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Search Results (1,429)

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23 pages, 55462 KiB  
Review
Lichens and Health—Trends and Perspectives for the Study of Biodiversity in the Antarctic Ecosystem
by Tatiana Prado, Wim Maurits Sylvain Degrave and Gabriela Frois Duarte
J. Fungi 2025, 11(3), 198; https://doi.org/10.3390/jof11030198 - 4 Mar 2025
Viewed by 199
Abstract
Lichens are an important vegetative component of the Antarctic terrestrial ecosystem and present a wide diversity. Recent advances in omics technologies have allowed for the identification of lichen microbiomes and the complex symbiotic relationships that contribute to their survival mechanisms under extreme conditions. [...] Read more.
Lichens are an important vegetative component of the Antarctic terrestrial ecosystem and present a wide diversity. Recent advances in omics technologies have allowed for the identification of lichen microbiomes and the complex symbiotic relationships that contribute to their survival mechanisms under extreme conditions. The preservation of biodiversity and genetic resources is fundamental for the balance of ecosystems and for human and animal health. In order to assess the current knowledge on Antarctic lichens, we carried out a systematic review of the international applied research published between January 2019 and February 2024, using the PRISMA model (Preferred Reporting Items for Systematic Reviews and Meta-Analyses). Articles that included the descriptors “lichen” and “Antarctic” were gathered from the web, and a total of 110 and 614 publications were retrieved from PubMed and ScienceDirect, respectively. From those, 109 publications were selected and grouped according to their main research characteristics, namely, (i) biodiversity, ecology and conservation; (ii) biomonitoring and environmental health; (iii) biotechnology and metabolism; (iv) climate change; (v) evolution and taxonomy; (vi) reviews; and (vii) symbiosis. Several topics were related to the discovery of secondary metabolites with potential for treating neurodegenerative, cancer and metabolic diseases, besides compounds with antimicrobial activity. Survival mechanisms under extreme environmental conditions were also addressed in many studies, as well as research that explored the lichen-associated microbiome, its biodiversity, and its use in biomonitoring and climate change, and reviews. The main findings of these studies are discussed, as well as common themes and perspectives. Full article
(This article belongs to the Section Fungal Evolution, Biodiversity and Systematics)
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<p>Number of publications in the PubMed database from January 1980 to December 2023 that include the descriptor “lichen” (light blue, with scale on the left); number of publications on lichens related to Antarctic ecosystems in the PubMed database from January 1980 to December 2023, including the descriptors “lichen” and “Antarctic” (dark blue, with scale on the right).</p>
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<p>Flowchart of selection steps for studies related to lichen research in Antarctic ecosystem (January 2019 to February 2024).</p>
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<p>Number of studies included by thematic area (January 2019–February 2024).</p>
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<p>Heatmap showing the number of studies according to the country of the first author involved in lichen research in the Antarctic ecosystem by thematic area (January 2019–February 2024). Data spanned from white (low number of articles) to dark blue (higher number of articles), as illustrated by the color scale in the bar.</p>
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19 pages, 6589 KiB  
Article
Atmospheric Corrosion Behavior of Typical Aluminum Alloys in Low-Temperature Environment
by Tengfei Cui, Jianguo Wu, Jian Song, Di Meng, Xiaoli Jin, Huiyun Tian and Zhongyu Cui
Metals 2025, 15(3), 277; https://doi.org/10.3390/met15030277 - 4 Mar 2025
Viewed by 80
Abstract
The atmospheric corrosion behavior of type 2024, 5083, 6061, and 7075 aluminum alloys in the Antarctic environment was investigated by outdoor exposure tests and indoor characterization. After one year of exposure to the Antarctic atmosphere, significant differences in surface corrosion states were observed [...] Read more.
The atmospheric corrosion behavior of type 2024, 5083, 6061, and 7075 aluminum alloys in the Antarctic environment was investigated by outdoor exposure tests and indoor characterization. After one year of exposure to the Antarctic atmosphere, significant differences in surface corrosion states were observed among the specimens. The results revealed that the corrosion rate of the 2024 aluminum alloy was the highest, reaching 14.5 g/(m2·year), while the 5083 aluminum alloy exhibited the lowest corrosion rate of 1.36 g/(m2·year). The corrosion products formed on the aluminum alloys exposed to the Antarctic environment were primarily composed of AlOOH and Al2O3. In the Antarctic atmosphere environment, the pits were dominated by a freezing–thawing cycle and salt deposition. The freezing–thawing cycle promotes the wedge effect of corrosion products at the grain boundary, resulting in exfoliation corrosion of high-strength aluminum alloys. Full article
(This article belongs to the Special Issue Corrosion of Metals: Behaviors and Mechanisms)
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<p>Microstructure characteristics of 2024 (<b>a</b>,<b>a1</b>), 5083 (<b>b</b>,<b>b1</b>), 6061 (<b>c</b>,<b>c1</b>), and 7075 (<b>d</b>,<b>d1</b>) aluminum alloys, as well as the fraction of the granular intermetallic compounds of a typical aluminum alloy field area (<b>e</b>). The red boxes are the EDS test area.</p>
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<p>Corrosion rates of 2024, 5083, 6061, and 7075 aluminum alloys exposed to Antarctic atmospheric environment.</p>
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<p>XRD spectra of 2024, 5083, 6061, and 7075 aluminum alloys exposed to Antarctic atmospheric environment.</p>
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<p>Macromorphology of the skyward and groundward surfaces of 2024 aluminum alloy (<b>a</b>,<b>b</b>), 5083 aluminum alloy (<b>c</b>,<b>d</b>), 6061 aluminum alloy (<b>e</b>,<b>f</b>), and 7075 aluminum alloy (<b>g</b>,<b>h</b>) under Antarctic atmospheric environment.</p>
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<p>The magnified surface morphologies at 100× and 500×, along with the results of EDS (energy-dispersive spectroscopy, point analysis), of 2024 (<b>a<sub>1</sub></b>,<b>b<sub>1</sub></b>), 5083 (<b>a<sub>2</sub></b>,<b>b<sub>2</sub></b>), 6061 (<b>a<sub>3</sub></b>,<b>b<sub>3</sub></b>), and 7075 (<b>a<sub>4</sub></b>,<b>b<sub>4</sub></b>) aluminum alloys after one year of exposure to the Antarctic atmospheric environment.</p>
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<p>The cross-sectional morphologies and EDS mapping results of 2024 (<b>a</b>), 5083 (<b>b</b>), 6061 (<b>c</b>), and 7075 (<b>d</b>) aluminum alloys after one year of exposure to the Antarctic atmospheric environment. The light-gray sections represent the substrate, while the areas marked with blue dashed lines indicate the corrosion products.</p>
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<p>XPS spectra of 2024 (<b>a</b>), 5083 (<b>b</b>), 6061 (<b>c</b>), and 7075 (<b>d</b>) aluminum alloys exposed to the Antarctic atmospheric environment.</p>
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<p>Surface morphologies of 2024 (<b>a</b>,<b>b</b>), 5083 (<b>c</b>,<b>d</b>), 6061 (<b>e</b>,<b>f</b>), and 7075 (<b>g</b>,<b>h</b>) aluminum alloys after removing corrosion products.</p>
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<p>3D corrosion morphologies of 2024 (<b>a</b>,<b>b</b>), 5083 (<b>c</b>,<b>d</b>), 6061 (<b>e</b>,<b>f</b>), and 7075 (<b>g</b>,<b>h</b>) aluminum alloys after removing corrosion products.</p>
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<p>Pit cumulative probability (<b>a</b>), pit depth statistics (<b>b</b>), average depth of corrosion defects (<b>c</b>), and maximum depth of corrosion defects (<b>d</b>) for 2024, 5083, 6061, and 7075 aluminum alloys.</p>
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<p>Schematic illustration of corrosion process of aluminum alloy in Antarctic environment (<b>a</b>), pit initiation process (<b>b</b>), intergranular corrosion process (<b>c</b>), exfoliation corrosion process (<b>d</b>).</p>
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21 pages, 3918 KiB  
Article
Biodegradation of Polyhydroxybutyrate, Polylactide, and Their Blends by Microorganisms, Including Antarctic Species: Insights from Weight Loss, XRD, and Thermal Studies
by Volodymyr Skorokhoda, Ihor Semeniuk, Taras Peretyatko, Viktoria Kochubei, Oleksandr Ivanukh, Yuriy Melnyk and Yurij Stetsyshyn
Polymers 2025, 17(5), 675; https://doi.org/10.3390/polym17050675 - 2 Mar 2025
Viewed by 246
Abstract
This study explores the biodegradation of polyhydroxybutyrate (PHB), polylactide (PLA), and their blends by 11 bacterial species (including Antarctic strains) and 6 fungal species. Aeration significantly enhanced PHB degradation by mold fungi (Aspergillus oryzae, Penicillium chrysogenum) and bacteria (Paenibacillus [...] Read more.
