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Antony R, Mongad D, Sanyal A, Dhotre D, Thamban M. Holed up, but thriving: Impact of multitrophic cryoconite communities on glacier elemental cycles. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 933:173187. [PMID: 38750762 DOI: 10.1016/j.scitotenv.2024.173187] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/11/2023] [Revised: 05/10/2024] [Accepted: 05/10/2024] [Indexed: 05/20/2024]
Abstract
Cryoconite holes (water and sediment-filled depressions), found on glacier surfaces worldwide, serve as reservoirs of microbes, carbon, trace elements, and nutrients, transferring these components downstream via glacier hydrological networks. Through targeted amplicon sequencing of carbon and nitrogen cycling genes, coupled with functional inference-based methods, we explore the functional diversity of these mini-ecosystems within Antarctica and the Himalayas. These regions showcase distinct environmental gradients and experience varying rates of environmental change influenced by global climatic shifts. Analysis revealed a diverse array of photosynthetic microorganisms, including Stramenopiles, Cyanobacteria, Rhizobiales, Burkholderiales, and photosynthetic purple sulfur Proteobacteria. Functional inference highlighted the high potential for carbohydrate, amino acid, and lipid metabolism in the Himalayan region, where organic carbon concentrations surpassed those in Antarctica by up to 2 orders of magnitude. Nitrogen cycling processes, including fixation, nitrification, and denitrification, are evident, with Antarctic cryoconite exhibiting a pronounced capacity for nitrogen fixation, potentially compensating for the limited nitrate concentrations in this region. Processes associated with the respiration of elemental sulfur and inorganic sulfur compounds such as sulfate, sulfite, thiosulfate, and sulfide suggest the presence of a complete sulfur cycle. The Himalayan region exhibits a higher potential for sulfur cycling, likely due to the abundant sulfate ions and sulfur-bearing minerals in this region. The capability for complete iron cycling through iron oxidation and reduction reactions was also predicted. Methanogenic archaea that produce methane during organic matter decomposition and methanotrophic bacteria that utilize methane as carbon and energy sources co-exist in the cryoconite, suggesting that these niches support the complete cycling of methane. Additionally, the presence of various microfauna suggests the existence of a complex food web. Collectively, these results indicate that cryoconite holes are self-sustaining ecosystems that drive elemental cycles on glaciers and potentially control carbon, nitrogen, sulfur, and iron exports downstream.
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Affiliation(s)
- Runa Antony
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Vasco-da-Gama, India; GFZ German Research Centre for Geosciences, Potsdam, Germany.
| | - Dattatray Mongad
- National Centre for Microbial Resource, National Centre for Cell Science, Pune, India
| | - Aritri Sanyal
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Vasco-da-Gama, India
| | - Dhiraj Dhotre
- National Centre for Microbial Resource, National Centre for Cell Science, Pune, India
| | - Meloth Thamban
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Vasco-da-Gama, India
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2
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Gladkov GV, Kimeklis AK, Tembotov RK, Ivanov MN, Andronov EE, Abakumov EV. Linking the composition of cryoconite prokaryotic communities in the Arctic, Antarctic, and Central Caucasus with their chemical characteristics. Sci Rep 2024; 14:15838. [PMID: 38982048 PMCID: PMC11233692 DOI: 10.1038/s41598-024-64452-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/31/2023] [Accepted: 06/10/2024] [Indexed: 07/11/2024] Open
Abstract
Cryoconites are the deposits on the surface of glaciers that create specific ecological niches for the development of microorganism communities. The sediment material can vary in origin, structure, and nutrient content, creating local variations in the growth conditions. An additional factor of variability is the location of the glaciers, as they are found in different climatic zones in the high mountain regions and closer to the poles. Here, using the analysis of amplicon sequencing of the 16S rRNA gene, we studied the taxonomic composition of the prokaryotic communities from glaciers from remote regions, including the Arctic (Mushketova on the Severnaya Zemlya, IGAN in Polar Ural), Antarctic (Pimpirev on the Livingstone Island) and Central Caucasus (Skhelda and Garabashi) and connected it with the variation of the physicochemical characteristics of the substrate: pH, carbon, nitrogen, macro- and microelements. The cryoconite microbiomes were comprised of specific for this environment phyla (mostly Pseudomonadota, Cyanobacteria, Bacteroidota, Acidobacteriota, and Actinobacteriota), but each glacier had a unique taxonomic imprint. The core microbiome between regions was composed of only a few ASVs, among which the most likely globally distributed ones attributed to Polaromonas sp., Rhodoferax sp., Cryobacterium sp., and Hymenobacter frigidus. The WGSNA defined clusters of co-occurring ASVs between microbiomes, that significantly change their abundance corresponding with the variation of chemical parameters of cryoconites, but do not fully coincide with their regional separation. Thus, our work demonstrates that the chemical characteristics of the sediment material can explain the variation in the cryoconite prokaryotic community which is not always linked to geographic isolation.
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Affiliation(s)
- Grigory V Gladkov
- Department of Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia, 199034
- Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia, 196608
| | - Anastasiia K Kimeklis
- Department of Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia, 199034
- Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia, 196608
| | - Rustam Kh Tembotov
- Department of Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia, 199034
- Tembotov Institute of Ecology of Mountain Territories, Russian Academy of Sciences, Nalchik, Russia, 360051
| | - Mikhail N Ivanov
- Department of Cryolithology and Glaciology, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow, Russia, 119991
| | - Evgeny E Andronov
- Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia, 196608
- V.V. Dokuchaev Soil Science Institute, Moscow, Russia, 119017
| | - Evgeny V Abakumov
- Department of Applied Ecology, St. Petersburg State University, Saint-Petersburg, Russia, 199034.
- Laboratory of Microbiological Monitoring and Bioremediation of Soils, All-Russian Research Institute for Agricultural Microbiology, Pushkin, Russia, 196608.
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Hassan S, Mushtaq M, Ganiee SA, Zaman M, Yaseen A, Shah AJ, Ganai BA. Microbial oases in the ice: A state-of-the-art review on cryoconite holes as diversity hotspots and their scientific connotations. ENVIRONMENTAL RESEARCH 2024; 252:118963. [PMID: 38640991 DOI: 10.1016/j.envres.2024.118963] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/09/2023] [Revised: 04/13/2024] [Accepted: 04/16/2024] [Indexed: 04/21/2024]
Abstract
Cryoconite holes, small meltwater pools on the surface of glaciers and ice sheets, represent extremely cold ecosystems teeming with diverse microbial life. Cryoconite holes exhibit greater susceptibility to the impacts of climate change, underlining the imperative nature of investigating microbial communities as an essential module of polar and alpine ecosystem monitoring efforts. Microbes in cryoconite holes play a critical role in nutrient cycling and can produce bioactive compounds, holding promise for industrial and pharmaceutical innovation. Understanding microbial diversity in these delicate ecosystems is essential for effective conservation strategies. Therefore, this review discusses the microbial diversity in these extreme environments, aiming to unveil the complexity of their microbial communities. The current study envisages that cryoconite holes as distinctive ecosystems encompass a multitude of taxonomically diverse and functionally adaptable microorganisms that exhibit a rich microbial diversity and possess intricate ecological functions. By investigating microbial diversity and ecological functions of cryoconite holes, this study aims to contribute valuable insights into the broader field of environmental microbiology and enhance further understanding of these ecosystems. This review seeks to provide a holistic overview regarding the formation, evolution, characterization, and molecular adaptations of cryoconite holes. Furthermore, future research directions and challenges underlining the need for long-term monitoring, and ethical considerations in preserving these pristine environments are also provided. Addressing these challenges and resolutely pursuing future research directions promises to enrich our comprehension of microbial diversity within cryoconite holes, revealing the broader ecological and biogeochemical implications. The inferences derived from the present study will provide researchers, ecologists, and policymakers with a profound understanding of the significance and utility of cryoconite holes in unveiling the microbial diversity and its potential applications.
