Lecture 2 Flashcards

(61 cards)

1
Q

What is an ecosystem, and what does microbial ecology study?

A

An ecosystem is a community of organisms and their natural environment.

Microbial ecology studies how microorganisms interact with each other and with their physical environment. It aims to:
1. Understand microbial biodiversity and community interactions.
2. Measure microbial activities in nature and their effects on ecosystem functions.

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2
Q

What components exist within an ecosystem?

A

Populations: All the individuals of one microbial species in a place

Guilds: Metabolically related organisms that use similar resources

Communities: Multiple populations / guilds interacting

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3
Q

What did M.W. Beijerinck say?

A

“Everything is everywhere, the environment selects”

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4
Q

What does “Everything is everywhere, the environment selects” mean?

A

Microbes disperse globally, but local environmental conditions (e.g., pH, temperature, nutrient levels) determine which organisms grow and dominate.

Ex. If a hot spring is 70C, only heat loving microbes will survive

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5
Q

What physicochemical factors influence microbial growth in nature?

A

Microbial growth requires:

Nutrients
Proper temperature
pH
Water activity (a_w)
Oxygen
Light
Pressure

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6
Q

What is a niche?

A

A niche is the functional role of an organism within a system — including:

  • Where it lives
  • What nutrients/resources it uses
  • When it uses them
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7
Q

What is a microenvironment, and why is it usually heterogeneous?

A

A microenvironment is the specific physical space where a microbe actually lives and metabolizes.

It is heterogeneous because conditions (nutrients, O₂, pH) change rapidly over micrometer scales, creating many micro‑niches supporting physiologically distinct groups.

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8
Q

What is meant by a “feast‑or‑famine” lifestyle in microbes?

A

Nutrients in nature enter ecosystems intermittently, so microbes often experience:

  • Short “feast” periods with abundant nutrients
  • Long “famine” periods with scarcity

To survive, microbes evolved storage polymers (e.g., PHB, glycogen) to store carbon/energy for starvation periods.

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9
Q

Why is exponential growth rare in natural environments?

A

Because:

  1. Nutrients are limited
  2. Nutrients are unevenly distributed
  3. Competition is intense

e.g.
E. coli t_gen ≈ 20 min in lab
E. coli t_gen ≈ 12 hours in the intestinal tract

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10
Q

Why are surfaces important for microbial growth?

A

Microbial growth is often optimal on surfaces because they provide:

  • Nutrient accumulation
  • Protection from flow/shear
  • Stability for attachment
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11
Q

What is a biofilm?

A

A biofilm is a community of microorganisms embedded in EPS (extracellular polymeric substances) attached to a surface.

Biofilms show strong cooperation, nutrient sharing, resistance to antimicrobials, and structured microenvironments.

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12
Q

What is a microbial mat, and how does it differ from a biofilm?

A

A microbial mat is a thick, layered, macroscopic community (e.g., hot springs, beaches).

It includes multiple trophic layers, strong vertical gradients, and extremely high microbial numbers and activity.

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13
Q

What are major consequences of biofilms (positive and negative)?

A

Problems:
- Colonize artificial implants
- Cause dental disease
- Reduce pipeline flow
- Lower water quality
- Increase corrosion rates

Useful roles:
- Biological filtration (water/wastewater)
- Microbial ore leaching
- Food fermentation

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14
Q

What is competition in microbial ecology?

A

Competition occurs when distinct microorganisms attempt to acquire the same limiting resource.

This is governed by the competitive exclusion principle — two species competing for the same resource cannot stably coexist.

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15
Q

What is antagonism?

A

A form of competition where one microbe inhibits another by releasing:

  • Specific inhibitors
  • Antibiotics
  • Toxic metabolites
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16
Q

What is syntrophy, and why does it occur?

A

Syntrophy is a cooperative interaction where two or more microorganisms work together to perform a transformation neither can carry out alone.

Characteristics:
- They share the same microenvironment

  • Often involves complementary metabolisms

Examples:
- Nitrification: NH₃ → NO₂⁻ (nitrosifiers) → NO₃⁻ (nitrifiers)

  • Sulfur coupling: SO₄²⁻ → H₂S (sulfate reducers); H₂S → S⁰ (sulfide oxidizers)
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17
Q

What are the major carbon reservoirs on Earth according to this lecture?

