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Applied and Environmental Microbiology, June 2004, p. 3383-3391, Vol. 70, No. 6
0099-2240/04/$08.00+0 DOI: 10.1128/AEM.70.6.3383-3391.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
Center of Marine Biotechnology, University of Maryland Biotechnology Institute, Baltimore, Maryland 21202
Received 25 August 2003/ Accepted 5 March 2004
| ABSTRACT |
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| INTRODUCTION |
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Dimethylsulfoniopropionate (DMSP) is the major source of organic sulfur in the world's oceans and plays a significant role in the global sulfur cycle (reviewed in reference 45). During blooms of marine unicellular algae, cellular DMSP is released due to algal senescence, predation, or stress and is degraded by both algal and bacterial enzymes. In marine environments, dinoflagellates and prymnesiophytes are the major producers of DMSP, with intracellular concentrations as high as 0.5 M (45). Although the exact function of DMSP is unclear, it has possible roles in osmoprotection (9, 40) and cryoprotection (23), antiherbivory (44), and protection from oxidative stress (37).
Bacteria and certain species of phytoplankton produce an enzyme, dimethylpropiothetin dethiomethylase (DMSP lyase) (EC 4.4.1.3) (Fig. 1, reaction 1), which degrades DMSP to produce dimethylsulfide (DMS) and acrylate (46). As shown in Fig. 1, DMS produced from this reaction is oxidized by some bacterial species to form dimethyl sulfoxide (Fig. 1, reaction 6) (39). Acrylate is readily consumed by bacteria and is converted to ß-hydroxypropionate by
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-proteobacterial species (2, 3). Bacteria may also demethylate DMSP at the DMS moiety (Fig. 1, reaction 2), producing 3-methylmercaptopropionate (MMPA) (20), which may be further demethylated to 3-mercaptopropionate (MPA; Fig. 1, reaction 4) (41) or demethiolated to produce acrylate (Fig. 1, reaction 3) and methanethiol (MeSH); (38). The products of these reactions provide a rich source of carbon and sulfur for bacterial production (26, 42). It is estimated that
15% of the DMSP produced by marine phytoplankton is degraded by the lyase pathway and 85% or more is degraded by bacterial demethylation of DMSP, suggesting an essential bacterial role in controlling DMS emissions from the world's oceans (33, 47).
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-proteobacteria phylogenetically related to Roseobacter spp. are predominantly responsible for the degradation of DMSP, its catabolites, and other sulfonium compounds (15). Although Roseobacter spp. are cosmopolitan in nature, their production and activity are significantly correlated with DMSP-producing algae, including dinoflagellates and prymnesiophytes (16, 47). Furthermore, some Roseobacter spp. exhibit close physical or physiological relationships with toxic, DMSP-producing dinoflagellates, including Prorocentrum spp. (30), Alexandrium spp. (8, 12), and Pfiesteria spp. (1). In the environment, dinoflagellates coexist and interact with a diverse community of bacteria and other microorganisms. These interactions can be studied in monocultures of dinoflagellates obtained from environmental samples. Within these cultures, bacteria native to the algal niche assimilate dinoflagellate-derived nutrients and are intrinsically propagated with the dinoflagellates in continuous subcultures. In a recent study, we characterized the bacterial community inhabiting several Pfiesteria dinoflagellate cultures isolated from the Chesapeake Bay, Md. (1). All of the dinoflagellate cultures examined contained one or more Roseobacter spp. representing the second most abundant clone obtained from 16S ribosomal DNA (rDNA) clone libraries. In addition, several bacteria were found attached to these dinoflagellates by using fluorescent in situ hybridization and confocal scanning laser microscopy. After a stringent washing procedure to remove unattached bacteria, the predominant bacterial species present was a bacterium closely related to Sulfitobacter pontiacus, a Roseobacter clade organism. Also, a Roseobacter sp. was found to be necessary for the growth of Pfiesteria in culture (1).
In this study, we measured the production of DMSP by P. piscicida and P. shumwayae and then assessed DMSP catabolism by the Pfiesteria cultures and the bacterial communities associated with them. New dinoflagellate-associated roseobacters capable of DMSP degradation by both the lyase and demethylation pathways were isolated and identified.
| MATERIALS AND METHODS |
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105 per ml, whereupon feeding was stopped for 36 h, which allowed complete removal of the Rhodomonas algae (monitored by inverted microscopy).
Bacterial strains and media.