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Affiliation(s)
- Shahnawaz Hassan
- Department of Environmental Science, University of Kashmir, Srinagar, 190006, India.
| | - Misba Mushtaq
- Centre of Research for Development, University of Kashmir, Srinagar, 190006, India
| | - Shahid Ahmad Ganiee
- Department of Environmental Science, University of Kashmir, Srinagar, 190006, India
| | - Muzafar Zaman
- Department of Environmental Science, University of Kashmir, Srinagar, 190006, India
| | - Aarif Yaseen
- Department of Environmental Science, University of Kashmir, Srinagar, 190006, India
| | - Abdul Jalil Shah
- Department of Pharmaceutical Sciences, University of Kashmir, Srinagar, 190006, India
| | - Bashir Ahmad Ganai
- Centre of Research for Development, University of Kashmir, Srinagar, 190006, India.
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Sanyal A, Antony R, Samui G, Thamban M. Autotrophy to Heterotrophy: Shift in Bacterial Functions During the Melt Season in Antarctic Cryoconite Holes. J Microbiol 2024:10.1007/s12275-024-00140-1. [PMID: 38814540 DOI: 10.1007/s12275-024-00140-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/03/2023] [Revised: 03/27/2024] [Accepted: 04/23/2024] [Indexed: 05/31/2024]
Abstract
Microbes residing in cryoconite holes (debris, water, and nutrient-rich ecosystems) on the glacier surface actively participate in carbon and nutrient cycling. Not much is known about how these communities and their functions change during the summer melt-season when intense ablation and runoff alter the influx and outflux of nutrients and microbes. Here, we use high-throughput-amplicon sequencing, predictive metabolic tools and Phenotype MicroArray techniques to track changes in bacterial communities and functions in cryoconite holes in a coastal Antarctic site and the surrounding fjord, during the summer season. The bacterial diversity in cryoconite hole meltwater was predominantly composed of heterotrophs (Proteobacteria) throughout the season. The associated functional potentials were related to heterotrophic-assimilatory and -dissimilatory pathways. Autotrophic Cyanobacterial lineages dominated the debris community at the beginning and end of summer, while heterotrophic Bacteroidota- and Proteobacteria-related phyla increased during the peak melt period. Predictive functional analyses based on taxonomy show a shift from predominantly phototrophy-related functions to heterotrophic assimilatory pathways as the melt-season progressed. This shift from autotrophic to heterotrophic communities within cryoconite holes can affect carbon drawdown and nutrient liberation from the glacier surface during the summer. In addition, the flushing out and export of cryoconite hole communities to the fjord could influence the biogeochemical dynamics of the fjord ecosystem.
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Affiliation(s)
- Aritri Sanyal
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Goa, 403804, India.
- School of Earth, Ocean and Atmospheric Sciences, Goa University, Goa, 403206, India.
| | - Runa Antony
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Goa, 403804, India
- GFZ German Research Centre for Geosciences, 14473, Potsdam, Germany
| | - Gautami Samui
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Goa, 403804, India
- Department of Environmental Science, Savitribai Phule Pune University, Ganeshkhind, Pune, 411007, India
| | - Meloth Thamban
- National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Goa, 403804, India
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5
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Lu Q, Liu Y, Zhao J, Yao M. Successive accumulation of biotic assemblages at a fine spatial scale along glacier-fed waters. iScience 2024; 27:109476. [PMID: 38617565 PMCID: PMC11015461 DOI: 10.1016/j.isci.2024.109476] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/10/2023] [Revised: 01/14/2024] [Accepted: 03/08/2024] [Indexed: 04/16/2024] Open
Abstract
Glacier-fed waters create strong environmental filtering for biota, whereby different organisms may assume distinct distribution patterns. By using environmental DNA-based metabarcoding, we investigated the multi-group biodiversity distribution patterns of the Parlung No. 4 Glacier, on the Tibetan Plateau. Altogether, 642 taxa were identified from the meltwater stream and the downstream Ranwu Lake, including 125 cyanobacteria, 316 diatom, 183 invertebrate, and 18 vertebrate taxa. As the distance increased from the glacier terminus, community complexity increased via sequential occurrences of cyanobacteria, diatoms, invertebrates, and vertebrates, as well as increasing taxa numbers. The stream and lake showed different community compositions and distinct taxa. Furthermore, the correlations with environmental factors and community assembly mechanisms showed group- and habitat-specific patterns. Our results reveal the rapid spatial succession and increasing community complexity along glacial flowpaths and highlight the varying adaptivity of different organisms, while also providing insight into the ecosystem responses to global change.
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Affiliation(s)
- Qi Lu
- School of Life Sciences, Peking University, Beijing 100871, China
- Institute of Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
| | - Yongqin Liu
- Center for Pan-Third Pole Environment, Lanzhou University, Lanzhou 730000, China
- State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
- University of Chinese Academy of Sciences, Beijing 101408, China
| | - Jindong Zhao
- School of Life Sciences, Peking University, Beijing 100871, China
- Institute of Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
| | - Meng Yao
- School of Life Sciences, Peking University, Beijing 100871, China
- Institute of Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
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6
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Hay MC, Mitchell AC, Soares AR, Debbonaire AR, Mogrovejo DC, Els N, Edwards A. Metagenome-assembled genomes from High Arctic glaciers highlight the vulnerability of glacier-associated microbiota and their activities to habitat loss. Microb Genom 2023; 9. [PMID: 37937832 DOI: 10.1099/mgen.0.001131] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2023] Open
Abstract
The rapid warming of the Arctic is threatening the demise of its glaciers and their associated ecosystems. Therefore, there is an urgent need to explore and understand the diversity of genomes resident within glacial ecosystems endangered by human-induced climate change. In this study we use genome-resolved metagenomics to explore the taxonomic and functional diversity of different habitats within glacier-occupied catchments. Comparing different habitats within such catchments offers a natural experiment for understanding the effects of changing habitat extent or even loss upon Arctic microbiota. Through binning and annotation of metagenome-assembled genomes (MAGs) we describe the spatial differences in taxon distribution and their implications for glacier-associated biogeochemical cycling. Multiple taxa associated with carbon cycling included organisms with the potential for carbon monoxide oxidation. Meanwhile, nitrogen fixation was mediated by a single taxon, although diverse taxa contribute to other nitrogen conversions. Genes for sulphur oxidation were prevalent within MAGs implying the potential capacity for sulphur cycling. Finally, we focused on cyanobacterial MAGs, and those within cryoconite, a biodiverse microbe-mineral granular aggregate responsible for darkening glacier surfaces. Although the metagenome-assembled genome of Phormidesmis priestleyi, the cyanobacterium responsible for forming Arctic cryoconite was represented with high coverage, evidence for the biosynthesis of multiple vitamins and co-factors was absent from its MAG. Our results indicate the potential for cross-feeding to sustain P. priestleyi within granular cryoconite. Taken together, genome-resolved metagenomics reveals the vulnerability of glacier-associated microbiota to the deletion of glacial habitats through the rapid warming of the Arctic.
