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Chemoorganotroph
Organisms that get their energy and electrons by oxidizing organic chemical compounds (e.g. sugars, fats, proteins)
Metabolism
Consists of catabolism and anabolism
Catabolism
Precursor/metabolite generation
Substrate —> catabolic pathway —> ATP + NAD(P)H + building blocks
Leads to the production of 12 key precursors
Reducing power (NADH + NADPH)
ATP
Anabolism
Assembly
ATP + NAD(P)H + building blocks —> anabolic pathway —> C1H1.8O0.5N0.2 (make themselves)
Redox reactions
Explains the movement of electrons from donor to acceptor
NADH + H+ + ½ O2 —> H2O + NAD+ (E0 = 1.14 V)
Standard Reduction Potential
Ability to donate or accept electrons
More -E0 —> better electron donor
More +E0 —> better electron acceptor
Electron Bifurcation
Couples an energetically favorable reaction to an unfavorable one
Used to perform more niche reactions
Catabolic Diversity
There are several ways to obtain carbon, electrons, energy, etc
Not only from organic materials; can be from light, inorganic molecules, chemicals, CO2
Photolithoautotroph
Energy source = light
Electron source = inorganic e- donor
Carbon source = CO2
e.g. purple and green sulfur bacteria, cyanobacteria, diatoms
Photoorganoheterotroph
Energy source = light
Electron source = organic e- donor
Carbon source = organic carbon
e.g. purple nonsulfur bacteria, green nonsulfur bacteria
Chemolithoautotroph
Energy source = inorganic chemicals
Electron source = inorganic e- donor
Carbon source = CO2
e.g. sulfur-oxidizing bacteria, hydrogen-oxidizing bacteria, methanogens, nitrifying bacteria, iron-oxidizing bacteria
Chemolithoheterotroph
Energy source = inorganic chemicals
Electron source = inorganic e- donor
Carbon source = organic carbon
e.g. some sulfur-oxidizing bacteria
Chemoorganoheterotroph
Energy source = organic chemicals, often same as C source
Electron source = organic e- donor, often same as C source
Carbon source = organic carbon
e.g. most nonphotosynthetic microbes, including most pathogens, fungi, and many protists
Incoming reduced organic carbon serves 3 purposes: energy, electrons, and C for anabolism
Glucose
Excellent source of energy
Can donate up to 24 e-
Pathways to convert glucose —> PGALD to produce pyruvate
Glycolysis (Embden-Meyerhof-Parnas Pathway)
Pentose Phosphate Pathway (PPP)
Entner-Doudoroff Pathway (ED)
Glycolysis
2 key stages
6C Phase: Glucose (C6) —> split into 2 PGALD (C3); must invest 2 ATP
3C Phase: Oxidation of PGALD —> pyruvate
Substrate level phosphorylation
Contributes to anabolic pathways
Substrate level phosphorylation
Individually moving a phosphate from 1 molecule onto ADP
Inefficient
Pentose Phosphate Pathway
Can run parallel to glycolysis
Breaks down G6P to generate reducing equivalents + anabolic precursors (5-carbon sugars which are needed for DNA)
3 key stages:
Step 1: oxidation-decarboxylation of G6P
Step 2: isomerization of ribulose
Step 3: sugar rearrangement reactions
Contributes to anabolic pathways
Nucleic acid synthesis
Aromatic amino acid synthesis
Some organisms rely solely on this
Entner-Doudoroff Pathway
Alternative metabolic pathways to catabolize glucose —> pyruvate
Growth on aldonic acids aka sugar acids which can’t be used in glycolysis
Less enzyme requirements; advantageous in limited nutrient niches
Generates only 1 ATP + 1 NADH + 1 NADPH
Similar initial reactions EMP but more inefficient
Conversion of gluconate to KDGP leads to formation of 1 pyruvate + 1 PGALD
Only 1 ATP formed
Specific to prokaryotes
Some organisms rely solely on this
Direct production of NADPH
Disaccharides
Broken apart by hydrolysis or phosphorylation reactions
TCA Cycle
1 Acetyl-CoA oxidized —> 2 CO2 + 3 NADH + 1 FADH2 + 1 GTP
Pyruvate oxidized —> acetyl-CoA in a process called pyruvate dehydrogenase
Pre-req to TCA cycle
Net production of 1 NADH