Bacteria were isolated from P. piscicida CCMP1830 culture by first spreading a 10-fold dilution series of the dinoflagellate culture on 0.5x Zobell marine agar 2216 (18.7 g of Difco marine broth 2216, 15 g of Difco Bacto Agar, and 1,000 ml of distilled H2O), hereafter referred to as marine agar. After 5 to 7 days of incubation at 30°C, colonies with unique morphologies were picked at random and streaked to purity on marine agar, resulting in the strains TM1034 to TM1042. The bacterial cultures were used after incubation in marine broth (same as marine agar but lacking the agar) at 30°C in a shaking water bath for 1 to 3 days. Escherichia coli INV
F' was grown in Luria-Bertani (LB) broth (4) or on LB agar containing 1.5% Bacto Agar (Becton Dickinson, Franklin Lakes, N.J.).
Chemicals.
DMSP was synthesized from acrylate and DMS according to the method of Chambers et al. (7). The purity of the resulting DMSP was confirmed by chemical analyses, including flash point, melting point, and total C, H, O, N, S, and Cl (Galbraith Laboratories, Inc., Knoxville, Tenn.). MMPA was synthesized by alkaline hydrolysis of its methyl ester, methyl-3-(methylthio)propionate (Aldrich, Milwaukee, Wis.) (21). Other organic sulfur compounds were purchased from Aldrich. All chemicals used were of the highest purity commercially available.
DMSP content and metabolism.
To measure the DMSP contents of the dinoflagellates P. piscicida CCMP1830 and P. shumwayae CCMP2089 and the prey alga Rhodomonas sp. strain CCMP768, cells were grown to a maximum density of
105 per ml in 500-ml batch cultures, except for Rhodomonas sp., which was grown in 1-liter batch cultures to a maximum density of 106 cells per ml. The abundance and cellular volume of the cells were measured in the 7- to 20-µm-diameter particle range from three or more 1-ml samples of culture using a Coulter Multisizer II particle counter (Becton-Dickinson). Because the particle counter does not distinguish between Pfiesteria dinoflagellates and Rhodomonas prey algae, all dinoflagellate cultures were starved to reduce the Rhodomonas population to below detectable limits (as described above).
DMSP was measured in 2-ml whole-culture aliquots and in concentrated cell lysates. To obtain concentrated cell lysates, 200-ml culture aliquots were centrifuged at 4,000 x g for 15 min and the cell pellets were resuspended in 2 ml of sterile distilled water on ice. For Rhodomonas sp. strain CCMP768, multiple cell pellets were combined and resuspended in a final 2-ml aliquot of sterile distilled water. A cell homogenate of each sample was then obtained using a Sonic Dismembrator sonicator (Fisher, Hampton, N.H.). DMSP was measured in 2-ml samples as described in "Analytical techniques" below.
To measure the degradation of DMSP by dinoflagellate and prey algal cultures, cells were grown as described above and the cell density was normalized across all cultures to 104 per ml by diluting the cultures with sterile medium. DMSP was added to the culture from a sterile neutralized stock at a final concentration of 200 µM, and its degradation was measured at intervals throughout the duration of the experiment, as described in "Analytical techniques" below.
The catabolism of DMSP by the bacterial component of each culture was measured in suspensions containing a mixture of dinoflagellate-associated bacteria that were isolated as follows. A 10-fold dilution series of each dinoflagellate culture at peak dinoflagellate density (
105 cells per ml) was spread on marine agar and incubated at 30°C for 5 days. The resulting colonies from plates containing 50 to 200 colonies were resuspended from the agar surface using sterile 10-psu artificial seawater (Instant Ocean, Mentor, Ohio) and washed twice by centrifugation at 14,000 x g, whereupon the optical density was normalized to 0.6 at 600 nm for each suspension. An aliquot of DMSP was then added from a sterile neutralized stock to a final concentration of 1 mM, and DMS, MeSH, MMPA, and acrylate were measured as described in "Analytical techniques" below.
DMSP catabolism was also measured in four bacterial strains (TM1035, TM1038, TM1040, and TM1042) isolated from the dinoflagellate culture. Each strain was grown in a 50-ml marine broth culture amended with 1 mM DMSP to induce the production of enzymes necessary for DMSP catabolism. The cultures were grown to an optical density at 600 nm of 0.6 and washed twice with sterile 10-psu artificial seawater. DMSP was added to a final concentration of either 0.1 or 1 mM, and 1-ml aliquots of the bacterial cultures were dispersed into 26-ml serum bottles. The bottles were immediately capped with a butyl rubber septum and incubated at 30°C with shaking. At intervals throughout the experiment, samples were sacrificed for measurement of DMSP, DMS, MeSH, acrylate, and MMPA as described below.
