Contribution to the European Pollen Database in Neotoma: a pollen diagram of Rokytecká slať mire, Bohemian Forest/Šumava (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985939%3A_____%2F21%3A00546271" target="_blank" >RIV/67985939:_____/21:00546271 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/21:10436254

Výsledek na webu

<a href="https://doi.org/10.1007/s00334-021-00824-3" target="_blank" >https://doi.org/10.1007/s00334-021-00824-3</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s00334-021-00824-3" target="_blank" >10.1007/s00334-021-00824-3</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Contribution to the European Pollen Database in Neotoma: a pollen diagram of Rokytecká slať mire, Bohemian Forest/Šumava (Czech Republic)

Popis výsledku v původním jazyce

The vegetation developmet of the largest montane oligo-ombrotrophic raised bog situated on the Modrava plains has been evaluated by pollen analysis. In the Late Glacial the mire developed around a spring close to the melting glacier on open heliophytic tundra. Propagation of woodland with birch, pine and willow is evidenced in the Boreal. In 8300BC an abrupt climatic change was indicated by furter invasion of trees hazel, spruce, oak, eml and ash. Spruce became the most importat species in taiga landscape. Beech expanded massively, replacing hazel and pine in 5200BC. Dense, high-montane mixed spruce-beech woodlands developed. In 4900 BC fir expanded gradually, whereas pine declined. In 2200BC spruce invaded the highest evevations. The woodlans, where fir became the most abundant climax tree, were dense with closed canopy. Human activity related to the Bronze Age (2200-775 BC) at lower elevation is shown by regular occurence of cereal pollen and indicators of woodland oppenings. The main colonization with intesifying land use occurs in the Middle Ages.

Název v anglickém jazyce

Contribution to the European Pollen Database in Neotoma: a pollen diagram of Rokytecká slať mire, Bohemian Forest/Šumava (Czech Republic)

Popis výsledku anglicky

The vegetation developmet of the largest montane oligo-ombrotrophic raised bog situated on the Modrava plains has been evaluated by pollen analysis. In the Late Glacial the mire developed around a spring close to the melting glacier on open heliophytic tundra. Propagation of woodland with birch, pine and willow is evidenced in the Boreal. In 8300BC an abrupt climatic change was indicated by furter invasion of trees hazel, spruce, oak, eml and ash. Spruce became the most importat species in taiga landscape. Beech expanded massively, replacing hazel and pine in 5200BC. Dense, high-montane mixed spruce-beech woodlands developed. In 4900 BC fir expanded gradually, whereas pine declined. In 2200BC spruce invaded the highest evevations. The woodlans, where fir became the most abundant climax tree, were dense with closed canopy. Human activity related to the Bronze Age (2200-775 BC) at lower elevation is shown by regular occurence of cereal pollen and indicators of woodland oppenings. The main colonization with intesifying land use occurs in the Middle Ages.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10611 - Plant sciences, botany

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2021

Kód důvěrnosti údajů

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

Název periodika

Vegetation History and Archaeobotany

ISSN

0939-6314

e-ISSN

1617-6278

Svazek periodika

30

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

4

Strana od-do

831-834

Kód UT WoS článku

000619754400001

EID výsledku v databázi Scopus

2-s2.0-85100955074