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Affiliation(s)
- Melanie C Hay
- Department of Life Sciences (DLS), Aberystwyth University, Wales, UK
- Interdisciplinary Centre for Environmental Microbiology (iCEM), Aberystwyth University, Wales, UK
- Department of Geography and Earth Sciences (DGES), Aberystwyth University, Wales, UK
- Present address: Department of Pathobiology and Population Sciences, The Royal Veterinary College, North Mymms, Hertfordshire, UK
| | - Andrew C Mitchell
- Interdisciplinary Centre for Environmental Microbiology (iCEM), Aberystwyth University, Wales, UK
- Department of Geography and Earth Sciences (DGES), Aberystwyth University, Wales, UK
| | - Andre R Soares
- Department of Life Sciences (DLS), Aberystwyth University, Wales, UK
- Interdisciplinary Centre for Environmental Microbiology (iCEM), Aberystwyth University, Wales, UK
- Department of Geography and Earth Sciences (DGES), Aberystwyth University, Wales, UK
- Present address: Environmental Metagenomics, Research Center One Health Ruhr of the University Alliance Ruhr, Faculty of Chemistry, University of Duisburg-Essen, Essen, Germany
| | - Aliyah R Debbonaire
- Department of Life Sciences (DLS), Aberystwyth University, Wales, UK
- Interdisciplinary Centre for Environmental Microbiology (iCEM), Aberystwyth University, Wales, UK
| | - Diana C Mogrovejo
- Dr. Brill + Partner GmbH Institut für Hygiene und Mikrobiologie, Hamburg, Germany
| | - Nora Els
- Department of Lake and Glacier Research, Institute of Ecology, University of Innsbruck, Innsbruck, Austria
| | - Arwyn Edwards
- Department of Life Sciences (DLS), Aberystwyth University, Wales, UK
- Interdisciplinary Centre for Environmental Microbiology (iCEM), Aberystwyth University, Wales, UK
- Department of Arctic Biology, University Centre in Svalbard (UNIS), Longyearbyen, Svalbard and Jan Mayen
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7
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Hattori S, Li Z, Yoshida N, Takeuchi N. Isotopic Evidence for Microbial Nitrogen Cycling in a Glacier Interior of High-Mountain Asia. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:15026-15036. [PMID: 37747413 DOI: 10.1021/acs.est.3c04757] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 09/26/2023]
Abstract
Glaciers are now acknowledged as an important biome globally, but biological processes in the interior of the glacier (englacial) are thought to be slow and to play only a minor role in biogeochemical cycles. In this study, we demonstrate extensive, microbially driven englacial nitrogen cycling in an Asian glacier using the stable isotopes (δ15N, δ18O, and Δ17O values) of nitrate. Apparent decreases in Δ17O values of nitrate in an 8 m shallow firn core from the accumulation area indicate that nitrifiers gradually replaced ∼80% of atmospheric nitrate with nitrate from microbial nitrification on a decadal scale. Nitrate concentrations did not increase with depth in this core, suggesting the presence of nitrate sinks by microbial assimilation and denitrification within the firn layers. The estimated englacial metabolic rate using isotopic mass balance was classified as growth metabolism, which is approximately 2 orders of magnitude more active than previously known cold-environment metabolisms. In a 56 m ice core from the interior of the ablation area, we found less nitrification but continued microbial nitrate consumption, implying that organic matter is microbially accumulated over centuries before appearing on the ablating surface. Such englacial microbial products may support supraglacial microbes, potentially promoting glacial darkening and melting. With predicted global warming and higher nitrogen loads, englacial nutrient cycling and its roles may become increasingly important in the future.
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Affiliation(s)
- Shohei Hattori
- International Center for Isotope Effects Research (ICIER), Nanjing University, Nanjing 210023, China
- Frontiers Science Center for Critical Earth Material Cycling, State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
| | - Zhongqin Li
- State Key Laboratory of Cryospheric Sciences/Tien Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
| | - Naohiro Yoshida
- Department of Chemical Science and Engineering, School of Materials and Chemical Technology, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8502, Japan
- Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8551, Japan
- National Institute of Information and Communications Technology, Tokyo 184-8795, Japan
| | - Nozomu Takeuchi
- Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba 263-8522, Japan
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Wejnerowski Ł, Poniecka E, Buda J, Klimaszyk P, Piasecka A, Dziuba MK, Mugnai G, Takeuchi N, Zawierucha K. Empirical testing of cryoconite granulation: Role of cyanobacteria in the formation of key biogenic structure darkening glaciers in polar regions. JOURNAL OF PHYCOLOGY 2023; 59:939-949. [PMID: 37572353 DOI: 10.1111/jpy.13372] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/03/2023] [Revised: 06/18/2023] [Accepted: 07/03/2023] [Indexed: 08/14/2023]
Abstract
Cryoconite, the dark sediment on the surface of glaciers, often aggregates into oval or irregular granules serving as biogeochemical factories. They reduce a glacier's albedo, act as biodiversity hotspots by supporting aerobic and anaerobic microbial communities, constitute one of the organic matter (OM) sources on glaciers, and are a feeder for micrometazoans. Although cryoconite granules have multiple roles on glaciers, their formation is poorly understood. Cyanobacteria are ubiquitous and abundant engineers of cryoconite hole ecosystems. This study tested whether cyanobacteria may be responsible for cryoconite granulation as a sole biotic element. Incubation of Greenlandic, Svalbard, and Scandinavian cyanobacteria in different nutrient availabilities and substrata for growth (distilled water alone and water with quartz powder, furnaced cryoconite without OM, or powdered rocks from glacial catchment) revealed that cyanobacteria bind mineral particles into granules. The structures formed in the experiment resembled those commonly observed in natural cryoconite holes: they contained numerous cyanobacterial filaments protruding from aggregated mineral particles. Moreover, all examined strains were confirmed to produce extracellular polymeric substances (EPS), which suggests that cryoconite granulation is most likely due to EPS secretion by gliding cyanobacteria. In the presence of water as the only substrate for growth, cyanobacteria formed mostly carpet-like mats. Our data empirically prove that EPS-producing oscillatorialean cyanobacteria isolated from the diverse community of cryoconite microorganisms can form granules from mineral substrate and that the presence of the mineral substrate increases the probability of the formation of these important and complex biogeochemical microstructures on glaciers.
