Primary Productivity and Nutrients Flashcards

1
Q

What are nutrients?

A

Chemical substances required to support life, present as dissolved salts, used by PP for synthesis of energy-rich organic compounds and for synthesis of cells walls and skeletons

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2
Q

Why are nutrients important?

A

Regulate PP

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3
Q

What are some major nutrients used in metabolic processes?

A

N, P, Na, Mg, S, Cl, K, Ca, I, Si, Fe, Cu, Zb

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4
Q

How can nutrients affect community composition?

A

Different phytoplankton species have different nutrient requirements

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5
Q

What are some essential elements for phytoplankton growth?

A

C, N, Fe, Zn, H, P, Cu, Mo, O, Mg, Mn

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6
Q

What are some nutrients essential for only some phytoplankton?

A

Na, Se, B, Co, Si, I, Vn, Cl

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7
Q

What are some vitamins that phytoplankton require?

A

Vitamin B12, B1, Biotin

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8
Q

What are macronutrients?

A

Nutrients that are typically present in micronolar concentrations (C, N, P, H, O, Si)

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9
Q

What are micronutrients?

A

Nutrients that are typically present in the nanomolar range (Fe, Zn, Cu, Mn)

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10
Q

Are macronutrients more important than micronutrients?

A

No, they’re just more abundant than micronutrients

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11
Q

What are some limiting nutrients?

A

N, P, Si, Fe, organic substances (i.e. vitamins)

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12
Q

How are nutrients biolimited?

A

Photosynthetic organisms deplete nutrient concentrations in sunlit surface waters.

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13
Q

How are nutrients added back into the water?

A

Bacterial degradation of organic matter.

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14
Q

Where does accumulation of nutrients occur?

A

At depth, where nutrients are not used by primary producers

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15
Q

What is the redfield ratio?

A

The ratio of carbon, nitrate and phosphate (106:16:1mol/mol) from linear regression analysis of dissolved [nutrient] and the analysis of particulate matter from photosynthesis and respiration

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16
Q

What are biogeochemical cycles?

A

Nutrient, mineral cycles. The flow of nutrients between the land, atmosphere and ocean.

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17
Q

What are the components of the biogeochemical cycle?

A

Inorganic matter -> organic matter (photosynthesis) -> up through food web -> through microbial loop -> back into photosynthetic zone -> inorganic matter

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18
Q

What are biotic processes of the biogeochemical cycles?

A

Conversion of inorganics (CO2, Si(OH)4, NO3) into organics by photoplankton, decomposition of sinking organic organic matter by bacteria returns inorganic nutrients to water column

19
Q

What are the abiotic processes of the biogeochemical cycle?

A

Wind mixing and upwelling bringing nutrient-rich deep water to surface, river discharge and water runoff from land sewage outfalls

20
Q

What are the forms of nitrogen and their sources (in decreasing concentration)

A

Inorganic: N2, NO3, NO2,NH4,NH3; Organic: CO(NH2)2, Amino acids, other forms

21
Q

What is the most cited cause of limitation of PB and PP in marine ecosystems?

A

Nitrogen

22
Q

What is nitrogen used for?

A

Amino acids, building enzymes and proteins, nucleotides, ATP, chlorophyll

23
Q

What form of N is used in amino acids?

A

NH4, if phytoplankton takes in N in other forms, they must be reduced to NH4.

24
Q

How is NH4 produced?

A

Organisms use ATP and enzymes (nitrate reductase and nitrite reductase) to reduce other compounds to NH4, it can be produced as an excretory product of zooplankton, fish and other heterotrophs.

25
Q

What form of N do phytoplankton take in the most?

A

NH4 is the easiest, but NO3 is present in higher concentrations,

26
Q

What are some processes that bring N into the surface ocean?

A

Atmospheric inputes (Precipitation, N2 fixation by cyanobacteria), runoff (rivers, coastal waters, farm runoff, sewage), advection (upwelling, wind mixing), nitrification

27
Q

What are processes that contribute to loss of N from the surface ocean?

A

Sedimentation of phytoplankton, zooplankton, fecal pellets, marine snow to deep waters, and seafloor basin, denitrification (formation of reduced N compounds from NO3 - bacterial process where they use nitrogen as an oxygen source)

28
Q

What affects the location of the nutricline?

A

Physical properties of the water column

29
Q

What is new production?

A

The portion of primary production that results from the utilization of new nitrogen (NO3, N2)

30
Q

What is regenerated production?

A

The portion of primary production that results from the utilization of regenerated nitrogen

31
Q

What does new production equal?

A

Export production (over the long term, in a steady state ocean)

32
Q

What affects the proportion of new/regenerated production?

A

The type of system there is: if there is more regenerated production, small organisms dominate (greater SA:V ratio), if there is more new production, larger organisms dominate (i.e diatoms)

33
Q

What are some sources of silicon to the surface ocean?

A

River input, groundwater, weathering, hydrothermal vents, deposits, upwelling/wind mixing

34
Q

What are some processes that contribute to the loss of Si from surface waters?

A

Sedimentation of diatoms and other silica-containing organisms (radiolarians, silicaflagellates) which go to deeper waters/seafloor burial

35
Q

What are the main biogeochemical fluxes internall cycling Si in the oceans?

A

Production and dissolution of biogenic Si

36
Q

What affects the rate of nutrient uptake?

A

Transport mechanism

37
Q

What is the rate of nutrient uptake in passive diffusion?

A

Uptake rate is proportional to the concentration of the nutrient (nutrients go from [low] to [high]

38
Q

What is the rate of nutrient uptake in facilitated diffusion/active transport?

A

Carriers of nutrients can be saturated as the concentration of the nutrient increases (different nutrients have different carriers)

39
Q

What is Ks?

A

The concentration of nutrients at Vmax/2

40
Q

What does it mean if a nutrient has a low Ks?

A

There is a higher affinity of the carrier for a particular molecule/iron (faster at uptake)

41
Q

What is the paradox of the plankton?

A

Why are there so many different phytoplankton species coexisting at one time in the oceans?

42
Q

How to answer the paradox of the plankton?

A

Although the auphotic zone appears homogeneous, there are vertical gradients in temperature, salinity, light, nutrients, and miximing moves phytoplankton throughout the surface layer, so they experience average conditions.

43
Q

Why don’t phytoplankton outcompete each other since they need the same things?

A

Each species has slightly different nutrient requirements, Ks, Kl, so at any time some species will do better than others. But nutrient concentrations and phystical characteristics can change quickly, making favorable conditions for different species, so the balance can go back and forth (Contemporaneous disequilibrium)