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256 pages, Paperback
First published January 1, 2005
Earth’s size gives it a double advantage: Not only does it have a comparatively small surface area through which to lose heat, but the planet also has a sizable store of radioactive elements to generate more. While Earth has experienced some net cooling over the past 4.5 billion years, its heat loss and heat production have remained more nearly in balance than on Mercury, Mars, and the Moon. These small worlds died young, but Earth still has a warm and mobile mantle that keeps its crustal plates dancing even at an advanced age. (p. 10)
Carbon, water, sulfur, phosphorus, and nitrogen are in constant motion at and near the Earth’s surface, reincarnated again and again as minerals in rocks, gases in the atmosphere, ions in the ocean, schools of fish, leaves on trees. Each year, for example, even in the absence of human activities, 440 million tons of carbon are transferred from one form to another, with about 45 percent of this carbon “remanufactured” and shipped by biological processes. Similarly, 5.8 billion tons of nitrogen and 740 billion kilograms of phosphorous change hands in a year. Organisms are involved in 87 percent of the nitrogen trades and more than 99 percent of the phosphorus transactions. (p. 32-33)