NITROGEN FIXATION,HYDROGEN CYCLING,AND ELECTRON TRANSPORT KINETICS IN TRICHODESMIUM ERYTHRAEUM (CYANOBACTERIA) STRAIN IMS1011

This study describes the relationships between dinitrogen (N₂) fixation, dihydrogen (H₂) production, and electron transport associated with photosynthesis and respiration in the marine cyanobacterium Trichodesmium erythraeum Ehrenb. strain IMS101. The ratio of H₂ produced:N₂ fixed (H₂:N₂) was controlled by the light intensity and by the light spectral composition and was affected by the growth irradiance level. For Trichodesmium cells grown at 50 μmol photons · m^?2 · s^?1, the rate of N₂ fixation, as measured by acetylene reduction, saturated at light intensities of 200 μmol photons · m^?2 · s^?1. In contrast, net H₂ production continued to increase with light levels up to 1,000 μmol photons · m^?2 · s^?1. The H₂:N₂ ratios increased monotonically with irradiance, and the variable fluorescence measured using a fast repetition rate fluorometer (FRRF) revealed that this increase was accompanied by a progressive reduction of the plastoquinone (PQ) pool. Additions of 2,5‐dibromo‐3‐methyl‐6‐isopropyl‐p‐benzoquinone (DBMIB), an inhibitor of electron transport from PQ pool to PSI, diminished both N₂ fixation and net H₂ production, while the H₂:N₂ ratio increased with increasing level of PQ pool reduction. In the presence of 3‐(3,4‐dichlorophenyl)‐1,1‐dimethylurea (DCMU), nitrogenase activity declined but could be prolonged by increasing the light intensity and by removing the oxygen supply. These results on the coupling of N₂ fixation and H₂ cycling in Trichodesmium indicate how light intensity and light spectral quality of the open ocean can influence the H₂:N₂ ratio and modulate net H₂ production.     

GROWTH AND CARBON CONTENT OF THREE DIFFERENT‐SIZED DIAZOTROPHIC CYANOBACTERIA OBSERVED IN THE SUBTROPICAL NORTH PACIFIC1

To develop tools for modeling diazotrophic growth in the open ocean, we determined the maximum growth rate and carbon content for three diazotrophic cyanobacteria commonly observed at Station ALOHA (A Long‐term Oligotrophic Habitat Assessment) in the subtropical North Pacific: filamentous nonheterocyst‐forming Trichodesmium and unicellular Groups A and B. Growth‐irradiance responses of Trichodesmium erythraeum Ehrenb. strain IMS101 and Crocosphaera watsonii J. Waterbury strain WH8501 were measured in the laboratory. No significant differences were detected between their fitted parameters (±CI) for maximum growth rate (0.51 ± 0.09 vs. 0.49 ± 0.17 d^?1), half‐light saturation (73 ± 29 vs. 66 ± 37 μmol quanta · m^?2 · s^?1), and photoinhibition (0 and 0.00043 ± 0.00087 [μmol quanta · m^?2 · s^?1]^?1). Maximum growth rates and carbon contents of Trichodesmium and Crocosphaera cultures conformed to published allometric relationships, demonstrating that these relationships apply to oceanic diazotrophic microorganisms. This agreement promoted the use of allometric models to approximate unknown parameters of maximum growth rate (0.77 d^?1) and carbon content (480 fg C · μm^?3) for the uncultivated, unicellular Group A cyanobacteria. The size of Group A was characterized from samples from the North Pacific Ocean using fluorescence‐activated cell sorting and real‐time quantitative PCR techniques. Knowledge of growth and carbon content properties of these organisms facilitates the incorporation of different types of cyanobacteria in modeling efforts aimed at assessing the relative importance of filamentous and unicellular diazotrophs to carbon and nitrogen cycling in the open ocean.     

Combined effects of different CO2 levels and N sources on the diazotrophic cyanobacterium Trichodesmium

To predict effects of climate change and possible feedbacks, it is crucial to understand the mechanisms behind CO₂ responses of biogeochemically relevant phytoplankton species. Previous experiments on the abundant N₂ fixers Trichodesmium demonstrated strong CO₂ responses, which were attributed to an energy reallocation between its carbon (C) and nitrogen (N) acquisition. Pursuing this hypothesis, we manipulated the cellular energy budget by growing Trichodesmium erythraeum IMS101 under different CO₂ partial pressure (pCO₂) levels (180, 380, 980 and 1400 µatm) and N sources (N₂ and NO₃^?). Subsequently, biomass production and the main energy‐generating processes (photosynthesis and respiration) and energy‐consuming processes (N₂ fixation and C acquisition) were measured. While oxygen fluxes and chlorophyll fluorescence indicated that energy generation and its diurnal cycle was neither affected by pCO₂ nor N source, cells differed in production rates and composition. Elevated pCO₂ increased N₂ fixation and organic C and N contents. The degree of stimulation was higher for nitrogenase activity than for cell contents, indicating a pCO₂ effect on the transfer efficiency from N₂ to biomass. pCO₂‐dependent changes in the diurnal cycle of N₂ fixation correlated well with C affinities, confirming the interactions between N and C acquisition. Regarding effects of the N source, production rates were enhanced in NO₃^? grown cells, which we attribute to the higher N retention and lower ATP demand compared with N₂ fixation. pCO₂ effects on C affinity were less pronounced in NO₃^? users than N₂ fixers. Our study illustrates the necessity to understand energy budgets and fluxes under different environmental conditions for explaining indirect effects of rising pCO₂.     

