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Tundra Disturbance Studies, III: Short-term Effects of Aeolian Sand and Dust, Yamal Region, Northwest Siberia

Published online by Cambridge University Press:  24 August 2009

Bruce C. Forbes
Bruce C. Forbes
Affiliation:
Arctic Centre, University of Lapland, PO Box 122, SF-96101 RovaniemiFinland.
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Extract

This paper describes the short-term responses of tundra vegetation and soils to aeolian sand and dust emanating from anthropogenically-bared surfaces in the low-arctic region of northwestern Siberia. Such surfaces, including roads and quarries, are increasing substantially each year as the region undergoes massive gas- and oil-producing development. Data are presented which emphasize the ‘cumulative’ impacts of corridor construction, namely those effects which are measurable laterally, at some distance from the actual surfaces of roads and quarries, four years after their creation. In particular, changes in plant communities are documented, in addition to the chemistry and macronutrient status of mineral soils and dominant vascular plants and mosses, respectively, as affected by road-dust.

Dramatic changes in plant community composition and cover were evident up to 200 m downwind from a ‘typical’ sand quarry. Although a few species appeared to respond favourably to rapid sand deposition, the great majority that were beset with it have declined in status or disappeared altogether. The exceptions were those growth-forms having the ability to keep perennating buds at or above the surface of the deepening sand (e.g. Betula nana, Salix spp., and Polytrichum spp.). The most pronounced decreases recorded were among lichens, hepatics, Sphagnum spp., and pleurocarpous mosses. The decline in Sphagnum spp., which dominate the moss layer and contribute much of the hummock-hollow microtopography, is already having a profound impact on community structure by virtually eliminating surface heterogeneity.

Type
Main Papers
Information
Environmental Conservation , Volume 22 , Issue 4 , Winter 1995 , pp. 335 - 344
Copyright
Copyright © Foundation for Environmental Conservation 1995

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