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Acta Geologica Polonica

Acta Geologica Polonica

Opis

Acta Geologica Polonica publishes original papers on all aspects of geology. These papers must not have been published or submitted for publication elsewhere, in entirety or in part. The articles should be of moderate length (up to 80 manuscript pages). Longer manuscripts may be accepted but authors should consult the editor before submitting these.

Starting with 2012 you have free access to full texts of all published articles.

Acta Geologica Polonica is now (beginning with volume 54(1) for 2004) in the following Clarivate Analytics products: Science Citation Index-Expanded (SCIE), including the Web of Science, Current Contents/Physical, Chemical & Earth Sciences, ISI Alerting Services.


IMPACT FACTOR 2022: 1.1

CiteScore 2022: 2.1

SCImago Journal Rank (SJR) 2022: 0.477

Source Normalized Impact per Paper (SNIP) 2022: 0.613


Score of the Ministry of Science and Higher Education = 100

ISSN
ISSN 0001-5709
Wydawcy
Komitet Nauk Geologicznych PAN, Wydział Geologii UW

Editorial Team


Editor-in-Chief

Piotr Łuczyński, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland


Editors

Piotr Łuczyński, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland

Anna Żylińska, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland


Assistant Editors

Bogusław Bagiński, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland

Andrzej Konon, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland

Ewa Krogulec, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland


Editorial Board

Zdzisław Bełka, Isotope Laboratory, Adam Mickiewicz University, Krygowskiego Str. 10, PL-61-680 Poznań, Poland

Olaf Elicki, Geological Institute, TU Bergakademie Freiberg (Freiberg University), Bernhard-von-Cotta Str. 2, 09599 Freiberg, Germany

Jerzy Fedorowski, Institute of Geology, Adam Mickiewicz University, Krygowskiego Str. 12, PL-61-680 Poznań, Poland

Peter J. Harries, NC State University, 1020 Main Campus Drive, Raleigh, NC 27695-7102, United States

John W.M. Jagt, Natuurhistorisch Museum Maastricht, de Bosquetplein 6, NL-6211 KJ Maastricht, Netherlands

William James Kennedy, Oxford University, Museum of Natural History, Parks Road, OX1 3PW Oxford, United Kingdom

Jacek Matyszkiewicz, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Mickiewicza Str. 30, PL-30-059 Kraków, Poland

Stanislaw Mazur, Institute of Geological Sciences, Polish Academy of Sciences, Senacka Str. 1, PL-31-002 Kraków, Poland

Jozef Michalik, Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta Str. 9, SK-840-05, Bratislava, Slovakia

Nestor Oszczypko, Institute of Geological Sciences, Jagiellonian University, Gronostajowa Str. 3a, PL-30-387 Kraków, Poland

Grzegorz Racki, Faculty of Earth Sciences, University of Silesia, Będzińska Str. 60, PL-41-200 Sosnowiec, Poland

Ewa Słaby, Institute of Geological Sciences, Polish Academy of Sciences, Twarda Str. 51/55, PL-00-818 Warszawa, Poland

Michał Szulczewski, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland

Susan Turner, Queensland Museum, 122 Gerler Rd., Hendra 4101, Queensland, Australia

Alfred Uchman, Institute of Geological Sciences, Jagiellonian University, Gronostajowa Str. 3a, PL-30-387 Kraków, Poland

Ireneusz Walaszczyk, Faculty of Geology, University of Warsaw, Żwirki i Wigury Str. 93, PL-02-089 Warszawa, Poland

Markus Wilmsen, Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Königsbrücker Landstr. 159, D-01109 Dresden, Germany

Andrzej Ryszard Żelaźniewicz, Institute of Geological Sciences, Polish Academy of Sciences, Podwale Str. 75, PL-50-449 Wrocław, Poland

Faculty of Geology,
University of Warsaw
Al. Zwirki i Wigury 93
02-089 Warszawa, Poland
Phone: +48-22-5540434
Fax: +48-22-5540001
e-mail: agp@uw.edu.pl

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Zawartość

Acta Geologica Polonica | 2022 | vol. 72 | No 3

1 Bashkirian Rugosa (Anthozoa) from the Donets Basin (Ukraine). Part 12. Concluding considerations
Jerzy Fedorowski
Acta Geologica Polonica | 2022 | vol. 72 | No 3 | 247-316 | DOI: 10.24425/agp.2022.140426
Słowa kluczowe: Rugosa (Anthozoa) Global overview Serpukhovian/Bashkirian crisis Lowermost Bashkirian recovery
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Abstrakt