A REVISED ESTIMATE OF THE IRON USE EFFICIENCY OF NITROGEN FIXATION,WITH SPECIAL REFERENCE TO THE MARINE CYANOBACTERIUM TRICHODESMIUM SPP. (CYANOPHYTA)1

Estimates of the iron use efficiency (IUE) for diazotrophic plant growth have been used to suggest iron limitation of marine N₂ fixation. However, in the course of these inferences, neither the physiological complexity of these estimates nor the specific physiological parameters of marine diazotrophs were evaluated. Here, a semiempirical prediction of the IUE of diazotrophic growth for Trichodesmium was computed from considerations of the Fe content and reaction rates of the nitrogenase complex and PSI:PSII ratios, as well as field measurements of Mehler activity, cellular Fe‐superoxide dismutase activity, and diel variability in C and N₂ fixation. With a PSI:PSII ratio of 1 and 48% Mehler activity, the instantaneous IUE (0.33 mol C fixed·mol cellular Fe ^{? 1} 1 Received 16 August 2001. Accepted 7 October 2002. ·s ^{? 1} 1 Received 16 August 2001. Accepted 7 October 2002. ) was only 4‐fold lower than that calculated for a phytoplankter growing on reduced N. We computed a range of daily integrated IUE values from 2900 to 7700 mol C·mol Fe ^{? 1} 1 Received 16 August 2001. Accepted 7 October 2002. ·d ^{? 1} 1 Received 16 August 2001. Accepted 7 October 2002. , accounting for the diel variability in C and N₂ fixation as well as the uncertainties in cyanobacterial nitrogenase biochemistry and PSI:II ratios of field‐collected Trichodesmium. The lowest observed Fe‐superoxide dismutase:C quota of 2.9 (μmol:mol) suggests a maintenance requirement for this enzyme. The maintenance Fe:C requirement of 13.5 μmol:mol (derived from cultures of Trichodesmium IMS 101) and values of the IUE yielded an Fe requirement ranging from 27 to 48 Fe:C (μmol:mol) to achieve a diazotrophic growth rate of 0.1 d ^{? 1} 1 Received 16 August 2001. Accepted 7 October 2002. . Based on these predicted requirements, the Fe:C contents of Caribbean Sea and most North Atlantic Ocean populations sampled thus far exceed that required to support the observed rates of N₂ fixation.     

THE EFFECT OF IRON NUTRITION ON PHOTOSYNTHESIS AND NITROGEN FIXATION IN CULTURES OF TRICHODESMIUM (CYANOPHYCEAE)1

Cultures of Trichodesmium NIBB 1067 were grown in the synthetic medium AQUIL with a range of iron added from none to 5 × 10^?7 M Fe for 15 days. Chlorophyll-a, cell counts, and total cell volume were two or three times higher in medium with 10^?7 M Fe than with no added Fe. Oxygen production rate per chlorophyll-a was over 60% higher with higher iron. Increased iron stimulated photosynthesis at all irradiances from about 12–250 μE · m^?2· s^?1. Nitrogen fixation rate, estimated from acetylene reduction, for 10^?7 and 10^?8 M Fe cultures was approximately twice that of the cultures with no added Fe. The range of rates of O₂ production and N₂ fixation in cultures at the iron concentrations we used were similar to the rates from natural samples of Trichodesmium from both the Atlantic, and the Pacific oceans. This similarity may allow this clone to be used, with some caution, for future physiological ecology studies. This study demonstrates the importance of iron to photosynthesis and nitrogen fixation and suggests that Trichodesmium plays a central role in the biogeochemical cycles of iron, carbon and nitrogen.     

PHOSPHATE UPTAKE AND GROWTH KINETICS OF TRICHODESMIUM (CYANOBACTERIA) ISOLATES FROM THE NORTH ATLANTIC OCEAN AND THE GREAT BARRIER REEF,AUSTRALIA1

We compared inorganic phosphate (P_i) uptake and growth kinetics of two cultures of the diazotrophic cyanobacterium Trichodesmium isolated from the North Atlantic Ocean (IMS101) and from the Great Barrier Reef, Australia (GBRTRLI101). Phosphate‐limited cultures had up to six times higher maximum P_i uptake rates than P‐replete cultures in both strains. For strain GBRTRLI101, cell‐specific P_i uptake rates were nearly twice as high, due to larger cell size, but P‐specific maximum uptake rates were similar for both isolates. Half saturation constants were 0.4 and 0.6 μM for P_i uptake and 0.1 and 0.2 μM for growth in IMS101 and GBRTRLI101, respectively. Phosphate uptake in both strains was correlated to growth rates rather than to light or temperature. The cellular phosphorus quota for both strains increased with increasing P_i up to 1.0 μM. The C:P ratios were 340–390 and N:P ratios were 40–45 for both strains under severely P‐limited growth conditions, similar to reported values for natural populations from the tropical Atlantic and Pacific Oceans. The C:P and N:P ratios were near Redfield values in medium with >1.0 μM P_i. The North Atlantic strain IMS101 is better adapted to growing on P_i at low concentrations than is GBRTRLI101 from the more P_i‐enriched Great Barrier Reef. However, neither strain can achieve appreciable growth at the very low (nanomolar) P_i concentrations found in most oligotrophic regimes. Phosphate could be an important source of phosphorus for Trichodesmium on the Great Barrier Reef, but populations growing in the oligotrophic open ocean must rely primarily on dissolved organic phosphorus sources.     