Contributes to anabolic pathways (mostly produces reducing power)
ETC carriers
Works similarly between bacterium and eukaryotes
Quinones are the complexes embedded in the membrane
Differs from bacteria to bacteria (unlike eukarya which have the same set up every time)
Chemoorganotrophic fueling processes
Use reduced organic compounds for catabolic and anabolic processes
Processes used to catabolize energy source:
Respiration
Fermentation
Respiration
Involves use of the ETC (most of the time)
2 types:
Aerobic - TEA is oxygen
Anaeorbic - TEA is different oxidized molecule e.g. NO3-, SO42-, Fe3+
PMF is generated and used to synthesize ATP as e- pass through the ETC to the TEA
Electron Transport Chain
Electron carriers are membrane-bound
Bacteria don’t have a dedicated organelle for this
Gram +: PM
Gram -: IM
1st electron carrier has the most negative reduction potential and each successive carrier is slightly less negative
Reducing power
NAD+ - nicotinamide adenine dinucleotide
Reduced to NADH
NADP+ - nicotinamide adenine dinucleotide phosphate
Reduced to NADPH
FAD - flavin adenine dinucleotide
Redox active cofactor
FMN - flavin mononucleotide
Redox active cofactor
Electron carriers
Coenzyme Q (CoQ) - ubiquinone
Soluble lipid carrier
Tail group embedded in membrane
Head harvest e-
Cytochromes
Usually involves intermediates
Contains heme groups (ring-shaped to hold iron)
Ferredoxin & other non-heme iron proteins
Iron-sulfur cluster containing protein
Aerobic Respiration (eukaryotes)
NADH/FADH2 —> Complex I or II —> CoQ —> Complex III —> Cyt c —> Complex IV —> O2
Aerobic Respiration (bacteria)
Located in PM
Flexible - electron carriers can be replaced or different terminal oxidases may be used to respond to different environmental conditions
Branched - electrons may enter the chain at several points and leave through several terminal oxidases
>46 respiratory dehydrogenases to harvest e-
Why does E. coli use two different cytochrome oxidases?
Both utilize O2 as a TEA
1 is made/used when O2 is at high levels
The other when O2. is at low levels
Different affinities based on nutrient availability
Different efficiencies
Anaerobic Respiration
Uses electron acceptors other than oxygen
Generally yields less ATP than aerobic respiration because of a lower difference in standard reduction potentials
Denitrification
Reduction of nitrate to nitrogen gas
Important environmentally
Aerobic vs. Anaerobic Respiration
Similarities -
Organic substrate is oxidized (CH2O —> CO2)
Resulting NADH and FADH2 used to “kick off” the ETC
Still couples energetic favorability of moving electron to unfavorably pumping protons (PMF)
Differences -
O2 is not the TEA
SO4, NO3, Fe3+ are common TEA
Less energy is obtained because of lower difference between standard reduction potential (but as long as there is a difference they will use it)
Electron acceptors used in anaerobic respiration by E. coli + enteric bacteria
Electron acceptor: NO3-
Reduced products: NO2-
Electron acceptors used in anaerobic respiration by Paracoccus denitrificans + Pseudomonas
Electron acceptor: NO3-
Reduced products: NO2-, N2O, N2
Electron acceptors used in anaerobic respiration by methanogens
Electron acceptor: CO2
Reduced products: CH4
Electron acceptors used in anaerobic respiration by acetogens
Electron acceptor: CO2
Reduced products: acetate
Electron acceptors used in anaerobic respiration by Geobacter sulfurreducens
Electron acceptor: Fe3+
Reduced products: Fe2+
Shewanella oneidensis
Uses multiple electron acceptors
Steps to transfer electrons to TEA
An electron donor supplies electrons to the ETC in the membrane.
The electrons pass to a reductase, an enzyme that transfers electrons to the final acceptor.
The acceptor gains electrons and is reduced. The respiratory process helps create a proton gradient that powers ATP production.