Analytical techniques.
DMSP was measured as DMS following alkaline hydrolysis. An aliquot of the sample was added to a 26-ml serum bottle with the addition of an equal volume of either 5 M NaOH or distilled water, and the bottle was capped with a butyl rubber septum. Solutions of pure DMSP at 1 to 500 µM dissolved in distilled water were prepared in exactly the same manner in parallel with each experiment. After overnight incubation, DMS resulting from alkaline hydrolysis of DMSP was measured in 500 µl of headspace gas using a Hewlett-Packard 5890 gas chromatograph equipped with flame ionization detection (GC-FID). DMS produced without alkaline hydrolysis was subtracted from the total, and the result was compared to DMS produced from the hydrolysis of pure DMSP standards to obtain the final molar concentration of DMSP in the unknown sample. The retention time of DMS was determined by injecting 50 µl of headspace gas from a capped serum bottle containing 5 µl of pure DMS that had completely volatilized.
DMS and MeSH production in the cultures was measured by direct sampling of 500 µl of headspace gas without prior alkaline hydrolysis of the sample. The concentration of DMS was determined using standard curves generated from known concentrations of DMS produced by complete alkaline hydrolysis of known amounts of DMSP. The concentrations of gaseous MeSH in the cultures were determined from standard curves using a dilution series of pure MeSH gas.
The presence and concentrations of acrylate and MMPA in the cultures were measured by high-performance liquid chromatography (Agilent [Palo Alto, Calif.] 1100 equipped with diode array detection) and a Zorbax XDB C18 column (2.1 by 150 mm; 5-µm pore size) (Agilent) according to the method of Ansede et al. (2).
Statistics.
The Mann-Whitney test for two independent samples was used to compare the DMSP contents of P. piscicida CCMP1830 and P. shumwayae CCMP2089. The apparent first-order rate constants for DMSP degradation and catabolite production by bacterial strains TM1035, TM1038, TM1040, and TM1042 was calculated using a linear least-squares regression analysis of the data, where the slope of the line equals the first-order rate constant (r > 0.90).
DNA methods.
Chromosomal DNA was extracted from bacterial cells by routine methods (36) and used as a template in a PCR to amplify the near-full-length (
1,300-bp) 16S rDNA gene. The PCR conditions were as previously described (1). The resulting PCR products were analyzed by electrophoresis using a 1.0% agarose gel in 1x TAE (4) to confirm the presence of a single 1,300-bp product, which was then excised from the gel using a sterile razor blade, purified using the QIAGEN gel extraction kit, and cloned into the TA cloning vector pCR2.1 (Invitrogen, Carlsbad, Calif.) under the ligation conditions recommended by the manufacturer. Plasmid DNA was transformed into E. coli INV
F' competent cells (Invitrogen). Transformants were selected and screened for DNA insertion using LB agar containing kanamycin (80 µg per ml) plus X-Gal (5-bromo-4-chloro-3-indolyl-ß-D-galactopyranoside; 40 µg per ml). White colonies, i.e., those harboring recombinant plasmids, were picked at random and grown overnight with antibiotic selection. Plasmid DNA was extracted by alkaline lysis and purified by standard methods using a cesium chloride gradient (4). The presence of a near-full-length 16S rDNA insert was confirmed by agarose gel electrophoresis analysis of EcoRI-digested plasmid DNA. The nucleotide sequence of each 16S rDNA was determined as previously described (1).
Nucleotide sequence analysis and phylogenetic-tree construction.
The construction of phylogenetic trees was done as described by Alavi et al. (1). Briefly, evolutionary trees were generated using the neighbor-joining (35), Fitch-Margoliash (11), and maximum-parsimony (29) algorithms in the PHYLIP package (10). Evolutionary-distance matrices for the neighbor-joining and Fitch-Margoliash methods were generated as described by Jukes and Cantor (22). The confidence in tree topology was evaluated after 1,000 bootstrap resamplings of the neighbor-joining data, and only values of
500 were shown on the tree.
Nucleotide sequence accession numbers.
