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Global Litter Invertebrate Decomposition Experiment

Biosphere Reserve in South Bohemia, Czech Republic

Site Manager

Dr. Marcela Kovarova
Institute of Botany
Academy of Sciences
252 43 Pruhonice
Czech Republic

Site Description

This GLIDE site is located at the southwestern part of Bohemia, Czech Republic, on the boundaries with Austria and Germany. The mountains belong to the Hercynic central european mountains with the highest mount on the German territory (Grosser Arber, 1456 m above sea level). They are mostly built up by acid bedrocks (mica, schists, and granite). The climate in the lower part of the _umava (about 1200 m above sea level) where the GLIDE experimental site is situated is moderately cold and humid. The vegetation is composed of climax spruce forests. The plant communities and soil biota of the studied area were extensively studied in the last years in a joint botanical and soil zoological grant project.

Site Location

Site location is in the Czech Republic, South Bohemia, 13°45’- 13° 46’E and 48° 97’- 48° 98’N.

Site Area

Site area is 10 kilometers squared.

Site Elevation

Site elevation is 1205-1255 m above sea level.

Annual Rainfall

Annual rainfall is 1486-1200 mm.

Annual Temperature

Annual temperature is 3.7° - 5.1° C.

Soil

Soil type is mountain brunisols with moder humus form.

Native Forest/Vegetation Types

Native vegetation is mountain climax spruce forest Calamagrostio villosae-Piceetum fagetosum.

Principal Biome/Ecoregion

Principal biome is central european mountain taiga

Photo Gallery

Photo courtesy of Marcela Kovarova


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This webpage is funded by the Soil Science Society of America.

Please contact the GLIDE headquarters (email: glide@nrel.colostate.edu) if you have any comments or questions.

GLIDE was a project of the International Biodiversity Observation Year 2001-2002

This material is based upon work supported in part by the National Science Foundation under Grant No. 98 06437 Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.

 
 
 


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