Molybdopterin reductases
Molybdopterin cofactor
Reduce e- acceptors such as nitrate, DMSO
Flavin reductases
FAD or FMN cofactor
Reduce e- acceptors such as fumarate
Extracellular Electron Transfer
Process where microbes exchange electrons with solid materials outside the cell - such as metal oxides or artificial electrodes - to drive respiration or energy conservation
Extracellular Electron Transfer Methods
Direct Extracellular Electron Transfer
Redox protein: a protein on the cell surface transfers electrons to an acceptor touching the cell
Nanowire: a conductive structure carries electrons from the cell to an acceptor farther away
“e- tube”
lots of heme units
Indirect Extracellular Electron Transfer
Mediated electron transfer: mobile soluble carrier picks up electrons from the cell, carries them to the acceptor, and returns for more
Fermentation
Some bacteria cannot make an ETC, so they rely on fermentation to produce ATP
Microbes perform any sort of respiration first (if possible) until all alternative electron acceptors are depleted
Oxygen is not needed
ATP formed by substrate level phosphorylation
Max ATP yield = 4
Big problem of fermentation: how do you re-oxidize NADH without using the ETC?
Solution: dump electrons onto pyruvate produced by initial oxidation (pyruvate = electron sink)
Same input molecule serves as both the electron donor and acceptor
Die of starvation if NADH is not re-oxidized
Fermentation pathways
Named based on end product
Main fermentation pathways
Lactic acid (enteric bacteria)
Ethanol (yeast)
Acetate (enteric bacteria)
Ethanol (enteric bacteria)
Alcoholic fermentation
Pyruvate decarboxylated to acetalaldehyde —> reduced to ethanol by alcohol dehydrogenase
Homofermentative: homolactic fermenter
Only makes lactic acid (pyruvate —> lactate via lactate dehydrogenase)
Heterofermentative: heterolactic fermenter
Makes lactic acid and other byproducts e.g. ethanol and CO2
Mixed acid fermentation
Excretion of a mixture of acids (acetic, lactic, succinic, formic acids)
Pyruvate dehydrogenase is repressed
Pyruvate formate lyase is active
Pyruvate —> Acetyl-CoA + Formate
Gas is produced if the microbe makes formate hydrogen lyase
Formate —> CO2 + H2
2nd big problem of fermentation: acidification
Fermenters need to pump protons out to prevent internal acidification and make PMF for transport without an ETC
Solution: use an ATPase to pump protons into the environment
Biosynthetic issues of fermentation
The cell still needs TCA intermediates to build molecules, even though it cannot rely on that respiratory pathway to recycle NADH
The horseshoe TCA cycle is used to make building blocks for the cell
2 main branches:
Oxidative - Oxaloacetate → citrate → isocitrate → α-ketoglutarate
produce precursor for amino acids
Reductive - Oxaloacetate → malate → fumarate → succinate
consumes reducing power and supplies biosynthetic intermediates
Fermentation vs. Anaerobic Respiration

Energy generation (theoretical max)
Aerobic - 38
Anaerobic - 36 or less
Fermentation - 2
Binomial system
formal two-part scientific naming system used to identify living organisms
First capitalized, latinized names
Genus species
Escherichia coli
Pseudomonas aeruginosa
Write full name out first, then shorten
Carolus Linnaeus - formulated this system
Classification systems (past —> present)
Phenetic —> Phyolgenetic —> Genotypic
Phenetic was based on similarities and didn’t take into account evolution
Phylogenetic was based on evolution
Genotypic is based on genetic material
Classical characteristics for identification
Morphology
Biochemistry
Metabolism
Ecology
Genetic
Molecular
Carl Woese
Revealed that despite morphological similarities, archaea represented a totally distinct domain of life
His analysis relied instead on 16S rRNA (universal genes) analysis
Use of rRNA
Helps scientists identify organisms and determine evolutionary relationships
Bacteria and Archaea: 16S
Eukarya: 18S
Conserved regions: similar across many organisms, allowing primers to bind
Variable regions: differ among organisms, helping scientists distinguish them
27F and 1492R are universal primers that amplify the 16S gene in all branches of life
You need both on either side for PCR
A forward primer (27F) binds near one end
A reverse primer (1492R) binds near the other end, on the opposite DNA strand
The primers point toward each other, so DNA synthesis copies the region between them. Having both primers lets PCR repeatedly double that region
Archaea
Methanogens
Hyperthermophiles
Extreme halophiles
Mesophiles
Methanogens (euryarchaeota)
Use the Wolfe Cycle
Source of electrons —> CO2
What is the acceptor —> H2
Environmental conditions —> anaerobic
CO2 + 4H2 —> CH4 + 2H2O
In Methano-bacteriota, halobacteriota, and thermoplasmatatota
Halobacteriota (euryarchaeota)
Extreme halophilic archaea
Require at least 1.5M NaCl, optima at 3-4M
Thermoplasmas (euryarchaeota)
Plasmas lack cell walls
No peptidoglycan
Rely on extensive lipoglycans for membrane stability; some grow at pH 0-1
Thermoproteota
Pyrodictium spp.