Combined Effects of CO2 and Light on the N2-Fixing Cyanobacterium Trichodesmium IMS101: A Mechanistic View

The marine diazotrophic cyanobacterium Trichodesmium responds to elevated atmospheric CO₂ partial pressure (pCO₂) with higher N₂ fixation and growth rates. To unveil the underlying mechanisms, we examined the combined influence of pCO₂ (150 and 900 μatm) and light (50 and 200 μmol photons m⁻² s⁻¹) on Trichodesmium IMS101. We expand on a complementary study that demonstrated that while elevated pCO₂ enhanced N₂ fixation and growth, oxygen evolution and carbon fixation increased mainly as a response to high light. Here, we investigated changes in the photosynthetic fluorescence parameters of photosystem II, in ratios of the photosynthetic units (photosystem I:photosystem II), and in the pool sizes of key proteins involved in the fixation of carbon and nitrogen as well as their subsequent assimilation. We show that the combined elevation in pCO₂ and light controlled the operation of the CO₂-concentrating mechanism and enhanced protein activity without increasing their pool size. Moreover, elevated pCO₂ and high light decreased the amounts of several key proteins (NifH, PsbA, and PsaC), while amounts of AtpB and RbcL did not significantly change. Reduced investment in protein biosynthesis, without notably changing photosynthetic fluxes, could free up energy that can be reallocated to increase N₂ fixation and growth at elevated pCO₂ and light. We suggest that changes in the redox state of the photosynthetic electron transport chain and posttranslational regulation of key proteins mediate the high flexibility in resources and energy allocation in Trichodesmium. This strategy should enable Trichodesmium to flourish in future surface oceans characterized by elevated pCO₂, higher temperatures, and high light.The marine filamentous N₂-fixing (diazotrophic) cyanobacteria Trichodesmium spp. bloom extensively in the oligotrophic subtropical and tropical oceans (Carpenter and Capone, 2008). Trichodesmium contributes 25% to 50% of the estimated rates of N₂ fixation in these areas, where the new nitrogen inputs stimulate carbon and nitrogen cycling (Capone and Subramaniam, 2005; Mahaffey et al., 2005). The increases in atmospheric CO₂ partial pressure (pCO₂) and the subsequent impacts on ocean acidification are predicted to influence diazotrophs and specifically Trichodesmium.The reported sensitivity of Trichodesmium to changes in pCO₂ prompted further investigation into the cellular responses and underlying mechanisms, specifically when combined with other environmental parameters such as temperature, nutrient availability, and light. Elevated pCO₂ significantly increased growth and N₂ fixation rates of Trichodesmium cultures (Barcelos é Ramos et al., 2007; Hutchins et al., 2007; Levitan et al., 2007, 2010). The physiological response was also characterized by changes in inorganic carbon acquisition, limited flexibility of carbon-nitrogen ratios, and conservation of photosynthetic activities with increased pCO₂. These manifestations suggested that ATP and reductants [ferredoxin, NAD(P)H] are reallocated in the cells (Levitan et al., 2007, 2010; Kranz et al., 2009, 2010).In Trichodesmium, as in all cyanobacteria, the metabolic pathways of respiration and photosynthesis share several cellular complexes/proteins such as the plastoquinone (PQ) pool, succinate dehydrogenase, and ferredoxin (Fig. 1; Kana, 1993; Bergman et al., 1997; Lin et al., 1998). Energetic currencies [reduced ferredoxin, ATP, NAD(P)H] are also shared and can be allocated and utilized according to cellular requirements. N₂ fixation by nitrogenase and the subsequent assimilation of NH₄⁺ by Gln synthetase requires carbon skeletons from the tricarboxylic acid reactions. Moreover, linear and pseudocyclic photosynthesis can also generate additional ATP and reductants essential for N₂ fixation (Fig. 1; Berman-Frank et al., 2001).Open in a separate windowFigure 1.Schematic representation of major cellular complexes involved in energy flow [electron, ATP, NAD(P)H, carbon skeletons] in Trichodesmium IMS101. Dashed arrows represent movement direction of electrons, and solid arrows represent directions of protons, ATP, and NAD(P)H. Measured protein subunits are represented by gray diamonds. See Kranz et al. (2010) for measurements of O₂ evolution, inorganic carbon fixation, and fluxes of N₂ fixation.To understand the regulation of these metabolic pathways in Trichodesmium under varying pCO₂ levels and light intensities, we designed an experiment to characterize changes in the fluxes of carbon, nitrogen, and oxygen (O₂), related protein pool sizes, and variable fluorescence parameters of PSII. Elevated atmospheric pCO₂ combined with enhanced sea surface temperatures are forecast to stabilize thermal stratification, resulting in a shallower, more acidified, upper mixed layer characterized by higher mean light intensities (Doney, 2006). Thus, Trichodesmium IMS101 cultures were acclimated to past and future pCO₂ levels (150 and 900 μatm) at low and high light (50 and 200 μmol photons m⁻² s⁻¹).In the first part of this combined report (Kranz et al., 2010), we examined the physiological responses to the different acclimation conditions. The combination of elevated pCO₂ and light enhanced the production of particulate organic carbon and nitrogen (270% and 390% increase, respectively) as well as growth rates (180% increase; percentages are calculated from Kranz et al., 2010). Generally, the pCO₂-dependent stimulation was higher in cultures acclimated to low light. The pCO₂ effect was also reflected in other measured physiological parameters, particularly the diel patterns of N₂ fixation and the integrated N₂ fixation rates during the day, which increased approximately 30-fold between the low-pCO₂/low-light and the high-pCO₂/high-light acclimations (Kranz et al., 2010). While at high light, elevated pCO₂ extended the period of high N₂ fixation, which lasted from 5 h after the onset of light throughout the end of the photoperiod, the high-pCO₂ contribution to the integrated N₂ fixation was more significant at low light (Kranz et al., 2010). Light, but not pCO₂, influenced gross photosynthesis as measured by PSII O₂ evolution, which increased by approximately 250% in high-light-acclimated cultures. To supply the Calvin cycle with sufficient CO₂, Trichodesmium possesses a CO₂-concentrating mechanism mainly based on HCO₃⁻ uptake (Kranz et al., 2009, 2010). When Trichodesmium was acclimated to elevated pCO₂ (900 μatm), a decline in the cellular affinity to dissolved inorganic carbon was observed (Kranz et al., 2009), while the specific uptake of CO₂ showed a 9-fold increase between the low-pCO₂/low-light and the high-pCO₂/high-light acclimations (Kranz et al., 2010).Proteins are fundamental cellular components that influence the underlying mechanisms subsequently reflected in the cells’ physiology. In this study, we extend the experimental results presented by Kranz et al. (2010) by examining the influence of pCO₂ at different light regimes on the photosynthetic fluorescence parameters of PSII and on the pool sizes of key proteins involved in carbon and nitrogen fixation and their subsequent assimilation processes.     

