Introduction to Environmental Microbiology Flashcards
Anthropogenic environments?
Bioreactors, water treatment plants, waste ponds, houses…
Explain how typhoid fever and cholers led to microbiology.
At turn of 20th century the incidence of typhoid fever and
cholera were high
• tools were needed to protect public health
• disinfection and filtrations systems were develope
Old school microbiology? New?
Water Food Pollution safety safety and
bioremediation
The study of microbial fate and activity within all habitiats and the resulting impact on human health and welfare
Whats biogeochemistry?
The study of biological controls on the chemistry of the environment and geochemical regulation of ecological structure and function.
How is biogeochemist important?
Microbes play critical roles in energy transformations and biogeochemical
processes that result in the recycling of elements to living systems
What are 5 traits that make MO’s particularly good geochemical agents? Explain why for each.
- Rapid growth and cell division
• many individuals on which natural selection can act; take advantage of environments - Metabolic diversity- able to do many things
- Infallible
• have ability to go dormant in env where they won’t grow well - ubiquitous
• wide range of tolerance to various environmental conditions - Alter environment as a byproduct of metabolic activity
• O2 rich atmosphere a direct result of microbial metabolic activity
What were the first organism to perform metabolism? Seconds?
-Obligate heterotrophs – small organic molecules (CH3COOH) converted to CO2 and CH4
-S-based photosynthesis…
CO2 + 2H2S → CH2O + 2S +H2O
sunlight
- O2- producing photosynthesis… sunlight
CO2 + H2O → CH2O + O2
Whats the 1’ objective for MOs?
Survival, maintenance, generation of ATP, and sporadic growth - DIVIDE
3 microbe evolutions that changed atm?
methane spewing bacteria, O2 evolving microbes, N2 fixing microbes, and decomposition
What was the great dying?
90% of species on earth died from volcanos and methane spewing bacteria.
What was the single most significant effect of life on Earth’s geochemistry
Formation of O2 rich atmosphere
What was the great oxidation event?
-Was the biologically induced appearance of dioxygen (O2) in Earth’s atmosphere
GOE
Stage 1 of the GOE
- reducing atmosphere
- no production of O2
- prior to GOE- reducing env- mainly methane and H2
Stage 2 of the GOE
- Production of O2 by cyanobacteria
- absorption in oceans and seabed rock
- O2 oxidized iron to iron oxide in oceans and seabeds (absorbed)
- All O2 that cyano producing oxidized iron and turned into rust
Stage 3 of the GOE
- Outgassing of O2 from oceans -Absorption in lithosphere (earths crust)
- Eventually sink (amount of iron to be oxidized depleted)
Stage 4 and 5 of the GOE
-Oxidation of methane to CO2 and water= sink
-Evolution of new aerobic life forms
-Oxidative processes in all geospheres
End- Large O2 accumulation
-Once O2 was in a steady state- new aerobic life forms
-O2 source was > sinks
-Now- Source= sinks
Why did it take so long for o2 to build up in the GOE?
-Rate of O2 generation must be more than that of injection
of reduced gases by volcanoes
-Material on seafloor removes O2 from water and atmosphere, but if it is buried, it is not decomposed- O2 can’t be accessed
- Sudden buildup in burial rates allowed O2 to accumulate in atmosphere
How did nitrate help O2?
Resulted in rapid proliferation of O2- greater source
Whats the nickel famine?
- Methanogens need a lot of nickel
- 2.7 bill years old- reduced nickel
- methanogens decreases-sink decreases= O2 buildup
How was the P reserve changes? When?
So phytoplankton could use more
During the GOE
What did the presence of O2 allow for? How is the energy obtained?
- The development variety of other metabolic pathways
- Metabolic energy is obtained from flow of electrons between oxidized or reduced states