The PRP8 inteins in Cryptococcus are a source of phylogenetic and epidemiological information

Only two nuclear encoded inteins have been described. The first, SceVMA, was found in a vacuolar ATPase gene of Saccharomyces cerevisiae and related yeasts. The second, CnePRP8, was found in the PRP8 gene of Cryptococcus neoformans. CnePRP8 contains protein sequences associated with intein splicing but no endonuclease domain. We compared allelic mini-inteins in both varieties of C. neoformans (var. neoformans and var. grubii) and in the related primary pathogen C. gattii to study the evolution of both the mini-intein and the host. We also describe a full-length, endonuclease-containing intein in Cryptococcus laurentii, a moderately distant relation of C. neoformans. We did not detect an intein in the PRP8 gene of other species of Cryptococcus including species closely related to the C. neoformans/C. gattii group. It is therefore probable that the C. neoformans/C. gattii mini-intein was derived from horizontal transfer in which C. laurentii or another intein-containing species was the source.     

Causes of slowing‐down seasonal CO2 amplitude at Mauna Loa

Changing amplitude of the seasonal cycle of atmospheric CO₂ (SCA) in the northern hemisphere is an emerging carbon cycle property. Mauna Loa (MLO) station (20°N, 156°W), which has the longest continuous northern hemisphere CO₂ record, shows an increasing SCA before the 1980s (p < .01), followed by no significant change thereafter. We analyzed the potential driving factors of SCA slowing‐down, with an ensemble of dynamic global vegetation models (DGVMs) coupled with an atmospheric transport model. We found that slowing‐down of SCA at MLO is primarily explained by response of net biome productivity (NBP) to climate change, and by changes in atmospheric circulations. Through NBP, climate change increases SCA at MLO before the 1980s and decreases it afterwards. The effect of climate change on the slowing‐down of SCA at MLO is mainly exerted by intensified drought stress acting to offset the acceleration driven by CO₂ fertilization. This challenges the view that CO₂ fertilization is the dominant cause of emergent SCA trends at northern sites south of 40°N. The contribution of agricultural intensification on the deceleration of SCA at MLO was elusive according to land–atmosphere CO₂ flux estimated by DGVMs and atmospheric inversions. Our results also show the necessity to adequately account for changing circulation patterns in understanding carbon cycle dynamics observed from atmospheric observations and in using these observations to benchmark DGVMs.     

Chain elongation in the isoprenoid biosynthetic pathway

Isoprenyl diphosphate synthases catalyze addition of allylic diphosphate primers to the isoprene unit in isopentenyl diphosphate to produce polyisoprenoid diphosphates with well defined chain lengths. Phylogenetic correlations suggest that the synthases which catalyze formation of isoprenoid diphosphates with (E) double bonds have evolved from a common ancestor. X-ray crystallographic studies of farnesyl diphosphate synthase in conjunction with site-directed mutagenesis have provided important new information about the residues involved in binding and catalysis and the source of chain length selectivity for the enzymes that catalyze chain elongation.     

Potent nonpeptide vasopressin receptor antagonists based on oxazino- and thiazinobenzodiazepine templates

Vasopressin receptor antagonists can elicit ion-sparing diuretic effects (i.e., aquaresis) in vivo by blunting the action of the circulating hypophyseal hormone arginine vasopressin. We have identified two new series of basic tricyclic benzodiazepines, represented by general structure 1, which contain compounds that bind with high affinity to human V2 receptors. For example, (S)-(+)-8 and 5 are potent and selective V2 receptor antagonists with pronounced aquaretic activity in rats on oral administration.     

Salinity thresholds for understory plants in coastal wetlands

The effects of sea level rise and coastal saltwater intrusion on wetland plants can extend well above the high-tide line due to drought, hurricanes, and groundwater intrusion. Research has examined how coastal salt marsh plant communities respond to increased flooding and salinity, but more inland coastal systems have received less attention. The aim of this study was to identify whether ground layer plants exhibit threshold responses to salinity exposure. We used two vegetation surveys throughout the Albemarle-Pamlico Peninsula (APP) of North Carolina, USA to assess vegetation in a low elevation landscape (≤?3.8 m) experiencing high rates of sea level rise (3–4 mm/year). We examined the primary drivers of community composition change using Non-metric Multidimensional Scaling (NMDS) and used Threshold Indicator Taxa Analysis (TITAN) to detect thresholds of compositional change based on indicator taxa, in response to potential indicators of exposure to saltwater (Na, and the Σ Ca?+?Mg) and elevation. Salinity and elevation explained 64% of the variation in community composition, and we found two salinity thresholds for both soil Na⁺ (265 and 3843 g Na⁺/g) and Ca⁺ +?Mg⁺ (42 and 126 µeq/g) where major changes in community composition occur on the APP. Similar sets of species showed sensitivity to these different metrics of salt exposure. Overall, our results showed that ground layer plants can be used as reliable indicators of salinity thresholds in coastal wetlands. These results can be used for monitoring salt exposure of ecosystems and for identifying areas at risk for undergoing future community shifts.

