Past fuel wood exploitation and natural forest vegetation in the Black Forest, the Vosges and neighbouring regions in western Central Europe

2010 ◽  
Vol 291 (1-2) ◽  
pp. 154-165 ◽  
Author(s):  
Thomas Ludemann
Oryx ◽  
1995 ◽  
Vol 29 (3) ◽  
pp. 212-214 ◽  
Author(s):  
Steven M. Goodman ◽  
William T. Stanley ◽  
William D. Newmark ◽  
Kim M. Howell

Ambangulu Forest is one of the few remaining tracts of natural forest between 800 and 1200 m in the West Usambara Mountains of Tanzania. It may be the biologically richest area in the region but it is threatened by illegal felling of timber trees, wind damage, grazing and browsing livestock, and collection of fuel-wood and building poles. A proposed project aims to protect the forest and benefit local people at the same time.


Author(s):  
Martin Schütze ◽  
Gegeensuvd Tserendorj ◽  
Marta Pérez-Rodríguez ◽  
Manfred Rösch ◽  
Harald Biester

Forest vegetation plays a key role in the cycling of mercury (Hg) and organic matter (OM) in terrestrial ecosystems. Litterfall has been indicated as the major transport vector of atmospheric Hg to forest soils, which is eventually transported and stored in the sediments of forest lakes. Hence, it is important to understand how changes in forest vegetation affect Hg in soil and its biogeochemical cycling in lake systems. We investigated the pollen records and the geochemical compositions of sediments from two lakes (Schurmsee and Glaswaldsee) in the Black Forest (Germany) to evaluate whether long-term shifts in forest vegetation induced by climate or land use influenced Hg accumulation in the lakes. We were particularly interested to determine whether coniferous forests were associated with a larger export of Hg to aquatic systems than deciduous forests. Principal components analysis followed by principal component regression enabled us to describe the evolution of the weight of the latent processes determining the accumulation of Hg over time. Our results emphasize that the in-lake uptake of Hg during warm climate periods, soil erosion after deforestation and emissions from mining and other human activities triggered changes in Hg accumulation during the Holocene stronger than the changes caused by forest vegetation alone.


Geosciences ◽  
2018 ◽  
Vol 8 (10) ◽  
pp. 358 ◽  
Author(s):  
Martin Schütze ◽  
Gegeensuvd Tserendorj ◽  
Marta Pérez-Rodríguez ◽  
Manfred Rösch ◽  
Harald Biester

Forest vegetation plays a key role in the cycling of mercury (Hg) and organic matter (OM) in terrestrial ecosystems. Litterfall has been indicated as the major transport vector of atmospheric Hg to forest soils, which is eventually transported and stored in the sediments of forest lakes. Hence, it is important to understand how changes in forest vegetation affect Hg in soil and its biogeochemical cycling in lake systems. We investigated the pollen records and the geochemical compositions of sediments from two lakes (Schurmsee and Glaswaldsee) in the Black Forest (Germany) to evaluate whether long-term shifts in forest vegetation induced by climate or land use influenced Hg accumulation in the lakes. We were particularly interested to determine whether coniferous forests were associated with a larger export of Hg to aquatic systems than deciduous forests. Principal components analysis followed by principal component regression enabled us to describe the evolution of the weight of the latent processes determining the accumulation of Hg over time. Our results emphasize that the in-lake uptake of Hg during warm climate periods, soil erosion after deforestation and emissions from mining and other human activities triggered changes in Hg accumulation during the Holocene stronger than the changes caused by forest vegetation alone.


1989 ◽  
Vol 16 (2) ◽  
pp. 129-136 ◽  
Author(s):  
V.P. Singh ◽  
J.S. Singh

The present study analyses the energy-budget of ‘village ecosystems’ in a dry tropical environment. These systems depend to a great extent on the surrounding natural forest/savanna ecosystems. Accordingly the objectives of the study were to quantify (i) the energy efficiency of rain-fed agriculture at the ecosystem level, and (ii) the indirect impact of agricultural activity on the surrounding forest/savanna ecosystems.Agronomic output from farming is not sufficient to meet the food-energy requirements of the villagers, hence 27.0 to 51.0% of the requirement is met from outside markets. Operation of the agro-ecosystems involved requires a considerable amount of subsidy from the surrounding forest/savanna ecosystems in terms of fodder and fuel-wood. About 81 to 100% of the fuel needs, and 80–87% of the fodder needs, are met from the natural forest/savanna ecosystems. Thus, for each unit of energy obtained in agronomic yield (including milk), 3.1 units of energy are expended from the surrounding natural ecosystems in the form of fodder and fuel-wood.The erratic and ill-distributed nature of monsoon rains results in moisture deficit which affects the crop production in dry-land farming, causing partial or total failure of the crops. For achieving increased and stable agronomic production under rain-fed conditions, improved dry-land farming techniques have to be applied. Some of these techniques are: (1) introduction of crops and varieties that would be capable of maturing in a period of 90–100 days, and adequate use of appropriate fertilizers; (2) planned rain-water management including storage of surface runoff; and (3) practices of intercropping with crops of longer duration than those currently grown, having slow growth-rates in the early part of their life-cycles.


2014 ◽  
Vol 76 ◽  
pp. 1-175 ◽  
Author(s):  
Jacek Herbich

Yarious geobotanical, photointerpretative, cartographical and pedological methods were used to study the vegetation and the habitat conditions under which it occurred in the valleys of a representative fragment of a young-glacial landscape. The author determined changes in the real and potential natural vegetation in lake depressions during their transformations into river valleys and then during the development of the latter. A geobotanical description has been worked out for various valley types (subglacial channels, river valleys, gullies and denudation-caused valleys) in a young-glacial landscape, taking into account the origin of the latter. The role has been established of denudation and erosion processes and their intensity as habitat-forming factors in the formation of contemporary vegetation of valleys. Relationships were determined between the vegetation and the age of slopes and soils, measured in absolute years, and then the resultant changes in the natural forest vegetation. A relationship has been revealed between the distribution of oak-hornbeam forests and beech forests in lowlands, and erosion and denudation processes, and habitat age. Relationships were determined between the vegetation and slope microrelief during its development, and the differentiation-causing effect of the direction of slope on the vegetation. The historical real vegetation of the period preceding the current wave of anthropopressure has been reconstructed and contemporary changes in valley vegetation have been interpreted. More information has been gained on the role of the direction of sloping as a community-forming factor. The vegetation was analysed from the viewpoint of its bioindicative potential.


2021 ◽  
Author(s):  
Rob Tanner

Abstract I. parviflora is an exceptionally successful invader of many European countries. Its spread has been rapid, it is abundant in many parts of its exotic range and is one of few plants to successfully invade undisturbed forest vegetation. It is consequently regarded as undesirable by some, though there is little evidence of negative economic, social or environmental impacts. Further spread in central Europe is not likely as the species is already very abundant. In North America, on the other hand, it is still very localized. Even without clear evidence for impacts, a further spread there should not be encouraged by deliberate or careless transport of the species.


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