This study explores the biodegradation of polyhydroxybutyrate (PHB), polylactide (PLA), and their blends by 11 bacterial species (including Antarctic strains) and 6 fungal species. Aeration significantly enhanced PHB degradation by mold fungi (Aspergillus oryzae, Penicillium chrysogenum) and bacteria (Paenibacillus tundrae, Bacillus mycoides), while Aspergillus awamori was most effective under non-aerated conditions. For PLA, degradation peaked under aeration with Penicillium chrysogenum and Bacillus subtilis. PHB/PLA blends degraded slower overall, with maximum degradation under aeration by Penicillium chrysogenum, Pseudoarthrobacter sp., and Flavobacterium sp. Biodegradation was assessed via weight-loss measurements, X-ray diffraction (XRD), and thermal analysis. PHB samples showed reduced crystallinity and thermal stability linked to weight loss, while PLA samples exhibited varied changes, often with increased crystallinity and stability depending on the microorganism. PHB/PLA blends displayed variable crystallinity changes, generally decreasing under microbial action. The search for effective plastic-degrading microorganisms, particularly from extreme environments like Antarctica, is vital for addressing plastic pollution and advancing sustainable polymer degradation. Full article
(This article belongs to the Section Biobased and Biodegradable Polymers)
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<p>Sample of diffractogram with a “baseline” dividing it into crystalline peaks and an amorphous region. The red line shows the distribution between the amorphous and crystalline phases.</p>
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<p>A general scheme illustrating the relationship between the preparation of polymer samples, their cultivation in a medium with microorganisms, and the analysis of their properties.</p>
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<p>Degree of degradation (%) of PHB films without aeration (orange colour) and under aeration (green colour) after 14 days of cultivation in Sabouraud medium and by various mold fungi species (1m.—<span class="html-italic">Aspergillus oryzae</span>; 2m.—<span class="html-italic">Penicillium chrysogenum</span>; 3m.—<span class="html-italic">Trichoderma lignorum</span>; 4m.—<span class="html-italic">Aspergillus niger;</span> 5m.—<span class="html-italic">Aspergillus awamori</span>; 6m.—<span class="html-italic">Trichothecium roseum</span>) (<b>a</b>) and in TSB and by various bacteria species (1b.—<span class="html-italic">Paenibacillus tundrae</span> IMV B-7915; 2b.—<span class="html-italic">Pseudomonas yamanorum</span> IMV B-7916; 3b.—<span class="html-italic">Paenarthrobacter</span> sp. 28-in-78; 4b.—<span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981; 5b.—<span class="html-italic">Flavobacterium</span> sp. 2B-in-99; 6b.—<span class="html-italic">Bacillus mesentericus</span>; 7b.—<span class="html-italic">Bacillus megaterium</span>; 8b.—<span class="html-italic">Bacillus cereus</span>; 9b.—<span class="html-italic">Bacillus mycoides</span>; 10b.—<span class="html-italic">Bacillus subtilis</span>; 11b.—<span class="html-italic">Streptomyces griseus</span>) (<b>b</b>). The red lines are a guide for the eyes.</p>
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<p>Degree of degradation (%) of PLA films without aeration (orange colour) and under aeration (green colour) after 14 days of cultivation in Sabouraud medium and by various mold fungi species (1m.—<span class="html-italic">Aspergillus oryzae</span>; 2m.—<span class="html-italic">Penicillium chrysogenum</span>; 3m.—<span class="html-italic">Trichoderma lignorum</span>; 4m.—<span class="html-italic">Aspergillus niger;</span> 5m.—<span class="html-italic">Aspergillus awamori</span>; 6m.—<span class="html-italic">Trichothecium roseum</span>) (<b>a</b>) and in TSB and by various bacteria species (1b.—<span class="html-italic">Paenibacillus tundrae</span> IMV B-7915; 2b.—<span class="html-italic">Pseudomonas yamanorum</span> IMV B-7916; 3b.—<span class="html-italic">Paenarthrobacter</span> sp. 28-in-<span class="html-italic">78</span>; 4b.—<span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981; 5b.—<span class="html-italic">Flavobacterium</span> sp. 2B-in-99; 6b.—<span class="html-italic">Bacillus mesentericus</span>; 7b.—<span class="html-italic">Bacillus megaterium</span>; 8b.—<span class="html-italic">Bacillus cereus</span>; 9b.—<span class="html-italic">Bacillus mycoides</span>; 10b.—<span class="html-italic">Bacillus subtilis</span>; 11b.—<span class="html-italic">Streptomyces griseus</span>) (<b>b</b>). The red lines are a guide for the eyes.</p>
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<p>Degree of degradation (%) of PHB/PLA (62/38) films without aeration (orange colour) and under aeration (green colour) after 14 days of cultivation in Sabouraud medium and by various mold fungi species (1m.—<span class="html-italic">Aspergillus oryzae</span>; 2m.—<span class="html-italic">Penicillium chrysogenum</span>; 3m.—<span class="html-italic">Trichoderma lignorum</span>; 4m.—<span class="html-italic">Aspergillus niger;</span> 5m.—<span class="html-italic">Aspergillus awamori</span>; 6m.—<span class="html-italic">Trichothecium roseum</span>) (<b>a</b>) and in TSB and by various bacteria species (1b.—<span class="html-italic">Paenibacillus tundrae</span> IMV B-7915; 2b.—<span class="html-italic">Pseudomonas yamanorum</span> IMV B-7916; 3b.—<span class="html-italic">Paenarthrobacter</span> sp. 28-in-78; 4b.—<span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981; 5b.—<span class="html-italic">Flavobacterium</span> sp. 2B-in-99; 6b.—<span class="html-italic">Bacillus mesentericus</span>; 7b.—<span class="html-italic">Bacillus megaterium</span>; 8b.—<span class="html-italic">Bacillus cereus</span>; 9b.—<span class="html-italic">Bacillus mycoides</span>; 10b.—<span class="html-italic">Bacillus subtilis</span>; 11b.—<span class="html-italic">Streptomyces griseus</span>) (<b>b</b>). The red lines are a guide for the eyes.</p>
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<p>Correlation between crystallinity changes and polymer weight loss due to degradation by molds and bacteria for PHB, PLA, and PHB/PLA (62/38) blend.</p>
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<p>Combined TG, DTA, and DTG curves for PHB cultivated in Sabouraud medium under aeration (<b>a</b>) and PHB exposed to <span class="html-italic">Trichoderma roseum</span> under aeration (<b>b</b>), including DTA (<b>c</b>), TGA (<b>d</b>), and DTG (<b>e</b>) curves comparing the thermal characteristics of PHB in Sabouraud medium (black line) and PHB exposed to <span class="html-italic">Trichoderma roseum</span> (red line).</p>
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<p>Combined TG, DTA, and DTG curves for PHB cultivated in TSB medium under aeration (<b>a</b>) and PHB exposed to <span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981 (<b>b</b>) and <span class="html-italic">Streptomyces griseus</span> (<b>c</b>) under aeration, including DTA (<b>d</b>), TGA (<b>e</b>), and DTG (<b>f</b>) curves comparing the thermal characteristics of PHB in a TSB medium (black line) and a PHB sample exposed to <span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981 (red line) and <span class="html-italic">Streptomyces griseus</span> (green line).</p>
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<p>Combined TG, DTA, and DTG curves for PLA cultivated in Sabouraud medium with aeration (<b>a</b>) and PLA exposed to <span class="html-italic">Trichoderma roseum</span> under aeration (<b>b</b>), including DTA (<b>c</b>), TGA (<b>d</b>), and DTG (<b>e</b>) curves comparing the thermal characteristics of PLA in Sabouraud medium (black line) and PLA exposed to <span class="html-italic">Trichoderma roseum</span> (red line).</p>
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<p>Combined TG, DTA, and DTG curves for PLA cultivated in TSB medium without aeration (<b>a</b>) and PLA exposed to <span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981 (<b>b</b>) and <span class="html-italic">Streptomyces griseus</span> (<b>c</b>) under aeration, including DTA (<b>d</b>), TGA (<b>e</b>), and DTG (<b>f</b>) curves comparing the thermal characteristics of PLA in a TSB medium (black line) and a PHB sample exposed to <span class="html-italic">Pseudoarthrobacter</span> sp. IMV B-7981 (red line) and <span class="html-italic">Streptomyces griseus</span> (green line).</p>
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12 pages, 255 KiB  
Review
Pollution Has No Borders: Microplastics in Antarctica
by Daniela Pellegrino, Daniele La Russa and Laura Barberio
Environments 2025, 12(3), 77; https://doi.org/10.3390/environments12030077 - 2 Mar 2025
Viewed by 173
Abstract
In recent years, microplastic pollution has become one of the major global concerns and represents a complex, multidimensional, and multisectoral reality. The considerable existing data relating to microplastic pollution in matrices such as water and soil suggests that microplastics are widespread globally, but [...] Read more.
In recent years, microplastic pollution has become one of the major global concerns and represents a complex, multidimensional, and multisectoral reality. The considerable existing data relating to microplastic pollution in matrices such as water and soil suggests that microplastics are widespread globally, but there are several knowledge gaps regarding their actual distribution mostly in remote locations far from sources. In this review we examine current knowledge on microplastic pollution in the Antarctic continent. Antarctica, the unique continent not permanently anthropized, is the southernmost part of the planet but its geographic isolation does not protect against the harmful impact of human activities. This continent is characterized by limited internal pollution sources but high-burden external routes of contaminants and represents a unique natural laboratory to analyze how pollution can reach every part of the biosphere. This review reports the presence of microplastics in organic and inorganic matrices not only at marine level (water, sediments, benthic organisms, krill, and fish) but also in freshwater (lakes, rivers, snow, and glaciers) highlighting that microplastic contamination is endemic in the Antarctic environment. Microplastic pollution is of great environmental concern everywhere, but the characteristics of remote ecosystems suggest that they could be more sensitive to harm from this pollution. Full article
29 pages, 10898 KiB  
Article
Antioxidant and Antidiabetic Potential of the Antarctic Lichen Gondwania regalis Ethanolic Extract: Metabolomic Profile and In Vitro and In Silico Evaluation
by Alfredo Torres-Benítez, José Erick Ortega-Valencia, Nicolás Jara-Pinuer, Jaqueline Stephanie Ley-Martínez, Salvador Herrera Velarde, Iris Pereira, Marta Sánchez, María Pilar Gómez-Serranillos, Ferdinando Carlo Sasso, Mario Simirgiotis and Alfredo Caturano
Antioxidants 2025, 14(3), 298; https://doi.org/10.3390/antiox14030298 - 28 Feb 2025
Viewed by 198
Abstract
Lichens are an important source of diverse and unique secondary metabolites with recognized biological activities through experimental and computational procedures. The objective of this study is to investigate the metabolomic profile of the ethanolic extract of the Antarctic lichen Gondwania regalis and evaluate [...] Read more.
