How did life begin?
13-17 billion years ago = Big Bang formed the universe
4.6 billion years ago = solar system formed
4.55 billion years ago = Earth formed
4 billion years ago = Earth has cooled enough for outer layers to solidify and oceans to form
4 - 3.5 billion years ago = life emerged
! Life requires interplay between DNA, RNA, and proteins
Living cells come from pre-existing cells
4 overlapping stages:
Nucleotides and amino acids produced prior to existence of cells
Nucleotides and amino acids became polymerized to form DNA, RNA, and proteins
Polymers became enclosed in membranes
Polymers enclosed in membranes evolved cellular properties
Primitive Earth
Reducing Atmosphere Hypothesis (1920s)
Primitive atmosphere
H2O vapor, N2, CO2
Small amounts of H2 and CO
Little free oxygen (reducing atmosphere)
Originally too hot for liquid water
As Earth cooled, water vapor condensed to liquid water
Primordial soup
Spontaneous formation of organic molecules
Monomers evolved and joined to form polymers
Abiotic (prebiotic) synthesis
Primitive Earth - video
TAKE NOTES!!
First Biomolecules
Miller’s and Urey’s Apparatus and Experiment (1953)
Showed that biochemicals could be produced from simple nonbiological sources
Primitive atmospheric gases
Strong energy sources
Yielded HCN, CH2O, glycine, sugars, amino acids, N-bases
More recent:
Neutral environment – CO, CO2, N2, H2O
Organics can be made under a variety of conditions
Alternative Mechanisms
Extraterrestrial Hypothesis
Organic carbon from asteroids and comets stocked prebiotic soup
Meteorite studies → Carbonaceous chondrites, lots of organic carbon, amino acid, nucleic acid bases
Controversy → destroyed by intense heat of impact?
Deep-sea vent Hypothesis (1988)
Key organics arose at deep-sea vents
Superheated water (150 C) rich in H2S and Metal ions mixes with cold seawater
Organics formed in temperature gradient around vents
Origin of the 1st Cell
Clay hypothesis
Simple organics polymerize on solid surface (clay, mud, inorganic crystals) into more complex organics
Cell-like structures - Protobiont
Boundary (ex. membrane)
Polymers inside contain info
Polymers inside with enzymatic function
Self-replication
Chemical Selection – RNA World
RNA in Protobionts
Can store info
Capacity for replication
Enzymatic functions (ribozymes)
Stromatolites = mats of mineralized cyanobacteria
Replaced by DNA/RNA/Protein World
Advantages of DNA/RNA/Protein World
Information storage
DNA would have relieved RNA of informational role and allowed RNA to do other functions
DNA = less likely to suffer mutations
Metabolism and other cellular functions
Proteins have a greater catalytic potential and efficiency
Proteins can perform other tasks → cytoskeleton, transport, etc.
Fossil Dating
Fossils = remains and traces of past life
Paleontology = the study of the fossil record
Most fossils are traces of organisms embedded in sediments
Sediment converted to rock
Becomes recognizable stratum in stratigraphic sequence of rocks
Strata of the same age tend to contain the similar fossil assemblages
Helps geologists determine relative dates of embedded fossils despite upheavals
Strata:
Index species
Wide distribution
Large number of individuals
Fossilize easily
Factors that Affect the Fossil Record
Anatomy
Size
Number
Environment
Time
Geological processes
Paleontology
Fossil Dating (Absolute)
Half-lives !!
Geologic Time Scale
Changes in organisms result from:
Genetic changes
Environmental changes
Patterns correlated with:
Climate/Temperature
Atmosphere
Land masses (continental drift 1-10cm/yr)
Floods/Glaciation
Volcanic eruptions
Meteorite impacts
Precambrian Time
Includes ~87% of geologic time → Hadean, Archaeon, and Proterozoic Eons
Little or no atmospheric oxygen
Lack of ozone shield allowed UV radiation to bombard Earth
First cells came into existence in aquatic environments
Prokaryotes ~3.5 billion years
Cyanobacteria left many ancient stromatolite fossils
Added first oxygen to the atmosphere
Evolution of aerobic species
Eukaryotic cells ~2 billion years
Multicellular organisms ~1.5 billion years
Ediacaran Period
635-541 million years
Multicellular animals appear, including sponges
Mudflat animals, unusual forms, no internal organs, no shells or bones
Mass Extinction occurred
Mass extinctions
Changes to the environment that dramatically increase the rate of extinction
Permian mass extinction
Lost 95% of marine species
Occurred over 500 thousand years
Period of extreme volcanic activity
Climate change – Earth warming 6 C, ocean acidification, etc.
Cretaceous mass extinction
Lost 76% of marine species, but also 75% of all animals and plants
Likely due to an asteroid impact – Chicxulub crater in Mexico
Paleozoic Era → Cambrian Explosion
Warm, wet climate, O2, no ice at poles
All existent phyla developed (?)
