Oceanography set 4

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149 Terms

1
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What does it mean that plankton have the same phenology as land plants?

They follow similar seasonal cycles of growth and productivity, with blooms during periods of maximum light and nutrients

2
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When does the phytoplankton bloom occur in the Northern Hemisphere?

Around May

3
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Describe phytoplankton productivity in tropical oceans

It remains fairly constant year-round

4
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Describe phytoplankton productivity in polar oceans

Blooms occur during maximum sunlight and ice melt (June/July), with little stratification

5
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Describe phytoplankton productivity in temperate oceans

Two blooms: one in spring (March/April) and one in fall (September/October). Strong stratification develops in spring as nutrients are used up

6
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What is the photic zone?

The upper 0-200 m of the ocean where sunlight supports photosynthesis

7
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What is the compensation depth?

About 125 m deep, where the rate of photosynthesis equals the rate of respiration

8
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What happens above the compensation depth?

The ecosystem produces oxygen and consumes carbon dioxide

9
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What happens below the compensation depth?

Respiration dominates, oxygen is consumed, and carbon dioxide is produced

10
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Does respiration occur at all depths?

Yes

11
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What type of organisms are diatoms?

Eukaryotic protists (unicellular algae)

12
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Where are diatoms most important?

In coastal areas, especially during spring blooms

13
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What are diatom shells made of?

Silica/glass, called frustules

14
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What nutrients do diatoms require?

Silica, nitrate, and phosphate

15
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Can diatoms swim?

No, but they can regulate buoyancy and sometimes migrate vertically

16
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What are coccolithophores?

Single-celled eukaryotic protists encased in calcium carbonate disks (coccoliths)

17
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Where do coccolithophores live?

In the photic zone, since they are photosynthetic

18
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What do coccolithophores’ calcium carbonate disks do?

They may help shade the cell from excessive sunlight

19
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What can large coccolithophore blooms cause?

Milky-white seawater

20
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What are dinoflagellates?

Eukaryotic protists with cellulose plates and two flagella for movement

21
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How do dinoflagellates move?

With flagella that allow vertical migration toward light

22
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What feeding strategies do dinoflagellates use?

They can be autotrophic (photosynthetic), heterotrophic (consume others), or mixotrophic (both)

23
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Where do dinoflagellates thrive?

In nutrient-rich (eutrophic) waters

24
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What are red tides and what causes them?

Toxic blooms caused by certain dinoflagellates

25
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What is Noctiluca?

A bioluminescent dinoflagellate (“light at night”)

26
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What type of organisms are cyanobacteria?

Photosynthetic bacteria

27
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What is the size range of cyanobacteria?

0.2-2 microns (picoplankton)

28
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When did oceanographers realize cyanobacteria’s abundance and importance?

In the 1980s

29
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What is the modern ecological role of cyanobacteria?

They likely dominate photosynthesis and oxygen production in today’s oceans

30
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What major event are cyanobacteria responsible for in Earth’s history?

The initial oxygenation of Earth’s atmosphere about 2 billion years ago

31
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What does “algae” refer to?

Photosynthetic eukaryotes (includes most phytoplankton, but not cyanobacteria)

32
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What are macroalgae?

Large algae like seaweeds and kelp

33
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What are protists?

Mostly unicellular eukaryotes that can reproduce sexually or asexually and have great genetic diversity

34
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What type of dinoflagellates live in symbiosis with coral polyps?

Zooxanthellae

35
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What do dinoflagellates provide to coral?

Food (through photosynthesis)

36
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What do corals provide to dinoflagellates?

Protection from predation

37
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What causes coral’s bright colors?

Pigments in zooxanthellae

38
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What is coral bleaching?

When stressed zooxanthellae die or leave the coral host, often due to high temperature

39
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What organism causes red tides in Florida?

Karenia brevis, a red-pigmented dinoflagellate

40
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What diatom is known for harmful blooms in Rhode Island?

Pseudo-nitzschia

41
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Why are HABs harmful?

Some algae produce toxins that bioaccumulate in higher trophic levels

42
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Which organisms can accumulate algal toxins?

Clams, fish, and humans

43
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Have HABs always existed?

Yes, they date back to ancient times and appear in historical texts

44
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Why might HABs be increasing in frequency?

More nutrient pollution, species introductions, and increased monitoring

45
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What two factors most commonly limit primary production in the ocean?

Light and nutrients

46
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What is fixed nitrogen used for?

Making proteins

47
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What is phosphate used for?

Cell membranes and DNA/RNA

48
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Which organisms require silicate?

Diatoms and some plants

49
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Who discovered that nutrient ratios in seawater match phytoplankton composition?

Alfred Redfield

50
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What is the Redfield ratio for phytoplankton?

106 C : 16 N : 1 P

51
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What is the extended Redfield ratio for diatoms?