A detailed analysis of the upper Viséan, Serpukhovian and Bashkirian Rugosa of the Donets Basin confirms their Mississippian/Pennsylvanian turnover during the Eumorphoceras / Homalophyllites–Hudsonoceras Zone, as postulated earlier (Fedorowski 1981a). The deterioration of rugose corals, globally diverse in time and space in the late Viséan and Serpukhovian, has resulted in the patchy distribution of survivors and newcomers, present in the Bashkirian. Difficulties in inter-basinal communication and the isolation of some sites have resulted in a different content of Bashkirian Rugosa in particular patches, with only rare genera in common. New data has made it possible to document the appearance of the first late Carboniferous genera in the Donets Basin as early as the lower Voznessenkian Horizon (= lower Chokierian Substage), i.e., close to the beginning of the Bashkirian Stage. The two stages of diversification, established in the Bashkirian rugose corals of the Donets Basin, cannot find their counterparts elsewhere. A palaeogeographic overview of the most important sites of diversified rugose corals documents the need to re-examine many taxa, which should be based on complete specimen studies. This and the precise placement of taxa in the modern stratigraphy must be done in order to make rugose corals globally comparable. Simple repetitions of names, commonly used in general summaries, is strongly misleading in both stratigraphic and palaeogeographic reconstructions.
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Autorzy i Afiliacje

Jerzy Fedorowski
1
  1. Institute of Geology, Adam Mickiewicz University, Bogumiła Krygowskiego 12, 61-680 Poznań, Poland
2 Unusual echinoid resting trace records change in the position of the redox boundary (Palaeogene of the Lesser Caucasus in Georgia)
Alfred Uchman , Zurab Lebanidze , Nino Kobakhidze , Tamar Beridze , Davit Makadze , Koba Lobzhanidze , Sophio Khutsishvili , Rusudan Chagelishvili , Kakha Koiava , Nino Khundadze
Acta Geologica Polonica | 2022 | vol. 72 | No 3 | 317-330 | DOI: 10.24425/agp.2022.140429
Słowa kluczowe: Ichnotaxonomy New ichnotaxa Irregular echinoids Deep sea Flysch Redoxboundary Oxygenation
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Abstrakt

The first recognition of a tracemaker responding to a temporary shift in the redox boundary is recognized. This is recorded by a new trace fossil, Sursumichnus orbicularis igen. et isp. nov., which is established for mound-like structures on the upper surfaces of sandstone beds from the Borjomi Flysch (upper Paleocene–lower Eocene) in the Lesser Caucasus (Georgia). It is connected with the spatangoid echinoid burrow Scolicia de Quatrefages, 1849 and interpreted as a resting trace of the same tracemaker produced after moving up from a deeper position within the sediment. The resting is caused by an episode of unfavourable conditions related to shallowing of the redox boundary. The trace fossil is a component of the Nereites ichnofacies.
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Autorzy i Afiliacje

Alfred Uchman
1
Zurab Lebanidze
2
Nino Kobakhidze
3
Tamar Beridze
3
Davit Makadze
4
Koba Lobzhanidze
3
Sophio Khutsishvili
3
Rusudan Chagelishvili
5
Kakha Koiava
2
Nino Khundadze
4
  1. Faculty of Geography and Geology, Institute of Geological Sciences, Jagiellonian University, Gronostajowa3a, 30-387 Kraków, Poland
  2. Department of Geology, Faculty of Exact and Natural Sciences, Iv. Javakhishvili Tbilisi State University, University str. 13, 0186 Tbilisi, Georgia
  3. Alexander Janelidze Institute of Geology, Iv. Javakhishvili Tbilisi State University, Politkovskaia 31, 0186 Tbilisi, Georgia
  4. Alexander Tvalchrelidze Caucasian Institute of Mineral Resources, Tbilisi State University, 12 Mindeli str., 0186 Tbilisi, Georgia
  5. Department of Geology and Paleontology, Georgian National Museum, 3 Purtseladze str., 0105 Tbilisi, Georgia
3 Calcareous nannofossil biostratigraphy and paleogeographic significance in the lower Maastrichtian of the Miechów Trough (southern Poland)
Urszula Ciołko , Elżbieta Gaździcka
Acta Geologica Polonica | 2022 | vol. 72 | No 3 | 331-352 | DOI: 10.24425/agp.2022.140428
Słowa kluczowe: Lower Maastrichtian Calcareous nannofossil biostratigraphy paleoecology Cooling event Boreal Province Miechów Trough
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Abstrakt