Lichens are an important source of diverse and unique secondary metabolites with recognized biological activities through experimental and computational procedures. The objective of this study is to investigate the metabolomic profile of the ethanolic extract of the Antarctic lichen Gondwania regalis and evaluate its antioxidant and antidiabetic activities with in vitro, in silico, and molecular dynamics simulations. Twenty-one compounds were tentatively identified for the first time using UHPLC/ESI/QToF/MS in negative mode. For antioxidant activity, the DPPH assay showed an IC50 value of 2246.149 µg/mL; the total phenolic content was 31.9 mg GAE/g, the ORAC assay was 13.463 µmol Trolox/g, and the FRAP assay revealed 6.802 µmol Trolox/g. Regarding antidiabetic activity, enzyme inhibition yielded IC50 values of 326.4513 µg/mL for pancreatic lipase, 19.49 µg/mL for α-glucosidase, and 585.216 µg/mL for α-amylase. Molecular docking identified sekikaic acid as the most promising compound, with strong binding affinities to catalytic sites, while molecular dynamics confirmed its stability and interactions. Toxicological and pharmacokinetic analyses supported its drug-like potential without significant risks. These findings suggest that the ethanolic extract of Gondwania regalis is a promising source of bioactive compounds for developing natural antioxidant and antidiabetic therapies. Full article
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Figure 1
<p>(<b>a</b>) Aspect of thallus and the apothecia of <span class="html-italic">G. regalis</span> (scale bar = 1 cm); (<b>b</b>) cross section of an apothecium of <span class="html-italic">G. regalis</span> (scale bar = 100 µm); (<b>c</b>) aspect of asci, paraphyses, and photobiont (scale bar = 10 µm); (<b>d</b>) polarilocular spores of <span class="html-italic">G. regalis</span> (scale bar = 10 µm).</p>
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<p>Distribution of <span class="html-italic">G. regalis</span> in the world (GBIF).</p>
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<p>UHPLC/ESI/QToF/MS chromatogram of <span class="html-italic">G. regalis</span> ethanolic extract. The numbers above the peaks correspond to major compounds identified in the extract.</p>
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<p>Evaluation of the pharmacokinetic properties based on Lipinski’s rules using the Osiris Data Warrior software of the phytochemicals identified in the <span class="html-italic">G. regalis</span> species.</p>
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<p>Analysis of toxicological risks (mutagenicity, tumorigenicity, reproductive effects, and irritant effects) using the Osiris Data Warrior software of the phytochemicals identified in the <span class="html-italic">G. regalis</span> species.</p>
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<p>Molecular docking between the compound sekikaic acid and α-amylase. (<b>A</b>) Adopted molecular geometry of the sekikaic acid compound in the catalytic pocket of the α-amylase enzyme; (<b>B</b>) zoom view of the geometry adopted by the compound sekikaic acid in the catalytic pocket of α-amylase; (<b>C</b>) analysis of hydrogen bonds of the sekikaic acid–α-amylase complex; (<b>D</b>) map of predominant interactions of the molecular docking of the compound sekikaic acid and α-amylase; (<b>E</b>) binding energies of the identified compounds of the <span class="html-italic">G. regalis</span> species and the reference inhibitor acarbose. A one-way ANOVA was performed with a Dunnet test of multiple comparisons where the asterisks above the standard error of the mean bars between the groups indicate that the differences were statistically significant at <span class="html-italic">p</span> &lt; 0.0001 (****) and ns = there is no significant difference.</p>
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<p>Molecular docking between the compound sekikaic acid and α-glucosidase. (<b>A</b>) Adopted molecular geometry of the sekikaic acid compound in the catalytic pocket of the α-glucosidase enzyme; (<b>B</b>) zoom view of the geometry adopted by the compound sekikaic acid in the catalytic pocket of α-glucosidase; (<b>C</b>) analysis of hydrogen bonds of the sekikaic acid–α-glucosidase complex; (<b>D</b>) map of predominant interactions of the molecular docking of the compound sekikaic acid and α-glucosidase; (<b>E</b>) binding energies of the identified compounds of the <span class="html-italic">G. regalis</span> species and the reference inhibitor acarbose. A one-way ANOVA was performed with a Dunnet test of multiple comparisons where the asterisks above the standard error of the mean bars between the groups indicate that the differences were statistically significant at <span class="html-italic">p</span> &lt; 0.001 (***), or <span class="html-italic">p</span> &lt; 0.0001 (****) and ns = there is no significant difference.</p>
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<p>The molecular docking between the compound sekikaic acid and human pancreatic lipase. (<b>A</b>) Adopted molecular geometry of the sekikaic acid compound in the catalytic pocket of the human pancreatic lipase enzyme; (<b>B</b>) zoom view of the geometry adopted by the compound sekikaic acid in the catalytic pocket of human pancreatic lipase; (<b>C</b>) analysis of hydrogen bonds of the sekikaic acid human pancreatic lipase complex; (<b>D</b>) map of predominant interactions of the molecular docking of the compound sekikaic acid and human pancreatic lipase; (<b>E</b>,<b>F</b>) binding energies of the identified compounds of the <span class="html-italic">G. regalis</span> species and the references inhibitors MUP y orlistat. A one-way ANOVA was performed with a Dunnet test of multiple comparisons where the asterisks above the standard error of the mean bars between the groups indicate that the differences were statistically significant at <span class="html-italic">p</span> &lt; 0.01 (**), or <span class="html-italic">p</span> &lt; 0.0001 (****) and ns = there is no significant difference.</p>
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<p>Results obtained from molecular dynamics simulation over a 30 ns simulation period of the compound sekikaic acid with the proteins α-amylase (PDB ID: 2QV4), α-glucosidase (PDB ID: 2QMJ), and human lipase pancreatic (PDB ID: 1LPB). (<b>A</b>–<b>C</b>) Root mean square deviation (RMSD), root mean square fluctuation (RMSF), and number of hydrogen bonds, respectively, of the sekikaic acid and α-amylase complex (PDB ID: 2QV4); (<b>D</b>–<b>F</b>) root mean square deviation (RMSD), root mean square fluctuation (RMSF), and number of hydrogen bonds, respectively, of the sekikaic acid and α-glucosidase complex (PDB ID: 2QMJ); (<b>G</b>–<b>I</b>) root mean square deviation (RMSD), root mean square fluctuation (RMSF), and number hydrogen bonds, respectively, of the sekikaic acid and human pancreatic lipase complee (PDB ID: 1LPB).</p>
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18 pages, 14465 KiB  
Article
Environmentally Friendly Sampling and Observation System for Exploration of Antarctic Subglacial Lakes
by Zhipeng Deng, Youhong Sun, Xiaopeng Fan, Pavel Talalay, Bing Li, Ting Wang, Yazhou Li, Haibin Yu, Dongliang Wang, Jing Xu, Liping Xu, Chunlei An, Shilin Peng, Nan Zhang, Zhiyong Chang, Yanji Chen, Yunchen Liu, Xiao Yang, Yu Wang, Xianzhe Wei, Rusheng Wang, Zhigang Wang, Xiaokang Ni, Wei Wu and Da Gongadd Show full author list remove Hide full author list
Water 2025, 17(5), 696; https://doi.org/10.3390/w17050696 - 27 Feb 2025
Viewed by 226
Abstract
The sampling and observation of subglacial lakes play a vital role in studying the physical and chemical properties as well as the microbial characteristics of water within these Antarctic subglacial lakes. Compared to existing techniques, such as deep ice core drilling and clean [...] Read more.
