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POKORNÝ, R. EDWARDS, K. J. KRMÍČEK, L. VŠIANSKÝ, D. DÁŇOVÁ P. V.
Original Title
Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands
Type
journal article in Web of Science
Language
English
Original Abstract
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.
Keywords
Faroe Islands; Holocene; pedogenesis; peat; Fe-oxyhydroxide; rhizoconcretion
Authors
POKORNÝ, R.; EDWARDS, K. J.; KRMÍČEK, L.; VŠIANSKÝ, D.; DÁŇOVÁ P. V.
Released
3. 9. 2018
Publisher
Swedish Society for Anthropology and Geography
Location
Stockholm
ISBN
0435-3676
Periodical
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY
Year of study
100
Number
3
State
United Kingdom of Great Britain and Northern Ireland
Pages from
272
Pages to
284
Pages count
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" }