural selection
Finches in Galápagos:
Dry years → larger beaks survive
Wet years → smaller beaks survive
Insects & pesticides:
Some insects resistant
Survivors reproduce → resistance spreads
Natural selection:
Does not create traits
Selects traits already present
Fossil evidence
Fossils = remains of past organisms.
Types:
Bones/shells
Casts and molds
Footprints (trace fossils)
Preserved in amber, ice, and bogs
The fossil record shows:
Layers of rock = timeline
Older fossils deeper
Shows a gradual change over time
Examples:
Early humans (Homo erectus)
Whale evolution from land mammals
Mammals from reptile ancestors
Oldest fossils
~3.5 billion years old (prokaryotes)
Biogeography (location of species)
Species resemble nearby species.
Galápagos animals similar to those in South America.
Australia → marsupials evolved separately.
Conclusion:
Species evolved from local ancestors.
Comparative anatomy (body structures)
Homologous structures
Same structure, different function.
Example:
Human arm
Cat leg
Whale flipper
Bat wing
Shows common ancestor.
Embryology
Embryos of vertebrates share features:
Tails
Pharyngeal pouches
Shows shared ancestry.
Vestigial structures
Leftover parts from ancestors:
Whale pelvis bones
Blind cave fish eyes
Molecular evidence
DNA similarities show relationships.
Similar DNA → closer ancestor
Different DNA → distant ancestor
All life:
Uses DNA
Uses the same genetic code
→ Suggests all life has a common origin.
Evolutionary trees
Show relationships between species.
Branch point = common ancestor.
Example traits:
Tetrapod limbs
Amnion
Feathers
Trees are based on:
Fossils
Anatomy
DNA
Key ideas to remember
Evolution = change in populations over time
Natural selection = main mechanism
Evidence comes from:
Fossils
Anatomy
DNA
Geography
Observations of selection
All life shares a common ancestor
Evolution at the Population Level
Evolution Does NOT Happen to Individuals
Common misconception:
Individuals do not evolve during their lifetime.
Natural selection acts on individuals, but evolution occurs in populations.
Example:
Some insects survive pesticides because they carry resistant alleles.
Those insects reproduce more.
Over generations, the population becomes more resistant.
Populations and Gene Pools
Population
A population =
A group of individuals of the same species living in the same area that interbreed.
Characteristics:
Populations may be somewhat isolated.
Individuals usually mate with nearby members.
Members of the same population are genetically more similar.
Gene Pool
The gene pool =
All the genes and alleles in a population.
Example:
In an insect population:
One allele gives pesticide resistance
Another allele does not
If pesticides are used:
Resistant allele increases
Non-resistant allele decreases
Microevolution
Microevolution =
A change in allele frequencies in a population over generations.
Example:
Increase in pesticide-resistant insects.
Genetic Variation (Required for Evolution)
Evolution needs variation between individuals.
Example differences:
Appearance
Behavior
Physiology
DNA sequences
Example species with variation:
Lady beetles
Garter snakes
Phenotype vs Genotype
Phenotype
Observable traits
Influenced by genes AND environment
Genotype
Genetic makeup
Inherited
Important:
Only genetic variation can be passed to offspring.
Example:
Building muscle from exercise cannot be inherited.
Types of Genetic Traits
Polygenic Traits
Controlled by many genes.
Result:
Continuous variation.
Example:
Human height
Single-Gene Traits
Controlled by one gene.
Example:
Pea flower color
Human blood type
Sources of Genetic Variation
1. Mutation
Mutation = change in DNA sequence.
Important points:
Ultimate source of new alleles
Only mutations in gametes can be inherited
Most mutations:
Harmful or neutral
Rarely:
Beneficial (increase survival)
Example:
DDT-resistant flies
2. Gene Duplication
Sometimes genes are copied during meiosis.
Effects:
Extra gene copies accumulate mutations
Can evolve new functions
Example:
Mammals have many olfactory receptor genes for smell.
3. Sexual Reproduction
Major source of variation.
Three mechanisms:
Crossing Over
Chromosomes exchange genes during meiosis.
Independent Assortment
Chromosomes separate randomly into gametes.
Random Fertilization
Any sperm can fertilize any egg.
Result:
Every offspring has a unique combination of alleles.
Hardy–Weinberg Principle
Scientists use the Hardy–Weinberg principle to test if evolution is occurring.
Idea:
If no evolution occurs, allele frequencies stay constant.
This state is called the Hardy–Weinberg equilibrium.
Example (Blue-Footed Boobies)
Allele frequencies:
p = 0.8
q = 0.2
Genotypes:
WW = p² = 0.64
Ww = 2pq = 0.32
ww = q² = 0.04
If no evolutionary forces occur:
These frequencies stay the same each generation.
