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

25
HNLP areas
High nutrients low production. Eg gulf of alaska, equatorial pacific ocean, antarctic ocean
26
Critical depth
Point at which total gross photosynthesis of the phytoplankton in the water column equals total respiration
27
Compensation depth
Depth at which the rate of photosynthesis equals the rate of respiration
28
PAR
Photosynthetically active radiation
29
Spring bloom
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
Summer recycling
Summer period dominated by recycling
31
Fall bloom
May occur because of breakdown of thermocline and deeper mixing bringing nutrients to the euphotic zone
32
Low light
Declining growth because of declining light