     

Regional trends and drivers of the global methane budget

The ongoing development of the Global Carbon Project (GCP) global methane (CH₄) budget shows a continuation of increasing CH₄ emissions and CH₄ accumulation in the atmosphere during 2000–2017. Here, we decompose the global budget into 19 regions (18 land and 1 oceanic) and five key source sectors to spatially attribute the observed global trends. A comparison of top-down (TD) (atmospheric and transport model-based) and bottom-up (BU) (inventory- and process model-based) CH₄ emission estimates demonstrates robust temporal trends with CH₄ emissions increasing in 16 of the 19 regions. Five regions—China, Southeast Asia, USA, South Asia, and Brazil—account for >40% of the global total emissions (their anthropogenic and natural sources together totaling >270 Tg CH₄ yr^?1 in 2008–2017). Two of these regions, China and South Asia, emit predominantly anthropogenic emissions (>75%) and together emit more than 25% of global anthropogenic emissions. China and the Middle East show the largest increases in total emission rates over the 2000 to 2017 period with regional emissions increasing by >20%. In contrast, Europe and Korea and Japan show a steady decline in CH₄ emission rates, with total emissions decreasing by ~10% between 2000 and 2017. Coal mining, waste (predominantly solid waste disposal) and livestock (especially enteric fermentation) are dominant drivers of observed emissions increases while declines appear driven by a combination of waste and fossil emission reductions. As such, together these sectors present the greatest risks of further increasing the atmospheric CH₄ burden and the greatest opportunities for greenhouse gas abatement.     

Cloning and expression of IspDF from Mesorhizobium loti. Characterization of a bifunctional protein that catalyzes non-consecutive steps in the methylerythritol phosphate pathway

Gram-negative bacteria, plant chloroplasts, green algae and some Gram-positive bacteria utilize the 2-C-methyl-d-erythritol phosphate (MEP) pathway for the biosynthesis of isoprenoids. IspD, ispE, and ispF encode the enzymes required to convert MEP to 2-C-methyl-d-erythritol 2,4-cyclodiphosphate (cMEDP) during the biosynthesis of isopentenyl diphosphate and dimethylallyl diphosphate in the MEP pathway. Upon analysis of the Mesorhizobium loti genome, ORF mll0395 showed homology to both ispD and ispF and appeared to encode a fusion protein. M. loti ispE was located elsewhere on the chromosome. Purified recombinant IspDF protein was mostly a homodimer, MW approximately 46 kDa/subunit. Incubation of IspDF with MEP, CTP, and ATP gave 4-diphosphocytidyl-2-C-methyl-d-erythritol (CDP-ME) as the only product. When Escherichia coli IspE protein was added to the incubation mixture, cMEDP was formed. In addition, M. loti ORF mll0395 complements lethal disruptions in both ispD and ispF in Salmonella typhimurium. These results indicate that IspDF is a bifunctional protein, which catalyzes the first and third steps in the conversion of MEP to cMEDP.     

Differential regulation of corticotropin releasing factor 1alpha receptor endocytosis and trafficking by beta-arrestins and Rab GTPases

