An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany

The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresp...

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Autores: Rusakov, Alexey V., Korkka, Mariya A.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2018
País:México
Institución:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositorio:Revista Mexicana de Ciencias Geológicas
Idioma:inglés
OAI Identifier:oai:ojs.rmcg.geociencias.unam.mx:article/906
Acceso en línea:http://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906
Access Level:acceso abierto
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spelling An isotopic study of a late Quaternary loess-paleosol sequence in SW GermanyEstudio isotópico de una secuencia de loess-paleosuelos del Cuaternario tardío en el suroeste de AlemaniaRusakov, Alexey V.Korkka, Mariya A.The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation. The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shown that the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in the center of the Russian Plain.Se describen las características analítico-morfológicas del suelo fósil Bryansk clasificado como Gleysol úmbrico formado en sedimentos morrénicos y sobreyacido por morrenas de la glaciación Valday (Würmian) del Pleistoceno superior. Este paleosuelo, formado durante el interestadial Dunaevo del Pleistoceno superior y correspondiente a la etapa isotópica marina 3, está confinado a la zona extraglacial del la glaciación Valday. El paleosuelo marca el área más al norte donde se presenta el suelo Bryansk en Europa. Se demuestra que este suelo fósil puede servir como indicador directo de los procesos formadores de paisaje y suelo en el centro de la Planicie Rusa.Universidad Nacional Autónoma de México2018-05-18info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906Revista Mexicana de Ciencias Geológicas; Vol 21 No 1 (2004); 94-100Revista Mexicana de Ciencias Geológicas; Vol 21 No 1 (2004); 94-1002007-29021026-8774reponame:Revista Mexicana de Ciencias Geológicasinstname:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICOinstacron:UNAMenghttp://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906/755info:eu-repo/semantics/openAccessoai:ojs.rmcg.geociencias.unam.mx:article/9062024-08-16T19:51:48Z
dc.title.none.fl_str_mv An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
Estudio isotópico de una secuencia de loess-paleosuelos del Cuaternario tardío en el suroeste de Alemania
title An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
spellingShingle An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
Rusakov, Alexey V.
title_short An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
title_full An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
title_fullStr An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
title_full_unstemmed An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
title_sort An isotopic study of a late Quaternary loess-paleosol sequence in SW Germany
dc.creator.none.fl_str_mv Rusakov, Alexey V.
Korkka, Mariya A.
author Rusakov, Alexey V.
author_facet Rusakov, Alexey V.
Korkka, Mariya A.
author_role author
author2 Korkka, Mariya A.
author2_role author
description The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation. The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shown that the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in the center of the Russian Plain.
publishDate 2018
dc.date.none.fl_str_mv 2018-05-18
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906
url http://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv http://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/906/755
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidad Nacional Autónoma de México
publisher.none.fl_str_mv Universidad Nacional Autónoma de México
dc.source.none.fl_str_mv Revista Mexicana de Ciencias Geológicas; Vol 21 No 1 (2004); 94-100
Revista Mexicana de Ciencias Geológicas; Vol 21 No 1 (2004); 94-100
2007-2902
1026-8774
reponame:Revista Mexicana de Ciencias Geológicas
instname:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
instacron:UNAM
instname_str UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
instacron_str UNAM
institution UNAM
reponame_str Revista Mexicana de Ciencias Geológicas
collection Revista Mexicana de Ciencias Geológicas
repository.name.fl_str_mv
repository.mail.fl_str_mv
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