Biogeochemical Cycles Lecture 11 Chapter 23. Nutrients – Macronutrients: Organism would fail...
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Transcript of Biogeochemical Cycles Lecture 11 Chapter 23. Nutrients – Macronutrients: Organism would fail...
Nutrients –
Macronutrients: Organism would fail completely C, H, O, N, P, K, Ca, Mg, S
Micronutrients: required as cofactors, components of certain moleculesCl, Fe, Mn, B, Cu,. Mo, Zn, Ni
Availability is influenced by pH …
(See 6.12)
• Life depends on recycling chemical elements• Nutrient circuits in ecosystems involve biotic
and abiotic components and are often called biogeochemical cycles
• Focus on:– Each chemical’s biological importance– Forms in which each chemical is available or used
by organisms– Major reservoirs for each chemical– Key processes driving movement of each chemical
through its cycle
Two food chains:• Grazing food chain
– Herbivore carnivore
• Detritus food chain– Dead matter and
waste from grazing food chain and primary production
– Provides input to grazing food chain
Detrivore food chainheterotrophs: feed on dead material
Provide prey in herbivore foodchain
Fragmentation: 1. Microfauna and flora <100um
Protozoans and nematodes
2. Mesofauna 100um 2mmMites, potworms, springtails
3. MacrofaunaMillipedes, earthworms, snails,
amphipods & isoods
Decomposition:Bacteria and fungi – produce
extracellular enzymes
Fungi belong to a separate kingdomseveral groups produce long, thread-like strands (hyphae)reproductive structures may be large and visible
Bacteria: two distinct kingdoms
Single celledMicroscopicVarious shapesMany may not be easily
culturedMay develop populations
quickly
Study of Decomposition – Litterbag Studies• Weighed sample in mesh bag placed in
soil• Withdrawn after time to determine
remaining dry-weight– Dry weight estimate distorted by biomass of
decomposer
• Gives estimate of decomposition impacted by
– Species– conditions
Decomposition of red maple leaves more
rapid in warmer, more humid climatesdde
Other factors which may impact rate of decomposition?
Two types of biogeochemical cycles based input source to ecosystems
• Sedimentary– Rock and salt solution phases
• Gaseous– Global
• Many cycles hybrid – Exchange pool– Reservoir
Carbon cycle:• Closely tied to energy flux• Major exchange pool: atm CO2 (at
~0.03% )• Uptake via photosynthesis• Immobilized in carbonates of
shells, fossil fuels• Subject to daily + seasonal flux
The Phosphorus Cycle• Phosphorus is a major constituent of nucleic
acids, phospholipids, and ATP• Phosphate (PO4
3–) is the most important inorganic form of phosphorus
• The largest reservoirs are sedimentary rocks of marine origin, the oceans, and organisms
• Phosphate binds with soil particles, and movement is often localized
Fig. 55-14d
Leaching
Consumption
Precipitation
Plantuptakeof PO4
3–
Soil
Sedimentation
Uptake
Plankton
Decomposition
Dissolved PO43–
Runoff
Geologicuplift
Weatheringof rocks
Nitrogen cycle:• N essential to life – amino acids, nucleic acids• Atm. N2 stable, difficult bond to break• Fixation largely biological (ca 90%); agricultural use requires
fossil fuel input
• Fixation of N N– Free living aerobics as Azotobacter, & certain cyanobacter– Lichen symbionants– Mutualists associated with certain plant groups
(Rhizobium spp. on leguminous plants)
N2 N + N (NH3)2 NH4
H + energy
NO3
Ammonia (gas)
Ammonium form available
to plants
Under acidic conditions converts to ammonium
but may be lost to atmosphere
Nitrate produced by soil bacteria from ammonium may also be taken up by plants or mineralized to
N2
• Organic nitrogen is decomposed to NH4+ by
ammonification, and NH4+ is decomposed to
NO3– by nitrification (2 step processes, involving
2 different soil bacteria: Nitrosomonas and Nitrobacter)
• Denitrification converts NO3– back to N2
– Anaerobic, involves Pseudomonas spp
• Soil pH impacts both processes (low pH inhibits)
Fig. 55-14c
Decomposers
N2 in atmosphere
Nitrification
Nitrifyingbacteria
Nitrifyingbacteria
Denitrifyingbacteria
Assimilation
NH3 NH4 NO2
NO3
+ –
–
Ammonification
Nitrogen-fixingsoil bacteria
Nitrogen-fixingbacteria
Human activities now dominate most chemical cycles on Earth
• As the human population has grown, our activities have disrupted the trophic structure, energy flow, and chemical cycling of many ecosystems
Nutrient Enrichment
• In addition to transporting nutrients from one location to another, humans have added new materials, some of them toxins, to ecosystems
Agriculture and Nitrogen Cycling
• The quality of soil varies with the amount of organic material it contains
• Agriculture removes from ecosystems nutrients that would ordinarily be cycled back into the soil
• Nitrogen is the main nutrient lost through agriculture; thus, agriculture greatly affects the nitrogen cycle
• Industrially produced fertilizer is typically used to replace lost nitrogen, but effects on an ecosystem can be harmful
Contamination of Aquatic Ecosystems
• Critical load for a nutrient is the amount that plants can absorb without damaging the ecosystem
• When excess nutrients are added to an ecosystem, the critical load is exceeded
• Remaining nutrients can contaminate groundwater as well as freshwater and marine ecosystems
• Sewage runoff causes cultural eutrophication, excessive algal growth that can greatly harm freshwater ecosystems