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Microbiology Fixation and fate of C and N in the cyanobacterium Trichodesmium using nanometer-scale secondary ion mass spectrometry aWrigley Institute for Environmental Studies and Department of Biological Sciences, University of Southern California, 3616 Trousdale Parkway, Los Angeles, CA 90089-0373; bLawrence Livermore National Laboratory, PO Box 808, L-231, Livermore, CA 94551-0808; cDepartment of Biology, Portland State University, PO Box 751, Portland, OR 97207-0751; and dResearch School of Earth Sciences, The Australian National University, Mills Road, Canberra ACT 0200, Australia 2To whom correspondence should be addressed. E-mail: jahart/at/usc.edu Edited by David M. Karl, University of Hawaii, Honolulu, HI, and approved February 20, 2009 Author contributions: J.A.F.-H., R.P., and D.G.C. designed research; J.A.F.-H., J.P.-R., P.K.W., S.J.F., and T.G. performed research; P.K.W., I.D.H., and K.H.N. contributed new reagents/analytic tools; J.A.F.-H., J.P.-R., and P.K.W. analyzed data; and J.A.F.-H., J.P.-R., P.K.W., and D.G.C. wrote the paper. 1J.A.F.-H. and J.P.-R contributed equally to this work. Received October 22, 2008. This article has been corrected. See Proc Natl Acad Sci U S A. 2009 June 16; 106(24): 9931.Abstract The marine cyanobacterium Trichodesmium is ubiquitous in tropical and subtropical seas and is an important contributor to global N and C cycling. We sought to characterize metabolic uptake patterns in individual Trichodesmium IMS-101 cells by quantitatively imaging 13C and 15N uptake with high-resolution secondary ion mass spectrometry (NanoSIMS). Trichodesmium fix both CO2 and N2 concurrently during the day and are, thus, faced with a balancing act: the O2 evolved during photosynthesis inhibits nitrogenase, the key enzyme in N2 fixation. After performing correlated transmission electron microscopy (TEM) and NanoSIMS analysis on trichome thin-sections, we observed transient inclusion of 15N and 13C into discrete subcellular bodies identified as cyanophycin granules. We speculate that Trichodesmium uses these dynamic storage bodies to uncouple CO2 and N2 fixation from overall growth dynamics. We also directly quantified both CO2 and N2 fixation at the single cell level using NanoSIMS imaging of whole cells in multiple trichomes. Our results indicate maximal CO2 fixation rates in the morning, compared with maximal N2 fixation rates in the afternoon, bolstering the argument that segregation of CO2 and N2 fixation in Trichodesmium is regulated in part by temporal factors. Spatial separation of N2 and CO2 fixation may also have a role in metabolic segregation in Trichodesmium. Our approach in combining stable isotope labeling with NanoSIMS and TEM imaging can be extended to other physiologically relevant elements and processes in other important microbial systems. Keywords: NanoSIMS, stable isotope labeling, cyanophycin The marine cyanobacterium Trichodesmium is ubiquitous in tropical and subtropical seas and is an important contributor to global N and C cycling (1). As a diazotrophic cyanobacterium, Trichodesmium is capable of both CO2 and N2 fixation. Studies have estimated that it may leak up to 30–50% of its newly fixed N (2), providing a valuable source of bioavailable N to other nondiazotrophic phytoplankton species cohabitating in the N-limited subtropical gyres. Capone et al. (3) estimate that it contributes ≈5.7 Tmol new N y−1 in the North Atlantic Ocean, which is comparable with the rate of NO3− that diffuses from depth into oligotrophic upper ocean ecosystems (3, 4). Although Trichodesmium is not the sole diazotrophic cyanobacteria in the open ocean (5–7), it is the most conspicuous and well-studied. Also, it has been in culture since 1992 (8), allowing numerous studies of its physiology and response to different limiting and controlling factors. Trichodesmium is often included in ecosystem models that attempt to describe CO2 and N2 fixation in open ocean systems (9). A better understanding of CO2 and N2 fixation in Trichodesmium is critical, because this species has a large role in global C and N cycling in the open ocean. Commonly referred to as “saw dust” on the surface of the sea (10), Trichodesmium grows in filaments (referred to as trichomes) that can have 100–200 cells (Fig. 1