Combined Effects of CO2 and Light on the N2-Fixing Cyanobacterium Trichodesmium IMS101: Physiological Responses

Recent studies on the diazotrophic cyanobacterium Trichodesmium erythraeum (IMS101) showed that increasing CO₂ partial pressure (pCO₂) enhances N₂ fixation and growth. Significant uncertainties remain as to the degree of the sensitivity to pCO₂, its modification by other environmental factors, and underlying processes causing these responses. To address these questions, we examined the responses of Trichodesmium IMS101 grown under a matrix of low and high levels of pCO₂ (150 and 900 μatm) and irradiance (50 and 200 μmol photons m⁻² s⁻¹). Growth rates as well as cellular carbon and nitrogen contents increased with increasing pCO₂ and light levels in the cultures. The pCO₂-dependent stimulation in organic carbon and nitrogen production was highest under low light. High pCO₂ stimulated rates of N₂ fixation and prolonged the duration, while high light affected maximum rates only. Gross photosynthesis increased with light but did not change with pCO₂. HCO₃⁻ was identified as the predominant carbon source taken up in all treatments. Inorganic carbon uptake increased with light, but only gross CO₂ uptake was enhanced under high pCO₂. A comparison between carbon fluxes in vivo and those derived from ¹³C fractionation indicates high internal carbon cycling, especially in the low-pCO₂ treatment under high light. Light-dependent oxygen uptake was only detected under low pCO₂ combined with high light or when low-light-acclimated cells were exposed to high light, indicating that the Mehler reaction functions also as a photoprotective mechanism in Trichodesmium. Our data confirm the pronounced pCO₂ effect on N₂ fixation and growth in Trichodesmium and further show a strong modulation of these effects by light intensity. We attribute these responses to changes in the allocation of photosynthetic energy between carbon acquisition and the assimilation of carbon and nitrogen under elevated pCO₂. These findings are supported by a complementary study looking at photosynthetic fluorescence parameters of photosystem II, photosynthetic unit stoichiometry (photosystem I:photosystem II), and pool sizes of key proteins in carbon and nitrogen acquisition.Human-induced climate change will significantly alter the marine environment within the next century and beyond. Future scenarios predict an increase from currently approximately 380 to about 750 to 1,000 μatm CO₂ partial pressure (pCO₂) in the atmosphere until the end of this century (Raven et al., 2005; Raupach et al., 2007). As the ocean takes up this anthropogenic CO₂, dissolved inorganic carbon (DIC) in the surface ocean increases while the pH decreases (Wolf-Gladrow et al., 1999). Rising global temperatures will increase surface ocean stratification, which may affect the light regime in the upper mixed layer as well as nutrient input from deeper waters (Doney, 2006). Uncertainties remain regarding both the magnitude of the physicochemical changes and the biological responses of organisms, including species and populations of the oceanic primary producers at the basis of the food webs.In view of potential ecological implications and feedbacks on climate, several studies have examined pCO₂ sensitivity in phytoplankton key species (Burkhardt and Riebesell, 1997; Riebesell et al., 2000; Rost et al., 2003; Tortell et al., 2008). Pronounced responses to elevated pCO₂ were observed in N₂-fixing cyanobacteria (Barcelos é Ramos et al., 2007; Hutchins et al., 2007; Levitan et al., 2007; Fu et al., 2008; Kranz et al., 2009), which play a vital role in marine ecosystems by providing a new source of biologically available nitrogen species to otherwise nitrogen-limited regions. Recent studies focused on the impact of different environmental factors on the filamentous Trichodesmium species, which is known for high abundance and the formation of massive blooms in tropical and subtropical areas (Capone et al., 2005; Mahaffey et al., 2005). Higher pCO₂ levels stimulated growth rates, biomass production, and N₂ fixation (Hutchins et al., 2007; Levitan et al., 2007; Kranz et al., 2009) and affected inorganic carbon acquisition of the cells (Kranz et al., 2009). While elevated sea surface temperatures are predicted to shift the spatial distribution of Trichodesmium species toward higher latitudes (Breitbarth et al., 2007), the combined effects of pCO₂ and temperature may favor this species and extend its niche even farther (Hutchins et al., 2007; Levitan et al., 2010a). An increase in the average light intensity, caused by the predicted shoaling of the upper mixed layer, may further