NifB, X, and Y share a common domain of about 90 amino acid; moreover, NifB has
an additional SAM domain, found in proteins that catalyze see more diverse reactions. Similarly, NifV proteins cluster with metabolic proteins, such as Isopropylmalate synthase. Data obtained revealed that different molecular mechanisms might have shaped nitrogen fixation. In some cases it can be suggested that nif genes might have been recruited from other metabolic pathways, whereas the origin of other ones remains mysterious. Stijn van Dongen. A cluster algorithm for graphs. Technical Report INS-R0010, National Research Institute for Mathematics and Computer Science in the Netherlands, Amsterdam, May 2000. Lio’ P, Brilli M, Fani R (accepted BIRD 2008 conference). Topological Metrics in Blast Data Mining: Plasmid and Nitrogen-Fixing Proteins Case Studies. Lecture Notes in Computer Science, Springer E-mail: renato.fani@unifi.it Hydrogen and Metal Catalysts in the Initiation and Early Evolution of Life Mikhail Fedonkin Paleontological Institute, Russian Academy of sciences, Moscow Most of known enzymes contain the transition metal
ions as a cofactor of their active sites. These metalloenzymes loose their catalytic activity when the metal ions are being removed from the protein molecule. These Gemcitabine facts indicate to the primary role of the metals in the origin of biocatalysis. Taxonomic distribution of the metalloenzymes gives a hint on the biogenesis as well. For example, the tungsten enzymes are discovered so far in prokaryotes only. However, obligatory dependence on tungsten is documented merely for hyperthermophylic Archea. Their basal position on the molecular tree of life points to the W-rich hydrothermal systems as a cradle of life. But the major catalysts on the earliest stages of the biogenesis were iron and nickel. Tolmetin The fact that nickel makes 5–20% of the iron meteorites indicates that both metals were this website abundant on young Earth. At present iron and nickel are actively involved
in hydrogen metabolism which plays a key role in the prokaryotic and even eukaryotic organisms: virtually all hydrogenases contain Fe and/or Ni cofactor. This should turn our attention to the role of hydrogen in biogenesis. Hydrogen, the most abundant element in the Universe, well could be the primary fuel for early life. The availability of hydrogen on early Earth was much higher than at present. Two major sources of hydrogen were (1) the degassing of the mantle that released the neutral or slightly acidic fluids saturated with H2, CH4 and H2S, and (2) the serpentinization, reaction of the rocks, rich with olivine and pyroxene, with water. Two additional processes, such as photolysis of water by UV light and radiation-induced dissociation of H2O could contribute to the hydrogen budget as well.