Chapter 2: Primary Production Flashcards

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1
Q

Name all the different sizes of plankton

A
Femtoplankton - 0.02-0.2um
Picoplankton - 0.2-um
Nanoplankton - 2-20um
Microplankton - 20-200um
Mesoplankton - 0.-20mm
Macroplankton - 2-20cm
Megaplankton - 0.2-2m
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2
Q

Describe Diatoms

A

Class Baccilariophyceae

  • silica frustule
  • no visible flagella
  • centric or pinnate
  • pelagic/benthic forms
  • solitary/colonial
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3
Q

Describe dinoflagellates

A

Class Dinophyceae

  • 2 visible flagella
  • cellulose plates
  • typically solitary
  • reproduce via mitosis, no size change
  • harmful algae in blooms
  • some bioluminescent
  • many heterotrophs
  • endosymbiotic zooxanthellae (symbiotically work with other species, illumination etc.)
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4
Q

Describe Haptophyceae

A

Naked cells, mainly solitary forms

Motile: 2 flagella, 1 haptonema

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5
Q

Describe Coccolithophores

A

Covered in coccolits (small calcium plates)

-solitary w/ complex life cycles

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6
Q

What is probably the most common phytoplankton in the ocean?

what does it contribute?

A

Prochlorophytes (a cyanobacteria)

  • > 30-70% of Chl.a in open oceans
  • > 30-80% of total ocean productivity
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7
Q

Name the big 3 algal toxins and human health issues

A
  • PSP (paralytic shellfish poisoning)
  • NSP (Neurotoxic shellfish poisoning)
  • DSP (Diarrhetic shellfish poisoning)
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8
Q

Photosynthesis equation.

A

6CO(2) + 6H(2)O C(6)H(12)O(6) +6O(2)

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9
Q

name 3 ways to measure primary production

A

1) from the reaction, measure changes in O2 or in CO2
2) Light/dark-bottle method, where you use a clear (photosynthesis) + opaque (respiration) bottle, and measures of oxygen are taken by winkler titration.
3) 14C method where radioactive carbon is added to the water sample, and tested for algae growth.

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10
Q

Photosynthesis in the ocean is affected by:

A
  • Radiation level
  • Availability of nutrients
  • Water mass properties
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11
Q

In the light spectrum, what is the Photosynthetic Active Radiation (PAR) range?

A

the visible light spectrum, from 380-710nm

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12
Q

name some systematic and unsystematic variations for solar radiation

A

systematic: with season, over the day.
unsystematic: cloud cover, vegetation, competition

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13
Q

Light penetration in the water column depends on:

A
  • water clarity (absorption, reflectance)

- wavelength (red colors are absorbed more rapidly than blue)

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14
Q

Which law describes the attenuation of radiation?

A

Beer’s law

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15
Q

Compensation depth

A

The depth in the water column where photorespiration = photosynthesis
(ie: primary productivity = 0)

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16
Q

what are the four main nutrient salts?

A

Nitrate, Nitrite, ammonia and phosphate

17
Q

describe the phytoplankton community succession of temperate and tropical seas.

A

Temp:
small diatoms->large diatoms -> dinoflagellates
Trop:
coccolithophors and dinoflagellates dominate throughout the seasons, but minor diatom blooms are common.

18
Q

what factors are proposed to regulate the succession of phytoplankton?

A
  • temperature
  • changes in nutrient salt concentrations
  • biological conditioning
  • biological control
19
Q

What is the theoretical reason for ‘high nutrient low chlorophyl’ subarctic waters, and how does iron influence this?

A
  • waters may not receive enough light
  • too much grazing pressure
  • not enough iron (iron is introduced from land, and may not reach these offshore areas)
20
Q

what is the typical elemental composition of an algal cell?

A

protein: 40%
carbohydrate: 40%
lipid: 15%
nucleic acid: 5%

21
Q

how is the ocean’s capability of acting as a ‘carbon sink’ being affected by global warming?

A

1) as the oceans warm, they have less capability of absorbing the CO2
2) As more CO2 is absorbed there will be a reduction of pH in the water, resulting in the process of ocean acidification.

22
Q

the main limiting inorganic nutrients are what?

A
  • nitrogen
  • phosphorus
  • some areas iron
23
Q

what large-scale processes influence the rate of primary productivity in the ocean?

A

frontal systems, gyres, river plumes and coastal upwelling

they transport nutrient-rich waters to the sea surface