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1. PHOTOSYNTHESIS• During photosynthesis, plants, algae, and cyanobacteria remove Carbon dioxide from the air and fix, or incorporate it into complex organic compounds such as glucose.

2. DECOMPOSITION, ANIMAL & PLANT RESPIRATION, SOIL MICROORGANISM RESPIRATION. • Many of the compounds are used as fuel for cellular respiration by the producer that made them, by a consumer that eats producer, or by a decomposer that breaks down the remains of the producer or consumer.

3. PARTLY DECOMPOSED PLANT REMAINS (COAL) Millions of years ago vast coal beds formed from the bodies of ancient trees that were buried and subjected to anaerobic conditions before they had fully decayed.

4. MARINE PLANKTON REMAINS• The oils of unicellular marine organisms probably gave rise to the underground deposits of oil and natural gas that accumulated in the geologic past. Coal, oil, and natural gas, called fossil fuels because they formed from the remains of ancient organisms. Fossil fuels are non- renewable resources.

5.COMBUSTION (HUMAN & NATURAL) The process of burning orcombustion, may return the carbon inoil, coal, natural gas, and wood to the atmosphere. In combustion, organic molecules are rapidly oxidized (combined with oxygen) and converted carbon dioxide and waterwith an accompanying release of light and heat.

6. BURIAL AND COMPACTION TO FORM ROCK (LIMESTONE)An even greater amount of carbon that is stored for millions of years isincorporated into the shells of marineorganisms. When these organisms die,their shells sink to the ocean floor and sediments cover them formingcemented together to form limestone, a meter thick.

7. EROSION OF LIMESTONE TO FORM DISSOLVED CO2 When the process of geologic uplift expose limestone, chemical andphysical weathering processes slowlyerode it away. This returns carbon tothe water and atmosphere where it isavailable to participate in the carbon cycle once again.

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Uploaded by Andrew Taylor on 2013-10-02.

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Intermediate form in the deprotonation of carbonic acid. It is a polyatomic anion with the chemical formula HCO− 3. Bicarbonate serves a crucial biochemical role in the physiological pH buffering system.

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The process of burning something.

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Substances in the soil that were once alive. Dead plants, animals, bacteria and fungi are all examples of organic material. Organic materialis distinguished from organic matter by the amount of decomposition that has taken place. Organic matter has decomposed as much as it can.

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The series of processes by which carbon compounds are interconverted in the environment, chiefly involving the incorporation of carbon dioxide into living tissue by photosynthesis and its return to the atmosphere through respiration, the decay of dead organisms, and the burning of fossil fuels.

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Powering the Cell: Mitochondria Animation

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Energy
The strength and vitality required for sustained physical or mental activity.

Thermal Energy
The internal energy of an object due to the kinetic energy of its atoms and/or molecules. The atoms and/or molecules of a hotter object have greater kinetic energy than those of a colder one, in the form of vibrational, rotational, or, in the case of a gas, translational motion.

Elastic Energy
The potential mechanical energy stored in the configuration of a material or physical system as work is performed to distort its volume or shape. [citation needed] Elastic energy occurs when objects are compressed and stretched, or generally deformed in any manner.

Gravitational Energy
The potential energy held by an object because of its high position compared to a lower position. In other words, it is energy associated with gravity or gravitational force.

Kinetic Energy
The energy of a body or a system with respect to the motion of the body or of the particles in the system.

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Tertiary Consumer
Eagle

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Secondary Consumer
Carnivore
Omnivore
Bear
Deer
Coyote
Snake

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Primary Consumer
Herbivore
Rabbit

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Producer
Autotrophs
Carrot Plants
Oats