Lecture 10: Notes, etc.
Nutrient Cycling in Terrestrial Ecosystems
Elements necessary for life
C, H, O
- We don’t consider these “nutrients” or “nutrient cycles”
- They are closely connected with energy flows
- (You will hear people talk about “carbon cycling” in an ecosystem, but C does not typically cycle the way nutrients do)
- N and P: most commonly limiting to growth
- The focus of most nutrient cycling resaerch
- Also cause problems in downstream aquatic ecosystems if they are lost from terrestrial ecosystems
Macronutrients: Ca, K, Mg, S
Micronutrients: Fe, Mn, and others
“N fixation”: biological conversion of atmospheric N2 gas into biologically reactive forms of N: primarily NH3
- This is an energy-consuming reaction. It requires ATP
Cyanobacteria = blue-green algae
- N fixers in both aquatic and terrestrial ecosystems
- Live in water column, or form films on surfaces, or in soils or sediments, or in decaying logs
In terrestrial systems
- When “free-living” bacteria, in which case it is called non-symbiotic N fixation
- Can be bacteria living in symbiosis with plant roots, requiring anaerobic conditions, called symbiotic N fixation
Root nodules of plants seal out the oxygen. The N-fixing bacteria live in these nodules in a mutualistic symbiosis with the plant.
Some N-Fixing Plants: Red alder, black locust, some herbaceous plants, legumes (i.e. beans and peanuts). We also wondered if rice was one: maybe this article will answer the question?
[http://en.wikipedia.org/wiki/Rice]
Please add more, and also notes on the readings on N saturation
page revision: 5, last edited: 07 Nov 2009 00:49