Can survive the autoclave
Nanoarchaeota
Nanoarchaeum equitans - parasitic archaeon
Lives in hydrothermal vents associated with Ignicoccus hospitalis (thermoproteota)
Asgard Archaea
Closest clade to eukarya (new clade)
Non-proteobacterial Gram (-) bacteria
Hyperthermophiles
Aquificota
Thermogota
Photosynthetic bacteria
Chloroflexota
Chlorobiota
Cyanobacteria
Bizarre cell walls
Deinococcota
Unique morphologies
Spirochaetota
Cyanobacteria
Come in all shapes and sizes
Also known as blue-green algae
Predominantly photosynthetic
Deinococcus species
Weird envelope
Stain Gram + but have OM
No teichoic acid
Altered PL content
Highly resistant to radiation b/c of really good DNA repair mechanisms
Planctomycetes
Highly organized membrane systems
Some have membrane-bound organelles
Anammox (anaerobic ammonium oxidation) bacteria
Paryphoplasm: outermost peripheral compartment
Riboplasm: central compartment containing ribosomes + nucleoid
Anammoxosome: largest internal compartment dedicated to energy metabolism
Anammoxosome
Primary site for the anammox process, where ammonium (NH4+) and nitrite (NO2-) are converted directly into diatomic nitrogen gas (N2) and H2O

Spirochetes
Treponema
Borrelia
Spirochaeta
They are shaped the way they are because there are flagella all over the outside
“Corkscrew itself through environment”
Important member of gut biome
Bacteroides
Proteobacteria
One of the largest and most diverse phyla of Gram - bacteria
Vibrionaceace
Nitrifying bacteria
Photoheterotrophs
Enterobacteriaceae
Pseudomonadaceae
Rhizobiaceae
Caulobacteracaeae
Gammaproteobacteria
Largest bacterial class
Enterobacteriaceae
E. coli
Salmonella enteriditis
Pseudomonadaceae
Pseudomonas aeruginosa
Alphaproteobacteria
Rhizobiaceae
Caulobacteracaeae
Caulobacter (alphaproteobacteria)
Asymmetric cell division
Developmental cycle leads to different cell morphologies
Nitrobacter (alphaproteobacteria)
Nitrifying bacteria
Oxidize nitrite to nitrate
Agrobacterium (alphaproteobacteria)
Negative association with plants (invade plants and cause tumors)
Rhizobium (alphaproteobacteria)
Positive association with plants (invade leguminous plants to produce nitrogen-fixing root nodules)
Pelagibacterales (alphaproteobacteria)
SAR11 clade
Comprise 25-50% of all prokaryotic cells in the world’s oceans
Main driver of the marine carbon cycle
Never cultured in lab
Gram + Bacteria
Firmicutes
Low GC
Actinobacteria
High GC
Firmicutes
2 very important classes:
Clostridia
Clostridium spp.
Bacilli
Bacillus spp.
Staphylococcus spp.
Lactobacillus spp.
Streptococcus spp.
