TY - JOUR A1 - Cesar Fernández, Guillermo A1 - Lecomte, Karina A1 - Vignoni, Paula A1 - Soto-Rueda, Eliana Marcela A1 - Coria, Silvia H. A1 - Lirio, Juan Manuel A1 - Mlewski, Estela Cecilia T1 - Prokaryotic diversity and biogeochemical characteristics of benthic microbial ecosystems from James Ross Archipelago (West Antarctica) JF - Polar biology : current research and development in science and technology N2 - The James Ross archipelago houses numerous lakes and ponds. In this region, a vast diatom and cyanobacterial variety has been reported; however, the prokaryotic diversity in microbial mats from these lakes remains poorly explored. Here, a high-throughput sequencing of 16S rRNA gene in microbial mats from Lake Bart-Roja in James Ross Island and lakes Pan Negro and North Pan Negro located in Vega Island was performed. Combined with mineralogical and environmental characteristics, we analyzed the diversity and structure of the microbial communities. Sequences assigned to Archaea were extremely low, while Bacteria domain prevailed with the abundance of Proteobacteria (mostly Betaproteobacteriales) followed by Bacteroidetes, Verrucomicrobia, Firmicutes, and Cyanobacteria. Local environmental conditions, such as conductivity and Eh, provided differential microbial assemblages that might have implications in the oligotrophic status of the lakes. Consequently, a clear segregation at the family level was observed. In this sense, the assigned diversity was related to taxa recognized as denitrifiers and sulfur oxidizers. Particularly, in Lake Pan Negro sulfur-reducing and methanogenic representatives were also found and positively correlate with alkalinity and water depth. Moreover, Deinococcus-Thermus was observed in Lake Bart-Roja, while Melainabacteria (Cyanobacteria)-poorly reported in Antarctic mats-was detected in Lake Pan Negro. Epsilonbacteraeota was exclusively found in this lake, suggesting new potential phylotypes. This study contributes to the understanding of the diversity, composition, and structure of Antarctic benthic microbial ecosystems and provides highly valuable information, which can be used as a proxy to evaluate environmental changes affecting Antarctic microbiota. KW - Antarctica KW - microbial mats KW - microbial diversity KW - 16S rRNA genes KW - James Ross archipelago Y1 - 2022 U6 - https://doi.org/10.1007/s00300-021-02997-z SN - 0722-4060 SN - 1432-2056 VL - 45 IS - 3 SP - 405 EP - 418 PB - Springer CY - Berlin ; Heidelberg ER - TY - JOUR A1 - Ilicic, Doris A1 - Woodhouse, Jason A1 - Karsten, Ulf A1 - Zimmermann, Jonas A1 - Wichard, Thomas A1 - Quartino, Maria Liliana A1 - Campana, Gabriela Laura A1 - Livenets, Alexandra A1 - Van den Wyngaert, Silke A1 - Grossart, Hans-Peter T1 - Antarctic Glacial Meltwater Impacts the Diversity of Fungal Parasites Associated With Benthic Diatoms in Shallow Coastal Zones JF - Frontiers in microbiology N2 - Aquatic ecosystems are frequently overlooked as fungal habitats, although there is increasing evidence that their diversity and ecological importance are greater than previously considered. Aquatic fungi are critical and abundant components of nutrient cycling and food web dynamics, e.g., exerting top-down control on phytoplankton communities and forming symbioses with many marine microorganisms. However, their relevance for microphytobenthic communities is almost unexplored. In the light of global warming, polar regions face extreme changes in abiotic factors with a severe impact on biodiversity and ecosystem functioning. Therefore, this study aimed to describe, for the first time, fungal diversity in Antarctic benthic habitats along the salinity gradient and to determine the co-occurrence of fungal parasites with their algal hosts, which were dominated by benthic diatoms. Our results reveal that Ascomycota and Chytridiomycota are the most abundant fungal taxa in these habitats. We show that also in Antarctic waters, salinity has a major impact on shaping not just fungal but rather the whole eukaryotic community composition, with a diversity of aquatic fungi increasing as salinity decreases. Moreover, we determined correlations between putative fungal parasites and potential benthic diatom hosts, highlighting the need for further systematic analysis of fungal diversity along with studies on taxonomy and ecological roles of Chytridiomycota. KW - Antarctica KW - aquatic fungi KW - Chytridiomycota KW - phytoplankton host KW - salinity gradient KW - Illumina amplicon sequencing KW - Carlini Station Y1 - 2022 U6 - https://doi.org/10.3389/fmicb.2022.805694 SN - 1664-302X IS - 13 PB - Frontiers Media CY - Lausanne ER - TY - JOUR A1 - Ferrero, Silvio A1 - Godard, Gaston A1 - Palmeri, Rosaria A1 - Wunder, Bernd A1 - Cesare, Bernardo T1 - Partial melting of ultramafic granulites from Dronning Maud Land, Antarctica BT - constraints from melt inclusions and thermodynamic modeling JF - American mineralogist : an international journal of earth and planetary materials N2 - In the Pan-African belt of the Dronning Maud Land, Antarctica, crystallized melt inclusions (nanogranitoids) occur in garnet from ultramafic granulites. The granulites contain the peak assemblage pargasite+garnet+clinopyroxene with rare relict orthopyroxene and biotite, and retrograde symplectites at contacts between garnet and amphibole. Garnet contains two generations of melt inclusions. Type 1 inclusions, interpreted as primary, are isolated, < 10 mu m in size, and generally have negative crystal shapes. They contain kokchetavite, kumdykolite, and phlogopite, with quartz and zoisite as minor phases, and