No major reorganizations of body plans since
Many marine invertebrates – 520 million years
High diversity of the Cambrian may be due to:
Favorable environment – oxygen
Evolution of Hox genes
Predator/prey “arms race” – shells, reef-building
Paleozoic Era – Ordovician Period
Warm temperatures and atmosphere very moist
Diverse marine invertebrates including trilobites and brachiopods
Primitive plants and arthropods first invade land
At end, abrupt climate change (large glaciers) resulted in mass extinction
Paleozoic Era – Invasion of Land
Silurian Period
Stable climate, glaciers melted
Significant vertebrates (many fishes) and plants, coral reefs appeared
Large colonization by terrestrial plants (seedless vascular) and animals (arthropods)
Devonian Period
North dry, South wet (oceans)
Many more terrestrial species
Gymnosperms emerge
Insects emerge
Tetrapods – amphibians emerge
Invertebrates flourish in the oceans
The Age of Fishes
Paleozoic Era – Carboniferous Period
Rich coal deposits formed
Cooler with land covered by forested swamps
Plants and animals further diversified
Very large plants and trees prevalent
First flying insects
Amphibians prevalent
Amniotic egg emerges → reptiles
Paleozoic Era – Permian Period
Continental drift formed supercontinent Pangea
Interior regions dry with seasonal fluctuations
Forest shift to gymnosperms
Amphibians prevalent but reptiles became dominant
First mammal-like reptiles appeared
At the end → largest known mass extinction event
Mesozoic Era – Age of Reptiles
Hot climate, dry terrestrial environments, little if any ice at poles
Triassic Period
Gymnosperms dominant
Reptiles abundant (1st dinosaurs appeared)
1st true mammals
Jurassic Period
Dinosaurs achieved enormous size
Mammals remained small and insignificant
1st bird
Cretaceous Period
Dinosaurs began precipitous decline
Mammals began an adaptive radiation and moved into habitats left vacated by dinosaurs
Cenozoic Era – Age of Mammals
Tropical conditions replaced by a colder, drier climate
Mammals continued adaptive radiation (birds, fishes, insects diversified)
Flowering plants already diverse and plentiful
Primate evolution began
Quatemary Period (1.8 mya to today)
Age of Man (hominids)
Homo sapiens appear 130,000 years ago
Primate Evolution
Lemurs, tarsiers, monkeys, apes, humans
Descended from tree-dwellers
All adapted for climbing trees
Rotating shoulder joint
Big toe and thumb widely separated from others
Stereoscopic vision
Also: larger brain, 1 offspring/pregnancy, upright body
Humans (homo) → bipedalism, increased brain size, fully opposable thumb
6th Mass Extinction (Holocene, Anthropocene Extinction)
Currently experiencing the worst spate of species die-off
Humans = global superpredators
Living Planet Report 2020
Average 68% decline in monitored populations of mammals, birds, amphibians, reptiles, and fish between 1970 and 2016
Most significant declines in tropical subregions of the Americans and Africa
Freshwater biodiversity declining faster than terrestrial or oceanic
Megafauna particularly vulnerable
Plant extinction risk is comparable to that of mammals and higher than for birds
>⅕ of wild species are at risk of extinction this century due to climate change alone
Evolution → heritable change in one or more characteristics of a population or species from one generation to the next
Species → group of related organisms that share a distinctive form
Among species that reproduce sexually, members of the same species are capable of interbreeding to produce viable and fertile offspring
Population → members of the same species that are likely to encounter each other and thus have the opportunity to interbreed
Microevolution → changes in a single gene in a population over time
Macroevolution → formation of new species or groups of species
History of Evolutionary Thought
Pre-Darwinian = influenced by myth, religion, and superstition
Anaximander (611-547 BC) = Organisms evolve from other organisms
Plato (427-347 BC) = Objects are temporary reflections of ideal forms
Aristotle (384-322 BC) = All living things can be arranged in a linear hierarchy (Scala
naturae)
Creationism = a god is absolute creator of heaven and earth, out of nothing, by an act of
free will; includes Christians, Jews, and Muslims
Spontaneous Generation (5th - 14th century AD)
Sweaty rags in open jar with grain after 21 days produces mice
Rotting meat produces maggots
Dust gives rise to flies
Scala Naturae
Establishes humans as dominant and a perfect form of life
Sets humans above and apart from nature
Incorporated into the religious belief that the Earth and its creatures are the result of special creation, that they have not changed since they were created
History of Evolutionary Thought
Taxonomy matured during late 17th to mid 18th century
John Ray
Carolus Linnaeus → fixity of species, binomial system of nomenclature
Count George Buffon = catalog of all plants and animals, suggested life forms change over time
Erasmus Darwin = suggested common descent, evidence in developmental patterns
Georges Cuvier = first to use comparative anatomy to develop a system of classification, founded paleontology, proposed catastrophism
Jean-Baptiste Lamarck = first biologist to propose evolution and link diversity with environmental adaptation
Concluded more complex organisms are descended from less complex organisms
Proposed inheritance of acquired characteristics = Lamarckism
James Hutton and Charles Lyell = Earth is subject to slow but continuous cycles of erosion and uplift
Proposed Uniformitarianism, rates and processes of change are constant
Principles of geology
Darwin’s theory of evolution
Geological observations consistent with those of Hutton and Lyell
Biogeographical observations:
The study of the geographic distribution of life forms on earth
Darwin saw similar species in similar habitats
Reasoned related species could be modified according to the environment
Galapagos Islands
Tortoises → observed tortoise neck length varied from island to island, proposed that speciation on islands correlated with a difference in vegetation
Finches → observed 13 species of finches on various islands, speculated they could have descended from a single pair of mainland finch
Darwin and Origin of Species
Returned to England and wrote the Origin of Species about his voyages on the HMS Beagle and what he discovered
Darwin’s Explanatory Model of Evolution by Natural Selection
Survival of the Fittest
Fitness = the relative reproductive success of an individual
Most-fit individuals in a population capture a disproportionate share of resources
Interactions with the environment determine which individuals reproduce the most
Adaptation
Changes that help a species become more suited to its environment
Product of natural selection
Evolution in Action – Industrial Melanism
Before industrial revolution → peppered moths = 10% dark colored, 90% light
After IR → soot in atmosphere, tree trunks darkened, lichens killed, peppered moths = 80% dark colored, 20% light (currently we have moved back to more light colored)
Adaptive Melanism
Melanin = makes skin darker or lighter depending on amount, keeps us safe from UV sun rays
Videos on slides
Melanin genes targeted by evolution → ex. Pocket mice
Evolution of bacteria on a mega agar plate petri dish
Evidence of Evolution – Comparative Anatomy
Homologous Structures:
Anatomically similar because they are inherited from a common ancestor
May be functionally similar or not
Analogous Structures:
Serve the same function
Not constructed similarly
Do not share a common ancestor
Convergent evolution
Convergent Evolution = similarity due to convergence
Evidence of Evolution – Comparative Anatomy
Vestigial structures:
Fully-developed anatomical structure
Reduced or obsolete function
Human appendix
Male breast tissue/nipple
Wisdom teeth in humans
Human tailbone (coccyx)
Erector pili and body hair
Blind fish - Astyanax mexicanus
Sex organs in dandelions
Wings on flightless birds
Hind leg bones in whales/snakes
Fake sex in virgin whiptail lizards
Comparative Development
All vertebrate embryos have:
A postanal tail
Paired pharyngeal (gill) pouches
Dorsal, hollow nerve cord
Notochord
Evidence of Evolution – Fossil Record
Fossils record the history of life from the past
Document a succession of life forms from the simple to the more complex
Sometimes the fossil record is complete enough to show descent from an ancestor
Whales
Fossil record spans 50 million years
Terrestrial tetrapod to aquatic animal lacking hind limbs
Order Cetacea: whales, dolphins, porpoises
Evidence of Evolution – Biogeography
Alfred Russell Wallace - Father of Biogeography
Study of geographical distributions of plants and animals across Earth
Different mixes of plants and animals in areas separated by water, continents, and islands
Consistent with origin in one locale and then spread to accessible regions
Evidence of Evolution – Plate Tectonics
Evidence of Evolution – Molecular Homologies
Almost all living organisms:
Use the same basic biochemical molecules
Utilize the same DNA triplet code
Utilize the same 20 amino acids in their proteins
Utilize ATP as an energy source
Genetic homologies (DNA base-sequence differences)
When very similar, suggest recent common descent
When more different, suggest more ancient common descent
Evidence of Evolution – Genetic Homologies
Process of Evolution
Variations are produced by chance mutations and sexual reproduction
Natural selection selects the ‘fittest’ organisms
Natural selection leads to adaptation to a particular environment
Process occurs constantly in all species of life on Earth
Natural selection acts on individuals in a species
Evolution = a property of populations
Occurs generation to generation
Descendants are different from ancestors
Change in allele (gene) frequencies; change in genetic makeup of population over time (generations)
Genes in Populations
Populations genetics = study of genes and genotypes in a population
Want to know extent of genetic variation, why it exists, how it is maintained, + how it changes over the course of many generations
Helps us understand how genetic variation is related to phenotypic variation
Genes in Natural Populations
Genes can be monomorphic (99% = 1 allele)
Or polymorphic (2 or more alleles in population)
Polymorphism comes about through various changes:
Duplication of gene region
Deletion of significant region of gene
Change in a single nucleotide (SNP) (smallest and most common change in a gene)
Allele frequency = # of copies of a specific allele in a population/total# of all alleles for that gene in population
Genotype frequency = # of individuals with a particular genotype/total # of individuals in a population
Hardy-Weinberg Principle
1908 → G.H. Hardy and W. Weinberg independently recognized that:
Genes remain in equilibrium (constant frequency) over time (in each succeeding generation of a sexually reproducing population) as long as 5 conditions are met
Relates allele and genotype frequencies in a population
Can be described by the binomial equation
Using the Hardy-Weinberg Equation
p + q = 1
p^2 + 2pq + q^2 = 1 (expansion)
Hardy-Weinberg Equilibrium
Conditions to be met:
No mutations → allelic changes do not occur, or changes in one direction are balanced y changes in the opposite direction (also no gene duplication, exon shuffling, or horizontal gene transfer)
No gene flow → migration of alleles into or out of the population does not occur
Random mating → individuals pair by chance and not according to their genotypes
No genetic drift → the population is very large, and changes in allele frequencies due to chance alone are insignificant
No selection → no selective agent favors one genotype over another, all genotypes are equally adapted
If p or q is changed in next generation → evolution has occurred!!
Hardy-Weinberg identifies factors that cause evolution
Evolution detected by noting any deviation from a Hardy-Weinberg equilibrium of allele frequencies in the gene pool of a population
Equilibrium population = hypothetical population in which evolution does not occur
Conditions for Hardy-Weinberg are rarely met
Hardy-Weinberg population provides starting point for studying mechanisms of evolution
Microevolution = accumulation of small changes in the gene pool of a population over a relatively short period of time
Causes of Microevolution – Genetic Mutations
The raw material for evolutionary change → source of genetic variability
Source of new alleles → leads to new combinations of alleles
Not goal-directed → not a result of environmental necessity
Random events → can be good, bad, or neutral (depending on environmental conidtions)
Other forces act to either maintain the variation or remove it from the population
Causes of Microevolution – Gene Flow/Gene Migration
Movement of alleles between populations when:
Gametes or seeds (in plants) are carried into another population
Breeding individuals migrate into or out of population
Continual gene flow reduces genetic divergence between populations
Typically increases genetic diversity within the population
Populations of relatively sedentary organisms are more isolated from one another than populations of very mobile organisms (subspecies)
Causes of Microevolution – Non-random Mating
Non-random Mating = when individuals do not choose mates randomly
Assortative Mating
Individuals select mates with their phenotype and reject opposites
Increases the number of homozygotes
Disassortative Mating
Dissimilar phenotypes mate preferentially
Increases the number of heterozygotes
Inbreeding
Mating of 2 genetically related individuals
Chose a mate from same genetic lineage
Causes of Microevolution – Genetic Drift
Changes to allele frequency due to random chance
Can cause the gene pools of two isolated populations to become dissimilar
Some alleles are lost (0%) and others become fixed (100%)
Likely to occur:
After a bottleneck
With severe inbreeding
When founders start a new population
A random event prevents a majority of individuals from entering the next generation → next generation composed of alleles that just happened to make it
Stronger effect in small populations
Bottleneck Effect
African Cheetah
Fastest living land animals (70+mph)
Lost nearly all genetic variability (monomorphic for almost all genes)
Prolonged inbreeding following a Bottleneck (10-20,000 years ago)
Very low sperm count, motility, deformed flagella
Northern Elephant Seals
Low genetic variability
Human inflicted (1890’s)
Hunted to 20 individuals → now 100,000
May be susceptible to pollution/disease
Founder Effect
When a new population is started from just a few individuals
The alleles carried by population founders are dictated by chance
Formerly rare alleles will either:
Occur at a higher frequency in the new population
Be absent in the new population
Ex. Amish Ellis-van Creveld syndrome
Causes of Microevolution – Natural Selection
Adaption of a population to the biotic and abiotic environment
Biotic = competition, predation, sexual selection
Abiotic = climate, water availability, minerals
Requires:
Variation = the members of a population differ from one another
Inheritance = many differences are heritable genetic differences
Differential Adaptiveness = some differences affect survivability
Differential Reproduction = some differences affect likelihood of successful reproduction
Results in:
A change in allele frequencies in the gene pool
Improved fitness of the population
Major cause of microevolution
Types of Selection
Directional Selection
Individuals at one extreme of a phenotypic range have greater reproductive success in a particular environment
Curve shifts in that direction
Ex. size of modern horse, industrial/adaptive melanism, DDT-resistant mosquitos
Stabilizing Selection
Intermediate phenotype is favored
The peak of the curve increases and tails decrease
Ex. human babies with low or high birth weight = less likely to survive
Disruptive (Diversifying) Selection
Two or more extreme phenotypes are favored over intermediates → bimodal distribution
Ex. Capeta snails vary because a wide geographic range causes selection to vary
Types of Selection (cont.)