The GenBank accession numbers for the 16S rDNA sequences used to generate phylogenetic trees are as follows: Roseovarius tolerans, Y11551; Roseovarius sp. strain DFL-24, AJ534215; marine bacterium ATAM407-61, AF359525; Sagittula stellata, U58356;
-proteobacterium GMD29C12, AY162070; Roseovarius nubinhibens, AF098495; uncultured Rhodobacter LA1-B32N, AF513928; Roseobacter sp. strain LA7, AF513438; marine bacterium HP29w, AY239008;
-proteobacterium MBIC1887, AB026492; Silicibacter lacuscaerulensis, U77644; Silicibacter pomeroyi, AF098491; marine bacterium P20, AY082668; Reugeria atlantica, AF124521; Reugeria algocolus, X78313; Roseobacter gallaciensis, Y13244; Sulfitobacter mediterraneus, Y17387; Roseobacter denitrificans, X69159; Roseobacter litoralis, X78312; Sulfitobacter sp. strain GAI-37, AF007260; Sulfitobacter sp. strain GAI-21, AF007257; Sulfitobacter pontiacus, Y13155; and Sulfitobacter sp. strain EE36, AF007254. The nucleotide sequences incorporating 1,300 bp of the 16S rDNA gene from strains TM1035, TM1038, TM1040, and TM1042 have been deposited in the GenBank database under accession numbers AY332660, AY332661, AY332662, and AY332663, respectively.
| RESULTS |
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3.44 µM, while that of P. shumwayae is estimated to be 4.25 µM (Table 1). Statistical analyses show that the mean DMSP concentrations and the mean intracellular volumes for the species are not significantly different (P > 0.05).
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Degradation of DMSP by dinoflagellate cultures.
Cultures of P. piscicida, P. shumwayae, and a taxonomically similar dinoflagellate, Cryptoperidiniopsis sp., lacking Rhodomonas, as well as a culture of the prey algae, were analyzed for the ability to degrade DMSP. While Rhodomonas cultures failed to degrade DMSP (data not shown), P. piscicida and Cryptoperidiniopsis cultures degraded exogenously added DMSP within 20 to 30 h of incubation (Fig. 3). In contrast, the P. shumwayae culture was much slower to degrade DMSP, requiring >72 h to achieve complete degradation of the DMSP (data not shown). P. piscicida CCMP1830, Cryptoperidiniopsis sp. strain CCMP1829, and P. shumwayae CCMP2089 were chosen for further analysis.
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100-fold) than the concentration of either MMPA or acrylate. In general, the concentrations of the DMSP catabolites eventually decreased over 20 h, except for MeSH gas, which continued to increase throughout the period. In contrast to these results, the bacterial suspension obtained from the P. shumwayae culture produced only DMS and acrylate and failed to produce either MMPA or MeSH. These data demonstrate that one or more species of DMSP-degrading bacteria are associated with the P. piscicida and Cryptoperidiniopsis dinoflagellates and that both the demethylase and lyase pathways are active. Since the bacterial communities from both the P. piscicida CCMP1830 and Cryptoperidiniopsis sp. strain CCMP1829 cultures showed similar profiles of DMSP catabolism, only bacteria from the P. piscicida CCMP1830 culture were selected for further analysis.
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The kinetics of DMSP degradation and catabolite production were examined in greater detail (Fig. 6). Strains TM1035 and TM1042 have similar colony morphologies (medium size; pink), suggesting that they may be taxonomically closely related. The two strains also produce some of the same DMSP catabolites; however, they differ in both the rate of DMSP degradation and the rate of production of DMS (Fig. 6A and B). Strain TM1035 removed
33% (330 µM) of the added DMSP during a 3-h period and produced
65 µM DMS, 60 µM MMPA, and 16 µM MeSH as a result (Fig. 6A). Production of DMS and MMPA occurred within 30 min, with MeSH production following 1 h later. On the other hand, strain TM1042 removed 19% (190 µM) of the added DMSP during the same 3-h period, producing 236 µM MeSH, 38 µM DMS, and 73 µM MMPA (Fig. 6B). Production of these compounds occurred simultaneously and within 30 min. The first-order rate constants for DMSP degradation and catabolite production were calculated from linear regions of Fig. 6 and are presented in Table 2. TM1035 and TM1042 produced MMPA at similar rates (19.5 and 17.5 µM per h, respectively). MeSH production by strain TM1035 was highly variable across replicate experiments. Therefore, it was not possible to compare the rates of MeSH production in these two strains, although TM1042 always produced higher levels of MeSH (Fig. 5B). TM1042 also had a lower rate of DMSP degradation (32.6 µM per h) than TM1035 (95 µM per h) and a higher rate of DMS production (59.0 µM per h) than TM1035 (22.7 µM per h). These data suggest that, while they produce similar colony phenotypes, TM1035 and TM1042 are physiologically unique, at least in their metabolism of DMSP.
