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Formula: Efficiency = Energy at current trophic level/Energy at previous trophic level × 100%. Measures the percentage of energy transferred between trophic levels, typically averaging 10%. High efficiency retains more energy across levels, supporting higher-tier carnivores. Low efficiency explains why terrestrial food chains rarely exceed four or five levels due to heavy entropy losses.
A diagram illustrating the rate of energy flow through each trophic level over time; strictly upright due to thermodynamic laws.
The amount of energy or biomass remaining per unit area per unit time after subtracting respiratory losses NP = GP - R.
Formula: GPP = NPP + R. GPP is the total solar energy fixed into organic matter by producers per unit area per unit time. High GPP values signal optimal growing conditions (warmth, abundant water, rich nutrients), yielding rapid biomass production as seen in tropical rainforests. Low GPP reflects harsh limiting factors such as extreme cold or severe drought in tundra or desert systems.
Formula: NPP = GPP - R. The biomass remaining in producers per unit area per unit time after subtracting respiratory losses. High NPP provides a large energy base, enabling long food chains and supporting high consumer biodiversity. Low NPP restricts energy availability, creating short food chains and limiting animal biomass.
Formula: GSP = Food Eaten - Fecal Loss. The total biomass assimilated by heterotrophs from ingested food. High GSP indicates efficient assimilation, common in carnivores digesting protein-rich meat. Low GSP stems from indigestible dietary content, such as cellulose in herbivore diets, leading to heavy fecal losses.
Formula: NSP = GSP - R. The net biomass accumulated by consumers per unit area per unit time after accounting for respiratory heat loss. High NSP reflects rapid body growth and high reproductive output. Low NSP means consumers expend nearly all assimilated energy on metabolic maintenance and thermoregulation.
Formulas: Respiration (R) = Initial DO - Dark DO; NPP = Light DO - Initial DO; GPP = Light DO - Dark DO. Measures aquatic productivity using dissolved oxygen (DO) changes. High GPP/NPP values identify nutrient-rich photic waters. Negative NPP values indicate net oxygen consumption, signaling organic pollution or eutrophication.
Formula: MSY = NPP (for producers) or MSY = NSP (for consumers). The highest rate of resource harvesting that avoids long-term stock depletion. Harvesting equal to or below MSY maintains capital biomass indefinitely. Harvesting above MSY causes population collapse and system degradation.
The conversion of atmospheric nitrogen gas into plant-available nitrogen forms like ammonia or nitrates by specialized bacteria (e.g., Rhizobium) or lightning.
The oxidation of ammonia into nitrites and subsequently into nitrates by soil bacteria (e.g., Nitrosomonas, Nitrobacter).
The conversion of soil nitrates back into gaseous atmospheric nitrogen by anaerobic bacteria in waterlogged conditions.
Insolation angle, elevation (1.C temperature drop per 100m gain), continentality, atmospheric pressure belts, seasonal axial tilt (23.5.), and precipitation regimes.
Arid biomes receive under 50 cm of annual precipitation, are subject to extreme daily temperature swings, have nutrient-rich but water-deficient soils, and have xerophytic vegetation.
The final, stable equilibrium stage of ecological succession is characterized by complex food webs, high biomass, balanced productivity (GPP = R, NPP = 0), and mature soil structure.