Lecture 5 cards Flashcards

1
Q

Formula for photosynthesis

A

6 CO2 + 6 H2O = C6H12O6 + 6 O2

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2
Q

How do we measure primary productivity

A

O2 evolution or C14 uptake

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3
Q

Which increases more with temperature, photosynthesis or respiration?

A

Respiration, resulting in decrease in net productivity and more carbon dioxide, negative feedback loop, decreased biomass in terrestrial systems also

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4
Q

Expected effect of 4C increase in temperature

A

20% increase in net primary production and 43% increase in oxygen consumption

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5
Q

Redfield ratio

A

106 C : 16 N : 1 P

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6
Q

Monod relationship

A

Formula for direct growth on substrate

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7
Q

Michaelis-Menten relationship

A

General enzyme relationship, how rapidly nutrients get into the cells

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8
Q

Droop relationship

A

Growth on internal substrate

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9
Q

Variable internal stores model

A

2 steps, uptake and utilization (view slide 34)

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10
Q

DIP

A

Dissolved inorganic phosphotous, HPO4(2-). This is what algae use.

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11
Q

N2

A

Dissolved nitrogen gas in equilibrium with the air

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12
Q

DIN

A

Dissolved inorganic nitrogen, NH4(+), NO2(-), NO3(-). Algae use these ions.

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13
Q

Nitrate assimilation

A

NO3(-) to NH4(+), requires energy and nitrate reductase

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14
Q

Nitrification

A

NH4(+) to NO3(-), energy source for bacteria

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15
Q

Denitrification

A

NO3(-) to NO2(-) to N2O to N2. Anaerobic, requires energy-rich organics

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16
Q

Nitrogen fixation

A

N2 to NO3(-), anaerobic, reduced to oxidized form, cyanobacteria

17
Q

Ammonification

A

Organic matter to NH4(+)

18
Q

Amino acid synthesis

A

NH4(+) to amino acids

19
Q

Trichodesmium thiebautii

A

Cyanobacterium in the open ocean, requires moderately warm temperature and non-rough seas. Fixes nitrogen, does not have heterocysts, requires a lot of iron to fix.

20
Q

Sources of nitrogen

A

Uptake into phytoplankton and bacteria, regeneration of N from food web, upwelling from below mixed layer, primary production

21
Q

Old production of nitrogen

A

Recycling and regeneration

22
Q

New production of nitrogen

A

Upwelling and N2 fixation

23
Q

Losses of nitrogen to the atmosphere

A

Volatilization, denitrification, sedimentation

24
Q

Volatization of nitrogen

A

NH3

25
Q

HNLP areas

A

High nutrients low production. Eg gulf of alaska, equatorial pacific ocean, antarctic ocean

26
Q

Critical depth

A

Point at which total gross photosynthesis of the phytoplankton in the water column equals total respiration

27
Q

Compensation depth

A

Depth at which the rate of photosynthesis equals the rate of respiration

28
Q

PAR

A

Photosynthetically active radiation

29
Q

Spring bloom

A

Caused by increases in light, abundant nutrients that have accumulated over winter period, shallower critical depth. Brought to an end by nutrinet limitation and increases in grazing.

30
Q

Summer recycling

A

Summer period dominated by recycling

31
Q

Fall bloom

A

May occur because of breakdown of thermocline and deeper mixing bringing nutrients to the euphotic zone

32
Q

Low light

A

Declining growth because of declining light