Nitrogen loss by anaerobic oxidation of ammonium in rice rhizosphere

Anaerobic oxidation of ammonium (anammox) is recognized as an important process for nitrogen (N) cycling, yet its role in agricultural ecosystems, which are intensively fertilized, remains unclear. In this study, we investigated the presence, activity, functional gene abundance and role of anammox bacteria in rhizosphere and non-rhizosphere paddy soils using catalyzed reporter deposition–fluorescence in situ hybridization, isotope-tracing technique, quantitative PCR assay and 16S rRNA gene clone libraries. Results showed that rhizosphere anammox contributed to 31–41% N₂ production with activities of 0.33–0.64 nmol N₂ g⁻¹ soil h⁻¹, whereas the non-rhizosphere anammox bacteria contributed to only 2–3% N₂ production with lower activities of 0.08–0.26 nmol N₂ g⁻¹ soil h⁻¹. Higher anammox bacterial cells were observed (0.75–1.4 × 10⁷ copies g⁻¹ soil) in the rhizosphere, which were twofold higher compared with the non-rhizosphere soil (3.7–5.9 × 10⁶ copies g⁻¹ soil). Phylogenetic analysis of the anammox bacterial 16S rRNA genes indicated that two genera of ‘Candidatus Kuenenia'' and ‘Candidatus Brocadia'' and the family of Planctomycetaceae were identified. We suggest the rhizosphere provides a favorable niche for anammox bacteria, which are important to N cycling, but were previously largely overlooked.     

MAIR‐II deficiency ameliorates cardiac remodelling post‐myocardial infarction by suppressing TLR9‐mediated macrophage activation

Macrophages are fundamental components of inflammation in post‐myocardial infarction (MI) and contribute to adverse cardiac remodelling and heart failure. However, the regulatory mechanisms in macrophage activation have not been fully elucidated. Previous studies showed that myeloid‐associated immunoglobulin–like receptor II (MAIR‐II) is involved in inflammatory responses in macrophages. However, its role in MI is unknown. Thus, this study aimed to determine a novel role and mechanism of MAIR‐II in MI. We first identified that MAIR‐II–positive myeloid cells were abundant from post‐MI days 3 to 5 in infarcted hearts of C57BL/6J (WT) mice induced by permanent left coronary artery ligation. Compared to WT, MAIR‐II–deficient (Cd300c2 ^−/−) mice had longer survival, ameliorated cardiac remodelling, improved cardiac function and smaller infarct sizes. Moreover, we detected lower pro‐inflammatory cytokine and fibrotic gene expressions in Cd300c2 ^−/−‐infarcted hearts. These mice also had less infiltrating pro‐inflammatory macrophages following MI. To elucidate a novel molecular mechanism of MAIR‐II, we considered macrophage activation by Toll‐like receptor (TLR) 9–mediated inflammation. In vitro, we observed that Cd300c2 ^−/− bone marrow–derived macrophages stimulated by a TLR9 agonist expressed less pro‐inflammatory cytokines compared to WT. In conclusion, MAIR‐II may enhance inflammation via TLR9‐mediated macrophage activation in MI, leading to adverse cardiac remodelling and poor prognosis.     

LincRNA‐EPS impairs host antiviral immunity by antagonizing viral RNA–PKR interaction

LincRNA‐EPS is an important regulator in inflammation. However, the role of lincRNA‐EPS in the host response against viral infection is unexplored. Here, we show that lincRNA‐EPS is downregulated in macrophages infected with different viruses including VSV, SeV, and HSV‐1. Overexpression of lincRNA‐EPS facilitates viral infection, while deficiency of lincRNA‐EPS protects the host against viral infection in vitro and in vivo. LincRNA‐EPS ^−/− macrophages show elevated expression of antiviral interferon‐stimulated genes (ISGs) such as Mx1, Oas2, and Ifit2 at both basal and inducible levels. However, IFN‐β, the key upstream inducer of these ISGs, is downregulated in lincRNA‐EPS ^−/− macrophages compared with control cells. RNA pulldown and mass spectrometry results indicate that lincRNA‐EPS binds to PKR and antagonizes the viral RNA–PKR interaction. PKR activates STAT1 and induces antiviral ISGs independent of IFN‐I induction. LincRNA‐EPS inhibits PKR‐STAT1‐ISGs signaling and thus facilitates viral infection. Our study outlines an alternative antiviral pathway, with downregulation of lincRNA‐EPS promoting the induction of PKR‐STAT1‐dependent ISGs, and reveals a potential therapeutic target for viral infectious diseases.     

