Chapter 14 Flashcards
(31 cards)
aquatic system
- The biological activity of an aquatic ecosystem depends, utlimately, on the activities of the primary producers (oxygenic photoautotrophs, phytoplankton; phyto=plant):
- Algae
- Cyanobacteria (also fix nitrogen)
- These organisms serve as a food source for chemoheterotrophs: bacteria, protozoa (zooplankton, zoo=animal), fish, and other aquatic organisms
- The activities and net numbers of phytoplankton depend on a variety of factors:
1. Temperature
2. Light received- Availability of specific limiting nutrients such as nitrogen and phosphorous
photic zone
- in clear water, light will penetrate to a max depth of 300m: photic zone
Microorganisms must be able to harvest light that reaches them (accessory pigments)
marine environment + open ocean
- High salinity (3%): organisms are halotolerant
- 75% of the ocean is deeper than 1000m (deep sea, pelagic zone); at its deepest, 11 km below the water surface, pressure is about 110 atmospheres (environ 1 atm/10m)
- Below 100m the temperature is constant 2-3C
In the open ocean (pelagic zone), primary productivity is very low due to the lack of inorganic nutrients (nitrogen, phosphorous, iron) that are required by phyloplankton. The open ocean is OLIGOTROPHIC
- Tempé are cooler and more constant than areas closer to shore
In some regions, wind and ocean currnts cause an upwelling of water from the ocean floor bringing nutrients to the surface and promoting productivity
open ocean
- Bulk of primary productivity comes from prochlorophytes (tiny phototrophs phylogenetically related to the cyanobacteria): prochlorococcus
- General adaptations seen in pelagic (open ocean) microorganisms:
1. Reduced size (high surface/volume ratio)
2. High affinity transport systems - Trichodesmium:
1. Filamentous cyanobacteria
2. Contains phycobilins
Nitrogen fixation
- General adaptations seen in pelagic (open ocean) microorganisms:
coastal water
- Primary producers: algae, cyanobacteria
- Productivity is usually higher due to the influx of nutrients from ivers and other polluted water sources (ex: agricultural runoff = excess nitrogen, phosphorus). EUTROPHIC
- Can cause red tides (algal bloom, dinoflagellates, neurotoxins). Nitrogen is a limiting nutrient
- Higher level of primary productivity supports a higher concentration of zooplankton and aquatic animals
deep sea
- Between 200 and 1000m, chemoheterotrophs degrade organic matter that falls from the photic sones. 2-3C, psychrophiles
- Below 1000m, organic carbon is very scarce, oligotrophic, no light. Very few microorganisms (psychrophilic and barophilic or barotolerant)
- Whale fall (1600m deep): a source of nutrients
Ex of a large protist (xenophyophore) found on the deep sea flour (5000 deep), bar= 100um
hydrothermal vent
- Source of heat, source of nutrients, electron donors, electron acceptors
- Community of microorganisms, animals
Tube worms: symbiosis with sulfur oxidizing chemoautotrophs. Tube worms trap and transport nutrients to the bacterial symbionts
- Community of microorganisms, animals
freshwater environment
- Highly variable (isolated system compared to ocean)
- Microbial populations will depend on the availability of nutrients, oxygen and light. Limited by the availability of nitrogen and phosphorus
- Lakes (poor mixing/aeration)
Rivers (good mixing/aeration)
oligotrophic lakes (N and P are limiting)
- Primary production is low, availability of organic matter is low
- Growth of aerobic chemoheterotrophs is limited by nutrients supply; O2 concentrations remains high: rate of O2 dissolution is higher than the consumption rate
- Lake remains aerobic even at depth and organic matter is degraded completely
- Oxygen saturated
Clear water (deep penetration light)
eutrophic lake (nutrients rich)
- Primary production is high (algal bloom), availability of organic matter is high
- Rapid growth of chemoheterotrophs, rapid depletion of dissolved O2
- Low O2 concentration
- Anaerobic zones are created
- Poor light penetration
Health risks: pathogens, bloom of cyanobacteria/algae (secrete toxins)
eutrophic lake , presence of H2S
- Bottom sediments are anaerobic and contain organic matter (dead primary producers..) which support the growth of denitrifiers, methanogens and sulfate reducers (H2S)
- Anaerobic photosynthesis uses H2S as electron donor and produces sulfate which is used by sulfate reducers
Excessive production of H2S and the production of organic acis from fermentation can give the water a bad odoré the lack of O2 and/or presence of H2S may kill fish and other aerobic organisms
- Anaerobic photosynthesis uses H2S as electron donor and produces sulfate which is used by sulfate reducers
lake in temperature climates
- Anaerobic zones may develop as a result of summer stratification. Lakes become thermally stratified.