A
  • Sediments and rocks of the Earth’s crust (largest long‑term reservoir)
  • Humus (recalcitrant organic matter in soils)
  • Land plants (large, active organic C reservoir)
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18
Q

Define humus and explain its significance in the C cycle.

A

Humus is a complex mixture largely derived from resistant plant material and soil microorganisms; it is resistant to decomposition and thus slows carbon turnover, acting as a long‑lived soil carbon pool

Soil that is highly fertile is usually high in humus

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19
Q

How is the carbon cycle closely linked to the oxygen cycle?

A

CO₂ fixation during oxygenic photosynthesis produces O₂.

Respiration consumes O₂ and returns CO₂ to the atmosphere.

These opposing fluxes couple the C and O cycles.

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20
Q

Who performs oxygenic vs anoxygenic photosynthesis in this course?

A

Oxygenic phototrophs: Green plants, cyanobacteria, algae.

Anoxygenic phototrophs (anaerobic): Purple and green sulfur bacteria. [BI374 lect…2-26 post | PDF]

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21
Q

What are the two primary processes that create new organic carbon?

A
  1. Oxygenic photosynthesis (carried out by higher plants and microbes)
  2. Chemosynthesis: Autotrophic CO₂ fixation powered by chemical energy (not light).
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22
Q

What is the relationship between photosynthetic rate and respiration for biomass increase?

A

Net biomass increases only if photosynthetic CO₂ fixation rate is greater than the respiration rate (i.e., a net positive photosynthesis–respiration balance).

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23
Q

What are the dominant carbon end‑states produced during organic matter decomposition and why is their balance critical?

A
  • Carbon dioxide CO₂ (oxidized end‑state)
  • Methane CH₄ (reduced end‑state)

A proper balance between oxidative (CO₂‑forming) and reductive (CH₄‑forming) processes is critical for ecosystem stability and greenhouse gas fluxes.

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24
Q

Write the methanogenesis reaction and name the key enzyme.