Balancing Selection
Maintains genetic diversity
Balanced polymorphism
Two or more alleles are kept in balance and therefore are maintained in a population over the course of many generations
Two common ways:
For a single gene, heterozygote favored
Negative frequency-dependent selection – rare individuals have a higher fitness (predator-prey)
Sexual Selection → a special case of Natural Selection
Directed at certain traits of sexually reproducing species that make it more likely for individuals to find or choose a mate and/or engage in successful mating
In many species, male characteristics affected more intensely than female (secondary sex characteristics, sexual dimorphism)
Intrasexual – same sex
Males directly compete for mating opportunities or territories
Intersexual – opposite sex
Females choose with males possessing a particular phenotype
Ex. birds of paradise
Maintenance of Variations
Genetic variability
Populations with limited variation may not be able to adapt to new conditions
Maintenance of variability is advantageous to population
Only exposed alleles are subject to natural selection
Natural selection does not cause genetic changes
Natural selection acts on individuals
Population evolves as gene frequencies change
Macroevolution = evolutionary changes that create new species and groups of species, accumulation of microevolutionary changes over long periods of time
Speciation:
The splitting of one species into two = Cladogenesis
The transformation of one species into a new species over time = Anagenesis
What is a species?
Typographical (Morphological) Species Concept
Species is defined by fixed, essential features
Each species has a unique structure that makes it distinct
Biological Species Concept
A species is a reproductive community of populations (reproductively isolated from others) that occupies a specific niche in nature → interbreeding with common gene pool to produce viable, fertile offspring
Drawbacks = species have dimensions in space and time, sexual and asexual reproduction, unit of evolution and taxonomic category
Ecological Species Concept
Using the ability of organisms to successfully occupy their own ecological niche or habitat, including their use of resources and impact on the environment → to distinguish species
Phylogenetic (Evolutionary) Species Concept
A species is an irreducible group of organisms diagnosably distinct from other such groupings and within which there is parental pattern of ancestry and descent
Morphological, chromosomal, molecular characters used
Reproductive Isolating Mechanisms
Reproductive isolating mechanisms inhibit gene flow between species and maintain distinctiveness of species
Prezygotic Mechanisms
Discourage attempts to mate
Habitat isolation
Temporal isolation
Behavioral isolation
Mechanical isolation
Gamete isolation
Postzygotic Mechanisms
Prevent hybrid offspring from developing or breeding
Hybrid inviability (zygote mortality)
Hybrid sterility
Hybrid breakdown
Modes of Speciation
Allopatric Speciation
Two geographically isolated populations of one species
Become different species over time – gene flow interrupted
Can be due to differing selection pressures in differing environments
Ex. Kaibab and Abert squirrels on North vs. South rim of Grand Canyon = two different species now, Grunts of the sea = Panamic vs. Atlantic Porkfish
Classification of Living Things
1.75 million species described
10-100 million actually exist
Systematics and Taxonomy
Systematics = the study of the biological diversity and evolutionary history of life on Earth
Taxonomy = branch of biology concerned with identifying, naming, and classifying organisms
Name → only 1 scientist gets to “name” a species
Identify → anyone can with a key
Classify → group a species with its closest relatives
Began with the ancient Greeks and Romans
Aristotle classified organisms into groups such as horses, birds, and oaks (Scala naturae)
Every organism should have a set name (creds to John Ray)
Taxonomy
Carolus Linnaeus (mid 1700s)
Binomial System of Nomenclature
First word is GENUS name
Second word is SPECIFIC EPITHET
= refers to one species within its genus
Species is referred to by the full binomial name (Genus species) or Genus species (specific epithet)
Genus name can be used alone to refer to a group of related species
Whole thing should be in italics
Scientific Names
Some names are super long, some super short, some unusual, some after celebs
Classification Categories
Modern taxonomists use the following classification:
Domain = one or more supergroups
Supergroup = one or more kingdoms
Kingdom = one or more phyla
Phylum = one or more classes
Class = one or more orders
Order = one or more families
Family = one or more genera
Genus = one or more species
Species
Whole thing is called the taxon
Did King Phillip Come Over For Good Sushi? ACRONYM FOR MEMORIZATION!!
