3.4 Carbon cycle

The ​ (a)   cycle is the basic building block of the carbohydrates, fats, proteins, DNA and all other ​ (b)   compounds required for life.

It is part of the ​ (c)   molecules produced through ​ (d)   and eaten or decomposed by ​ (e)   .

• carbon
• organic
• carbohydrate
• photosynthesis
• consumers

Tags

NGSS.MS-LS1-6

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What is the key component of the carbon cycle?

• Oxygen

• Carbon dioxide

• NItrogen

• Sulfur

Tags

NGSS.MS-LS1-6

NGSS.MS-LS2-3

What process removes carbon dioxide from the air?

• Photosynthesis

• Metabolism

• Cellular respiration

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NGSS.MS-LS1-6

The cells of oxygen consuming producers, consumers and decomposers carry out

• Photosynthesis

• Metabolism

• Cellular or Aerobic respiration

Use the diagram to answer question:

What is the only way that carbon is taken out of the atmosphere?

• Evaporation

• Combustion

• Respiration

• Photosynthesis

Tags

NGSS.MS-LS1-6

Use the diagram to answer the question:

How do plants and animals put Carbon dioxide back into the air

• Combustion

• respiration

• Photosynthesis

• Evaporation

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NGSS.MS-LS1-6

On the land, which organisms release carbon stored in the soil back into the atmosphere?

• Plants

• Animals

• Decomposers

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NGSS.MS-LS2-3

Over millions of years, the ​ (a)   in deeply buried marine deposits of​ (b)   were converted into carbon containing fossil fuels. The ​ (c)   of overlying sediments and heat released during the ​ (d)   of dead matter formed coal, oil, and natural gas (​ (e)   )

• carbon
• dead plant matter and algae
• high pressure from the weight
• decomposition
• fossil fuels

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NGSS.MS-ESS2-1

What about (a)   ? This forms in a similar way – organic matter accumulates in a place with little (b)   , is buried, ‘cooked’ and turned into a useful substance and store of energy. Coal forms from (c)   which is plant matter in wet places on land. Oil forms from organic matter that settled on the (d)   to form a substance called (e)   .

• oil
• Oxygen
• peat
• sea bed
• oil shale

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NGSS.MS-ESS3-1

If we removed too much ​ (a)   from the atmosphere, the primary effect would be a significant ​ (b)   , leading to a colder climate with potentially widespread impacts like increased ​ (c)   , reduced ​ (d)   , and disruptions to ecosystems due to the ​ (e)   , making Earth significantly colder and potentially inhospitable to life as we know it

• carbon dioxide
• drop in global temperature
• ice cover
• plant growth
• weakened greenhouse effect

Tags

NGSS.MS-ESS3-5