The sampling and observation of subglacial lakes play a vital role in studying the physical and chemical properties as well as the microbial characteristics of water within these Antarctic subglacial lakes. Compared to existing techniques, such as deep ice core drilling and clean hot water drilling, recoverable autonomous sondes, inspired by the spinning and reeling silk behavior of spiders, offer several advantages, including lightweight design, low power consumption, and minimal external pollution. Over the past six years, Jilin University, with support from the Ministry of Science and Technology of China, has developed an environmentally friendly sampling and observation system for Antarctic subglacial lakes, utilizing a recoverable autonomous sonde. The whole system includes a melting sonde, detection and control unit, scientific load platform, and ice surface auxiliaries. Extensive laboratory and joint system tests were conducted, both on key components and the complete system, including field tests in ice lakes. The results of these tests validated the feasibility of the underlying principles, the long-term reliability of the system operation, and the cleanliness of the drilling process. Ice penetration speed up to 2.14 m/h was reached with 6~6.5 kW melting tip power and a 660 mL lake water sample was collected. The relevant design concepts and technologies of the system are expected to play an important role in the clean detection and sampling of subglacial lakes in Antarctica, Greenland, and other regions. Full article
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<p>(<b>a</b>) Schematic diagram of spiders’ behavior of ascending and descending through spinning and reeling silk; (<b>b</b>) Schematic diagram of RECAS sonde’s automatic process of drilling downward and climbing upward (modified from Talalay and others [<a href="#B14-water-17-00696" class="html-bibr">14</a>]).</p>
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<p>Concept of EFSOS system.</p>
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<p>Characteristics of the non-smooth body surface of the earthworm (modified from Zhang D. and others [<a href="#B21-water-17-00696" class="html-bibr">21</a>]) (<b>a</b>), the heating tube–water–ice contact interface (<b>b</b>), and the bionic structure of lateral heaters (<b>c</b>).</p>
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<p>Structural diagram of RECAS prototype.</p>
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<p>Schematic diagram of RECAS detection and control system.</p>
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<p>Structural diagram of RECAS scientific load platform.</p>
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<p>Structural diagram (<b>a</b>), working process (<b>b</b>), and photograph (<b>c</b>) of RECAS surface deployment system.</p>
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<p>RCUPS system: (<b>a</b>) 3D model; (<b>b</b>) top view of RCUPS system; (<b>c</b>) AGC controller in generator cabin; (<b>d</b>) two diesel generators; (<b>e</b>) high power UPS.</p>
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<p>Drilling testing in ice well: (<b>a</b>) RECAS sonde; (<b>b</b>) drilling downward in ice well; (<b>c</b>) drilling upward in transparent lake ice above the ice well.</p>
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<p>Temperature measurement of upper melting tip: (<b>a</b>) whole tip is in water; (<b>b</b>) half the tip is in air.</p>
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<p>Drilling testing in field lake: (<b>a</b>) layout of field lake testing; (<b>b</b>) drilling downward; (<b>c</b>) the lower part of RECAS sonde in the lake; (<b>d</b>) drilling upward; (<b>e</b>) inside view of control room; (<b>f</b>) collecting the water sample from the sampler.</p>
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<p>Variation of drilling parameters with depth during downward drilling of the second borehole.</p>
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17 pages, 5098 KiB  
Article
Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
by Jae N. Lee and Dong L. Wu
Remote Sens. 2025, 17(5), 835; https://doi.org/10.3390/rs17050835 - 27 Feb 2025
Viewed by 108
Abstract
This study investigates the impact of dynamic variability of the Southern Hemisphere (SH) polar middle atmosphere on the ozone hole area. We analyze the influence of the southern annular mode (SAM) and planetary waves (PWs) on ozone depletion from 19 years (2005–2023) of [...] Read more.
This study investigates the impact of dynamic variability of the Southern Hemisphere (SH) polar middle atmosphere on the ozone hole area. We analyze the influence of the southern annular mode (SAM) and planetary waves (PWs) on ozone depletion from 19 years (2005–2023) of aura microwave limb sounder (MLS) geopotential height (GPH) measurements. We employ empirical orthogonal function (EOF) analysis to decompose the GPH variability into distinct spatial patterns. EOF analysis reveals a strong relationship between the first EOF (representing the SAM) and the Antarctic ozone hole area (γ = 0.91). A significant negative lag correlation between the August principal component of the second EOF (PC2) and the September SAM index (γ = −0.76) suggests that lower stratospheric wave activity in August can precondition the polar vortex strength in September. The minor sudden stratospheric warming (SSW) event in 2019 is an example of how strong wave activity can disrupt the polar vortex, leading to significant temperature anomalies and reduced ozone depletion. The coupling of PWs is evident in the lag correlation analysis between different altitudes. A “bottom-up” propagation of PWs from the lower stratosphere to the mesosphere and a potential “top-down” influence from the mesosphere to the lower stratosphere are observed with time lags of 21–30 days. These findings highlight the complex dynamics of PW propagation and their potential impact on the SAM and ozone layer. Further analysis of these correlations could improve one-month lead predictions of the SAM and the ozone hole area. Full article
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<p>First three EOFs derived from MLS GPH during austral winter and spring months (MJJASON) at 10 hPa ((<b>a</b>) EOF1) and at 21.5 hPa ((<b>b</b>) EOF2 and (<b>c</b>) EOF3). Numbers in parentheses indicate the percentage of total variance explained by each mode.</p>
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<p>Time–height variations in the (<b>a</b>) SAM index, (<b>b</b>) PC2, and (<b>c</b>) PWA averaged over the period 2005–2023. The PCs and PWA are normalized by the standard deviation at each level for better comparison across altitudes. The PWA is presented in log scale to show the upper troposphere and the stratosphere at the same time. The black dotted lines indicate 10 hPa pressure level.</p>
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<p>(<b>a</b>) Variance (in %) of each mode of EOF patterns to the total variance at each pressure level. (<b>b</b>) Linear correlation between September SAM (at 10 hPa) and August PC2 index and September PWA (at 21.5 hPa).</p>
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<p>The latitude–height cross sections of the MLS GPH (m) across 90°W to 90°E during extreme positive and negative phases of the two leading principal components (PCs) for (<b>a</b>) low (negative), (<b>b</b>) high (positive) SAM phases at 10 hPa, (<b>c</b>) low and high SAM phases at 10 hPa, (<b>d</b>) low PC2 phases, (<b>e</b>) high PC2 phases at 21.5 hPa, and (<b>f</b>) low and high PC2 phases at 21 hPa. The GPH patterns for each phase represent an average of months with PC values exceeding (positive phase) or falling below (negative phase) one standard deviation from the 19-year mean monthly PC index.</p>
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<p>Similar to <a href="#remotesensing-17-00835-f004" class="html-fig">Figure 4</a>, but for the latitude–height cross sections of the MLS T (K) (<b>a</b>–<b>c</b>) and O<sub>3</sub> (ppmv) (<b>d</b>–<b>f</b>) for low and high SAM (PC1) index. The black dotted lines in temperature composites (<b>a</b>,<b>b</b>) indicate the location of the stratopause.</p>
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<p>Similar to <a href="#remotesensing-17-00835-f005" class="html-fig">Figure 5</a>, but for the low and high PC2 index at 21.5 hPa.</p>
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<p>Relationship between Antarctic ozone hole area and SAM. The left axis represents the average Antarctic ozone hole area in millions of square kilometers (10<sup>6</sup> km<sup>2</sup>), averaged from 7 September to 13 October. The right axis represents the September SAM index at 10 hPa (blue line), the negative of the August PC2 index at 21.5 hPa (red line), and scaled September PWA at 21.5 hPa. The PC2 index and PWA are inverted here for better visualization.</p>
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<p>Vertical profiles of the linear correlation between the September SAM index (blue line), August PC2 index (red line), September PWA (yellow line) and the Antarctic ozone hole area. For better visualization, PC2 and PAW correlations are plotted as their negative values (−1x<span class="html-italic">γ</span>).</p>
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<p>Evolution of zonal mean monthly (<b>a</b>) T (K) and (<b>b</b>) O<sub>3</sub> (ppmv) anomalies during May to November 2019 (with a base period 2005–2023).</p>
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<p>Daily PWAs during SSW2019 at two latitudes, (<b>a</b>) 70S and (<b>b</b>) 62S. PWA values are plotted on a logarithmic scale to visualize both the upper troposphere and the stratosphere. The x-axis shows time in days with 28 August 2019 (denoted as D) marked as the reference date for SSW2019 onset.</p>
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<p>Lag correlations between amplitudes of the PWs in higher latitudes (70S–82S) during the 30 days of the SSW2019 with those in lower latitudes (60S–72S). The x-axis represents the vertical levels of the PW amplitudes in lower latitude while the y-axis represents the PWAs in higher latitudes. White contour lines indicate 99% confidence level of the correlation. Two black crosses indicate the locations for the time series plots for <a href="#remotesensing-17-00835-f012" class="html-fig">Figure 12</a>.</p>
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<p>The 30 days average of the daily PWAs in two different latitude bands: higher latitudes (70S–82S) and lower latitudes (58S–70S) with −21 days lag.</p>
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20 pages, 8703 KiB  
Article
Atmospheric Variability and Sea-Ice Changes in the Southern Hemisphere
by Carlos Diego Gurjão, Luciano Ponzi Pezzi, Claudia Klose Parise, Flávio Barbosa Justino, Camila Bertoletti Carpenedo, Vanúcia Schumacher and Alcimoni Comin
Atmosphere 2025, 16(3), 284; https://doi.org/10.3390/atmos16030284 - 27 Feb 2025
Viewed by 298
Abstract
The Antarctic sea ice concentration (SIC) plays a crucial role in global climate dynamics by influencing atmospheric and oceanic circulation. This study examines SIC variability and its relationship with major climate modes, including the El Niño-Southern Oscillation (ENSO), Pacific-South American (PSA) pattern, Southern [...] Read more.
