Productivity Flashcards

1
Q

what drives the productivity in the ocean?

A

plankton and coastal macroalgae (kelp forests)

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2
Q

what are phytoplankton?

A
  • microscopic algal cells that use chlorophyll to photosynthesize, uses sunlight and nutrients to make proteins, fats and carbs
  • live in upper part of ocean where sunlight hits
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3
Q

what are zooplankton?

A

microscopic to macroscopic animals that graze on phytoplankton

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4
Q

how are phytoplankton distributed?

A

discontinuous patches
- non-random clumped population
- concentrated at interfaces between water bodies

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5
Q

what color on a map shows the highest productivity?

A
  • red
  • most nutrients
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6
Q

why are there patterns of productivity?

A
  • turbulence and current transport at many spatial scales (conveyor belt, marginal seas)
  • different physical conditions seasonally and spatially
    ->light, temp, salinity
  • spatially discontinuous levels of grazing by zooplankton - food is patchy
  • localized reproduction -> max and min productivity depends on sunlight
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7
Q

what is the main cause of productivity?

A

turbulence or mixing

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8
Q

what causes spreading and mixing?

A

currents and wind

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9
Q

what causes Langmuir circulation?

A

currents converging

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10
Q

what causes eddies?

A

currents and coastlines

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11
Q

what do seasonal patterns depend on to cause differences?

A

latitude
- depending on the sunlight phytoplankton are either abundant or non-existent which causes zooplankton to fluctuate

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12
Q

which latitude has consistent levels of phytoplankton?

A

tropical

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13
Q

describe the mixing depth in the winter

A
  • storms mix water to a greater depth
  • less light
  • light doesn’t reach as deep so nutrients are deeper
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14
Q

describe the mixing depth in spring

A
  • water is mixed less
  • more light
  • light penetrates further
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15
Q

what changes as a result of mixing depth?

A

blooms and declining phytoplankton

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16
Q

compensation depth

A

photosynthesis = respiration
- above this depth is where phytoplankton photosynthesize

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17
Q

mixing depth

A

depth to which water column is mixed by winds
determines critical depth
-> more respiration than photosynthesis

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18
Q

critical depth

A

depth above which total oxygen produced in the water column = total oxygen consumed
- more respiration = more zooplankton to control phytoplankton = no bloom

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19
Q

what happens when the mixing depth is less than critical depth?

A

bloom

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20
Q

what happens when the mixing depth is more than the critical depth?

A

no bloom

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21
Q

what happens as a result of winter mixing?

A

brings nutrients to the surface

22
Q

what happens in spring sun to the bloom?

A

heats water and less mixing by wind so thermocline develops and cells are in nutrient rich calmer water = bloom

23
Q

how do you catch plankton?

A

plankton net
- cod end - name of tube at the end that catches plankton

24
Q

why do we study plankton?

A

carbon cycle -> phyto = uptake
zoo -> respiration

25
what nutrients do phytoplankton need for growth?
- nitrogen - phosphorus - silicon - iron
26
what is nitrogen used for?
make proteins
27
what 3 forms does N come in?
ammonium -> excretion by animals in water column (taken up the fastest) nitrate - most abundant nitrite - less common
28
what does nitrate and nitrite need?
need enzymatic reduction to convert to ammonium - nitrate reductase and nitrite reductase
29
how is N formed?
new production - deep waters by mixing or upwelling regenerated production - nutrients derived from excretion in surface waters nitrogen fixation - some algal phytoplankton cells
30
purpose of P
- synthesis of ATP - required for lipids, DNA, fats/oils
31
what forms do P come in?
- dissolved inorganic phosphate - particulate phosphorus from sediments/rivers - some dissolved P in organic molecules
32
redfield rations
- constant ratio of N:P = 16:1 in oceans - phyto have 16:1 ratio - ocean have 14.7:1 ratio - nitrogen fixation by some plankton might make difference
33
why is the ratio of N to P constant in all ocenas?
residence time of nutrients way longer than mixing time of oceans
34
where does P come from?
land
35
why is Si needed?
for diatom skeletons - from land by weathering
36
what is Fe used for?
cofactor in oxygen production step of photosynthesis - crucial in parts of ocean where N is not limited
37
what are the areas of where N is not limited called?
high nutrient/low productivity areas (HNLP)
38
where are HNLP found?
antarctic ocean north Pacific
39
how do Si and Fe enter oceans?
by wind as dust
40
where is a major source of iron dust?
Sahara
41
what controls phytoplankton growth?
bottom up feeding
42
what are organic trace substances important for?
auxotrophic
43
how is C produced at the ocean surface taken deep?
physical: mixing at poles - taking dissolving CO2 down with cold saline water - bringing up CO2 from deep biological: productivity - taken up into phytoplankton by photosynthesis - eaten and moved down as organic matter
44
who eats most of the carbon?
zooplankton and nekton
45
carbon sink
sinking water - ecosystems where C is sequestered
46
what are Larvacean houses?
big structures of mucus and cellulose that allow filter feeders to get C
47
how is C transported to the seafloor?
larvaceans
48
how is C caught?
- put traps for sediment - caught larvacean houses
49
how many blooms do polar regions have?
1
50
how many blooms do temperate regions have?
2