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The Carbon Cycle Presented by: Shannon Mar Iliana Swick Chris Butler Helia Ansari.

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Presentation on theme: "The Carbon Cycle Presented by: Shannon Mar Iliana Swick Chris Butler Helia Ansari."— Presentation transcript:

1 The Carbon Cycle Presented by: Shannon Mar Iliana Swick Chris Butler Helia Ansari

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3 Carbon Carbon is the major chemical constituent of the majority of organic matter It is in: –Fossil Fuels –DNA –RNA

4 What is Organic Matter? Organic matter: is matter that has come from a once-living organism; is capable of decay, or the product of decay; or is composed of organic compounds.

5 How is it stored? As organic moleculesAs organic molecules As the gas carbon dioxideAs the gas carbon dioxide As organic matterAs organic matter As fossil fuels and sedimentary rocksAs fossil fuels and sedimentary rocks As dissolved atmospheric carbon dioxide and calcium carbonated shellsAs dissolved atmospheric carbon dioxide and calcium carbonated shells

6 The Cycle Itself Carbon Dioxide is absorbed by several autotrophs and used to help them grow. Autotroph: organism that uses solar energy to manufacture the organic compounds it needs as nutrients from simple inorganic compounds obtained from its environment

7 The Cycle Continued… Photosynthesis incorporates the carbon atoms from carbon dioxide into sugars Photosynthesis: Complex process that takes place in cells of green plants. Radiant energy from the sun is used to combine carbon dioxide, and water to produce oxygen, carbohydrates, and other nutrient molecules

8 The Cycle Continued… Primary consumers eat the plants and use the carbon to build their own tissues Secondary consumers eat the primary consumers and use the carbon for their own needs

9 The Cycle continued… The carbon is returned into the environment when the animals breathe and dies, since carbon is returned to the soil during decomposition The carbon atoms in the soil are used for new plants And repeat

10 Carbon cycle in the Ocean Enters water through diffusion Converted into carbonate Combined with Calcium to make calcium carbonate Change to sedimentary rocks Diffusion: to spread though out from an area of higher concentration to an area of lower concentration

11 Carbon Levels Over the last billions of years the quantity has been steadily decreasing in the atmosphere Higher levels help regulate the Earth’s Temperature Due to the greater concentration of carbon dioxide the greenhouse effect has been enhanced

12 Carbon in the lithosphere 2 categories: organic and inorganic Organic: litter, organic matter, human substances in soils Inorganic: fossil fuels (coal, oil, natural gas), carbonated in sedimentary deposits like limestone Carbon dioxide can be released from the lithosphere by volcanoes

13 Carbon has greatly increased since the Industrial Revolution Atmospheric levels have increased over 30%, from 275 ppm to 365 ppm

14 The Importance of Carbon in the Carbon Cycle: Biological Carbon (C) is the fourth most abundant element in the Universe It’s the element that anchors all organic substances such as fossil fuels, fats, proteins, carbohydrates, and DNA

15 The Importance of Carbon in the Carbon Cycle: Ecological The carbon cycle is based on carbon dioxide gas, which makes up.038% of the volume of the troposphere and is also dissolved in water.

16 Continued… If the carbon cycle removes too much carbon dioxide form the atmosphere, the atmosphere will cool. If it generates too much carbon dioxide it will warm. Human activites have increased the amount of carbon dioxide release into the atmosphere contributing to global warming.

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18 Amounts of Carbon The amount of carbon in the lithosphere: 66 to 100 million gigatons.The amount of carbon in the lithosphere: 66 to 100 million gigatons. Amount of carbon in the hydrosphere: 38,000 to 40,000 gigatons.Amount of carbon in the hydrosphere: 38,000 to 40,000 gigatons. Amount of carbon in the biosphere: 540 to 610 gigatons.Amount of carbon in the biosphere: 540 to 610 gigatons. The amount of carbon in the atmosphere has increased from 578 gigatons to about 766 gigatons.The amount of carbon in the atmosphere has increased from 578 gigatons to about 766 gigatons.

19 Works Citied http://earthobservatory.nasa.gov/Library/CarbonC ycle/carbon_cycle4.html: 09/23/08http://earthobservatory.nasa.gov/Library/CarbonC ycle/carbon_cycle4.html http://earthobservatory.nasa.gov/Library/CarbonC ycle/carbon_cycle.html: 09/23/08http://earthobservatory.nasa.gov/Library/CarbonC ycle/carbon_cycle.html http://www.encyclopedia.com/doc/1G2- 3408600217.html: 09/22/08http://www.encyclopedia.com/doc/1G2- 3408600217.html http://www.lenntech.com/carbon-cycle.htm: 09/22/08http://www.lenntech.com/carbon-cycle.htm http://www.oznet.ksu.edu/ctec/Carbon/carboncycl e.htm: 09/23/08http://www.oznet.ksu.edu/ctec/Carbon/carboncycl e.htm


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