106 C : 16 N : 1 P : 16 Si

52
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What does the Redfield ratio suggest about nutrients in seawater?

They are largely recycled from the decomposition of phytoplankton

53
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What does Liebig’s Law of the Minimum state?

Growth is limited by the scarcest resource, not the total available amount

54
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Examples of limiting nutrients in the ocean?

N, P, Si, and micronutrients like Fe, Mn, Cu, Zn, B, Mo

55
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What organisms supply new nitrate to the ocean?

Nitrogen-fixing bacteria

56
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Where does most phosphate come from?

Runoff from continents

57
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What are major anthropogenic sources of nutrients?

Wastewater treatment and agricultural runoff

58
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What does respiration consume?

Oxygen

59
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What does respiration produce?

Carbon dioxide

60
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How does respiration contribute to nutrient cycling?

It regenerates nutrients

61
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What is marine snow?

Sinking biomass produced by plankton, representing dead phytoplankton

62
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Why is marine snow important?

It helps scientists understand how nutrients are recycled in the ocean

63
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What tool is used to study sinking organic matter?

Sediment traps

64
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What happens to nutrients and oxygen at the surface of the ocean?

Nutrients are depleted by photosynthesis, oxygen is high

65
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How do nutrients and oxygen change with depth?

Oxygen decreases while nutrients increase due to remineralization

66
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Why are deep waters below the thermocline high in both nutrients and oxygen?

They inherit oxygen and nutrient-rich water from deep water formation in polar regions

67
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Who fixes nutrients into biomass?

Autotrophs (primary producers)

68
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How do nutrients move through marine ecosystems?

From producers → consumers → decomposers → back to seawater

69
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How are deep nutrients returned to the surface?

upwelling

70
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What CO₂ levels correspond to warm interglacial periods?

High CO2

71
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What CO₂ levels correspond to cold glacial periods?

Low CO2

72
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What causes glacial–interglacial changes in atmospheric CO₂?

Changes in deep ocean storage of dissolved inorganic carbon

73
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During glacial periods, where does carbon shift?

From the atmosphere → into the ocean

74
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How fast is atmospheric CO₂ currently increasing?

About 2-2.5 ppm per year

75
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What fraction of human CO₂ emissions does the ocean absorb?

About one-third to one-half

76
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Why is ocean CO₂ especially high in the North Atlantic?

Deep water formation brings down CO2 from the surface

77
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How much more inorganic CO₂ does the ocean contain compared to the atmosphere?

About 50 times more

78
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What are the two major processes that regulate atmospheric CO₂ via the ocean?

The solubility pump and the biological pump

79
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What does the solubility pump do?

Moves inorganic carbon from the atmosphere into the deep ocean via physical and chemical processes

80
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Where is CO₂ most soluble?

In cold water, especially at the poles (CO2 sinks)

81
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What determines air-sea CO₂ flux?

CO2 solubility (temperature, chemistry) and thermohaline circulation

82
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Which form of dissolved inorganic carbon is dominant in seawater?

Bicarbonate

83
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What happens when carbonate upwells to the surface?

It reacts with atmospheric CO2 to form bicarbonate

84
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What drives the biological pump?

Primary producers (phytoplankton)

85
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Why is carbon below the thermocline important for climate?

It’s isolated from the atmosphere and acts as a long-term CO2 sink

86
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What controls the strength of the biological pump?

Nutrient availability

87
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Why is carbon export inefficient?

Most organic carbon is respired as it sinks

88
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What percentage of organic matter leaves the epipelagic zone?

5-10%

89
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What percentage reaches the deep ocean?

1-5%

90
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What percentage reaches the seafloor sediment?

About 0.1%

91
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Q: What did John Martin (1990) propose about low CO₂ during glacial periods?

That low CO2 was caused by a stronger biological pump driven by more iron-rich dust fertilizing the ocean

92
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How did glacial winds contribute to stronger biological pumping?

They transported iron-rich soil dust into the ocean, stimulating phytoplankton growth

93
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What does HNLC stand for?

High Nutrient, Low Chlorophyll

94
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Why are nutrients “left on the table” in HNLC regions?

Because phytoplankton growth is limited by micronutrients, especially iron

95
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What characterizes HNLC regions?

High surface nutrients and low phytoplankton productivity

96
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Why are micronutrients important for primary producers?

They are required in small amounts for enzymes involved in biochemical processes

97
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How do Fe and Zn vertical profiles compare to major nutrients?

Both are depleted in surface waters and abundant in deep waters

98
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Why is iron limited in many parts of the ocean surface?

Because there is low iron input from both upwelling/mixing and atmospheric dust

99
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What do microcosm (bottle) experiments show about iron?

Adding iron to iron-limited seawater increases phytoplankton productivity

100
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How are field iron fertilization experiments performed?

A small ocean patch is enriched with iron and a tracer, then tracked via ships and satellites