stimulate photosynthesis and thus growth and N₂ fixation of Trichodesmium (Breitbarth et al., 2008). To our knowledge, the combined effects of light and pCO₂ have not been studied yet, although these environmental factors are likely to influence photosynthesis and other key processes in Trichodesmium.To understand the responses of an organism to changes in environmental conditions, metabolic processes must be studied. In Trichodesmium, photosynthetically generated energy (ATP and NADPH) is primarily used for the fixation of CO₂ in the Calvin-Benson cycle. A large proportion of this energy, however, is also required for the process of N₂ fixation via nitrogenase and for the operation of a CO₂-concentrating mechanism (CCM). The latter involves active uptake of inorganic carbon, which functions to increase the rate of carboxylation reaction mediated by Rubisco. This ancient and highly conserved enzyme is characterized by low affinities for its substrate CO₂ and a susceptibility to a competing reaction with oxygen (O₂) as substrate (Badger et al., 1998); the latter initiates photorespiration. As cyanobacterial Rubisco possesses one of the lowest CO₂ affinities among phytoplankton (Badger et al., 1998), a considerable amount of resources have to be invested to achieve sufficient rates of carbon fixation and to avoid photorespiration. A first step toward a mechanistic understanding of responses in Trichodesmium has been taken by Levitan et al. (2007), focusing on pCO₂ dependency of nitrogenase activity and photosynthesis. Subsequently, Kranz et al. (2009) described variations in CCM efficiency with pCO₂ and suggested that the observed plasticity in CCM regulation allowed energy reallocation under high pCO₂, which may explain the observed pCO₂-dependent changes in nitrogenase activity, growth, and elemental composition (Barcelos é Ramos et al., 2007; Hutchins et al., 2007; Levitan et al., 2007).In this study, we measured growth responses as well as metabolic key processes in Trichodesmium erythraeum (IMS101) under environmental conditions that likely alter the energy budget and/or energy allocation of the cell. Cultures were acclimated to a matrix of low and high pCO₂ (150 and 900 μatm) at two different light intensities (50 and 200 μmol photons m⁻² s⁻¹). For each of the four treatments, changes in growth rates, elemental ratios, and the accumulation of particulate carbon and nitrogen were measured. Metabolic processes (gross photosynthesis, CCM activity, and O₂ uptake) were obtained by means of membrane-inlet mass spectrometry (MIMS), while N₂ fixation was detected by gas chromatography. As these processes may vary over the diurnal cycle in Trichodesmium (Berman-Frank et al., 2001; Kranz et al., 2009), measurements were performed in the morning and around midday. The results on metabolic processes were accompanied by measurements of the fluorescence of PSII, ratios of the photosynthetic units (PSI:PSII), and pool sizes of key proteins involved in carbon and nitrogen fixation as well as assimilation (Levitan et al., 2010b).     

SPATIAL SEGREGATION OF CO2 FIXATION IN TRICHODESMIUM SPP.: LINKAGE TO N2 FIXATION POTENTIAL1

The aggregate-forming, nonheterocystous, filamentous blue-green alga (cyanobacteria) Trichodesmium spp. is a widespread and important planktonic N₂ fixer and primary producer in tropical and subtropical oceans. It is unique among nonheterocystous genera because it conducts N₂ and CO₂ fixation (O₂ evolution) simultaneously; a notable achievement, because O₂ is a potent inhibitor of N₂ fixation. Spatial and temporal CO₂ fixation patterns were examined in trichomes and aggregates from natural and cultured populations, utilizing microautoradiographic detection of ¹⁴CO₂ incorporation. Parallel N₂ fixation (acetylene reduction) measurements were also made. Diel N₂ and CO₂ fixation patterns were similar, with co-optimization of both processes near midday. Microautoradiographs revealed several trichome-level ¹⁴CO₂ incorporation patterns: 1)uniform, heavy labeling, 2)uniform, light labeling, 3) heavier labeling in distal as opposed, to proximal regions, and 4) virtually no labeling throughout. Similar patterns were observed in natural and cultured populations. Given previous immunochemical findings that N₂ fixation potential is widespread in Trichodesmium spp. trichomes and aggregates, current results suggest a high degree of individuality, and possibly a “division of labor” in terms of CO₂ fixation, among trichomes comprising active N₂-fixing aggregates. Segregation of photosynthesis within and among trichomes facilitates simultaneous N₂ and CO₂ fixation in Trichodesmium spp. trichomes and aggregates.     