undevitrified glass was identified in one inclusion. Type 2 inclusions are < 30 mu m in size, secondary, and contain amphibole, feldspars, and zoisite. Type 2 inclusions appear to be the crystallization products of a melt that coexisted with an immiscible CO2-rich fluid. The nanogranitoids were re-homogenized after heating in a piston-cylinder in a series of four experiments to investigate their composition. The conditions ranged between 900 and 950 degrees C at 1.5-2.4 GPa. Type 1 inclusions are trachytic and ultrapotassic, whereas type 2 melts are dacitic to rhyolitic. Thermodynamic modeling of the ultramafic composition in the MnNCKFMASHTO system shows that anatexis occurred at the end of the prograde P-T path, between the solidus (at ca. 860 degrees C-1.4 GPa) and the peak conditions (at ca. 960 degrees C-1.7 GPa). The model melt composition is felsic and similar to that of type 1 inclusions, particularly when the melting degree is low (< 1 mol%), close to the solidus. However the modeling fails to reproduce the highly potassic signature of the melt and its low H2O content. The combination of petrology, melt inclusion study, and thermodynamic modeling supports the interpretation that melt was produced by anatexis of the ultramafic boudins near peak P-T conditions, and that type 1 inclusions contain the anatectic melt that was present during garnet growth. The felsic, ultrapotassic composition of the primary anatectic melts is compatible with low melting degrees in the presence of biotite and amphibole as reactants. KW - Nanogranitoids KW - partial melting KW - thermodynamic modeling KW - Antarctica KW - ultramafic granulites KW - kumdykolite KW - kokchetavite KW - High-Grade Metamorphism KW - Anatexis KW - and Granite Magmatism Y1 - 2018 U6 - https://doi.org/10.2138/am-2018-6214 SN - 0003-004X SN - 1945-3027 VL - 103 IS - 4 SP - 610 EP - 622 PB - Mineralogical Society of America CY - Chantilly ER - TY - JOUR A1 - Jose Clemente-Moreno, Maria A1 - Omranian, Nooshin A1 - Saez, Patricia A1 - Maria Figueroa, Carlos A1 - Del-Saz, Nestor A1 - Elso, Mhartyn A1 - Poblete, Leticia A1 - Orf, Isabel A1 - Cuadros-Inostroza, Alvaro A1 - Cavieres, Lohengrin A1 - Bravo, Leon A1 - Fernie, Alisdair R. A1 - Ribas-Carbo, Miquel A1 - Flexas, Jaume A1 - Nikoloski, Zoran A1 - Brotman, Yariv A1 - Gago, Jorge T1 - Cytochrome respiration pathway and sulphur metabolism sustain stress tolerance to low temperature in the Antarctic species Colobanthus quitensis JF - New phytologist : international journal of plant science N2 - Understanding the strategies employed by plant species that live in extreme environments offers the possibility to discover stress tolerance mechanisms. We studied the physiological, antioxidant and metabolic responses to three temperature conditions (4, 15, and 23 degrees C) of Colobanthus quitensis (CQ), one of the only two native vascular species in Antarctica. We also employed Dianthus chinensis (DC), to assess the effects of the treatments in a non-Antarctic species from the same family. Using fused LASSO modelling, we associated physiological and biochemical antioxidant responses with primary metabolism. This approach allowed us to highlight the metabolic pathways driving the response specific to CQ. Low temperature imposed dramatic reductions in photosynthesis (up to 88%) but not in respiration (sustaining rates of 3.0-4.2 mu mol CO2 m(-2) s(-1)) in CQ, and no change in the physiological stress parameters was found. Its notable antioxidant capacity and mitochondrial cytochrome respiratory activity (20 and two times higher than DC, respectively), which ensure ATP production even at low temperature, was significantly associated with sulphur-containing metabolites and polyamines. Our findings potentially open new biotechnological opportunities regarding the role of antioxidant compounds and respiratory mechanisms associated with sulphur metabolism in stress tolerance strategies to low temperature. KW - Antarctica KW - antioxidant capacity KW - low temperature KW - photosynthesis KW - respiration KW - stress tolerance KW - sulphur metabolism Y1 - 2019 U6 - https://doi.org/10.1111/nph.16167 SN - 0028-646X SN - 1469-8137 VL - 225 IS - 2 SP - 754 EP - 768 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Albrecht, Torsten A1 - Levermann, Anders T1 - Spontaneous ice-front retreat caused by disintegration of adjacent ice shelf in Antarctica JF - Earth & planetary science letters N2 - Antarctic ice-discharge constitutes the largest uncertainty in future sea-level projections. Floating ice shelves, fringing most of Antarctica, exert retentive forces onto the ice flow. While abrupt ice-shelf retreat has been observed, it is generally considered a localized phenomenon. Here we show that the disintegration of an ice shelf may induce the spontaneous retreat of its neighbor. As an example, we reproduce the spontaneous but gradual retreat of the Larsen B ice front as observed after the disintegration of the adjacent Larsen A ice shelf. We show that the Larsen A collapse yields a change in spreading rate in Larsen B via their connecting ice channels and thereby causes a retreat of the ice front to its observed position of the year 2000, prior to its collapse. This mechanism might be particularly relevant for the role of East Antarctica and the Antarctic Peninsula in future sea level. KW - Antarctica KW - Larsen Ice Shelf KW - glaciology KW - numerical ice modeling KW - sea level KW - iceberg calving Y1 - 2014 U6 - https://doi.org/10.1016/j.epsl.2014.02.034 SN - 0012-821X SN - 1385-013X VL - 393 SP - 26 EP - 30 PB - Elsevier CY - Amsterdam ER -