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Evolution & Taxonomy

QuestionAnswer
Microbiome: The community of microorganisms—bacteria, fungi, viruses, and others—and their genes living in a specific environment, including their interactions and activities.
Three Key Concepts for Understanding the Microbe: evolution, diversity, and ecology.
Evolution: how did life get started on Earth? How does life change and diversify over time?
Diversity: phylogenetic diversity-evolutionary relationships, metabolic diversity-cellular processes, ecological diversity-microbial interactions.
Ecology: interactions among organisms, interactions between organisms and their environment.
Three Grand “Flows” in Microbiology: information flow, energy flow, and carbon flow.
Information Flow (Fidelity vs. Mutation): Genetics: Information passes from parent cells to daughter cells. Evolution: Information passes from ancestral species to descendant species
Energy Flow (Electron transfer): Electrons flow from donors to acceptors. Results in ATP production. Generates reducing power (NADH, NADPH)
Carbon Flow: Inorganic carbon → organic carbon (carbon fixation). Organic carbon → organic carbon (metabolism, biosynthesis). Organic carbon → inorganic carbon (respiration, mineralization).
The Bacterial Perspective (Scale): 500 bacteria can fit in the space of a single period (.) 2mm for bacteria = 2km for humans (1000× scale difference).
Remarkable Capabilities of Bacteria: they can sprint 50–60 body lengths per second, swim through water as if it were honey, use molecular motors strong enough to pack DNA into viral capsids, and possess such high relative strength that, if scaled to human size, they could lift an airliner.
Early Evidence of Life: The Earth is 4.5 billion years old, liquid water — which is required for life — first appeared 4.3 billion years ago, fossilized remains from 3.45-3.86 billion years ago can be found in rocks.
Microfossils: Evidence of ancient microorganisms. 3.45-billion-year-old rocks from Barberton, South Africa, show bacterial structures. 1-billion-year-old microfossils from central Australia include primitive filamentous cyanobacteria and green algae.
Stromatolites: Ancient (3.5 billion years old) and relatively recent (1.6 billion years old) examples exist. Layered structures created by microbial mat communities.
Isotope Fractionation: Organisms preferentially use light isotopes (e.g., ¹²C over ¹³C), creating distinct isotopic signatures. Carbon isotope patterns can indicate past biological activity, preserved in ancient plants and petroleum deposits.
Oldest Evidence of Life (Hematite Tubes): Hematite tubes and filaments discovered in the Nuvvuagittuq rocks of Canada (reported in 2017) may represent some of the oldest signs of life.
Hematite Tubes & Biological Origins: Tubes and filaments in Nuvvuagittuq rocks resemble iron-feeding vent bacteria. Their attachment structures and organic carbon suggest a biological origin, unlikely to form without life.
Advantages for Hydrothermal Vents as the Site for Life's Origin: Vents provide stable, UV-protected environments with chemical energy from H₂ and H₂S. Their geochemistry forms prebiotic molecules, and mineral structures concentrate molecules, stabilize reactions, and conserve energy, supporting life’s emergence.
Hydrothermal Mounds: Mineral pores concentrate nutrient-rich fluids, enabling abiotic biomolecule formation, energy-coupled reactions, and replication, eventually leading to lipid membranes and the first cells.
Evidence that RNA Came First: Backbone of ATP, NADH, CoA Binds nucleotides & amino acids Catalytic activity (ribozymes) Self-replication Supports protein synthesis and gene regulation
Transition from RNA to Cellular Life: Proteins eventually replaced RNA as primary catalysts (more efficient). DNA replaced RNA as the genome (more stable for long-term storage).
Earliest cells probably had: — DNA (genetic storage) — RNA (intermediary) — Proteins (catalysts and structures) — Membrane systems for energy conservation
Last Universal Common Ancestor (LUCA): LUCA, the first cellular organism, existed 3.7-3.8 billion years ago, then Bacteria and Archaea diverged.
Metabolic Evolution After LUCA: LUCA used chemolithotrophy for energy from inorganic compounds. Later, organisms evolved heterotrophy, phototrophy (oxygenic photosynthesis), and respiration, shifting from anaerobic to aerobic metabolism.
Horizontal Gene Transfer (HGT): Genetic material transferred between organisms (not just parent to offspring). Major force in early evolution. Continues to drive microbial evolution today.
Prebiotic Chemistry: Composed mostly of biological building blocks (amino acids, nucleosides, and sugars).
Precellular Life: Started with the RNA world (catalytic and self-replicating RNA), then protein synthesis (RNA-templated translation), DNA (replication & transcription).
Early Cellular Life Composition (Right Before LUCA): composed of lipid bilayers, early cells likely had high rates of HGT.
Evolutionary Diversification (Right After LUCA): divergence of bacteria and archaea, components of DNA replication, transcription, and translation all in one place.
Genetic Chimera: Modern eukaryotic cells contain both bacterial and archaeal genes. Evidence of endosymbiotic origins.
LUCA Structural Characteristics: distinctly eukaryotic features, such as a nucleus, mitochondria (respiring O₂), various organelles, cytoskeleton, spliceosomal machinery, introns.
