Bacteria Flashcards

(37 cards)

1
Q

What type of cell is a bacteria?

A

Prokaryotes
Membrane bound with no organelles

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2
Q

What technique made it possible to estimate bacterial concentrations

A

Epifluorecent microscopy

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3
Q

Most oceanic bacteria are heterotrophs, what are they eating?

A
  • Carbon!
  • Bacteria feed on DOC from phytoplankton (respiration)
  • Bacterial abundance will increase with phytoplankton abundance
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4
Q

What is remineralization

A

Taking organic matter and turning it into inorganic matter (mineral form)
Ex:
DOC —> CO2
DON —> NH4+
DOP —> PO4^-3

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5
Q

Describe phytoplankton-bacterial coupling

A
  • Phytoplankton produce organic matter via photosynthesis
  • Bacteria consume the DOM released by phytoplankton
  • Bacteria remineralize organic matter (ammonium (NH4+), phosphate (PO4 ^-3) etc.) providing nutrients that phytoplankton need to grow
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6
Q

What increases the rate of bacteria remineralization?

A

Temperature

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7
Q

What increases the rate of bacterial growth (respiration)?

A

Temperature

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8
Q

What is labile organic matter?

A
  • Bioavailable/decays fast (seconds old)
  • Larger molecules
  • Surface ocean
  • Near Redfield ratio (106:16:1)
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9
Q

What is refractory organic matter?

A
  • Resilient to degradation (thousands of years old)
  • Smaller molecules
  • Deep ocean
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10
Q

How do bacteria degrade large organic compounds?

A

Ectoenzymes located on the surface break down large complex molecules for bacteria to take in

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11
Q

What is autochthonous?

A

Generated in the ecosystem (ex: phytoplankton)

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12
Q

What is allochthonous?

A

External, introduced from the land

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13
Q

Net autotrophic

A

Phytoplankton C production exceeds bacterial community respiration (oxygen is produced)
Only autochthonous C is supported

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14
Q

Net heterotrophic

A

Bacterial community respiration exceeds phytoplankton C production (oxygen is consumed)
* Large allochthonous contribution*

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15
Q

What is marine snow?

A
  • Sinking organic matter
  • Will be highly colonized by bacteria
  • Production from bacteria feeds into pelagic food web
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16
Q

What are the four different zones of the ocean?

A
  • Epipelagic (0-200m)
  • Mesopelagic (200-1000m)
  • Bathypelagic (1000-4000m)
  • Abyssopelagic (4000-6000m)
17
Q

Where is the euphotic zone?

18
Q

Where is the aphotic zone?

A

Mesopelagic and below

19
Q

Where do bacteria dominate in the ocean?

A

The aphotic zone (top of the mesopelagic)

20
Q

Describe the epipelagic zone?

A
  • Only zone with photosynthesis
  • Phytoplankton processes dominate
  • O2 = high
  • Nutrients = low
  • Organic matter = produced
21
Q

Describe the top of the mesopelagic?

A
  • Aphotic
  • Flux of labile organic matter from above
  • Remineralization dominates
  • O2 = consumed
  • Organic matter = consumed
  • Nutrients = regenerated
22
Q

Describe the bottom of the mesopelagic?

A
  • High quality and quantity of organic matter consumed
  • Bacterial respiration/O2 consumption slows
23
Q

Describe the bathypelagic?

A
  • All labile organic matter gone
  • Horizontal mixing dominates over biological processes
24
Q

What causes hypoxia in the ocean?

A
  • The ideal gas law: PV=nRT
  • As temperature goes up dissolved gas concentrations go down
25
What are processes that contribute to hypoxia?
- Warm temperatures - Stratification - Increased bacterial growth (respiration) - Nitrogen loading
26
Where is the OMZ located?
Top of the mesopelagic (200-1000m) *Why?*
27
How does a dead zone form?
- Excess nutrients enter the water from agricultural runoff, sewage etc. resulting in a phytoplankton bloom - The bloom will eventually die off and the dead phytoplankton will sink to the bottom - The DOC fuels bacterial growth (respiration) using up O2 in the process - Sustained phytoplankton decomposition results in hypoxia (ex: Gulf of Mexico from Mississippi River runoff - the higher the river runoff the larger the dead zone)
28
As hypoxia increases what happens to fishery yields?
As hypoxia increases, fishery yields decrease
29
What can occur as a result of hypoxia?
Ocean acidification *Increase in CO2 leads to low PH*
30
What is the ocean conveyor belt?
Cold water + ice formation exudes salt making ocean water dense (sink)
31
Do algal blooms drive a high or low PH?
High *Why?*
32
Does bacterial respiration drive a high or low PH?
Low (acidification) *Why?*
33
Describe diurnal gasification and acidification
- Day: photosynthesis dominates (DO and PH = high) - Night: bacterial respiration dominates (DO and = PH low)
34
What is ammonification?
DON ---> NH4
35
What is denitrification?
NO3 ---> N2
36
What is nitrification?
NH4 ---> NH2OH ---> NO2 ---> NO3
37
How can bacteria be a source or sink for N?
- When C:N ratio of organic matter is low, more N is remineralized (bacterial growth efficiency is maximum) - When C:N ratio of organic matter is high, more N is taken up