2020
Biomechanical and Biochemical Effects of Trees in Soil Evolution and Memory in Temperate Old Growth Forests
ŠAMONIL, Pavel; Pavel DANĚK; Anna ROUSOVÁ a Jakub JAROŠZákladní údaje
Originální název
Biomechanical and Biochemical Effects of Trees in Soil Evolution and Memory in Temperate Old Growth Forests
Název česky
Biomechanické a biochemické vlivy stromů v evoluci a paměti půd temperátních pralesů
Autoři
ŠAMONIL, Pavel; Pavel DANĚK; Anna ROUSOVÁ a Jakub JAROŠ
Vydání
Brno, Contemplating Earth: Soil and Landscape Considerations, s. 145-145, 2020
Nakladatel
Mendelova univerzita v Brně
Další údaje
Jazyk
angličtina
Typ výsledku
Stať ve sborníku
Obor
10611 Plant sciences, botany
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Forma vydání
elektronická verze "online"
Odkazy
Označené pro přenos do RIV
Ne
Organizační jednotka
Přírodovědecká fakulta
ISBN
978-80-7509-766-8
UT WoS
Klíčová slova anglicky
forest soil evolution; spatial pedocomplexity; tree-soil interaction; biogeomorphology; soil chemistry; Europe
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 18. 1. 2022 14:11, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
The recent scientific studies have revealed a surprisingly significant influence of individual trees in the soil evolution and in the formation of spatial pedocomplexity of various forest ecosystems. In Central European natural forests, the pedogenetic and biogeomorphologic effects of trees have been neglected for a long time. We enlarged this knowledge by studying the evolution of soils on dated treethrows, by studying the soil properties under standing tree stumps and by studying the evolution of soils under decayed lying trunks. The individual studies originated mainly from the flysch region (Razula Reserve in the Beskydy Mountains), granite (Žofínský Primeval Forest Reserve in the Novohradské Mountains) and gneiss (Boubínský Primeval Forest Reserve in the Šumava Mountains). We were interested in (i) what the trajectory of the soil evolution under the direct influence of trees is compared to unaffected soils (including the proportion of convergent, divergent, chaotic and regressive components of pedogenesis), (ii) how long the traces of trees remain in the soil memory (iii) how the influence of individual trees is reflected in spatial pedocomplexity. The results demonstrated that the individual trees can effectively accelerate, decelerate or even redirect the trajectory of the development of mountain forest soils. Among the studied phenomena, the most significant ones were treethrows with their traces in the soil lasting for thousands of years. In treethrows, a surprisingly complex process combines the mechanical overlay of the material, the sedimentation and microclimatic specifics of the newly formed treethrow mound and treethrow pit area with the biochemical effects of a decomposing uprooted tree trunk and root system. The development of soils in treethrows as well as the development of soils under standing trees and decaying trunks was strongly dependent on the properties of the geological subsoil, and thus on regionally prevailing soil-forming processes (e.g. podzolization, clay formation and its illuviation, etc.). Although the soil development was frequently convergent (particularly within the biochemical effects of the trees), the manifestations of the alternative divergent or chaotic soil development were found out, as well. The progressive trajectory of the evolution dominated, the regressive direction of the development was documented rather sporadically. The outcomes suggest that trees can act as ecosystem engineers in forests and may effectively form ecological niches.