RESUMEN
Aerobic anoxygenic phototrophic bacteria (AAPB) contribute profoundly to the global carbon cycle. However, most AAPB in marine environments are uncultured and at low abundance, hampering the recognition of their functions and molecular mechanisms. In this study, we developed a new culture-independent method to identify and sort AAPB using single-cell Raman/fluorescence spectroscopy. Characteristic Raman and fluorescent bands specific to bacteriochlorophyll a (Bchl a) in AAPB were determined by comparing multiple known AAPB with non-AAPB isolates. Using these spectroscopic biomarkers, AAPB in coastal seawater, pelagic seawater, and hydrothermal sediment samples were screened, sorted, and sequenced. 16S rRNA gene analysis and functional gene annotations of sorted cells revealed novel AAPB members and functional genes, including one species belonging to the genus Sphingomonas, two genera affiliated to classes Betaproteobacteria and Gammaproteobacteria, and function genes bchCDIX, pucC2, and pufL related to Bchl a biosynthesis and photosynthetic reaction center assembly. Metagenome-assembled genomes (MAGs) of sorted cells from pelagic seawater and deep-sea hydrothermal sediment belonged to Erythrobacter sanguineus that was considered as an AAPB and genus Sphingomonas, respectively. Moreover, multiple photosynthesis-related genes were annotated in both MAGs, and comparative genomic analysis revealed several exclusive genes involved in amino acid and inorganic ion metabolism and transport. This study employed a new single-cell spectroscopy method to detect AAPB, not only broadening the taxonomic and genetic contents of AAPB in marine environments but also revealing their genetic mechanisms at the single-genomic level.
Asunto(s)
Metagenómica , Agua de Mar , Metagenómica/métodos , Agua de Mar/microbiología , ARN Ribosómico 16S/genética , Espectrometría Raman , Filogenia , Análisis de la Célula IndividualRESUMEN
During summer, plants often experience increased light inputs and high temperatures, two major environmental factors with contrasting effects on thermomorphological traits. The integration of light and temperature signaling to control thermomorphogenesis in plants is critical for their acclimation in such conditions, but the underlying mechanisms remain largely unclear. We found that heat shock transcription factor 1d (HSFA1d) and its homologs are necessary for plant thermomorphogenesis during the day. In response to warm daytime temperature, HSFA1s markedly accumulate and move into the nucleus where they interact with phytochrome-interacting factor 4 (PIF4) and stabilize PIF4 by interfering with phytochrome B-PIF4 interaction. Moreover, we found that the HSFA1d nuclear localization under warm daytime temperature is mediated by constitutive photomorphogenic 1-repressed GSK3-like kinase BIN2. These results support a regulatory mechanism for thermomorphogenesis in the daytime mediated by the HSFA1s-PIF4 module and uncover HSFA1s as critical regulators integrating light and temperature signaling for a better acclimation of plants to the summer high temperature.
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Proteínas de Arabidopsis , Arabidopsis , Fitocromo , Arabidopsis/metabolismo , Proteínas de Arabidopsis/genética , Proteínas de Arabidopsis/metabolismo , Factores de Transcripción con Motivo Hélice-Asa-Hélice Básico/genética , Factores de Transcripción con Motivo Hélice-Asa-Hélice Básico/metabolismo , Glucógeno Sintasa Quinasa 3 , Temperatura , Plantas/metabolismo , Regulación de la Expresión Génica de las Plantas , Proteínas QuinasasRESUMEN
Carbon fixation by chemoautotrophic microorganisms in the dark ocean makes a large contribution to oceanic primary production and the global carbon cycle. In contrast to the Calvin cycle-dominated carbon-fixing pathway in the marine euphotic zone, carbon-fixing pathways and their hosts in deep-sea areas are diverse. In this study, four deep-sea sediment samples close to hydrothermal vents in the southwestern Indian Ocean were collected and processed using metagenomic analysis to investigate carbon fixation potential. Functional annotations revealed that all six carbon-fixing pathways had genes to varied degrees present in the samples. The reductive tricarboxylic acid cycle and Calvin cycle genes occurred in all samples, in contrast to the Wood-Ljungdahl pathway, which previous studies found mainly in the hydrothermal area. The annotations also elucidated the chemoautotrophic microbial members associated with the six carbon-fixing pathways, and the majority of them containing key carbon fixation genes belonged to the phyla Pseudomonadota and Desulfobacterota. The binned metagenome-assembled genomes revealed that key genes for the Calvin cycle and the 3-hydroxypropionate/4-hydroxybutyrate cycle were also found in the order Rhodothermales and the family Hyphomicrobiaceae. By identifying the carbon metabolic pathways and microbial populations in the hydrothermal fields of the southwest Indian Ocean, our study sheds light on complex biogeochemical processes in deep-sea environments and lays the foundation for further in-depth investigations of carbon fixation processes in deep-sea ecosystems.
