Science and earth science

Polish Polar Research

Description

The quarterly Polish Polar Research edited by the Committee on Polar Research of the Polish Academy of Sciences is an international journal publishing original research articles presenting the results of studies carried out in polar regions.

All papers are peer-reviewed and published in English.

The Editorial Advisory Board includes renowned scientist from Poland and from abroad.

Polish Polar Research is indexed in Science Citation Index Expanded, Journal Citation Reports/Science Edition, Biological Abstracts, BIOSIS Previews, Cold Regions Bibliography, Antarctic Literature, Geological Abstracts, Polish Scientific Journals Contents - Agricultural and Biological Sciences, Quarterly Review, and Zoological Record.

Journal Metrics:
Impact Factor 2022: 1.3
CiteScore metrics from Scopus 2022: 2.4
SCImago Journal Rank (SJR) 2022: 0.288
Source Normalized Impact per Paper (SNIP) 2022: 0.512

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We have been made aware of certain fraudulent activities that have been claiming to represent Polish Polar Research. These activities include a fake, predatory website and unsolicited emails. The aim of the fraud is to trick suspected authors/researchers into believing they are communicating with a journal editor in order to obtain their personal information, scientific results and/or money. Polish Polar Research’s name, logo and other information have been used without permission to try to convey authenticity. If you have any concerns or see suspicious communications that reference Polish Polar Research, please report to Editors-in-Chief. Legitimate information regarding Polish Polar Research and its manuscripts can always be found on our website at http://journals.pan.pl/ppr/. We recommend that authors do not respond to any unsolicited offers of manuscript submissions nor enter any monetary agreement.

Polish Polar Research is an open-access journal in which archive issues are freely accessible and articles are published at no cost to authors.

ISSN

ISSN 0138-0338, eISSN 2081-8262

Publishers

Polish Academy of Sciences, Committee on Polar Research

Editorial Advisory Board

Robert BIALIK (Warszawa, Poland)

Magda BŁAŻEWICZ (Łódź, Poland)

Alistair CRAME (Cambridge, UK)

Josef ELSTER (České Budějovice, Czechia)

Jacek JANIA (Sosnowiec, Poland)

Cezary KABAŁA (Wrocław, Poland)

Jerónimo LÓPEZ-MARTINEZ (Madrid, Spain)

Krzysztof MIGAŁA (Wrocław, Poland)

Jerzy NAWROCKI (Warszawa, Poland)

Maria OLECH (Kraków, Poland)

Sergej OLENIN (Klaipeda, Litva)

Sandra PASSCHIER (Montclair, USA)

Jan PAWŁOWSKI (Sopot, Poland)

Żaneta POLKOWSKA (Gdańsk, Poland)

Gerhard SCHMIEDL (Hamburg, Germany)

Peter SCHWEITZER (Vienna, Austria)

Janne SOREIDE (UNIS, Svalbard)

Lech STEMPNIEWICZ (Gdańsk, Poland)

Mateusz STRZELECKI (Wrocław, Poland)

Witold SZCZUCIŃSKI (Poznań, Poland)

Slawek TULACZYK (Santa Cruz, USA)

Jan Marcin WĘSŁAWSKI (Sopot, Poland) - President

Editor-in-Chief

Wojciech MAJEWSKI (Geosciences), Institute of Paleobiology PAS, Poland

e-mail: wmaj@twarda.pan.pl

Co-Editors:

Monika KĘDRA (Life Sciences), Institute of Oceanology PAS, Poland
e-mail: kedra@iopan.gda.pl

Michał ŁUSZCZUK (Social Science and Humanities), UMCS, Poland
e-mail: michal.luszczuk@poczta.umcs.lublin.pl

Associate Editors

Piotr JADWISZCZAK (Białystok),

e-mail: piotrj@uwb.edu.pl

Ewa ŁUPIKASZA (Sosnowiec)

e-mail: ewa.lupikasza@us.edu.pl

Krzysztof ZAWIERUCHA (Poznań)

email: k.p.zawierucha@gmail.com

Editorial Advisory Board

Robert BIALIK (Warszawa, Poland)

