Microorganism parts

Luibrand RT, Erdman TR, Vollmer JJ, Scheuer PJ, Finer J, Clardy J (1979) Ilimaquinone a sesquit-erpenoid quinone from a marine sponge (Hippospongia metachromia).Tetrahedron 35 609-612 Moore BS (2005) Biosynthesis of marine natural products microorganisms (Part A). Nat Prod Rep 22 580-593... 

Moore BS (2005) Biosynthesis of marine natural products microorganisms (Part A). Nat Prod Rep 22 580-593... 

Challenger, F., Higginbottom, C. and Ellis, L. (1933) The formation of organo-metalloidal compounds by microorganisms. Part I. Trimethylarsine and dimethylarsine. Journal of the Chemical Society, 95-101. 

Besides the study of intact microorganisms or microorganism parts, Py-MS has been used for other related purposes such as the characterization of semi-synthetic vaccines. An example is the characterization using Py-MS of a polysaccharide-tetanus toxoid conjugate [71c]. The Py-MS results were used in conjunction with the immunologic results. 

Laneelle, G. and Clement, Y. (1986) Glutamate excretion mechanism in Corynehacterium glutamicum. 5th International Symposium on the Genetics of Industrial Microorganisms, Part B, pp. 247-252. 

Moser, A. (1980b). In Theoretical Basis of Kinetics of Growth, Metabolism and Product Formation of Microorganisms, Part 2. UNEP/UNESCO/ICRO Training Course, Zentralinstitut fiir Mikrobiologie und Experimentelle Therapie, Academy of Science, Jena, (Knorre W., ed.) East Germany (publisher) p. 27. 

Source Noma, Y. et at.. Formation of 8 kinds of p menthane-2,8-diols from carvone and related compounds by Euglena gracilis Z. Biotransformation of monoterpenes by photosynthetic microorganisms. Part VIII, Proceedings of 37th TEAC, 1993, pp. 23-25. 

Yamada, K., S. Horiguchi, and J. Tatahashi, 1965. Studies on the utilization of hydrocarbons by microorganisms. Part VI. Screening of aromatic hydrocarbon-assimilating microorganisms and cumic acid formation from p cvmene.Agn c. Biol. Chem.. 29 943-948. 

An accompanyiag effect of eutrophication that is more readily observable ia Table 1 is a decrease ia siUca coaceatratioa ia Lake Oatario. Some decliae ia dissolved siUca appareatiy has occurred ia all of the lakes except Lake Superior. This decliae is brought about by the growth of diatoms, a species of aquatic microorganisms ia the upper layers of lake water that is widespread ia all types of water impouadmeats where the water is clear and exposed to the sun. The siUca is used by these microorganisms to form their skeletons and is later precipitated and becomes part of the bed sediment. 

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