Lecture 19 Flashcards

1
Q

How are microbes connected to their physical surroundings?

A

Microbial communities are affected by changes in:

  • temperature
  • rainfall/moisture
  • pH
  • salinity
  • etc.
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2
Q

How are microbes connected to climate change?

A

As the claim the changes, microbes will respond, adapt, and evolve in their surroundings.

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3
Q

What are the 2 interconnected sub cycles that are included in the global carbon cycle?

A
  1. Rapid carbon exchange among living organisms (fast cycles).
  2. Long-tmr cycling of carbon through geological processes (slow cycles).
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4
Q

What are long-term and rapid carbon cycles driven by?

A

Long-term: plate tectonics, weathering, eroding carbon from mountains - sequestration.

Rapid: living organisms - carbon is moving through different realms on a faster time scale.

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5
Q

What is the role of microbes in the global carbon cycle?

A

Photosynthetic microorganisms (i.e. phytoplankton) drawdown CO2 from the atmosphere during photosynthesis.

Photosynthesis creates usable carbon for other organisms - creates organic matter that goes to the bottom of the ocean.

Bacteria in the ocean will decompose or eat the organic material produced by phytoplankton - consuming a carbon source = release of CO2 by bacteria.

This is a biological carbon pump.

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6
Q

Why does microbial respiration and decomposition lead to the release of CO2?

A

Heterotrophs microbes break down organic carbon compounds for cellular growth and energy - gets released by bacteria that consume it.

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7
Q

What is organic matter and where does it come from?

A

Organic matter is material that has come from a recently living organism.

It includes the remains of organisms, such as plants and animals and their waste products in the environment.

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8
Q

Where does soil organic matter derive from?

A

Terrestrial environments.

On land almost all organic matter is derived from plants.

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9
Q

Where does marine organic matter derive from?

A

Marine environments.

In the ocean most organic matter is derived from phytoplankton.

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10
Q

What is a major constituent of organic matter?

A

Carbon.

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11
Q

What determines the fate of organic matter?

A

The activity of microorganisms that live in the sediment.

If the carbon is degraded it is released as CO2, but if not it will be buried and sequestered for a long time.

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12
Q

How is bioavailability determined?

A

By intrinsic chemical properties of the compound - its size and structure.

Size: low molecular wight (most bioavailable), high molecular weight (least bioavailable).

Structure: aliphatic (most bioavailable), highly aromatic (least bioavailable).

It is not always te case (e.g. lignin).

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13
Q

Is bioavailability of organic matter only affected by chemical properties?

A

No lol.

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14
Q

What is the goal of the novel bioreactor system that probes organic matter degradation?

A

Monitor respiratory CO2 production and collect it sequentially for carbon isotope analysis.

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15
Q

What can carbon isotopes tell us?

A

C13 signature: differences in source and where something came from.

C14 signature: tells us the age of something.

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16
Q

Explain the “you are what you eat (and breathe) principle for microbes. How do we apply this idea?

A

Heterotrophic microbes show similar isotopic signature as carbon sources.

The isotopic carbon respirometer-bioreactor measure and collects CO2 for carbon isotope analyses.

It allows us to track the source, age, and sequences of carbon compounds that are degraded by microorganisms.

17
Q

For the degradation of most organic matter, what do they require?

A

The use of extra cellular enzymes.

Extracellular enzyme activity is a key step in organic matter degradation in the ocean.

18
Q

How do we use genomic characteristic to observe patterns of organic matter degradation?

A

We can count the total copy number of genes encoding for known extra cellular enzymes.

Organic matter degradation patterns are consistent with genomic characteristics for the two example species. .

19
Q

Explain the organic matter in the permafrost.

A

Permafrost contains large stores of organic matter that have been locked for thousands of years.

Microbial organisms are seasonally frozen and preserved within the permafrost.

20
Q

What is the positive feedback cycles happening in the arctic and what are its consequences?

A

Positive feedback cycle: less ice and snow causes more warming (less reflection of sun’s radiation) - more warming causes less ice and snow.

Thawing permafrost = microbes are making a shift from dormancy to activity.

When the claim the warms, the microbes become active and degrade organic matter leading to the release f greenhouse gases.

21
Q

What kind of microbes might become active when permafrost thaws?

A

Most bacteria release CO2 as a byproduct of their metabolism. Some microorganisms can release methane (more potent).