Abstract
The earth with all its inhabitants, including man, has had a long history as a slowly evolving complex system which normally exists in a state of stable dynamic equilibrium. Explosive growth in the human population, in the per capita use of nonrenewable resources, and in the degree of human disruption of established ecosystems — the hallmark of man's recent and rapid emergence as the dominant species on the face of the earth — represents a major departure from this state of equilibrium and an ecological crisis of global dimensions. This growth, and the rapid changes that arise from it, have had such a pervasive influence on the collective experience of man that they have come to be regarded as the normal course of events on a stable earth. This has fostered the notion that growth will always be essential for further improvements in the quality of human life.
The emergence of a global technological civilization results from man's ingenuity in devising ways of using an ever increasing proportion of energy available at the earth's surface. Rapid growth began only two hundred years ago when the developing technology of the industrial revolution made possible the large-scale exploitation of the earth's fossil-fuel resources and the creation of positive feedback between growth in technology and growth in fossil-fuel production.
Annual growth rates in world production of fossil fuels and ores of representative industrial metals, when compared with the nature and finite magnitude of the earth's resources, lead to the inescapable conclusion that the present episode of exponential growth can only be a transitory epoch of a few centuries duration within the totality of human history. Solar radiation offers the prospect of large supplies of energy with minimal environmental impact. However, constraints on growth due to the finite nature of food and mineral resources and the effects of environmental degradation can only be loosened in this way, not removed. Mankind faces an inevitable transition from a brief interlude of exponential growth to a stable condition characterized by rates of growth so slow as to be regarded essentially as a state of no growth. Failure to respond rationally and promptly to this situation could be disastrous.
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References
Anonymous, 1972, Kupfer: Bundesandstalt fur Bodenforschung, Hanover; und Deutsches Institut fur Wirstschafts forschung, Berlin.
Averitt, P., 1973, Coal,in Brobst, D.A., and W.P. Pratt, eds., United States mineral resources, U.S. Geol. Survey Prof. Paper 820, p. 133–142.
Brobst, D. A., and W. P. Pratt., 1973, Introductionin Brobst, D. A., and W. P. Pratt, eds., United States mineral resources, U.S. Geol. Survey Prof. Paper 820, p. 1–8.
Brooks, David B., and P. W. Andrews, 1974, Mineral resources, economic growth, and world population: Science, v. 185, No. 4145, p. 13–19.
Butzer, K. W., 1971, Environment and archeology: an ecological approach to prehistory: Chicago, Aldine, 703 p.
Butzer, K. W., 1974, Accelerated soil erosion: a problem of man-land relationships,in Manner, I. R., and M. W. Mikesell, eds., Perspectives on environment: Assoc. American Geographers, Publ. No. 13, p. 57–78.
Cloud, Preston, 1974, Evolution of ecosystems, American Scientist, v. 62, p. 54–66.
Commoner, B., 1971, The closing circle: nature, man and technology: New York, A. A. Knopf, 326 p.
Erickson, R. L., 1973, Crustal abundance of elements, and mineral reserves and resources,in Brobst, D. A., and W. P. Pratt, eds., United States mineral resources, U.S. Geol. Survey Prof. Paper 820, p. 21–25.
Förstner, U., G., and G. Müller, 1973, Schwermetalle in Flüssen and Seen als Ausdruck der Umweltverschmutzung: Berlin. Springer Verlag, 225 p.
Govier, G. W., 1973, Alberta's oil sands in the energy supply picture,in Laidler, K. J. Ed., Energy resources: Ottawa, Canada, Royal Society of Canada Symposium Proc. p. 55–70.
Halbouty, M. J., A. Meyerhoff, R. Dott, R. E. King, H. D. Klemme, and T. Shabad, 1970, World's giant oil and gas fields: geologic factors affecting their formation and basin classification geologicin Halbouty, M. T. ed., Geology of giant petroleum fields: Am. Assoc. Petroleum Geologists, Mem. 14, p. 502–555.
Heath, R. C., B. L. Foxworthy, and P., Cohen, The changing pattern of ground water development on Long Island, New York: U. S. Geol. Survey Circ. 524.
Horn, D. R., B. Horn, and M. N. Delach, 1972, Copper and nickel content of ocean ferromanganese deposits and their relation to properties of the substrate,in Morgenstein, M. ed The origin and distribution of manganese nodules in the Pacific and prospects for exploration: Symposium/Workshop Proceedings, Honolulu, Hawaii, October 16–17, 1972, p. 77–83.
Hubbert, M. King, 1962, Energy Resources, a report to the Committee on Natural Resources, Natl. Acad. Sciences — Natl. Research Council, Pub. 1000-D, 141 p.; reprinted 1973 Natl. Tech. Inf. Service, U. S. Dept. Commerce, no. PB-222401.
