A-ATP Synthase

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Introduction

The archaeal A1A0 ATP synthase represent a class of chimeric ATPases/synthase , whose function and general structural design share characteristics both with vacuolar V1V0 ATPases and with F1Fo ATP synthases [1]. A1A0 ATP synthase catalyzes the formation of the energy currency ATP by a membrane-embedded electrically-driven motor. The archaeon in this study,Pyrococcushorikoshii OT3 is an anaerobic thermophile residing in oceanic deep sea vents with an optimal growth temperature of 100 degrees C. Anaerobic fermentation is its principle metabolic pathway. A hyperthermophilic, anaerobic archaeon was isolated from hydrothermal fluid samples obtained at the Okinawa Trough vents in the NE Pacific Ocean, at a depth of 1395m. The strain is obligately heterotrophic, and utilizes complex proteinaceous media (peptone, tryptone, or yeast extract), or a 21-amino-acid mixture supplemented with vitamins, as growth substrates. Sulfur greatly enhances growth. The cells are irregular cocci with a tuft of flagella, growing optimally at 98 degrees C (maximum growth temperature 102 degrees C), but capable of prolonged survival at 105 degrees C. [2] The specific enzymatic process in A-ATP synthase reveals novel, exceptional subunit composition and coupling stoichiometries that may reflect the differences in energy-conserving mechanisms as well as adaptation to temperatures at or above 100 degrees C. Because some archaea are rooted close to the origin in the tree of life, these unusual mechanisms are considered to have developed very early in the history of life and, therefore, may represent the first energy-conserving mechanisms. [3]

Structure

A-ATP synthase ATP synthase is composed of two parts A1 and A0 which are composed of at least nine subunits A3B3C:D:E:F:H2:a:cx that function as a pair of rotary motors connected by central and peripheral stalk(s) [3].This structure is similar to the known structure of F ATP synthase. The A0 domain is the hydrophobic membrane embedded ion-translocating sector that uses the H+ gradient to power ATP synthase in domain A1. A1 is catalytic and water soluble containing A and B subunits. These subunits are comparable to F-ATP synthase ATP synthase alpha/beta subunits. The A subunit of A1 is catalytic and the B subunit is regulatory, with a substrate-binding site on each. [http://www.youtube.com/watch?v=W3KxU63gcF4 http://www.youtube.com/watch?v=KU-B7G6anqw&feature=related]


PDB ID 3p20

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Comparasons to other known structures

This P-loop has an arched conformation unique to A-ATP Synthase, indicating that the mode of nucleotide binding and the catalytic mechanism is different from that of other syntheses. [5]

For example, in A-ATP Synthases is involved in P-Loop stabilization, but its equivalent (alanine) in subunit B of the F-ATP syntheses subunit beta is a key residue in the catalytic process in moving towards the y-phosphate of ATP during catalysis. By comparing the average distances of the alpha carbons of the P-loop residues to the sulfate, vanadate, and PNP molecules, it was found that the PNP molecule is closest, followed by the vanadate then the sulfate.


In "'F-ATP Synthase"' the homolog to S238 is the non polar A158. Since A158 cannot form hydrogen bonds to interact with the substrate, the P-loop undergoes a conformational change. In A-ATP Synthase the close proximity needed between S238 and the first vandate during transition state is achieved with a hydrogen bond, not a conformational change in the P-loop. These increased proximities of the catalytically important residues clearly demonstrate that structural rearrangement occurs during catalysis in subunit A. [4]




Template:STRUCTURE 3p20

Contents

References

  1. Schafer IB, Bailer SM, Duser MG, Borsch M, Bernal RA, Stock D, Gruber G. Crystal structure of the archaeal A1Ao ATP synthase subunit B from Methanosarcina mazei Go1: Implications of nucleotide-binding differences in the major A1Ao subunits A and B. J Mol Biol. 2006 May 5;358(3):725-40. Epub 2006 Mar 10. PMID:16563431 doi:http://dx.doi.org/10.1016/j.jmb.2006.02.057
  2. Gonzalez JM, Masuchi Y, Robb FT, Ammerman JW, Maeder DL, Yanagibayashi M, Tamaoka J, Kato C. Pyrococcus horikoshii sp. nov., a hyperthermophilic archaeon isolated from a hydrothermal vent at the Okinawa Trough. Extremophiles. 1998 May;2(2):123-30. PMID:9672687
  3. 3.0 3.1 Muller V, Lemker T, Lingl A, Weidner C, Coskun U, Gruber G. Bioenergetics of archaea: ATP synthesis under harsh environmental conditions. J Mol Microbiol Biotechnol. 2005;10(2-4):167-80. PMID:16645313 doi:10.1159/000091563
  4. 4.0 4.1 Manimekalai MS, Kumar A, Jeyakanthan J, Gruber G. The Transition-Like State and P(i) Entrance into the Catalytic A Subunit of the Biological Engine A-ATP Synthase. J Mol Biol. 2011 Mar 16. PMID:21396943 doi:10.1016/j.jmb.2011.03.010
  5. Priya R, Kumar A, Manimekalai MS, Gruber G. Conserved Glycine Residues in the P-Loop of ATP Synthases Form a Doorframe for Nucleotide Entrance. J Mol Biol. 2011 Sep 8. PMID:21925186 doi:10.1016/j.jmb.2011.08.045

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Kaitlin Chase MacCulloch, Michal Harel, Alexander Berchansky

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