WK10: Communities & Ecosystems: Nutrient Cycling and Retention
Learning Objectives
- Understand nutrient cycling: what it is, why it matters, and human impacts.
- Describe the role of decomposition in nutrient cycling.
- Describe factors driving changes in nutrient cycling (case studies).
Roadmap
- Ecosystem part of the unit: nutrient dynamics.
- Previous lecture: limits to productivity (bottom-up and top-down).
- Today: movement of energy and materials through ecosystems.
Nutrient Flows and Productivity
- Nutrients drive productivity.
- Example: Wetland system.
- Influx of nitrogen and phosphorus (fertilizers).
- Algal blooms.
- Changes in abiotic environment for macrophytes.
- Changes in wetland structure and function (animals colonize or leave).
- Nutrients at base of food web: large-scale, multi-level impacts.
- Nutrient flow depends on the ecosystem type.
- Pristine vs. agricultural forest.
Nutrients: Elements
- Periodic table:
- Red: 97% of body weight (H, C, N, O).
- Dotted circle: Important (Na, K, Mg).
- Blue: Trace elements (Cu, Zn).
- Green: Possibly essential for some species.
Origin of Elements
- Unlike energy from the Sun, elements are generated by stars.
- Matter is neither created nor destroyed (thermodynamics).
- Focus on pools (storage) and fluxes (movement).
Nutrient Definition
- Elements required for development, maintenance, and reproduction.
- Examples: phosphorus, carbon, nitrogen.
- Used over and over.
Nutrient Cycling Example: Phosphorus
- Phosphorus ion in a lake.
- Diatom skeleton uptake.
- Cladoserine eats diatom.
- Minnow eats cladoserine.
- Pike eats minnow.
- Pike dies, phosphorus released.
- Diatom reuptake.
Nutrient Cycling Defined
- Use, transformation, movement, and reuse of nutrients in ecosystems.
- Involves:
- Storage in nutrient pools.
- Nutrient flux (movement).
- Ecological interest:
- Factors controlling nutrient cycling rate (e.g., log decomposition).
- Nutrient retention: How much stays vs. is lost.
- Human impact: Radically changing nutrient cycling and productivity.
Why Care About Nutrient Cycling?
- Monetary argument: Ecosystem services.
- Ecologically mediated functional processes essential for biodiversity and humans.
- Implications:
- Public health.
- Economy.
- Human well-being.
- Examples:
- Clean air and drinking water (soil filtration, tree roots).
- Greenhouse gas removal (plants).
- Biomass (trees, fish, crops).
- Pollination services (insects, mammals).
- Nutrients underpin everything from monetary goods to biodiversity.
Nutrient-Specific Discussion
- Phosphorus, nitrogen, and carbon.
- Structure:
- Diagram of pools and fluxes.
- Description of pools and fluxes.
- Importance of nutrient.
- Examples of human influences.
Phosphorus Cycle
- Pools (Teragrams grams):
- Marine sediments (massive).
- Oceans (dissolved).
- Mineable rock.
- Land: organisms (moderate), soil (a lot).
- Mostly a rock thing.
- No substantial atmospheric pool.
- Large quantities in mineral deposits and oceans/marine sediments.
- A lot in soil, but much unavailable to plants (bound compounds); mycorrhizae help.
- Importance:
- ATP (energy molecule).
- DNA, RNA.
- Fluxes:
- Inputs: weathering of rocks, decomposition, geological uplift.
- Outputs: fixation (insoluble compounds), leaching.
- Internal cycling: plant and microbial demand.
- Human impact:
- Experimental lakes in Canada (adding N vs. P).
- Phosphorus is limiting in many systems.
- Phosphate in laundry detergents (banned in 80s).
- Phosphate-based fertilizers.
- Soil disturbance during agriculture/forestry releases phosphorus.
- Consequence: Eutrophication (often with nitrogen).
Nitrogen Cycle
- Significant amount in oceans, soil, and atmosphere.
- Fluxes: Denitrification (N to atmosphere), fixation (atmosphere N to usable form).
- Nitrogen fixing bacteria do fixation.
- Large atmospheric pool (80%), but inaccessible as a gas.
- Oceans, plants, soil, organic matter are pools.
- Amount available to organisms is very small.
- Importance:
- Amino acids and nucleic acids.
- Fluxes:
- Inputs: precipitation, nitrogen fixation.
- Outputs: denitrification, leaching.
- Internal: plant demand, denitrification, nitrogen fixation.
- Nitrogen-fixing bacteria:
- Free-living soil bacteria.
- Rhizobia (legume roots).
- Denitrification: Bacteria produce molecular nitrogen.
- Nitrogen fixing bacteria: N2 to NH3 (usable form).
- Rate-limiting step: Nitrogen fixation from the atmosphere.
- Energetically demanding, anaerobic conditions.
- Lightning can fix nitrogen.
- All nitrogen in ecosystems is fixed to be used.
- Human impacts:
- Global nitrogen fixation over time.
- Industrialization: Haber-Bosch process (N to NH3).
- Requires high pressure/temperature.
- Depletes soils, increases nitrous oxide.
- Crop rotation (legumes).
- Intensive agriculture, fossil fuel combustion, clear cutting.