Magda BŁAŻEWICZ (Łódź, Poland)

Alistair CRAME (Cambridge, UK)

Josef ELSTER (České Budějovice, Czechia)

Jacek JANIA (Sosnowiec, Poland)

Cezary KABAŁA (Wrocław, Poland)

Jerónimo LÓPEZ-MARTINEZ (Madrid, Spain)

Krzysztof MIGAŁA (Wrocław, Poland)

Jerzy NAWROCKI (Warszawa, Poland)

Maria OLECH (Kraków, Poland)

Sergej OLENIN (Klaipeda, Litva)

Sandra PASSCHIER (Montclair, USA)

Jan PAWŁOWSKI (Sopot, Poland)

Żaneta POLKOWSKA (Gdańsk, Poland)

Gerhard SCHMIEDL (Hamburg, Germany)

Peter SCHWEITZER (Vienna, Austria)

Janne SOREIDE (UNIS, Svalbard)

Lech STEMPNIEWICZ (Gdańsk, Poland)

Mateusz STRZELECKI (Wrocław, Poland)

Witold SZCZUCIŃSKI (Poznań, Poland)

Slawek TULACZYK (Santa Cruz, USA)

Jan Marcin WĘSŁAWSKI (Sopot, Poland) - President

Geosciences
Wojciech MAJEWSKI
e-mail: wmaj@twarda.pan.pl
phone: (48 22) 697 88 53

Instytut Paleobiologii PAN
ul. Twarda 51/55
00-818 Warszawa, POLAND

Life Sciences
Monika KĘDRA
e-mail: kedra@iopan.gda.pl
phone: (48 58) 731 17 79

Instytut Oceanologii PAN
Powstańców Warszawy 55
81-712 Sopot, POLAND, P.O. Box 148

Social Science and Hummanities
Michał ŁUSZCZUK
e-mail: michal.luszczuk@poczta.umcs.lublin.pl
phone: (48 81) 537 68 99

Instytut Geografii Społeczno-Ekonomicznej i Gospodarki Przestrzennej UMCS
Al. Kraśnicka 2D
20-718 Lublin, POLAND

Polish Polar Research is an open access journal with all content available with no charge in full text version.

The journal content is available under the Creative Commons Attribution 4.0 International License ( http://creativecommons.org/licenses/by/4.0/).

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Volumes
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Content

Polish Polar Research | 2015 | No 2

1 Crustal and upper mantle seismic structure of the Svalbard Archipelago from the receiver function analysis

Monika Wilde-Piórko

Polish Polar Research | 2015 | No 2 | 89-107 | DOI: 10.1515/popore−2015−0009

Keywords: Arctic Svalbard teleseismic waves seismogram rotation parameterization quality check

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Abstract

Receiver function provides the signature of sharp seismic discontinuities and the information about the shear wave (S−wave) velocity distribution beneath the seismic station. This information is very valuable in areas where any or few reflection and/or refraction studies are available and global and/or regional models give only rough information about the seismic velocities. The data recorded by broadband seismic stations have been analysed to investigate the crustal and upper mantle structure of the Svalbard Archipelago. Svalbard Archipelago is a group of islands located in Arctic, at the north−western part of the Barents Sea continental platform, which is bordered to the west and to the north by passive continental margins. The new procedure of parameterization and selection of receiver functions (RFs) has been proposed. The back−azimuthal sections of RF show a strong variation for the HSPB and KBS stations. Significant amplitudes of transversal component of RF (T−RF) for the HSPB station indicate a shallow dipping layer towards the southwest. The structure of the crust beneath the SPITS array seems to be less heterogeneous, with very low amplitudes of converted phase comparing to the KBS and HSPB stations. Forward modelling by trial−and−error method shows a division of the crust into 3–4 layers beneath all stations and layering of the uppermost mantle beneath the SPITS array and the HSPB stations. The thickness of the mantle transition zone is larger for western part of archipelago and smaller for eastern part comparing to iasp91 model.