The Antarctic sea ice concentration (SIC) plays a crucial role in global climate dynamics by influencing atmospheric and oceanic circulation. This study examines SIC variability and its relationship with major climate modes, including the El Niño-Southern Oscillation (ENSO), Pacific-South American (PSA) pattern, Southern Annular Mode (SAM), and Antarctic Dipole (ADP). Using NSIDC satellite-derived sea ice data and ERA5 reanalysis from 1980 to 2022, we analyzed SIC anomalies in the Weddell, Ross, and Bellingshausen and Amundsen (B&A) Seas, assessing their response to climatic forcings across different timescales. Our findings reveal strong linkages between SIC variability and large-scale atmospheric circulation. ENSO-related teleconnections drive a dipolar SIC response, with warming in the Pacific sector and cooling in the Atlantic during El Niño, and the opposite pattern during La Niña. PSA and ADP further modulate this response by altering Rossby wave propagation and heat fluxes, leading to significant SIC fluctuations. The ADP emerges as a dominant driver of interannual SIC anomalies, showing an out-of-phase relationship between the Atlantic and Pacific sectors of the Southern Ocean. Regional SIC trends exhibit contrasting patterns: the Ross Sea shows a significant positive SIC trend, while the B&A and Weddell Seas experience persistent negative anomalies due to enhanced meridional heat transport and stronger westerly winds. SAM strongly influences SIC, particularly in the Atlantic sector, with delayed responses of up to six months, likely due to ice-albedo feedbacks and ocean memory effects. These results enhance our understanding of Antarctic sea ice variability and its sensitivity to large-scale climate oscillations. Given the observed trends and ongoing climate change, further research is needed to assess how these processes will evolve under future warming scenarios. This study highlights the importance of continuous satellite observations and high-resolution climate modeling for improving projections of Antarctic sea ice behavior and its implications for the global climate system. Full article
(This article belongs to the Section Climatology)
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<p>Selected areas to represent the sectors: Ross Sea (160° E–130° W, 60° S–70° S), B&amp;A Seas (130° W–70° W, 60° S–70° S), and Weddell Sea (60° W–10° W, 60° S–70° S).</p>
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<p>(<b>a</b>) Bar chart illustrates the seasonal variation in SIC in three different Antarctic regions: Amundsen and Bellingshausen (black), Weddell (gray), and Ross (blue). The <span class="html-italic">x</span>-axis represents the months of the year (J: January, F: February, etc.), while the <span class="html-italic">y</span>-axis shows SIC as a percentage. Climatology of the Antarctic sea ice concentration (SIC) (%) for summer (DJF) (<b>b</b>), autumn (MAM) (<b>c</b>), winter (JJA) (<b>d</b>), and spring (SON) (<b>e</b>). The SIC data comes from the National Snow and Ice Data Center - NSIDC between 1980 to 2022.</p>
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<p>The SIC trend data come from the NSIDC between 1980 to 2022 (left panels); (<b>a</b>) summer (DJF), (<b>b</b>) autumn (MAM), (<b>c</b>) winter (JJA) and (<b>d</b>) spring (SON). Seasonal climatology of <math display="inline"><semantics> <msub> <mi mathvariant="normal">T</mi> <mrow> <mi>T</mi> <mi>a</mi> <mi>i</mi> <mi>r</mi> </mrow> </msub> </semantics></math> trends (°C/decade) for the period of 1980–2022 based on ERA5 (right panels); (<b>e</b>) Summer (DJF), (<b>f</b>) Autumn (MAM), (<b>g</b>) Winter (JJA), and (<b>h</b>) Spring (SON). SIC trend in seasonal climatology means (%/decade). Black dotting represents the statistically significant values at the 95% confidence level.</p>
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<p>Seasonal correlation coefficients between SIC anomalies and the main climate variability modes: Niño<sub>3.4</sub>: (<b>a</b>–<b>d</b>); SAM: (<b>e</b>–<b>h</b>); PSA: (<b>i</b>–<b>l</b>); <math display="inline"><semantics> <msub> <mi>ADP</mi> <mrow> <mi>s</mi> <mi>i</mi> <mi>c</mi> </mrow> </msub> </semantics></math>: (<b>m</b>–<b>p</b>); and <math display="inline"><semantics> <msub> <mi>ADP</mi> <mrow> <mi>T</mi> <mi>a</mi> <mi>i</mi> <mi>r</mi> </mrow> </msub> </semantics></math>: (<b>q</b>–<b>t</b>). Black dotting represents the statistically significant values at the 95% confidence level.</p>
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<p>Lag correlation between main variability modes and Antarctic SIC anomalies over the Weddell, B&amp;A, and Ross Sea sectors: (<b>a</b>) Niño<sub>3.4</sub>, (<b>b</b>) SAM, (<b>c</b>) PSA, (<b>d</b>) <math display="inline"><semantics> <msub> <mi>ADP</mi> <mrow> <mi>S</mi> <mi>I</mi> <mi>C</mi> </mrow> </msub> </semantics></math>, and (<b>e</b>) <math display="inline"><semantics> <msub> <mi>ADP</mi> <mrow> <mi>T</mi> <mi>a</mi> <mi>i</mi> <mi>r</mi> </mrow> </msub> </semantics></math>.</p>
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<p>Seasonal composites of SIC (%) anomalies for seven neutral, El Niño, and La Niña events, representing the before and after of the maturation of ENSO, between 1980 and 2022. SON<sub>0</sub> (<b>a</b>–<b>c</b>), DJF<sub>0–1</sub> (<b>d</b>–<b>f</b>), MAM<sub>1</sub> (<b>g</b>–<b>i</b>), JJA<sub>1</sub> (<b>j</b>–<b>l</b>), and SON<sub>1</sub> (<b>m</b>–<b>o</b>).</p>
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<p>Same as <a href="#atmosphere-16-00284-f006" class="html-fig">Figure 6</a> but for seven neutral, SAM+, and SAM− phases representing the before and after of the maturation of SAM, between 1980 and 2022. SON<sub>0</sub> (<b>a</b>–<b>c</b>), DJF<sub>0–1</sub> (<b>d</b>–<b>f</b>), MAM<sub>1</sub> (<b>g</b>–<b>i</b>), JJA<sub>1</sub> (<b>j</b>–<b>l</b>), and SON<sub>1</sub> (<b>m</b>–<b>o</b>).</p>
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<p>Same as <a href="#atmosphere-16-00284-f006" class="html-fig">Figure 6</a> but for seven neutral, PSA+, and PSA− phases representing the before and after of the maturation of PSA, between 1980 and 2022. SON<sub>0</sub> (<b>a</b>–<b>c</b>), DJF<sub>0–1</sub> (<b>d</b>–<b>f</b>), MAM<sub>1</sub> (<b>g</b>–<b>i</b>), JJA<sub>1</sub> (<b>j</b>–<b>l</b>), and SON<sub>1</sub> (<b>m</b>–<b>o</b>).</p>
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18 pages, 2871 KiB  
Article
Unveiling the Mechanism of Action of Palmitic Acid, a Human Topoisomerase 1B Inhibitor from the Antarctic Sponge Artemisina plumosa
by Alessio Ottaviani, Davide Pietrafesa, Bini Chhetri Soren, Jagadish Babu Dasari, Stine S. H. Olsen, Beatrice Messina, Francesco Demofonti, Giulia Chicarella, Keli Agama, Yves Pommier, Blasco Morozzo della Rocca, Federico Iacovelli, Alice Romeo, Mattia Falconi, Bill J. Baker and Paola Fiorani
Int. J. Mol. Sci. 2025, 26(5), 2018; https://doi.org/10.3390/ijms26052018 - 26 Feb 2025
Viewed by 139
Abstract
Cancer remains a leading cause of death worldwide, highlighting the urgent need for novel and more effective treatments. Natural products, with their structural diversity, represent a valuable source for the discovery of anticancer compounds. In this study, we screened 750 Antarctic extracts to [...] Read more.
Cancer remains a leading cause of death worldwide, highlighting the urgent need for novel and more effective treatments. Natural products, with their structural diversity, represent a valuable source for the discovery of anticancer compounds. In this study, we screened 750 Antarctic extracts to identify potential inhibitors of human topoisomerase 1 (hTOP1), a key enzyme in DNA replication and repair, and a target of cancer therapies. Bioassay-guided fractionation led to the identification of palmitic acid (PA) as the active compound from the Antarctic sponge Artemisina plumosa, selectively inhibiting hTOP1. Our results demonstrate that PA irreversibly blocks hTOP1-mediated DNA relaxation and specifically inhibits the DNA religation step of the enzyme’s catalytic cycle. Unlike other fatty acids, PA exhibited unique specificity, which we confirmed through comparisons with linoleic acid. Molecular dynamics simulations and binding assays further suggest that PA interacts with hTOP1-DNA complexes, enhancing the inhibitory effect in the presence of camptothecin (CPT). These findings identify PA as a hTOP1 inhibitor with potential therapeutic implications, offering a distinct mechanism of action that could complement existing cancer therapies. Full article
(This article belongs to the Special Issue Discovering Novel Bioactive Compounds Against Cancers)
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<p>Relaxation of supercoiled DNA in presence of PA. (<b>A</b>) 2D structure representation of PA. (<b>B</b>) Relaxation of negative supercoiled DNA plasmid by hTOP1 at increasing PA concentrations (lanes 2–8), lane 1 DMSO and lane 9 with 200 μM PA and no protein added. (<b>C</b>) Relaxation of negative supercoiled DNA plasmid in a time course experiment with DMSO (lanes 1–6), with 100 µM PA (lanes 7–12), and 100 μM CPT (lanes 13–18); lanes 19 and 20 correspond to samples with 100 µM PA and 100 µM CPT, respectively, with no protein added. Reaction products were resolved on agarose gel and visualized with ethidium bromide (EtBr). DSC—dimer supercoiled DNA plasmid; MSC—monomer super-coiled DNA plasmid; C—negative control (corresponding to samples with 100 µM PA and 100 µM CPT, respectively, with no protein added).</p>
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<p>Analysis of religation of hTOP1 catalytic mechanism using FITC (fluorescein isothiocyanate) oligonucleotide labeled SS. (<b>A</b>) Top panel displays sequences of fluorescently FITC labeled SS used in religation assay, asterisk indicates that FITC was conjugated to guanine. (<b>B</b>) Representation of a denaturing polyacrylamide gel of the religation assay. Samples were incubated for 1 h at 25 °C followed by 30 min at 37 °C. Reaction was initiated by adding a 200-fold excess of R11 oligonucleotide, either with or without 100 µM PA, then stopped at various time points with 0.5% SDS. CL1 represents cleaved strand (TOP1cc), C is negative control (no protein added), and 0 denotes TOP1cc starting condition before addition of R11. (<b>C</b>) Plot illustrates percentage of religated bands over time from religation assay. Figure presents cumulative data with mean ± SD from three independent experiments. Statistical significance is indicated with asterisks: *** <span class="html-italic">p</span> ≤ 0.001.</p>
