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3 - Infertile and unstable habitats

Published online by Cambridge University Press:  11 September 2009

Roger del Moral
Affiliation:
University of Washington
Lawrence R. Walker
Affiliation:
University of Nevada, Las Vegas
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Summary

INTRODUCTION

Some of the most dramatic landscapes on earth scarcely support life because they are infertile and unstable. Infertility limits growth and instability limits establishment. These neglected, barren habitats of our world once escaped human impact because of their isolation and because productive habitats were more profitable. Today, humans are creating similarly impoverished habitats, but unlike natural ones, human-created barrens are close to human habitats and less productive. Due to the continuing global loss of usable habitat, these unproductive environments could be restored for human use.

Volcanoes, moving sands and glaciers all form infertile and unstable habitats. In the aftermath of violent cataclysms, volcanoes can create unstable surfaces such as lahars and scoria. The slow advance of sterile sand dunes across the landscape has both beneficial and catastrophic aspects. While coastal dunes protect the shores, interior dunes are expanding at alarming rates to threaten many communities and ruin pastoral lands. However, many interior dunes also support rare and complex ecosystems. The grinding, global retreat of glacial ice reveals jumbled barrens. The biota colonizes these inhospitable sites only with difficulty and persistence. Plants and animals eventually colonize the empty habitats formed by volcanoes, dunes and melting glaciers and when they do their success offers lessons for restoration of similar infertile and unstable habitats. In this chapter, we explore the constraints to establishment on these severely altered ecosystems and suggest that even they have value for sustaining economies and easing pressure on other habitats.

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Publisher: Cambridge University Press
Print publication year: 2007