Conditions for Hardy–Weinberg Equilibrium
A population must meet 5 conditions:
Very large population
No migration (no individuals moving in/out)
No mutations
Random mating
No natural selection
Reality:
Real populations rarely meet all conditions
So evolution usually occurs.
Factors That Cause Evolution
If Hardy–Weinberg conditions are broken, evolution happens.
Main factors:
Small population size
Migration (gene flow)
Mutation
Nonrandom mating
Natural selection
Key Takeaways
Evolution occurs in populations, not individuals.
Evolution = change in allele frequencies.
Genetic variation comes from:
Mutations
Gene duplication
Sexual reproduction
Hardy–Weinberg equilibrium describes populations not evolving.
Breaking its conditions leads to microevolution.
Causes of Microevolution
Microevolution = change in allele frequencies in a population.
Hardy–Weinberg equilibrium stays constant only if 5 conditions are met.
If they are broken → evolution occurs.
Main causes of evolutionary change:
Natural selection
Genetic drift
Gene flow
Mutation and nonrandom mating matter, but usually less.
Mutation
Creates new alleles.
Happens randomly.
Rare in sexually reproducing organisms.
Alone → usually small effect on allele frequencies.
Nonrandom mating
Individuals choose mates based on traits.
Changes genotype frequencies.
Usually does NOT change allele frequencies by itself.
Natural Selection
Condition broken:
All individuals must reproduce equally (never true in nature).
Reality:
Individuals vary.
Some survive better.
Some reproduce more.
Example:
Webbed-foot birds swim better → survive more → allele increases.
Result:
Allele frequency changes.
Population evolves.
Natural selection leads to adaptive evolution
= better fit to the environment.
Genetic Drift
Genetic drift =
Random change in allele frequencies due to chance.
More likely when the population is small.
Example idea:
Flip a coin 10 times → uneven result possible.
Flip a coin 1000 times → closer to 50/50.
Same with genes:
Small populations change more by chance.
Effects:
Alleles can disappear.
Alleles can become common randomly.
Bottleneck Effect
Bottleneck = drastic population reduction.
Causes:
Fire
Flood
Earthquake
Hunting
Habitat loss
Result:
Survivors have different allele frequencies.
Less genetic variation.
Example:
Greater prairie chickens
The population dropped to <50
Lost 30% of alleles
Low egg hatch rate
Human-caused bottlenecks:
Florida panther
African cheetah
Even if the population grows again:
Variation stays low.
Founder Effect
Founder effect = a small group starts a new population.
Small group ≠ original gene pool.
Result:
Different allele frequencies.
Some traits become common.
Example:
Tristan da Cunha island
15 founders
One carried a blindness allele
Much higher frequency later.
Gene Flow
Gene flow = movement of alleles between populations.
Happens when:
Individuals move
Gametes move (pollen)
Effects:
Adds new alleles
Removes alleles
Makes populations more similar.
Example:
Prairie chickens
New birds added
Genetic diversity increased
Hatch rate improved.
Natural Selection = Chance + Sorting
Chance:
Mutation
Recombination
Sorting:
The environment favors some traits.
Only natural selection consistently produces:
Adaptive evolution
Relative Fitness
Fitness = reproductive success.
Not strength.
Not survival alone.
Fitness =
Number of offspring that survive and reproduce.
Traits that increase fitness:
Better camouflage
Better mating success
Better food gathering
Example:
Moths hidden from predators → more offspring.
Types of Natural Selection
Use the mouse fur color example.
Population starts with:
Light
Medium
Dark
Bell curve distribution.
1. Stabilizing Selection
Favors middle traits.
Removes extremes.
Result:
Less variation.
Example:
Human birth weight
Too small → risk
Too large → risk
Medium survives best.
2. Directional Selection
Favors one extreme.
Population shifts.
Example:
Dark fur better after fire
Larger beaks during drought
Pesticide resistance
Antibiotic resistance
Common when:
Environment changes
Species move to a new area.
3. Disruptive Selection
Favors both extremes.
Middle selected against.
Result:
Two phenotypes.
Example:
Finches:
Big beaks eat hard seeds
Small beaks eat soft seeds
Medium bad at both
Can lead to new species.
Sexual Selection
Sexual selection = traits that help get mates.
Not always good for survival.
Example:
Peacock tail
Bright feathers
Lion mane
Two types:
Intrasexual selection
Same sex compete.
Example:
Male vs male fights.
Intersexual selection
Mate choice.
Usually:
Females choose males.
Traits females prefer:
Bright color
Long call
Strong display
Good genes hypothesis:
Preferred traits show health.
Example:
Gray tree frogs
Long calls → healthier offspring.
Antibiotic Resistance
Example of directional selection.
Antibiotics kill most bacteria.