Diazotrophy is a significant challenge for unicellular microorganisms, because the O2 produced from CO2 fixation is inhibitory to nitrogenase, the key enzyme in N2 fixation. Therefore, diazotrophs have developed different behavioral, biochemical, and physical strategies to protect nitrogenase from the O2 evolved during photosynthesis. Certain cyanobacteria, such as Gloeothece spp., temporally segregate the processes over a diel cycle by fixing CO2 during the day and fixing N2 at night (15). Others, such as Anabaena spp., have terminally differentiated cells, termed heterocysts, with thickened cell walls, and reduced PS II and rubisco activity (16). These cells serve to spatially segregate the 2 processes, with N2 fixation occurring in the heterocysts, whereas oxygenic photosynthesis and CO2 fixation occurs in vegetative cells. Trichodesmium is unique in that it is a nonheterocystous cyanobacteria that fixes both CO2 and N2 concurrently during the day (1). There is considerable current debate among researchers as to how these processes co-occur. Current theories, and sometimes conflicting data, suggest increased O2 consumption within cells protects nitrogenase [e.g., increased hydrogenase (17), Mehler (18, 19), and superoxide dismutase activity (20)], in addition to both spatial (21–23) and temporal segregation of CO2 and N2 fixation (19, 24, 25). Much of the current debate revolves around the metabolic potential of individual cells in a trichome, and how those capabilities may differ among cells in a trichome or within individual cells over time (26). To investigate the dynamics of C and N metabolism at this level, we combined tracer-level additions of inorganic 13C and 15N with high-resolution secondary ion mass spectrometry (NanoSIMS; Cameca). NanoSIMS imaging allowed us to track C and N stable isotope incorporation rates and subsequent cellular fates by mapping distributions of isotopes (27) in multiple trichomes. The results of our NanoSIMS investigations are compared with bulk isotopic analyses and related to existing models of Trichodesmium metabolism. Results and Discussion NanoSIMS imaging was performed on Trichodesmium trichomes spiked with NaH13CO3 and 15N2, and harvested sequentially during 24 h (see Materials and Methods). Both whole- and thin-sectioned samples were imaged to quantify the distribution of newly fixed 13C and 15N within trichomes. The distribution of newly fixed 13C and 15N was determined by simultaneously imaging C and N isotopes and calculating quantitative 13C/12C and 15N/14N ratio images. Each 10-μm2 image includes 2 to 3 cells, and was scanned with 150-nm resolution to capture intercellular variability. Multiple adjacent cells along multiple trichomes were analyzed to quantify cell–cell variability. For thin-sectioned trichomes, we used transmission electron microscopy (TEM) imaging to morphologically map samples before NanoSIMS analysis. NanoSIMS analysis showed substantial subcellular spatial variability in 15N and 13C enrichment along Trichodesmium trichomes and with depth through individual cells (Figs. 2
NanoSIMS analysis also allowed us to examine subcellular isotope enrichment in the vertical dimension of cells. Based on analyses of multiple cells examined from multiple trichomes and time points, we determined that cyanophycin granules can comprise up to 6.4% (± 0.7%) of cell area/volume, and are evenly distributed along trichomes. In depth profile analyses of whole cells, as the NanoSIMS analyzed deeper and deeper layers, individual cyanophycin granules became apparent, and then disappeared as the ion beam sputtered through them (Fig. 4 Previous studies have examined the transient nature of cyanophycin granules in single-celled and heterocystous diazotrophs. Sherman et al. (30) used immunocytochemical analysis to demonstrate the localization of cyanophycin at the polar plugs of mature heterocysts in Anabaena sp. PCC7120. Mackerras et al. (33) used cultures of Anabaena cylindrica (a heterocystous cyanobacteria) and Synechocystis 6308 (a unicellular cyanobacteria that temporally segregates CO2 and N2 fixation) grown in media with limited ammonium concentration ([NH4+]). They demonstrate that synthesis and subsequent degradation of cyanophycin granules in these 2 organisms as [NH4+] in the media is drawn down, indicating that the 2 cyanobacteria produce cyanophycin granules in N-replete conditions and use the stores during N-deplete conditions. Our study demonstrates the dynamic nature of the cyanophycin pool in Trichodesmium grown under diazotrophic conditions. Transient accumulation of cyanophycin indicates an uncoupling of CO2 and N2 fixation with cell growth. Interestingly, recent modeling of Trichodesmium metabolism (34) suggested that storage pools of C and N are dynamic over the diel cycle, accumulating during the day and consumed during the dark period. Our results provide direct evidence for this prediction. In more than half of the trichomes analyzed from the 8- and 24-h incubations, we observed a marked reduction in 13C and 15N enrichment in cells located near the middle of trichomes (Fig. 5