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33% (330 µM) DMSP during a 4-h period, producing 502 µM MeSH and 61 µM MMPA (Fig. 6C). Of the four strains, TM1038 was slowest in degrading DMSP (22.3 µM per h) but had the highest rate of MeSH production (132 µM per h), which was at least an order of magnitude above that of TM1042 (Table 2). The rate of production of MMPA by TM1038 (15.9 µM per h) was quite similar to those of TM1035 (19.5 µM per h) and TM1042 (17.5 µM per h).
The fourth strain, TM1040, catabolized DMSP to produce only MMPA. The cells removed
7% (70 µM) DMSP in a 3-h period while producing only 15 µM MMPA (Fig. 6D). Thus, strain TM1040 has a high rate of DMSP degradation (91 µM per h), but a very low rate of MMPA production (5.1 µM/h), compared to the other three DMSP-degrading strains (Table 2).
Taxonomic identification of DMSP-degrading bacteria.
A taxonomic analysis of the DMSP-metabolizing strains placed the four isolates in the
-Proteobacteria, closely related to the Roseobacter clade (Fig. 7). Strains TM1042 and TM1035 are closely related to each other (99% identity; 1,306 of 1,310 bp) and cluster with another dinoflagellate-associated bacterium, strain ATAM407_61, isolated from the dinoflagellate Alexandrium lustanicum (19). Both TM1035 and TM1042 are also more distantly related to R. tolerans from Ekho Lake (96% [1,246 of 1,294 bp] and 96% [1,248 of 1,294 bp] identity, respectively), which, like strains TM1035 and TM1042, is capable of producing both DMS and MeSH from DMSP (14).
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-proteobacterium, MBIC1887 (99% sequence identity; 1,275 of 1,284 bp), and to a lesser extent showed some relatedness to two well-characterized Silicibacter species, S. pomeroyi and S. lacuscaerulensis (Fig. 7). Both of these Silicibacter species are capable of DMSP degradation (14). | DISCUSSION |
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The results show that both P. piscicida and P. shumwayae contain significant levels of DMSP, which to our knowledge is the first report of DMSP in Pfiesteria and only the second observation of DMSP in a heterotrophic dinoflagellate (28). The DMSP contents of the two Pfiesteria species (3.44 to 4.25 µM) (Table 1) are similar to those measured in other dinoflagellates. For example, the intracellular DMSP concentrations in photosynthetic species, such as Prorocentrum, Gymnodinium, and Amphidinium species, are reported to be 1 to 10 µM (24). Interestingly, the concentration of DMSP in another heterotrophic dinoflagellate, Crypthecodinium cohnii, has been reported to be 10 pg per cell (24), a value that is much higher than those observed in either Pfiesteria species (
0.4 pg per cell). This difference undoubtedly reflects physiological and taxonomic differences between Pfiesteria and Crypthecodinium and underscores the difficulty in making general statements about DMSP physiology among taxonomically diverse dinoflagellate species.
Both P. piscicida and P. shumwayae contain significant levels of DMSP, yet the P. piscicida cultures that include dinoflagellates plus associated bacteria degrade DMSP at significantly higher rates (Fig. 3). Previous data have demonstrated differences in the bacterial flora associated with Pfiesteria cultures (1). Thus, it is conceivable that differences in the compositions of the bacterial communities may affect the rates of DMSP decomposition in P. piscicida and P. shumwayae cultures. The data in Fig. 4 showing the difference between DMSP catabolite kinetics in the mixed culturable heterotrophic bacteria support this idea. Other factors may also be important, including the possibility that slow-growing bacteria in the P. shumwayae culture may have a low rate of DMSP degradation or that the concentration of DMSP used may have a deleterious effect specific to the P. shumwayae bacterial community.
