4 - Energy Flow and Material Cycling through the Ecosystems
Earth Spheres
Lithosphere: Solid Earth layer.
Hydrosphere: All water found on, under, and over the Earth's surface.
Atmosphere: Gases that surround the Earth.
Biosphere: All life forms on Earth.
Interaction of these four spheres is essential for understanding Earth System Science.
Energy Flow in the Ecosystem
Energy Flow:
Fundamental ecological concept unifying studies of plants, animals, and microorganisms.
Based on trophic relationships among organisms; a driving force for ecosystem function.
Sources of Energy in Ecosystems
The primary energy source for the biosphere is solar radiation.
Plants, algae, and some bacteria utilize sunlight through photosynthesis.
Key Concepts in Energy Flow
Biomass
Definition: The energy content or organic matter content of an organism, population, or ecosystem.
Renewable organic material from plants and animals, can be converted to usable fuels.
Production vs. Productivity
Production: Increase in biomass amount.
Productivity: Increase in production per time period.
Biomass and production measured in energy units (calories) or mass units (grams).
Trophic Levels in Ecosystems
Organisms classified into three groups:
Producers: Autotrophic and photosynthetic organisms that grow using sunlight (e.g., plants, algae).
Consumers: Heterotrophic organisms that consume plants or animals for energy; they acquire organic matter after obtaining energy from producers.
Decomposers: Bacteria and fungi that break down dead organic matter to release nutrients back into the ecosystem.
Energy Transition Between Trophic Levels
As energy flows between trophic levels, available energy decreases.
Energy loss occurs in forms of waste and heat during respiration.
Only about 10% efficiency is observed in energy transfer to the next trophic level, with the remaining 90% lost.
Biomagnification
Describes the concentration of toxic substances as energy moves up the food chain.
Example: Pollutants like PCBs are absorbed by phytoplankton and biomagnified through consumption by higher trophic levels (e.g., zooplankton, herring, salmon, and orca whales).
The Water Cycle
Water is vital for life, with human bodies containing about 63% water.
Exists in three phases: solid, liquid, and gas, with uneven distribution in biosphere.
Biogeochemical Cycles
Carbon Cycle
Carbon: Primary element of life, undergoing rapid cycling through food chains.
Involves exchanges of carbon between living organisms and CO2.
Plants use CO2 through photosynthesis; oxygen is produced, completing this cycle.
Nitrogen Cycle
Nitrogen: Essential for protein synthesis, but largely inert in atmospheric form (N2).
Usable forms include ammonium and nitrates, which are absorbed by producers.
Cycle includes fixation, nitrification, and denitrification processes to return nitrogen to the atmosphere.
Oxygen Cycle
Oxygen is necessary for aerobic respiration; however, excess levels can be toxic.
Oxygen cycle works oppositely to the carbon cycle, primarily through photosynthesis and respiration.
Human actions, like deforestation and fossil fuel combustion, affect the oxygen cycle significantly.
Phosphorous Cycle
Phosphorous (P): Key element for living organisms, often limiting in ecosystems.
Cycle includes recycling through decomposition, but significant loss occurs in deep ocean deposits leading to scarcity.
Human activity, such as fertilizer use, exacerbates natural losses causing eutrophication in aquatic systems.
Sulphur Cycle
Sulphur (S): Integral to some amino acids; cycles mainly in aquatic environments and soils.
Sulphur is absorbed by plants for protein production, and human-induced activities like fossil fuel combustion enrich the biosphere with sulphur compounds.