Lazy hazy days

Scientists have warned about the looming climate crisis for decades, but the world has been slow to act. Are we in danger of making a similar mistake, by neglecting the dangers of other climactic catastrophes? Subject Categories: Biotechnology & Synthetic Biology, Economics, Law & Politics, Evolution & Ecology

On one of my trips to Antarctica, I was enjoined to refer not to “global warming” or even to “climate change.” The former implies a uniform and rather benign process, while the second suggests just a transition from one state to another and seems to minimize all the attendant risks to survival. Neither of these terms adequately or accurately describes what is happening to our planet''s climate system as a result of greenhouse gas emissions; not to mention the effects of urbanization, intensive agriculture, deforestation, and other consequences of human population growth. Instead, I was encouraged to use the term “climate disruption,” which embraces the multiplicity of events taking place, some of them still hard to model, that are altering the planetary ecosystem in dramatic ways.With climate disruption now an urgent and undeniable reality, policymakers are finally waking up to the threats that scientists have been warning about for decades. They have accepted the need for action (UNFCCC Conference of the Parties, ²⁰²¹), even if the commitment remains patchy or lukewarm. But to implement all the necessary changes is a massive undertaking, and it is debatable whether we have enough time left. The fault lies mostly with those who resisted change for so long, hoping the problem would just go away, or denying that it was happening at all. The crisis situation that we face today is because the changes needed simply cannot be executed overnight. It will take time for the infrastructure to be put in place, whether for renewable electricity, for the switch to carbon‐neutral fuels, for sustainable agriculture and construction, and for net carbon capture. If the problems worsen, requiring even more drastic action, at least we do have a direction of travel, though we would be starting off from an even more precarious situation.However, given the time that it has taken—and will still take—to turn around the juggernaut of our industrial society, are we in danger of making the same mistakes all over again, by ignoring the risks of the very opposite process happening in our lifetime? The causes of historic climate cooling are still debated, and though we have fairly convincing evidence regarding specific, sudden events, there is no firm consensus on what is behind longer‐term and possibly cyclical changes in the climate.The two best‐documented examples are the catastrophe of 536–540 AD and the effects of the Laki Haze of 1783–1784. The cause of the 536–540 event is still debated, but is widely believed to have been one or more massive volcanic eruptions that created a global atmospheric dust‐cloud, resulting in a temperature drop of up to 2°C with concomitant famines and societal crises (Toohey et al, ²⁰¹⁶; Helama et al, ²⁰¹⁸). The Laki Haze was caused by the massive outpouring of sulfurous fumes from the Laki eruption in Iceland. Its effects on the climate, though just as immediate, were less straightforward. The emissions, combined with other meteorological anomalies, produced a disruption of the jetstream, as well as other localized effects. In northwest Europe, the first half of the summer of 1783 was exceptionally hot, but the following winters were dramatically cold, and the mean temperature across much of the northern hemisphere is estimated to have dropped by around 1.3°C for 2–3 years (Thordarson & Self, ²⁰⁰³). In Iceland itself, as well as much of western and northern Europe, the effects were even more devastating, with widespread crop failures and deaths of both livestock and humans exacerbated by the toxicity of the volcanic gases (Schmidt et al, ²⁰¹¹).Other volcanic events in recorded time have produced major climactic disturbances, such as the 1816 Tambora eruption in Indonesia, which resulted in “the year without a summer,” marked by temperature anomalies of up to 4°C (Fasullo et al, ²⁰¹⁷), again precipitating worldwide famine. The 1883 Krakatoa eruption produced similar disruption, albeit of a lesser magnitude, though the effects are proposed to have been much longer lasting (Gleckler et al, ²⁰⁰⁶).Much more scientifically challenging is the so‐called Little Ice Age in the Middle Ages, approximately from 1250 to 1700 AD, when global temperatures were significantly lower than in the preceding and following centuries. It was marked by particularly frigid and prolonged winters in the northern hemisphere. There is no strong consensus as to its cause(s) or even its exact dates; nor even that it can be considered a global‐scale event rather than a summation of several localized phenomena. A volcanic eruption in 1257 with similar effects to the one of 1816 has been suggested as an initiating event. Disruption of the oceanic circulation system resulting from prolonged anomalies in solar activity is another possible explanation (Lapointe & Bradley, ²⁰²¹). Nevertheless, and despite an average global cooling of < 1°C, the effects on global agriculture, settlement, migration and trade, pandemics such as the Black Death and perhaps even wars and revolutions, were profound.Once or twice in the past century, we have faced devastating wars, tsunamis and pandemics that seemed to come out of the blue and exacted massive tolls on humanity. From the most recent of each of these, there is a growing realization that, although these events are rare and poorly predictable, we can greatly limit the damage if we prepare properly. Devoting a small proportion of our resources over time, we can build the infrastructure and the mechanisms to cope, when these disasters do eventually strike.Without abandoning any of the emergency measures to combat anthropogenic warming, I believe that the risk of climate cooling needs to be addressed in the same way. The infrastructure for burning fossil fuels needs to be mothballed, not destroyed. Carbon capture needs to be implemented in a way that is rapidly reversible, if this should ever be needed. Alternative transportation routes need to be planned and built in case existing ones become impassable due to ice or flooding. Properly insulated buildings are not just a way of saving energy. They are essential for survival in extreme cold, as those of us who live in the Arctic countries are well aware—but many other regions also experience severe winters, for which we should all prepare.Biotechnology needs to be set to work to devise ways of mitigating the effects of sudden climactic events such as the Laki Haze or the Tambora and Krakatoa eruptions, as well as longer‐term phenomena like the Little Ice Age. Could bacteria be used, for example, to detoxify and dissipate a sulfuric aerosol such as the one generated by the Laki eruption? Methane is generally regarded as a major contributor to the greenhouse effect, but it is short‐lived in the atmosphere. So, could methanogens somehow be harnessed to bring about a temporary rise in global temperatures to offset short‐term cooling effects of a volcanic dust‐cloud?We already have a global seed bank in Svalbard (Asdal & Guarino, ²⁰¹⁸): It might easily be expanded to include a greater representation of cold‐resistant varieties of the world''s crop plants that might one day be vital to human survival. And, the experience of the Laki Haze indicates a need for varieties capable of withstanding acid rains and other volcanic pollutants, as well as drought and water saturation. An equivalent (embryo) bank for strains of agriculturally important animals potentially threatened by the effects of abrupt cooling of the climate or catastrophic toxification of the atmosphere is also worth considering.It has generally been thought impractical and pointless to prepare for even rarer events, such as cometary impacts, but events that have occurred repeatedly in recorded history and over an even longer time scale (Helama et al, ²⁰²¹) are likely to happen again. We should and can be better prepared. This is not to say that we should pay attention to every conspiracy theorist or crank, or paid advocates for energy corporations that seek short‐term profits at the expense of long‐term survival, but the dangers of climate disruption of all kinds are too great to ignore. Instead of our current rather one‐dimensional thinking, we need an “all‐risks” approach to the subject: learning from the past and the present to prepare for the future.     