Actinobacteria
Present in gut microbiome
Bifidobacterium
Micrococcus
Propionibacterium
Pathogen
Mycobacterium
Mycobacterium tuberculosis = leading cause of death from a single infectious agent
Antibiotics
Streptomyces
Source of up to 80% of naturally occurring, clinically useful antiobiotics
Uncultivated clades
Many of them!
Know about them because of sequencing
Biogeochemical cycling
Sum of the microbial, physical, and chemical processes that drive the flow of elements
Abiotic processes
Nonliving (erosion, sedimentary rock)
e.g. phosphorus cycle
Biotic processes
Nutrient cycling
What determines microbial activity?
Redox potential
What products can you reduce and consume?
Determines available terminal electron acceptors for anaerobic respiration
Determines what reduced molecules are present for electron donors
Winogradsky column
Different microbes in each layer
Efficiency (energy yield) is highest at the top and decreases as you go down
Top = oxic (aerobic respiration)
Bottom = anoxic (anaerobic respiration)
Sergei Winogradsky discovered multiple types of lithotrophy involved in nutrient cycling
Elements important in Biogeochemical Cycling and their Redox States
Reduced Form: donates electrons
Methane: CH4
Ammonium: NH4+; organic N
Hydrogen sulfide: H2S; SH groups in organic matter
Ferrous iron: Fe2+
Phosphonates and phosphite: PO3-
Manganese ion: Mn2+; Manganous oxide: MnO
Oxidized Form: accepts electrons
Carbon dioxide: CO2
Nitrate: NO3-
Sulfate: SO42-
Ferric ion: Fe3+
Polyphosphate, phosphate: PO4-
Manganese dioxide: MnO2
Carbon cycle
Carbon is continuously transformed from one form to another
First plants and microbes fix CO2
CO2 is reduced to CH4
Methanogenesis
Wolfe Cycle
Archaea only, in extreme environment & guts
CO2 +4H2 —> CH4 + 2H2O
Also possible from acetate, methanol, and methylated contaminants
Methanotrophy
O2 required
Methanotrophic bacteria + archaea
Specific to methane
Methylotrophic bacteria + archaea
Using single C molecules as electron donor
Use methane as source of electrons and O2 as TEA
Anoxic alternatives:
One microbe: anaerobic methane oxidation coupled to dentrification- uses CH4 as e- donor to reduce nitrate
Two microbes: methanotrophic archaea + SO4- reducing bacteria do reverse methanogenesis
Degradation of organic matter
Influenced by several factors:
Oxidation-reduction potential
Availability of competing nutrients
Abiotic conditions
pH, temperature, O2, and osmic conditions
Microbial community present
Lignin (organic polymer found in wood and plants)
Microorganisms secrete hydrolytic enzymes that degrade lignin
Only contain carbon, hydrogen, oxygen
Microbes must acquire remaining nutrients
Often difficult because of concentration of nitrogen, phosphorus, and iron may be very low
The nutrient that is insufficient for maximal growth is said to be limiting
Liebig’s law of the minimum: doesn’t matter if you have everything else you need b/c something else may be limiting
Nitrogen cycle
Nitrogen exists in dynamic redox states from -3 to +5
Serve as electron donors or acceptors
Nitrogen fixation: reduction of inorganic N2 to organic form
Redox neutral —> reduced form
Performed by some bacteria and archaea
Can be carried out under both oxic and anoxic conditions
Product is ammonia NH3
Immediately incorporated into organic matter as amine
Nitrification: ammonium donates electrons (oxidized to nitrite/nitrate)
NH4+ —> NO2-
NO2- —> NO3-
Fate of NO3-
Assimilatory nitrate reduction: NO3- is reduced and incorporated into microbial and plant cell biomass
Dissimilatory nitrate reduction: when nitrate is fully reduced to N2, nitrogen is removed from ecosystem and returned to atmosphere
Denitrification
Anammox reaction
Anaerobic
NH4+ = electron donor
NO2- = TEA
Shortcut to produce N2 without having to cycle through nitrate
Well characterized genes associated with nitrogen fixation
nifHDK
Well characterized genes associated with denitrification
narG, nas
Well characterized genes associated with nitrite reduction
nirK