Classification Categories
The higher the category → the more inclusive
Organisms in the same domain have general characteristics in common
In most cases, classification categories can be subdivided into additional categories → superorder, suborder, infraorder
Distinguishing species on the basis of structure can be difficult
Members of the same species can vary in structure
Attempts to demonstrate reproductive isolation is problematic because:
Some species hybridize
Reproductive isolation is difficult to observe
Phylogenetic Trees
Goals of systematics:
To discover all species
To reconstruct the phylogeny (evolutionary history) of a group
To classify accordingly
Phylogeny often represented as a phylogenetic tree
A diagram indicating lines of descent
Each branching point:
= a divergence from a common ancestor
Represents an organism that gives rise to two new groups
Phylogenetic Trees
Classification lists the unique characters of each taxon and is intended to reflect phylogeny
Primitive characters = present in all members of a group, present in the common ancestor
Derived characters = present in some members of a group, but absent in the common ancestor
Tracing Phylogeny
Fossil Record
Fossil record = incomplete
Often difficult to determine the phylogeny of a fossil
Homology
Refers to features that stem from a common ancestor
Homologous structures are related to each other through common descent
Tracing Phylogeny
X Convergent Evolution – Analogy
The acquisition of a feature in distantly related of descent
The feature is not present in a common ancestor
X Parallel Evolution
= the independent evolution of similar traits → starting from a similar ancestral condition
Several species respond to similar challenges in a similar way
Molecular Data
Protein Comparisons
Immunological techniques
Degree of cross-reaction used to judge relationship
Amino acid sequencing
Similar sequence in same protein indicates close relationship
RNA and DNA Comparisons
Systematics assumes:
2 species with similar base-pair sequences are assumed to be closely related
2 species with differing base-pair sequences are assumed to be only distantly related
Molecular Clocks
Use non adaptive nucleotide sequences
Assumed constant rate of (neutral) mutations over time
Favorable mutations are rare
Detrimental mutations are quickly eliminated
→ means most mutations are neutral
mtDNA = 2% nucleotide changes/1 million years
SSU(18S) rRNA = 1% sequence change/50 million years
DNA – DNA Hybridization
Traditional Systematics
Mainly uses anatomical data
Classify organisms using assumed phylogeny with emphasis on phenotype
Stress both common ancestry and degree of structural difference among divergent groups
Construct phylogenetic trees by applying evolutionary principles to categories
Not strict in making sure all taxa are monophyletic
Monophyly
Paraphyly = includes common ancestor but not all descendants
Polyphyly = members traced to separate ancestors, does not contain the most recent common ancestor of the group
Cladistic Systematics
Traces evolutionary history of the group under study
Uses shared derived characters = Synapomorphies to:
Classify organisms
Arrange taxa into a cladogram
Cladogram = special type of phylogenetic tree
Clade = evolutionary branch that includes:
A common ancestor, together with:
All its descendant species
Monophyletic group = taxon whose units all evolved from a single parent stock, most recent common ancestor and all of its descendants
Parsimony
Cladists are always guided by the principle of parsimony
The arrangement requiring the fewest assumptions is preferred
This would:
Leave the fewest number of shared derived characters unexplained
Minimize the number of assumed evolutionary changes
The reliability of a cladogram is dependent on the knowledge and skill of the investigation
Cladistic vs Traditional Phylogeny
Classification System – Previous
Until the mid-1800s → biologists recognized only 2 kingdoms:
Plantae (plants)
Animalia (animals)
Protista (protists) were added as a third kingdom in the 1880s
Whittaker expanded to five kingdoms in 1969 by adding Fungi and Monera
The Three-Domain System of Classification
The bacteria and archaea are so different that they have been assigned to separate domains
Distinguishable by:
Difference in rRNA base sequences
Plasma membrane chemistry
Cell wall chemistry
Domain Eukarya
Uni- and multicellular organisms
Cells with a membrane-bound nucleus
Sexual reproduction common
Contains kingdoms – Fungi, Plantae, and Animalia
Protists, now New Kingdom = Hemimastigotes
General characteristics
Noncellular → cannot be classified with cellular organisms, generally <200nm in diameter
Each type has at least 2 parts:
Capsid
Outer layer composed of protein subunits
Some enveloped by membrane, others non-enveloped or “naked”
Generally symmetrical
Nucleic acid core
DNA or RNA (3-100 genes)
Single or double-stranded, linear or circular
4 morphological categories → very diverse (over 4000 types)
Icosahedral
Complex
Helical
Spherical
Categorization
Unique
Obligate intracellular parasites
Cannot reproduce outside a living cell
Can be cultured only inside living cells
Cannot move, metabolize, or respond to stimuli
All are infectious!