Attenuation of SARS‐CoV‐2 replication and associated inflammation by concomitant targeting of viral and host cap 2'‐O‐ribose methyltransferases

The SARS‐CoV‐2 infection cycle is a multistage process that relies on functional interactions between the host and the pathogen. Here, we repurposed antiviral drugs against both viral and host enzymes to pharmaceutically block methylation of the viral RNA 2''‐O‐ribose cap needed for viral immune escape. We find that the host cap 2''‐O‐ribose methyltransferase MTr1 can compensate for loss of viral NSP16 methyltransferase in facilitating virus replication. Concomitant inhibition of MTr1 and NSP16 efficiently suppresses SARS‐CoV‐2 replication. Using in silico target‐based drug screening, we identify a bispecific MTr1/NSP16 inhibitor with anti‐SARS‐CoV‐2 activity in vitro and in vivo but with unfavorable side effects. We further show antiviral activity of inhibitors that target independent stages of the host SAM cycle providing the methyltransferase co‐substrate. In particular, the adenosylhomocysteinase (AHCY) inhibitor DZNep is antiviral in in vitro, in ex vivo, and in a mouse infection model and synergizes with existing COVID‐19 treatments. Moreover, DZNep exhibits a strong immunomodulatory effect curbing infection‐induced hyperinflammation and reduces lung fibrosis markers ex vivo. Thus, multispecific and metabolic MTase inhibitors constitute yet unexplored treatment options against COVID‐19.     

