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Earth’s Life Support Systems

Natural sequestration in oceans, vegetation, sediments and rock

  • 3 things to know
  • Component 01

Overview

Recall questions on carbon sequestration, the solubility, biological and carbonate pumps, the formation of limestone, net carbon uptake by the oceans and land biosphere, soil carbon, carbon in sedimentary rock and silicate weathering, and blue carbon.

What you need to know

Answer each one before you reveal it.

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Key term

What is carbon sequestration?

Key term

Why does warm tropical seawater hold less dissolved carbon dioxide than cold polar water?

Process

How does limestone form from marine organisms?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is carbon sequestration?

    Model answer

    Carbon sequestration is the long-term capture and storage of carbon in a store that holds it out of the atmosphere.

  2. 2

    How does the solubility pump carry carbon into the deep ocean?

    Model answer

    Cold, dense water at high latitudes dissolves carbon dioxide readily and then sinks as part of the thermohaline circulation, carrying that dissolved carbon to depths where it stays for centuries.

  3. 3

    Why does warm tropical seawater hold less dissolved carbon dioxide than cold polar water?

    Model answer

    The solubility of a gas falls as temperature rises, so warm water can hold less carbon dioxide and tends to release it back to the atmosphere.

  4. 4

    Describe the biological pump.

    Model answer

    Phytoplankton fix carbon dioxide in the sunlit surface ocean, and when they and the animals that eat them die the organic carbon sinks as detritus into the deep ocean and onto the sea floor.

  5. 5

    What is the carbonate pump?

    Model answer

    The carbonate pump is the process by which marine organisms build shells and skeletons of calcium carbonate that sink when they die and accumulate as carbonate sediment on the sea bed.

  6. 6

    How does limestone form from marine organisms?

    Model answer

    Calcium carbonate shells and skeletons settle on the sea floor, build up as sediment and are compacted and cemented over millions of years into limestone.

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Earth’s Life Support Systems

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Hotter magma is .
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AThe lower quartile is the 2nd value, 11 cm.
BThe upper quartile is the 6th value, 16 cm.
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The sunspot cycle lasts about 11 years.
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