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The Carbon Cycle and Energy Security

Biological processes sequestering carbon (fast carbon cycle)

  • 3 things to know
  • Papers 1 and 3

Overview

How phytoplankton sequester carbon and the carbonate pump and thermohaline circulation carry it to the deep ocean, terrestrial primary producers and consumers, carbon in soils and decomposition, and why these biological processes form the fast carbon cycle.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Process

What is the carbonate pump?

Key term

Give examples of terrestrial primary producers that sequester atmospheric carbon.

Key term

How do phytoplankton remove carbon dioxide from the atmosphere?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    How do phytoplankton remove carbon dioxide from the atmosphere?

    Model answer

    Phytoplankton sequester atmospheric carbon dioxide through photosynthesis in surface ocean waters.

  2. 2

    Why are phytoplankton particularly effective at capturing atmospheric CO₂ compared to organisms in deeper waters?

    Model answer

    Phytoplankton live in surface ocean waters where they have access to sunlight needed for photosynthesis and direct contact with atmospheric CO₂ dissolving into the water.

  3. 3

    What structures do phytoplankton produce from the carbon they sequester?

    Model answer

    Phytoplankton produce carbonate shells or tests from sequestered carbon.

  4. 4

    What is the carbonate pump?

    Model answer

    The carbonate pump is the mechanism that transfers carbonate shells and tests from surface waters to the deep ocean.

  5. 5

    Explain how the carbonate pump moves carbon from the ocean surface to the deep ocean.

    Model answer

    When phytoplankton die, their carbonate shells and tests sink through the water column, transferring carbon from surface waters to the deep ocean floor.

  6. 6

    What role does thermohaline circulation play in the carbon cycle?

    Model answer

    Thermohaline circulation transports carbon-containing material from surface waters to deep ocean waters.

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