Phytoplankton Ecophysiology Flashcards

1
Q
  • Why are phytoplankton so important on Earth?
A

Form large blooms

Influence atmospheric chemistry and biogeochemistry of nutrient cycling

Fix ~1/2 of the total carbon fixed by photosynthesis on earth

Formed oil, siliceous and limestone deposits

Represent base of food chain supporting fisheries, marine mammals and bird populations

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2
Q
  • Describe the biological carbon pump.
A

CO2 is fixed into organic matter by photosynthesis

Organic matter passes from producers to consumers a and can sink into deeper waters

Carbon returned to seawater: Respiration by animals and algae + Bacterial decay of organic matter

Ultimate deposition locks C away in sediments = C sequestration

Atmospheric CO2 –> Algae –> Consumers –> sink –>
deposition/remineralization –> sequestration

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3
Q

What is the difference between primary productivity and phytoplankton
biomass?

A

Biomass = the standing stock
Total phytoplankton in a given area or volume of water
(# of cells/L or g chlorophyll a / L

Primary Productivity: rate at which organic matter is produced by primary producers via photosynthesis (photosynthetic rate)
g of O2 produced per m^2 per day
g of C fixed per m^2 per day

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4
Q

How can you measure Chlorophyll?

A

In vivo fluorescence: a flow-through fluorometer either towed in the water as part of a CTD package
Emits blue light which causes chlorophyll to fluoresce red light, the intensity of which can be converted to an estimate of Chl a

In vitro fluorescence: Collect water sample and filter a known amount on a filter
Extract the chlorophyll a with acetone (or methanol) for 24 h Measure chlorophyll fluorescence in a fluorometer (like above) (not flow-through).

Sattelite sensors: Convert measures of ocean color into estimates of Chlorophyll a
Enables oceanographers to examine global patterns
Depth of water imaged ranges from 5-25 m.

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5
Q

How can you measure Primary productivity?

A

Variety of methods – as long as they measure rate

Special fluorescence instruments (Scale = Minutes/Single cells)

Incubations with isotopes (Scale = Days/Specific depths)

O2 mass balance (Scale = Weeks/Mixed layer)

Satellites (Scales = Months/Globally)

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6
Q
  • Why is size relevant in phytoplankton eco-physiology?
A

It is the most important characteristic affecting phytoplankton eco-physiology
As they grow the volume grows faster than the SA

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7
Q
  • How does the surface area to volume ratio (SA/V) vary with algal size?
A

As cells grow the volume increases by radius^3 and SA increases by radius^2

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8
Q
  • Is SA/V related to growth rate? Explain how.
A

Yes as cells get larger they grow slower
Because at small size the SA/V is much higher and they have higher nutrient uptake so faster growth

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9
Q
  • How does size affect sinking?
A

Small cells are more buoyant
Large cells tend to sink faster

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10
Q

Explain the importance of considering spatial and temporal scales in phytoplankton ecology

A

Nutrient regeneration/grazing: seconds to minutes over mm

Growth rates: hours to days

Phytoplankton patches: weeks and km

Succession of species: entire season across lake basins and oceans

So the problem is how to accurately determine the abundance

What volume or area to measure and how often

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11
Q

Describe how certain aspects of the aquatic physical environment (discussed in lecture) affect phytoplankton

A

The density of freshwater changes with the temperature

Salinity increases density and depresses the freezing point to -1.91 Celcius

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12
Q
  • Give four examples of nutrients essential for phytoplankton and their role in their physiology.
A

Nitrogen: amino acids, nucelotides
Phosphorus: ATP,DNA
Silica: diatom frustules, silica skeletons
Magnesium: Chlorophyll

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13
Q
  • Define net and gross growth rates.
A

Net growth rate is r and is the gross growth rate minus the death rate
Gross growth rate: lambda is the birth rate or rate of reproduction

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14
Q

How do you calculate the growth rate of a phytoplankton population by using exponential or logistic growth models? How do you calculate
doubling time and divisions per time (e.g. divisions per day)?

A

The exponential growth rate equation is defined as follows: N = No*e^rt
This can be done as a logistic equation as well:
ln(N) = rt + ln(No)

Doubling time: td = ln(2)/r
Divisions per time = 1/td

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15
Q

Describe, using a well-labeled graph, the relationship between phytoplankton photosynthesis (y-axis) and irradiance (x-axis)? Check your notes from lecture for all the parameters included in the graph.

A
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16
Q
  • Define net and gross primary production or photosynthetic rate
A

Gross (GPP): total primary productivity
Net (NPP): GPP - Respiration rate

17
Q

What parameters of the photosynthesis-irradiance relationship are commonly used to determine the success of some phytoplankton species
relative to others?

A

Compensation point and compensation depth

Defines where an algal species can live and photosynthesize

18
Q

What is compensation depth and how do you determine it using a graph of photosynthetic rate (x-axis) versus depth (y-axis)?

A

Compensation Depth: the depth at which there is enough light to allow for enough photosynthesis to equal the respiration rate

19
Q

Based on the Michaelis-Menten nutrient uptake model or the Monod model, how can you determine which species (e.g. A or B) will outcompete the other for the limiting nutrient? Use a graph/s to answer this
question.

A

IDK

20
Q

Using well-labelled graphs, describe the Droop and Monod nutrient-based growth models for phytoplankton.

A
21
Q
  • Briefly describe the loss processes in phytoplankton populations.
A

Loss due to :
Grazing
Perennation
Sedimentation
Death or mortality
Parasitism
Washout
Competition

22
Q

Compare the general relationships and the effects to energy transfer of a marine food web dominated by larger phytoplankton cells (e.g. diatoms) with one dominated by picophytoplankton. Where in the oceans are these different types of food webs most commonly found?

A

Systems dominated by nano and diatoms:
Feed herbivorous crustaceans then fish – High nutrients and High Si:N
Occur in cold waters, temperate and boreal seas and coastal upwelling zones

Systems dominated by picoplankton: feed ciliates, crustaceans and tunicates and in the end fish and cnidarians – low nutrients
Occur in subtropical ocean gyres, summer stratified temperate oceans

Systems dominated by large flagellates: generally feed crustaceans – high nutrients and low Si:N
Occur coastal and eutrophic waters