- As the temp. Increases, the surface water is warmed resulting in the formation of a warm upper layer- EPILIMNION- less dense, aerobic
- The colder, bottom layer - HYPOLIMNION, denser anaerobic- is separated from the epilimnion by a zone of rapid temp. Change - THERMOCLINE
Mixing in the spring and fall only. Brings nutrient back up the watre column
rivers
- Rivers: good mixing/aeration ensures that organic matter, within limites, is degraded effectively (no fermentation, no H2S production)
Excess organic matter may still result in anaerobic areas with consequences similar to those senn in eutrophic lakes
pollution
- Pollution of freshwater: deliberate discharge of effluents into a waterway (major source is sewage)
- Sewage is rich in organic matter and contains larger number of organisms (some may be pathogens)
- Aerobic and facultative organisms oxidize organic matter using the dissolved wO2
Biochemical oxygen demand (BOD) is high (used as a measure of the extent of pollution by organic matter). Water tends to become anaerobic, microbial metabolisms: fermentation, sulfate reduction, nitrate reduction…
biofilms
- Biofilms: microbial cells embedded inside an extracellular matrix
- Usually produced by a mixed population of species
- Extracellular matric composed of proteins, polysaccharides, DNA
- Cells inside the biofilm are more resistant ot stress than planktonic (free-living) cells
- Biofilms are found in water systems (natural and man-made), on wet surfaces, growing on medical devices…
4 steps
1. Attachment: adhesion of a few motile cells to a suitablesolid surfaces
2. Colonization: intercellular communication, growth and polyssacharides formation
3. developmentL more growth and polysaccharides
Active dispersal: triggere by environmental factors such as nutrient availability
water-borne pathogens
- Most of these pathogens grow in the intestinal tract and transmission is mediated by fecal contamination of water supplies
- Source of infection:
1. Potable water (drinking and food preparation)
Recreational water (swimming)
- Source of infection:
water-borne bacteria pathogens and virus
- salmonella typhi: typhoid fever in humans, systemic infection, healthy carriers
- Vibrio cholera: cholera, severe diarrhea (enterotoxin)
- Shigella spp.: shigellosis; bacterial dysentery (bloody diarrhea, inflammation of the intestinal mucosa)
- Salmonella spp. (other than typhi): salmonellosis, gastroenteritis
- Campylobacter spp.: gastroenteritis, most common cause of gastroenteritis in canada
- enterovirusL norovirus, rotavirus (children)
- Hepatitis A virus
water-brone pathogenic protozoa
- Entamoeba histolytica: amoebic dysentery
- Giardia lamblia: giardiasis (backpacker’s disease/beaver fever), chronic diarrhea, often associated with drinking water in wilderness areas (beavers and muskrats are frequent carriers- source of contamination of streams)
Cryptosporidium parvumL chronic and acute diarrhea, self limiting in healthy individuals, major problem in immunocompromised individuals, nor reliable tratment. Present in 90% sewage samples, 75% river waters (intracellular C. parvum)
- Giardia lamblia: giardiasis (backpacker’s disease/beaver fever), chronic diarrhea, often associated with drinking water in wilderness areas (beavers and muskrats are frequent carriers- source of contamination of streams)
cysts of G. lamblia and C. parvum
- Both form cysts that are resistant to a number of disinfectants, including chlorine
c. Parvum cysts are not effectively removed by filtration process in water plants (too small)
water quality control
- Impossible to check for all pathogens. Most water-borne pathogens are associated with fecal material
- Test the water for organisms that are present in large numbers in feces - these organisms are used as indicators of fecal pollution- if these organisms are present, there is a chance that the water may also contain pathogens
- 2 indicators:
1. coliformsL facultative aerobic, gram-negative, non spore-forming, rod-shaped bacteria that can ferment lactose with gas formation within 48 hours at 35C. Includes a variety of bacteria not all of intestinal origin.
2. Fecal coliforms: coliforms derived from the intestines of warm-blooded animals (can grow at 44,5C, thermotolerant) - The presence of fecal coliforms, especially E.coli, indicate fecal contamination and that the water is unsafe for human consumption
Absence of fecal foliforms does not ensure good water quality (cysts are more resistant than fecal coliforms)
most probable number (MPN)
- Test for coliforms: samples are added to lactose broth. If gas production is detected, test is positive
- Use statistical tables to estimate the MPN of coliforms in the original sample
Presumptive tests, further testes needed for confirmation
- Use statistical tables to estimate the MPN of coliforms in the original sample
membrane filtration
- Coliforms and fecal coliforms
- Test large volume of water (100ml)
- Faster and easier than MPN
Eosin-methylene blue medium is selctive and differential for lactose-fermenting bacteria
water treatment
- Aims:
- Remove pathogens
- Improve clarity of water
- Removes compunds that give bad smell or taste
- Soften the water
Extent of treatment needed depends on the quality of the source of water
steps 1-3 water treatment
1) SEDIMENTATION:
- Water is left to stand in a reservoir (sedimentation bassin)
- Allow to large particle (sands) to settle
2) FLOCCULATION TREATMENT (chemical coagulation) - A flocculating chemical (coagulant) is added - Water is transferred to a flocculation basin and allowed to settle for 6h - As the flocks (flaky precipitates) form, they trap fine particles (clay, bacteria, viruses, protists) - Some organics chemicals are also absorbed by the flocs - 80% of bacteria, color and particluates are removed 3) FILTRATION - The water is filtered through sand to remove remaining particles, even more bacteria and any remaining G. lamblia cysts - After this stage, 98-99,5% of the bacteria have been removed Filter is backflushed regularly to prevent clogging