David Bowman is Professor of Forest Ecology in the School of Plant Science at the University of Tasmania. He uses a range of tools, including remote sensing and geographic information analysis, stable isotopes, ecophysiological analysis, mathematical modelling, biological survey and molecular analysis to understand how Australian landscapes have evolved in response to climatic change, varying fire regimes, the introduction of large vertebrate herbivores, and the impacts of contemporary and prehistoric management.
Inhaltsangabe
Preface 1. Introduction 2. What is Australian rainforest? 3. The sclerophyll problem 4. The edaphic theory I. The control of rainforest by soil phosphorus 5. The edaphic theory II. Soil types, drainage and fertility 6. The climate theory I. Water stress 7. The climate theory II. Light and temperature 8. The fire theory I. Field evidence 9. The fire theory II. Fire, nutrient cycling and topography 10. The fire theory III. Fire frequency, succession and ecological drift 11. The fire theory IV. Aboriginal landscape-burning 12. The fire theory V. Aridity and the evolution of flammable forests 13. Fire management and rainforest conservation 14. Summary References.
Preface 1. Introduction 2. What is Australian rainforest? 3. The sclerophyll problem 4. The edaphic theory I. The control of rainforest by soil phosphorus 5. The edaphic theory II. Soil types, drainage and fertility 6. The climate theory I. Water stress 7. The climate theory II. Light and temperature 8. The fire theory I. Field evidence 9. The fire theory II. Fire, nutrient cycling and topography 10. The fire theory III. Fire frequency, succession and ecological drift 11. The fire theory IV. Aboriginal landscape-burning 12. The fire theory V. Aridity and the evolution of flammable forests 13. Fire management and rainforest conservation 14. Summary References.
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