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Authors and Affiliations

Monika Wilde-Piórko

2 The recognition of transient compressional fault slow−slip along the northern shore of Hornsund Fjord, Sw Spitsbergen, Svalbard

Josef Stemberk , Miloš Briestenský , Stefan Cacoń

Polish Polar Research | 2015 | No 2 | 109-123 | DOI: 10.1515/popore−2015−0007

Keywords: Arctic Svalbard Hornsund 3−D fault displacement monitoring transient slow fault slip

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Abstract

This paper presents the results of direct 3−D fault displacement monitoring along the northern shore of Hornsund Fjord, SW Spitsbergen, Svalbard. The fault displacements have been recorded using three permanently installed optical−mechanical crack gauges since 2009. The monitoring data from all three sites provided evidence for a remarkable slip event that lasted from September 2011 to May 2012. The cause is discussed in some detail with consideration given to both exogenic (temperature changes, surface processes) and endogenic processes (isostatic rebound and regional seismicity). It is proposed that transient fault slips recorded had a tectonic origin and were caused by approximately W−E oriented compression corresponding to regional compression in the Svalbard area.

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Authors and Affiliations

Josef Stemberk

Miloš Briestenský

Stefan Cacoń

3 Sedimentological characteristics of debris flow Deposits within ice−cored moraine of Ebbabreen, central Spitsbergen

Krzysztof Pleskot

Polish Polar Research | 2015 | No 2 | 125-144 | DOI: 10.1515/popore−2015−0006

Keywords: Arctic Svalbard debris flow moraine redeposition micromorphology

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Abstract

The Ebbabreen ice−cored moraine area is covered with a sediment layer of up to 2.5 m thick, which mostly consists of massive diamicton. Due to undercutting by lateral streams, debris flow processes have been induced in marginal parts of this moraine. It was recognized that the sedimentology of deposits within the deposition area of debris flows is the effect of: (1) the origin of the sediments, (2) the nature of the debris flow, and (3) post−debris flow reworking. Analysis of debris flow deposits in microscale (thin sections) suggests a common mixing during flow, even though a small amount of parent material kept its original structure. The mixing of sediments during flow leads to them having similar sedimentary characteristics across the deposition area regardless of local conditions ( i.e. slope angle, water content, parent material lithology). After the deposition of sediments that were transported by the debris flow, they were then reworked by a further redeposition process, primarily related to meltwater stream action.

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Authors and Affiliations

Krzysztof Pleskot

4 Glacio−meteorology of Ebbabreen, Dickson Land, central Svalbard, during 2008–2010 melt seasons

Jakub Małecki

Polish Polar Research | 2015 | No 2 | 145-161 | DOI: 10.1515/popore−2015−0010

Keywords: Arctic Spitsbergen glacier meteorology energy balance

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Authors and Affiliations

Jakub Małecki

5 Morphology, ultrastructure and ecology of Muriella decolor (Chlorophyta) from subaerial habitats in Poland and the Antarctic

Maria Olech , Joanna Czerwik-Marcinkowska , Andrzej Massalski , Anna Wojciechowska

Polish Polar Research | 2015 | No 2 | 163-174 | DOI: 10.1515/popore−2015−0011

Keywords: Antarctic moraine Polish caves Muriella decolor ultrastructure

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Abstract

This paper offers a comparison of Muriella decolor specimens from different geographical regions and habitats (limestone caves in Poland and ice denuded areas near the Ecology Glacier, King George Island, South Shetland Islands, West Antarctic). Morphological and cytological variability, ecology and life strategies of M. decolor were studied in fresh samples, and also in cultures grown on agar plates. The complete life cycle, with de − tailed ultrastructural (LM and TEM) analysis are presented. The electron microscopic observations prove that materials identified as M. decolor collected in Poland and the Antarctic have distinct ultrastructural features. These include the chloroplast lamella arrangement, mitochondrial cristae structure and the cell wall thickness.