——, 1969, Energy resources,in Resources and man: Natl. Acad. Sciences — Natl. Research Council, Report of the Committee on Resources and Man: San Francisco W. H. Freeman, p. 157–242.
—— 1971, The energy resources of the earth: Scientific American v. 224, p. 60–70.
—— 1972, Man's conquest of energy: Its ecological and human consequences,in The Environmental and ecological forum: U.S. Atomic Energy Commission, Tech. Information Center, Oak Ridge, Tennessee, p. 1–50.
—— 1974, United States energy resources, a review as of 1972, Part 1: U. S. Senate Committee on Interior and Insular Affairs Report 93-40 (92-75), United States Senate, Washington 267 p.
Judson, Sheldon, 1968, Erosion of land, or what's happening to our continents: American Scientist, v. 56, no. 4, p. 356–374.
Lasky, S. G., 1950, How tonnage-grade relations help predict ore reserves: Eng. and Mining Jour., v. 151, no. 4, p. 81–35.
Lee, T., and C., Yao, 1970, Abundance of chemical elements in the earth's crust and its major tectonic units: Internat. Geology Review, v. 12, p. 778–786.
Lovering, T. S., 1969, Mineral resources from the land,in Resources and man: Natl. Acad. Sci. — Natl. Research Council, Report of the Committee on Resources and Man; San Francisco, W. H. Freeman, p. 109–134.
Marowsky, G., and K. H. Wedepohl, 1971, General trends in the behavior of Cd, Hg, Tl and Bi in some major rock forming processes: Geochimica et Cosmochimica Acta, v. 35, p. 1255–1267.
McKelvey, V. E., 1972, Mineral resource estimates and public policy: American Scientist, v. 60, p. 32–40.
Meadows, D. H., D. L., Meadows, J., Randers and W. W. Behrens, III, 1972, The limits to growth: a report for the Club of Rome's Project on the Predicament of Mankind: New York, Universe Books, 205 p.
Metallgesellschaft, AG, 1933 to 1972, Metallstatistik; Annual editions for the period 1933 to 1972, Metallgesellschaft Aktiengesellschaft, Frankfurt am Main, Fed. Republic of Germany.
Moiseyev, A. N., 1971, A non-magmatic source for Mercury ore deposits: Econ. Geol., v. 66, p. 591–601.
Page, R. W., 1973, Non-renewable resource subsystem,in Freeman, C., M. Jahoda, and K. L. R. Pavitt, eds., Thinking about the future: a critique of the Limits to growth: Sussex University Press-Chatto and Windus Ltd., London, 218 p.
Ronov, A. B., and A. A., Yaroshevskiy, 1967, Chemical structure of the earth's crust: Geochem. Internat., v. 4, p. 1041–1066.
Taylor, S. R., 1964, Abundance of chemical elements in the continental crust: a new table: Geochimica et Cosmochimica Acta, v. 28, p. 1273–1285.
Tunnell, G., 1970, Mercury,in Handbook of geochemistry: Berlin, Springer Verlag, Ch. 80, B-M.
United Nations, 1970, Survey of world iron resources: occurrence and appraisal: Dept Economic and Social Affairs, United Nations, New York.
United Nations, 1948 to 1971, Statistical yearbook: annual editions for the period 1948–1971: Statistical Office, Dept. Social and Economic Affairs, United Nations, New York.
U. S. Bureau of Mines, 1970, Mineral facts and problems: U. S. Bur. Mines Bull. 650, 1291 p.
U. S. Bureau of Mines, 1953 to 1971, Minerals yearbook: annual editions for the period 1953 to 1971: U. S. Bur. Mines, Dept. Interior, Washington, D. C.
Vinogradov, A. P., 1962, Average contents of chemical elements in the principal types of igneous rocks of the earth's crust: Geochemistry, v. 7, p. 641–664.
Walker, J. C. G., 1974, Stability of atmospheric oxygen: Am. Jour. Sci., v. 274, p. 193–214.
Warman, H. R., 1971, Future problems in petroleum exploration: Petroleum Review, v. 25, no. 291, p. 96–101.
Wedepohl, K. H., in press, Cooper.,in Handbook of geochemistry: Berlin, Springer Verlag, Ch. 29.
White, D. E., 1965, Geothermal energy: U. S. Geol. Survey Circ. 519, 17 p.
Yannacone, V. J., 1974, Fossil fuels are not just for burning,in Yannacone V. J. Jr., ed., Energy crisis — danger and opportunity: New York, West Publishing Company, p. 151–194.
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von Engelhardt, W., Goguel, J., Hubbert, M.K. et al. Earth resources, time, and man — A geoscience perspective. Geo 1, 193–206 (1976). https://doi.org/10.1007/BF02407506
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DOI: https://doi.org/10.1007/BF02407506