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Nutrient Cycling

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Energy, as we understand it, moves in a straight shot' i.e. it is ... Moves between organisms and atmosphere as a consequence of photosynthesis and respiration. ... – PowerPoint PPT presentation

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Title: Nutrient Cycling


1
Nutrient Cycling
  • BIO 325 Chapter 19

2
Generalizations
  • Matter moves around the earth in cycles
  • Energy, as we understand it, moves in a straight
    shot i.e. it is not cycled
  • We will look at decomposition
  • We will look at the following cycles
  • Phosphorus
  • Nitrogen
  • Carbon (already looked at with global warming)
  • Affects of disturbance on cycles

3
Phosphorus
  • Why is it important to organisms?

4
Phosphorus Cycle
  • Global phosphorus cycle does not include
    substantial atmospheric pool.
  • Largest quantities found in mineral deposits and
    marine sediments.
  • Much of this in forms not directly available to
    plants.
  • Slowly released in terrestrial and aquatic
    ecosystems via weathering of rocks.

5
Phosphorus cycle
6
Phosphate in Florida
  • Marine deposits
  • Made into phosphate fertilizer
  • Most U.S. phosphate fertilizer comes from Florida
  • Hardee, Polk counties

7
Why is Nitrogen important to organisms?
8
Nitrogen Cycle
  • Includes major atmospheric pool - N2.
  • Only nitrogen fixers can use atmospheric supply
    directly.
  • Energy-demanding process.
  • N2 reduced to ammonia (NH3).
  • Once N is fixed it is available to organisms.
  • Upon death of an organism, N can be released by
    fungi and bacteria during decomposition.

9
Nitrogen cycle
10
Nitrogen Fixation
Root Nodules
  • Atmospheric nitrogen converted to ammonia
  • N2 ? NH4 or NH3
  • Conducted either by soil bacteria
  • Or by bacteria in roots (e.g. Rhizobium)
  • Example Alder

11
Nitrogen Fixation found in legumes
Root Nodules
12
Denitrification is opposite of fixation
  • Denitrification
  • or NO2 or NO3 ? N2
  • Also occurs by bacteria
  • Nitrogen goes into atmosphere

13
Carbon cycle
  • Moves between organisms and atmosphere as a
    consequence of photosynthesis and respiration.
  • In aquatic ecosystems, CO2 must first dissolve
    into water before being used by primary
    producers.
  • Although some C cycles rapidly, some remains
    sequestered in unavailable forms for long periods
    of time.

14
Carbon Cycle
15
Decomposition
  • It happens
  • You will experience it
  • Hopefully, after you die

16
Changes in Carbon Cycle results in
  • Global climate change changes
  • Local/regional disturbance (e.g. storms, floods,
    fires) regime changes
  • Vegetation (forests)
  • Example change of forest fires in the Western
    U.S.
  • 60 minutes video

17
Decomposition varies with
  • Temperature, moisture and chemical composition

18
Lignin vs. nitrogen content in leaves
  • Lignin makes leaves tough
  • Resist fungal decomposition

19
Memorize this molecule!!
Our Dear Friend, Lignin
20
Nitrogen cycling changes by invasive species
  • N-fixing tree Myrica faya is altering N dynamics
    of Hawaiian ecosystems.
  • Introduced in late 1800s as ornamental or
    medicinal plant, and later used for watershed
    reclamation.
  • Nitrogen fixation by Myrica large N input.

21
Dont forget
  • 1st test next Friday ,November 2nd (changed from
    Wednesday ,Oct. 31st)
  • Powerpoints and study guide will be posted on
    website faculty.saintleo.edu/miller
  • 2nd reading due on November 5th

22
Ecosystem is Completely Altered with M. faya
  • M. faya high N inputs allow other species to
    invade
  • Also this N-fixing ability allows for M. faya to
    overtop native trees and shade them out
  • High N content of leaves changes soil
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