The Lateglacial and Holocene in Central Europe: a multiproxy environmental record from the Bohemian Forest, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10311942" target="_blank" >RIV/00216208:11310/15:10311942 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/15:00084639 RIV/49777513:23420/15:43925537

Výsledek na webu

<a href="http://dx.doi.org/10.1111/bor.12126" target="_blank" >http://dx.doi.org/10.1111/bor.12126</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/bor.12126" target="_blank" >10.1111/bor.12126</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The Lateglacial and Holocene in Central Europe: a multiproxy environmental record from the Bohemian Forest, Czech Republic

Popis výsledku v původním jazyce

The Hercynian mountain ranges were islands of mountain glaciation and alpine tundra in a Central European ice-free corridor during the Late Pleistocene. Today they are notable areas of glacial landforms, alpine-forest free areas, peatlands and woodlands.However, our knowledge of the Lateglacial and early Holocene environmental changes in this region is limited. We present a new multi-proxy reconstruction of a mid-altitude environment in the Bohemian Forest spanning this period. A core (5.2 m length) inthe Cerne Lake cirque (1028 m a.s.l.) was subjected to lithological, geochemical, pollen and macrofossil analysis supplemented by two optically stimulated luminescence (OSL) and 10 AMS radiocarbon dates. We determined the impact of regional and supraregional climate changes on the environment. The two most significant changes in sedimentation during the Lateglacial (17.6 and 15.8-15.5 cal. ka BP) were synchronous with regional glacial chronostratigraphy. Unlike Central European mountain

Název v anglickém jazyce

The Lateglacial and Holocene in Central Europe: a multiproxy environmental record from the Bohemian Forest, Czech Republic

Popis výsledku anglicky

The Hercynian mountain ranges were islands of mountain glaciation and alpine tundra in a Central European ice-free corridor during the Late Pleistocene. Today they are notable areas of glacial landforms, alpine-forest free areas, peatlands and woodlands.However, our knowledge of the Lateglacial and early Holocene environmental changes in this region is limited. We present a new multi-proxy reconstruction of a mid-altitude environment in the Bohemian Forest spanning this period. A core (5.2 m length) inthe Cerne Lake cirque (1028 m a.s.l.) was subjected to lithological, geochemical, pollen and macrofossil analysis supplemented by two optically stimulated luminescence (OSL) and 10 AMS radiocarbon dates. We determined the impact of regional and supraregional climate changes on the environment. The two most significant changes in sedimentation during the Lateglacial (17.6 and 15.8-15.5 cal. ka BP) were synchronous with regional glacial chronostratigraphy. Unlike Central European mountain

Druh

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

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

—

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Boreas

ISSN

0300-9483

e-ISSN

—

Svazek periodika

44

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

DK - Dánské království

Počet stran výsledku

16

Strana od-do

769-784

Kód UT WoS článku

000362769600010

EID výsledku v databázi Scopus

2-s2.0-84942296220