Lecture 15- Ocean Primary Production I Flashcards

(40 cards)

1
Q

why study primary production?

A
  • Base of the food web
  • Essential element of the global carbon cycle
  • Represents half of the total global photosynthesis
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2
Q

why is the global carbon a big topic?

A

it is closely related to our global warming problem

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3
Q

photosyntheis

A

consumes carbon dioxide gas to form the particulate carbon of algae

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4
Q

respiration

A

by all organisms produces carbon dioxide gas

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5
Q

difference between photosynthesis and respiration by all of the organisms

A

is what sinks to the ocean floor

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6
Q

half of oxygen comes from

A

photosynthesis in the ocean

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7
Q

global carbon cycle- atmosphere

A

0.5%

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8
Q

global carbon cycle- respiration and decay

A

0.01%

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9
Q

global carbon cycle- lithosphere

A

99.5%

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10
Q

Plankton

A

small organisms that drift with the ocean currents

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11
Q

Phytoplankton

A

small cells (often single cells but sometimes chains or colonies of many cells) that contain chlorophyll and drift with ocean currents

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12
Q

glucose from photosynthesis

A

serves as the energy source for all subsequent biochemical reactions

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13
Q

Photosynthesis only depends on

A

the availability of water, carbon dioxide, and sunlight

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14
Q

Primary production of photosynthesis requires

A

the uptake of plant nutrients for the construction of complex molecules that are needed to form new cellular components

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15
Q

magnitude of the primary production

A

depends on the availability of essential plant nutrients as well as sunlight

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16
Q

Net Primary Production (NPP)

A
  • difference between the amount of CO2 consumed by photosynthesis and the amount of CO2 produced by respiration
  • also known as the net gain or net loss of carbon within the cell
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17
Q

primary production effectively consumes carbon dioxide and forms

A

particulate organic carbon that can sink into the deep ocean

18
Q

primary production

A
  • makes oxygen

- requires light AND essential plant nutrients such as nitrogen, phosphorous, Si, and Fe

19
Q

phytoplankton

A

single celled organisms that carry out the vast majority of primary production in the ocean via chlorophyll

20
Q

diatoms

A

require silica

21
Q

Flagellates

A

mobile so they are able to avoid sinking in calm waters

22
Q

photosynthetic bacteria

A
  • able to grow at very low nutrient concentrations

- main photosynthesizers

23
Q

At compensation light level

A

photosynthesis is on the speed of respiration

24
Q

photosynthesis increases with

A

intensity of light but respiration is constant

25
At light levels below the compensation light level
- phytoplankton cells do not have sufficient light to photosynthesize fast enough to meet their basal metabolic needs - respiration exceeds photosynthesis
26
below compensation light level
Negative values of net primary production
27
At low light level
phytoplankton are light limited
28
At optimal light levels
phytoplankton are light saturated
29
At very high light levels
phytoplankton are photoinhibited
30
compensation depth
depth at which the ambient light intensity is equal to the compensation light intensity
31
The amount of nutrient needed for growth by an individual phytoplankton cell is proportional to
the cell's mass or equivalently to the cell's volume
32
amount of nutrient that can be transported into a cell is proportional to
the cell's surface area
33
smaller cells
can grow better at lower nutrient concentrations
34
4 Phytoplankton Nutrients of Interest
- Nitrogen - Phosphorous - Silica (for diatoms) - Iron
35
main source of nitrogen, phosphorous and silica
vertically mixing or upwelling of nutrient rich deep water to the surface
36
What do you expect to happen to ocean primary production under a global warming scenrtio that enhances only temperatures of the surface layer of the ocean and leaves the deep layer cold (strengthens the thermocline/pcynocline)?
decrease
37
thermocline
- hold phytoplankton near the sunlit surface ocean - significant barrier to upward mixing of nutrient rich deep water - stronger the thermal stratification, the stronger the inhibition of nutrient mixing
38
Source of Iron
- Main source of iron input to the surface ocean is from dust blowing off of continents - Not abundant in the deep ocean
39
Iron Limited Regions
Southern Ocean
40
Primary production is enhanced
- high light | - high nutrients