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Affiliation(s)
- Łukasz Wejnerowski
- Department of Hydrobiology, Institute of Environmental Biology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Ewa Poniecka
- Department of Environmental Microbiology and Biotechnology, Faculty of Biology, University of Warsaw, Warsaw, Poland
| | - Jakub Buda
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Piotr Klimaszyk
- Department of Water Protection, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Agnieszka Piasecka
- Department of Gene Expression, Institute of Molecular Biology and Biotechnology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Marcin Krzysztof Dziuba
- Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, Michigan, USA
| | - Gianmarco Mugnai
- Department of Agriculture, Food and Environmental Sciences, University of Perugia, Perugia, Italy
| | - Nozomu Takeuchi
- Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, Japan
| | - Krzysztof Zawierucha
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
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Sorokovikova E, Tikhonova I, Evseev P, Krasnopeev A, Khanaev I, Potapov S, Gladkikh A, Nebesnykh I, Belykh O. Limnofasciculus baicalensis gen. et sp. nov. (Coleofasciculaceae, Coleofasciculales): A New Genus of Cyanobacteria Isolated from Sponge Fouling in Lake Baikal, Russia. Microorganisms 2023; 11:1779. [PMID: 37512951 PMCID: PMC10385159 DOI: 10.3390/microorganisms11071779] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/24/2023] [Revised: 07/06/2023] [Accepted: 07/07/2023] [Indexed: 07/30/2023] Open
Abstract
The proliferation of benthic cyanobacteria has been observed in Lake Baikal since 2011 and is a vivid manifestation of the ecological crisis occurring in the littoral zone. The cyanobacterium Symplocastrum sp. has formed massive fouling on all types of benthic substrates, including endemic Baikal sponges. The strain BBK-W-15 (=IPPAS B-2062T), which was isolated from sponge fouling in 2015, was used for further taxonomic determination. A polyphasic approach revealed that it is a cryptic taxon of cyanobacteria. Morphological evaluation of the strain indicated the presence of cylindrical filaments with isodiametric cells enclosed in individual sheaths and coleodesmoid false branching. Strain ultrastructure (fascicular thylakoids and type C cell division) is characteristic of the Microcoleaceae and Coleofasciculaceae families. An integrated analysis that included 16S rRNA gene phylogeny, conserved protein phylogeny and whole-genome comparisons indicated the unique position of BBK-W-15, thus supporting the proposed delineation of the new genus Limnofasciculus. Through characterisation by morphology, 16S, ITS and genomic analysis, a new cyanobacterium of the family Coleofasciculaceae Limnofasciculus baicalensis gen. et sp. nov. was described.
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Affiliation(s)
- Ekaterina Sorokovikova
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Irina Tikhonova
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Peter Evseev
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
- Shemyakin-Ovchinnikov Institute of Bioorganic Chemistry of the Russian Academy of Sciences, 16/10 Miklukho-Maklaya Str., GSP-7, Moscow 117997, Russia
| | - Andrey Krasnopeev
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Igor Khanaev
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Sergey Potapov
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Anna Gladkikh
- Saint-Petersburg Pasteur Institute, 14 Mira Str., Saint-Petersburg 197101, Russia
| | - Ivan Nebesnykh
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
| | - Olga Belykh
- Limnological Institute of the Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya Str., Irkutsk 664033, Russia
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10
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Trebuch LM, Bourceau OM, Vaessen SMF, Neu TR, Janssen M, de Beer D, Vet LEM, Wijffels RH, Fernandes TV. High resolution functional analysis and community structure of photogranules. THE ISME JOURNAL 2023; 17:870-879. [PMID: 36997724 DOI: 10.1038/s41396-023-01394-0] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/30/2022] [Revised: 02/28/2023] [Accepted: 03/03/2023] [Indexed: 03/31/2023]
Abstract
AbstractPhotogranules are spherical aggregates formed of complex phototrophic ecosystems with potential for “aeration-free” wastewater treatment. Photogranules from a sequencing batch reactor were investigated by fluorescence microscopy, 16S/18S rRNA gene amplicon sequencing, microsensors, and stable- and radioisotope incubations to determine the granules’ composition, nutrient distribution, and light, carbon, and nitrogen budgets. The photogranules were biologically and chemically stratified, with filamentous cyanobacteria arranged in discrete layers and forming a scaffold to which other organisms were attached. Oxygen, nitrate, and light gradients were also detectable. Photosynthetic activity and nitrification were both predominantly restricted to the outer 500 µm, but while photosynthesis was relatively insensitive to the oxygen and nutrient (ammonium, phosphate, acetate) concentrations tested, nitrification was highly sensitive. Oxygen was cycled internally, with oxygen produced through photosynthesis rapidly consumed by aerobic respiration and nitrification. Oxygen production and consumption were well balanced. Similarly, nitrogen was cycled through paired nitrification and denitrification, and carbon was exchanged through photosynthesis and respiration. Our findings highlight that photogranules are complete, complex ecosystems with multiple linked nutrient cycles and will aid engineering decisions in photogranular wastewater treatment.
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Pittino F, Zawierucha K, Poniecka E, Buda J, Rosatelli A, Zordan S, Azzoni RS, Diolaiuti G, Ambrosini R, Franzetti A. Functional and Taxonomic Diversity of Anaerobes in Supraglacial Microbial Communities. Microbiol Spectr 2023; 11:e0100422. [PMID: 36939373 PMCID: PMC10100660 DOI: 10.1128/spectrum.01004-22] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/20/2022] [Accepted: 02/16/2023] [Indexed: 03/21/2023] Open
Abstract
Cryoconite holes are small ponds present on the surface of most glaciers filled with meltwater and sediment at the bottom. Although they are characterized by extreme conditions, they host bacterial communities with high taxonomic and functional biodiversity. Despite that evidence for a potential niche for anaerobic microorganisms and anaerobic processes has recently emerged, the composition of the microbial communities of the cryoconite reported so far has not shown the relevant presence of anaerobic taxa. We hypothesize that this is due to the lower growth yield of anaerobes compared to aerobic microorganisms. In this work, we aim at evaluating whether the anaerobic bacterial community represents a relevant fraction of the biodiversity of the cryoconite and at describing its structure and functions. We collected sediment samples from cryoconite holes on the Forni Glacier (Italy) and sequenced both 16S rRNA amplicon genes and 16S rRNA amplicon transcripts at different times of the day along a clear summer day. Results showed that a relevant fraction of taxa has been detected only by 16S rRNA transcripts and was undetectable in 16S rRNA gene amplicons. Furthermore, in the transcript approach, anaerobic taxa were overrepresented compared with DNA sequencing. The metatranscriptomics approach was used also to investigate the expression of the main metabolic functions. Results showed the occurrence of syntrophic and commensalism relationships among fermentative bacteria, hydrogenothrophs, and consumers of fermentation end products, which have never been reported so far in cryoconite. IMPORTANCE Recent evidence disclosed the presence of a potential niche for anaerobic microorganisms and anaerobic processes in supraglacial sediments (cryoconite), but a detailed description of the structure and functions of the anaerobic population is still lacking. This work used rRNA and mRNA sequencing and demonstrated that anaerobes are very active in these environments and represent a relevant albeit neglected part of the ecosystem functions in these environments.
