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An overview of the carbon cycle, explaining how carbon moves between the atmosphere, oceans, plants, and animals. Students are encouraged to draw a diagram to illustrate the process, using arrows to show the direction of carbon flow and labels to identify each stage. The document also discusses the importance of carbon as a greenhouse gas and the impact of human activities on the carbon cycle.
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Title: The Carbon Cycle Name______________________________ Procedures:
carbon that is released from fuels, 3.3 billion tons enters the atmosphere and most of the rest becomes dissolved in seawater. Carbon moves from the atmosphere to the oceans. The oceans, and other bodies of water, soak up some carbon from the atmosphere. Animals that live in the ocean use the carbon to build their skeletons and shells. Carbon dioxide is a greenhouse gas and traps heat in the atmosphere. Without it and other greenhouse gases, Earth would be a frozen world. But humans have burned so much fuel that there is about 30% more carbon dioxide in the air today than there was about 150 years ago. The atmosphere has not held this much carbon for at least 420,000 years according to data from ice cores. More greenhouse gasses such as carbon dioxide in our atmosphere are causing our planet to become warmer. Carbon moves through our planet over longer time scales as well. For example, over millions of years weathering of rocks on land may add carbon to surface water which eventually runs off to the ocean. Chemical weathering of silicate minerals, in particular, can have an effect on the amount of carbon dioxide in the atmosphere. Additionally, over long time scales, carbon is removed from seawater when the shells and bones of marine animals and plankton collect on the sea floor. These shells and bones are made of limestone, which contains carbon. When they are deposited on the sea floor, carbon is stored from the rest of the carbon cycle for some amount of time. The amount of limestone deposited in the ocean depends somewhat on the amount of warm, tropical, shallow oceans on the planet because this is where prolific limestone-producing organisms such as corals live. The carbon can be released back to the atmosphere if the limestone melts or is metamorphosed in a subduction zone. Drawing: