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Glutamate transporters: a broad review of the most recent archaeal and human structures.
Pavić, A, Holmes, AOM, Postis, VLG, Goldman, A
Biochemical Society transactions. 2019;(4):1197-1207
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Abstract
Glutamate transporters play important roles in bacteria, archaea and eukaryotes. Their function in the mammalian central nervous system is essential for preventing excitotoxicity, and their dysregulation is implicated in many diseases, such as epilepsy and Alzheimer's. Elucidating their transport mechanism would further the understanding of these transporters and promote drug design as they provide compelling targets for understanding the pathophysiology of diseases and may have a direct role in the treatment of conditions involving glutamate excitotoxicity. This review outlines the insights into the transport cycle, uncoupled chloride conductance and modulation, as well as identifying areas that require further investigation.
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2.
In Search for the Membrane Regulators of Archaea.
Salvador-Castell, M, Tourte, M, Oger, PM
International journal of molecular sciences. 2019;(18)
Abstract
Membrane regulators such as sterols and hopanoids play a major role in the physiological and physicochemical adaptation of the different plasmic membranes in Eukarya and Bacteria. They are key to the functionalization and the spatialization of the membrane, and therefore indispensable for the cell cycle. No archaeon has been found to be able to synthesize sterols or hopanoids to date. They also lack homologs of the genes responsible for the synthesis of these membrane regulators. Due to their divergent membrane lipid composition, the question whether archaea require membrane regulators, and if so, what is their nature, remains open. In this review, we review evidence for the existence of membrane regulators in Archaea, and propose tentative location and biological functions. It is likely that no membrane regulator is shared by all archaea, but that they may use different polyterpenes, such as carotenoids, polyprenols, quinones and apolar polyisoprenoids, in response to specific stressors or physiological needs.
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Physiology and Distribution of Archaeal Methanotrophs That Couple Anaerobic Oxidation of Methane with Sulfate Reduction.
Bhattarai, S, Cassarini, C, Lens, PNL
Microbiology and molecular biology reviews : MMBR. 2019;(3)
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Abstract
In marine anaerobic environments, methane is oxidized where sulfate-rich seawater meets biogenic or thermogenic methane. In those niches, a few phylogenetically distinct microbial types, i.e., anaerobic methanotrophs (ANME), are able to grow through anaerobic oxidation of methane (AOM). Due to the relevance of methane in the global carbon cycle, ANME have drawn the attention of a broad scientific community for 4 decades. This review presents and discusses the microbiology and physiology of ANME up to the recent discoveries, revealing novel physiological types of anaerobic methane oxidizers which challenge the view of obligate syntrophy for AOM. An overview of the drivers shaping the distribution of ANME in different marine habitats, from cold seep sediments to hydrothermal vents, is given. Multivariate analyses of the abundance of ANME in various habitats identify a distribution of distinct ANME types driven by the mode of methane transport. Intriguingly, ANME have not yet been cultivated in pure culture, despite intense attempts. Further advances in understanding this microbial process are hampered by insufficient amounts of enriched cultures. This review discusses the advantages, limitations, and potential improvements for ANME laboratory-based cultivation systems.
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4.
Molecular underpinnings for microbial extracellular electron transfer during biogeochemical cycling of earth elements.
Jiang, Y, Shi, M, Shi, L
Science China. Life sciences. 2019;(10):1275-1286
Abstract
Microbial extracellular electron transfer (EET) is electron exchanges between the quinol/quinone pools in microbial cytoplasmic membrane and extracellular substrates. Microorganisms with EET capabilities are widespread in Earth hydrosphere, such as sediments of rivers, lakes and oceans, where they play crucial roles in biogeochemical cycling of key elements, including carbon, nitrogen, sulfur, iron and manganese. Over the past 12 years, significant progress has been made in mechanistic understanding of microbial EET at the molecular level. In this review, we focus on the molecular mechanisms underlying the microbial ability for extracellular redox transformation of iron, direct interspecies electron transfer as well as long distance electron transfer mediated by the cable bacteria in the hydrosphere.
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5.
Properties and Applications of Extremozymes from Deep-Sea Extremophilic Microorganisms: A Mini Review.
Jin, M, Gai, Y, Guo, X, Hou, Y, Zeng, R
Marine drugs. 2019;(12)
Abstract
The deep sea, which is defined as sea water below a depth of 1000 m, is one of the largest biomes on the Earth, and is recognised as an extreme environment due to its range of challenging physical parameters, such as pressure, salinity, temperature, chemicals and metals (such as hydrogen sulphide, copper and arsenic). For surviving in such extreme conditions, deep-sea extremophilic microorganisms employ a variety of adaptive strategies, such as the production of extremozymes, which exhibit outstanding thermal or cold adaptability, salt tolerance and/or pressure tolerance. Owing to their great stability, deep-sea extremozymes have numerous potential applications in a wide range of industries, such as the agricultural, food, chemical, pharmaceutical and biotechnological sectors. This enormous economic potential combined with recent advances in sampling and molecular and omics technologies has led to the emergence of research regarding deep-sea extremozymes and their primary applications in recent decades. In the present review, we introduced recent advances in research regarding deep-sea extremophiles and the enzymes they produce and discussed their potential industrial applications, with special emphasis on thermophilic, psychrophilic, halophilic and piezophilic enzymes.
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Sulfur metabolites in the pelagic ocean.
