Publications by authors named "Lena Rohe"

Article Synopsis
  • Nitrification, a crucial part of the nitrogen cycle, is mainly driven by ammonia-oxidizing microorganisms, particularly ammonia-oxidizing archaea (AOA), which have unique traits influencing their adaptations.
  • The study conducted comparative genomics on 39 AOA genomes, revealing the absence of typical ammonium transporters, suggesting distinctive physiological traits for AOA compared to other nitrifiers.
  • Findings indicate that AOA may utilize a different outer cell structure, providing insights into their ecological roles and adaptations in terrestrial ecosystems, and highlighting their significance in nitrogen cycling and environmental impacts like eutrophication and greenhouse gas emissions.
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Article Synopsis
  • Denitrification is an essential process in soil nitrogen cycling that primarily occurs in microbial hotspots around particulate organic matter (POM), affecting greenhouse gas emissions like dinitrogen and nitrous oxide.
  • To accurately predict these emissions, it's crucial to quantify the distribution of POM, as it influences local oxygen balance and microbial activity in soils.
  • Findings indicate that both proximal and distal POM contribute to greenhouse gas emissions, with distal POM significantly driving denitrification rates, particularly in grasslands, highlighting the intricate relationship between soil structure, organic carbon supply, and microbial activity.
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Nitrogen is an essential nutrient in the environment that exists in multiple oxidation states in nature. Numerous microbial processes are involved in its transformation. Knowledge about very complex N cycling has been growing rapidly in recent years, with new information about associated isotope effects and about the microbes involved in particular processes.

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Ammonia (NH) inhibition represents a major limitation to methane production during anaerobic digestion of organic material in biogas reactors. This process relies on co-operative metabolic interactions between diverse taxa at the community-scale. Despite this, most investigations have focused singularly on how methanogenic Archaea respond to NH stress.

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"Plastisphere", microbial communities colonizing plastic debris, has sparked global concern for marine ecosystems. Microbiome inhabiting this novel human-made niche has been increasingly characterized; however, whether the plastisphere holds crucial roles in biogeochemical cycling remains largely unknown. Here we evaluate the potential of plastisphere in biotic and abiotic denitrification and nitrous oxide (NO) production in estuaries.

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Nitrous oxide (NO) is a key climate change gas and nitrifying microbes living in terrestrial ecosystems contribute significantly to its formation. Many soils are acidic and global change will cause acidification of aquatic and terrestrial ecosystems, but the effect of decreasing pH on NO formation by nitrifiers is poorly understood. Here, we used isotope-ratio mass spectrometry to investigate the effect of acidification on production of NO by pure cultures of two ammonia-oxidizing archaea (AOA; Nitrosocosmicus oleophilus and Nitrosotenuis chungbukensis) and an ammonia-oxidizing bacterium (AOB; Nitrosomonas europaea).

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Rationale: Fungal denitrifiers can contribute substantially to N O emissions from arable soil and show a distinct site preference for N O (SP(N O)). This study sought to identify another process-specific isotopic tool to improve precise identification of N O of fungal origin by mass spectrometric analysis of the N O produced.

Methods: Three pure bacterial and three fungal species were incubated under denitrifying conditions in treatments with natural abundance and stable isotope labelling to analyse the N O produced.

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Rationale: The contribution of fungal denitrification to the emission of the greenhouse gas nitrous oxide (N2O) from soil has not yet been sufficiently investigated. The intramolecular (15)N site preference (SP) of N2O could provide a tool to distinguish between N2O produced by bacteria or fungi, since in previous studies fungi exhibited much higher SP values than bacteria.

Methods: To further constrain isotopic evidence of fungal denitrification, we incubated six soil fungal strains under denitrifying conditions, with either NO3(-) or NO2(-) as the electron acceptor, and measured the isotopic signature (δ(18)O, δ(15)Nbulk and SP values) of the N2O produced.

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Rationale: Fungi can contribute greatly to N2O production from denitrification. Therefore, it is important to quantify the isotopic signature of fungal N2O. The isotopic composition of N2O can be used to identify and analyze the processes of N2O production and N2O reduction.

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Rationale: An enhanced analytical approach for analyzing gaseous products from (15)N-enriched pools has been developed. This technique can be used to quantify nitrous oxide (N2O) and dinitrogen (N2) fluxes from denitrification. It can also help in distinguishing different N2- and N2O-forming processes, such as denitrification, nitrification, anaerobic ammonium oxidation or co-denitrification.

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Population-level effects of global warming result from concurrent direct and indirect processes. They are typically described by physiologically structured population models (PSPMs). Therefore, inverse modelling offers a tool to identify parameters of individual physiological processes through population-level data analysis, e.

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