2014
Landscape history, calcareous fen development and historical events in the Slovak Eastern Carpathians
JAMRICHOVÁ, Eva, Petra HÁJKOVÁ, Michal HORSÁK, Eliška RYBNÍČKOVÁ, Adam LACINA et. al.Základní údaje
Originální název
Landscape history, calcareous fen development and historical events in the Slovak Eastern Carpathians
Autoři
JAMRICHOVÁ, Eva (703 Slovensko, domácí), Petra HÁJKOVÁ (203 Česká republika, domácí), Michal HORSÁK (203 Česká republika, garant, domácí), Eliška RYBNÍČKOVÁ (203 Česká republika, domácí), Adam LACINA (203 Česká republika, domácí) a Michal HÁJEK (203 Česká republika, domácí)
Vydání
Vegetation History and Archaeobotany, 2014, 0939-6314
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10618 Ecology
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 2.648
Kód RIV
RIV/00216224:14310/14:00073894
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000340522800003
Klíčová slova anglicky
Forest development; Multi-proxy; Macrofossil; Pollen; Snail; Spring fen
Štítky
Změněno: 16. 2. 2018 14:56, prof. Mgr. Michal Hájek, Ph.D.
Anotace
V originále
We explored interactions among human activities, landscape development and changes in biotic proxies in two small calcareous spring fens in the Slovak Eastern Carpathians. These date back to cal. A.D. 930. Results of pollen, plant macrofossil, and mollusc analyses were compared with the settlement history. The regional pollen record reflected historical events and changes in the settlement density very well at both study sites. The natural mixed firbeech-spruce forests with fern undergrowth were suppressed and replaced by light-demanding trees in the periods of high human impact (e.g. Wallachian colonization). The study area was affected several times by wars and raids followed by a consequent decline in the settlement density. Some of these events are well reflected in the pollen records that document tree recovery and decline of cereals, weeds, and pasture indicators. In comparison, only some landscape changes were reflected in the local fen development. Both spring fens originated after deforestation, Rosˇkovce around A.D. 1347 and Mirol’a around A.D. 929. The most pronounced change involving the water regime stabilization and undisturbed development of plant and mollusc communities took place after the decline in human impact. We conclude that humans were the main drivers of landscape transformation in the last millennium; they directly created springfen ecosystems through deforestation and influenced fen species composition through husbandry activities.
Návaznosti
GAP504/11/0429, projekt VaV |
|