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Authors and Affiliations

Maria Olech

Joanna Czerwik-Marcinkowska

Andrzej Massalski

Anna Wojciechowska

6 Photosynthetic performance in Antarctic lichens with different growth forms reflect the diversity of lichenized algal adaptation to microhabitats

Shunan Cao , Jie Zhang , Hongyuan Zheng , Chuanpeng Liu , Qiming Zhou

Polish Polar Research | 2015 | No 2 | 175-188 | DOI: 10.1515/popore−2015−0012

Keywords: Antarctic lichens lichenized molecular phylogenetics photosynthesis Trebouxia

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Abstract

Lichens, as typical obligate associations between lichenized fungi and their photosynthetic partners, are dominant in Antarctica. Three Antarctic lichens, Ochrolechia frigida , Umbilicaria antarctica , and Usnea aurantiaco−atra with different growth forms, were sampled nearby the Great Wall Station, King George Island. Molecular data revealed that the photosynthetic algae in these three lichens were Trebouxia jamesii . The net photo − synthesis (Pn) of three individuals from these species, together with environmental factors such as light and temperature, were recorded by CO 2 gas exchange measurements using a CI−340 portable photosynthetic system in situ . Differences between T(leaf) (the temperature of the thalli) and T(air) (the air temperature) for these lichens were not consistent, which reflected that environment and the growth form of thalli could affect T(leaf) significantly. Strong irradiation was expected to have adverse effects on Pn of Ochrolechia frigida and Umbilicaria antarctica whose thalli spread flat; but this photoinhibition had little effect on Usnea aurantiaco−atra with exuberant tufted thallus. These results indicated that photo − synthetic activity in lichens was affected by the growth forms of thalli besides microhabitat factors. One species of lichenized alga could exhibit diversified types of photosynthetic behavior when it was associated with various lichenized fungi in different microhabitats. It will be helpful for understanding how lichens are able to adapt to and colonize in extreme environments.

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Authors and Affiliations

Shunan Cao

Jie Zhang

Hongyuan Zheng

Chuanpeng Liu

Qiming Zhou

7 New records of driftwood lichens in the Kaffiøyra Plain (NW Spitsbergen, Svalbard)

Michał Węgrzyn , Paulina Wietrzyk , Edyta Adamska , Paweł Nicia

Polish Polar Research | 2015 | No 2 | 189-195 | DOI: 10.1515/popore−2015−0008

Keywords: Arctic Svalbard lichen biota lichenized fungi lignicolous lichens

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Abstract

This paper refers to lichen biota growing on driftwood in the Kaffi ø yra Plain (NW Spitsbergen, Svalbard). The presented list of 25 lichenized fungi includes both the eurytopic, accidental, typical, and stenotopic species. Taxa that belong to the last two groups can be considered as lignicolous. This study confirms the existence of a specific group of lichen species, for which the driftwood is a main substrate in the Arctic. Additionally, five lichen species new for the whole Svalbard were recorded, namely: Candelariella coralliza , Elixia flexella , Lecanora saligna , Lecidea plebeja , and Xylographa sibirica .

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Authors and Affiliations

Michał Węgrzyn

Paulina Wietrzyk

Edyta Adamska

Paweł Nicia

Instructions for authors

The quarterly Polish Polar Research invites original scientific papers dealing with all aspects of polar research. The journal aims to provide a forum for publication of high-quality research papers, which are of international interest.

We warmly welcome review papers and proposals for thematic Special Issues.

Articles must be written in English. Authors are requested to have their manuscript read by a person fluent in English before submission. They should not be longer than 30 typescript pages, including tables, figures and references. However, upon request, longer manuscripts may be considered for publication. All papers are peer-reviewed. With a submitted manuscript, authors should provide e-mail addresses of at least three suggested reviewers.

Submission of the manuscript should be supported with a declaration that the work described has not been published previously nor is under consideration by another journal.

For text submission, Word file format is preferred. Please use the PPRes style template when preparing the final version of your paper. Pay special attention to writing correctly the list of references with doi. Manuscripts which are not prepared in line with the template will be returned to the authors. Please submit your manuscripts using our online submission system.

The journal does not have article processing charges (APCs) nor article submission charges. No honorarium will be paid to authors for publishing papers.