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<p>hTOP1–DNA cleavage complex reversal assay. (<b>A</b>) Top panel displays sequences of fluorescently labeled SS used in the assay. (<b>B</b>) Polyacrylamide gel reporting kinetics of formation of PA and CPT induced hTOP1-mediated DNA cleavage complexes. 3′-6-FAM end labeled 48 bp oligonucleotide was reacted with hTOP1 in presence or absence of 1 µM CPT, 10 µM PA, or both at 25 °C for 20 min. DNA cleavage was reversed by adding 0.35 M NaCl and monitored over time. (<b>C</b>) Graph reporting 35 bp band quantification as function of time for PA and CPT (blue line), CPT (red line), PA (black line), and hTOP1 (green line) as control. Samples are represented as mean value ± SD. * <span class="html-italic">p</span> &lt; 0.05 *** <span class="html-italic">p</span> &lt; 0.001.</p>
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<p>Pre-incubation dose-dependent relaxation assay. Relaxation of negative supercoiled plasmid DNA in a dose-dependent experiment with DMSO (lane 1), 150 μM and 200 μM PA in pre-incubation condition, indicated as PRE (lanes 2–3), and 150 μM and 200 μM PA in simultaneous condition, indicated as SIM (lane 4–5), with no protein added in lane 6. Reaction products are resolved on agarose gel and visualized with EtBr. C indicates negative control.</p>
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<p>Essential motions of MD simulations. (<b>A</b>) Representation of two extreme projections of motions described by first eigenvector (PC1), interpolated onto 3D structures of hTOP1-DNA (left), hTOP1-DNA-CPT (center) and hTOP1-DNA-CPT-PAs (right) systems. Direction and amplitude of the internal motions are shown as color shift from blue to red and width of ribbons, respectively. (<b>B</b>) 2D projections of first (PC1) and second (PC2) eigenvectors of hTOP1-DNA (left), hTOP1DNA-CPT (center) and hTOP1-DNA-CPT-PAs (right) systems. Color coding shows progression from starting (violet) to final (yellow) stages of the simulations.</p>
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<p>MD of PA-DNA systems. Representative snapshots for first replica are shown at 0 ns, 75 ns, 125 ns, and 250 ns. For each figure, DNA is shown using a cyan surface representation, while PA molecules are shown in Van der Waals representation.</p>
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19 pages, 5600 KiB  
Article
Antarctic Sea Ice Extraction for Remote Sensing Images via Modified U-Net Based on Feature Enhancement Driven by Graph Convolution Network
by Wu Feng, Xiulin Geng, Xiaoyu He, Miao Hu, Jie Luo and Meihua Bi
J. Mar. Sci. Eng. 2025, 13(3), 439; https://doi.org/10.3390/jmse13030439 - 25 Feb 2025
Viewed by 352
Abstract
Antarctic true-color imagery synthesized using multispectral remote sensing data is effective in reflecting sea ice conditions, which is crucial for monitoring. Deep learning has been explored for sea ice extraction, but traditional convolutional neural network models are constrained by a limited perceptual field, [...] Read more.
Antarctic true-color imagery synthesized using multispectral remote sensing data is effective in reflecting sea ice conditions, which is crucial for monitoring. Deep learning has been explored for sea ice extraction, but traditional convolutional neural network models are constrained by a limited perceptual field, making it difficult to obtain global contextual information from remote sensing images. A novel model named GEFU-Net, a modification of U-Net, is presented. The self-established graph reconstruction module is employed to convert features into graph data and construct the adjacency matrix using a global adaptive average similarity threshold. Graph convolutional networks are utilized to aggregate the features at each pixel, enabling the rapid capture of global context, enhancing the semantic richness of the features, and improving the accuracy of sea ice extraction through graph reconstruction. Experimental results using the sea ice dataset of the Ross Sea in the Antarctic, produced by Sentinel-2, demonstrate that our GEFU-Net achieves the best performance compared to other commonly used segmentation models. Specifically, it achieves an accuracy of 97.52%, an Intersection over Union of 95.66%, and an F1-Score of 97.78%. Additionally, fewer model parameters and good inference speed are demonstrated, indicating strong potential for practical ice mapping applications. Full article
(This article belongs to the Section Physical Oceanography)
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<p>The area of interest for this study. (<b>a</b>) The red rectangles represent specific geographic areas. (<b>b</b>) The specific location of each scene.</p>
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<p>A schematic diagram of the Sentinel-2 data preprocessing.</p>
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<p>A schematic diagram of the sea ice annotation.</p>
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<p>A flowchart of sea ice extraction using Sentinel-2 data in our scheme.</p>
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<p>The overall structure of the proposed GEFU-Net.</p>
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<p>A schematic diagram of the encoder, consisting of ResBlocks and ConvBlocks.</p>
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<p>Different down-sampling operations in the residual branch. (<b>a</b>) Convolution, (<b>b</b>) average pool.</p>
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<p>A schematic diagram of the decoder, consisting of UpsampleBlocks.</p>
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<p>A schematic diagram of the SEGR module.</p>
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<p>Sea ice extraction results from different models. (<b>a</b>) TCI, (<b>b</b>) ground truth, (<b>c</b>) SegNet, (<b>d</b>) PSPNet, (<b>e</b>) DeepLab, (<b>f</b>) U-Net, (<b>g</b>) TransU-Net, (<b>h</b>) ABU-Net, (<b>i</b>) GEFU-Net.</p>
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<p>Comparison of different adjacency matrix generation methods. (<b>a</b>) Euclidean distance. (<b>b</b>) Manhattan distance.</p>
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<p>Effect of GCN layers in SEGR module on extraction results.</p>
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<p>GEFU-Net applied for automatic ice mapping using Sentinel-2 data. (<b>a</b>) Flowchart of ice mapping. (<b>b</b>) Ice mapping results—dark blue for open water, light blue for sea ice.</p>
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<p>Parameter size and inference time of different models.</p>
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22 pages, 1907 KiB  
Article
Lipid Production in Cultivable Filamentous Fungi Isolated from Antarctic Soils: A Comprehensive Study
by Victor Gallardo, Jéssica Costa, Marcela Sepúlveda, Yasna Cayún, Christian Santander, Excequel Ponce, Juliana Bittencourt, César Arriagada, Javiera Soto, Romina Pedreschi, Vania Aparecida Vicente, Pablo Cornejo and Cledir Santos
Microorganisms 2025, 13(3), 504; https://doi.org/10.3390/microorganisms13030504 - 25 Feb 2025
Viewed by 242
Abstract
Antarctic soil represents an important reservoir of filamentous fungi (FF) species with the ability to produce novel bioactive lipids. However, the lipid extraction method is still a bottleneck. The objective of the present work was to isolate and identify cultivable FF from Antarctic [...] Read more.
Antarctic soil represents an important reservoir of filamentous fungi (FF) species with the ability to produce novel bioactive lipids. However, the lipid extraction method is still a bottleneck. The objective of the present work was to isolate and identify cultivable FF from Antarctic soils, to assess the most effective methods for fatty acid (FA) extraction, and to characterise the obtained lipids. A total of 18 fungal strains belonging to the Botrytis, Cladosporium, Cylindrobasidium, Mortierella, Penicillium, Pseudogymnoascus, and Talaromyces genera and the Melanommataceae family were isolated and identified. The Folch, Bligh and Dyer, and Lewis extraction methods were assessed, and methyl esters of FA (FAMEs) were obtained. The Lewis method was the best in recovering FAMEs from fungal biomass. A total of 17 FAs were identified, and their chemical compositions varied depending on fungal species and strain. Oleic, linoleic, stearic, and palmitic acids were predominant for all fungal strains in the three assessed methods. Among the analysed strains, Cylindrobasidium eucalypti, Penicillium miczynskii, P. virgatum, and Pseudogymnoascus pannorum produced high amounts of FA. This suggests that the soils of Antarctica Bay, as well as harbouring known oleaginous fungi, are also an important source of oleaginous filamentous fungi that remain poorly analysed. Full article
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<p>Map of Fildes Bay with the geographic distribution of sampling points used in the present study. Adapted from Gallardo et al. [<a href="#B3-microorganisms-13-00504" class="html-bibr">3</a>].</p>
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<p>Infrared spectra for fungal biomass. (<b>A</b>) <span class="html-italic">Botrytis cinerea</span> (UFRO22.262); (<b>B</b>) <span class="html-italic">C. herbarum</span> (UFRO22.551); (<b>C</b>) <span class="html-italic">M. truficola</span> (UFRO22.261); (<b>D</b>) <span class="html-italic">M. globulifera</span> (UFRO22.317); (<b>E</b>) <span class="html-italic">P. pannorum</span> (UFRO22.138); (<b>F</b>) Melanommataceae family (UFRO22.418) before (black line) and after extraction with the Lewis (green line), Bligh and Dyer (blue line), and Folch (red line) methods. The control (biomass before extraction) is presented for each strain.</p>
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<p>Heat maps of fatty acids from Antarctic fungi according to the performance obtained with the Bligh and Dyer (<b>A</b>), Folch (<b>B</b>), and Lewis (<b>C</b>) methods. The left dendrograms group Antarctic fungi according to similarities of their fatty acid profiles, while the top dendrograms group fatty acids according to their yields. The colour gradient in each heat map varies from darkest (high yield) to lightest (trace yield).</p>
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11 pages, 1028 KiB  
Communication
Molecular Detection of blaTEM and blaSHV Genes in ESBL-Producing Acinetobacter baumannii Isolated from Antarctic Soil
by Clara Pazos, Miguel Gualoto, Tania Oña, Elizabeth Velarde, Karen Portilla, Santiago Cabrera-García, Carlos Banchón, Gabriela Dávila, Fernanda Hernández-Alomia and Carlos Bastidas-Caldes
Microorganisms 2025, 13(3), 482; https://doi.org/10.3390/microorganisms13030482 - 21 Feb 2025
Viewed by 512
Abstract
The phenomenon of antimicrobial resistance (AMR) in cold environments, exemplified by the Antarctic, calls into question the assumption that pristine ecosystems lack clinically significant resistance genes. This study examines the molecular basis of AMR in Acinetobacter spp. Isolated from Antarctic soil, focusing on [...] Read more.