A

CO2 + 4H2 -> CH4 + 2H2O

Catalyzed by methyl reductase within methanogenic pathways

Methanogenesis happens only in anaerobic environments

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25
Who are methanogens, what is notable about their substrate range, and which alternative substrate can some use?
Methanogens are a specialized group of archaea that produce methane. Many have a narrow substrate range and therefore depend on syntrophic partners to supply intermediates; some can use acetate (CH₃COOH) to produce CH₄.
26
List typical habitats where methanogenesis occurs.
Swamps, marshes, anoxic microsites in grasslands and forest soils, freshwater sediments, rumen of ruminants, and marine hydrothermal vents—all characterized by anoxia and adequate substrates.
27
Summarize syntrophic relationships driving anoxic carbon cycling (who does what).
Hydrolyzers: Break down polymers (e.g., cellulolytic bacteria). Primary fermenters: Convert monomers (e.g., glucose) into acetate + CO₂. Secondary fermenters: Produce H₂ (e.g., Syntrophomonas wolfei). Methanogens: Consume H₂ (and sometimes acetate), keeping H₂ low and pulling fermentations forward.
28
What organic compounds are not degraded anaerobically, and what process counters methane production under oxic conditions?
Not degraded anaerobically: Lignin and aliphatic saturated hydrocarbons. Counter‑process: Methane oxidation (CH₄ → CO₂) in the presence of O₂. [
29
Define methanotrophs vs methylotrophs and give an applied example.
Methanotrophs: Microbes that oxidize methane (CH₄) as a carbon/energy source. Methylotrophs: Microbes that utilize C₁ compounds (e.g., methane, methanol, methylamine) for carbon/energy.
30
How do greenhouse gases relate to microbial C cycling, and what human activity exacerbates the issue discussed in class?
CO₂ and CH₄ trap infrared heat (greenhouse effect), influencing climate. A contributing factor covered in class is the decrease in forested land that otherwise would fix CO₂ via photosynthesis, thereby altering the atmospheric C balance.
31
Why is nitrogen cycling fundamental in ecosystems?
Nitrogen cycling is critical because several key reactions—such as nitrogen fixation, nitrification, and denitrification—are carried out exclusively by prokaryotes, making microbes essential for converting nitrogen into biologically usable forms. Without nitrogen cycling the world wouldn't exist
32
List the major oxidation states of nitrogen relevant to the nitrogen cycle.
−3: Organic N (R–NH₂), ammonia (NH₃), ammonium (NH₄⁺) 0: Nitrogen gas (N₂) +1: Nitrous oxide (N₂O) +2: Nitric oxide (NO) +3: Nitrite (NO₂⁻) +4: Nitrogen dioxide (NO₂) +5: Nitrate (NO₃⁻)
32
Why is nitrogen required by living organisms?
Nitrogen is needed for synthesizing amino acids, proteins, nucleic acids, nucleotides, and coenzymes. The largest nitrogen reservoir is the atmosphere (N₂), but atmospheric N₂ is unusable unless fixed biologically.
33
Why is N₂ difficult to use biologically?
N₂ is a highly stable molecule with a triple bond, making it unusable by most organisms. Only a small group of nitrogen‑fixing prokaryotes can reduce N₂ to ammonia.
34
What is nitrification and what are its two steps?
Nitrification is an aerobic, chemolithotrophic process consisting of: 1. NH₄⁺ → NO₂⁻ by Nitrosomonas (ammonia‑oxidizers) 2. NO₂⁻ → NO₃⁻ by Nitrobacter (nitrite‑oxidizers) These microbes obtain energy by oxidizing ammonia or nitrite. It occurs in well‑drained soils with neutral pH.
35
Why is nitrate (NO₃⁻) important in soils?
Nitrate is: - Mobile in soil water - Readily absorbed by plants - The dominant form of plant‑available nitrogen Adding high‑protein materials (manure) enhances nitrification rates because they increase ammonia levels.
36
What is denitrification, and when does it occur?
Denitrification is the stepwise reduction of nitrate to nitrogen gas. Occurs under low‑oxygen (anoxic or hypoxic) conditions when microbes use NO₃⁻ as an alternative electron acceptor. Performed by facultative anaerobes (e.g., Pseudomonas, Paracoccus, Bacillus). It results in loss of available nitrogen from soils.
37
What is ammonification?
Ammonification is the microbial decomposition of organic nitrogen (R‑NH₂) into ammonia (NH₃) or ammonium (NH₄⁺). NH₄⁺ is stable under anoxic conditions; under oxic conditions it is assimilated Ammonification can be done on both sides (nitric. & denitri.)
38
What is nitrogen fixation? Provide the reaction and key enzyme.
Biological nitrogen fixation converts N₂ → NH₃: N2 + 8H + 8e -> 2NH3 + H2 Catalyzed by nitrogenase, which is composed of: - Dinitrogenase reductase (Fe‑protein) - Dinitrogenase (MoFe‑protein) Nitrogenase is extremely O₂‑sensitive.
39
What are the two major categories of nitrogen‑fixing organisms?
Nonsymbiotic (free‑living) fixers: - Azotobacter, cyanobacteria, Clostridium - Many possess mechanisms to protect nitrogenase from O₂ (e.g., slime layers, high respiration rates). Symbiotic fixers: - Rhizobium, Bradyrhizobium, Frankia - Form intimate associations with plants (particularly legumes).
40
How do symbiotic nitrogen‑fixing bacteria benefit plants?
They convert atmospheric N₂ into ammonia, a form plants can assimilate to build amino acids and proteins. This dramatically increases soil nitrogen and plant growth, especially in legumes.
41
Describe the sequence of events leading to root nodule formation.