Corals shed bacteria as a potential mechanism of resilience to organic matter enrichment

Understanding the mechanisms of resilience of coral reefs to anthropogenic stressors is a critical step toward mitigating their current global decline. Coral–bacteria associations are fundamental to reef health and disease, but direct observations of these interactions remain largely unexplored. Here, we use novel technology, high-speed laser scanning confocal microscopy on live coral (Pocillopora damicornis), to test the hypothesis that corals exert control over the abundance of their associated bacterial communities by releasing (‘shedding'') bacteria from their surface, and that this mechanism can counteract bacterial growth stimulated by organic inputs. We also test the hypothesis that the coral pathogen Vibrio coralliilyticus can evade such a defense mechanism. This first report of direct observation with high-speed confocal microscopy of living coral and its associated bacterial community revealed a layer (3.3–146.8 μm thick) on the coral surface where bacteria were concentrated. The results of two independent experiments showed that the bacterial abundance in this layer was not sensitive to enrichment (5 mg l⁻¹ peptone), and that coral fragments exposed to enrichment released significantly more bacteria from their surfaces than control corals (P<0.01; 35.9±1.4 × 10⁵ cells cm⁻² coral versus 1.3±0.5 × 10⁵ cells cm⁻² coral). Our results provide direct support to the hypothesis that shedding bacteria may be an important mechanism by which coral-associated bacterial abundances are regulated under organic matter stress. Additionally, the novel ability to watch this ecological behavior in real-time at the microscale opens an unexplored avenue for mechanistic studies of coral–microbe interactions.     

Coumarins effectively inhibit bacterial α-carbonic anhydrases

Coumarins are known to act as prodrug inhibitors of mammalian α-carbonic anhydrases (CAs, EC 4.2.1.1) but they were not yet investigated for the inhibition of bacterial α-CAs. Here we demonstrate that such enzymes from the bacterial pathogens Neisseria gonorrhoeae (NgCAα) and Vibrio cholerae (VchCAα) are inhibited by a panel of simple coumarins incorporating hydroxyl, amino, ketone or carboxylic acid ester moieties in various positions of the ring system. The nature and the position of the substituents in the coumarin ring were the factors which strongly influenced inhibitory efficacy. NgCAα was inhibited with K_Is in the range of 28.6–469.5 µM, whereas VchCAα with K_Is in the range of 39.8–438.7 µM. The two human (h)CA isoforms included for comparison reason in the study, hCA I and II, were less prone to inhibition by these compounds, with K_Is of 137–948.9 µM for hCA I and of 296.5–961.2 µM for hCA II, respectively. These findings are relevant for discovering coumarin bacterial CA inhibitors with selectivity for the bacterial over human isoform, with potential applications as novel antibacterial agents.     

Engineering defensin α‐helix to produce high‐affinity SARS‐CoV‐2 spike protein binding ligands

The binding of severe acute respiratory syndrome coronavirus 2 (SARS‐CoV‐2) spike protein to the angiotensin‐converting enzyme 2 (ACE2) receptor expressed on the host cells is a critical initial step for viral infection. This interaction is blocked through competitive inhibition by soluble ACE2 protein. Therefore, developing high‐affinity and cost‐effective ACE2 mimetic ligands that disrupt this protein–protein interaction is a promising strategy for viral diagnostics and therapy. We employed human and plant defensins, a class of small (2–5 kDa) and highly stable proteins containing solvent‐exposed alpha‐helix, conformationally constrained by two disulfide bonds. Therefore, we engineered the amino acid residues on the constrained alpha‐helix of defensins to mimic the critical residues on the ACE2 helix 1 that interact with the SARS‐CoV‐2 spike protein. The engineered proteins (h‐deface2, p‐deface2, and p‐deface2‐MUT) were soluble and purified to homogeneity with a high yield from a bacterial expression system. The proteins demonstrated exceptional thermostability (Tm 70.7°C), high‐affinity binding to the spike protein with apparent K _d values of 54.4 ± 11.3, 33.5 ± 8.2, and 14.4 ± 3.5 nM for h‐deface2, p‐deface2, and p‐deface2‐MUT, respectively, and were used in a diagnostic assay that detected SARS‐CoV‐2 neutralizing antibodies. This work addresses the challenge of developing helical ACE2 mimetics by demonstrating that defensins provide promising scaffolds to engineer alpha‐helices in a constrained form for designing of high‐affinity ligands.     