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Affiliation(s)
- Francesca Pittino
- Department of Earth and Environmental Sciences (DISAT)–University of Milano-Bicocca, Milano, Italy
- Biodiversity and Conservation Biology, Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
| | - Krzysztof Zawierucha
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
- Faculty of Forestry and Wood Sciences, Czech University of Life Sciences, Prague, Czech Republic
| | - Ewa Poniecka
- Department of Environmental Microbiology and Biotechnology, Faculty of Biology, University of Warsaw, Warsaw, Poland
| | - Jakub Buda
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Asia Rosatelli
- Department of Earth and Environmental Sciences (DISAT)–University of Milano-Bicocca, Milano, Italy
| | - Simone Zordan
- Department of Earth and Environmental Sciences (DISAT)–University of Milano-Bicocca, Milano, Italy
| | - Roberto S. Azzoni
- Department of Earth Science “Ardito Desio,” University of Milan, Milano, Italy
| | - Guglielmina Diolaiuti
- Department of Environmental Science and Policy (ESP), University of Milan, Milano, Italy
| | - Roberto Ambrosini
- Department of Environmental Science and Policy (ESP), University of Milan, Milano, Italy
| | - Andrea Franzetti
- Department of Earth and Environmental Sciences (DISAT)–University of Milano-Bicocca, Milano, Italy
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12
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Trivedi CB, Keuschnig C, Larose C, Rissi DV, Mourot R, Bradley JA, Winkel M, Benning LG. DNA/RNA Preservation in Glacial Snow and Ice Samples. Front Microbiol 2022; 13:894893. [PMID: 35677909 PMCID: PMC9168539 DOI: 10.3389/fmicb.2022.894893] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/12/2022] [Accepted: 04/29/2022] [Indexed: 11/13/2022] Open
Abstract
The preservation of nucleic acids for high-throughput sequencing is an ongoing challenge for field scientists. In particular, samples that are low biomass, or that have to be collected and preserved in logistically challenging environments (such as remote sites or during long sampling campaigns) can pose exceptional difficulties. With this work, we compare and assess the effectiveness of three preservation methods for DNA and RNA extracted from microbial communities of glacial snow and ice samples. Snow and ice samples were melted and filtered upon collection in Iceland, and filters were preserved using: (i) liquid nitrogen flash freezing, (ii) storage in RNAlater, or (iii) storage in Zymo DNA/RNA Shield. Comparative statistics covering nucleic acid recovery, sequencing library preparation, genome assembly, and taxonomic diversity were used to determine best practices for the preservation of DNA and RNA samples from these environments. Our results reveal that microbial community composition based on DNA was comparable at the class level across preservation types. Based on extracted RNA, the taxonomic composition of the active community was primarily driven by the filtered sample volume (i.e., biomass content). In low biomass samples (where <200 ml of sample volume was filtered) the taxonomic and functional signatures trend toward the composition of the control samples, while in samples where a larger volume (more biomass) was filtered our data showed comparable results independent of preservation type. Based on all comparisons our data suggests that flash freezing of filters containing low biomass is the preferred method for preserving DNA and RNA (notwithstanding the difficulties of accessing liquid nitrogen in remote glacial field sites). Generally, RNAlater and Zymo DNA/RNA Shield solutions work comparably well, especially for DNA from high biomass samples, but Zymo DNA/RNA Shield is favored due to its higher yield of preserved RNA. Biomass quantity from snow and ice samples appears to be the most important factor in regards to the collection and preservation of samples from glacial environments.
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Affiliation(s)
- Christopher B Trivedi
- Interface Geochemistry, GFZ German Research Centre for Geosciences, Potsdam, Germany
| | | | - Catherine Larose
- Environmental Microbial Genomics, Université de Lyon, Ecully Cedex, France
| | | | - Rey Mourot
- Interface Geochemistry, GFZ German Research Centre for Geosciences, Potsdam, Germany.,Department of Earth Sciences, Freie Universität Berlin, Berlin, Germany
| | - James A Bradley
- Interface Geochemistry, GFZ German Research Centre for Geosciences, Potsdam, Germany.,School of Geography, Queen Mary University of London, London, United Kingdom
| | - Matthias Winkel
- Interface Geochemistry, GFZ German Research Centre for Geosciences, Potsdam, Germany
| | - Liane G Benning
- Interface Geochemistry, GFZ German Research Centre for Geosciences, Potsdam, Germany.,Department of Earth Sciences, Freie Universität Berlin, Berlin, Germany
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13
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Murakami T, Takeuchi N, Mori H, Hirose Y, Edwards A, Irvine-Fynn T, Li Z, Ishii S, Segawa T. Metagenomics reveals global-scale contrasts in nitrogen cycling and cyanobacterial light-harvesting mechanisms in glacier cryoconite. MICROBIOME 2022; 10:50. [PMID: 35317857 PMCID: PMC8941735 DOI: 10.1186/s40168-022-01238-7] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/02/2021] [Accepted: 01/27/2022] [Indexed: 06/14/2023]
Abstract
BACKGROUND Cryoconite granules are mineral-microbial aggregates found on glacier surfaces worldwide and are hotspots of biogeochemical reactions in glacier ecosystems. However, despite their importance within glacier ecosystems, the geographical diversity of taxonomic assemblages and metabolic potential of cryoconite communities around the globe remain unclear. In particular, the genomic content of cryoconite communities on Asia's high mountain glaciers, which represent a substantial portion of Earth's ice masses, has rarely been reported. Therefore, in this study, to elucidate the taxonomic and ecological diversities of cryoconite bacterial consortia on a global scale, we conducted shotgun metagenomic sequencing of cryoconite acquired from a range of geographical areas comprising Polar (Arctic and Antarctic) and Asian alpine regions. RESULTS Our metagenomic data indicate that compositions of both bacterial taxa and functional genes are particularly distinctive for Asian cryoconite. Read abundance of the genes responsible for denitrification was significantly more abundant in Asian cryoconite than the Polar cryoconite, implying that denitrification is more enhanced in Asian glaciers. The taxonomic composition of Cyanobacteria, the key primary producers in cryoconite communities, also differs between the Polar and Asian samples. Analyses on the metagenome-assembled genomes and fluorescence emission spectra reveal that Asian cryoconite is dominated by multiple cyanobacterial lineages possessing phycoerythrin, a green light-harvesting component for photosynthesis. In contrast, Polar cryoconite is dominated by a single cyanobacterial species Phormidesmis priestleyi that does not possess phycoerythrin. These findings suggest that the assemblage of cryoconite bacterial communities respond to regional- or glacier-specific physicochemical conditions, such as the availability of nutrients (e.g., nitrate and dissolved organic carbon) and light (i.e., incident shortwave radiation). CONCLUSIONS Our genome-resolved metagenomics provides the first characterization of the taxonomic and metabolic diversities of cryoconite from contrasting geographical areas, highlighted by the distinct light-harvesting approaches of Cyanobacteria and nitrogen utilization between Polar and Asian cryoconite, and implies the existence of environmental controls on the assemblage of cryoconite communities. These findings deepen our understanding of the biodiversity and biogeochemical cycles of glacier ecosystems, which are susceptible to ongoing climate change and glacier decline, on a global scale. Video abstract.
