Nauki Ścisłe i Nauki o Ziemi

Polish Polar Research

Opis

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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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

Wydawcy

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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Zawartość

Polish Polar Research | 2015 | No 4

1 Eocene age of the Baranowski Glacier Group at Red Hill, King George Island, West Antarctica

Anna Mozer , Zoltán Pécskay , Krzysztof P. Krajewski

Polish Polar Research | 2015 | No 4 | 307-324 | DOI: 10.1515/popore−2015−0022

Słowa kluczowe: Antarctica King George Island Red Hill Eocene volcanogenic succession K−Ar dating flora

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Abstrakt

Radiometric and geochemical studies were carried out at Red Hill in the southern part of King George Island (South Shetland Islands, northern Antarctic Peninsula) on the Bransfield Strait coast. The rock succession at Red Hill has been determined to represent the Baranowski Glacier Group that was previously assigned a Late Cretaceous age. Two formations were distinguished within this succession: the lower Llano Point Formation and the upper Zamek Formation. These formations have stratotypes defined further to the north on the western coast of Admiralty Bay. On Red Hill the Llano Point Formation consists of terrestrial lavas and pyroclastic breccia; the Zamek Formation consist predominantly of fine to coarse tuff, pyroclastic breccia, lavas, tuffaceous mud− , silt−, and sandstone, locally conglomeratic. The lower part of the Zamek Formation contains plant detritus (Nothofagus , dicotyledonous, thermophilous ferns) and numerous coal seams (vitrinitic composition) that confirm the abundance of vegetation on stratovolcanic slopes and surrounding lowlands at that time. Selected basic to intermediate igneous rocks from the succession have been analysed for the whole−rock K−Ar age determination. The obtained results indicate that the Red Hill succession was formed in two stages: (1) from about 51–50 Ma; and (2) 46–42 Ma, i.e. during the Early to Middle Eocene. This, in combination with other data obtained from other Baranowski Glacier Group exposures on western coast of Admiralty Bay, confirms the recently defined position of the volcano−clastic succession in the stratigraphic scheme of King George Island. The new stratigraphic position and lithofacies development of the Red Hill succession strongly suggest its correlation with other Eocene formations containing fossil plants and coal seams that commonly occur on King George Island.

Przejdź do artykułu

Autorzy i Afiliacje

Anna Mozer

Zoltán Pécskay

Krzysztof P. Krajewski

2 Late Cenozoic Bryozoa from diamictites of Cape Lamb, Vega Island, Antarctic Peninsula

Susana Adamonis , Urszula Hara , Andrea Concheyro

Polish Polar Research | 2015 | No 4 | 325-341 | DOI: 10.1515/popore−2015−0021

Słowa kluczowe: Antarctica James Ross Basin upper Cenozoic diamictites Bryozoans Pleistocene

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Abstrakt

Bryozoans were found in upper Cenozoic diamictite debris that crops out at the southwestern tip of Cape Lamb, Vega Island. The diamictite is the youngest deposit on the island and richly composed of foraminifers, brachiopods and scallops. The foraminifera assemblage recovered from the Cape Lamb diamictite and 87 Sr/ 86 Sr isotopic age obtained from the pectinid Adamussium colbecki in the nearby locality of Terrapin indicates a Pleistocene age for this deposit. The main goal of this contribution is to present a bryozoan assemblage of Microporella stenoporta Hayward et Taylor, Hippothoa flagellum Manzoni, Ellisina antarctica (Kluge), Micropora notialis Hayward et Ryland and an indeterminate crisiid constituting the first record of these bryozoan taxa in Cenozoic diamictites of the Antarctic Peninsula.

Przejdź do artykułu

Autorzy i Afiliacje

Susana Adamonis

Urszula Hara

Andrea Concheyro

3 Another look at tarsometatarsi of early penguins

Piotr Jadwiszczak

Polish Polar Research | 2015 | No 4 | 343-354 | DOI: 10.1515/popore−2015−0024

Słowa kluczowe: Antarctica Eocene Holocene Sphenisciformes foot anatomy reconstruction

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Abstrakt

The tarsometatarsus, a compound bone from the lower leg in birds, is the most important skeletal element in fossil penguin taxonomy, especially in the case of early members of this group. However, any attempt to go beyond the problem of mere classification obviously requires the better understanding of osteological traits under consideration. This in turn touches on the issue of interplay between bone and concomitant soft−tissue structures, such as muscles, tendons and vessels. This paper focuses on the more holistic comprehension of the tarsometatarsal section of the Eocene penguin foot, based on the analysis of the myology and the vascular system of its modern counterparts. A number of graphical reconstructions are provided with a discussion of the role of the hypotarsus and inter− metatarsal foramina.

Przejdź do artykułu

Autorzy i Afiliacje

Piotr Jadwiszczak

4 Two-element acoustic array gives insight into ice-ocean interactions in Hornsund Fjord, Spitsbergen

Oskar Głowacki , Grant B. Deane , Mateusz Moskalik , Jarosław Tęgowski , Philippe Blondel

Polish Polar Research | 2015 | No 4 | 355-367 | DOI: 10.1515/popore−2015−0025

Słowa kluczowe: Tidewater glaciers ice melting passive acoustics Spitsbergen Hornsund

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Abstrakt

Glacierized fjords are dynamic regions, with variable oceanographic conditions and complex ice−ocean interactions, which are still poorly understood. Recent studies have shown that passive underwater acoustics offers new promising tools in this branch of polar research. Here, we present results from two field campaigns, conducted in summer 2013 and spring 2014. Several recordings with a bespoke two−hydrophone acoustic buoy were made in different parts of Hornsund Fjord, Spitsbergen in the vicinity of tidewater glaciers to study the directionality of underwater ambient noise. Representative segments of the data are used to illustrate the analyses, and determine the directions of sound sources by using the time differences of arrivals between two horizontally aligned, broadband hydrophones. The results reveal that low frequency noise (< 3 kHz) is radiated mostly from the ice cliffs, while high−frequency (> 3 kHz) noise directionality strongly depends on the distribution of floating glacial ice throughout the fjord. Changing rates of iceberg production as seen for example in field photographs and logs are, in turn, most likely linked to signal amplitudes for relevant directions. These findings demonstrate the potential offered by passive acoustics to study the dynamics of individual tidewater glaciers.