Some have mutations → survive.
Survivors reproduce.
Result:
Resistant bacteria spread.
Human causes:
Overuse of antibiotics
Using antibiotics for viruses
Not finishing medicine
Antibiotics in livestock
Example:
MRSA bacteria
Evolution makes treatment harder.
Why Variation Does NOT Disappear
Natural selection removes bad traits…
But variation stays.
Reasons:
Diploidy
Two alleles per gene.
Recessive alleles can hide in heterozygotes.
So, selection cannot remove them easily.
Balancing Selection
Keeps multiple alleles.
Heterozygote advantage
Heterozygotes survive best.
Example:
Sickle-cell allele
AA → malaria risk
SS → sickle-cell disease
AS → protected
Both alleles stay.
Frequency-dependent selection
A rare phenotype has an advantage.
Example:
Scale-eating fish
Left-mouth vs right-mouth
If one type is common:
Prey defend against it.
Rare type survives better.
Result:
Frequencies stay balanced.
Imperfect Organisms
Evolution does not make perfect organisms.
Reasons:
Works with existing traits
Limited by history
Environment changes
Trade-offs exist
Natural selection makes:
Better than before, not perfect.
Key Points
Evolution caused by:
Natural selection
Genetic drift
Gene flow
Small populations change faster.
Selection can be:
Stabilizing
Directional
Disruptive
Sexual selection affects mating traits.
Variation maintained by:
Diploidy
Balancing selection
Mutation
Evolution of Populations
Key Vocabulary
Population
A group of individuals of the same species living in the same area
Gene Pool
All the genes (alleles) in a population
What produces variation?
Mutations (random DNA changes)
Sexual reproduction (crossing over, independent assortment, fertilization)
Hardy-Weinberg Principle
Definition:
A population will NOT evolve if certain conditions are met
It’s a baseline to compare real populations to
Equation:
p² + 2pq + q² = 1
p = dominant allele frequency
q = recessive allele frequency
p + q = 1
Five Assumptions (SUPER IMPORTANT)
A population must have ALL of these to stay in equilibrium:
No mutations
Random mating
No natural selection
Extremely large population (no genetic drift)
No gene flow (no immigration/emigration)
If ANY of these are broken → evolution occurs
Mechanisms of Evolution
Natural Selection
Individuals with helpful traits survive & reproduce more
Genetic Drift
Random changes in allele frequencies (strong in small populations)
Gene Flow
Movement of genes between populations (migration)
Founder Effect
A small group starts a new population → less genetic diversity
Types of Natural Selection
Stabilizing Selection
Favors average traits
Reduces variation
Example: average birth weight
Directional Selection
Favors one extreme
Shifts population
Example: darker moths during pollution
Disruptive Selection
Favors both extremes
Can lead to speciation
Sexual Selection
Traits increase mating success (not survival)
Sexual Dimorphism
Males & females look different
Example: peacocks
Antibiotic Resistance
How it happens:
Some bacteria randomly have resistance
Antibiotics kill non-resistant bacteria
Resistant ones survive & reproduce
Why it’s a problem:
Infections become harder (or impossible) to treat
Balancing Selection
Keeps multiple alleles in a population
Frequency-Dependent Selection
Fitness depends on how common a trait is
Rare traits often have an advantage
Charles Darwin & Evolution
Charles Darwin
Traveled to the Galápagos Islands
Studied finches → noticed variation
Evolution
Change in allele frequencies over time
Fossils
Preserved remains of ancient organisms
On the Origin of Species
Introduced natural selection
Steps of Natural Selection
Variation exists
Overproduction of offspring
Competition
Survival of the fittest
Traits passed on
Natural vs Artificial Selection
Natural Selection
The environment selects traits
Artificial Selection
Humans select traits
Example: dog breeding
Evidence of Evolution
Fossils
Show changes over time
Biogeography
Species distribution (islands = unique species)
Comparative Anatomy
Homologous structures → common ancestry
Molecular Biology
DNA similarities
Evolutionary Trees
Show relationships between species
Observing Evolution Today
Antibiotic-resistant bacteria
Pesticide-resistant insects
Changes in finch beaks
Quick Summary
Evolution = change in allele frequencies
Variation is required
Hardy-Weinberg = “no evolution” model
Natural selection is NOT random (but mutations are)
Multiple types of selection shape populations
Species & Speciation
Defining Species
Biological Species Concept
Species = organisms that can interbreed and produce fertile offspring
Other Concepts
Morphological: based on physical traits
Ecological: based on niche
Phylogenetic: based on evolutionary history
Speciation
Formation of new species
Hybrids
Offspring of two species
Often:
Infertile (ex, mule)
Less viable
Reproductive Isolation
Prezygotic Barriers (before fertilization)
Habitat Isolation (different locations)
Temporal Isolation (different times)
Behavioral Isolation (different mating behaviors)
Mechanical Isolation (incompatible structures)
Gametic Isolation (sperm/egg can’t fuse)
Postzygotic Barriers (after fertilization)
Reduced viability (offspring weak)
Reduced fertility (offspring sterile)
Hybrid breakdown (offspring weak over generations)
Types of Speciation
Allopatric Speciation
Geographic separation
Sympatric Speciation
Same area, but reproductive isolation
Polyploidy
Extra chromosome sets (common in plants)
Can instantly create new species
Adaptive Radiation (again)
One species → many quickly
Key to biodiversity
Hybrid Zones
Regions where different species interbreed
Punctuated Equilibria
Evolution happens in quick bursts
Followed by long periods of little change
Darwin & Early Ideas of Evolution
Charles Darwin studied the Galápagos Islands
Noticed:
Islands were geologically young
Full of unique species (ex, flightless cormorant)
Realization:
Species are new and changing over time
Called the origin of new species the “mystery of mysteries.”