The corticotropin releasing factor (CRF) type 1alpha receptor, a member of the G protein-coupled receptor (GPCR) subfamily B, is involved in the aetiology of anxiety and depressive disorders. In the present study, we examined the internalization and trafficking of the CRF1alpha receptor in both human embryonic kidney (HEK)293 cells and primary cortical neurons. We found that CRF1alpha receptor activation leads to the selective recruitment of beta-arrestin2 in both HEK293 cells and neurons. We observed distinct distribution patterns of CRF1alpha receptor and beta-arrestin2 in HEK293 cells and cortical neurons. In HEK293 cells, beta-arrestin2-green fluorescent protein (GFP) co-localized with CRF1alpha receptor in vesicles at the plasma membrane but was dissociated from the receptor in endosomes. In contrast, in primary cortical neurons, beta-arrestin2 and CRF1alpha receptor were internalized in distinct endocytic vesicles. By bioluminescence resonance energy transfer, we demonstrated that beta-arrestin2 association with CRF1alpha receptor was increased in cells transfected with G protein-coupled receptor kinase (GRK)3 and GRK6 and decreased in cells transfected with GRK2 and GRK5. In both HEK293 cells and cortical neurons, internalized CRF1alpha receptor transited from Rab5-positive early endosomes to Rab4-positive recycling endosomes and was not targeted to lysosomes. However, CRF1alpha receptor resensitization was blocked by the overexpression of wild-type, but not dominant-negative, Rab5 and Rab4 GTPases. Taken together, our results suggest that beta-arrestin trafficking differs between HEK293 cells and neurons, and that CRF1alpha receptor resensitization is regulated in an atypical manner by Rab GTPases.     

Effects of site-directed mutagenesis of the highly conserved aspartate residues in domain II of farnesyl diphosphate synthase activity.

Comparison of the farnesyl diphosphate (FPP) synthase amino acid sequences from four species with amino acid sequences from the related enzymes hexaprenyl diphosphate synthase and geranylgeranyl diphosphate synthase show the presence of two aspartate rich highly conserved domains. The aspartate motif ((I, L, or V)XDDXXD) of the second of those domains has homology with at least 9 prenyl transfer enzymes that utilize an allylic prenyl diphosphate as one substrate. In order to investigate the role of this second aspartate-rich domain in rat FPP synthase, we mutated the first or third aspartate to glutamate, expressed the wild-type and mutant enzymes in Escherichia coli, and purified them to apparent homogeneity using a single chromatographic step. Approximately 12 mg of homogeneous protein was isolated from 120 mg of crude bacterial extract. The kinetic parameters of the purified wild-type recombinant FPP synthase containing the DDYLD motif were as follows: Vmax = 0.84 mumol/min/mg; GPP Km = 1.0 microM; isopentenyl diphosphate (IPP) Km = 2.7 microM. Substitution of glutamate for the first aspartate (EDYLD) decreased the Vmax by over 90-fold. The Km for IPP increased, whereas the Km for GPP remained the same in this D243E mutant. Substitution of glutamate for the third aspartate (DDYLE) did not result in altered enzyme kinetics in the D247E mutant. These results suggest that the first aspartate in the second domain is involved in the catalysis by FPP synthase.     

Modeled production,oxidation, and transport processes of wetland methane emissions in temperate,boreal, and Arctic regions

Wetlands are the largest natural source of methane (CH₄) to the atmosphere. The eddy covariance method provides robust measurements of net ecosystem exchange of CH₄, but interpreting its spatiotemporal variations is challenging due to the co-occurrence of CH₄ production, oxidation, and transport dynamics. Here, we estimate these three processes using a data-model fusion approach across 25 wetlands in temperate, boreal, and Arctic regions. Our data-constrained model—iPEACE—reasonably reproduced CH₄ emissions at 19 of the 25 sites with normalized root mean square error of 0.59, correlation coefficient of 0.82, and normalized standard deviation of 0.87. Among the three processes, CH₄ production appeared to be the most important process, followed by oxidation in explaining inter-site variations in CH₄ emissions. Based on a sensitivity analysis, CH₄ emissions were generally more sensitive to decreased water table than to increased gross primary productivity or soil temperature. For periods with leaf area index (LAI) of ≥20% of its annual peak, plant-mediated transport appeared to be the major pathway for CH₄ transport. Contributions from ebullition and diffusion were relatively high during low LAI (<20%) periods. The lag time between CH₄ production and CH₄ emissions tended to be short in fen sites (3 ± 2 days) and long in bog sites (13 ± 10 days). Based on a principal component analysis, we found that parameters for CH₄ production, plant-mediated transport, and diffusion through water explained 77% of the variance in the parameters across the 19 sites, highlighting the importance of these parameters for predicting wetland CH₄ emissions across biomes. These processes and associated parameters for CH₄ emissions among and within the wetlands provide useful insights for interpreting observed net CH₄ fluxes, estimating sensitivities to biophysical variables, and modeling global CH₄ fluxes.