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the use of microorganisms to produce commercially desired products or to perform commercially desired transformations
-this may involve natural products made by wild-type microorganisms
-this may involve new, non natural products produced by genetically modified microorganisms
major products of industrial microbiology
-industrial and agricultural products
-food additives
-products for human and animal health (antibiotics and medicines)
-biofuels
types of microbial products
primary metabolites, secondary metabolites, and other microbial products
primary metabolites
-Substances synthesized by microbial cells during exponential growth phase
-Include amino acids, nucleotides, fermentation end products, and enzymes
secondary metabolities
-Primarily made during stationary phase
-Include many antibiotics and mycotoxins
other microbial products
-Antibiotics and other medical products
-Industrial and agricultural products
-Food additives: amino acids, other
-Products for human and animal health
-Biofuels: i.e., ethanol
-Cells: i.e., yeast cells for baking
Commercial food, alcohol, and fermentation processes
-Fermentation of milk: Yogurt, cheese, buttermilk, sour cream
-Fermentation of fruits and vegetables: Pickles, cabbage
-Baking
-Brewing
-Major fermentations used are lactic, propionic, and alcoholic fermentations
Example of microbial food processes fermented milks
rely on lactic acid bacteria
Example of microbial food processes cheese production
classified based on texture, hardness
Example of microbial food processes wine
Glucose fermented to ethanol and CO₂ by S. cerevisiae or S. liposideus
Example of microbial food processes production of breads
growth of S. cerevisiae under aerobic conditions
Genetic manipulation of microorganisms
-Used to produce microorganisms with new and desirable characteristics
-Classical methods of genetic exchange coupled with recombinant DNA technology play vital role in industrial microbiology
Role of microorganisms in genetic engineering
-Nearly all techniques & materials for genetic engineering, cloning, etc. are from microorganisms
genetic engineering
modification of organism's genetic information by directly changing the sequence of nucleic acids in its genome
recombinant DNA technology
procedures used to carry out genetic engineering
recombinant DNA
DNA molecule composed of DNA from 2 different sources
restriction enzymes
-Prokaryote enzymes that recognize and bind specific sequences in DNA called recognition sites
-May produce sticky ends or blunt ends
how do restriction enzymes work?
-Cleave DNA at this site or a defined distance from it in any DNA from any source
-Can combine DNA from 2 sources cut with same enzyme into 1 molecule
first recombinant molecule
-1982
-Produced new source of human insulin
-First commercial use for recombinant molecules
growing microbes in industrial settings requires
precise control of agitation, temperature, pH changes, and oxygenation
growing microbes in industrial settings occurs
in large vessels called fermentors
fermentation
any aerobic or anaerobic metabolism occurring in a fermenter for mass culture of microorganisms
-most processes are aerobic
continuous culture
continual addition of a critical nutrient prevents accumulation of undesirable metabolic waste products
microorganisms & ecosystems
-Microorganisms account for ~50% of all biomass on Earth
-They are ubiquitous (found all over) on the surface and deep within the earth and in water
-Many microorganisms are free living; others in symbiotic associations
freshwater environments
-highly variable in the resources and conditions available for microbial growth
-Water available in excess
-Oxygen, nutrients, light, temperature more variable
-Solute concentration ~0.9%
marine (salt water) environments
-Open ocean environment is saline (salty and hypertonic - 3-4%)
-Low nutrient, especially nitrogen, phosphorus, and iron
-Cooler
-Microbial activities major factors in Earth's carbon balance
zones in lakes & ponds
photic zone, freshwater upper layer (photic zone), lower layers, and lake zones
photic zone
-The water from the surface to depth to which light penetrates
-Photosynthesis can occur
Freshwater upper layer (photic zone)
-Many phytoplankton
-Oxygenic photolithoautotrophs suspended freely in water
-Includes algae and cyanobacteria
-Also protozoa and some prokaryotes
Lower layers - Profundal and Benthic
-Benthic species: microorganisms attached to bottom or sides
-Mostly anaerobic and facultative anaerobic chemoorganoheterotrophic bacteria and chemolithoautotrophs
-The activity of chemoheterotrophic microbes dependent upon primary producers
Lake zones
Benthic - bottom and sides below profundal level
Profundal zone - anoxic in deep lakes
Littoral and limnetic zone are in photic zone
Important physical factors determining which microorganisms can live in different environments
-Dissolved oxygen content: defines where strict aerobes/anaerobes reside
-CO₂: for photolithoautotrophs
-Temperature
-pH
-Light penetration: for photolithoautotrophs and chemolithoautotrophs
dissolved oxygen
