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Hydrochemical Characteristics of Four Retreating Glacier Forefields Off the Coast of Admiralty Bay (King George Island, Maritime Antarctic)

Diverse Sources of Metals and Metalloids

Bibliographic Data

ID21649529
AuthorsJoanna Potapowicz (0000-0003-1942-8093, Department of Hydrology Faculty of Oceanography and Geography, Gdańsk University Gdańsk Poland, corresponding author), Krystyna Kozioł (0000-0003-1678-3647, Institute of Geography, Kazimierz Wielki University Bydgoszcz Poland), Joanna Plenzler (0000-0002-0566-0062, Institute of Biochemistry and Biophysics, Polish Academy of Science Warsaw Poland), Robert Józef Bialik (0000-0002-0254-6352, Institute of Biochemistry and Biophysics, Polish Academy of Science Warsaw Poland), Justyna Dudek (0000-0001-6233-5381, Department of Environmental Resources and Geohazards Institute of Geography and Spatial Organisation of the Polish Academy of Sciences Torun Poland), Marcin Frankowski (0000-0001-6315-3758, Faculty of Chemistry, Adam Mickiewicz University Poznań Poznań Poland), Anetta Zioła‐Frankowska (0000-0002-8409-5689, Faculty of Chemistry, Adam Mickiewicz University Poznań Poznań Poland), Sara Lehmann‐Konera (0000-0002-8318-0224, Institute of Earth and Environmental Sciences, Faculty of Earth Sciences and Spatial Management, Maria Curie‐Skłodowska University in Lublin Lublin Poland), Żaneta Polkowska (0000-0002-2730-0068, Department of Analytical Chemistry Faculty of Chemistry, Gdansk University of Technology Gdansk Poland, corresponding author)
Year2026
Volume37
Issue4
Pages1330-1352
Publication date2026-02-28
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.70176
OpenAlexW4414340493
LanguageEN
References cited112

This study examines the impact of geological, marine and anthropogenic sources on metal and metalloid concentrations in the forefields of four glaciers (Ecology, Sphinx, Tower and Windy) on King George Island, Antarctic. Water samples were collected at the beginning and end of the hydrological season (austral summer, December 2021 to February 2022), while snow samples were taken from the remaining snow cover at the start of the season. The study area, underlain by the Llano Point and Zamek formations—comprised mainly of basalt and andesite—reveals significant geological contributions of elements such as Fe, Al and Mg due to active weathering processes amplified by glacial retreat. The research highlights how meteorological condition change‐induced temperature and precipitation increases accelerate sediment erosion and weathering, mobilising metals and metalloids from glaciers and snowmelt. Significant concentrations of Cr, V and Ba in collected samples align with the local geological substratum. Statistical analyses (Kruskal–Wallis ANOVA) identified notable differences in Mo and Ba levels between glacier forefields, consistent with geological influences, as these elements occur in varying concentrations within the local basaltic and andesitic bedrock. Seasonal variations were also observed, particularly for Mg and K ions, indicating that meltwater dynamics influence element mobilisation throughout the season. Furthermore, Tower Glacier's eastward exposure explains the higher concentrations of Zn and Cd, suggesting atmospheric deposition as a contributing factor. This study underscores the complex interactions between geological, climatic and atmospheric processes, illustrating how geogenic sources and cryosphere degradation influence the chemical landscape of Antarctic glacier forefields

Climate change · Cryosphere · Glacial period · Glacier · Meltwater · Sediment · Snow · Weathering · Cryospheric studies and observations · Mercury impact and mitigation studies · Polar Research and Ecology

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