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Detail publikačního výsledku
POKORNÝ, R.; EDWARDS, K. J.; KRMÍČEK, L.; VŠIANSKÝ, D.; DÁŇOVÁ P. V.
Originální název
Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands
Anglický název
Druh
Článek WoS
Originální abstrakt
The Faroe Islands are characterized by high rates of Holocene geomorphological activity and demonstrable vegetation change, including substantial peat formation. Pedogenesis, especially in the late Holocene, is less well known. Numerous ferruginous rhizoconcretions consisting predominantly of Fe-oxyhydroxides were identified in loam and silty sands in Søltuvík on the island of Sandoy, dated prior to AD 1000. Their formation is related to intensive podzolization and they take the form of the source woody vegetation. The sub-fossil material represents the first evidence for ferruginous rhizoconcretions in the Faroese archipelago.
Anglický abstrakt
Klíčová slova
Faroe Islands; Holocene; pedogenesis; peat; Fe-oxyhydroxide; rhizoconcretion
Klíčová slova v angličtině
Autoři
Rok RIV
2019
Vydáno
03.09.2018
Nakladatel
Swedish Society for Anthropology and Geography
Místo
Stockholm
ISSN
0435-3676
Periodikum
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY
Svazek
100
Číslo
3
Stát
Spojené království Velké Británie a Severního Irska
Strany od
272
Strany do
284
Strany počet
13
BibTex
@article{BUT149630, author="Richard {Pokorný} and Kevin {Edwards} and Lukáš {Krmíček} and Dalibor {Všianský} and Dáňová {Petra}", title="Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands", journal="GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY", year="2018", volume="100", number="3", pages="272--284", doi="10.1080/04353676.2018.1463142", issn="0435-3676" }