Moran, MA, Durham, BP
Nature reviews. Microbiology. 2019;(11):665-678
Abstract
Marine microorganisms play crucial roles in Earth's element cycles through the production and consumption of organic matter. One of the elements whose fate is governed by microbial activities is sulfur, an essential constituent of biomass and a crucial player in climate processes. With sulfur already being well studied in the ocean in its inorganic forms, organic sulfur compounds are emerging as important chemical links between marine phytoplankton and bacteria. The high concentration of inorganic sulfur in seawater, which can readily be reduced by phytoplankton, provides a freely available source of sulfur for biomolecule synthesis. Mechanisms such as exudation and cell lysis release these phytoplankton-derived sulfur metabolites into seawater, from which they are rapidly assimilated by marine bacteria and archaea. Energy-limited bacteria use scavenged sulfur metabolites as substrates or for the synthesis of vitamins, cofactors, signalling compounds and antibiotics. In this Review, we examine the current knowledge of sulfur metabolites released into and taken up from the marine dissolved organic matter pool by microorganisms, and the ecological links facilitated by their diversity in structures, oxidation states and chemistry.
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Metal-dependent anaerobic methane oxidation in marine sediment: Insights from marine settings and other systems.
Liang, L, Wang, Y, Sivan, O, Wang, F
Science China. Life sciences. 2019;(10):1287-1295
Abstract
Anaerobic oxidation of methane (AOM) plays a crucial role in controlling global methane emission. This is a microbial process that relies on the reduction of external electron acceptors such as sulfate, nitrate/nitrite, and transient metal ions. In marine settings, the dominant electron acceptor for AOM is sulfate, while other known electron acceptors are transient metal ions such as iron and manganese oxides. Despite the AOM process coupled with sulfate reduction being relatively well characterized, researches on metal-dependent AOM process are few, and no microorganism has to date been identified as being responsible for this reaction in natural marine environments. In this review, geochemical evidences of metal-dependent AOM from sediment cores in various marine environments are summarized. Studies have showed that iron and manganese are reduced in accordance with methane oxidation in seeps or diffusive profiles below the methanogenesis zone. The potential biochemical basis and mechanisms for metal-dependent AOM processes are here presented and discussed. Future research will shed light on the microbes involved in this process and also on the molecular basis of the electron transfer between these microbes and metals in natural marine environments.
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Bacteria, Fungi and Archaea Domains in Rhizospheric Soil and Their Effects in Enhancing Agricultural Productivity.
Odelade, KA, Babalola, OO
International journal of environmental research and public health. 2019;(20)
Abstract
The persistent and undiscriminating application of chemicals as means to improve crop growth, development and yields for several years has become problematic to agricultural sustainability because of the adverse effects these chemicals have on the produce, consumers and beneficial microbes in the ecosystem. Therefore, for agricultural productivity to be sustained there are needs for better and suitable preferences which would be friendly to the ecosystem. The use of microbial metabolites has become an attractive and more feasible preference because they are versatile, degradable and ecofriendly, unlike chemicals. In order to achieve this aim, it is then imperative to explore microbes that are very close to the root of a plant, especially where they are more concentrated and have efficient activities called the rhizosphere. Extensive varieties of bacteria, archaea, fungi and other microbes are found inhabiting the rhizosphere with various interactions with the plant host. Therefore, this review explores various beneficial microbes such as bacteria, fungi and archaea and their roles in the environment in terms of acquisition of nutrients for plants for the purposes of plant growth and health. It also discusses the effect of root exudate on the rhizosphere microbiome and compares the three domains at molecular levels.
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Characterization and Repurposing of Type I and Type II CRISPR-Cas Systems in Bacteria.
Hidalgo-Cantabrana, C, Goh, YJ, Barrangou, R
Journal of molecular biology. 2019;(1):21-33
Abstract
CRISPR-Cas systems constitute the adaptive immune system of bacteria and archaea, as a sequence-specific nucleic acid targeting defense mechanism. The sequence-specific recognition and cleavage of Cas effector complexes has been harnessed to developed CRISPR-based technologies and drive the genome editing revolution underway, due to their efficacy, efficiency, and ease of implementation in a broad range of organisms. CRISPR-based technologies offer a wide variety of opportunities in genome remodeling and transcriptional regulation, opening new avenues for therapeutic and biotechnological applications. To repurpose CRISPR-Cas systems for these applications, the various elements of the system need to be first identified and functionally characterized in their native host. Bioinformatic tools are first used to identify putative CRISPR arrays and their associated genes, followed by a comprehensive characterization of the CRISPR-Cas system, encompassing predictions for guide and target sequences. Subsequently, interference assays and transcriptomic analyses should be performed to probe the functionality of the CRISPR-Cas system. Once an endogenous CRISPR-Cas system is characterized as functional, they can be readily repurposed by delivering an engineered synthetic CRISPR array or a small RNA guide for targeted gene manipulation. Alternatively, developing a plasmid-based system for heterologous expression of the necessary CRISPR components can enable exploitation in other organisms. Altogether, there is a wide diversity of native CRISPR-Cas systems in many bacteria and most archaea that await functional characterization and repurposing for genome editing applications in prokaryotes.
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10.
Sulfur-dependent microbial lifestyles: deceptively flexible roles for biochemically versatile enzymes.
Crane, EJ
Current opinion in chemical biology. 2019;:139-145
Abstract
A wide group of microbes are able to "make a living" on Earth by basing their energetic metabolism on inorganic sulfur compounds. Because of their range of stable redox states, sulfur and inorganic sulfur compounds can be utilized as either oxidants or reductants in a diverse array of energy-conserving reactions. In this review the major enzymes and basic chemistry of sulfur-based respiration and chemolithotrophy are outlined. The reversibility and versatility of these enzymes, however, means that they can often be used in multiple ways, and several cases are discussed in which enzymes which are considered to be hallmarks of a particular respiratory or lithotrophic process have been found to be used in other, often opposing, metabolic processes. These results emphasize the importance of taking into account the geochemistry, biochemistry and microbiology of an organism and/or environment when trying to interpret the function of a particular sulfur-dependent redox enzyme.