Similar
Can make copies of themselves (although they need a host)
Can evolve/mutate
Are parasites/infect organisms
Contain genetic material as their instructions
Viruses can stay dormant until ideal conditions
Can respond to their environment
Classification is based on:
Type of nucleic acid (DNA/RNA, single or double-stranded)
Size and shape
Presence/absence of outer envelope
Viral Replication
Bacteriophages
Portions of capsid adhere to specific receptor on the host cell
Not easily recognized by host immune system
Viral nucleic acid enters the cell
Once inside, the virus takes over metabolic machinery of the host cell
Viral Assembly
During assembly → the components of the virus that were produced during replication are organized into viral particles before being released by the cell
Viral Infections
Viruses are best known for causing infectious diseases in plants and animals
Most common entry point → respiratory tract, open wounds
Herpes, HIV, cancer
Viruses lack metabolism → antibiotics have no effect
Controlled by preventing transmission (vaccines, antiviral drugs)
Viroids
Naked strands of RNA
Many crop diseases
Prions
Protein molecules with contagious tertiary structure
Some human and other animal diseases: TSE’s (Scrapie, Kuru, Mad cow)
Emerging Diseases
An emerging disease is one that has appeared in a population for the first time, or that may have existed previously but is rapidly increasing in incidence or geographic range
AIDS
West Nile Encephalitis
SARS
Ebola Hemorrhagic Fever
Bird Flu
HPS
Chikungunya Virus
COVID-19
Re-emerging → cholera, plague, dengue hemorrhagic fever, yellow fever, malaria, tuberculosis
HIV and AIDS
Human Immunodeficiency Virus (HIV) = causative agent of Acquired Immune Deficiency Syndrome (AIDS)
Primarily spread by sexual contact between infected and uninfected individuals
Can also be spread:
By transfusion of HIV-infected blood
By sharing of needles among drug users
From infected mother to unborn child
Globally there are ~38 million people living with HIV as of 2019
65% of all new HIV infections are in Sub-Saharan Africa
Influenza Virus – the ‘Flu’
The Flu = viral, respiratory disease with fevers, headache, cough, runny nose, muscle pain
4 Influenza Viruses → A, B, C, D
Seasonal Flu → A, B
Characterized by surface antigens
More health complications and hospitalizations, harder to prevent
Mutates faster than others
Hard to prevent with vaccination
SARS-CoV-2
Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2) = a strain of coronavirus that causes COVID-19, the respiratory illness responsible for the COVID-19 pandemic
It is a positive-sense single-stranded RNA (+ssRNA) virus, with a single linear RNA segment
SARS-CoV-2 is a strain of the species Betacoronavirus pandemic (SARSrCoV), as is SARS-CoV-1 (the virus that caused the 2002-4 SARS outbreak)
The virus is airborne and primarily spreads between people through close contact and via aerosols and respiratory droplets
It enters human cells by binding to angiotensin-converting enzyme 2 (ACE2), a membrane protein that regulates the renin-angiotensin system
SARS-CoV-2 strain tree
There are many thousands of variants of SARS-CoV-2 → which can be grouped into the much larger clades
Gives understanding of the evolutionary relationships between a set of species
Designing vaccines, for ex. SARS-CoV2
The Tree of Life
Domains, Bacteria, and Archaea
Fully functioning Prokaryotic cells
More numerous than all other organisms
Fossils to 3.5 billion years ago, alone on Earth for over 1 billion years
Very diverse (50+ bacterial phyla)
Horizontal gene transfer important in their diversification
Differ from each other in metabolism, genetics, and membrane structure
Horizontal Gene Transfer
Movement of one or more genes from one species to another
Contrasts with vertical gene transfer from parent to progeny
Increases genetic diversity
Common among archaea and bacteria
Can result in large genetic changes
At least 17% of the genes present in E. Coli came from other bacteria
About 80% of prokaryotic genes have been involved in horizontal transfer at one point or another
Prokaryotic Cell Structure
Reproduction in Prokaryotes
Prokaryotes reproduce asexually by means of binary fission
Methods of genetic recombination:
Conjugation = sex pilus forms between 2 cells, donor cell passes DNA to recipient cell through pilus
Transformation = occurs when bacterium picks up free pieces of DNA from other prokaryotes, becomes incorporated into genome
Transduction = occurs when bacteriophages carry portions of bacterial DNA from one cell to another (vectors)
Endospores
Response to unfavorable conditions
Dormant stage
Resistant to heat, radiation, disinfectants, and desiccation
Difficult to eliminate from medical and pharmaceutical materials
Frequent cause of contamination
Exs. anthrax, tetanus, botulism, botox
Some bacteria form resistant endospores
Prokaryotic Nutrition
Oxygen requirements:
Obligate aerobes = unable to grow in the absence of free oxygen
Facultative aerobes = able to grow in either the presence or absence of free oxygen
Obligate anaerobes = unable to grow in the presence of free oxygen (botulism, gangrene, tetanus)
Aerotolerant anaerobes = do not use oxygen but are not poisoned by it
Autotrophic Prokaryotes
Photoautotrophs
Some do not produce O2 (green/purple bacteria)
Some use solar energy to reduce carbon dioxide to organic compounds
Photosynthetic
Chemoautotrophs
Oxidize inorganic compounds to obtain the necessary energy
Use it to reduce CO2 to an organic compound
Chemosynthetic
Heterotrophic Prokaryotes
Most prokaryotes are chemoheterotrophs that take in organic nutrients
Aerobic saprotrophs decompose most large organic molecules to smaller molecules (detritivores)
Essential components of healthy ecosystem
May be free-living or symbiotic
Nitrogen fixation (diazotrophs)
Commensalism
Parasites
Commercial uses:
Produce chemicals (ethanol), butter, cheese, rubber, cotton, silk, coffee, cocoa, antibiotics, yogurt
Bacterial Cell Wall !!
Gram-positive vs. gram-negative (GN much more virulent)
Bacteria
Classified in terms of their five basic shapes:
Round (coccus)
Rod (bacillus)
Comma (vibrio)
Flexible Spiral (spirochete)
Rigid Spiral (spirillus)
Pathogenic Bacteria
Sexually transmitted → Syphilis, Gonorrhea
Systemic → Plague, Typhoid fever
Respiratory → Strep throat, Scarlet fever
Skin → Boils, carbuncles
Digestive tract → Gastroenteritis, food poisoning
Nervous system → Botulism, Tetanus
Others → Tularemia, Lyme disease
Outbreaks
Salmonella
Group of rod-shaped enterobacteria
Passed from infected feces of people/animals
Common sources → pet feces, reptiles, amphibians, poultry, beef, eggs, vegetables, milk, peanut butter
Symptoms → last 4-7 days, diarrhea, fever, abdominal cramps
1.35 million American cases per year
Also causes typhoid fever
E. coli
Hundreds of strains, most harmless
Reside in intestines of healthy humans and animals
Escherichia coli
95,000 American cases a year
Infection often leads to severe stomach cramps, bloody diarrhea, and occasionally kidney failure.