LUCA Gene Percentages: — >70% of genes are uniquely eukaryotic — ~2/3 of shared genes come from Bacteria (mostly metabolic functions) — ~1/3 of shared genes come from Archaea (mostly information processing)
Endosymbiotic Theory: Eukaryotic cells originated when one prokaryote engulfed another, and the engulfed cell became a mitochondrion or chloroplast, providing energy or photosynthesis capabilities.
Endosymbiosis Evidence: Mitochondria and chloroplasts resemble bacteria in size, replicate independently, have circular genomes, bacterial-type ribosomes and 16S rRNA, are antibiotic-sensitive, and the nucleus contains genes derived from them.
Serial Endosymbiosis Hypothesis (Slide 33): Eukaryotic cells evolved through multiple, separate endosymbiotic events, with the nucleus forming first, then mitochondria, and later chloroplasts in plant lineages.
Symbiogenesis Hypothesis (Slide 33): Eukaryotic complexity evolved because of an early endosymbiosis between an archaeal host and the mitochondrial ancestor, with the nucleus forming afterward; chloroplasts were acquired later in plants.
Carl Woese’s Universal Tree of Life: Carl Woese used DNA and RNA sequence comparisons—"living fossils" acting as molecular clocks—to construct the first universal tree of life. This work revealed the domain Archaea.
Small Subunit rRNA (SSU rRNA) as a Molecular Chronometer: SSU rRNA—16S in Bacteria/Archaea, 18S in Eukaryotes—traces evolution because it is universal, functionally conserved, slowly evolving, and contains both conserved and variable regions, allowing easy sequencing and comparison across organisms.
Small Subunit rRNA Gene Organization (Slide 37): The SSU rRNA gene is part of an rRNA operon with 23S and 5S rRNAs and tRNAs. Transcribed as a single long RNA with spacers, which are removed during processing to produce mature rRNAs for ribosome assembly.
According to SSU rRNA comparative analysis, the three domains of life are: bacteria, archaea, and eukaryotes.
Supporting Evidence from Genomics for Three Domains of Life: Comparative SSU rRNA analysis revealed that all life falls into three domains with genomic evidence showing that 60+ core genes for transcription, translation, and DNA replication were inherited from a universal ancestor.
Key Relationships Between the Three Domains: Eukaryotic and Archaeal genes share more similarity, Bacteria and Archaea likely diverged before Eukarya existed.
Timeline of Divergence: Bacteria and Archaea likely split around 3.7 billion years ago, while Eukarya branched from within Archaea between roughly 1.5–2.7 billion years ago; after these splits, each lineage developed and fixed its own defining traits.
Systematics: Study of diversity of organisms and their relationships. Links phylogeny with taxonomy. Characterizes, names, and classifies organisms
The Polyphasic Approach to Taxonomy (Three Integrated Methods): phenotypic analysis, genotypic analysis, and phylogenetic analysis.
Phenotypic analysis: Morphological characteristics, Metabolic capabilities, Physiological properties, Chemical characteristics.
Genotypic analysis: Genome composition, DNA sequences, Genetic markers.
Phylogenetic analysis: Evolutionary relationships, Based on molecular data
Phylogeny: evolutionary history of related DNA sequences.
Phylogenetic Trees: Diagrams showing evolutionary history by comparing DNA sequences. The number of mutations between homologous genes indicates how long ago organisms shared a common ancestor, helping infer relationships among Bacteria, Archaea, and Eukarya.
Building Phylogenetic Trees – Methodology: PCR: Amplify 16S rRNA gene. Clone & Sequence: Obtain sequences. Alignment: Identify homologous positions. Tree Construction: Calculate distances and build the tree.
Homology: Inheritance from a common ancestor, Phylogenetic analysis requires homologous sequences
Sequence Similarity: Percentage of nucleotides shared between sequences, Can be used to infer homology, Can be calculated regardless of function or ancestry
Orthologs (Types of Homologous Genes): Have the same function, Originate from a single ancestral gene in a common ancestor, Result from speciation events, Phylogenetic analyses typically focus on orthologs
Paralogs (Types of Homologous Genes): Have evolved different functions, Result from gene duplication within a genome, Can complicate phylogenetic analysis
Making a Phylogenetic Tree Yourself (Slide 46): the first step to making a tree is to align sequences. Then, a distance matrix is calculated from the number of sequence differences. Finally, the tree is constructed by adding nodes to join lineages that have the fewest differences.
Genomic Evolution: evolution is the accumulation of DNA sequence changes over time, an increase in genetic diversity of time. The flow of genetic information from old species to new species.
Evolution & Alleles: an allele is a sequence variant of a given gene. Alleles are different versions of the same gene. Evolution is a change in allele frequencies in a population over time.
What causes evolution: Random DNA changes and selection.
The Evolution of Interdependence in Microbial Communities: initially, all cells can make all products. Genes with redundant functions are lost over time. Individual cells are dependent on functions provided by the community.
