Early Evolutionary Thought
Darwin and Natural Selection
Evidence of Evolution
Microevolution
Evolutionary Processes
Macroevolution and Speciation
Evolution concepts predate Darwin.
Farmers and breeders (dog/flower) noted variations in species and bred for desired traits.
Colonialism exposed Western scientists to diverse new species.
Darwin’s grandfather, Erasmus Darwin, proposed early evolutionary ideas.
Jean-Baptiste Lamarck's Hypothesis:
Proposed that acquired characteristics could be inherited (e.g., giraffe necks).
Did not provide a mechanism for inheritance, leading to flaws in the theory.
Charles Lyell:
Proposed the Earth is much older than previously thought, gradual geological change continues.
Thomas Malthus:
Suggested human population growth is exponential, while resources grow linearly.
Darwin (1809-1882) came from a wealthy family, with a physician father and a Wedgwood mother.
His career path was uncertain; he shifted from medical school to clergy at Cambridge, ultimately becoming a naturalist on the H.M.S. Beagle at age 22.
Key locations explored:
North America, South America, Galápagos Islands, Australia, New Zealand.
Observations made during voyages contributed to his evolutionary theories.
Darwin's studies on the Beagle revealed:
Diverse habitats and species with adaptive traits.
Similar species in different regions fit local environments.
Collaboration with Alfred Russell Wallace on the concept of natural selection.
Components of Darwin’s Theory:
Heritable variation exists within populations.
Organisms compete for finite resources (food, habitat, mates).
Some variations enhance reproductive success.
Traits that promote reproductive success spread, leading to adaptation.
Adaptation: characteristic advantageous for survival; also a process of fitting to the environment.
The Theory of Evolution by Natural Selection is supported by comprehensive evidence from different fields.
Not merely a theory; incorporates extensive research findings from:
Fossils
Biogeography
Anatomy
Biochemistry
Fossil ages can be dated using:
Relative dating (rock layers)
Isotope dating
Fossilization conditions are scarce; specific requirements include hard body structures and appropriate burial conditions.
Transitional fossils (e.g., Ambulocetus, Archaeopteryx) illustrate evolutionary links.
Earth is 4.6 billion years old, divided into four eons:
Hadean: no life, high CO2, water vapor atmosphere.
Archean: emergence of rock, first prokaryotic fossils (3.5 BYA).
Proterozoic: eukaryotes appear (2.1 BYA).
Phanerozoic: divided into
Paleozoic: marine life to land colonization.
Mesozoic: age of reptiles, rise of birds/mammals.
Cenozoic: diversification of modern life forms.
Major periods and events:
Cambrian (488.3 MYA): emergence of non-vascular land plants.
Ordovician (443.7 MYA): marine algae flourish.
Devonian (416.0 MYA): first terrestrial vertebrates.
Mass Extinctions:
Great Dying: 83% species extinction.
Other significant events affecting biodiversity.
Mass Extinctions:
A significant decline in biodiversity.
Adaptive radiation follows extinctions.
Notable extinctions (e.g., Cretaceous asteroid impact killing dinosaurs).
Current species decline believed to be driven by human activity.
Biogeography examines species distribution patterns and adaptation.
Continental drift has caused species lineage to spread and diverge.
Historical climates have shaped current distribution.
Island species show evidence of colonization and adaptation.
Darwin’s finches and Hawaiian silver swords illustrate adaptive radiation based on environmental pressures.
Comparison of species anatomy reveals:
Homologous Structures: similar underlying structure due to common ancestry despite different functions.
Analogous Structures: similar function but different evolutionary origin.
Early embryonic development shows similarities among species.
Pharyngeal structures; human gills vs. fish.
Demonstrates common ancestry despite different adult forms.
Genetic similarities across species:
All organisms share DNA, ATP usage, and many proteins.
Mutations accumulate, leading to diversification over time.
Natural selection, mutations, migrations, and chance events drive microevolution.
Population genetics studies allele frequencies and distributions.
Established to explain variation in populations:
Conditions for equilibrium: no mutation, no migration, random mating, large population, no natural selection
Shift away from HWE indicates evolutionary change.
Investigating allele frequencies provides a basis for formulating hypotheses.
Practical applications in identifying potential evolutionary pressures within a population.
Understanding allele frequencies in a population:
Simple dominant/recessive traits: A and a determination of frequencies (p and q).
Using phenotype frequencies to derive genotype frequencies:
Homozygous recessives (aa) provide a starting point for calculations.
Key agents influencing variations in allele frequencies:
Mutations: source of genetic variation, critical for selection.
Genetic Drift: random shifts in allele frequencies.
Gene Flow: movement of alleles between populations.
Non-Random Mating: influences genotype frequencies.
Natural Selection: primary mechanism aligning traits to environment.
Founder Effect: Loss of genetic diversity when new populations form.
Bottleneck Effect: Population reduction leading to loss of variation impacting evolution.
Allows populations to become more alike; may introduce new traits.
Essential for maintaining genetic diversity through crossover of alleles.
Influences trait distributions in predictable ways:
Assortative mating increases homozygosity, while disassortative increases heterozygosity.
Mechanism requiring variation, competition, and reproductive success.
Adaptations emerge and spread over generations; unfavorable traits are reduced.
Fitness assessment as a measure of reproductive success:
High fitness associated with surviving offspring; factors like lifespan and mate attraction included.
Selection pressures on traits result in diverse effects, including
Disruptive, directional, and stabilizing selection pressures affecting phenotype distributions.
Variation persists despite natural selection, due to:
Frequency-dependent selection and oscillating selection strategies that shield against fixation.
Maintains genetic diversity by favoring heterozygotes in certain environments, as seen with sickle-cell anemia in malaria-prone regions.
Defining species through the Biological Species Concept (BSC): capable of mating and producing fertile offspring.
Maintained through reproductive isolation mechanisms.
Prezygotic isolation: includes ecological, behavioral, temporal, mechanical, and gametic barriers.
Postzygotic isolation: zygote mortality, hybrid sterility, and reduction in F2 fitness impact species continuation.
Allopatric speciation: geographic separation leading to genetic divergence.
Sympatric speciation: new species formation without geographic isolations, often through mechanisms like polyploidy.
Evolution of diverse species from a common ancestor in varying habitats, following extinction events or colonization of new environments.
Gradualism: conception of slow, gradual evolution over time.
Punctuated equilibrium: rapid bursts of evolution interspersed with longer periods of stability in species forms.
Evolutionary theory is a dynamic framework grounded in evidence from various biological fields, illustrating the intricate processes that shape life on Earth.