Sources → undercooked ground beef, unpasteurized milk and juice, raw fruits and vegetables, contaminated water
Evolution of the Eukarya Domain
Eukarya
Paraphyletic group – very diverse
Morphology:
All life activities carried on within limits of one membrane (mostly)
Most unicellular and microscopic, specialized organelles
Many with amazingly high level of structural and functional complexity
Life cycles:
Asexual reproduction common
Sexual reproduction may occur when conditions deteriorate
Some life cycles simple, many extremely complex
Features of Eukarya
Cells with nuclei surrounded by nuclear envelope with pores
Chromosomes organized by histones
Cytoskeleton of microtubules and microfilaments
Mitochondria
Cilia and flagella
Mitosis
Sexual reproduction – meiosis
Cell walls (cellulose, chitin)
Ecology/evolution
Protists are of enormous ecological importance
Photoautotrophic forms:
Produce oxygen - primary producers in both freshwater and saltwater ecosystems
Major component of plankton → suspended in the water
Serve as food for heterotrophic protists and animals
Many protists are symbionts (parasitism to mutualism)
Coral reefs greatly aided by symbiotic photoautotrophic protists in tissues of corals → Zooxanthellae
Some with great medical importance → pathogenic/parasitic
Difficult to classify
Plant-like = multicellular algae are not plants, do not protect gametes/zygote from desiccation
Fungi-like = lack flagella, no chitin in cell wall
Animal-like = heterotrophs but no embryonic development
Protists:
Large group of eukaryotic organisms
Live in water-based environments
Majority of them are unicellular, microscopic, and motile
Archaeplastida – Red Algae
Generally multicellular, light red to dark green, about 6500 species
Marine (mostly in warmer seawater), can be as deep as 200m
Some filamentous, most branched, feathery, flat
Economic importance:
Agar, agarose → capsules, dental impressions, cosmetics, culture medium, electrophoresis, food prep.
Carrageen → emulsifying agent used in chocolate, low-fat foods, cosmetics
Reddish-black wrappings around sushi rolls consist of processed Porphyra blades
Archaeplastida – Green Algae
Over 7000 species
Variety of environments → oceans, freshwater, snowbanks, tree bark, turtles’ backs
Many symbiotic with fungi, plants, or animals
Morphology varied:
Majority unicellular, but many are filamentous or colonial
Some are multicellular and resemble leaves of lettuce
Plants thought to be derived from Charophytes
Have a cell wall that contains cellulose
Possess chlorophylls a and b
Store excess food as starch
Amoebozoa – Amoebas
Amoeboids are protists that move and ingest their food with pseudopods – phagocytize food
Pseudopods form when cytoplasm streams forward in a particular direction
Entamoeba histolytica – parasite of the human colon (50 million cases/year)
Causes amoebic dysentery
Can be fatal
Naegleria fowleri
Primary amoebic meningoencephalitis (PAM)
Amoebozoa – Slime molds
They are not actually molds
Can be:
Plasmodial = single multinucleated cells
Cellular = single cells that can aggregate to form multicellular organisms
Opisthokonta
Contrary to other protists, have a single flagellum at the back
Choanoflagellates:
Animal-like
~250 species
Marine and freshwater
Solitary or colonial
Attached or free-swimming
Single flagellum surrounded by collar of microvilli
Rhizaria
Many can make shells (tests) → varied shapes + materials, silica, calcium carbonate, etc.
Important for the carbon and nitrogen cycles
Cercozoans
Can have or lack a shell
Vampyrella = the vampire amoeba
Chromalveolata – Dinoflagellates
About 4000 species of unicellular aquatic and marine organisms
Morphology:
Cell = usually bounded by protective cellulose plates impregnated with silicates
Two flagella
One in a longitudinal groove with its distal end free
Other lies in a transverse groove that encircles the organism
Some photosynthetic, some heterotrophic, some parasitic
Symbiotic dinoflagellates in corals called Zooxanthellae
Dinoflagellates provide their host with organic nutrients
Corals provide wastes to fertilize the algae
Chromalveolata – Apicomplexans
Non-motile obligate parasites
Apical complex of organelles on merozoites/sporozoites → penetrate host
Most serious parasitic human disease = malaria → caused by Plasmodium spp
Millions of cases, hundreds of thousands of deaths
Transmitted by the pregnant female mosquito
Pregnant women + children = most vulnerable
Few treatments + preventions
Malaria life cycle
Chromalveolata – Ciliates
Ciliates are among the most complex of the protozoans
Hundreds of cilia beat in coordinated rhythm
Most are holozoic, swallowing food whole
Divide by transverse binary fission during asexual reproduction
Two nuclei of differing types:
Micronucleus – heredity
Macronucleus – metabolism
Chromalveolata – Diatoms + Golden Algae
Diatoms = the most numerous unicellular algae in the oceans (also important in freshwater)
Significant portion of phytoplankton
Primary producers
Cell wall
Two valves → larger valve acts as a lid
Contains silica
Diatomaceous earth used as:
Filtering agents
Sound-proofing materials
Polishing abrasives
Chromalveolata – Brown Algae
About 1500 species
Most live in colder ocean waters along rocky coasts
No unicellular or colonial brown forms
Morphology:
Some small forms with simple filaments
Others large multicellular forms that may exceed 200m in length
Pigments:
Chlorophylls A and C
Fucoxanthin (type of carotinoid pigment) gives them their color
Excess food stored as a carbohydrate called laminarin
Excavata – Euglenozoans
Euglenoids
Small freshwater unicellular organisms
Have 1 flagellum and an eyespot
1 flagellum much longer than the other
Projects out of an anterior, vase-shaped invagination
Called a tinsel flagellum because of hair-like projections
Cell bounded by flexible pellicle
Chloroplasts:
Surrounded by three rather than two membranes
With a pyrenoid → which produces an unusual type of carbohydrate called paramylon
Kinetoplastids
Colorless heterotrophs – unusual mitochondria
Most symbiotic and many parasitic
Well known for causing various diseases in humans
Trypanosomes
African sleeping sickness → tsetse fly
Chagas disease → kissing bug
Leishmania spp.
