Methods in Oceanography Flashcards

1
Q

microscopy

A

1mm - 3 micrometer

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2
Q

Flow cam

A

1mm - 6 micrometer

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3
Q

Flow cytometry

A

20 micrometer - 0.5 micrometer

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4
Q

molecular barcoding problems

A

data base incomplete, DNA content variable among species/difficult to quantify

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5
Q

what do you measure with biomass, bulk measurements

A

POC > 0.7 micrometer, Chl a > 0.7 micrometer

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6
Q

POC measurement problems

A

Unspecific for photosynthetic organisms

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7
Q

Concentration of Cal a depends on

A

irradiance, amount of nutrients present, composition and phytoplankton size

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8
Q

What does an argo float measure?

A

Temperature, Salinity, Chl a, carbon, nitrate

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9
Q

Remote sensing

A

Satellite sensors estimate cal a from irradiance leaving the water.

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10
Q

How does remote sensing work?

A

Chl a absorbs sunlight in red and blue waves. The irradiance that leaves the water becomes greener, depending on the chl a concentrations.

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11
Q

Remote sensing can also measure

A

Organic carbon pool, Photophysiology, composition

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12
Q

bloom

A

increase in biomass above a treshold

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13
Q

phenology

A

timing of periodic biological events as influenced by the environment

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14
Q

Phases of a bloom

A

Start day, intensity, duration

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15
Q

Limitations of remote sensing

A

Cloud an sea ice cover, high altitude in winter not measurable bc of low sun angles, Coastal not reliable due to detritus and sediments, satellites are expensive, no vertical profile, needs validation by in situ data

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16
Q

Why not measure POC or chlorine a as indicator for primary production in the ocean?

A

POC can be zooplankton, chl a reflects composition and physiological changes, growth = loss, growth < loss, cal a concentration can change due to mixing.

17
Q

Gross primary production (GPP)

A

Total rate of organic carbon produced by autotrophs

18
Q

Respiration

A

Energy used for maintenance and growth (10-20% of GPP)

19
Q

Net Primary Production NPP

A

Total organic carbon production minus respiration of autotrophs

20
Q

Oxygen evolution, Winkler technique

A

Light bottle: respiration and photosynthesis, dark bottle: respiration –> measure amount of oxygen used

21
Q

disadvantage winkle technique

A

Inaccurate due to long incubation, includes respiration heterotrophs

22
Q

Carbon assimilation

A

add 14C labeled bicarbonate, measure 14C incorporated in organic carbon.

23
Q

Issues with 14c incorporation

A

Unnatural irradiance, unnatural irradiance, extracellular release of DOC ignored.

24
Q

active chlorophyll a fluoresence

A

Measure electron transport rate through photosystem 2

25
Q

Global ocean productivity is estimated by combining

A

Biomass, irradiance, in situ productivity vs irradiance measurements

26
Q
A