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Affiliation(s)
- Takumi Murakami
- Department of Informatics, National Institute of Genetics, Shizuoka, Japan
- Advanced Genomics Center, National Institute of Genetics, Shizuoka, Japan
| | - Nozomu Takeuchi
- Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, Japan
| | - Hiroshi Mori
- Department of Informatics, National Institute of Genetics, Shizuoka, Japan
- Advanced Genomics Center, National Institute of Genetics, Shizuoka, Japan
| | - Yuu Hirose
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, Aichi, Japan
| | - Arwyn Edwards
- Institute of Biological, Environmental & Rural Sciences (IBERS), Aberystwyth University, Aberystwyth, UK
- Interdisciplinary Centre for Environmental Microbiology, Aberystwyth University, Aberystwyth, UK
| | - Tristram Irvine-Fynn
- Interdisciplinary Centre for Environmental Microbiology, Aberystwyth University, Aberystwyth, UK
- Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, UK
| | - Zhongqin Li
- State Key Laboratory of Cryospheric Sciences/Tien Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China
| | - Satoshi Ishii
- Department of Soil, Water and Climate, University of Minnesota, St. Paul, MN USA
- BioTechnology Institute, University of Minnesota, St. Paul, MN USA
| | - Takahiro Segawa
- Center for Life Science Research, University of Yamanashi, Yamanashi, Japan
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14
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Rozwalak P, Podkowa P, Buda J, Niedzielski P, Kawecki S, Ambrosini R, Azzoni RS, Baccolo G, Ceballos JL, Cook J, Di Mauro B, Ficetola GF, Franzetti A, Ignatiuk D, Klimaszyk P, Łokas E, Ono M, Parnikoza I, Pietryka M, Pittino F, Poniecka E, Porazinska DL, Richter D, Schmidt SK, Sommers P, Souza-Kasprzyk J, Stibal M, Szczuciński W, Uetake J, Wejnerowski Ł, Yde JC, Takeuchi N, Zawierucha K. Cryoconite - From minerals and organic matter to bioengineered sediments on glacier's surfaces. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 807:150874. [PMID: 34627905 DOI: 10.1016/j.scitotenv.2021.150874] [Citation(s) in RCA: 15] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/08/2021] [Revised: 10/03/2021] [Accepted: 10/04/2021] [Indexed: 06/13/2023]
Abstract
Cryoconite is a mixture of mineral and organic material covering glacial ice, playing important roles in biogeochemical cycles and lowering the albedo of a glacier surface. Understanding the differences in structure of cryoconite across the globe can be important in recognizing past and future changes in supraglacial environments and ice-organisms-minerals interactions. Despite the worldwide distribution and over a century of studies, the basic characteristics of cryoconite, including its forms and geochemistry, remain poorly studied. The major purpose of our study is the presentation and description of morphological diversity, chemical and photoautotrophs composition, and organic matter content of cryoconite sampled from 33 polar and mountain glaciers around the globe. Observations revealed that cryoconite is represented by various morphologies including loose and granular forms. Granular cryoconite includes smooth, rounded, or irregularly shaped forms; with some having their surfaces covered by cyanobacteria filaments. The occurrence of granules increased with the organic matter content in cryoconite. Moreover, a major driver of cryoconite colouring was the concentration of organic matter and its interplay with minerals. The structure of cyanobacteria and algae communities in cryoconite differs between glaciers, but representatives of cyanobacteria families Pseudanabaenaceae and Phormidiaceae, and algae families Mesotaeniaceae and Ulotrichaceae were the most common. The most of detected cyanobacterial taxa are known to produce polymeric substances (EPS) that may cement granules. Organic matter content in cryoconite varied between glaciers, ranging from 1% to 38%. The geochemistry of all the investigated samples reflected local sediment sources, except of highly concentrated Pb and Hg in cryoconite collected from European glaciers near industrialized regions, corroborating cryoconite as element-specific collector and potential environmental indicator of anthropogenic activity. Our work supports a notion that cryoconite may be more than just simple sediment and instead exhibits complex structure with relevance for biodiversity and the functioning of glacial ecosystems.
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Affiliation(s)
- Piotr Rozwalak
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland; Geohazards Research Unit, Institute of Geology, Adam Mickiewicz University, Poznan, Poland
| | - Paweł Podkowa
- Department of Avian Biology and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Jakub Buda
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Przemysław Niedzielski
- Department of Analytical Chemistry, Faculty of Chemistry, Adam Mickiewicz University, Poznań, Poland
| | | | - Roberto Ambrosini
- Department of Environmental Science and Policy, University of Milan, Milan, Italy
| | - Roberto S Azzoni
- Department of Earth Sciences, "Ardito Desio", University of Milan, Milan, Italy
| | - Giovanni Baccolo
- Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
| | - Jorge L Ceballos
- Institute of Hydrology, Meteorology and Environmental Studies, IDEAM, Bogota, Colombia
| | - Joseph Cook
- Department of Environmental Sciences, Aarhus University, Aarhus, Denmark
| | - Biagio Di Mauro
- Institute of Polar Sciences, National Research Council, Venice, Italy
| | - Gentile Francesco Ficetola
- Department of Environmental Science and Policy, University of Milan, Milan, Italy; Laboratoire d'Ecologie Alpine, University Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, France
| | - Andrea Franzetti
- Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
| | - Dariusz Ignatiuk
- University of Silesia in Katowice, Institute of Earth Sciences, Bedzinska 60, 41-200 Sosnowiec, Poland
| | - Piotr Klimaszyk
- Department of Water Protection, Faculty of Biology, Adam Mickiewicz University, 61-614 Poznań, Poland
| | - Edyta Łokas
- Department of Mass Spectrometry, Institute of Nuclear Physics, Polish Academy of Sciences, Kraków, Poland
| | - Masato Ono
- Graduate School of Science and Engineering, Chiba University, Chiba, Japan
| | - Ivan Parnikoza
- State Institution National Antarctic Center of Ministry of Education and Science of Ukraine, Kyiv, Ukraine; Institute of Molecular Biology and Genetics, National Academy of Sciences of Ukraine, Kyiv, Ukraine
| | - Mirosława Pietryka
- Department of Botany and Plant Ecology, Wrocław University of Environmental and Life Science, pl. Grunwaldzki 24a, 50-363 Wrocław, Poland
| | - Francesca Pittino
- Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
| | - Ewa Poniecka
- Department of Environmental Microbiology and Biotechnology, Faculty of Biology, University of Warsaw, Warsaw, Poland
| | - Dorota L Porazinska
- Department of Entomology and Nematology, University of Florida, Gainesville, FL, USA
| | - Dorota Richter
- Department of Botany and Plant Ecology, Wrocław University of Environmental and Life Science, pl. Grunwaldzki 24a, 50-363 Wrocław, Poland
| | - Steven K Schmidt
- Ecology and Evolutionary Biology Department, University of Colorado, Boulder, CO, USA
| | - Pacifica Sommers
- Ecology and Evolutionary Biology Department, University of Colorado, Boulder, CO, USA
| | - Juliana Souza-Kasprzyk
- Department of Analytical Chemistry, Faculty of Chemistry, Adam Mickiewicz University, Poznań, Poland
| | - Marek Stibal
- Department of Ecology, Faculty of Science, Charles University, Prague, Czech Republic
| | - Witold Szczuciński
- Geohazards Research Unit, Institute of Geology, Adam Mickiewicz University, Poznan, Poland
| | - Jun Uetake
- Field Research Center for Northern Biosphere, Hokkaido University, Sapporo, Japan
| | - Łukasz Wejnerowski
- Department of Hydrobiology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - Jacob C Yde
- Department of Environmental Sciences, Western Norway University of Applied Sciences, Sogndal, Norway
| | - Nozomu Takeuchi
- Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, Japan
| | - Krzysztof Zawierucha
- Department of Animal Taxonomy and Ecology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland.