The phenomenon of antimicrobial resistance (AMR) in cold environments, exemplified by the Antarctic, calls into question the assumption that pristine ecosystems lack clinically significant resistance genes. This study examines the molecular basis of AMR in Acinetobacter spp. Isolated from Antarctic soil, focusing on the blaTEM and blaSHV genes associated with extended-spectrum beta-lactamase (ESBL) production; Soil samples were collected and processed to isolate Antarctic soil bacteria. Molecular detection was then conducted using polymerase chain reaction (PCR) to identify the bacteria species by 16S rRNA/rpoB and 10 different beta-lactamase-producing genes. PCR amplicons were sequenced to confirm gene identity and analyze genetic variability. Acinetobacter baumannii were identified by both microbiological and molecular tests. Notably, both the blaTEM and blaSHV genes encoding the enzymes responsible for resistance to penicillins and cephalosporins were identified, indicating the presence of resistance determinants in bacteria from extreme cold ecosystems. The nucleotide sequence analysis indicated the presence of conserved ARGs, which suggest stability and the potential for horizontal gene transfer within microbial communities. These findings emphasize that AMR is not confined to human-impacted environments but can emerge and persist in remote, cold habitats, potentially facilitated by natural reservoirs and global microbial dispersal. Understanding the presence and role of AMR in extreme environments provides insights into its global dissemination and supports the development of strategies to mitigate the spread of resistance genes in both environmental and clinical contexts. Full article
(This article belongs to the Special Issue Antibiotic and Resistance Gene Pollution in the Environment)
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<p>Location of the Ecuadorian scientific station Pedro Vicente Maldonado on Greenwich Island, Antarctica. (<b>A</b>) The geographic context of the Antarctic Peninsula highlights in red the location of Greenwich Island, which corresponds to the sampling site. (<b>B</b>) Station equipment and a close-up view showcasing the environmental conditions characteristic of the polar region. (<b>C</b>) Soil sampling conducted by the Ecuadorian scientific team near the station. The main map displays the precise location of the station on Greenwich Island, projected in the EPSG 3031 system (Antarctic Polar Stereographic).</p>
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<p>Concatenated (<span class="html-italic">rpoB</span>-16SrRNA) phylogenetic tree construction using the maximum likelihood method using the GTR + G + I model in NGPhylogeny software with 500 bootstraps. The bootstrap value is presented in the tree nodes.</p>
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39 pages, 4035 KiB  
Article
Feedback Trends with ECS from Energy Rates: Feedback Doubling and the Vital Need for Solar Geoengineering
by Alec Feinberg
Climate 2025, 13(3), 43; https://doi.org/10.3390/cli13030043 - 21 Feb 2025
Viewed by 350
Abstract
This paper provides climate feedback trends, quantifies the feedback-doubling (FD) period, considers urbanization influences, and provides related equilibrium climate sensitivity (ECS) estimates using data from 1880 to 2024. Data modeling is accomplished by focusing on statistically significant stable normalized correlated rates (NCRs, i.e., [...] Read more.
This paper provides climate feedback trends, quantifies the feedback-doubling (FD) period, considers urbanization influences, and provides related equilibrium climate sensitivity (ECS) estimates using data from 1880 to 2024. Data modeling is accomplished by focusing on statistically significant stable normalized correlated rates (NCRs, i.e., normalized related slopes). Estimates indicate that the global warming NCR is increasing by a factor of 1.65 to 2.33 times faster than the energy consumption NCR, from 1975 to 2024. The reason is feedback amplification. This is supported by the fact that the NCR for forcing and energy consumption shows approximate equivalency in the period studied. Results provide feedback yearly trend estimates at the 95% confidence level that key results will fall within the IPCC AR6 likely range. The projected 2017–2024 feedback amplification estimates, using the EC approach, range from 2.0 to 2.16, respectively. A feedback amplification of 2.0 (approximately equal to −2.74 Wm−2 K−1) doubles the forcing, indicating that in 2024, more than half of global warming (53.7%) is likely due to feedback. Relative to the feedback-doubling (FD) threshold (i.e., the point where feedback exceeds forcing), the FD overage is 3.7% in 2024. This is the amount of feedback exceeding the forcing portion found to have a surprisingly aggressive 3.1% to 3.9% estimated overage growth rate per decade. We now ask, shouldn’t we try to mitigate feedback as well as GHG forcing, and if forcing could be removed, would global warming fully “self-mitigate”? Additionally, CO2 yearly increases are complex, with poor reduction progress. Therefore, this study’s risk assessment urgently recommends that supplementary “mild” annual solar geoengineering is necessary, to reduce the dominant aggressive feedback. SG reduces the primary solar warming source creating 62% higher mitigation efficiency than CDR. Urgency is enhanced since solar geoengineering must be timely and can take years to develop. This study also estimates that 75% to 90.5% (83% average) of the feedback problem is due to water vapor feedback (WVF). High WVF also plagues many cities needing local SG. Trend analysis indicates that by 2047, the earliest we may reach 10 billion people, feedback amplification could reach a value of 2.4 to 2.8. Furthermore, by 2082, the year estimated for 2× CO2, at the current rate, feedback amplification could range from 2.88 to 3.71. This yields an ECS range from 2.4 °C to 3.07 °C, in reasonable agreement with the reported estimated range in AR6. An overview of recent urbanization forcing attribution indicates the ECS value may be lower by 10.7% if this forcing is considered. For numerous reasons, the lack of albedo urbanization Earth brightening requirements in the Paris Agreement, is unsettling. In addition, a model assesses effective forced feedback (EFF) temperature characteristics of up to 1.9 °C, providing interesting feedback insights that may relate to high GW land and pipeline temperature estimates. Lastly in addition to urbanization, solar geoengineering in the Arctic and Antarctic is advised. Worldwide efforts in GHG mitigation, with no significant work in SG, appears highly misdirected. Full article
(This article belongs to the Collection Adaptation and Mitigation Practices and Frameworks)
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Graphical abstract

Graphical abstract
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<p>(<b>a</b>) Feedback amplification trends, (<b>b</b>) 2024 feedback and forcing GW estimates.</p>
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<p>Topline, global EC [<a href="#B28-climate-13-00043" class="html-bibr">28</a>], and bottom line GW [<a href="#B30-climate-13-00043" class="html-bibr">30</a>] (see <a href="#app1-climate-13-00043" class="html-app">Appendix A</a>). The equations shown are for the linear trend lines.</p>
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<p>Topline, population growth [<a href="#B31-climate-13-00043" class="html-bibr">31</a>] (see <a href="#app1-climate-13-00043" class="html-app">Appendix A</a>), and bottom line, global warming [<a href="#B30-climate-13-00043" class="html-bibr">30</a>] (see <a href="#app1-climate-13-00043" class="html-app">Appendix A</a>). The equations shown are for the linear trend lines.</p>
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<p>(<b>a</b>) IPCC AR6 (Ch. 7) [<a href="#B32-climate-13-00043" class="html-bibr">32</a>] forcing estimates for 2011 and 2019, (<b>b</b>) normalized forcing showing a rate of 0.0127 per year.</p>
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<p>Topline, normalized population growth (<a href="#app1-climate-13-00043" class="html-app">Appendix A</a>), and bottom line, global warming (<a href="#app1-climate-13-00043" class="html-app">Appendix A</a>). The equations shown are for the linear trend lines.</p>
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<p>(<b>a</b>) Topline, normalized energy consumption increase, and bottom line, global warming (<a href="#app1-climate-13-00043" class="html-app">Appendix A</a>). The equations shown are correlated slopes with linear trend lines from 1975 to 2021. (<b>b</b>) Normalized global warming with correction estimates from 1880 to 2021.</p>
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<p>Topline, normalized global warming increase, and bottom line, normalized CO<sub>2</sub> increase. The equations shown are correlated slopes with linear trend lines from 1975 to 2021.</p>
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<p>Feedback amplification trend analysis (<a href="#climate-13-00043-t002" class="html-table">Table 2</a>) assessed using NCR methods: (<b>a</b>) 1975–2019 data–linear fit (<b>b</b>) 2000–2019 data plus 2025 Hansen et al. [<a href="#B34-climate-13-00043" class="html-bibr">34</a>] point–linear fit (<b>c</b>) 1870–2082 Exponential fit with added unity and 2× CO<sub>2</sub> point from linear fit (<b>d</b>) 1940–2082 Exponential fit with added unity, plus Hansen et al. [<a href="#B34-climate-13-00043" class="html-bibr">34</a>] point and 2× CO<sub>2</sub> estimate from linear fit.</p>
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<p>Linear fit to recent yearly CO<sub>2</sub> ppm increases.</p>
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<p>Global warming components with the urbanization contribution.</p>
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<p>Feedback rates for EFF temperature above global ambient.</p>
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<p>Stratospheric water vapor mixing ratios from 1980 to 2024 [<a href="#B49-climate-13-00043" class="html-bibr">49</a>], with black estimated average trend lines, a normalized axis on the right side, and NCR equations on top.</p>
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<p>Tropospheric normalized water vapor (weighted land and ocean) content increases with the NCR equation extrapolated from Patel et al. [<a href="#B45-climate-13-00043" class="html-bibr">45</a>].</p>
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<p>Recent trends in GW. Fluctuations appear to have followed El Niño and La Niña cycles.</p>
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15 pages, 2854 KiB  
Article
Antarctic Soil and Viable Microbiota After Long-Term Storage at Constant −20 °C
by Cristian-Emilian Pop, Sergiu Fendrihan, Nicolai Crăciun, Garbis Vasilighean, Daniela Ecaterina Chifor, Florica Topârceanu, Andreea Florea, Dan Florin Mihăilescu and Maria Mernea
Biology 2025, 14(3), 222; https://doi.org/10.3390/biology14030222 - 20 Feb 2025
Viewed by 330
Abstract
During an Antarctic expedition that took place in December 2010–January 2011 in the East Antarctic coastal region, soil samples were collected in aseptic conditions and stored for over a decade in freezers at −20 °C. Due to the shortly afterward passing of the [...] Read more.
