nitrogen cycling Flashcards
nitrogen inputs?
chemical weathering, atmospheric deposition, anthropogenic fixation, biological fixation of atmospheric o2
outputs?
gaseous and solute
denitrification
roles of N gases
what does nutrient cycling involve
- nutrient inputs
- internal cycling
- nutrient loss
transfers among plants microbes consumers & enivronment
describe chemical weather of rocks
sedimentary rocks 75% surface rock - can contain N
minor contribution in most ecosystems
describe deposition
gaseous, particulate, and dissolved sources
from other ecosystems - > leaching
atmospheric:
-wet (precip/fog) and dry (dust/aerosols)
-lightning N2 to No3-
approx. 5% total N fixed in systems
anthropogenic fixation (increasing importance)
production of fertilizers (N2 to NH3)
fossil fuel combustion - releases NOx
domestic animals (NH3 to atmosphere)
often transported long distances
biological fixation
main pathway for N entry into natural systems
reduction of N2 to NH4 by microbes
role of nitrogenase in biol fix
catalyst
denatured in presence of O2 - needs anaerobic environment
- energetically expensive; needs souce of C and P (ATP)
- temp constrains C supply and nitrogenase activity - prominant in tropics and contstrained at high lat.
organisms involved in biol fix?
- N fixing bacteria in symbiotic association with plants have the highest rates of N fixation
○ Rhizobium bacteria symbiotic with legumes
○ Frankia spp associated with alders
○ Physical association
describe bacteria symbiosis with plant for N fixation
heterotrophic N fixers
○ Plants provide high energy © environment in return for N
○ From root nodules around bacteria (protect from O2 - it degrades)
○ Also free living bacterial (low fixation); bacteria in termite guts (important in tropics)
○ Even the absoprtion of nutrients is not a free process- active transport involved
phototrophic N fixers
○ Free living cyanobacteria (bluegreen algae, Nostoc)
○ Cyanobacteria symbiotic with fungi (ie lichens)
§ Important in early successional ecosystems
○ Cyanobacteria symbiotic with plants (Azolla fern and Nostoc in rice paddies)
Often have specialized cells (heterocysts) that protect nitrogenase from O2
Biotic and Abiotic limits on N fixation
- Biotic and abiotic constraints on N fixation
- Energetically expensive
* Approx 2-4x higher cost than N uptake from soil
* Association with symbiotic N fixers strongest in N poor soils
* High energy = high light environments (photosynthesis of symbiotic plants) -> most common in early successional species - Nutrient co-limitation (e.g. P (for ATP))
* May be ultimate control over N supply and NPP in some systems - Herbivory
* High N content of N-fixing plants makes them preferred forage (tradeoff)
- Energetically expensive
N and P in natural ecosystems -
inputs and outputs «< internal tranfers
closed systems
but human activities = open system
look at nitrogen inputs graph
- Time series
- Human caused inputs now = or exceed natural inputs
Trade off btwn human needs and planets needs
- Human caused inputs now = or exceed natural inputs