Asunto(s)
Respiraderos Hidrotermales , Metagenoma , Océano Índico , Ecosistema , Carbono , FilogeniaRESUMEN
Brassinosteriod (BR) plays important roles in regulation of plant growth, development and environmental responses. BR signaling regulates multiple biological processes through controlling the activity of BES1/BZR1 regulators. Apart from the roles in the promotion of plant growth, BR is also involved in regulation of the root foraging response under low nitrogen, however how BR signaling regulate this process remains unclear. Here we show that BES1 and LBD37 antagonistically regulate root foraging response under low nitrogen conditions. Both the transcriptional level and dephosphorylated level of BES1, is significant induced by low nitrogen, predominantly in root. Phenotypic analysis showed that BES1 gain-of-function mutant or BES1 overexpression transgenic plants exhibits progressive outgrowth of lateral root in response to low nitrogen and BES1 negatively regulates repressors of nitrate signaling pathway and positively regulates several key genes required for NO3 - uptake and signaling. In contrast, BES1 knock-down mutant BES1-RNAi exhibited a dramatical reduction of lateral root elongation in response to low N. Furthermore, we identified a BES1 interacting protein, LBD37, which is a negative repressor of N availability signals. Our results showed that BES1 can inhibit LBD37 transcriptional repression on N-responsive genes. Our results thus demonstrated that BES1-LBD37 module acts critical nodes to integrate BR signaling and nitrogen signaling to modulate the root forging response at LN condition.
RESUMEN
The aim of present study was to explore the vasodilatation mechanism of angiotensin II (AngII) at the molecular level by investigating the effect of AngII on large-conductance Ca²âº-activated potassium channels (BK(Ca)) in human mesenteric artery smooth muscle cells. The effect of AngII on BK(Ca) was observed by using patch clamp single channel recording technique and amphotericin-perforated whole-cell recording technique. AngII type 1 receptor (AT1R) and AngII type 2 receptor (AT2R) mRNA expression in human mesenteric artery was detected by RT-PCR. In cell-attached patch (Vm = +40 mV), AngII (100 nmol/L) had no significant effect on BK(Ca). After pretreatment with Valsartan (a specific inhibitor of AT1R, 10 µmol/L), 25, 100 and 250 nmol/L AngII stimulated BK(Ca) activity significantly in a dose response manner. After pretreatment of Valsartan, AngII (100 nmol/L) enhanced BK(Ca) open probability (NP(O)) from 0.010 ± 0.003 to 0.039 ± 0.015, decreased the mean close time (T(C)) of BK(Ca) markedly from (2 729.5 ± 808.6) ms to (487.7 ± 182.5) ms (n = 11, P < 0.05) , but AngII had no significant influences on the amplitude (Amp) and the mean open time (T(O)) of BK(Ca). Further PD123,319 (a specific inhibitor of AT2R) treatment prevented the stimulatory effect of AngII: PD123,319 decreased the NP(O) of BK(Ca) from 0.016 ± 0.003 to 0.004 ± 0.001 (n = 5, P < 0.05), but had no significant influences on Amp, T(O) and T(C) of BK(Ca). In addition, after pretreatment with Valsartan and PD123,319, AngII (100 nmol/L) had no significant effect on BK(Ca). In the amphotericin-perforated whole-cell patch-clamp configuration, after pretreatment with Valsartan, the current density of BK(Ca) at the voltage of -60 - +30 mV had no significant changes before and after adding 100 nmol/L AngII, but the current density of BK(Ca) at the voltage of +40 mV, +50 mV and +60 mV increased significantly after adding 100 nmol/L AngII, from (9.03 ± 2.23) pA/pF, (12.88 ± 2.55) pA/pF and (17.26 ± 2.84) pA/pF to (12.47 ± 2.22) pA/pF, (18.71 ± 2.51) pA/pF and (27.21 ± 3.12) pA/pF (n = 6, P < 0.05), respectively. Using RT-PCR, the AT1R mRNA and AT2R mRNA from isolated human mesenteric artery were detected. So we can draw a conclusion, AngII can stimulate BK(Ca) activity in human mesenteric artery smooth muscle cells after pretreatment with Valsartan, which is possibly mediated by AT2R.