-Oxygen diffuses from atmosphere
-Produced by aquatic photoautotrophs
-Varies with depth and temperature
-Decreases with depth
-Decreases with colder temperatures
nutrients
-Microbial species richness and abundance is a function of kinds and amounts of nutrients
-Phytoplankton are major source of organic matter
freshwater organisms
-Phytoplankton: oxygenic photolithoautotrophs
-Protozoa
-Prokaryotes
-Anaerobic and facultative anaerobic -chemoorganoheterotrophic bacteria
-Chemolithoautotrophs
marine (saltwater) organisms
-Photosynthetic microbes fix ~half the world's carbon
-Virioplankton are the most numerous members
-Phage particles are the most abundant life form on Earth
-Halotolerant microbes where freshwater meets saltwater
-Microbes in nearshore waters due to higher nutrient levels
Hydrothermal Vent Microbial Ecosystems
-Deep-sea hot springs (hydrothermal vents) support thriving animal communities
-Fueled by chemolithoautotrophic prokaryotes
Benthic marine environments
-Largest microbial biomass under the sea
-Subsurface equals that of all terrestrial and marine plants
-Some microbes are barophilic and able to tolerate atmospheric pressures up to 1,100 atm
Habitats where microorganisms reside
-Marine environments
-Freshwater environments
-Soil
Soils as a Microbial Habitat
complex and contains a large variety of habitats as a result
-microbial diversity in soils is greater than any other habitat (supported by complex physical & chemical environments)
most important factor in influencing microbial activity in surface soils
the availability of water
most important factor in influencing microbial activity subsurface environments
nutrient availability
Soil particles pore space
critical for movement of water and gases optimum environment for microbial growth
soil composition
Soils are mixtures composed of:
-composed of inorganic mineral matter (~40% of soil volume)
-organic matter (~5%) from decomposition and waste production
-air and water (~50%)
-living organisms including animals, plants, fungi, prokaryotes
-few algae or protozoa
In soils, fungi and prokaryotes are the most numerous microorganisms
-many fungi
-many prokaryotes (chemoheterotrophs & chemolithotrophs)
soil profile
-Soil is the loose outer material of Earth's surface.
-Consists of four distinct layers: O horizon, A horizon, B horizon, and C horizon
O horizon
at the surface, with undecomposed plant material
A horizon
with most microbial growth, rich in organic material and nutrients
B horizon
the subsoil where organic material leached from the A horizon gathers, little microbial activity
C horizon
the base that is directly above the bedrock and forms from the bedrock
location of microbial growth
-Most microbial growth takes place on the surfaces of soil particles
-Soil aggregates can contain many different microenvironments supporting the growth of several types of microbes
categories of soil
mineral soil and organic soil
mineral soil
from weathering of rock contains less than 20% organic carbon; most of Earth's soils are in this category.
organic soil
in bogs and marshes possesses at least 20% organic carbon
Bacteria, archaea, fungi, and protozoa use
different functional strategies to take advantage of the complex physical matrix in soi
Soil archaea
are on surfaces of soil particles
soil prokaryotes of domain Bacteria
are on surfaces within smaller soil pores
Terrestrial filamentous fungi
bridge open areas between soil particles
large numbers of terrestrial mo's in soil
only a very small fraction of them can be cultured
Soil populations play roles in
biogeochemical cycling and the carbon, nitrogen, sulfur, iron, and manganese cycles.
Molecular techniques used to help understand
the complex ecosystems found in soil environment
productivity of terrestrial mo's differs from
those operating in photic zone of the open ocean.
Plants rather than microbes
account for most primary production in terrestrial environments
microorganisms play a role in
recycling the organic matter
microbes commensalistic or mutualistic relationships with plants is...
-the major source of terrestrial primary production
-in some, the microbe is a plant pathogen and harms the host
-in all, here is a molecular signaling between the plant and microorganism for two-way communication
phyllosphere
refers to the aerial (above-group) surfaces of a plant
Phyllosphere Microorganisms
-SSU rRNA analysis shows millions of new bacteria yet to be discovered.
-Now know it can support a diverse microbial community.
Rhizosphere
volume of soil around the root influenced by materials released from root
Rhizoplane
surface of root
Plant roots receive between
30% to 60% of the net photosynthesized carbon and ~40% to 90% enters the soil
mycorrhizae
-Mutualistic fungus-plant associations
-mycorrhizal fungi colonize plant roots
-Are not saprophytic; instead use photosynthetically derived carbohydrate provided by host
-Provide enhanced nutrient uptake for plant
nitrogen fixation
-Occurs in soil as a result of a symbiotic relationship between bacteria and plants
-Results in the enzymatic conversion of gaseous nitrogen to ammonium
-important part of global nitrogen cycle