Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F18%3A00506812" target="_blank" >RIV/67985831:_____/18:00506812 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/18:00102853 RIV/44555601:13520/18:43893683 RIV/00216305:26110/18:PU128868

Výsledek na webu

<a href="https://www.tandfonline.com/doi/full/10.1080/04353676.2018.1463142" target="_blank" >https://www.tandfonline.com/doi/full/10.1080/04353676.2018.1463142</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1080/04353676.2018.1463142" target="_blank" >10.1080/04353676.2018.1463142</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

Late Holocene soil processes and the first evidence for ferruginous rhizoconcretions in cool subpolar environments of the Faroe Islands

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2018

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geografiska Annaler Series A-Physical Geography

ISSN

0435-3676

e-ISSN

—

Svazek periodika

100

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

13

Strana od-do

272-284

Kód UT WoS článku

000443871700004

EID výsledku v databázi Scopus

2-s2.0-85045755622