Nutrient Dynamics Flashcards
Redfield Ratio
1P:16N:106C
N:P drawdown in the environment is 16:1
Si requirement in phytoplsnkton
Only those with Si shells need it
No consistent ratio of Si:N needed
Different species use varying levels of Si to N
Dependent on species, nutrient availability and iron availability
2:1 and 0.5:1 are common
Phosphorus Cycle
Nutrient consumption occurs in the euphotic zone
Respiration releases nutrients from organic matter – occurs mainly at depth
So light and nutrients are physically separated
DIP in consumed by photosynthesis and produces organic phosphate
Respiration consumes organic phosphate and produces DIP in the euphotic zone
Most organic phosphate sinks and releases DIP in deep ocean through respiration
Mixing or upwelling required to bring nutrients to surface (most nutrients come from below)
Processes that bring nutrients to the surface
Upwelling
Mixing
Surface cooling - convention q
Mix Layer in June
Shallow mix layer
Warming surface and light winds
Mix Layer November
Mixed layer cool and deepening
Fall Nutrient/Phyto Dynamics
Decreasing light and increasing nutrients
Mix layer deepens
Nutrients in the layer below the summer mixed layer are added to the fall mix layer
Mix Layer February
Mix layer coldest and deepest
Cool surface leads to convection and strong winds
Summer Nutrient/Phyto Dynamics
High light and low nutrients
Previous productivity used up nutrients in the euphotic zone
Low productivity
Some mixing at euphotic base supplying small amount of nutrients upwards
Early Spring Nutrient/Phyto Dynamics
Increasing light and high nutrients
Mix layer shoals with warming surface
Critical depth becomes deeper than mixed layer
Bloom until nutrients consumed
Winter Nutrient/Phyto Dynamics
Low light and high nutrients
Deep mixed layer with high surface nutrients
Concentrations mixed from below
Not enough light so low productivity
Hawaii Waters Nutrient Dynamics
Mix layer never deeper than critical depth
Nutrients are always depleted
Labrador Sea Nutrient Dynamics
Winter mix layer to 1500m in some places
4 Types of Ocean Nutrient Dynamics
1) High nutrient winter and low nutrients summer
Classic bloom (North Atlantic)
2) Low nutrients always
High year-round light and shallow mix layer (Hawaii)
3) Episodic High Nutrients
Coastal upwelling zone
4) High Nutrients Always
Some other factor limits (Northern Pacific or Southern Ocean)
Typical Nitrogen and Phosphorus Levels
0-3 micromol P and 0-45 micromol N
Most data close to 16:1
Some data sit below