3 research outputs found
Abstract P-33: Structural Basis for the Growing Microtubule End Recognition by End Binding Proteins
Background: Eukaryotic end binding proteins (EBs) can follow the growing microtubule end. EBs play a crucial role in microtubule dynamic instability and promote simultaneously growth rate and catastrophe frequency. It makes EB-like proteins perspective drag targets for a wide number of diseases. But the molecular mechanism of tip tracking by EB-like proteins remains unknown. Studies of mutants have revealed that the conservative amino acid Q102 (numbering relative to the human EB1 protein) plays a key role in the recognition of the growing microtubule end. However, the 3D structure studies revealed that this amino acid has no bonds with tubulin. In this work, we performed structural and phylogenetic analysis of EBs proteins to identify a possible molecular mechanism behind the plus end tracking.
Methods: UCSF Chimera10 was used for structural analysis. Phylogenetic analysis was performed with MEGA X software. 3D structures of EBs and microtubules with different states of GTP hydrolysis were used (pdb 3JAK, 3JAS, 3JAT, 3JAW, 3JAL, 3JAR, 6DPU, 6DPV, 6DPW).
Results: We have shown that two conservative amino acids (K100, E106) should play an important role in the recognition of the microtubule plus end in addition to Q102. It was concluded that these amino acids together form the plus-end «navigation site» of EBs. Analysis of possible interaction of the «navigation site» amino acids with microtubules in different conformational states suggested that the main mechanism of growing microtubule end recognition is not due to an affinity increase for a certain state of tubulin in microtubules at their end, but it due to a significant affinity decrease in other parts of the microtubule as a result of steric clashes.
Conclusion: Thus, the results of the analysis suggested the possible molecular mechanism that provides the tip tracking by EB-like proteins and allowed us to identify the key amino acids of this mechanism
Abstract P-36: Structural Analysis of Conformational Changes of Bacterial and Eukaryotic Tubulins
Background: Eukaryotic α- and β-tubulin proteins stand out among tubulin-like proteins by their ability to form hollow dynamically unstable microtubules (MT) with 13 protofilaments. Microtubules are part of the cell cytoskeleton and play a key role in chromosome division in mitosis. A considerable amount of anticancer drugs works on microtubules level breaking its dynamic. But the mechanism of dynamic instability and works of these drugs remains unknown. Bacteria of the genus Prostecobacter have unique bacterial tubulins (BtubA/B) capable to form hollow dynamically unstable 5 protofilament MTs (miniMT). Instead of great differences, both tubulins have many common features. Eukaryotic tubulin was known to have structural changes through GTP hydrolysis (compactization for approximately 2 Å and a twist for 0,1˚). «Anchor point» structure in alpha-tubulin was noticed to be a fixed point in this movement.
Methods: We performed comparative structural analysis of BtubA/B and α- and β-tubulin proteins using USCF Chimera10 and MEGA X software. This data was obtained due to a comparison of 3 structures of microtubules with different nucleotides [pdb6DPU, 6DPV, 6DPW] and two structures for bacterial tubulins (miniMT [pdb5o09] and BtubA/B-dimer [pdb2BTQ]).
Results: We noticed that bacterial tubulins form shorter protofilaments in miniMT than eukaryotic ones. It can be explained as compaction in two sites instead of one site in eukaryotic MT. Also, the most motionless point of min MT turned out the same "anchor point." Phylogenetic analysis showed that this structure is very conservative in these orthologs. Moreover, the final state of both tubulins (GDP) repeats each other.
Conclusion: Our results suggest that bacterial tubulin can have movements through GTP hydrolysis similar to eukaryotic one. And it means that despite different amino acid sequences, bacterial and eukaryotic tubulins have similar keys structures for dynamic instability
Diversity of Metabolically Active Bacteria in Water-Flooded High-Temperature Heavy Oil Reservoir
The goal of this work was to study the overall genomic diversity of microorganisms of the Dagang high-temperature oilfield (PRC) and to characterize the metabolically active fraction of these populations. At this water-flooded oilfield, the microbial community of formation water from the near-bottom zone of an injection well where the most active microbial processes of oil degradation occur was investigated using molecular, cultural, radiotracer, and physicochemical techniques. The samples of microbial DNA and RNA from back-flushed water were used to obtain the clone libraries for the 16S rRNA gene and cDNA of 16S rRNA, respectively. The DNA-derived clone libraries were found to contain bacterial and archaeal 16S rRNA genes and the alkB genes encoding alkane monooxygenases similar to those encoded by alkB-geo1 and alkB-geo6 of geobacilli. The 16S rRNA genes of methanogens (Methanomethylovorans, Methanoculleus, Methanolinea, Methanothrix, and Methanocalculus) were predominant in the DNA-derived library of Archaea cloned sequences; among the bacterial sequences, the 16S rRNA genes of members of the genus Geobacillus were the most numerous. The RNA-derived library contained only bacterial cDNA of the 16S rRNA sequences belonging to metabolically active aerobic organotrophic bacteria (Tepidimonas, Pseudomonas, Acinetobacter), as well as of denitrifying (Azoarcus, Tepidiphilus, Calditerrivibrio), fermenting (Bellilinea), iron-reducing (Geobacter), and sulfate- and sulfur-reducing bacteria (Desulfomicrobium, Desulfuromonas). The presence of the microorganisms of the main functional groups revealed by molecular techniques was confirmed by the results of cultural, radioisotope, and geochemical research. Functioning of the mesophilic and thermophilic branches was shown for the microbial food chain of the near-bottom zone of the injection well, which included the microorganisms of the carbon, sulfur, iron, and nitrogen cycles