J 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
Název: Gradienty prostředí, vegetační dynamika a krajinné změny v Západních Karpatech od pozdního glaciálu po současnost (Akronym: PALAEO-CARPATHIANS)
Investor: Grantová agentura ČR, Environmental gradients, vegetation dynamics and landscape changes in the West Carpathians from the Late Glacial up to the present time