Four DMSP-degrading bacterial isolates were obtained from P. piscicida cultures and were found to be phylogenetically related to members of the Roseobacter clade (Fig. 7). As shown in the taxonomic tree, two of the isolates (TM1035 and TM1042) are most closely related to Roseovarius species, while TM1038 and TM1040 are unique Roseobacter species not related to known roseobacters. Despite their taxonomic differences, all four bacteria shared the common trait of demethylating DMSP to MMPA, while strains TM1035 and TM1042 further metabolize DMSP to produce DMS, indicating that demethylation is a major pathway by which Pfiesteria-associated roseobacters degrade DMSP. Equally interesting are the DMSP demethylation pathways used by these strains. As an example, TM1038 demethylates DMSP to produce MMPA and MeSH, a pathway that appears to be commonly used by marine bacteria (25). In contrast, TM1040 strictly demethylates DMSP to produce MMPA without MeSH, a pathway reported to be used by one other aerobic marine bacterium, strain BIS-6, isolated from Biscayne Bay, Fla. (41). This bacterium demethylates DMSP to MMPA (Fig. 1, reaction 2). followed by a further demethylation to MPA (Fig. 1, reaction 4). Although not measured in this study, TM1040 is likely also to produce MPA instead of MeSH, as has been observed for BIS-6.
The two Roseovarius-related strains, TM1035 and TM1042, are capable of both demethylation and lyase cleavage of DMSP. The presence of dual demethylation-lyase pathways in the same organism is a recently discovered phenomenon. Gonzalez et al. (15) reported that 5 out of 15 DMSP-catabolizing bacteria isolated from Georgia coastal seawater and the Caribbean Sea catabolized DMSP to produce both DMS and MeSH, as well as converted MMPA to MeSH. One of these five isolates was taxonomically identified as R. nubinhibens ISM (15). The capacity to use both DMSP pathways may provide these bacteria with a survival advantage, especially in environments where DMSP concentrations are high, such as the phycosphere surrounding DMSP-producing dinoflagellates. Bacteria that utilize the lyase cleavage pathway are capable of growing on DMSP as a sole carbon source (45). In contrast, while the demethylation pathway does not always lead to increased growth (20), much of the sulfur obtained from this pathway is utilized for protein synthesis and seems to be preferred over other sources of sulfur abundant in seawater (27). Thus, coupling of both DMSP-degradative pathways in the same organism may satisfy both the carbon and sulfur requirements of these dinoflagellate-associated marine bacteria.
In analyses of DMSP catabolism, it was occasionally observed that the sum of the DMSP catabolites produced did not always equal the amount of DMSP lost from the culture. There are several possible explanations for this. First, bacterial enzymes may have degraded the DMSP catabolites shortly after they were produced. This is a strong possibility in light of the high reaction rates observed. A good example supporting this is the failure to detect acrylate production in either TM1035 or TM1042, despite the presence of detectable levels of DMS, which constitutes the other half of lyase cleavage of DMSP. The absence of acrylate is most likely due to rapid conversion, a finding that was also noted by Ansede et al. (2), who, using nuclear magnetic resonance analysis, were unable to detect acrylate production by a Roseobacter species even though DMS was produced. The present results also agree with environmental studies that show rapid degradation of acrylate by bacterial communities associated with algal cells or debris (34).
Another possibility to explain the imbalance in DMSP catabolites is that these chemicals may have been degraded or lost due to abiotic factors, such as oxidation of a compound or the adherence of a catabolite to inanimate surfaces. For example, MeSH is readily oxidized to form dimethyl disulfide and may be lost from water samples due to binding with humic acids (25). In our experiments, a minor loss of MeSH due to sticking to inanimate surfaces was observed (data not shown) and may have resulted in a slight overestimation of total MeSH gas production, which in turn may have contributed to the imbalance between MeSH produced and DMSP degraded.
Pfiesteria and other heterotrophic dinoflagellates are in intimate association with a community of bacteria, many of which are members of the Roseobacter clade, which interact in a myriad of ways with their eukaryotic partner. Roseobacter clade bacteria have been observed attached to or physically associated with dinoflagellate cells, while other Roseobacter species are required for dinoflagellate growth (1). It is tantalizing to think that DMSP is involved in these associations, particularly in view of the diversity of DMSP pathways and the high rates of reactions seen in the Pfiesteria cultures and the Roseobacter isolates obtained from them. These results also bring up new questions about roseobacters, DMSP, and dinoflagellate interactions. Are Roseobacter clade bacteria attracted to DMSP or one of its catabolites, which may bring them into close proximity to dinoflagellate cells? Do the catabolites of DMSP have physiological functions in dinoflagellate metabolism, behavior, or growth? In the long term, answers to these questions will provide significant clues about the molecular and cellular natures of the interactions between bacteria, dinoflagellates, and other single-cell eukaryotes.
| ACKNOWLEDGMENTS |
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This work was supported by grants from NOAA ECOHAB (NA86OP0492) and NIH NIEHS (PO1-ES9563).
| FOOTNOTES |
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This is COMB publication number O4-649 and ECOHAB publication number 121. ![]()
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