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Morava River floodplain development during the last millennium, Straznicke Pomoravi, Czech Republic

SYSNO ASEP	0324747
Document Type	J - Journal Article
R&D Document Type	Journal Article
Subsidiary J	Článek ve WOS
Title	Morava River floodplain development during the last millennium, Straznicke Pomoravi, Czech Republic
Title	Vývoj nivy řeky Moravy během posledního tisíciletí, Strážnické Pomoraví, Česká republika
Author(s)	Kadlec, Jaroslav (GLU-S)_{RID, SAI, ORCID} Grygar, Tomáš (UACH-T) Světlík, Ivo (UJF-V)_{RID, ORCID, SAI} Ettler, V. (CZ) Mihaljevič, M. (CZ) Diehl, J. F. (US) Beske-Diehl, S. (US) Svitavská-Svobodová, Helena (BU-J)_{RID, ORCID}
Source Title	Holocene. - : Sage - ISSN 0959-6836 Roč. 19, č. 3 (2009), s. 499-509
Number of pages	11 s.
Publication form	www - www
Language	eng - English
Country	GB - United Kingdom
Keywords	floodplain deposits ; river activity reconstruction ; last millenium ; Morava River (Czech Republic) ; expandable clay minerals ; Cu-trien analysis ; mineral magnetic measurements ; lead isotope analysis ; Holocene fluvial records ; land-use change ; pollution sources ; isotopic-ratios ; clay minerals ; soil-erosion
Subject RIV	DO - Wilderness Conservation
R&D Projects	IAAX00130801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
	IAA3013201 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
CEZ	AV0Z30130516 - GLU-S (2005-2011)
	AV0Z4032918 - UACH-T
	AV0Z10480505 - UJF-V (2005-2011)
	AV0Z60050516 - BU-J (2005-2011)
UT WOS	000265513100013
EID SCOPUS	67749129368
DOI	10.1177/0959683608101398
Annotation	The sediments exposed in up to 5 m high erosional river banks were analysed using mineral magnetic, geochemical and chemical approaches. The results reveal the alluvial history of the currently active river channel system since the end of the first millennium AD. Fine overbank clayey sediments deposited during the ‘Mediaeval Warm Period’ were eroded from cultivated fields newly formed during Mediaeval colonization between 1250 and 1450. These fine deposits are overlain by coarser floodplain sediments of the ‘Little Ice Age’, indicating a change in the sediment source since the sixteenth century AD, and a substantial increase in the sediment load in the second half of twentieth century.
Workplace	Institute of Geology
Contact	Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
Year of Publishing	2009

Number of the records: 1