Detailed Information on Publication Record
2009
Geochemical tools for the stratigraphic correlation of floodplain deposits of the Morava River in Strážnické Pomoraví, Czech Republic from the last millennium.
GRYGAR, T., I. SVĚTLÍK, Lenka LISÁ, L. KOPTÍKOVÁ, Aleš BAJER et. al.Basic information
Original name
Geochemical tools for the stratigraphic correlation of floodplain deposits of the Morava River in Strážnické Pomoraví, Czech Republic from the last millennium.
Authors
GRYGAR, T. (203 Czech Republic, guarantor), I. SVĚTLÍK (203 Czech Republic), Lenka LISÁ (203 Czech Republic), L. KOPTÍKOVÁ (203 Czech Republic), Aleš BAJER (203 Czech Republic), D.S. WRAY (826 United Kingdom of Great Britain and Northern Ireland), V. ETTLER (203 Czech Republic), M. MIHALJEVIČ (203 Czech Republic), Tereza NOVÁKOVÁ (203 Czech Republic), Magdaléna KOUBOVÁ (203 Czech Republic), Jan NOVÁK (203 Czech Republic), Zdeněk MÁČKA (203 Czech Republic, belonging to the institution) and Mirek SMETANA (203 Czech Republic)
Edition
Catena, 2009, 0341-8162
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 1.933
RIV identification code
RIV/00216224:14310/09:00028649
Organization unit
Faculty of Science
UT WoS
000277373600004
Keywords (in Czech)
fluviální archivy; enviromentální změny; chemostratigrafie; proxy analýzy
Keywords in English
fluvial archives; environmental change; chemostratigraphy; proxy analyses
Tags
Reviewed
Změněno: 20/12/2011 12:09, doc. RNDr. Zdeněk Máčka, Ph.D.
Abstract
V originále
The floodplain of the Morava River in Strážnické Pomoraví, south east Moravia, Czech Republic contains a very valuable record of regional environmental change. We studied 8 outcrops of floodplain deposits from 4 localities along a 6 km long part of the current meander belt of the Morava using geochemical proxy analyses, magnetic susceptibility measurements, 14C dating of wood remnants, and sediment micromorphology. The proxy methods are based on elemental analysis (EDXRF) and analysis of the cation exchange capacity of clay minerals; granulometric analyses provided the basis for lithological and facies assignment of the sediments. The mean depositional rate over the period from about 1000 to about 1900 AD ranged from 0.2 to 0.6 mmy depending on the sedimentary facies. The coeval lithological change in the majority of the studied sections indicated a change of the meander belt structure at between ~1200 AD and ~1600 AD probably as a consequence of changes of channel structure.
Links
IAAX00130801, research and development project |
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