scholarly journals Discovery and Characterization of a Naturally Occurring, Turn-On Yellow Fluorescent Protein Sensor for Chloride

Biochemistry ◽  
2018 ◽  
Vol 58 (1) ◽  
pp. 31-35 ◽  
Author(s):  
Jasmine N. Tutol ◽  
Weicheng Peng ◽  
Sheel C. Dodani
2020 ◽  
Vol 10 (10) ◽  
pp. 3508
Author(s):  
Haijun Yu ◽  
Haoxiang Li ◽  
Yao Zhou ◽  
Shengmin Zhou ◽  
Ping Wang

In this paper, a fluorescence resonance energy transfer (FRET)-based sensor for ultra-sensitive detection of H2O2 was developed by utilizing the unique enzymatic properties of peroxiredoxin (Prx) to H2O2. Cyan and yellow fluorescent protein (CFP and YFP) were fused to Prx and mutant thioredoxin (mTrx), respectively. In the presence of H2O2, Prx was oxidized into covalent homodimer through disulfide bonds, which were further reduced by mTrx to form a stable mixed disulfide bond intermediate between CFP-Prx and mTrx-YFP, inducing FRET. A linear quantification range of 10–320 nM was obtained according to the applied protein concentrations and the detection limit (LOD) was determined to be as low as 4 nM. By the assistance of glucose oxidase to transform glucose into H2O2, the CFP-Prx/mTrx-YFP system (CPmTY) was further exploited for the detection of glucose in real sample with good performance, suggesting this CPmTY protein sensor is highly practical.


2020 ◽  
Vol 86 (8) ◽  
Author(s):  
Celina Frank ◽  
Dieter Jendrossek

ABSTRACT Acidocalcisomes are membrane-enclosed, polyphosphate-containing acidic organelles in lower Eukaryota but have also been described for Agrobacterium tumefaciens (M. Seufferheld, M. Vieira, A. Ruiz, C. O. Rodrigues, S. Moreno, and R. Docampo, J Biol Chem 278:29971–29978, 2003, https://doi.org/10.1074/jbc.M304548200). This study aimed at the characterization of polyphosphate-containing acidocalcisomes in this alphaproteobacterium. Unexpectedly, fluorescence microscopic investigation of A. tumefaciens cells using fluorescent dyes and localization of constructed fusions of polyphosphate kinases (PPKs) and of vacuolar H+-translocating pyrophosphatase (HppA) with enhanced yellow fluorescent protein (eYFP) suggested that acidocalcisomes and polyphosphate are different subcellular structures. Acidocalcisomes and polyphosphate granules were frequently located close together, near the cell poles. However, they never shared the same position. Mutant strains of A. tumefaciens with deletions of both ppk genes (Δppk1 Δppk2) were unable to form polyphosphate but still showed cell pole-located eYFP-HppA foci and could be stained with MitoTracker. In conclusion, A. tumefaciens forms polyP granules that are free of a surrounding membrane and thus resemble polyP granules of Ralstonia eutropha and other bacteria. The composition, contents, and function of the subcellular structures that are stainable with MitoTracker and harbor eYFP-HppA remain unclear. IMPORTANCE The uptake of alphaproteobacterium-like cells by ancestors of eukaryotic cells and subsequent conversion of these alphaproteobacterium-like cells to mitochondria are thought to be key steps in the evolution of the first eukaryotic cells. The identification of acidocalcisomes in two alphaproteobacterial species some years ago and the presence of homologs of the vacuolar proton-translocating pyrophosphatase HppA, a marker protein of the acidocalcisome membrane in eukaryotes, in virtually all species within the alphaproteobacteria suggest that eukaryotic acidocalcisomes might also originate from related structures in ancestors of alphaproteobacterial species. Accordingly, alphaproteobacterial acidocalcisomes and eukaryotic acidocalcisomes should have similar features. Since hardly any information is available on bacterial acidocalcisomes, this study aimed at the characterization of organelle-like structures in alphaproteobacterial cells, with A. tumefaciens as an example.


Author(s):  
Alenka Hrovat ◽  
Apolonija Zavec ◽  
Azra Pogačnik ◽  
Robert Frangež ◽  
Milka Vrecl

AbstractThis study focused on establishing and making a comprehensive functional characterization of an HEK-293-transfected cell line that would coexpress the enhanced yellow fluorescent protein-actin (pEYFP-actin) construct and the neurokinin type 1 receptor (NK1-R), which is a member of the seven transmembrane (7TM) receptor family. In the initial selection procedure, the cloning ring technique was used alone, but failed to yield clones with homogenous pEYFP-actin expression. Flow cytometry sorting (FCS) was subsequently used to enrich the pEYFP-actin-expressing subpopulation of cells. The enzyme-linked immunosorbent assay (ELISA), FCS and quantitative real-time reverse transcription/polymerase chain reaction (RT-PCR) were then employed to monitor the passage-dependent effects on transgene expression and to estimate the total β-actin/pEYFP-actin ratio. NK1-R was characterized via radioactive ligand binding and the second messenger assay. The suitability of the pEYFP-actin as a marker of endogenous actin was assessed by colocalizing pEYFP-actin with rhodamine-phalloidine-stained F-actin and by comparing receptor- and jasplakinolide-induced changes in the actin cytoskeleton organization. These experiments demonstrated that: i) both constructs expressed in the generated transfected cell line are functional; ii) the estimated pEYFP-actin: endogenous β-actin ratio is within the limits required for the functional integrity of the actin filaments; and iii) pEYFP-actin and rhodamine-phalloidine-stained F-actin structures colocalize and display comparable reorganization patterns in pharmacologically challenged cells.


Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.


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