Biostratigraphic analysis of calcareous nannofossils from the Pełczyska section in the Miechów Trough (southern Poland) has revealed that the entire section covers the lowermost Maastrichtian. The UC16bTP Tethyan subzone is designated based on the presence of Broinsonia parca constricta Hattner, Wind and Wise, 1980, reworked remains of Uniplanarius trifidus (Stradner) Hattner and Wise in Wind and Wise, 1983 and the simultaneous lack of Eiffellithus eximius (Stover) Perch-Nielsen, 1968. The studied section spans also the interval between the LO of Zeugrhabdotus praesigmoides Burnett, 1997 and the FO of Prediscosphaera mgayae Lees, 2007 (UC16 S3 Boreal subzone). Quantitative analysis of nannofossil assemblages has shown the dominance of cold water species (up to 50%), e.g., Micula decussata Vekshina, 1959, Prediscosphaera spp., Arkhangelskiella spp., Calculites obscurus (Deflandre) Prins and Sissingh in Sissingh, 1977 and Lucianorhabdus cayeuxii Deflandre, 1959. In the early Maastrichtian, the studied area was more influenced by cool water masses from the Boreal Province rather than by warm water from the Tethyan Province. The significant predominance of cold water taxa and the elevated presence of Prediscosphaera cretacea (Arkhangelsky) Gartner, 1968 also supports the hypothesis of climate cooling in the early Maastrichtian.
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Autorzy i Afiliacje

Urszula Ciołko
1
Elżbieta Gaździcka
2
  1. Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland
  2. Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warszawa, Poland
4 A multi-analytical approach for the analysis of cation distribution in a aluminoceladonite structure
Mariola Kądziołka-Gaweł , Mateusz Dulski , Maria Czaja , Tomasz Krzykawski , Magdalena Szubka
Acta Geologica Polonica | 2022 | vol. 72 | No 3 | 353–368 | DOI: 10.24425/agp.2022.140430
Słowa kluczowe: Aluminoceladonite Ions position characterization isomorphic substitutions Fe‑bearing phyllosilicates X-ray photoelectron spectroscopy (XPS) Mössbauer spectroscopy Raman spectroscopy
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Abstrakt

In this paper cation arrangement in two samples of aluminoceladonite, emerald‑green and dark-green were studied by Mössbauer, Raman and X-ray photoelectron spectroscopies. The X-ray photoelectron spectroscopy (XPS) spectra obtained in the region of the Si2p, Al2p, Fe2p, K2p, and O1s core levels provided information, for the first time highlighting a route to identify the position of Si, Al, K, and Fe cations in a structure of layered silicates. The XPS analysis showed the presence of Al in tetrahedral and octahedral coordination while the K2p line indicated the possibility of K+ substitution by other cations in interlayer sites. Mössbauer spectroscopy provided information about crystal chemistry with respect to the local electronic and geometric environment around the Fe atom and to distortions of the polyhedra. It turned out that iron was located mostly in the cis-octahedra position wherein about 75% of iron appeared in the form of Fe 3+. The most preferred cation combinations around Fe corresponded to 3Fe 3+ ions and MgFe 2+Fe 3+/2MgFe 3+. Raman spectroscopy illustrated aluminium substitution in silicon and iron positions wherein the concentration of the aluminium determined the degree of structural distortion within the layered system. These isomorphic substitutions implied a typical band arrangement in the hydroxyl region, which has not been observed in celadonites so far.
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Autorzy i Afiliacje

Mariola Kądziołka-Gaweł
1
Mateusz Dulski
2
Maria Czaja
3
Tomasz Krzykawski
3
Magdalena Szubka
1
  1. Institute of Physics, University of Silesia, 75 Pułku Piechoty 1, 41-500 Chorzów, Poland
  2. Institute of Material Science, University of Silesia, 75 Pułku Piechoty 1a, 41-500 Chorzów, Poland
  3. Faculty of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland

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