DIAZOTROPHIC GROWTH OF THE MARINE CYANOBACTERIUM TRICHODESMIUM IMS101 IN CONTINUOUS CULTURE: EFFECTS OF GROWTH RATE ON N2‐FIXATION RATE,BIOMASS, AND C:N:P STOICHIOMETRY1

Trichodesmium N₂ fixation has been studied for decades in situ and, recently, in controlled laboratory conditions; yet N₂‐fixation rate estimates still vary widely. This variance has made it difficult to accurately estimate the input of new nitrogen (N) by Trichodesmium to the oligotrophic gyres of the world ocean. Field and culture studies demonstrate that trace metal limitation, phosphate availability, the preferential uptake of combined N, light intensity, and temperature may all affect N₂ fixation, but the interactions between growth rate and N₂ fixation have not been well characterized in this marine diazotroph. To determine the effects of growth rate on N₂ fixation, we established phosphorus (P)–limited continuous cultures of Trichodesmium, which we maintained at nine steady‐state growth rates ranging from 0.27 to 0.67 d^?1. As growth rate increased, biomass (measured as particulate N) decreased, and N₂‐fixation rate increased linearly. The carbon to nitrogen ratio (C:N) varied from 5.5 to 6.2, with a mean of 5.8 ± 0.2 (mean ± SD, N = 9), and decreased significantly with growth rate. The N:P ratio varied from 23.4 to 45.9, with a mean of 30.5 ± 6.6 (mean ± SD, N = 9), and remained relatively constant over the range of growth rates studied. Relative constancy of C:N:P ratios suggests a tight coupling between the uptake of these three macronutrients and steady‐state growth across the range of growth rates. Our work demonstrates that growth rate must be considered when planning studies of the effects of environmental factors on N₂ fixation and when modeling the impact of Trichodesmium as a source of new N to oligotrophic regions of the ocean.     

LIPID CLASS,CAROTENOID, AND TOXIN DYNAMICS OF KARENIA BREVIS (DINOPHYCEAE) DURING DIEL VERTICAL MIGRATION1

The internal lipid, carotenoid, and toxin concentrations of Karenia brevis (C. C. Davis) Gert Hansen and Moestrup are influenced by its ability to use ambient light and nutrients for growth and reproduction. This study investigated changes in K. brevis toxicity, lipid class, and carotenoid concentrations in low‐light, nitrate‐replete (250 μmol quanta · m^?2 · s^?1, 80 μM NO₃); high‐light, nitrate‐replete (960 μmol quanta · m^?2 · s^?1, 80 μM NO₃); and high‐light, nitrate‐reduced (960 μmol quanta · m^?2 · s^?1, <5 μM NO₃) mesocosms. Reverse‐phase HPLC quantified the epoxidation state (EPS) of the xanthophyll‐cycle pigments diadinoxanthin and diatoxanthin, and a Chromarod Iatroscan thin layer chromatography/flame ionization detection (TLC/FID) system quantified changes in lipid class concentrations. EPS did not exceed 0.20 in the low‐light mesocosm, but increased to 0.65 in the high‐light mesocosms. Triacylglycerol and monogalactosyldiacylglycerol (MGDG) were the largest lipid classes consisting of 9.3% to 48.7% and 37.3% to 69.7% of total lipid, respectively. Both lipid classes also experienced the greatest concentration changes in high‐light experiments. K. brevis increased EPS and toxin concentrations while decreasing its lipid concentrations under high light. K. brevis may mobilize its toxins into the surrounding environment by reducing lipid concentrations, such as sterols, limiting competition, or toxins are released because lipids are decreased in high light, reducing any protective mechanism against their own toxins.     

GROWTH AND NITROGEN FIXATION OF THE DIAZOTROPHIC FILAMENTOUS NONHETEROCYSTOUS CYANOBACTERIUM TRICHODESMIUM SP. IMS 101 IN DEFINED MEDIA: EVIDENCE FOR A CIRCADIAN RHYTHM1

Trichodesmium sp. IMS 101, originally isolated from coastal western Atlantic waters by Prufert-Bebout and colleagues and maintained in seawater-based media, was successfully cultivated in two artificial media. Its characteristics of growth, nitrogen fixation, and regulation of nitrogen fixation were compared to those of natural populations and Trichodesmium sp. NIBB 1067. Results indicate that the culture grown in artificial media had nitrogen fixation characteristics similar to those when the culture is grown in seawater-based medium and to those of Trichodesmium sp. in the natural habitat. The study provides practical artificial media to facilitate the physiological studies of these important diazotrophic cyanobacteria, as well as the cultivation of other Trichodesmium species in future studies. Manipulations of the light/dark cycle were performed to determine whether or not the daily cycle of nitrogen fixation is a circadian rhythm. Cultures grown under continuous light maintained the cycle for up to 6 days. We demonstrated that the daily cycle of nitrogen fixation in Trichodesmium sp. IMS 101 was at least partially under the control of a circardian rhythm.     