Soil minerals affect taxon-specific bacterial growth

Secondary minerals (clays and metal oxides) are important components of the soil matrix. Clay minerals affect soil carbon persistence and cycling, and they also select for distinct microbial communities. Here we show that soil mineral assemblages—particularly short-range order minerals—affect both bacterial community composition and taxon-specific growth. Three soils with different parent material and presence of short-range order minerals were collected from ecosystems with similar vegetation and climate. These three soils were provided with ¹⁸O-labeled water and incubated with or without artificial root exudates or pine needle litter. Quantitative stable isotope probing was used to determine taxon-specific growth. We found that the growth of bacteria varied among soils of different mineral assemblages but found the trend of growth suppression in the presence of short-range order minerals. Relative growth of bacteria declined with increasing concentration of short-range order minerals between 25–36% of taxa present in all soils. Carbon addition in the form of plant litter or root exudates weakly affected relative growth of taxa (p = 0.09) compared to the soil type (p < 0.01). However, both exudate and litter carbon stimulated growth for at least 34% of families in the soils with the most and least short-range order minerals. In the intermediate short-range order soil, fresh carbon reduced growth for more bacterial families than were stimulated. These results highlight how bacterial-mineral-substrate interactions are critical to soil organic carbon processing, and how growth variation in bacterial taxa in these interactions may contribute to soil carbon persistence and loss.Subject terms: Biogeochemistry, Microbial ecology, Biogeochemistry     

Phospholipase D1 promotes cervical cancer progression by activating the RAS pathway

This study aimed to further investigate the effect of PLD1 on the biological characteristics of human cervical cancer (CC) cell line, CASKI and the potential related molecular mechanism. CRISPR/Cas9 genome editing technology was used to knock out the PLD1 gene in CASKI cells. Cell function assays were performed to evaluate the effect of PLD1 on the biological function of CASKI cells in vivo and in vitro. A PLD1‐overexpression rescue experiment in these knockout cells was performed to further confirm its function. Two PLD1‐knockout CASKI cell lines (named PC‐11 and PC‐40, which carried the ins1/del4 mutation and del1/del2/ins1 mutation, respectively), were constructed by CRISPR/Cas9. PLD1 was overexpressed in these knockout cells (named PC11‐PLD1 and PC40‐PLD1 cells), which rescued the expression of PLD1 by approximately 71.33% and 74.54%, respectively. In vivo, the cell function assay results revealed that compared with wild‐type (WT)‐CASKI cells, the ability of PC‐11 and PC‐40 cells to proliferate, invade and migrate was significantly inhibited. The expression of H‐Ras and phosphorylation of Erk1/2 (p‐Erk1/2) was decreased in PC‐11 and PC‐40 cells compared with WT‐CASKI cells. PC‐11 and PC‐40 cells could sensitize CASKI cells to cisplatin. More importantly, the proliferation, migration and invasion of PC11‐PLD1 and PC40‐PLD1 cells with PLD1 overexpression were significantly improved compared with those of the two types of PLD1 knockout cells. The sensitivity to cisplatin was decreased in PC11‐PLD1 and PC40‐PLD1 cells compared with PC‐11 and PC‐40 cells. In vivo, in the PC‐11 and PC‐40 tumour groups, tumour growth was significantly inhibited and tumour weight (0.95 ± 0.27 g and 0.66 ± 0.43 g vs. 1.59 ± 0.67 g, p = 0.0313 and 0.0108) and volume (1069.41 ± 393.84 and 1077.72 mm³ ± 815.07 vs. 2142.94 ± 577.37 mm³, p = 0.0153 and 0.0128) were significantly reduced compared to those in the WT‐CASKI group. Tumour differentiation of the PC‐11 and PC40 cells was significantly better than that of the WT‐CASKI cells. The immunohistochemistry results confirmed that the expression of H‐Ras and p‐Erk1/2 was decreased in PC‐11 and PC‐40 tumour tissues compared with WT‐CASKI tumour tissues. PLD1 promotes CC progression by activating the RAS pathway. Inhibition of PLD1 may serve as an attractive therapeutic modality for CC.     

Macrofauna regulate heterotrophic bacterial carbon and nitrogen incorporation in low-oxygen sediments

Oxygen minimum zones (OMZs) currently impinge upon >1 million km² of sea floor and are predicted to expand with climate change. We investigated how changes in oxygen availability, macrofaunal biomass and retention of labile organic matter (OM) regulate heterotrophic bacterial C and N incorporation in the sediments of the OMZ-impacted Indian continental margin (540–1100 m; [O₂]=0.35–15 μmol l⁻¹). In situ pulse-chase experiments traced ¹³C:¹⁵N-labelled phytodetritus into bulk sediment OM and hydrolysable amino acids, including the bacterial biomarker 𝒟-alanine. Where oxygen availability was lowest ([O₂]=0.35 μmol l⁻¹), metazoan macrofauna were absent and bacteria assimilated 30–90% of the labelled phytodetritus within the sediment. At higher oxygen levels ([O₂]=2–15 μmol l⁻¹) the macrofaunal presence and lower phytodetritus retention with the sediment occur concomitantly, and bacterial phytodetrital incorporation was reduced and retarded. Bacterial C and N incorporation exhibited a significant negative relationship with macrofaunal biomass across the OMZ. We hypothesise that fauna–bacterial interactions significantly influence OM recycling in low-oxygen sediments and need to be considered when assessing the consequences of global change on biogeochemical cycles.     

