Chapter 8 Flashcards

(13 cards)

1
Q

What is the link between tectonic activity and the carbon cycle important to?

A

The regulation of atmospheric CO2 concentrations thus the climate aswell.

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2
Q

What 2 processes does the Global carbon cycle involve? And what type of reactions are there?

A

Involves processes that occur on land and in the ocean.

Involves both biological and non-biological chemical reactions.

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3
Q

How is CO2 removed from the atmosphere and how is it returned?

A

Removed during photosynthesis and returned during respiration and decomposition.

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4
Q

How is Methane realesed to the atmosphere?

A

Methane is realsed from soils from anaerobic metabolism.

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5
Q

What happens to the small amount of terresterial organic carbon that survives respiration and decomposition?

A

Is buried in sedimantary basins on land or is transported to the sea.

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6
Q

What is phytoplanktons role in the ocean?

A

Phytoplankton in the ocean produce organic matter that is consumed by zooplankton and gets decomposed by aerobic and anaerobic bacteria.

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7
Q

What happens to the small fraction of organic matter settling through the water column?

A

It’s not decomposed but isntead buried in the marine sediments.

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8
Q

What happens to organic matter on longer time scales?

A

Gets buried in the sediments and undergoes lithification. Forming shales!

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9
Q

What can form when sediments that contain high concentration of organic matter gets buried or lithificated.

A

Fossil fuel

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10
Q

Give an example of the inorganic carbon cycle in:
1. short time scale
2. Long time scale

A
  1. Short term: CO2 moves between the atmosphere and the ocean surface.
  2. Carbon gets locked into rocks, sediments and the deep ocean.
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11
Q

Why does the ocean absorb so much CO2?

A

When CO₂ enters seawater, it doesn’t just stay as CO₂. It reacts with other elements.

CO₂ + H₂O → carbonic acid

Carbonic acid → bicarbonate (HCO₃⁻)

Bicarbonate → carbonate (CO₃²⁻)

Because CO₂ is constantly being converted into other forms, more CO₂ can keep dissolving from the atmosphere.

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12
Q

On a long time scale (millions of years), what regulates atmospheric CO2?

And what does it do?

A

Over millions of years, the carbonate-silicate cycle regulates atmospheric CO₂ through a feedback where higher temperatures speed up rock weathering that removes CO₂

WHILE cooler conditions slow it down, allowing CO₂ to build back up.

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13
Q

What processes have important control on atmospheric CO2 on longer time scales?

A

Geological processes

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