Levels of Daily Light Doses Under Changed Day-Night Cycles Regulate Temporal Segregation of Photosynthesis and N2 Fixation in the Cyanobacterium Trichodesmium erythraeum IMS101

While the diazotrophic cyanobacterium Trichodesmium is known to display inverse diurnal performances of photosynthesis and N₂ fixation, such a phenomenon has not been well documented under different day-night (L-D) cycles and different levels of light dose exposed to the cells. Here, we show differences in growth, N₂ fixation and photosynthetic carbon fixation as well as photochemical performances of Trichodesmium IMS101 grown under 12L:12D, 8L:16D and 16L:8D L-D cycles at 70 μmol photons m^-2 s^-1 PAR (LL) and 350 μmol photons m^-2 s^-1 PAR (HL). The specific growth rate was the highest under LL and the lowest under HL under 16L:8D, and it increased under LL and decreased under HL with increased levels of daytime light doses exposed under the different light regimes, respectively. N₂ fixation and photosynthetic carbon fixation were affected differentially by changes in the day-night regimes, with the former increasing directly under LL with increased daytime light doses and decreased under HL over growth-saturating light levels. Temporal segregation of N₂ fixation from photosynthetic carbon fixation was evidenced under all day-night regimes, showing a time lag between the peak in N₂ fixation and dip in carbon fixation. Elongation of light period led to higher N₂ fixation rate under LL than under HL, while shortening the light exposure to 8 h delayed the N₂ fixation peaking time (at the end of light period) and extended it to night period. Photosynthetic carbon fixation rates and transfer of light photons were always higher under HL than LL, regardless of the day-night cycles. Conclusively, diel performance of N₂ fixation possesses functional plasticity, which was regulated by levels of light energy supplies either via changing light levels or length of light exposure.     

INORGANIC CARBON UTILIZATION BY ROSS SEA PHYTOPLANKTON ACROSS NATURAL AND EXPERIMENTAL CO2 GRADIENTS1

We present results from a field study of inorganic carbon (C) acquisition by Ross Sea phytoplankton during Phaeocystis‐dominated early season blooms. Isotope disequilibrium experiments revealed that HCO₃^? was the primary inorganic C source for photosynthesis in all phytoplankton assemblages. From these experiments, we also derived relative enhancement factors for HCO₃^?/CO₂ interconversion as a measure of extracellular carbonic anhydrase activity (eCA). The enhancement factors ranged from 1.0 (no apparent eCA activity) to 6.4, with an overall mean of 2.9. Additional eCA measurements, made using membrane inlet mass spectrometry (MIMS), yielded activities ranging from 2.4 to 6.9 U · [μg chl a]^?1 (mean 4.1). Measurements of short‐term C‐fixation parameters revealed saturation kinetics with respect to external inorganic carbon, with a mean half‐saturation constant for inorganic carbon uptake (K_1/2) of ～380 μM. Comparison of our early springtime results with published data from late‐season Ross Sea assemblages showed that neither HCO₃^? utilization nor eCA activity was significantly correlated to ambient CO₂ levels or phytoplankton taxonomic composition. We did, however, observe a strong negative relationship between surface water pCO₂ and short‐term ¹⁴C‐fixation rates for the early season survey. Direct incubation experiments showed no statistically significant effects of pCO₂ (10 to 80 Pa) on relative HCO₃^? utilization or eCA activity. Our results provide insight into the seasonal regulation of C uptake by Ross Sea phytoplankton across a range of pCO₂ and phytoplankton taxonomic composition.     

INTERACTIONS BETWEEN NITRATE UPTAKE AND NITROGEN FIXATION IN CONTINUOUS CULTURES OF THE MARINE DIAZOTROPH TRICHODESMIUM (CYANOBACTERIA)1

Diazotrophic cyanobacteria can take up combined nitrogen (nitrate, ammonium, amino acids, dissolved organic nitrogen) from solution, but the interaction between N₂ fixation and uptake of combined nitrogen is not well understood. We studied the effects of combined nitrogen ) additions on N₂ fixation rates in the cyanobacterium Trichodesmium erythraeum (IMS‐101) maintained in continuous culture in an N‐free medium (YBCII) and a 12:12‐h light:dark cycle. We measured acetylene reduction rates, nutrient concentrations, and biomass throughout the 12 h of illumination after the addition of nitrate (0.5–20 μM) at the start of the light period. Compared with unamended controls, Trichodesmium showed strong inhibition of acetylene reduction (up to 70%) in the presence of , with apparent saturation of the inhibition effect at an initial concentration of approximately 10 μM. The inhibition of acetylene reduction persisted through much of the light period as concentration in the culture vessel decreased. Recovery of N₂ fixation was observed late in the light period in cultures amended with low concentrations of (<5 μM) when ambient concentrations had decreased to 0.3–0.4 μM in the culture vessel. Nitrate uptake accounted for as much as 86% of total N uptake and, at the higher treatment concentrations, more than made up for the observed decrease in N₂ fixation rates. We conclude that Trichodesmium can obtain significant quantities of N through uptake of nitrate and does so in preference to N₂ fixation when sufficient is available.     