Przejdź do artykułu

Autorzy i Afiliacje

Oskar Głowacki

Grant B. Deane

Mateusz Moskalik

Jarosław Tęgowski

Philippe Blondel

5 Multidecadal (1960–2011) shoreline changes in Isbjørnhamna (Hornsund, Svalbard)

Anna Styszyńska , Mateusz Moskalik , Piotr Zagórski , Jan Rodzik , Mateusz C. Strzelecki , Michael Lim , Małgorzata Błaszczyk , Agnieszka Promińska , Grzegorz Kruszewski , Artur Malczewski

Polish Polar Research | 2015 | No 4 | 369-390 | DOI: 10.1515/popore−2015−0019

Słowa kluczowe: Tidewater glaciers ice melting passive acoustics Spitsbergen Hornsund

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Abstrakt

A section of a gravel−dominated coast in Isbjørnhamna (Hornsund, Svalbard) was analysed to calculate the rate of shoreline changes and explain processes controlling coastal zone development over last 50 years. Between 1960 and 2011, coastal landscape of Isbjørnhamna experienced a significant shift from dominated by influence of tide−water glacier and protected by prolonged sea−ice conditions towards storm−affected and rapidly changing coast. Information derived from analyses of aerial images and geomorphological mapping shows that the Isbjørnhamna coastal zone is dominated by coastal erosion resulting in a shore area reduction of more than 31,600 m 2 . With ~3,500 m 2 of local aggradation, the general balance of changes in the study area of the shore is negative, and amounts to a loss of more than 28,000 m 2 . Mean shoreline change is −13.1 m (−0.26 m a −1 ). Erosional processes threaten the Polish Polar Station infrastructure and may damage of one of the storage buildings in nearby future.

Przejdź do artykułu

Autorzy i Afiliacje

Anna Styszyńska

Mateusz Moskalik

Piotr Zagórski

e-mail:

ORCID:

Jan Rodzik

Mateusz C. Strzelecki

Michael Lim

Małgorzata Błaszczyk

Agnieszka Promińska

Grzegorz Kruszewski

Artur Malczewski

6 Variability of Salpa thompsoni population structure in the Drake Passage in summer season 2010

Angelika W. Słomska , Anna A. Panasiuk-Chodnicka , Maria I. Żmijewska , Maciej K. Mańko

Polish Polar Research | 2015 | No 4 | 391-404 | DOI: 10.1515/popore−2015−0020

Słowa kluczowe: Antarctic planktonic tunicate horizontal distribution population structure climate change

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Abstrakt

Dynamic climate changes have become noticeable in recent decades, especially in the vulnerable region of the West Antarctic. The relatively simple food web of this area relies on krill – Euphausia superba . Presumably, as a result of climatic fluctuations, a de− crease in the number of this crustacean has been recorded, followed by an increase in the population of the gelatinous zooplankter Salpa thompsoni . In the research presented herein, population and morphometric analyses of Salpa thompsoni have been conducted. Specimens for this research were collected from the Drake Passage, using a Bongo net in the summer season of 2010. It has been found that the horizontal distribution of this gelatinous zooplankter was significantly irregular (Kruskal−Wallis test, p < 0.001). In the northern part of the investigated area, both blastozooids and oozooids were recorded, which confirms the dynamic development of this species. The central part of the Drake Passage was characterized by the dominance of blastozooids, with embryos found at different stages of the development. Only in the region of the South Shetland Islands, the salpid population was characterized by reduced or even stopped reproduction. The immense reproductive efficiency observed in the Salpa thompsoni population was mostly induced by the favourable thermal conditions. These observations may suggest that the ongoing climat changes in the West Antarctic will promote the population expansion of this species.

Przejdź do artykułu

Autorzy i Afiliacje

Angelika W. Słomska

Anna A. Panasiuk-Chodnicka

Maria I. Żmijewska

Maciej K. Mańko

7 Diversity and abundance of isopod fauna associated with holdfasts of the brown alga Himantothallus grandifolius in Admiralty Bay, Antarctic

Karol Zemko , Krzysztof Pabis , Jacek Siciński , Magdalena Błażewicz-Paszkowycz

Polish Polar Research | 2015 | No 4 | 405-415 | DOI: 10.1515/popore−2015−0023

Słowa kluczowe: Antarctic Admiralty Bay Isopoda macroalgae habitat complexity

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Abstrakt

Fifteen species of isopods, representing 10 families, were recorded on holdfasts of the brown alga Himantothallus grandifolius . Material was collected in the 15–75 m depth range during the austral summer of 1979/80. The isopod community was dominated by Caecognathia antarctica (mean density 12.4 ± 13.1 ind./100 ml) followed by Cymodocella tubicauda (mean density 0.7 ± 2.1 ind./100 ml). Mean total density of isopods reached the value of 16.1 ± 14.0 ind./100 ml. The comparison with the other studies showed that hold− fasts are inhabited by a distinctive isopod community that differs from the isopod fauna associated with soft bottom of Admiralty Bay.

Przejdź do artykułu

Autorzy i Afiliacje

Karol Zemko

Krzysztof Pabis

Jacek Siciński

Magdalena Błażewicz-Paszkowycz

Instrukcja dla autorów

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.