12 million
Sand fly → vector
Life Cycles
Characteristics
Over 150K species growing
Mostly multicellular eukaryotes that share a common mode of nutrition
Heterotrophic (Sapotrophic decomposers)
Cells release digestive enzymes and then absorb resultant nutrient molecules
Some are parasitic:
Millions of dollars of crop losses per year
Human diseases: ringworm, athlete’s foot, yeast infections, fungal infections = mycosis
Several have mutualistic relationships
Structure
The body of most fungi is multicellular mycelium
Mycelium = a vast network of thread-like hyphae
Aseptate fungi – multinucleated
Septate fungi – hyphae with cross walls
Hyphae grow from tip (osmosis, cytoplasmic streaming)
Give the mycelium a large surface/volume ratio
Cell walls of chitin
Excess food stored as glycogen as in animals
Produce pigments, including melanin
Reproduction
Both sexual in most and asexual reproduction = results in nonmotile spores
Spores = used for reproduction means of dispersal of organism
Resistance to harsh conditions
Phylogeny
Zygomycota
Bread molds (Zygospore Fungi)
Mainly saprotrophs decomposing animal and plant remains, bakery goods in a pantry
Some parasites of soil protists, worms and insects
Black bread mold - Rhizopus stolonifer
Sac Fungi – Ascomycota
Most as saprotrophs that digest resistant materials containing cellulose, lignin, or collagen
Most are composed of septate hyphae
Neurospora = model organism
Morels and truffles, famous gourmet delicacies revered throughout the world
Many plant diseases → powdery mildews, leaf curl fungi, ergot of rye, chestnut blight, Dutch elm disease
Yeasts in baking/brewing, Aspergillus and Candida cause serious human infections
Penicillium spp. = source of penicillin
Sac Fungi – Asexual Reproduction
Asexual reproduction is the norm
Yeasts usually reproduce by budding
A small bulge forms on the side of cell
Receives a nucleus and gets pinched off and becomes full-size
The other ascomycetes produce spores called conidia or conidiospores → spores are 1n
Vary in size and shape and may be multicellular
Spores are haplotype
Conidia usually develop at the tips of conidiophores
Conidiophores differ in appearance and can be used for diagnostic
Conidia are windblown
Conidia of Cladosporium cause allergies
Sac Fungi – Sexual Reproduction
Ascus = fingerlike sac that develops during sexual reproduction
Asci usually surrounded and protected by sterile hyphae → fruiting body or ascocarp
In cup fungi → ascocarps are cup-shaped
In morels, they are stalked and pitted
Haploid hyphae fuse to make diploid nucleus
Mitosis and then meiosis produces 8 ascospores
Spores are windblown
Sac Fungi – Yeasts
Term ‘yeasts’ = loosely applied to unicellular fungi, many of which are ascomycetes
Budding = common form of asexual reproduction
Sexual reproduction → results in the formation of asci and ascospores
When some yeasts ferment → they produce ethanol and carbon dioxide
Yeast essential ingredient in making bread, beer, wine
Club Fungi
Toadstools, mushrooms, bracket fungi, puffballs, stinkhorns
Some deadly poisonous → Amanita spp. spreading across North America
Plant diseases - smuts and rusts (parasitize cereal crops, often 2 hosts)
Mycelium composed of septate hyphae
Club Fungi – Reproduction
Usually reproduce sexually
Haploid hyphae fuse, forming a dikaryotic (n+n) mycelium
Dikaryotic mycelium forms fruiting bodies called basidiocarps
Contain club-shaped structures called basidia
Nuclear fusion followed by meiosis produces basidiospores (40 million/hr)
Humongous Fungus – World’s Largest Organism
Weight = 605 tons
Age = 2400 - 7200 years old
Size = spread over 2384 acres
Location = high elevation on a mountain in Oregon
Known as = honey mushroom, shoestring rot
Rhizomorphs take water and nutrients from tree roots, killing trees
Mycelium = network of hyphae that increases the surface area for nutrient absorption, allowing fungi to efficiently decompose and absorb nutrients from their environment
Mushroom Life Cycle
Mushroom = tightly packed hyphae whose walled-off ends become basidia
Poisonous Mushrooms
Death cap
Fly amanita
Webcaps
Etc.
Humans and Fungi
Black mold
Ringworm
Athletes foot
Dermatophytes
Nail fungus
Etc.
Some Drugs from Fungi
Penicillin and Amoxicillin → antibiotic
Streptomycin → antibiotic
Cyclosporin A → immunosuppresant
Cephalosporin → antibiotic
Griseofulvin → antifungal
Ergot alkaloids → circulation and neurotransmission
Chloesterol Lowering Agents (Mevinolin)
Lovastatin (mevacor)
Simvastatin (zocor)
Pravastatin (pravachol)
Atorvastatin (lipitor)
Symbiosis – Lichens
Symbiotic association between a fungus (up to 3-2019) and a cyanobacterium or green algae (25,000 spp.)
Specialized fungal hyphae penetrate photosynthetic symbiont
Transfer nutrients directly to the fungus
Possibly mutualistic, but fungal symbiont may be a parasite of photosynthetic symbiont
Photosynthetic symbiont independent
Fungal symbiont usually can’t grow alone
Lichens
3 morphological types:
Compact crustose lichens = seen on bare rocks or on tree bark
Fruticose lichens = shrub-like
Foliose lichens = leaf-like
Can live in areas of extreme conditions and contribute to soil formation
Sensitive indicators of air pollution – no roots, absorb
Glomeromycota – Mycorrhizae
Mutualistic relationships between soil fungi and the roots of most familiar plants (80-90%)
Give plant greater absorptive surface
Help plants acquire mineral nutrients in poor soil (P, Cu, Zn)
Hyphae may enter cortex of root, but not cytoplasm
Ectomycorrhizae form a mantle that is exterior to the root, and they grow between cell walls, coat root surface
Ex. oak, beech, pine, spruce trees
Endomycorrhizae penetrate only the cell walls, grow along plasma membrane
Ex. apple trees, coffee, legumes
Earliest fossil plants have mycorrhizae associated with them
Some sac and cup fungi also form mycorrhizae