Microevolution vs. Speciation
Microevolution
Small changes in a population’s gene pool over generations
Leads to adaptation
Speciation
Formation of new species
Increases biodiversity
Without speciation, Earth would only have one evolving species, not millions
Big Picture of Evolution
Life started ~3.5 billion years ago
One ancestral species → split → more splits → millions of species
Explains:
Unity of life → shared ancestry
Diversity of life → branching evolution
What is a Species?
Hard to define because:
Some species look very different but are the same (humans)
Some look similar but are different (meadowlarks)
Biological Species Concept
A species = organisms that:
Can interbreed in nature
Produce fertile offspring
Key idea: reproductive compatibility
Reproductive Isolation
Prevents gene flow between species
Hybrids
Offspring of two species
Example:
Grizzly bear + polar bear → “grolar bear”
Often:
Rare
Less fit or sterile
Limits of the Biological Species Concept
Doesn’t work well for:
Fossils (can’t test breeding)
Asexual organisms (no mating)
Other Species Concepts
1. Morphological Species Concept
Based on physical traits
Pros:
Works for fossils & asexual species
Cons:
Subjective
2. Ecological Species Concept
Based on the ecological niche (role in the environment)
Example:
Same-looking fish but different diets/habitats
3. Phylogenetic Species Concept
Based on evolutionary history
Species = the smallest group with a common ancestor
Reproductive Barriers
Two types:
Prezygotic Barriers (BEFORE fertilization)
Prevent mating or fertilization
Types:
Habitat isolation
Same area, different habitats
Temporal isolation
Breed at different times
Behavioral isolation
Different mating behaviors/signals
Mechanical isolation
Body parts don’t fit
Gametic isolation
Sperm & egg can’t fuse
Postzygotic Barriers (AFTER fertilization)
Hybrids form, but have problems
Types:
Reduced hybrid viability
Offspring don’t survive
Reduced hybrid fertility
Offspring sterile (ex, mule)
Hybrid breakdown
Next generation weak or sterile
Key Takeaways
Evolution = change + branching
Speciation = source of biodiversity
Species are defined mainly by their ability to reproduce
Reproductive isolation keeps species separate
Multiple definitions exist because nature is messy and complex
How New Species Form (Speciation Basics)
Speciation often begins with population separation
Once isolated:
Gene pools evolve independently
No gene flow between populations
Changes happen via:
Natural selection
Genetic drift
Mutation
Allopatric Speciation (Geographic Separation)
Definition: New species form due to physical barriers
Barrier examples:
Mountains
Rivers/canyons (ex, Grand Canyon squirrels)
Oceans/continents splitting
Key idea:
Isolation → different environments → different adaptations → reproductive barriers
Evidence for Allopatric Speciation
Snapping shrimp split by the Isthmus of Panama
Closely related pairs on opposite sides
Shows:
Geographic separation → speciation
How Isolation Leads to New Species
Different environments cause:
Different food sources
Different predators
Different pollinators
Leads to:
Trait changes
Eventually reproductive barriers
Lab Evidence (Diane Dodd Experiment)
Flies raised on:
Starch vs. maltose
Result:
Preferred mating with the same diet group
Shows:
Prezygotic barrier forming
Speciation can begin quickly
Pollinator Isolation Example
Monkey flowers:
Pink → bees
Red → hummingbirds
Changing flower color → changed pollinators
Result:
Reproductive isolation
Sympatric Speciation (Same Location)
New species form without geographic separation
Happens through:
Polyploidy
Habitat differentiation
Sexual selection
Polyploidy (Common in Plants)
Organisms have extra chromosome sets
Key outcomes:
Tetraploid (4n) can form from diploid (2n)
Cannot reproduce with parent species → instant speciation
Hybrid Polyploidy:
Two species hybridize → sterile
Chromosomes double → fertile new species
Sympatric Speciation in Animals
Less common
Happens via:
Different habitats
Mate preferences
Example:
African cichlid fish
Different diets
Female choice based on color
Polyploidy in Agriculture
Many crops are polyploid:
Wheat
Bananas
Potatoes
Cotton
Example:
Bread wheat evolved through hybridization + chromosome doubling
Adaptive Radiation
One species → many species adapted to different niches
Happens in:
Isolated areas (like islands)
Darwin’s Finches (Classic Example)
Charles Darwin studied them in the Galápagos
14 species evolved from one ancestor
Differences:
Beak size/shape
