primary production & seasonality Flashcards

1
Q

summarise photosynthesis in terms of the photosystems

A

Light into PSII -> energy transferred across membrane -> provides energy to PSI

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2
Q

what happens to energy as wavelength decreases

A

energy also decreases
explain why plants don’t utilise radio waves (low energy) and prioritise visible wavelengths instead

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3
Q

what happens to absorption in water as wavelength increases

A

absorption also increases

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4
Q

what wavelengths get absorbed

A
  • ~50% infra red >780 nm
  • ~50% visible spectrum ~400-~700 nm
  • <1% ultraviolet <380 nm
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5
Q

why are only blues and blacks visible in deep waters

A

rest has been fully absorbed by water

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6
Q

what wavelengths have Things like phytoplankton have to evolve to make use of

A

the more blue/green parts of the visible spectrum
- also contain additional pigments to increase the amount of energy they are able to make use of e.g. photosynthetic carrotenoids

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7
Q

what happens to photosynthesis as light intensity increases

A

also increases - up to a certain point…..

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8
Q

what happens when phytoplankton receives too much light

A

sterilisation of the plankton will occur

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9
Q

how do plankton cope with sterilisation due to too much light

A

photoprotectant carrotenoids -> absorb the same light as the photosynthetic carrotenoids but do not pass it on to chlorophyll a (dissapate it as heat instead to get rid of it)

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10
Q

what allows us to identify groups of phytoplankton

A

The different proportions and types of accessory pigments

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11
Q

formula to calculate the diffuse attenuation coefficient (m-1) -> how mercy the water is

A

Iz = I0 e-kz (make K the subject)
big k = mercy water
Use k to calculate I (light) at any depth in the water column

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12
Q

what’s a thermocline

A

zone of sharply changing temperature

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13
Q

what’s a Halocline

A

zone of sharply changing salinity

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14
Q

what’s a Pycnocline

A

zone of sharply changing density

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15
Q

what’s a Ergocline

A

energy gradient (amount of energy needed to mix water down to that depth)

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16
Q

where does the most production occur

A

the mixed layer

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17
Q

what’s planktons movement controlled by

A

the surface mixed layer (SML) -> depth varies depending on wind speed and heating

18
Q

how to calculate average irradiance (I) in the SML

A

k (attenuation) x h (depth of SML)
- Phytoplankton experience fluctuating light in this SML

19
Q

Surface mixed layers in winter vs summer

A
  • winter it is deep + less light (but more nutrients)
  • summer its more shallow + more light (but less nutrients)
20
Q

formula to calculate gross primary production (Pg)

A

Ke + (I)
- Pmax = max rate of photosynthesis
- Ke = half-saturation constant
- (I) = ambient PAR
- Pmax and Ke varies between species, leading to succession of different phytoplankton species

21
Q

formula to calculate net primary production (Pn)

A

Ke + (I - Ic)
- takes respiration into consideration
- Ic = amount of light needed to balance respiration of the plankton at that depth

22
Q

formula to calculate compensation depth (Zc)

A

k
- depth at which photosynthetic production = respiratory losses i.e. Depth at which = I = Ic
- Compensation depth = bottom of euphotic zone
- Describes plankton when they are still (problem – they always move with the water)

23
Q

what’s critical depth (Zcrit)

A

depth of a SML in which respiration = photo over 24 h
- aka the depth at which the amount of light available for photosynthesis is just enough to support the metabolic needs of phytoplankton

24
Q

what happens when the critical depth is smaller and bigger than the depth of SML

A
  • If depth of SML > Zcrit -> no growth
  • If depth of SML < Zcrit -> growth (spring bloom) - getting enough energy from the sun to support increase in population
25
Q

what determines whether a community is able to survive

A

balance of total energy used for respiration in 24hr + total energy used for photo in 24hr

26
Q

what kind of community do we have when enery used for respiration is more and less than that used for photosynthesis

A
  • If total energy used for resp in 24hr > total energy used for photo in 24hr, community = heterotrophic – no growth of phytoplankton
  • If total energy used for resp in 24hr < total energy used for photo in 24hr, community = autotrophic – P > R = growth
27
Q

is phytoplankton conc higher in winter or summer

A

summer

28
Q

what does Phyto productivity, biomass & composition rely on

A

light, nutrients, mixing & grazing
- usually follows a seasonal pattern

29
Q

describe the thermocline in summer

A

quite steep - less energy, more light

30
Q

describe the thermocline in fall/autumn

A

Much smaller thermocline – less light, more energy (wind etc - more mixing)

31
Q

describe the thermocline in winter

A

very deep - Entire seabed = mixes waters - Loads of energy (more turnover), dark

32
Q

describe the thermocline in spring

A

Build-up of thermocline again - Less energy, more light

33
Q

is the winter SML more or less than Zcrit (critical depth)

A

SML > Zcrit = no phyto growth

34
Q

is the spring SML more or less than Zcrit (critical depth)

A

SML < Zcrit = phyto growth

35
Q

is the summer SML more or less than Zcrit (critical depth)

A

SML < Zcrit = phyto growth

36
Q

is the autumn SML more or less than Zcrit (critical depth)

A

SML > Zcrit = no phyto growth

37
Q

winter water characteristics

A
  • A lot of energy in system - Water column well mixed
  • Heterotrophic system
  • [Nutrient] (N, P, Si) high: decomposition of OM - no phyto to eat it
  • Low PAR: cloud, short days, sun low in sky
  • Sea: turbid, stirred sediment
  • Low ambient irradiance & high suspended particulate loading = shallow Zcrit
  • Mean resp > mean photo = no phyto growth
  • [Chl a] uniformly low
38
Q

spring water characteristics

A
  • Day length increases, wind speeds decrease
  • Sea-surface absorbs heat faster than turbulence can redistributed it
  • Thermocline forms: resists vertical mixing
  • Sediment settles – water gets clearer
  • High nutrients & light = high growth rate
  • Diatoms dominate – high growth rate
  • Result: high [chl a] = spring bloom
  • 1-2 weeks: diatoms exhaust NO3- in SML
  • Bloom ends quite quickly – not enough nutrients for diatom
  • Mesozooplankton: slow to respond
  • Most phyto OM exported to benthos
  • Heterotrophic dinoflagellates can respond more rapidly to feed on diatoms
39
Q

summer water characteristics

A
  • Big change in temp
  • Water column: highly stratified
  • SML:👇nutrients, ^ chl a
  • Small phyto: take up nutrients, maintain position
  • Prey & predator growth = well matched: little export
40
Q

autumn water characteristics

A
  • Reverse of spring
  • Increased turbulence: storms, lower temps
  • SML deepens: nutrients entrained into SML
  • Short lived diatom bloom
  • Stratification breaks down completely
41
Q

why does shallow water prevent phyto growth

A

mixed all year, high suspended sediment load

42
Q

what is temperate productivity

A

Summer = plenty of light, not enough nutrients – between the two is where we get plenty of light and nutrients for the phytoplankton
- Zooplankton will follow this phytoplankton trend