Lecture: Chapter 22 - Decomposition and Nutrient Cycling Flashcards
Internal cycling
refers to recycling of nutrients within an ecosystem as they are transformed between inorganic and organic forms
internal cycling is driven by primary production and decomposition
Nitrogen will be used as an example for internal cycling
Decomposition
Chemical and biological transformations in ecosystems alter the chemical form and supply of nutrients
Foremost among nutrient transformations is the decomposition of organic matter, which releases nutrients back into the ecosystem
Nutrient Transformations
Nutrients in detritus are made available by decomposition: the process by which detrivores break down detritus to obtain energy and nutrients
Decopoisiton releases nutrients as simple, soluble, inorganic compounds that can be taken up by other organisms
Decomposition processes:
Leaching - soluble compounds may be washed out from organic dead matter
Fragmentation
Chemical alteration (mineralization)
Litter
Fresh, undecomposed organic matter on the soil surface is known as litter
Fragmentation
Animals such as earthworms, termites and nematodes consume the litter, breaking it up into progressively finer particles. This fragmentation increases surface area, which facilitates chemical breakdown.
Bacteria
The main decomposers of dead animal matter
Fungi
Dominant decomposers of dead plants
Mineralization
The chemical conversion of organic matter into inorganic (mineral) nutrients by decomposers
Immobilization
Decomposers also need nutrients for their own metabolic processes, so they need to uptake and assimilate inorganic (mineral) nutrients (e.g. ammonia)
Net mineralization rate (NMR)
Mineralization rate - immobilization rate
NMR depends on nutrient content of the litter and the nutrient demand of the microbial population
Factors impacting decomposition rate
Litter quality
Environmental factors (e.g. temperature, precipitation - climate)
Litter Quality
Depends on types of carbon compounds present
- High : small molecules with high energy bonds (simple sugars)
- Moderate: Strucutrally more complex, harder to decmopose (cellulose)
- Low: Large molecules with much complexity, hardest to decompose (Lignin)
Temperature and decomposition
Decomposition and mineralization rates are faster in warm, moist conditions
Requirements for decomposers
Decomposers require energy and nutrients for their own growth and maintenance