Attributes | Values |
---|
rdf:type
| |
rdfs:seeAlso
| |
Description
| - Sandstone massifs with their deep ravines offer the instructive opportunity to study the response of organisms to steep environmental gradients. In 2008–2010, many groups of soil fauna were studied along transects across three ravines in the Bohemian Switzerland National Park (north-western Czechia), a part of the Elbe Sandstone Massif. Each transect included five sampling positions: two opposite edges, two opposite mid-slope positions, and the ravine bottom. The ravines had a specific microclimate characterized by temperature inversion. In general, the cooler and more humid ravine bottoms had also less acid soil with lower carbon content but enriched by litter of deciduous trees and herbs. The other transect positions were characterized by spruce (mid-slopes) and pine (edges) stands with mor humus, exposed to drought in the upper parts. The soil animal communities differed substantially in dependence on their position along the transects.
- Sandstone massifs with their deep ravines offer the instructive opportunity to study the response of organisms to steep environmental gradients. In 2008–2010, many groups of soil fauna were studied along transects across three ravines in the Bohemian Switzerland National Park (north-western Czechia), a part of the Elbe Sandstone Massif. Each transect included five sampling positions: two opposite edges, two opposite mid-slope positions, and the ravine bottom. The ravines had a specific microclimate characterized by temperature inversion. In general, the cooler and more humid ravine bottoms had also less acid soil with lower carbon content but enriched by litter of deciduous trees and herbs. The other transect positions were characterized by spruce (mid-slopes) and pine (edges) stands with mor humus, exposed to drought in the upper parts. The soil animal communities differed substantially in dependence on their position along the transects. (en)
|
Title
| - Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places
- Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places (en)
|
skos:prefLabel
| - Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places
- Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places (en)
|
skos:notation
| - RIV/00216224:14310/14:00079912!RIV15-MSM-14310___
|
http://linked.open...avai/riv/aktivita
| |
http://linked.open...avai/riv/aktivity
| - I, S, V, Z(AV0Z60660521), Z(MSM0021622416)
|
http://linked.open...iv/cisloPeriodika
| |
http://linked.open...vai/riv/dodaniDat
| |
http://linked.open...aciTvurceVysledku
| |
http://linked.open.../riv/druhVysledku
| |
http://linked.open...iv/duvernostUdaju
| |
http://linked.open...titaPredkladatele
| |
http://linked.open...dnocenehoVysledku
| |
http://linked.open...ai/riv/idVysledku
| - RIV/00216224:14310/14:00079912
|
http://linked.open...riv/jazykVysledku
| |
http://linked.open.../riv/klicovaSlova
| - soil fauna; ravines; gorges; environmental gradients; species richness; drought (en)
|
http://linked.open.../riv/klicoveSlovo
| |
http://linked.open...odStatuVydavatele
| |
http://linked.open...ontrolniKodProRIV
| |
http://linked.open...i/riv/nazevZdroje
| |
http://linked.open...in/vavai/riv/obor
| |
http://linked.open...ichTvurcuVysledku
| |
http://linked.open...cetTvurcuVysledku
| |
http://linked.open...UplatneniVysledku
| |
http://linked.open...v/svazekPeriodika
| |
http://linked.open...iv/tvurceVysledku
| - Devetter, Miloslav
- Háněl, Ladislav
- Starý, Josef
- Pižl, Václav
- Schlaghamerský, Jiří
- Tajovský, Karel
- Tuf, Ivan H.
|
http://linked.open...ain/vavai/riv/wos
| |
http://linked.open...n/vavai/riv/zamer
| |
issn
| |
number of pages
| |
http://bibframe.org/vocab/doi
| - 10.1016/j.apsoil.2013.11.014
|
http://localhost/t...ganizacniJednotka
| |