The hydro-ecosphere is the largest of all biomes which covers about 75% of the earth's surface
Freshwater environment
Low concentration of dissolved salt
Marine environment
High concentration of dissolved salt
Physical and chemical factors in aquatic environments
Light
Temperature
Flow
Pressure
Dissolved gases
Dissolved solids
Light
Necessary for photosynthesis
Affects the growth of microorganisms at varying depths
Photic zone
Upper 200 meters where sunlight can penetrate and photosynthesis can take place
Aphotic zone
Deeper areas where sunlight cannot penetrate
As temperature decreases
Dissolved oxygen availability increases
As temperature increases
Dissolved oxygen availability decreases
Temperature in freshwater environments
Highly fluctuating due to precipitation and run-off
Temperature in marine environments
More stable due to ocean currents and global climate patterns
Thermal stratification in deep lakes
1. Warm upper layer (epilimnion) does not mix with cool deeper layer (hypolimnion) in summer
2. Stratification is broken down during cooler seasons when surface layer becomes colder and denser, mixing with bottom layer
Flow of water
Influences availability of nutrients, food resources, and water itself
Pressure
Increases by 1 atm for every 10-meter increase in depth, affecting which microorganisms can grow
pH
Affected by pollutants, chemicals, bedrock/soil composition, and other compounds
Acidification of bodies of water
Results in loss of diversification due to sensitivity of organisms
Ocean pH
Averages 8.07, kept basic due to erosion of rocks adding alkalinity, buffered by dissolved CO2, boric acid, silicic acid
Dissolved gases
Used by microorganisms and oxygenic organisms like fish and algae in biological processes like respiration and photosynthesis
Dissolved organic matter in oceans
Influences production of most marine volatile gases, comes from marine biota like photosynthetic algae and bacteria, consequences of grazing and viral lysis
Dissolved organic matter in freshwater
Mostly composed of carbohydrates, aliphatics, and carboxyl-rich alicyclic molecules
Inorganic substances in oceanic water
Cations: Na+, Mg2+, Ca2+, K+
Anions: Cl-, SO4 2-
Inorganic substances in freshwater
Ca, Mg, Na, K
Oligotrophic state
Clear water, low nutrient concentration
Mesotrophic state
Sedimentation of nutrients forms anaerobic zone on bottom
Eutrophic state
High nutrient concentration, high presence of organisms, entire body anaerobic except air above
Types of microorganisms in aquatic environments
Resident (naturally occurring)
Transient (introduced)
Transient microorganisms
Introduced via precipitation, air dispersal, water flow
Freshwater body types
Lotic (flowing): springs, rivers, canals, estuaries, streams
Lentic (stagnant): lakes, ponds, wetlands
Lotic freshwater environments
Conditions vary more, harder for microorganisms to inhabit
Lentic freshwater environments
Conditions more stable, higher nutrient concentration and microbial diversity
Springs and groundwater are mostly oligotrophic and offer little to sustain life, with low microbial numbers