Ch 27 Environmental Microbiology

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Presentation transcript:

Ch 27 Environmental Microbiology What do Microbes do? How can we use this to our advantage?

Microbes have small genomes but can Not do a lot, but what do, do well Extremophiles Microbes live in extreme conditions of Temperature Acidity Alkalinity Salinity Eubacteria vs Archaebacteria

Biological definition of Organismal interactions Symbiosis: a relationship between two different species Parasitism: one org gets nutrients from another Mutualism: both partners benefit Commensalisms: one benefits more

Fig 27.5

Other examples? Mycorrhizae Endomycorrhizae or vesicular arbuscular mycorrhizae. Endo within And ectomycorrhizae, on the outside oaks ect.

Biogeochemical cycles Matter can neither be created or destroyed A constant amount of matter in the environment must be recycled Microbes are essential in the conversion of nutrients into organic and usable formats Microbes are essential in the conversion of nutrients into the inorganic form

The Biogeochemical cycles Also termed biological fire

The carbon cycle Photoautotrophs Chemoautorophs Both convert inorganic forms of carbon into organic forms using external sources of energy

Chemoheterotrophs release Inorganic form of carbon (CO2) to complete the cycle. Non living sinks include CaCO3 and fossil fuels

Discuss how carbon moves and the sinks or storage areas

The nitrogen cycle Local shortages because of Nitrogen stuff Microbes decompose proteins form dead cells and release amino acids Ammonia is liberated by microbial ammonificaiton of amino acids Ammonia is oxidized to produce nitrates for energy by nitrifying bacteria Again, look at how this nutrient moves and what causes local shortages

More nitrogen stuff Denitrifying bacteria reduce nitrogen in nitrates to molecular nitrogen N2 is converted into ammonia by nitrogen fixing bacteria Ammonium and nitrate are used by bacteria and plants to synthesize amino acids Denitrification occurs in watterlogged soils without air. The nitrates of agricultural fertilizer can act as an electron acceptor

Fertilization and microbes Cyanobacteria for a symbiosis with small floating fern Azolla in rice paddy waters.

Sulfur cycle Plants and certain microbes can use SO42- to make amino acids H2S is oxidized to form SO42-

Dissimilation Assimilation Oxidation Anaerobic rspiration

Sulfur Cycle Proteins and waste products Amino acids Amino acids (–SH) Microbial decomposition Proteins and waste products Amino acids Microbial dissimilation Amino acids (–SH) H2S Thiobacillus H2S SO42– (for energy, by respiration) Microbial & plant assimilation SO42– Amino acids

The Phosphorous Cycle

The Phosphorus Cycle Inorganic phosphorus is solubilized by microbial acids Made available to plants and other microbes Is soluble in water Combines with calcium in calcium phosphate deposits of ancient seas.

Life Without Sunshine Primary producers in most ecosystems are photoautotrophs Primary producers in deep ocean and endolithic communities are chemoautotrophic bacteria H2S SO42– Provides energy for bacteria which may be used to fix CO2 Calvin Cycle CO2 Sugars Provides carbon for cell growth

Use of chemicals in soil and water Many man made chemicals do not biodegrade because they are not made by living organisms Why?

Decomposition by Microbes Weed be gone a biodegradable herbicide Agent orange, a resilient herbicide Components of agent orange Figure 27.8

Bioremediation Use of microorganism to remove pollution Cheaper Can use natural organism Is helped by preventing limited nutrients

Solid Municipal Waste piles Many municipal waste piles are inefficiently run because they are dry and anaerobic

Aquatic conditions Biofilms are composed of whole communities of microbes that are metabolically diverse Bodies of water are naturally set up to process waste Tend to grow in presence of oxygen and light Use is best when oxygen content is increased Phytoplankton in oceans are primary producers in the open ocean

Freshwater Donation Figure 27.12

Roll of microorganism in water quality Biomagnifications Indicators of fecal contamination Blooms Eutrophication

Waterborne Diseases Table 27.2

Water quality tests Coliforms are aerobic or facultatively anaerobic, gram negative non endospore forming rods that ferment lactose with the production of acid and gas within 48 hours of been placed in a medium at 35’C Fecal Coliforms predominantly E. coli are used to indicate the presence of human fecies

Coliforms Aerobic or facultatively anaerobic, gram-negative, non–endospore forming rods that ferment lactose to acid + gas within 48 hr, at 35°C Indicator organisms Used to detect fecal contamination MPN Most probable number/100 ml of water

Water Treatment Water held in a holding reservoir long enough that suspended matter settles Flocculation treatment uses a chemical such as alum to coalesce and settle colloidal material Filtration removes protozoan cyst and other microbes Drinking water is disinfected with chlorine to kill remaining pathogenic bacteria

Sewage Treatment The quality of life that we see in our first world countries is due to our treatment of sewage Primary treatment: removal of solid materials (35% BOD) Secondary treatment: Reduction of BOD by the metabolic (95%BOD) degradation of organic matter

More sewage treatment BOD biochemical oxygen demand Tertiary provides essentially drinkable water is much more expensive to do

Activated Sludge Figure 27.20a,b

Alternative treatments of sewage Septic tanks Oxidation ponds

Sludge produced by sewage treatment plants.

Anaerobic Sludge Digester CO2 + 4 H2  CH4 + 2 H2O CH3COOH  CH4 + CO2 Most methan is derived from reduciton of carbon dioxide by hydrogen gas. Other methan producing microbe split acetic acid to yeald methan and carbon dioxide. Figure 27.23