Diet
Habitat
Real-Time Evolution (Grants Study)
Studied finches for decades
Found:
Drought → larger beaks survive
Competition → smaller beaks favored
Shows:
Evolution can happen quickly
Hybrid Zones
Areas where species meet and interbreed
Possible outcomes:
1. Reinforcement
Hybrids are weak → selection favors stronger reproductive barriers
Example:
Flycatcher birds evolve more distinct appearances
2. Fusion
Barriers are weak → species merge back into one
Example:
Cichlid fish (due to pollution affecting mate choice)
3. Stability
Hybrids continue, but species remain distinct
Example:
Some finch populations
Patterns in the Fossil Record
1. Punctuated Equilibrium
Long periods of little change
Short bursts of rapid speciation
2. Gradualism
Slow, steady evolution over time
Time Scale of Speciation
Can take:
4,000 to 40 million years
Average: ~6.5 million years
Big Picture Takeaways
Speciation often starts with isolation
Can happen:
With barriers (allopatric)
Without barriers (sympatric)
Evolution is:
Sometimes fast
Usually very slow
Leads to:
Biodiversity + major evolutionary changes
Evolution & History of Life
Abiotic Synthesis of Organic Molecules
Early Earth conditions allowed organic molecules to form from inorganic substances.
Supported by the Miller-Urey Experiment
Key idea: life’s building blocks can form naturally without life already existing
Macroevolution
Large-scale evolutionary changes over long time periods
Includes:
Origin of new species
Mass extinctions
Evolution of major groups
Major Events in the History of Life
First Cells
~3.5 billion years ago
Prokaryotic (simple, no nucleus)
Oxygen Revolution
Photosynthetic bacteria released oxygen
Led to the extinction of anaerobic organisms + new life forms
Colonization of Land
Plants first (~500 mya), then animals
Required adaptations like:
Preventing water loss
Structural support
Radiometric Dating
Uses radioactive decay to determine the age of fossils/rocks
Based on the half-life of isotopes
Geologic Record
The fossil record shows life’s history in rock layers
Older layers = deeper
Geologic Time Scale (Know Order)
Eons → Eras (focus here):
Precambrian
Paleozoic
Mesozoic
Cenozoic
Plate Tectonics & Continental Movement
Plate Tectonics
Earth’s crust is divided into moving plates
Continental Drift
Continents move over time
Pangaea
All continents were once joined together
Broke apart → modern continents
Mass Extinctions
Sudden loss of many species
Example: Cretaceous–Paleogene extinction event
Often followed by adaptive radiation
Adaptive Radiation
Rapid evolution of many species from a common ancestor
Happens after:
Mass extinctions
New environments
Phylogeny & Tree of Life
Phylogeny
Evolutionary history of a species/group
Represented with phylogenetic trees
Convergent Evolution
Unrelated species evolve similar traits
Due to similar environments (NOT common ancestry)
Taxonomy
Naming and classifying organisms
Hierarchy (DKPCOFGS)
Domain
Kingdom
Phylum
Class
Order
Family
Genus
Species
Clades
A group of organisms with a common ancestor
Includes all descendants
Traits
Shared ancestral character = trait from a distant ancestor
Shared derived character = trait unique to a group
Cladograms (How to Build)
Use shared derived traits
Steps:
List organisms
Identify traits
Arrange from least → most derived
Closer branches = more closely related
Origin of the Universe & Earth
Universe Basics
Earth is one of 8 planets orbiting the Sun
The Sun is one of billions of stars in the Milky Way galaxy
The Milky Way is one of the trillions of galaxies in the universe
Closest star to the Sun: ~40 trillion km away
Big Bang Theory
The universe began 12–14 billion years ago
All matter was once condensed into one mass
A massive explosion (Big Bang) caused the expansion
The universe has been expanding ever since
Formation of Earth
Earth formed ~4.6 billion years ago
Originated from a swirling cloud of dust and gas
Particles collided and stuck together → formed larger bodies
Gravity pulled in more material → formed planets
Early Earth Conditions
Very hot and molten due to:
Meteor impacts
Gravitational compression
Earth is separated into layers by density
Dense materials → core
Lighter materials → crust
Early Atmosphere & Oceans
Early atmosphere contained:
Water vapor
Carbon dioxide
Nitrogen
Methane
Ammonia
Hydrogen
Hydrogen sulfide
No oxygen (O₂) initially
As Earth cooled:
Water vapor condensed → oceans formed
Environment Differences
Much more:
Lightning
Volcanic activity
UV radiation
When Did Life Begin?
