Detailed Information on Publication Record
2012
Origin and contrasting succession pathways of the Western Carpathian calcareous fens revealed by plant and mollusc macrofossils
HÁJKOVÁ, Petra, Michal HORSÁK, Michal HÁJEK, Adam LACINA, Hana BUCHTOVÁ et. al.Basic information
Original name
Origin and contrasting succession pathways of the Western Carpathian calcareous fens revealed by plant and mollusc macrofossils
Name in Czech
Původ a kontrastní sukcesní řady západokarpatských vápnitých slatinišť odhaleny na základě rostlinných a měkkýších makrozbytků
Authors
HÁJKOVÁ, Petra (203 Czech Republic, guarantor, belonging to the institution), Michal HORSÁK (203 Czech Republic, belonging to the institution), Michal HÁJEK (203 Czech Republic, belonging to the institution), Adam LACINA (203 Czech Republic, belonging to the institution), Hana BUCHTOVÁ (203 Czech Republic, belonging to the institution) and Barbora PELÁNKOVÁ (703 Slovakia, belonging to the institution)
Edition
Boreas, WILEY-BLACKWELL, 2012, 0300-9483
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10600 1.6 Biological sciences
Country of publisher
United States of America
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 2.457
RIV identification code
RIV/00216224:14310/12:00057872
Organization unit
Faculty of Science
UT WoS
000309394800012
Keywords (in Czech)
sukcese; slatiny; multi-proxy
Keywords in English
succession; fens; multi-proxy
Tags
International impact, Reviewed
Změněno: 11/4/2013 12:37, Ing. Andrea Mikešková
V originále
Using plant macrofossil and mollusc analyses of 50 basal samples and three representative profiles we illustrate the most common developmental types of calcareous fens: (i) fens originating in the Lateglacial, having an open or semi-open character during the whole Holocene; (ii) open fens originating as wooded wetlands; and (iii) open fens starting their development de novo in the late Holocene. Human activities were responsible for the formation of a high number of calcareous fens, especially in the Outer Western Carpathians, and became important drivers of fen biodiversity development. Only a few recently existing calcareous fens contain old sequences of calcareous deposits.
In Czech
Za pomoci makrozbytkové analýzy 50 bazálních vrstev a 3 profilů jsme odhalili nejběžnější sukcesní řady vápnitých slatinišť v západních Karpatech. Za vznik celé řady slatinišť je odpovědný člověk, existují však i staré lokality z doby pozdního glaciálu.
Links
| GAP504/11/0429, research and development project |
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