Characterization of the glutathione‐dependent reduction of the peroxiredoxin 5 homolog PfAOP from Plasmodium falciparum

Peroxiredoxins use a variety of thiols to rapidly reduce hydroperoxides and peroxynitrite. While the oxidation kinetics of peroxiredoxins have been studied in great detail, enzyme‐specific differences regarding peroxiredoxin reduction and the overall rate‐limiting step under physiological conditions often remain to be deciphered. The 1‐Cys peroxiredoxin 5 homolog PfAOP from the malaria parasite Plasmodium falciparum is an established model enzyme for glutathione/glutaredoxin‐dependent peroxiredoxins. Here, we reconstituted the catalytic cycle of PfAOP in vitro and analyzed the reaction between oxidized PfAOP and reduced glutathione (GSH) using molecular docking and stopped‐flow measurements. Molecular docking revealed that oxidized PfAOP has to adopt a locally unfolded conformation to react with GSH. Furthermore, we determined a second‐order rate constant of 6 × 10⁵ M⁻¹ s⁻¹ at 25°C and thermodynamic activation parameters ΔH ^‡, ΔS ^‡, and ΔG ^‡ of 39.8 kJ/mol, −0.8 J/mol, and 40.0 kJ/mol, respectively. The gain‐of‐function mutant PfAOP^L109M had almost identical reaction parameters. Taking into account physiological hydroperoxide and GSH concentrations, we suggest (a) that the reaction between oxidized PfAOP and GSH might be even faster than the formation of the sulfenic acid in vivo, and (b) that conformational changes are likely rate limiting for PfAOP catalysis. In summary, we characterized and quantified the reaction between GSH and the model enzyme PfAOP, thus providing detailed insights regarding the reactivity of its sulfenic acid and the versatile chemistry of peroxiredoxins.     

Structural analyses of the malaria parasite aminoacyl‐tRNA synthetases provide new avenues for antimalarial drug discovery

Malaria is a parasitic illness caused by the genus Plasmodium from the apicomplexan phylum. Five plasmodial species of P. falciparum (Pf), P. knowlesi, P. malariae, P. ovale, and P. vivax (Pv) are responsible for causing malaria in humans. According to the World Malaria Report 2020, there were 229 million cases and ~ 0.04 million deaths of which 67% were in children below 5 years of age. While more than 3 billion people are at risk of malaria infection globally, antimalarial drugs are their only option for treatment. Antimalarial drug resistance keeps arising periodically and thus threatens the main line of malaria treatment, emphasizing the need to find new alternatives. The availability of whole genomes of P. falciparum and P. vivax has allowed targeting their unexplored plasmodial enzymes for inhibitor development with a focus on multistage targets that are crucial for parasite viability in both the blood and liver stages. Over the past decades, aminoacyl‐tRNA synthetases (aaRSs) have been explored as anti‐bacterial and anti‐fungal drug targets, and more recently (since 2009) aaRSs are also the focus of antimalarial drug targeting. Here, we dissect the structure‐based knowledge of the most advanced three aaRSs—lysyl‐ (KRS), prolyl‐ (PRS), and phenylalanyl‐ (FRS) synthetases in terms of development of antimalarial drugs. These examples showcase the promising potential of this family of enzymes to provide druggable targets that stall protein synthesis upon inhibition and thereby kill malaria parasites selectively.     