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15
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Buda J, Poniecka EA, Rozwalak P, Ambrosini R, Bagshaw EA, Franzetti A, Klimaszyk P, Nawrot A, Pietryka M, Richter D, Zawierucha K. Is Oxygenation Related to the Decomposition of Organic Matter in Cryoconite Holes? Ecosystems 2021. [DOI: 10.1007/s10021-021-00729-2] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/19/2022]
Abstract
AbstractCryoconite is a sediment occurring on glacier surfaces worldwide which reduces ice albedo and concentrates glacier surface meltwater into small reservoirs called cryoconite holes. It consists of mineral and biogenic matter, including active microorganisms. This study presents an experimental insight into the influence of sediment oxygenation on the cryoconite ability to produce and decomposition of organic matter. Samples were collected from five glaciers in the Arctic and the European mainland. Cryoconite from three glaciers was incubated in stagnant and mechanically mixed conditions to imitate inter-hole water–sediment mixing by meltwater occurring on glaciers in Northern Hemisphere, and its effect on oxygen profiles and organic matter content. Moreover, we investigated short-term changes of oxygen conditions in cryoconite from four glaciers in illuminated and dark conditions. An anaerobic zone was present or approaching zero oxygen in all illuminated cryoconite samples, varying in depth depending on the origin of cryoconite: from 1500 µm from Steindalsbreen (Scandinavian Peninsula) and Forni Glacier (The Alps) to 3100 µm from Russell Glacier and Longyearbreen (Arctic) after incubation. Organic matter content varied between glaciers from 6.11% on Longyearbreen to 16.36% on Russell Glacier. The mixed sediment from the Forni Glacier had less organic matter than stagnant, the sediment from Longyearbreen followed this trend, but the difference was not statistically significant, while the sediment from Ebenferner did not differ between groups. Our results have implications for the understanding of biogeochemical processes on glacier surfaces, the adaptation of organisms to changing physical conditions due to abrupt sediment mixing, but also on the estimation of productivity of supraglacial systems.
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16
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Hirose Y, Ohtsubo Y, Misawa N, Yonekawa C, Nagao N, Shimura Y, Fujisawa T, Kanesaki Y, Katoh H, Katayama M, Yamaguchi H, Yoshikawa H, Ikeuchi M, Eki T, Nakamura Y, Kawachi M. Genome sequencing of the NIES Cyanobacteria collection with a focus on the heterocyst-forming clade. DNA Res 2021; 28:6408441. [PMID: 34677568 PMCID: PMC8634303 DOI: 10.1093/dnares/dsab024] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/25/2021] [Accepted: 10/19/2021] [Indexed: 12/03/2022] Open
Abstract
Cyanobacteria are a diverse group of Gram-negative prokaryotes that perform oxygenic photosynthesis. Cyanobacteria have been used for research on photosynthesis and have attracted attention as a platform for biomaterial/biofuel production. Cyanobacteria are also present in almost all habitats on Earth and have extensive impacts on global ecosystems. Given their biological, economical, and ecological importance, the number of high-quality genome sequences for Cyanobacteria strains is limited. Here, we performed genome sequencing of Cyanobacteria strains in the National Institute for Environmental Studies microbial culture collection in Japan. We sequenced 28 strains that can form a heterocyst, a morphologically distinct cell that is specialized for fixing nitrogen, and 3 non-heterocystous strains. Using Illumina sequencing of paired-end and mate-pair libraries with in silico finishing, we constructed highly contiguous assemblies. We determined the phylogenetic relationship of the sequenced genome assemblies and found potential difficulties in the classification of certain heterocystous clades based on morphological observation. We also revealed a bias on the sequenced strains by the phylogenetic analysis of the 16S rRNA gene including unsequenced strains. Genome sequencing of Cyanobacteria strains deposited in worldwide culture collections will contribute to understanding the enormous genetic and phenotypic diversity within the phylum Cyanobacteria.