Horizontal Gene Transfer (HGT) The transfer of DNA between organisms outside of parent-to-offspring inheritance. Allows genes to move between distantly related species, significantly impacting microbial evolution by enabling rapid acquisition of new traits.
Recombination in HGT The process where donor DNA is passed to a recipient cell and becomes integrated into the recipient's genome. Unlike sexual recombination, HGT is unidirectional, involves small amounts of DNA, and can occur across species boundaries.
Transformation A mechanism of HGT where bacteria take up free DNA directly from their environment and incorporate it into their genome.
Transduction A mechanism of HGT where viruses transfer bacterial DNA from one cell to another during viral infection.
Conjugation A mechanism of HGT where bacteria transfer DNA directly to another cell through physical contact, typically via a connecting tube-like structure.
Vertical Gene Transfer Traditional inheritance where genetic material passes from parent to offspring during reproduction and cell division.
Comparative Genomics use whole genome sequencing technologies to analyze gene content and DNA sequence composition differences between genomes.
A Species Genome Has Two Parts: core genome and pan genome.
Core Genome The set of genes shared by all strains of a species. Represents the essential genetic toolkit common to every member of that species. Remains relatively constant in size as more genomes are analyzed.
Pan Genome The full gene set of a species, including the core genome and genes present in only some strains. It expands as more strains are sequenced due to horizontal gene transfer.
Strain Variation Strains of the same species can differ in genome size, gene content, and traits due to pan-genome genes outside the core. This variation comes from gene acquisition from other organisms.
Salmonella enterica Pan Genome: Contains 2,811 core genes shared by all strains, plus 29–504 strain-specific genes, showing high genetic diversity that gives strains distinct traits and capabilities.
Microbial Systematics names and classifies microorganisms, describes traits, and investigates histories.
Nomenclature (naming): follows a binomial system in which species are given descriptive genus names and species epithets.
Taxonomy: classifies organisms into groups based on similarity.
Allochromatium warmingii Classification: A purple sulfur bacterium identified through taxonomic levels using characteristics like bacterial cell structure, Gram-negative staining, phototrophic pigments, internal sulfur globule storage, rod shape, and specific cell size/rRNA sequences.
Microbial Species: A taxonomic group that is monophyletic, genomically coherent (~5–6% ANI), phenotypically coherent, and distinct from other species, identified using a polyphasic approach combining multiple methods.
Polyphasic Approach A classification method that uses multiple combined techniques (genetic, phenotypic, and other analyses) to identify, describe, and name prokaryotic species.
Phenotypic Analysis: Examines observable traits to differentiate microbial species. Traits are compared to known phenotypes for identification or clinical diagnostics, though they can vary with growth conditions.
Morphological Characteristics (Phenotypic Characteristics of Taxonomic Value): Structural features like colony shape, Gram reaction, cell size/shape, flagellation, spores, inclusion bodies, capsules, and appendages.
Motility Characteristics (Phenotypic Characteristics of Taxonomic Value): Movement types including nonmotile, gliding, swimming (flagellar), swarming, and gas vesicle motility.
Metabolic Characteristics (Phenotypic Characteristics of Taxonomic Value): Energy mechanisms (phototroph, chemotroph) and utilization of carbon, nitrogen, sulfur compounds, plus fermentation and nitrogen fixation.
Physiological Characteristics (Phenotypic Characteristics of Taxonomic Value): Growth conditions including temperature, pH, salt ranges, oxygen response, and enzyme production.
Cell Lipid Chemistry (Phenotypic Characteristics of Taxonomic Value): Fatty acid composition, polar lipids, and respiratory quinones.
Cell Wall Chemistry (Phenotypic Characteristics of Taxonomic Value): Peptidoglycan presence/absence, amino acid composition, and cross-link structures.
Other Taxonomic Traits (Phenotypic Characteristics of Taxonomic Value): Pigments, luminescence, antibiotic sensitivity, serotype, and unique compound production.
Requirements for New Species: A new strain must be shown to be different from existing species, described in detail, named properly, published in a peer-reviewed journal, and deposited in at least two international culture collections.
Prokaryotic Code: All new species must follow the International Code of Nomenclature of Prokaryotes, which sets the rules for naming and validating new taxa. Most new taxa are described in the Internal Journal of Systematic and Evolutionary Microbiology.
Provisional Taxonomic Name: if an organism is well-characterized but not yet cultured, a provisional taxonomic name with Candidatus can be used (e.g., Candidatus Pelagibacter ubique).
Bergey's Manual of Systematics of Archaea and Bacteria: The most widely accepted classification system for prokaryotes, providing concepts and detailed information on bacterial and archaeal biology. Primary resource for characterizing new organisms.
The Prokaryotes: A second major online resource offering concepts and details of bacterial and archaeal biology, used alongside Bergey's Manual for characterizing new organisms.
How many Bacteria and Archaea species are there? Although about 14,000 bacterial and archaeal species are formally named, 3.3 million SSU rRNA sequences in databases suggest over 225,000+ OTUs (species-like units). The true number of prokaryotic species is unknown.
Created by: smurtab
 

 



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