Arctic And Alpine Environments

Originally published in 1974, Arctic and Alpine Environments examines, the relatively simple ecosystems of arctic and alpine lands that still occupy extensive areas little disturbed by modern technology. The book argues that there is a necessity for carefully controlled development of the resources of these regions and suggests that there is a risk of irreversible disturbance without full understanding of these regions. This book provides a detailed documentation of cold-stressed arctic and alpine terrestrial environments and systematically deals with the present and past physical environment – climate, hydrology and glaciology; biota – treeline, vegetation, vertebrate zoology, and historical biogeography; abiotic processes – geomorphological and pedological and the role of man – bioclimatology, archaeology and technological impact, including radioecology. The book will appeal to academics and students of environmental and biological science, as well as providing a significant source for conservationists’, government agencies and industrial organizations.

This volume in the Greenwood Guides to Biomes of the World: series covers the biomes at high altitudes and near the poles, including the arctic tundra biomes, the Mid-Latitude Alpine Tundra Biome (found in the mountain ranges of North America, Asia, and South America), and the tropical alpine tundra biome (for example, Hawaii).

The European Arctic and Alpine regions are experiencing large environmental changes. These changes may have socio-economic effects if the changes affect the bioproduction, which form the basis for the marine and terrestrial food chains. This uniquely multidisciplinary book presents the various aspects of contemporary environmental changes in Arctic and Alpine Regions.

As human populations expand and have increasing access to technol ogy, two general environmental concerns have arisen. First, human pop ulations are having increasing impact on the earth system, such that we are altering the biospheric carbon pools, basic processes of elemental cycling and the climate system of the earth. Because of time lags and feedbacks, these processes are not easily reversed. These alterations are occurring now more rapidly than at any time in the last several million years. Secondly, human activities are causing changes in the earth's biota that lead to species extinctions at a rate and magnitude rivaling those of past geologic extinction events. Although environmental change is potentially reversible at some time scales, the loss of species is irrevo cable. Changes in diversity at other scales are also cause for concern. Habitat fragmentation and declines in population sizes alter genetic di versity. Loss or introduction of new functional groups, such as nitro gen fixers or rodents onto islands can strongly alter ecosystem processes. Changes in landscape diversity through habitat modification and frag mentation alter the nature of processes within and among vegetation patches. Although both ecological changes altering the earth system and the loss of biotic diversity have been major sources of concern in recent years, these concerns have been largely independent, with little concern for the environmental causes the ecosystem consequences of changes in biodiversity. These two processes are clearly interrelated. Changes in ecological systems cause changes in diversity.

During the summer of 1980, the First International symposium on Arctic and Alpine Mycology (ISAM-I) was held at the then extant Naval Arctic Research Laboratory near Barrow, Alaska, U.S.A., well within the Arctic Circle (Laursen and Ammirati, Arctic and Alpine Mycology. The First International symposium on Arcto-Alpine Mycology. Univ. Wash. Press, 1982). The facility is currently owned and operated by the Utkeagvik Inupiat community and is named the National Academic and Research Laboratory, thus retaining its acronym NARL. Twenty-five scientists participated in that historic first meeting. Their interests in the fungi spanned a vast geographic area of cold dominated habitats in both the northern and southern hemispheres that included four continents (N. and S. America, Eurasia,and Antarctica), nine countries, and numerous islands ranging from Greenland to Jan Mayen in the Svalbard group. ISAM-I helped to develop ongoing interests and initiate others. This is what ISAM-I founders hoped would happen. Asa result, the organizing committee for ISAM-II was formed. Its mandate was to: involve a maximum of one third new participants in future ISAM meetings: divide the responsibility for organizing future meetings at sites located in areas of interest to research thrusts in Arctic and alpine environments: keep the number of participants small enough to ensure manageability, taking full advantage of field collecting opportunities with minimal complications and cost.