We used NanoSIMS analysis of whole cells to calculate uptake rates of CO2 and N2 fixation at the single cell level. These data were averaged for 40–120 contiguous cells located in multiple trichomes from each time point (Fig. 6
A controversial and evolving area of debate in the field of Trichodesmium physiology has been the suggestion that CO2 and N2 fixation within Trichodesmium are spatially segregated between different cells. The earliest microautoradiography studies suggested that spatial segregation happens at the level of the colony, with anoxic microzones occurring near the center of aggregates, where N2 fixation was localized and photosynthesis down-regulated (36, 37). This theory was later questioned, when it was demonstrated that individual trichomes from disrupted colonies still fix both N2 and CO2 (38). More recently, conflicting immunochemical studies have examined the distribution of nitrogenase proteins along trichome cells. Some studies (23, 39) indicate that nitrogenase is dispersed throughout all cells in colonies, whereas other research suggests that only ≈15% of cells along a trichome contain nitrogenase (21, 22), and that these cells occur in clusters along the trichome (21, 32). These clusters, referred to as diazocytes, suggest a spatial segregation of N2 fixation and CO2 fixation. It should be noted that cells that contain nitrogenase are not necessarily photosynthetically inactive (15). In our study, after 2 h of exposure to labeled isotopes, newly fixed 13C and 15N was apparent and relatively evenly distributed in all cells along trichomes (Fig. 2 Nonetheless, the accumulation of recently fixed 13C and 15N in individual cells appears uniform, and is significantly correlated with an average r2 = 0.4 (Fig. 2 Conclusion In summary, the NanoSIMS approach has allowed us to examine in detail the distribution and uptake ratio of CO2 and N2 in individual cells of a Trichodesmium trichome, and to compare patterns of distribution and uptake among cells in the trichome and over the diel cycle. We observed the uptake of newly fixed CO2 and N2 within all cells along a Trichodesmium trichome, as well as the dynamic nature of cyanophycin granules, which accumulate in cells during the light period and are metabolized and assimilated into cellular biomass during the dark period. These patterns suggest a temporal uncoupling of metabolic processes operating over the diel period in Trichodesmium. We have also provided direct evidence at a cellular level for a temporal decoupling of CO2 and N2 fixation in the trichome, with maximal CO2 fixation occurring early in the day and maximal N2 fixation occurring later in the day. We did not find evidence for specialized diazocyte cells; and if there is a “division of labor” in Trichodesmium trichomes, it is very transient, or occurs by some other mechanism. Unraveling the ecological and physiological complexities of this globally important organism remains an ongoing challenge. As present investigations reveal, a combined analysis approach, incorporating stable isotope labeling, modern imaging technologies (NanoSIMS, TEM, and SEM), and in situ molecular identification, may be critical to advanced studies of microbial metabolism. Materials and Methods Trichodesmium IMS-101 cultures were grown at 27 °C in 2-L polycarbonate culture bottles with YBCII liquid media (43) at an irradiance of 80 μE m−2 s−1 on a 12-h light/12-h dark cycle beginning at 8 AM. Subsamples of 165 mL were incubated in sealed 165 mL of serum vials. To each vial, we injected 0.07 mL NaH13CO3 (≈99 atom percentage 13C, 0.04 M, final 13C enrichment 1.9 atom percentage DIC; Cambridge Isotope Laboratories) and 0.3 mL 99 atom percentage 15N2 gas (Isotech Associates) (final N2 enrichment 16.2 atom percentage). There was no headspace in the bottles to ensure no