The European Russian forests are described within the boreal, hemiboreal and nemoral forest regions; floodplain forests are also characterized. The book presents a classification and description of forest vegetation, soil characteristic and assessments of plant diversity and successional status of forest plant communities. Structure and composition of vegetation in early- and late-successional forests are analyzed with an emphasis on forests in State Nature reserves. Features of the historical land-use, such as slash-and-burn, forest cutting, grazing, influence of fires on forest ecosystems, etc. are discussed for each forest region. The book contains an analysis of the general dynamics of the forest cover during the last two decades based on satellite image processing. The main stages of transformation of forest landscapes in European Russia during the Holocene are briefly reviewed in connection with the development of the production economy of people.

The aim of this study is to describe the distribution and development of forest resources in the European part of Russia. Due to the availability of basic information, this study concentrates on lands under the authority of the Federal Forest Service of Russia.

Costlow explores the central place the forest came to hold in a century of intense seeking for articulations of national and spiritual identity.

The European Forest Institute (EFI) has five Research and Development priority ar eas: forest sustainability, forestry and possible climate change, structural changes in markets for forest products and services, policy analysis, and forest sector informa tion services and research methodology. In the area of forest sustainability our most important activity has been the project "Growth trends of European forests", the re sults of which are presented in this book. The project was started in August 1993 under the leadership of Prof. Dr. Heinrich Spiecker from the University of Freiburg, Germany, and it is one of the first EFI's research projects after its establishment in 1993. The main purpose of the project was to analyse whether site productivity has changed in European forests during the last decades. While several forest growth studies have been published at local, re gional and national levels, this project has aimed at stimulating a joint effort in iden tifying and quantifying possible growth trends and their spatial and temporal extent at the European level. Debate on forest decline and possible climate change, as well as considerations re lated to the long term supply of wood underline the importance of this project, both from environmental and industrial points of view. Knowledge on possible changes in growth trends is vital for the sustainable management of forest ecosystems.

The lntergovernmental Panel on Climate Change (IPCC) has recently summarized the state ofthe art in research on climate change (Climate Change 1995). The most up to date research findings have been divided into three volumes: • the Science ofClimate Change (working group I), • the Impacts, Adaption and Mitigation of Climate Change (working group II), and • the Economic and Social Dimensions ofClimate Change (working group III) There is a general consensus that a serious change in climate can only be avoided if the future emissions of greenhouse gases are reduced considerably from the business as usual projection and if at the same time the natural sinks for greenhouse gases, in particular that of CO , are maintained at the present level or 2 preferrably increased. Forests, forestry and forestry industry are important parts of the global carbon cycle and therefore they are also part of the mitigation potentials in at least a threefold way: 1. During the time period between 1980 and 1989 there was a net emission of CO from changes in tropical land use (mostly tropical deforestation) of 2 1. 6 +/- 1 GtC/a, but at the same time it was estimated that the forests in the northem hemisphere have taken up 0. 5 +/- 0. 5 GtC/a and additionally other terrestrial sinks (including tropical forests where no clearing took place) have been a carbon sink ofthe order of l. 3 +/- l.