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

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00073965" target="_blank" >RIV/00216224:14310/14:00073965 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985939:_____/14:00431752

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.yqres.2014.04.017" target="_blank" >http://dx.doi.org/10.1016/j.yqres.2014.04.017</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.yqres.2014.04.017" target="_blank" >10.1016/j.yqres.2014.04.017</a>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

<a href="/cs/project/GA206%2F08%2F0389" target="_blank" >GA206/08/0389: Současné a historické změny na horských rašeliništních Sudet</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary Research

ISSN

0033-5894

e-ISSN

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Svazek periodika

82

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

14

Strana od-do

107-120

Kód UT WoS článku

000339138400011

EID výsledku v databázi Scopus

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