dilution of the 15N2 added with atmospheric 15N2. Subsamples were returned to the incubator, and kept in the conditions described above until their predetermined harvest time. At 8 time points (0 min, 15 min, 30 min, 1 h, 2 h, 4 h, 8 h, and 24 h), 1 mL of sample was harvested and preserved in 2% glutaraldehyde for SIMS analysis. For the first time point (0 min), isotopes were injected, and then the sample was immediately harvested (i.e., within <30 s of injection). Experiments were initiated at 10 AM. For NanoSIMS microanalysis, multiple whole Trichodesmium trichomes were filtered, washed with Milli-Q H2O, and dried onto a silica chip. SIMS was performed at Lawrence Livermore National Laboratory by using a Cameca NanoSIMS 50 instrument, according to previously described methods (41). Briefly, a ≈2pA Cs+ primary beam focused to ≈150 nm was scanned across a 256 × 256 pixel 10–15 μm2 raster to generate secondary ions in ≈20 serial quantitative secondary ion images. Electron multiplier detectors collected 12C−, 13C−, 12C14N−, 12C15N−, and 31P− ions, and secondary electrons were simultaneously imaged. The NanoSIMS was tuned for ≈7,000 mass resolving power to resolve isobaric interferences. Samples were presputtered to at least 100 nm to achieve sputtering equilibrium; depth of measurement analysis ranged from 200 to 350 nm. For each time point, 4–5 trichomes were analyzed. We include data in Figs. 2 For each time point, a sample (50–75 mL) of bulk cell biomass was filtered onto precombusted GF/F filters and dried. The isotope ratio of these samples was analyzed at the University of Southern California Stable Isotope Facility on a VG IsoPrime interfaced to an elemental analyzer run in continuous flow mode. Supporting Information
Acknowledgments. We thank John Waterbury (Wood Hole Oceanographic Institution, Woods Hole, MA) for providing us his Trichodesmium culture, IMS-101; Rachel Foster (University of California Santa Cruz) and Ed Carpenter (San Francisco State University) for their aid in identifying cyanophycin in the TEM images; Larry Nittler (Carnegie Institute of Washington) for software development; Christina Ramon [Lawrence Livermore National Laboratory (LLNL)] for assistance with sample preparation for NanoSIMS and TEM analysis; and 3 anonymous reviewers, who provided valuable comments that helped improve the manuscript. This work was supported in part by the U.S. Department of Education Office of Biological and Environmental Research Genomics Genomes to Life Research Program (J.P.-R. and P.K.W.), and the National Science Foundation Ocean Science Program Grants OCE 0452765 and OCE 0753218. LLNL was supported by U.S. Department of Energy Contract DE-AC52-07NA27344. 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Appl Environ Microbiol. 1994 Nov; 60(11):3996-4000.
[Appl Environ Microbiol. 1994]Nature. 2001 Aug 9; 412(6847):635-8.
[Nature. 2001]Appl Environ Microbiol. 2004 Feb; 70(2):765-70.
[Appl Environ Microbiol. 2004]Nature. 2004 Aug 26; 430(7003):1027-32.
[Nature. 2004]Appl Environ Microbiol. 1993 May; 59(5):1367-1375.
[Appl Environ Microbiol. 1993]Annu Rev Microbiol. 1973; 27():283-316.
[Annu Rev Microbiol. 1973]Appl Environ Microbiol. 1998 Aug; 64(8):3052-8.
[Appl Environ Microbiol. 1998]Science. 2001 Nov 16; 294(5546):1534-7.
[Science. 2001]Plant Physiol. 2004 Aug; 135(4):2120-33.
[Plant Physiol. 2004]J Biol. 2006; 5(6):20.
[J Biol. 2006]Proc Natl Acad Sci U S A. 1971 Feb; 68(2):265-267.
[Proc Natl Acad Sci U S A. 1971]Appl Environ Microbiol. 1998 Aug; 64(8):3052-8.
[Appl Environ Microbiol. 1998]Microbiology. 2003 May; 149(Pt 5):1139-46.
[Microbiology. 2003]Appl Environ Microbiol. 2006 May; 72(5):3217-27.
[Appl Environ Microbiol. 2006]Science. 2001 Nov 16; 294(5546):1534-7.
[Science. 2001]Science. 2001 Nov 16; 294(5546):1534-7.
[Science. 2001]Plant Physiol. 2004 Aug; 135(4):2120-33.
[Plant Physiol. 2004]Science. 1976 Mar 26; 191(4233):1278-80.
[Science. 1976]Appl Environ Microbiol. 1989 Nov; 55(11):2965-2975.
[Appl Environ Microbiol. 1989]Appl Environ Microbiol. 1998 Aug; 64(8):3052-8.
[Appl Environ Microbiol. 1998]Microbiology. 2003 May; 149(Pt 5):1139-46.
[Microbiology. 2003]J Cell Biol. 1974 May; 61(2):440-53.
[J Cell Biol. 1974]ISME J. 2007 Aug; 1(4):354-60.
[ISME J. 2007]ISME J. 2007 Aug; 1(4):354-60.
[ISME J. 2007]ISME J. 2007 Aug; 1(4):354-60.
[ISME J. 2007]Appl Environ Microbiol. 2008 May; 74(10):3143-50.
[Appl Environ Microbiol. 2008]