During an Antarctic expedition that took place in December 2010–January 2011 in the East Antarctic coastal region, soil samples were collected in aseptic conditions and stored for over a decade in freezers at −20 °C. Due to the shortly afterward passing of the Antarctic researcher in charge, Teodor Negoiță, the samples remained unintentionally frozen for a long period and were made available for research 13 years later. A chemical analysis of soil as well as screening for viable microbial presence was performed; soil analysis was conducted via inductively coupled plasma atomic emission spectroscopy (ICP-AES) and Fourier-transform infrared spectroscopy coupled with attenuated total reflection (FTIR-ATR). The presence of aerobic and facultative aerobic microbiotas was evaluated through a Biolog Ecoplates assay, and isolated strains were 16S sequenced for final taxonomic identification. The results obtained new insights into Antarctic soil characteristics from both chemical and microbiological aspects, even after over a decade of conservation. Full article
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<p>(<b>a</b>) Hierarchical clustering dendrogram of spectra calculated based on pairwise Euclidean distances. (<b>b</b>) ATR-FTIR spectra of samples 1–4. (<b>c</b>) ATR-FTIR spectra of samples 5–7. (<b>d</b>) ATR-FTIR spectra of samples 8–10.</p>
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<p>The lower half of high positive and negative correlations (the module of the correlation value is larger than or equal to 0.7) between the concentrations of elements in each station. The high positive correlations are represented in shades of red, while the high negative correlations are represented in shades of blue. Locations are identified based on their coordinates: Camp Faraglione—top plot; Edmonson Point—middle plot; Apostrophe Island—bottom plot.</p>
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<p>Lower half of the correlation matrix of element concentrations in samples from all collection points. The color scale used shows the maximum positive correlations (value of 1) in red and the maximum negative correlations (value of −1) in blue.</p>
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<p>Average metabolic response for Biolog Ecoplates.</p>
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26 pages, 7006 KiB  
Article
Relation Between Major Climatic Indices and Subseasonal Precipitation in Rio Grande do Sul State, Brazil
by Angela Maria de Arruda, Luana Nunes Centeno and André Becker Nunes
Meteorology 2025, 4(1), 5; https://doi.org/10.3390/meteorology4010005 - 19 Feb 2025
Viewed by 96
Abstract
This study analyzed the correlation between climate indices—El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (ISSTRG2 + RG3), South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)—and precipitation in [...] Read more.
This study analyzed the correlation between climate indices—El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (ISSTRG2 + RG3), South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)—and precipitation in Rio Grande do Sul (RS) during 45-day subseasonal periods from 2006 to 2022. Precipitation data from 670 rain gauges were categorized into three clusters: cluster 1, located in western RS, displayed the lowest precipitation variation; cluster 2, in eastern RS, exhibited the greatest variability; and cluster 3, situated in northern RS. ENSO demonstrated the strongest positive correlation with precipitation during spring in clusters 1 and 3 (0.65–0.79), while PDO also correlated positively, especially in summer and spring. AOC exhibited negative correlations, most pronounced in spring. Significant inter-index correlations were identified, including a high positive correlation between SASH and AOC (0.7) and a high negative correlation between NINO34 and SOI (−0.73). Within clusters, NINO34 and PDO showed low positive correlations with precipitation (0.24–0.32), while SOI demonstrated low negative correlations (−0.21 to −0.30). Seasonal analysis revealed that NINO34 influenced summer and spring precipitation, correlating with above-average rainfall during El Niño events. SASH and PDO also showed positive correlations with summer and spring rainfall, with PDO’s positive phase associated with a 25% increase in precipitation. These findings provide valuable insights into the complex interactions between global climatic indices and regional precipitation patterns, enhancing the understanding of subseasonal climate variability in RS and supporting the development of more accurate climate prediction models for the region. Full article
(This article belongs to the Special Issue Early Career Scientists' (ECS) Contributions to Meteorology (2024))
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<p>Map of the location of the teleconnections addressed at the beginning of the study (1 January 2006). Red: positive phase; blue: negative phase. Source: [<a href="#B12-meteorology-04-00005" class="html-bibr">12</a>,<a href="#B13-meteorology-04-00005" class="html-bibr">13</a>].</p>
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<p>Distribution of the rain gauges consulted in RS. Source: [<a href="#B47-meteorology-04-00005" class="html-bibr">47</a>,<a href="#B48-meteorology-04-00005" class="html-bibr">48</a>].</p>
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<p>Verification of precipitation data homogeneity from rain gauges using the Mann–Kendall test.</p>
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<p>(<b>a</b>) Graph shows a gradual decrease starting from k = 3. (<b>b</b>) Spatial distribution of clusters in RS (red-cluster1; blue-cluster2 and purple-cluster3). (<b>c</b>) Visualization of the k-means cluster graph.</p>
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<p>(<b>a</b>) Graph shows a gradual decrease starting from k = 3. (<b>b</b>) Spatial distribution of clusters in RS (red-cluster1; blue-cluster2 and purple-cluster3). (<b>c</b>) Visualization of the k-means cluster graph.</p>
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<p>Descriptive statistics of the indices and precipitation (El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (SST23, South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)).</p>
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<p>Scatter matrix.</p>
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<p>Variation in climate indices (<b>a</b>) NINO34, (<b>b</b>) AOC, (<b>c</b>) SST23, (<b>d</b>) SASH, (<b>e</b>) SOI, (<b>f</b>) PDO, and (<b>g</b>) MJO. Blue and red bars represent La Niña and El Niño and (respectively). Source: Adapted from [<a href="#B13-meteorology-04-00005" class="html-bibr">13</a>].</p>
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<p>Variation in climate indices (<b>a</b>) NINO34, (<b>b</b>) AOC, (<b>c</b>) SST23, (<b>d</b>) SASH, (<b>e</b>) SOI, (<b>f</b>) PDO, and (<b>g</b>) MJO. Blue and red bars represent La Niña and El Niño and (respectively). Source: Adapted from [<a href="#B13-meteorology-04-00005" class="html-bibr">13</a>].</p>
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<p>Variation in climate indices (<b>a</b>) NINO34, (<b>b</b>) AOC, (<b>c</b>) SST23, (<b>d</b>) SASH, (<b>e</b>) SOI, (<b>f</b>) PDO, and (<b>g</b>) MJO. Blue and red bars represent La Niña and El Niño and (respectively). Source: Adapted from [<a href="#B13-meteorology-04-00005" class="html-bibr">13</a>].</p>
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<p>MJO index restricted to the phases with the greatest influence in RS. Blue and red bars represent El Niño and La Niña, respectively. Source: Adapted from [<a href="#B13-meteorology-04-00005" class="html-bibr">13</a>].</p>
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<p>Effect of the combination of El Niño/La Niña with negative and positive AOC phases, respectively, on the average precipitation in Rio Grande do Sul for 45-day periods.</p>
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<p>(<b>a</b>) Correlation between the indices and cluster averages (blue—positive; red—negative). (<b>b</b>) Highlight of the most significant correlations.</p>
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<p>Scatter matrix of indices and average precipitation for 45-day periods.</p>
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<p>Boxplot of data restricted to El Niño and La Niña events (El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (SST23), South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)).</p>
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<p>(<b>a</b>) Scatter matrix of the indices and average precipitation for 45-day periods, during El Niño and La Niña events. (<b>b</b>) Scatter matrix of the indices and average precipitation for 45-day periods.</p>
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<p>(<b>a</b>) Scatter matrix of the indices and average precipitation for 45-day periods, during El Niño and La Niña events. (<b>b</b>) Scatter matrix of the indices and average precipitation for 45-day periods.</p>
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<p>(<b>a</b>) Summer, (<b>b</b>) spring, (<b>c</b>) winter, (<b>d</b>) autumn; (El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (SST23), South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)).</p>
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<p>(<b>a</b>) Summer, (<b>b</b>) spring, (<b>c</b>) winter, (<b>d</b>) autumn; (El Niño–Southern Oscillation (NINO34), Southern Oscillation Index (SOI), Antarctic Oscillation (AOC), Sea Surface Temperature in the southwestern Atlantic (SST23), South Atlantic Subtropical High (SASH), Pacific Decadal Oscillation (PDO), and Madden–Julian Oscillation (MJO)).</p>
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<p>Correlation between the indices and the average values of the clusters divided by seasons: (<b>a</b>) summer, (<b>b</b>) spring, (<b>c</b>) winter, (<b>d</b>) autumn.</p>
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<p>Correlation between the indices and the average values of the clusters divided by seasons: (<b>a</b>) summer, (<b>b</b>) spring, (<b>c</b>) winter, (<b>d</b>) autumn.</p>
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<p>Classification of correlations between indices and precipitation cluster 1, 2, and 3.</p>
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