farnesyl-pyrophosphate and geosmin

The enzymatic synthesis of terpenes was investigated by using a cascade based on the mevalonic acid pathway. Suitable enzymes from all kingdoms of life were identified and combined to give rise to geosmin and patchoulol as representative compounds. The pathway was studied in three separate segments, which were subsequently combined in a ten-step cascade plus added cofactor regeneration systems. The cascade delivers farnesyl pyrophosphate with >40 % conversion and cyclises it to sesquiterpenes with >90 % conversion.

Topics: Acetic Acid; Archaea; Bacteria; Biocatalysis; Cyclization; Enzymes; Fungi; Mevalonic Acid; Naphthols; Plants; Polyisoprenyl Phosphates; Sesquiterpenes

Geosmin synthase from Streptomyces coelicolor (ScGS) catalyzes an unusual, metal-dependent terpenoid cyclization and fragmentation reaction sequence. Two distinct active sites are required for catalysis: the N-terminal domain catalyzes the ionization and cyclization of farnesyl diphosphate to form germacradienol and inorganic pyrophosphate (PPi), and the C-terminal domain catalyzes the protonation, cyclization, and fragmentation of germacradienol to form geosmin and acetone through a retro-Prins reaction. A unique αα domain architecture is predicted for ScGS based on amino acid sequence: each domain contains the metal-binding motifs typical of a class I terpenoid cyclase, and each domain requires Mg(2+) for catalysis. Here, we report the X-ray crystal structure of the unliganded N-terminal domain of ScGS and the structure of its complex with three Mg(2+) ions and alendronate. These structures highlight conformational changes required for active site closure and catalysis. Although neither full-length ScGS nor constructs of the C-terminal domain could be crystallized, homology models of the C-terminal domain were constructed on the basis of ∼36% sequence identity with the N-terminal domain. Small-angle X-ray scattering experiments yield low-resolution molecular envelopes into which the N-terminal domain crystal structure and the C-terminal domain homology model were fit, suggesting possible αα domain architectures as frameworks for bifunctional catalysis.

Topics: Alendronate; Bacterial Proteins; Crystallography, X-Ray; Cyclization; Magnesium; Models, Molecular; Naphthols; Polyisoprenyl Phosphates; Protein Structure, Tertiary; Sesquiterpenes; Streptomyces coelicolor

Geosmin is a secondary metabolite responsible for earthy tastes and odors in potable water supplies. Geosmin continues to be a challenge to water utility management regimes and remains one of the most common causes of consumer complaints, as the taste of "dirty" water may suggest a failed disinfection regime and that the water may be unsafe to drink. Although cyanobacteria have been reported to be largely responsible for these taste and odor events, the answer as to how or why geosmin is produced has eluded researchers. We describe here for the first time the mechanism by which geosmin is produced in a model cyanobacterium, Nostoc punctiforme PCC 73102 (ATCC 29133), which we demonstrate utilizes a single enzyme to catalyze the cyclization of farnesyl diphosphate to geosmin. Using this information, we have developed a PCR-based assay that allows the rapid detection of geosmin-producing cyanobacteria. This test may be utilized to confirm and track the emergence of taste and odor-producing cyanobacteria in any given water body and thus can be used as an early warning system by managers of water bodies that may suffer from adverse taste and odor episodes.

Topics: Amino Acid Sequence; Bacterial Proteins; Catalysis; Cyclization; DNA, Bacterial; Environmental Microbiology; Gas Chromatography-Mass Spectrometry; Genes, Bacterial; Molecular Sequence Data; Naphthols; Nostoc; Nucleic Acid Denaturation; Polyisoprenyl Phosphates; Polymerase Chain Reaction; Sequence Alignment; Sesquiterpenes

Topics: Bacterial Proteins; Naphthols; Polyisoprenyl Phosphates; Sesquiterpenes; Streptomyces coelicolor

