Holocene history and environmental reconstruction of a
Hercynian mire and surrounding mountain landscape based on
multiple proxies

J 2014

Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies

DUDOVÁ, Lydie, Petra HÁJKOVÁ, Věra OPRAVILOVÁ a Michal HÁJEK

Základní údaje

Originální název

Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies

Autoři

DUDOVÁ, Lydie (203 Česká republika, garant, domácí), Petra HÁJKOVÁ (203 Česká republika, domácí), Věra OPRAVILOVÁ (203 Česká republika, domácí) a Michal HÁJEK (203 Česká republika, domácí)

Vydání

Quaternary Research, Elsevier, 2014, 0033-5894

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10600 1.6 Biological sciences

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 2.544

Kód RIV

RIV/00216224:14310/14:00073965

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.yqres.2014.04.017

UT WoS

000339138400011

Klíčová slova česky

přechod slatina-vrchoviště; přenosové funkce; pylová a makrozbytková analýza

Klíčová slova anglicky

fen-bog transition; transfer functions; macrofossil and pollen analysis

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 16. 2. 2018 14:58, prof. Mgr. Michal Hájek, Ph.D.

Anotace

V originále

We discovered the first peat section covering the entire Holocene in the Hrubý Jeseník Mountains. We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry. The mire started to develop as a calcium-rich percolation fen with some species recently considered to be postglacial relicts (Meesia triquetra, Betula nana), shifted into ombrotrophy around 7450 cal yr BP by autogenic succession and changed into a pauperised, nutrient-enriched spruce woodland due to modern forestry activities. Further, we found that the landscape development differed from other Hercynian mountains located westward. This is represented by Pinus cembra and Larix during the Pleistocene/Holocene transition, the early expansion of spruce around 10,450 cal yr BP, and survival of Larix during the climatic optimum.

Návaznosti

GA206/08/0389, projekt VaV

Název: Současné a historické změny na horských rašeliništních Sudet

Investor: Grantová agentura ČR, Současné a historické změny na horských rašeliništích Sudet

Citovat

DUDOVÁ, Lydie, Petra HÁJKOVÁ, Věra OPRAVILOVÁ a Michal HÁJEK. Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies. Quaternary Research. Elsevier, 2014, roč. 82, č. 1, s. 107-120. ISSN 0033-5894. Dostupné z: https://dx.doi.org/10.1016/j.yqres.2014.04.017.

@article{1202767,
   author = {Dudová, Lydie and Hájková, Petra and Opravilová, Věra and Hájek, Michal},
   article_number = {1},
   doi = {http://dx.doi.org/10.1016/j.yqres.2014.04.017},
   keywords = {fen-bog transition; transfer functions; macrofossil and pollen analysis},
   language = {eng},
   issn = {0033-5894},
   journal = {Quaternary Research},
   title = {Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies},
   volume = {82},
   year = {2014}
}

TY  - JOUR
ID  - 1202767
AU  - Dudová, Lydie - Hájková, Petra - Opravilová, Věra - Hájek, Michal
PY  - 2014
TI  - Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies
JF  - Quaternary Research
VL  - 82
IS  - 1
SP  - 107-120
EP  - 107-120
PB  - Elsevier
SN  - 00335894
KW  - fen-bog transition
KW  - transfer functions
KW  - macrofossil and pollen analysis
N2  - We discovered the first peat section covering the entire Holocene in the Hrubý Jeseník Mountains. We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry. The mire started to develop as a calcium-rich percolation fen with some species recently considered to be postglacial relicts (Meesia triquetra, Betula nana), shifted into ombrotrophy around 7450 cal yr BP by autogenic succession and changed into a pauperised, nutrient-enriched spruce woodland due to modern forestry activities. Further, we found that the landscape development differed from other Hercynian mountains located westward. This is represented by Pinus cembra and Larix during the Pleistocene/Holocene transition, the early expansion of spruce around 10,450 cal yr BP, and survival of Larix during the climatic optimum.
ER  -

DUDOVÁ, Lydie, Petra HÁJKOVÁ, Věra OPRAVILOVÁ a Michal HÁJEK. Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies. \textit{Quaternary Research}. Elsevier, 2014, roč.~82, č.~1, s.~107-120. ISSN~0033-5894. Dostupné z: https://dx.doi.org/10.1016/j.yqres.2014.04.017.

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