Object's details: Environmental history of the Csorna Plain (Western Danube Plain, NW Hungary) from the Late Glacial to the Late Holocene as seen from data of multiproxy geoarchaeological investigations

Provider:Czasopisma PAN

Description

Title:
Environmental history of the Csorna Plain (Western Danube Plain, NW Hungary) from the Late Glacial to the Late Holocene as seen from data of multiproxy geoarchaeological investigations
Creator:
Törőcsik, Tünde;
Gulyás, Sándor;
Sümegi, Pál;
Sümegi, Balázs;
Molnár, Dávid;
Benyó-Korcsmáros, Réka
Description:
Studia Quaternaria is an official international journal of the Committee for Quaternary Research of the Polish Academy of Sciences that is the national representative of the International Union for Quaternary Research. The journal is a continuation of the journal Quaternary Studies in Poland, published irregularly since 1979. Studia Quaternaria (the name since 2000) is an interdisciplinary scientific journal that presents achievements of the Quaternary research, among others in geology, geomorphology, zoology, botany, pedology, archaeology, engineering geology, conducted not only in Poland and Europe, but also in other regions of the world. The published papers focus on various aspects of the Quaternary, including climate and environmental changes, environmental protection, vegetation and fauna development, landscape transformation and impact of human activity. Studia Quaternaria is a peer-reviewed journal with articles published in English and with a DOI number. Potential guest editors who are interested in a thematic volume are kindly requested to contact the Editor-in-Chief. Journal Metrics: IMPACT FACTOR 2022: 0.6 CiteScore 2022: 1.5 SCImago Journal Rank (SJR) 2022: 0.271 Source Normalized Impact per Paper (SNIP) 2022: 0.260;
Editorial Board: Editor-in-Chief: Leszek Marks, Polish Geological Institute, Warsaw, Poland Co-editors: Małgorzata Roman,Faculty of Geographical Sciences, University of Łódź, Łódź, Poland Michał Słowiński, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warsaw, Poland Fabian Welc, Institute of Archaeology, Cardinal Stefan Wyszynski University, Warsaw, Poland Secretary: Joanna Mirosław-Grabowska, Institute of Geological Sciences, Polish Academy of Sciences, Warsaw, Poland Editorial Advisory Board: T. Madeyska (Chairman), Polish Academy of Sciences, Warsaw, Poland S.W. Alexandrowicz, Academy of Mining and Metallurgy, Cracow, Poland K.E. Behre, Niedersachsisches Institut für Historische Küstenforschung, Wilhelmshaven, Germany J. Ehlers, Geologisches Landesamt, Hamburg, Germany P. Gozhik, Ukrainian Academy of Sciences, Kiev, Ukraine V. Ložek, Czech Academy of Sciences, Prague, Czech Republic J.E. Mojski, Gdansk University, Gdańsk, Poland J. Rose, University of London, London, United Kingdom K. Rotnicki, Adam Mickiewicz University, Poznań, Poland M. Sturm, EAWAG-ETH, Zürich, Switzerland J. Vandenberghe, University of Amsterdam, Amserdam, The Netherlands K. Wasylikowa, Polish Academy of Sciences, Cracow, Poland
Object availability:
free access
Rights:
Studia Quaternaria jest czasopismem wydawanym w wolnym dostępie na licencji CC BY-NC-SA 4.0.<a href=" https://creativecommons.org/licenses/by-nc-sa/4.0/">https://creativecommons.org/licenses/by-nc-sa/4.0/</a> Studia Quaternaria is an open access journal with all content available with no charge in full text version. The journal content is available under the licencse CC BY-NC-SA.<a href=" https://creativecommons.org/licenses/by-nc-sa/4.0/">https://creativecommons.org/licenses/by-nc-sa/4.0/</a>
Date:
2019.06.06
Type:
Artykuły / Articles
Source:
Studia Quaternaria; 2019; vol. 36; Iss.1; 19-43
Coverage:
19-43
Publisher:
Committee for Quaternary Research PAS;
Institute of Geological Sciences PAS
Subject:
fluvial geoarchaeology;
environmental history;
flood cycles;
Danube Plain;
NW Hungary;
Nauki o Ziemi
Identifier:
ISSN 1641-5558, e-ISSN 2300-0384
Data provider:
Czasopisma PAN

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Object's details: Environmental history of the Csorna Plain (Western Danube Plain, NW Hungary) from the Late Glacial to the Late Holocene as seen from data of multiproxy geoarchaeological investigations

Description

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