2018
Biotic controls on Holocene fire frequency in a temperate mountain forest, Czech Republic
BOBEK, Přemysl; Pavel ŠAMONIL a Eva JAMRICHOVÁZákladní údaje
Originální název
Biotic controls on Holocene fire frequency in a temperate mountain forest, Czech Republic
Autoři
BOBEK, Přemysl; Pavel ŠAMONIL a Eva JAMRICHOVÁ
Vydání
JOURNAL OF QUATERNARY SCIENCE, Longman, 2018, 0267-8179
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10508 Physical geography
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.846
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/18:00106719
Organizační jednotka
Přírodovědecká fakulta
UT WoS
EID Scopus
Klíčová slova anglicky
disturbance regime; fire history; Holocene; pedogenesis; soil charcoal
Změněno: 23. 4. 2024 14:46, Mgr. Michal Petr
Anotace
V originále
Mountain spruce-beech-fir mixed forests are an important type of vegetation at higher elevations in temperate Europe. We aimed to determine how fire disturbances have affected long-term vegetation dynamics and to assess their contribution to soil formation. We detected fire episodes using a soil charcoal record extensively dated based on C-14 and combined with pollen and macrocharcoal records from a local peat bog. Altitudinal shifts of the timberline during the Younger Dryas-Holocene transition seem to be responsible for an abrupt occurrence of fire at 11 200 cal a BP. The minimum fire frequency estimation based on dated soil charcoal particles showed variation during the early to mid-Holocene in response to climatic changes. A marked decrease of fire frequency since 6200 cal a BP is attributed to the transformation of vegetation from Picea abies-dominated forests into mixed Fagus sylvatica-Abies alba stands. Once Fagus sylvatica established a dense canopy a profound alteration of the disturbance regime occurred, leading to the exclusion of fire, and has indirectly accelerated the process of podzolization. Thus, the synergistic effects of biotic change are capable of amplifying a climatic impulse, illustrating the important influence of bottom-up controls on fire regimes and soil development.