Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F14%3A33153249" target="_blank" >RIV/61989592:15310/14:33153249 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60077344:_____/14:00432868 RIV/00216224:14310/14:00079912

Výsledek na webu

<a href="http://www.sciencedirect.com/science/article/pii/S0929139313003016" target="_blank" >http://www.sciencedirect.com/science/article/pii/S0929139313003016</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.apsoil.2013.11.014" target="_blank" >10.1016/j.apsoil.2013.11.014</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places

Popis výsledku v původním jazyce

Sandstone massifs with their deep ravines or gorges 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 Czech Republic), 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 specificmicroclimate 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 (identified to species level) differed substantially in dependence on their position along the transects.

Název v anglickém jazyce

Soil fauna across Central European sandstone ravines with temperature inversion: From cool and shady to dry and hot places

Popis výsledku anglicky

Sandstone massifs with their deep ravines or gorges 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 Czech Republic), 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 specificmicroclimate 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 (identified to species level) differed substantially in dependence on their position along the transects.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DO - Ochrana krajinných území

OECD FORD obor

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Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Applied Soil Ecology

ISSN

0929-1393

e-ISSN

—

Svazek periodika

83

Číslo periodika v rámci svazku

NOV

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

9

Strana od-do

30-38

Kód UT WoS článku

000343318400005

EID výsledku v databázi Scopus

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