Geosmin is responsible for the characteristic odor of moist soil. Incubation of recombinant germacradienol synthase, encoded by the SCO6073 (SC9B1.20) gene of the Gram-positive soil bacterium Streptomyces coelicolor, with farnesyl diphosphate (2, FPP) in the presence of Mg2+ gave a mixture of (4S,7R)-germacra-1(10)E,5E-diene-11-ol (3) (74%), (-)-(7S)-germacrene D (4) (10%), geosmin (1) (13%), and a hydrocarbon, tentatively assigned the structure of octalin 5 (3%). Individual incubations of recombinant germacradienol synthase with [1,1-2H2]FPP (2a), (1R)-[1-2H]-FPP (2b), and (1S)-[1-2H]-FPP (2c), as well as with FPP (2) in D2O, and GC-MS analysis of the resulting deuterated products supported a mechanism of geosmin formation involving proton-initiated cyclization and retro-Prins fragmentation of the initially formed germacradienol to give intermediate 5, followed by protonation of 5, 1,2-hydride shift, and capture of water.

Topics: Alkyl and Aryl Transferases; Cyclization; Mass Spectrometry; Molecular Structure; Naphthols; Polyisoprenyl Phosphates; Recombinant Proteins; Sesquiterpenes; Streptomyces coelicolor

Geosmin (1) is responsible for the characteristic odor of moist soil. The Gram-positive soil bacterium Streptomyces avermitilis produces geosmin (1) as well as its precursor germacradienol (3). The S. avermitilis gene SAV2163 (geoA) is extremely similar to the S. coelicolor A3(2) SCO6073 gene that encodes a germacradienol/geosmin synthase. S. avermitilis mutants with a deleted geoA were unable to produce either germacradienol (3) or geosmin (1). Biosynthesis of both compounds was restored by introducing an intact geoA gene into the mutants. Incubation of recombinant GeoA, encoded by the SAV2163 gene of S. avermitilis, with farnesyl diphosphate (2) in the presence of Mg2+ gave a mixture of (4S,7R)-germacra-1(10)E,5E-diene-11-ol (3) (66%), (7S)-germacrene D (4) (24%), geosmin (1) (8%), and a hydrocarbon, tentatively assigned the structure of octalin 5 (2%). Incubation of this germacradienol/geosmin synthase with [1,1-(2)H2] FPP (2a) gave geosmin-d1 (1a), as predicted. When recombinant GeoA from either S. avermitilis or S. coelicolor A3(2) was incubated with nerolidyl diphosphate (8), only the acyclic elimination products beta3-farnesene (10), (Z)-alpha-farnesene (11), and (E)-alpha-farnesene (12) were formed, thereby ruling out nerolidyl diphosphate as an intermediate in the conversion of farnesyl diphosphate to geosmin, germacradienol, and germacrene D.

Topics: Cloning, Molecular; Gene Expression Regulation, Bacterial; Naphthols; Polyisoprenyl Phosphates; Sesquiterpenes; Soil; Streptomyces

The biosynthesis of the trisnor sesquiterpenoid geosmin (4,8a-dimethyl-octahydro-naphthalen-4a-ol) (1) was investigated by feeding labeled [5,5-2H(2)]-1-desoxy-D-xylulose (11), [4,4,6,6,6-(2)H(5)]-mevalolactone (7) and [2,2-2H(2)]-mevalolactone (9) to Streptomyces sp. JP95 and the liverwort Fossombronia pusilla. The micro-organism produced geosmin via the 1-desoxy-D-xylulose pathway, whereas the liverwort exclusively utilized mevalolactone for terpenoid biosynthesis. Analysis of the labeling pattern in the resulting isotopomers of geosmin (1) by mass spectroscopy (EI/MS) revealed that geosmin is synthesized in both organisms by cyclization of farnesyl diphosphate to a germacradiene-type intermediate 4. Further transformations en route to geosmin (1) involve an oxidative dealkylation of an i-propyl substituent, 1,2-reduction of a resulting conjugated diene, and bicyclization of a germacatriene intermediate 13. The transformations largely resemble the biosynthesis of dehydrogeosmin (2) in cactus flowers but differ with respect to the regioselectivity of the side chain dealkylation and 1,2-reduction

Topics: Alkylation; Cyclization; Deuterium; Hepatophyta; Lactones; Naphthols; Oxidation-Reduction; Polyisoprenyl Phosphates; Sesquiterpenes; Spectrometry, Mass, Electrospray Ionization; Stereoisomerism; Streptomyces; Xylulose