- Climate change, acid rain, eutrophication.
- Hubbard Brook Experimental Forest: clear-cut basin example.
- Clear cutting increases nitrate concentration in stream.
- Nutrients not retained in deforested basin.
- Changes ecosystem processes and leads to eutrophication.
Carbon Cycle
- Major pools: oceans, soils, atmosphere.
- Fluxes: plant respiration, soil respiration, photosynthesis.
- Importance: essential part of all organic molecules.
- Inputs: photosynthesis (CO2 to O2).
- Outputs: respiration and decomposition.
- Carbon recycled via the detritol decomposition loop.
- Human impacts:
- Fossil fuel burning, deforestation (climate change).
- Need to reduce CO2 production.
- Policy changes.
- Alternative fuels.
- Increase CO2 uptake (forest cover, reduce forest clearance).
- Ocean fertilization experiments (add iron).
- Carbon injection into depleted gas/oil reservoirs or geological features.
Take Homes
- Humans have changed all nutrient cycles (P, N, C), typically increasing availability.
- Eutrophication in freshwater systems.
- Impacts on ecosystems and food webs.
- Implications are poorly understood.
- Hard to reverse radical changes.
Decomposition in Nutrient Cycling
- Mineralization: conversion of nutrients from organic to inorganic forms (e.g., animal carcass to ).
- Decomposition: breakdown of organic matter, releases . Mineralization occurs through decomposition.
- Detritus: mix of dead animal/plant remains and excretory products (previously alive stuff).
- Traditionally, detritus viewed as unimportant in food web studies due to difficulty isolating it and lack of techniques to measure energetic importance.
Decomposition: Biological Sources
- Bacteria and fungi: primary decomposers (terrestrial).
- Impact energy and nutrient cycling.
- Convert energy into more accessible forms.
- Symbiotic bacteria (cow guts) break down cellulose.
- Decomposers recycle essential chemical elements.
- Without decomposition, life on earth would stop (too many corpses, too few nutrients).
Decomposition: Biological, Chemical, and Physical Processes
- Biological: fungi, bacteria, invertebrates (fragment and digest).
- Chemical/physical: leaching, fragmentation (abrasion, streamflow).
- Plant detritus is a major food source, but plants are poor food source (high C:N, cellulose, toxins).
- Most plant detritus consumed after decomposition.
- River red gums example:
- Physical/chemical: leaching (25% mass loss/day of soluble material).
- Microbial colonization and decomposition: fungi and bacteria degrade cellulose.
- Biological/physical: invertebrates eat detritus, abrasion, crushing by flow.
Trophic Subsidy
Wetland food web.
Sun -> Autotrophs (paraphyton) -> Herbivores -> Higher Predators.
Parallel pathway with terrestrial input.
Leaves -> Detritus -> Decomposers -> Detritivores -> Higher Predators.
Detritus Decomposition Rate
- Influences availability and persistence of nutrients.
- Typically follows negative exponential decay.
- (half-life): time at which 50% of mass is gone.
- Rate depends on temperature, moisture, chemical composition, decomposer species.
- Example: precipitation (Spain) - higher rainfall leads to higher decomposition rates.
- Example: Lignin content (difficult to decompose) - higher lignin leads to lower decomposition rate.
Case Studies on Factors Influencing Nutrient Cycles
Biomanipulation: using organisms to manipulate ecosystems.
- Example: Lake Food web: Phytoplankton > Zooplankton > Fish.
Excess nutrients -> phytoplankton overgrowth.
Goal: to reduce phytoplankton.
Reduce fish -> zooplankton increase -> phytoplankton consumption -> macrophytes grow back -> nutrients taken up by macrophytes -> water clarity.
Success rates varied (8 definite, 8 partial out of 18)
Removing planktivorous fish increase zooplankton and decrease algal biomass, improving water quality and allowing macrophytes to grow.
Promotes a stable clear water state.
Does not always work because their is no redundancy in the system. Also strong overriding bottom up effects can reverse process.
Invasion of a plant, Mirakafea in Hawaii.
- Soils in Hawaii are volcanic in origin and low nitrogen.
Miracafea has a symbiosis with Frankia bacteria that allows it to fix nitrogen.
The amount of nitrogen that can be fixed is much greater with Miracafea.
- Miracafea invades Hawaii, fixes nitrogen, increases nitrogen and available to the organisms in the ecosystem.
- Alters trophic interactions and habitat structure.
Allows other plants to grow with the new increase nutrients that native plants, invasive plants, native earthworms, alien bird species feed on Miracafea.
*So a bit of mess, a bit of a massive disturbance is created.Meta Analysis, humans change nutrient cycles and pools by making more amount available. This increase carbon and nitrogen.
Far reaching impacts on nutrient cycles of plant invasions.
Take Homes
- Primary productivity drives food webs influenced by cycling and recycling of nutrients and of energy.
- Carbon, nitrogen, phosphorus and all nutrients described in terms of the flows through biotic and abiotic pools.
- Changes in these flows are evident due to human activities.
- Decomposers crucial component of nutrient cycling in all ecosystems.
- Changes in trophic structure and nutrient availability change nutrient cycles within ecosystems having impacts on ecosystem structure.