Gradients in microbial methanol uptake: productive coastal upwelling waters to oligotrophic gyres in the Atlantic Ocean

Methanol biogeochemistry and its importance as a carbon source in seawater is relatively unexplored. We report the first microbial methanol carbon assimilation rates (k) in productive coastal upwelling waters of up to 0.117±0.002 d⁻¹ (∼10 nmol l⁻¹d⁻¹). On average, coastal upwelling waters were 11 times greater than open ocean northern temperate (NT) waters, eight times greater than gyre waters and four times greater than equatorial upwelling (EU) waters; suggesting that all upwelling waters upon reaching the surface (⩽20 m), contain a microbial population that uses a relatively high amount of carbon (0.3–10 nmol l⁻¹d⁻¹), derived from methanol, to support their growth. In open ocean Atlantic regions, microbial uptake of methanol into biomass was significantly lower, ranging between 0.04–0.68 nmol l⁻¹d⁻¹. Microbes in the Mauritanian coastal upwelling used up to 57% of the total methanol for assimilation of the carbon into cells, compared with an average of 12% in the EU, and 1% in NT and gyre waters. Several methylotrophic bacterial species were identified from open ocean Atlantic waters using PCR amplification of mxaF encoding methanol dehydrogenase, the key enzyme in bacterial methanol oxidation. These included Methylophaga sp., Burkholderiales sp., Methylococcaceae sp., Ancylobacter aquaticus, Paracoccus denitrificans, Methylophilus methylotrophus, Methylobacterium oryzae, Hyphomicrobium sp. and Methylosulfonomonas methylovora. Statistically significant correlations for upwelling waters between methanol uptake into cells and both chlorophyll a concentrations and methanol oxidation rates suggest that remotely sensed chlorophyll a images, in these productive areas, could be used to derive total methanol biological loss rates, a useful tool for atmospheric and marine climatically active gas modellers, and air–sea exchange scientists.     

Targeted enzyme prodrug therapy for metastatic prostate cancer – a comparative study of L-methioninase,purine nucleoside phosphorylase,and cytosine deaminase

Background

Enzyme prodrug therapy shows promise for the treatment of solid tumors, but current approaches lack effective/safe delivery strategies. To address this, we previously developed three enzyme-containing fusion proteins targeted via annexin V to phosphatidylserine exposed on the tumor vasculature and tumor cells, using the enzymes L-methioninase, purine nucleoside phosphorylase, or cytosine deaminase. In enzyme prodrug therapy, the fusion protein is allowed to bind to the tumor before a nontoxic drug precursor, a prodrug, is introduced. Upon interaction of the prodrug with the bound enzyme, an anticancer compound is formed, but only in the direct vicinity of the tumor, thereby mitigating the risk of side effects while creating high intratumoral drug concentrations. The applicability of these enzyme prodrug systems to treating prostate cancer has remained unexplored. Additionally, target availability may increase with the addition of low dose docetaxel treatment to the enzyme prodrug treatment, but this effect has not been previously investigated. To this end, we examined the binding strength and the cytotoxic efficacy (with and without docetaxel treatment) of these enzyme prodrug systems on the human prostate cancer cell line PC-3.

Results

All three fusion proteins exhibited strong binding; dissociation constants were 0.572 nM for L-methioninase-annexin V (MT-AV), 0.406 nM for purine nucleoside phosphorylase-annexin V (PNP-AV), and 0.061 nM for cytosine deaminase-annexin V (CD-AV). MT-AV produced up to 99% cell death (p < 0.001) with limited cytotoxicity of the prodrug alone. PNP-AV with docetaxel created up to 78% cell death (p < 0.001) with no cytotoxicity of the prodrug alone. CD-AV with docetaxel displayed up to 60% cell death (p < 0.001) with no cytotoxicity of the prodrug alone. Docetaxel treatment created significant increases in cytotoxicity for PNP-AV and CD-AV.

Conclusions

Strong binding of fusion proteins to the prostate cancer cells and effective cell killing suggest that the enzyme prodrug systems with MT-AV and PNP-AV may be effective treatment options. Additionally, low-dose docetaxel treatment was found to increase the cytotoxic effect of the annexin V-targeted therapeutics for the PNP-AV and CD-AV systems.     

Typha for paludiculture—Suitable water table and nutrient conditions for potential biomass utilization explored in mesocosm gradient experiments