1Recognition & attachment of bacteria to root hair 2. Invasion of root hair 3. Formation of an infection thread through which bacteria travel 4. Movement to main root cortex 5.Formation of bacteroids inside plant cells 6.Continued plant + bacterial division → mature root nodule
42
What are bacteroids?
Bacteroids are swollen, irregular, branched forms of bacteria inside plant cells. (result from rapid multiplication f bacteria) They are the nitrogen‑fixing form but cannot divide. Their environment is controlled by the plant to optimize N₂ fixation.
43
What is leghemoglobin, and what is its role?
Leghemoglobin is an O₂‑binding Fe‑protein found in functional nodules. Functions: - Maintains extremely low free O₂ (≈ 10,000:1 bound:free O₂ ratio) - Protects O₂‑sensitive nitrogenase - Ensures enough O₂ for bacterial respiration while shielding nitrogenase
44
What is a symbiosome?
A symbiosome consists of bacteroids enclosed by plant‑derived membrane. It is the functional compartment where: - N₂ fixation occurs (nitrogenase localized in bacteroids) - The plant supplies energy (ATP, carbon sources) After plant death, bacteria are released to the soil; dormant cells remain and can infect again.
45
What is the ecological impact of Rhizobium–legume symbiosis?
Produces a significant increase in soil nitrogen Helps maintain fertility in agricultural systems Is the basis for legume crop rotation to restore soil nitrogen without fertilizer
46
Why are sulfur transformations widespread in nature?
Sulfur transformations are widespread because sulfur reactions occur under both oxic and anoxic conditions, and the reaction can occur chemically and biologically. Major sulfur reservoirs are found in the oceans and in sulfate minerals of sediments and rocks.
47
What are the three major oxidation states of sulfur in natural biogeochemical cycling?
−2: Sulfide (H₂S) 0: Elemental sulfur (S⁰) +6: Sulfate (SO₄²⁻) "big three" everything in the sulfur cycle is moving between these three forms.
48
Describe biological sulfate reduction and the conditions that promote it
Biological sulfate reduction converts SO₄²⁻ → H₂S Carried out by sulfate‑reducing bacteria (SRB), which are widespread but active only where sulphate is present. More H₂S is produced when electron donors are high
49
How is H₂S and S⁰ oxidized, and what role does light sometimes play?
H₂S oxidation occurs in oxic/anoxic zones by sulfur‑oxidizing bacteria. In illuminated, anoxic environments, anoxygenic phototrophic sulfur bacteria can oxidize H₂S using light as the energy source. S⁰ oxidation to SO₄²⁻ by sulfur‑oxidizing bacteria (e.g., Thiobacillus spp.) produces H⁺, lowering pH. (oxic)
50
What happens to pH during elemental sulfur (S⁰) oxidation, and why?
Oxidation of S⁰ → SO₄²⁻ releases H⁺, causing the environment to become acidic. (pH drops)
51
Give an example of anaerobic reduction of S⁰ and the type of organism involved.
Hyperthermophilic archaea can anaerobically reduce elemental sulfur (S⁰) to produce H₂S under anoxic conditions.
52
What is an example of an organic sulfur compound, and what are its ecological roles?
Example: Dimethyl sulfide DMS is abundant in marine environments and may be used by microbes as: - A substrate for growth - A component in CO₂ fixation pathways of certain bacteria
53
What are the major oxidation states of iron in nature, and why is the iron cycle important?
Iron cycles mainly between: - Fe²⁺ (ferrous, reduced) - Fe³⁺ (ferric, oxidized) These transformations occur in both oxic and anoxic environments and influence nutrient availability, metal mobility, and microbial respiration.
54
What is biological Fe(III) reduction and where does it occur?
Biological Fe³⁺ reduction occurs in anoxic environments, where microbes use Fe³⁺ as a terminal electron acceptor, reducing it to Fe²⁺.
55
Describe Fe²⁺ oxidation at neutral pH and what environmental interface supports it.
At neutral pH: Fe2+ + 1/4O2 + 2(1/2)H2O → Fe(OH)3 (s) +2H+ Fe‑oxidizing bacteria perform this reaction at oxygen–ferrous iron interfaces, commonly in sediments and groundwater seeps.
56
Which bacteria oxidize Fe²⁺ at low pH, and why is Fe²⁺ more stable there?
At low pH, Fe²⁺ remains soluble and is oxidized by: - Thiobacillus ferrooxidans (strict acidophile) - Leptospirillum ferrooxidans Fe²⁺ is more stable in acidic environments because precipitation as Fe(OH)₃ does not occur readily.
57
What is pyrite (FeS₂) and why is it important in the iron cycle?
Pyrite is iron disulfide, one of the most common iron minerals in coal and ore bodies. Its oxidation is central to acid mine drainage and microbial metal mobilization.
58
What is “yellow boy,” and what makes acid mine drainage toxic?
Yellow boy = jarosite, HFe₃(SO₄)₂(OH)₆, a yellow precipitate typical of AMD sites. AMD toxicity results from extremely low pH and high concentrations of dissolved metals, both lethal to aquatic life and harmful to water quality.
59
What is microbial leaching (bioleaching), and when is it used?
Microbial leaching is the extraction of metals from ores using acid‑producing, metal‑solubilizing bacteria. It is used when metal concentrations are too low for economically feasible chemical extraction, especially in ores that are easily oxidized.
60
What reaction maintains the leaching process?
The key sustaining reaction is the biological oxidation of Fe²⁺ → Fe³⁺ by Thiobacillus ferrooxidans