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Edited by
Dan Chamberlain, University of Turin,Aleksi Lehikoinen, Finnish Museum of Natural History, University of Helsinki,Kathy Martin, University of British Columbia, Vancouver
There are many definitions of what is a ‘mountain’ and what is a ‘mountain bird’. In this chapter, we first assess these different definitions, and then clearly outline our rationale for choosing to define a mountain bird as bird species where at least some populations of the species somewhere in their distribution spend at least one critical stage of their life cycle above treeline. We then provide an overview of the importance of mountains to biodiversity, and compare knowledge on mountain birds to lowland ecosystems. Zonation is an important aspect of mountain ecology – we review the evidence for consistent patterns in bird richness and diversity across elevation gradients, and consider the different hypotheses that might explain these patterns. Additionally, we consider variation along the elevation gradient in some general species characteristics and the extent to which these trends vary geographically. Furthermore, we give an overview of how mountain bird communities vary seasonally, in particular considering different dispersal and migration strategies, and the extent to which the prevalence of these strategies varies according to different regions. Finally, we summarise the history of human interventions in mountains and their impacts on bird communities from pre-history until the start of the mechanized age.
Human intelligence exercises a decisive influence on the ecological balance of the landscape, to store knowledge and to organise the use of natural resources. This chapter starts by considering some of the main physical characteristics of the Scandinavian landscape throughout the millennia that have passed since the Quaternary glaciations. A number of physical processes were responsible not only for the geological construction of the Scandinavian landscape but also for the later changes that took place. The soils in Scandinavia consist mainly of relatively coarse glacial deposits, which have generally proved difficult to cultivate. In the last 5,000 years, shore displacement around the Baltic has mainly been caused by land uplift. However, the Norwegian Sea has not undergone such drastic changes. The chapter also deals with the climatic changes, coastal landscapes, and the vegetation zones and animal life in the Scandinavian region.
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