e Marine bacteria form one of the largest living surfaces on Earth, and their metabolic activity is of fundamental importance for global nutrient cycling. Here, we explored the largely unknown intracellular pathways in 25 microbes representing different classes of marine bacteria that use glucose: Alphaproteobacteria, Gammaproteobacteria, and Flavobacteriia of the Bacteriodetes phylum. We used 13 C isotope experiments to infer metabolic fluxes through their carbon core pathways. Notably, 90% of all strains studied use the Entner-Doudoroff (ED) pathway for glucose catabolism, whereas only 10% rely on the Embden-Meyerhof-Parnas (EMP) pathway. This result differed dramatically from the terrestrial model strains studied, which preferentially used the EMP pathway yielding high levels of ATP. Strains using the ED pathway exhibited a more robust resistance against the oxidative stress typically found in this environment. An important feature contributing to the preferential use of the ED pathway in the oceans could therefore be enhanced supply of NADPH through this pathway. The marine bacteria studied did not specifically rely on a distinct anaplerotic route, but the carboxylation of phosphoenolpyruvate (PEP) or pyruvate for fueling of the tricarboxylic acid (TCA) cycle was evenly distributed. The marine isolates studied belong to clades that dominate the uptake of glucose, a major carbon source for bacteria in seawater. Therefore, the ED pathway may play a significant role in the cycling of mono-and polysaccharides by bacterial communities in marine ecosystems. Marine bacteria influence global environmental dynamics in fundamental ways by controlling the biogeochemistry and productivity of the oceans (1). Due to their importance, marine microorganisms have been studied intensively (2). In particular, their mechanisms for metabolizing carbon and other nutrients have attracted attention, because they directly or indirectly affect the biogeochemical status of seawater (3). A prominent nutrient in seawater is glucose, the most abundant free neutral aldose (4). Current estimates of glucose concentrations in seawater indicate an almost ubiquitous distribution in the oceans in a nanomolar range (5). Particularly, large amounts of glucose are available in coastal habitats, e.g., during bloom situations (6). In fact, a large fraction (Ͼ30%) of bacterial growth can be supported by this monosaccharide in some oceans (7,8). Furthermore, glucose is the dominant component of dissolved polysaccharides, which constitute up to 15% of marine dissolved organic matter (9). The turnover of the (monomeric and polymeric) glucose pool in different oceanic regions ranges from days to months, and glucose assimilation in marine surface waters may represent up to 40% of bacterial carbon production (5). Taken together, bacteria that use glucose are common in the sea (10), and glucose is a representative model nutrient to monitor carbon uptake by heterotrophic marine bacteria (11). At this point, questions that arise from current knowledge concern...

ABSTRACTProduction of the antibiotic tropodithietic acid (TDA) depends on the central phenylacetate catabolic pathway, specifically on the oxygenase PaaABCDE, which catalyzes epoxidation of phenylacetyl-coenzyme A (CoA). Our study was focused on genes of the upper part of this pathway leading to phenylacetyl-CoA as precursor for TDA.Phaeobacter gallaeciensisDSM 17395 encodes two genes with homology to phenylacetyl-CoA ligases (paaK1andpaaK2), which were shown to be essential for phenylacetate catabolism but not for TDA biosynthesis and phenylalanine degradation. Thus, inP. gallaeciensisanother enzyme must produce phenylacetyl-CoA from phenylalanine. Using random transposon insertion mutagenesis of apaaK1-paaK2double mutant we identified a gene (ior1) with similarity toiorAandiorBin archaea, encoding an indolepyruvate:ferredoxin oxidoreductase (IOR). Theior1mutant was unable to grow on phenylalanine, and production of TDA was significantly reduced compared to the wild-type level (60%). Nuclear magnetic resonance (NMR) spectroscopic investigations using13C-labeled phenylalanine isotopomers demonstrated that phenylalanine is transformed into phenylacetyl-CoA by Ior1. Using quantitative real-time PCR, we could show that expression ofior1depends on the adjacent regulator IorR. Growth on phenylalanine promotes production of TDA, induces expression ofior1(27-fold) andpaaK1(61-fold), and regulates the production of TDA. Phylogenetic analysis showed that the aerobic type of IOR as found in many roseobacters is common within a number of different phylogenetic groups of aerobic bacteria such asBurkholderia,Cupriavidis, andRhizobia, where it may also contribute to the degradation of phenylalanine.

Twenty-four strains of marine Roseobacter clade bacteria were isolated from macroalgae and investigated for the production of quorum-sensing autoinducers, N-acylhomoserine lactones (AHLs). GC/MS analysis of the extracellular metabolites allowed us to evaluate the release of other small molecules as well. Nineteen strains produced AHLs, ranging from 3-OH-C10:0-HSL (homoserine lactone) to (2E,11Z)-C18:2-HSL, but no specific phylogenetic or ecological pattern of individual AHL occurrence was observed when cluster analysis was performed. Other identified compounds included indole, tropone, methyl esters of oligomers of 3-hydroxybutyric acid, and various amides, such as N-9-hexadecenoylalanine methyl ester (9-C16:1-NAME), a structural analogue of AHLs. Several compounds were tested for their antibacterial and antialgal activity on marine isolates likely to occur in the habitat of the macroalgae. Both AHLs and 9-C16:1-NAME showed high antialgal activity against Skeletonema costatum, whereas their antibacterial activity was low.

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We examined the bacterial decomposition of humic acids (HA) in two flowthrough culture experiments, one inoculated by marine and one by estuarine bacterial communities. In both experiments, the cultures were fed with HA media of salinities of 28 and 14, close to their ambient and a distinctly different, foreign salinity. HA were decomposed to > 60% of the initial concentration within 70 days, and the foreign salinity yielded the highest decomposition. A detrended correspondence analysis of denaturing gradient gel electrophoresis (DGGE) banding patterns showed that during incubation, the bacterial community composition underwent distinct changes. A phylogenetic analysis of DGGE bands excised and bacteria isolated at the end on HA as the sole carbon source showed that Alphaproteobacteria and Gammaproteobacteria largely dominated the communities in the marine flow-through cultures, whereas Gammaproteobacteria, Actinobacteria and Alphaproteobacteria dominated the estuarine communities. Eleven of 13 isolates obtained from both experiments were able to grow on HA as the sole carbon source, seven on phenol and three, affiliated to the Roseobacter clade, on various aromatic acids. The bacteria retrieved from the flow-through cultures were closely (96-99%) affiliated to organisms capable of degrading humic matter, aromatic and aliphatic compounds and also to other bacteria reported previously from the Wadden Sea and Weser estuary.