Oldest fossils: ~3.5 billion years old
Example: stromatolites
Layered rocks formed by photosynthetic prokaryotes
Life may have started even earlier (~3.9 billion years ago)
Spontaneous Generation vs. Reality
Old belief: life comes from nonliving matter
Disproved by Louis Pasteur (1862)
Life comes from preexisting life
How Did Life Arise? (4 Stages Overview)
Scientists propose life formed through:
Abiotic synthesis of organic molecules
Formation of polymers (chains of molecules)
Formation of protocells (membrane-bound structures)
Self-replicating molecules (RNA)
Stage 1: Abiotic Synthesis (Miller-Urey Experiment)
Key Scientists
Stanley Miller (1953)
Based on ideas from:
A. I. Oparin
J. B. S. Haldane
Experiment Setup
Simulated early Earth with:
Water vapor
Hydrogen gas
Methane
Ammonia
Added electric sparks (lightning)
Results
Produced:
Amino acids
Organic molecules (building blocks of life)
Key Idea
Organic molecules can form without life
Other Sources of Organic Molecules
Volcanic environments
Hydrothermal vents (deep ocean)
Meteorites
Example: meteorite (1969, Australia)
Contained:
Amino acids
Lipids
Sugars
Nitrogen bases
Stage 2: Formation of Polymers
Monomers (small molecules) → polymers (chains)
Can happen without enzymes:
Heat + concentration → bonding
Possible early Earth scenario:
Waves splash molecules onto hot rocks
Chains form → washed back into the ocean
Stage 3: Protocells
Lipids in water → form vesicles (membrane bubbles)
Properties:
Can grow and divide
Create an internal environment
Clay may have helped:
Concentrates molecules
Speeds up reactions
Stage 4: Self-Replicating RNA (RNA World)
Key Idea
RNA may have been:
Genetic material
Catalyst (like enzymes)
Evidence
RNA can:
Self-assemble
Copy itself (with errors → mutations)
Some RNA acts as enzymes → called ribozymes
“RNA World” Hypothesis
Early life used RNA for:
Information storage
Chemical reactions
From RNA to DNA
Over time:
DNA replaced RNA as genetic storage (more stable)
Protocells evolved into true cells
Natural selection began shaping life
Big Picture Summary
Universe formed → Earth formed → conditions allowed chemistry
Simple molecules → complex molecules → protocells → RNA
RNA → DNA → first true cells → evolution of life
Macroevolution Overview
Macroevolution = large-scale patterns of evolutionary change over long time periods
Studies the history of life on Earth from origin → present
Geologic Time Scale
Eons of Earth’s History
Archaean + Proterozoic
Together = ~4 billion years
Early life forms develop
Phanerozoic
Last ~500 million years
Most visible life (plants, animals)
Origin of Prokaryotes
Oldest fossils (~3.5 billion years): stromatolites
Early life = prokaryotes only for ~1.5 billion years
Oxygen Revolution
Photosynthetic prokaryotes released oxygen (O₂)
Timeline:
~2.7 billion years ago → O₂ appears in atmosphere
~2.2 billion years ago → rapid increase (oxygen revolution)
Effects
Many anaerobic organisms → extinct
Some survived in oxygen-free environments
Others evolved cellular respiration → used O₂ for energy
Origin of Eukaryotes
First eukaryotic fossils: ~2.1 billion years ago
Formed by endosymbiosis:
Smaller prokaryotes lived inside larger cells
Key Developments
Diversity of single-celled eukaryotes
Multicellular ancestors: ~1.5 billion years ago
First multicellular fossils: ~1.2 billion years ago (algae)
Cambrian Explosion
Occurred ~535–525 million years ago
Rapid increase in animal diversity
Many major animal groups appear
Colonization of Land
Early life on land:
Photosynthetic prokaryotes (>1 billion years ago)
Major Land Colonization (~500 million years ago)
Plants + fungi moved onto land together (mutualism)
Animals followed:
Arthropods (insects, spiders)
Tetrapods (4-limbed vertebrates)
Humans
Human lineage split: 6–7 million years ago
Modern humans: ~195,000 years ago
On a 1-hour Earth timeline → humans appear in the last 0.2 seconds
Dating Fossils (Radiometric Dating)
Key Idea
Based on the decay of radioactive isotopes
Important Terms
Half-life = time for 50% of the isotope to decay
Example: Carbon-14
Half-life: 5,730 years
Used for fossils up to ~75,000 years old
Other Isotopes
Potassium-40
Half-life: 1.3 billion years
Used for very old rocks
Relative Dating
Fossil age estimated using:
Rock layers above and below
Fossil Record
Fossil record = sequence of fossils in rock layers
