Nutrient Dynamics Flashcards

1
Q

Redfield Ratio

A

1P:16N:106C
N:P drawdown in the environment is 16:1

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2
Q

Si requirement in phytoplsnkton

A

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

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3
Q

Phosphorus Cycle

A

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)

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4
Q

Processes that bring nutrients to the surface

A

Upwelling
Mixing
Surface cooling - convention q

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4
Q

Mix Layer in June

A

Shallow mix layer
Warming surface and light winds

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4
Q

Mix Layer November

A

Mixed layer cool and deepening

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4
Q

Fall Nutrient/Phyto Dynamics

A

Decreasing light and increasing nutrients
Mix layer deepens
Nutrients in the layer below the summer mixed layer are added to the fall mix layer

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4
Q

Mix Layer February

A

Mix layer coldest and deepest
Cool surface leads to convection and strong winds

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4
Q

Summer Nutrient/Phyto Dynamics

A

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

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5
Q

Early Spring Nutrient/Phyto Dynamics

A

Increasing light and high nutrients
Mix layer shoals with warming surface
Critical depth becomes deeper than mixed layer
Bloom until nutrients consumed

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5
Q

Winter Nutrient/Phyto Dynamics

A

Low light and high nutrients
Deep mixed layer with high surface nutrients
Concentrations mixed from below
Not enough light so low productivity

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6
Q

Hawaii Waters Nutrient Dynamics

A

Mix layer never deeper than critical depth
Nutrients are always depleted

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7
Q

Labrador Sea Nutrient Dynamics

A

Winter mix layer to 1500m in some places

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8
Q

4 Types of Ocean Nutrient Dynamics

A

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)

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9
Q

Typical Nitrogen and Phosphorus Levels

A

0-3 micromol P and 0-45 micromol N
Most data close to 16:1
Some data sit below

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10
Q

Nitrogen Cycle

A

Primary production consumes nitrate or ammonium in euphotic zone
Respiration releases ammonium in euphotic zone
Phytoplankton prefer ammonium

Organic phosphate sinks into dark ocean and respired to produce ammonium
Nitrification uses ammonium and O2 to produce nitrate in dark ocean (chemosynthesis)
Light inhibits nitrification, and little ammonium in dark O2 rich waters

Mixing and upwelling brings nitrate to surface
New production fueled by nitrate
Regenerated production fueled by ammonium

Denitrification comsumes nitrate when oxygen not available (NO3 to N2)

11
Q

Where does denitrification occur

A

Where O2 is not available

Anoxic Saanich Inlet: nitrate is consumed, ammonium builds up

North/South Eastern Tropical Pacific and Arabian Sea

12
Q

Nitrogen Fixation

A

Adds N to cycle
Use N2 gas to create more bioavailable Nitrogen
Energy intensive – only advantageous when nitrate and ammonium low

13
Q

Membrane Importance

A

Hydrophilic head and hydrophobic tail
Polar ions – phosphate, nitrate and ammonium can’t move across
Need transport enzymes to move through

14
Q

Energy Associated with Transport Enzymes

A

Specific transport enzymes for each nutrient
Need to make many

Transport Requires energy

There is therefore an energetic cost to make and use enzymes

15
Q

Small Size Advantage

A

Surface area to volume ratio
Smaller cell more SA per volume

15
Q

Why does Surface area matter and why does volume matter

A

Surface area matters for nutrient uptake
Volume matter for growth rate

16
Q

When is small cell size selected

A

Smaller cell more efficient nutrients supplied for growth
Nutrient limitations selects small cell size

17
Q

Growth vs Nutrients

A

At low nutrient levels: growth increases with increasing nutrients

At high nutrients: no relationship (other factor must limit)

18
Q

What does kN tell us?

A

Lower kN indicates more efficient nutrient uptake at low nutrient concentration
Will outcompete at low nutrients

19
Q

What drives species succession over blooms?

A

Mix layer nutrients concentration decreases over the bloom and light levels increase

These changes drive species succession

20
Q

Dominant species types in bloom successions

A

Early Spring: low light so low kI species dominate
Later: High nutrients and high light so higher Pmax and Gmax species dominate
Later Still: Low nutrients so low kN species dominate

21
Q

Transport Enzymes and Nutrient Uptake Tradeoff

A

More transport enzymes per SA mean higher nutrient uptake
But energetic cost tends to suppress Gmax

Species kN can acclimatize based on the environment, and adjust transport enzymes based on conditions

The energetic cost of enzymes only advantageous at low nutrient concentrations

22
Q

How are the requirements for Si different from N and P

A

Only phytoplankton with Si shells require Si and it has no consistent ratio

23
Q

Why do you think the plankton requirements for nutrients are so similar to the ratio of their availability in ocean water?

A
24
Q

Phytoplankton are generally very small, particularly compared to terrestrial plants. What advantages are conferred by such small size?

A

They don’t sink as easily and they can take up nutrients better due to SA:V ratio

25
Q
A