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References

Chester, D. (1993). Volcanoes and Society. London: Edward Arnold.Google Scholar
Dale, V. D., Swanson, F. J. and Crisafulli, C. M. (2005). Ecological Responses to the 1980 Eruption of Mount St. Helens. New York: Springer Science.CrossRefGoogle Scholar
del Moral, R., Wood, D. M. and Titus, J. H. (2005). Proximity, microsites, and biotic interactions during early succession. In Ecological Responses to the 1980 Eruption of Mount St. Helens, ed. Dale, V. D., Swanson, F. J. and Crisafulli, C. M.. New York: Springer Science, pp. 93–110.CrossRefGoogle Scholar
Cloudsley-Thompson, J. (1977). The Desert. New York: G. P. Putnam's Sons.Google Scholar
Cowles, H. C. (1899). The ecological relations of the vegetation on the sand dunes of Lake Michigan. Botanical Gazette, 27, 95–117.CrossRefGoogle Scholar
Fagan, B. (2004). The Long Summer: How Climate Change Changed Civilization. New York: Basic Books.Google Scholar
Gelbspan, R. (1997). The Heat is On. New York: Addison–Wesley Publishing.Google Scholar
Postel, S. (1999). Pillar of Sand: Can the Irrigation Miracle Last?New York: W. W. Norton & Company.Google Scholar
Sears, P. B. (1980). Deserts on the March. Norman, OK: University of Oklahoma Press.Google Scholar
Walker, J., Thompson, C. H., Fergus, I. F. and Tunstall, B. R. (1981). Plant succession and soil development in coastal sand dunes of subtropical eastern Australia. In Forest Succession: Concepts and Application, ed. West, D. C., Shugart, H. H. and Botkin, D. B.. New York: Springer, pp. 107–31.CrossRefGoogle Scholar
Chapin, F. S. III., Walker, L. R., Fastie, C. L. and Sharman, L. C. (1994). Mechanisms of primary succession following deglaciation at Glacier Bay, Alaska. Ecological Monographs, 64, 149–75.CrossRefGoogle Scholar
Matthews, J. A. (1992). The Ecology of Recently Deglaciated Terrain: A Geoecological Approach to Glacier Forelands and Primary Succession. Cambridge: Cambridge University Press.Google Scholar
Matthews, J. A. (1999). Disturbance regimes and ecosystem recovery on recently-deglaciated substrates. In Ecosystems of Disturbed Ground, Ecosystems of the World 16, ed. Walker, L. R.. Amsterdam: Elsevier, pp. 17–37.Google Scholar
Sever, M. (2005). Melting glaciers reveal ancient bodies. Geotimes, 50, 40–41.Google Scholar
Pearce, F. (2005). The flaw in the thaw. New Scientist, 187, 27–30.Google Scholar
Pearce, F. (2005). Arctic ice shrinking as it feels the heat. New Scientist, 188, 12.Google Scholar
Small, C. and Naumann, T. (2001). Holocene volcanism and the global distribution of human population. Environmental Hazards, 3, 93–109.CrossRefGoogle Scholar
Chester, D. (1993). Volcanoes and Society. London: Edward Arnold.Google Scholar
Dale, V. D., Swanson, F. J. and Crisafulli, C. M. (2005). Ecological Responses to the 1980 Eruption of Mount St. Helens. New York: Springer Science.CrossRefGoogle Scholar
del Moral, R., Wood, D. M. and Titus, J. H. (2005). Proximity, microsites, and biotic interactions during early succession. In Ecological Responses to the 1980 Eruption of Mount St. Helens, ed. Dale, V. D., Swanson, F. J. and Crisafulli, C. M.. New York: Springer Science, pp. 93–110.CrossRefGoogle Scholar
Cloudsley-Thompson, J. (1977). The Desert. New York: G. P. Putnam's Sons.Google Scholar
Cowles, H. C. (1899). The ecological relations of the vegetation on the sand dunes of Lake Michigan. Botanical Gazette, 27, 95–117.CrossRefGoogle Scholar
Fagan, B. (2004). The Long Summer: How Climate Change Changed Civilization. New York: Basic Books.Google Scholar
Gelbspan, R. (1997). The Heat is On. New York: Addison–Wesley Publishing.Google Scholar
Postel, S. (1999). Pillar of Sand: Can the Irrigation Miracle Last?New York: W. W. Norton & Company.Google Scholar
Sears, P. B. (1980). Deserts on the March. Norman, OK: University of Oklahoma Press.Google Scholar
Walker, J., Thompson, C. H., Fergus, I. F. and Tunstall, B. R. (1981). Plant succession and soil development in coastal sand dunes of subtropical eastern Australia. In Forest Succession: Concepts and Application, ed. West, D. C., Shugart, H. H. and Botkin, D. B.. New York: Springer, pp. 107–31.CrossRefGoogle Scholar
Chapin, F. S. III., Walker, L. R., Fastie, C. L. and Sharman, L. C. (1994). Mechanisms of primary succession following deglaciation at Glacier Bay, Alaska. Ecological Monographs, 64, 149–75.CrossRefGoogle Scholar
Matthews, J. A. (1992). The Ecology of Recently Deglaciated Terrain: A Geoecological Approach to Glacier Forelands and Primary Succession. Cambridge: Cambridge University Press.Google Scholar
Matthews, J. A. (1999). Disturbance regimes and ecosystem recovery on recently-deglaciated substrates. In Ecosystems of Disturbed Ground, Ecosystems of the World 16, ed. Walker, L. R.. Amsterdam: Elsevier, pp. 17–37.Google Scholar
Sever, M. (2005). Melting glaciers reveal ancient bodies. Geotimes, 50, 40–41.Google Scholar
Pearce, F. (2005). The flaw in the thaw. New Scientist, 187, 27–30.Google Scholar
Pearce, F. (2005). Arctic ice shrinking as it feels the heat. New Scientist, 188, 12.Google Scholar
Small, C. and Naumann, T. (2001). Holocene volcanism and the global distribution of human population. Environmental Hazards, 3, 93–109.CrossRefGoogle Scholar
Chester, D. (1993). Volcanoes and Society. London: Edward Arnold.Google Scholar
Dale, V. D., Swanson, F. J. and Crisafulli, C. M. (2005). Ecological Responses to the 1980 Eruption of Mount St. Helens. New York: Springer Science.CrossRefGoogle Scholar
del Moral, R., Wood, D. M. and Titus, J. H. (2005). Proximity, microsites, and biotic interactions during early succession. In Ecological Responses to the 1980 Eruption of Mount St. Helens, ed. Dale, V. D., Swanson, F. J. and Crisafulli, C. M.. New York: Springer Science, pp. 93–110.CrossRefGoogle Scholar
Cloudsley-Thompson, J. (1977). The Desert. New York: G. P. Putnam's Sons.Google Scholar
Cowles, H. C. (1899). The ecological relations of the vegetation on the sand dunes of Lake Michigan. Botanical Gazette, 27, 95–117.CrossRefGoogle Scholar
Fagan, B. (2004). The Long Summer: How Climate Change Changed Civilization. New York: Basic Books.Google Scholar
Gelbspan, R. (1997). The Heat is On. New York: Addison–Wesley Publishing.Google Scholar
Postel, S. (1999). Pillar of Sand: Can the Irrigation Miracle Last?New York: W. W. Norton & Company.Google Scholar
Sears, P. B. (1980). Deserts on the March. Norman, OK: University of Oklahoma Press.Google Scholar
Walker, J., Thompson, C. H., Fergus, I. F. and Tunstall, B. R. (1981). Plant succession and soil development in coastal sand dunes of subtropical eastern Australia. In Forest Succession: Concepts and Application, ed. West, D. C., Shugart, H. H. and Botkin, D. B.. New York: Springer, pp. 107–31.CrossRefGoogle Scholar
Chapin, F. S. III., Walker, L. R., Fastie, C. L. and Sharman, L. C. (1994). Mechanisms of primary succession following deglaciation at Glacier Bay, Alaska. Ecological Monographs, 64, 149–75.CrossRefGoogle Scholar
Matthews, J. A. (1992). The Ecology of Recently Deglaciated Terrain: A Geoecological Approach to Glacier Forelands and Primary Succession. Cambridge: Cambridge University Press.Google Scholar
Matthews, J. A. (1999). Disturbance regimes and ecosystem recovery on recently-deglaciated substrates. In Ecosystems of Disturbed Ground, Ecosystems of the World 16, ed. Walker, L. R.. Amsterdam: Elsevier, pp. 17–37.Google Scholar
Sever, M. (2005). Melting glaciers reveal ancient bodies. Geotimes, 50, 40–41.Google Scholar
Pearce, F. (2005). The flaw in the thaw. New Scientist, 187, 27–30.Google Scholar
Pearce, F. (2005). Arctic ice shrinking as it feels the heat. New Scientist, 188, 12.Google Scholar
Small, C. and Naumann, T. (2001). Holocene volcanism and the global distribution of human population. Environmental Hazards, 3, 93–109.CrossRefGoogle Scholar

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