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Affiliation(s)
- Yuu Hirose
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, 1-1 Hibarigaoka, Tenpaku, Toyohashi, Aichi, 441-8580, Japan
| | - Yoshiyuki Ohtsubo
- Graduate School of Life Sciences, Tohoku University, 2-1-1 Katahira, Aoba, Sendai, Miyagi, 980-0812, Japan
| | - Naomi Misawa
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, 1-1 Hibarigaoka, Tenpaku, Toyohashi, Aichi, 441-8580, Japan
| | - Chinatsu Yonekawa
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, 1-1 Hibarigaoka, Tenpaku, Toyohashi, Aichi, 441-8580, Japan
| | - Nobuyoshi Nagao
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, 1-1 Hibarigaoka, Tenpaku, Toyohashi, Aichi, 441-8580, Japan
| | - Yohei Shimura
- Biodiversity Division, National Institute for Environmental Studies, 16-1 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan
| | - Takatomo Fujisawa
- Department of Informatics, National Institute of Genetics, 1111 Yata, Mishima, Shizuoka, 411-8540, Japan
| | - Yu Kanesaki
- Research Institute of Green Science and Technology, Shizuoka University, 836 Oya, Suruga, Shizuoka, Shizuoka, 422-8529, Japan
| | - Hiroshi Katoh
- Advanced Science Research Promotion Center, Mie University, 1577 Kurima, Tsu, Mie, 514-8507, Japan
| | - Mitsunori Katayama
- College of Industrial Technology, Nihon University, 1-2-1 Izumi, Narashino, Chiba, 275-8575, Japan
| | - Haruyo Yamaguchi
- Biodiversity Division, National Institute for Environmental Studies, 16-1 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan
| | - Hirofumi Yoshikawa
- Department of Bioscience, Tokyo University of Agriculture, 1-1-1 Sakuragaoka, Setagaya, Tokyo, 156-8502, Japan
| | - Masahiko Ikeuchi
- Department of Life Sciences (Biology), The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo, Japan
| | - Toshihiko Eki
- Department of Applied Chemistry and Life Science, Toyohashi University of Technology, 1-1 Hibarigaoka, Tenpaku, Toyohashi, Aichi, 441-8580, Japan
| | - Yasukazu Nakamura
- Department of Informatics, National Institute of Genetics, 1111 Yata, Mishima, Shizuoka, 411-8540, Japan
| | - Masanobu Kawachi
- Biodiversity Division, National Institute for Environmental Studies, 16-1 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan
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17
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Park C, Takeuchi N. Unmasking photogranulation in decreasing glacial albedo and net autotrophic wastewater treatment. Environ Microbiol 2021; 23:6391-6404. [PMID: 34545673 PMCID: PMC9292683 DOI: 10.1111/1462-2920.15780] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/02/2021] [Revised: 09/13/2021] [Accepted: 09/16/2021] [Indexed: 11/29/2022]
Abstract
In both natural and built environments, microbes on occasions manifest in spherical aggregates instead of substratum‐affixed biofilms. These microbial aggregates are conventionally referred to as granules. Cryoconites are mineral rich granules that appear on glacier surfaces and are linked with expanding surface darkening, thus decreasing albedo, and enhanced melt. The oxygenic photogranules (OPGs) are organic rich granules that grow in wastewater, which enables wastewater treatment with photosynthetically produced oxygen and which presents potential for net autotrophic wastewater treatment in a compact system. Despite obvious differences inherent in the two, cryoconite and OPG pose striking resemblance. In both, the order Oscillatoriales in Cyanobacteria envelope inner materials and develop dense spheroidal aggregates. We explore the mechanism of photogranulation on account of high similarity between cryoconites and OPGs. We contend that there is no universal external cause for photogranulation. However, cryoconites and OPGs, as well as their intravariations, which are all under different stress fields, are the outcome of universal physiological processes of the Oscillatoriales interfacing with goldilocks interactions of stresses. Finding the rules of photogranulation may enhance engineering of glacier and wastewater systems to manipulate their ecosystem impacts.
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Affiliation(s)
- Chul Park
- Department of Civil and Environmental Engineering, University of Massachusetts Amherst, Amherst, Massachusetts, 01003, USA
| | - Nozomu Takeuchi
- Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, 263-8522, Japan
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18
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Spieck E, Wegen S, Keuter S. Relevance of Candidatus Nitrotoga for nitrite oxidation in technical nitrogen removal systems. Appl Microbiol Biotechnol 2021; 105:7123-7139. [PMID: 34508283 PMCID: PMC8494671 DOI: 10.1007/s00253-021-11487-5] [Citation(s) in RCA: 11] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/26/2021] [Revised: 07/29/2021] [Accepted: 07/31/2021] [Indexed: 01/10/2023]
Abstract
Abstract Many biotechnological applications deal with nitrification, one of the main steps of the global nitrogen cycle. The biological oxidation of ammonia to nitrite and further to nitrate is critical to avoid environmental damage and its functioning has to be retained even under adverse conditions. Bacteria performing the second reaction, oxidation of nitrite to nitrate, are fastidious microorganisms that are highly sensitive against disturbances. One important finding with relevance for nitrogen removal systems was the discovery of the mainly cold-adapted Cand. Nitrotoga, whose activity seems to be essential for the recovery of nitrite oxidation in wastewater treatment plants at low temperatures, e.g., during cold seasons. Several new strains of this genus have been recently described and ecophysiologically characterized including genome analyses. With increasing diversity, also mesophilic Cand. Nitrotoga representatives have been detected in activated sludge. This review summarizes the natural distribution and driving forces defining niche separation in artificial nitrification systems. Further critical aspects for the competition with Nitrospira and Nitrobacter are discussed. Knowledge about the physiological capacities and limits of Cand. Nitrotoga can help to define physico-chemical parameters for example in reactor systems that need to be run at low temperatures. Key points • Characterization of the psychrotolerant nitrite oxidizer Cand. Nitrotoga • Comparison of the physiological features of Cand. Nitrotoga with those of other NOB • Identification of beneficial environmental/operational parameters for proliferation Supplementary Information The online version contains supplementary material available at 10.1007/s00253-021-11487-5.
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Affiliation(s)
- Eva Spieck
- Department of Microbiology and Biotechnology, Universität Hamburg, Hamburg, Germany.
| | - Simone Wegen
- Department of Microbiology and Biotechnology, Universität Hamburg, Hamburg, Germany
| | - Sabine Keuter
- Department of Microbiology and Biotechnology, Universität Hamburg, Hamburg, Germany
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19
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Sagita R, Quax WJ, Haslinger K. Current State and Future Directions of Genetics and Genomics of Endophytic Fungi for Bioprospecting Efforts. Front Bioeng Biotechnol 2021; 9:649906. [PMID: 33791289 PMCID: PMC8005728 DOI: 10.3389/fbioe.2021.649906] [Citation(s) in RCA: 16] [Impact Index Per Article: 5.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/05/2021] [Accepted: 02/16/2021] [Indexed: 12/16/2022] Open
Abstract
The bioprospecting of secondary metabolites from endophytic fungi received great attention in the 1990s and 2000s, when the controversy around taxol production from Taxus spp. endophytes was at its height. Since then, hundreds of reports have described the isolation and characterization of putative secondary metabolites from endophytic fungi. However, only very few studies also report the genetic basis for these phenotypic observations. With low sequencing cost and fast sample turnaround, genetics- and genomics-based approaches have risen to become comprehensive approaches to study natural products from a wide-range of organisms, especially to elucidate underlying biosynthetic pathways. However, in the field of fungal endophyte biology, elucidation of biosynthetic pathways is still a major challenge. As a relatively poorly investigated group of microorganisms, even in the light of recent efforts to sequence more fungal genomes, such as the 1000 Fungal Genomes Project at the Joint Genome Institute (JGI), the basis for bioprospecting of enzymes and pathways from endophytic fungi is still rather slim. In this review we want to discuss the current approaches and tools used to associate phenotype and genotype to elucidate biosynthetic pathways of secondary metabolites in endophytic fungi through the lens of bioprospecting. This review will point out the reported successes and shortcomings, and discuss future directions in sampling, and genetics and genomics of endophytic fungi. Identifying responsible biosynthetic genes for the numerous secondary metabolites isolated from endophytic fungi opens the opportunity to explore the genetic potential of producer strains to discover novel secondary metabolites and enhance secondary metabolite production by metabolic engineering resulting in novel and more affordable medicines and food additives.
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Affiliation(s)
| | | | - Kristina Haslinger
- Groningen Institute of Pharmacy, Chemical and Pharmaceutical Biology, University of Groningen, Groningen, Netherlands
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