Lecture 2: Ecological Limiting Factors

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Reading:  Economy of Nature, pp. 34-59.

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Conditions

not consumed or used-up by other organisms
not made unavailable or less available by other organisms
climate and weather, physical environment, abiotic environmental factors

temperature
relative humidity (RH)
hydrogen ion concentration (pH)
salinity
wind speed
stream water flow velocity
pollutant concentration

Resources

something consumed, used, or incorporated or transformed
something eaten, incorporated in biomass
using it makes it unavailable or unusable for other organisms
reuse may occur after a period of use by another organism
water
nutrients (C, N, S, K, P)
minerals
food
mates
shelter
solar radiation

Major nutrients required by organisms (Ricklefs, 1996, p 41, Table 2.1)

Element Function
Nitrogen (N) Structural component of proteins and nucleic acids
Phosphorus (P) Structural component of nucleic acids, phospholipids, and bone
Sulfur (S) Structural component of many proteins
Potassium (K) Major solute in animal cells
Calcium (Ca) Structural component of bone and of material between woody plant cells; regulator of cell permeability
Magnesium (Mg) Structural component of chlorophyll; involved in the function of many enzymes
Iron (Fe) Structural component of hemoglobin and many enzymes
Sodium (Na) Major solute in extracellular fluids of animals

 

Solar radiation: a critical resource

arriving energy varies with latitude
        highest at the equator (see Ricklefs, 1996, pp 80 and 81, Fig. 4.1 and 4.2)
        varies with degree of atmospheric scattering and reflection
at leaf surface light can be
        reflected
        filtered and transmitted
        absorbed
eukaryotic chloroplasts absorb light between 380nm and 710nm
        visible light spectrum
        56% of incident radiation is outside visible range
        photosynthetically active radiation (PAR) (~400nm - 700nm)
prokaryotic chlorophylls: absorption peaks at 800nm, 850nm, and 870-890nm

 

Spectral distribution of sunlight (Ricklefs, 1996, p 45, Fig. 2.13)

 

Biological energy flow is an open system, not a cycle

Major energy transformation processes

Cellular respiration

Photosynthesis
       

 

Light intensity (energy/unit time/unit area) (Ricklefs, 1993, p 39, Table 2.2)

Measurement Units Typical Value
langley (ly) 1 cal cm ¯2 700 ly d ¯1
watt (W) 1 J s ¯1 1000 W m ¯2
einstein (E) 6 X 10 23 photons 2000 µE m ¯2 s ¯1
Source: M.G. Barbour, J. H. Burk, and W. D. Pitts, Terrestrial Plant Ecology, Benjamin Cummings, Menlo Park, California (1980).

Photosynthesis rate as a function of light intensity. The compensation point is the light intensity at which the rate of photosynthesis just compensates for the maintenance needs of the organism (cell respiration rate) (Ricklefs, 1996, p 46, Fig. 2.15).

Water absorbs light energy and scatters light

In sea water:  At 10m, the energy of visible light decreases 50%
                        At 100m, the energy of visible light decreases to <7%

Red is absorbed first
Blue and violet scatter easily
Green penetrates water best

 

Euphotic zone: Depth to which photosynthesis exceeds respiration in water.

Rarely the compensation point, the bottom of the euphotic
zone, is as deep as 100m. Examples, very clear ocean or
lakes near equator.
In highly turbid waters, the compensation point may be
reached at 1m.

 

Major Essential Elements

Calcium (Ca), Iron (Fe), Nitrogen (N), Magnesium (Mg), Potassium (K),
Phosphorus (P), Sodium (Na), Sulfur (S)
Limiting Nutrient Elements
        In aquatic (freshwater) environments: nitrogen and phosphorus
        In marine (saltwater) environments: iron
        In terrestrial environments: nitrogen and phosphorus (calcium)

Other Essential Resources

Carbon Dioxide: Not limiting
Oxygen: Can be limiting in water
Water: Often limiting in terrestrial environments

Limitations for one essential resources can influence the availability of other essential resources. This is the case among terrestrial plants for the relationships between photosynthetic rates, water loss, and gas exchange.

Photosynthetic Capacity and Water Conservation

Photosynthesis rate varies widely among species (100x) even with light saturation and all other resources in abundance. This variation is due in part to differences between plant species in the biochemistry of carbon fixation in photosynthesis (Calvin Cycle). Plants can be categorized as having C3, C4, or CAM metabolism.

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