Drainage has turned 650,000 km² of peatlands worldwide into greenhouse gas sources. To counteract climate change, large‐scale rewetting is necessary while agricultural use of rewetted areas, termed paludiculture, is still possible. However, more information is required on the performance of suitable species, such as cattail, in the range of environmental conditions after rewetting. We investigated productivity and biomass quality (morphological traits and tissue chemical composition) of Typha angustifolia and Typha latifolia along gradients of water table depth (−45 to +40 cm) and nutrient addition (3.6–400 kg N ha⁻¹ a⁻¹) in a six‐month mesocosm experiment with an emphasis on their high‐value utilization, e.g., as building material, paper, or biodegradable packaging. Over a wide range of investigated conditions, T. latifolia was more productive than T. angustifolia. Productivity was remarkably tolerant of low nutrient addition, suggesting that long‐term productive paludiculture is possible. Low water tables were beneficial for T. latifolia productivity and high water tables for T. angustifolia biomass quality. Rewetting will likely create a mosaic of different water table depths. Our findings that the yield of T. angustifolia and tissue chemical composition of T. latifolia were largely unaffected by water table depth are therefore promising. Depending on intended utilization, optimal cultivation conditions and preferable species differ. Considering yield or diameter, e.g., for building materials, T. latifolia is generally preferable over T. angustifolia. A low N, P, K content, high Si content and high C/N‐ratio can be beneficial for processing into disposable tableware, charcoal, or building material. For these utilizations, T. angustifolia is preferable at high water tables, and both species should be cultivated at a low nutrient supply. When cellulose and lignin contents are relevant, e.g., for paper and biodegradable packaging, T. angustifolia is preferable at high water tables and both species should be cultivated at nutrient additions of about 20 kg N ha⁻¹ a⁻¹.     

Transition metal cation inhibition of Mycobacterium tuberculosis esterase RV0045C

Mycobacterium tuberculosis virulence is highly metal‐dependent with metal availability modulating the shift from the dormant to active states of M. tuberculosis infection. Rv0045c from M. tuberculosis is a proposed metabolic serine hydrolase whose folded stability is dependent on divalent metal concentration. Herein, we measured the divalent metal inhibition profile of the enzymatic activity of Rv0045c and found specific divalent transition metal cations (Cu²⁺ ≥ Zn²⁺ > Ni²⁺ > Co²⁺) strongly inhibited its enzymatic activity. The metal cations bind allosterically, largely affecting values for k _cat rather than K _M. Removal of the artificial N‐terminal 6xHis‐tag did not change the metal‐dependent inhibition, indicating that the allosteric inhibition site is native to Rv0045c. To isolate the site of this allosteric regulation in Rv0045c, the structures of Rv0045c were determined at 1.8 Å and 2.0 Å resolution in the presence and absence of Zn²⁺ with each structure containing a previously unresolved dynamic loop spanning the binding pocket. Through the combination of structural analysis with and without zinc and targeted mutagenesis, this metal‐dependent inhibition was traced to multiple chelating residues (H202A/E204A) on a flexible loop, suggesting dynamic allosteric regulation of Rv0045c by divalent metals. Although serine hydrolases like Rv0045c are a large and diverse enzyme superfamily, this is the first structural confirmation of allosteric regulation of their enzymatic activity by divalent metals.     

Designed leucine‐rich repeat proteins bind two muramyl dipeptide ligands

Designed protein receptors hold diagnostic and therapeutic promise. We now report the design of five consensus leucine‐rich repeat proteins (CLRR4–8) based on the LRR domain of nucleotide‐binding oligomerization domain (NOD)‐like receptors involved in the innate immune system. The CLRRs bind muramyl dipeptide (MDP), a bacterial cell wall component, with micromolar affinity. The overall K _{d app} values ranged from 1.0 to 57 μM as measured by fluorescence quenching experiments. Biphasic fluorescence quenching curves were observed in all CLRRs, with higher affinity K _d1 values ranging from 0.04 to 4.5 μM, and lower affinity K _d2 values ranging from 3.1 to 227 μM. These biphasic binding curves, along with the docking studies of MDP binding to CLRR4, suggest that at least two MDPs bind to each protein. Previously, only single MDP binding was reported. This high‐capacity binding of MDP promises small, soluble, stable CLRR scaffolds as candidates for the future design of pathogen biosensors.     

Negative interactions determine Clostridioides difficile growth in synthetic human gut communities

Understanding the principles of colonization resistance of the gut microbiome to the pathogen Clostridioides difficile will enable the design of defined bacterial therapeutics. We investigate the ecological principles of community resistance to C. difficile using a synthetic human gut microbiome. Using a dynamic computational model, we demonstrate that C. difficile receives the largest number and magnitude of incoming negative interactions. Our results show that C. difficile is in a unique class of species that display a strong negative dependence between growth and species richness. We identify molecular mechanisms of inhibition including acidification of the environment and competition over resources. We demonstrate that Clostridium hiranonis strongly inhibits C. difficile partially via resource competition. Increasing the initial density of C. difficile can increase its abundance in the assembled community, but community context determines the maximum achievable C. difficile abundance. Our work suggests that the C. difficile inhibitory potential of defined bacterial therapeutics can be optimized by designing communities featuring a combination of mechanisms including species richness, environment acidification, and resource competition.