Shows evolutionary history over time
Helps build the geologic record
Eras of the Phanerozoic Eon
1. Paleozoic Era (“ancient life”)
Life was mostly aquatic at first
By ~400 million years ago:
Plants & animals established on land
2. Mesozoic Era (“middle life”)
Age of reptiles (dinosaurs)
First:
Mammals
Flowering plants
Ends with mass extinction
Dinosaurs die out (except birds)
3. Cenozoic Era (“recent life”)
Begins ~65 million years ago
Rapid evolution of:
Mammals
Birds
Insects
Flowering plants
Includes modern life forms
Mass Extinctions
Mark boundaries between eras
Many species disappear → survivors diversify
Smaller extinctions mark period boundaries
Big Picture Summary
Life started simple → prokaryotes → eukaryotes → multicellular life
Oxygen changed Earth dramatically
Life moved from water → land
Major events (like extinctions) reshaped evolution
Humans are a very recent addition
Factors Shaping Macroevolution
The fossil record shows major evolutionary changes, influenced by:
Plate tectonics
Mass extinctions
Adaptive radiations
Plate Tectonics & Continental Drift
Structure of Earth
Crust = outer layer (tectonic plates)
Mantle = hot, flowing layer beneath
Core:
Outer = liquid
Inner = solid
Plate Tectonics
Earth’s crust is broken into moving plates
Plates “float” on the mantle
Types of Plate Movement
Move apart → new crust forms
Slide past → earthquakes
Collide → mountains + volcanoes
Continental Drift
Continents slowly move over time
Example: North America & Europe → ~2 cm/year apart
Supercontinents
Continents have merged 3 times into supercontinents
Most recent: Pangaea (~250 million years ago)
Effects of Pangaea
Lower sea levels → loss of shallow marine habitats
The interior became cold & dry
Many species went extinct
Survivors adapted → new opportunities
Breakup of Pangaea
Split into:
Laurasia (north)
Gondwana (south)
Continents became isolated
→ organisms evolved separately
Example Effects
Australia → isolated → marsupials dominate
India colliding with Asia → formed the Himalayas (still growing)
Biogeography Evidence
Marsupials
Originated in Asia → spread → isolated in Australia
Evolved to fill many ecological roles
Lungfish
Fossils found worldwide → existed before continents split
Now only in:
Africa
South America
Australia
Plate Movement Dangers
Earthquakes
Caused by plates sticking → sudden release
Example:
1906 San Francisco
1989 Loma Prieta
2010 Haiti
Tsunamis
Caused by underwater earthquakes
Example: 2004 Indian Ocean tsunami
Volcanoes
Release:
Lava
Ash
Gases
Can cause local & global damage
Example: Mt. Vesuvius (Pompeii)
Extinction
Causes
Habitat destruction
Climate change
New predators/competition
Most species that have ever lived are now extinct
Mass Extinctions
5 major events in the last 500 million years
Each wiped out ≥50% of species
Major Examples
1. Permian Extinction (~251 MYA)
~96% of marine life died
Possible causes:
Massive volcanic eruptions
Global warming (~6°C increase)
Ocean oxygen loss
Toxic gases
2. Cretaceous Extinction (~65 MYA)
Killed:
Dinosaurs (except birds)
Many marine species
Evidence
Iridium layer (from asteroid)
Chicxulub crater (Mexico)
Effects
A dust cloud blocked the sunlight
Climate collapse
Massive die-off
After Mass Extinctions
Recovery
Takes 5–10 million years (or longer)
Example: Permian recovery → ~100 million years
Key Idea
Extinctions are random
Can remove even successful species
Possible 6th Mass Extinction
Caused by human activity:
Habitat destruction
Climate change
Extinction rate:
100–1000× normal
Not yet as severe as past events—but rising
Adaptive Radiation
Definition
Rapid evolution of many species from a common ancestor
When It Happens
After:
Mass extinctions
New habitats
New adaptations
Example
Mammals after dinosaur extinction:
Became larger
More diverse
Filled empty niches
Evo-Devo (Evolution + Development)
Studies how genes control body form
Small genetic changes → big physical differences
Changes in Timing (Heterochrony)
Example: Axolotl
Adults keep juvenile traits (gills)
Humans vs. Chimps
Humans:
Slower jaw growth
Larger brain
More “childlike” skull
Changes in Spatial Pattern
Homeotic Genes
Control body structure (e.g., limbs)
Example: Snakes
Lost limbs due to gene expression changes
Gene Changes
Gene Duplication
Extra gene copies → new functions
Helped evolve:
Backbone
Jaws
Limbs
Gene Regulation
Changes in when/where genes turn on
Example: Stickleback Fish
Ocean fish → spines present
Lake fish → spines absent
Same gene, different expression
Evolution of Complex Structures
Gradual Refinement
Complex traits evolve step-by-step
Example: Eyes
Simple light-sensitive cells → complex eyes
Each stage had a function
Exaptations
Definition
Trait evolves for one purpose → used for another
Example: Feathers
Originally:
Insulation/display
Later:
Flight
Other Example
Penguin wings → used for swimming
Evolutionary Trends (Horses)
Early horses:
Small
Multiple toes
Modern horses:
Large
One toe
Grazing teeth
Important Idea
Evolution is branching, not linear
No “goal” in evolution
Species Selection
Species that:
Survive longer
Produce more new species
→ shape long-term trends
Big Picture Summary
Earth’s movement reshapes habitats → drives evolution
Mass extinctions reset life → open niches
Adaptive radiation fills those niches
Small genetic changes → major differences
Evolution is:
Not goal-directed
Driven by environment + chance
Phylogeny & Classification
Phylogeny
Phylogeny = evolutionary history of a species or group
Based on:
Fossil record
Morphology (structure)
Molecular data (DNA)
Fossil Record Limits
Incomplete because:
Not all organisms fossilize
Fossils can be destroyed
Many haven’t been discovered
Homology vs. Analogy
Homologous Structures
Similar due to common ancestry
May have different functions
Example:
Whale flipper vs. bat wing → same bone structure
Analogous Structures
Similar due to convergent evolution
NOT from the common ancestor
Example:
Australian mole (marsupial) vs. North American mole (placental)
Convergent Evolution
Unrelated species evolve similar traits
Caused by:
Similar environments
Similar selective pressures
Systematics & Taxonomy
Systematics
Study of:
Classification
Evolutionary relationships
Taxonomy (developed by Carolus Linnaeus)
Naming & classifying organisms
Binomial Nomenclature
Two-part scientific name:
Genus (capitalized)
Species (lowercase)
Example:
Sciurus carolinensis
Classification Hierarchy
From smallest → largest:
Species
Genus
Family
Order
Class
Phylum
Kingdom
Domain
Key Term
Taxon = any classification group
Phylogenetic Trees
Show evolutionary relationships
Branching diagrams
Each branch point (node) = common ancestor
Important
Show pattern of descent, NOT exact time (usually)
Cladistics
Clades
Group = ancestor + ALL descendants
Called monophyletic
Key Idea
Group organisms by common ancestry
Shared Characters
Shared Ancestral Character
Trait from a distant ancestor
Example: backbone in mammals
Shared Derived Character
New trait unique to a group
Example: hair in mammals
Used to define clades
Ingroup vs. Outgroup
Ingroup = group being studied
Outgroup = related group used for comparison
Helps identify derived traits
Parsimony
Choose the simplest explanation
The tree with the fewest evolutionary changes is preferred
Trees Are Hypotheses
Based on current evidence
Can change with new data
Example Insight
Birds are actually part of the reptile clade
Molecular Systematics
Uses DNA/protein comparisons to determine relationships
Key Idea
More similar DNA → more closely related
Genome Evidence
Many genes are shared across species
Examples:
Humans & mice → ~99% homologous genes
Humans & yeast → ~50%
Strong evidence for common ancestry
Molecular Clocks
Definition
Use DNA mutation rates to estimate divergence time
How It Works
More differences in DNA → more time since split
Limitations
Mutation rates can vary
Example: HIV
The molecular clock is used to trace the origin
HIV-1 likely spread to humans in the 1930s
Gene Evolution
Gene Duplication
Creates extra gene copies
Allows new functions to evolve
Domains of Life
3-Domain System
Bacteria
Archaea
Eukarya
Key Insight
Archaea are closer to eukaryotes than bacteria
Horizontal Gene Transfer
Genes move between species (not just parent → offspring)
Methods:
Viruses
Plasmids
Impact
Early evolution may look like a network, not a tree
Tree vs. Ring of Life
Traditional view: tree
New idea: ring/network
Due to gene mixing early in evolution
Big Picture Summary
Phylogeny = evolutionary history
Classification reflects evolutionary relationships
Homology = shared ancestry; analogy = similar function
Cladistics groups organisms into clades
DNA evidence strengthens evolutionary trees
The evolution of life may be more complex than a simple tree