EFFECT OF TEMPERATURE,LIGHT AND pH ON GROWTH,PHOTOSYNTHESIS AND RESPIRATION OF THE DINOFLAGELLATE PERIDINIUM CINCTUM FA. WESTII IN LABORATORY CULTURES1

Optimum light, temperature, and pH conditions for growth, photosynthetic, and respiratory activities of Peridinium cinctum fa. westii (Lemm.) Lef were investigated by using axenic clones in batch cultures. The results are discussed and compared with data from Lake Kinneret (Israel) where it produces heavy blooms in spring. Highest biomass development and growth rates occurred at ca. 23° C and ≥50 μE· m^?2·s¹ of fluorescent light with energy peaks at 440–575 and 665 nm. Photosynthetic oxygen release was more efficient in filtered light of blue (BG 12) and red (RG 2) than in green (VG 9) qualities. Photosynthetic oxygen production occurred at temperatures ranging from 5° to 32° C in white fluorescent light from 10 to 105 μE·m^?2·s^?1 with a gross maximum value of 1500 × 10^?12 g·cell^?1·h^?1 at the highest irradiance. The average respiration amounted to ca. 12% of the gross production and reached a maximum value of ca. 270·10^?12 g·cell^?1·h^?1 at 31° C. A comparison of photosynthetic and respiratory Q₁₀-values showed that in the upper temperature range the increase in gross production was only a third of the corresponding increase in respiration, although the gross production was at maximum. Short intermittent periods of dark (>7 min) before high light exposures from a halogen lamp greatly increased oxygen production. Depending on the physiological status of the alga, light saturation values were reached at 500–1000 μE·m^?2·s^?1 of halogen light with compensation points at 20–40 μE·m^?2·s^?1 and I_k-values at 100–200 μE·m^?2·s^?1. The corresponding values in fluorescent light in which it was cultured and adapted, were 25 to 75% lower indicating the ability of the alga to efficiently utilize varying light conditions, if the adaptation time is sufficient. Carbon fixation was most efficient at ca. pH 7, but the growth rates and biomass development were highest at pH 8.3.     

MORPHOLOGICAL AND PHYSIOLOGICAL EFFECTS IN PROBOSCIA ALATA (BACILLARIOPHYCEAE) GROWN UNDER DIFFERENT LIGHT AND CO2 CONDITIONS OF THE MODERN SOUTHERN OCEAN1

The combined effects of different light and aqueous CO₂ conditions were assessed for the Southern Ocean diatom Proboscia alata (Brightwell) Sundström in laboratory experiments. Selected culture conditions (light and CO_2(aq)) were representative for the natural ranges in the modern Southern Ocean. Light conditions were 40 (low) and 240 (high) μmol photons · m^?2 · s^?1. The three CO_2(aq) conditions ranged from 8 to 34 μmol · kg^?1 CO_2(aq) (equivalent to a pCO₂ from 137 to 598 μatm, respectively). Clear morphological changes were induced by these different CO_2(aq) conditions. Cells in low [CO_2(aq)] formed spirals, while many cells in high [CO_2(aq)] disintegrated. Cell size and volume were significantly affected by the different CO_2(aq) concentrations. Increasing CO_2(aq) concentrations led to an increase in particulate organic carbon concentrations per cell in the high light cultures, with exactly the opposite happening in the low light cultures. However, other parameters measured were not influenced by the range of CO_2(aq) treatments. This included growth rates, chlorophyll a concentration and photosynthetic yield (F_V/F_M). Different light treatments had a large effect on nutrient uptake. High light conditions caused an increased nutrient uptake rate compared to cells grown in low light conditions. Light and CO₂ conditions co‐determined in various ways the response of P. alata to changing environmental conditions. Overall P. alata appeared to be well adapted to the natural variability in light availability and CO_2(aq) concentration of the modern Southern Ocean. Nevertheless, our results showed that P. alata is susceptible to future changes in inorganic carbon concentrations in the Southern Ocean.     

Light‐dependent oxygen consumption in nitrogen‐fixing cyanobacteria plays a key role in nitrogenase protection1

All colonial diazotrophic cyanobacteria are capable of simultaneously evolving O₂ through oxygenic photosynthesis and fixing nitrogen via nitrogenase. Since nitrogenase is irreversibly inactivated by O₂, accommodation of the two metabolic pathways has led to biochemical and/or structural adaptations that protect the enzyme from O₂. In some species, differentiated cells (heterocysts) are produced within the filaments. PSII is absent in the heterocysts, while PSI activity is maintained. In other, nonheterocystous species, however, a “division of labor” occurs whereby individual cells within a colony appear to ephemerally fix nitrogen while others evolve oxygen. Using membrane inlet mass spectrometry (MIMS) in conjunction with tracer ¹⁸O₂ and inhibitors of photosynthetic and respiratory electron transport, we examined the light dependence of O₂ consumption in Trichodesmium sp. IMS 101, a nonheterocystous, colonial cyanobacterium, and Anabaena flos‐aquae (Lyngb.) Bréb. ex Bornet et Flahault, a heterocystous species. Our results indicate that in both species, intracellular O₂ concentrations are maintained at low levels by the light‐dependent reduction of oxygen via the Mehler reaction. In N₂‐fixing Trichodesmium colonies, Mehler activity can consume ～75% of gross O₂ production, while in Trichodesmium utilizing nitrate, Mehler activity declines and consumes ～10% of gross O₂ production. Moreover, evidence for the coupling between N₂ fixation and Mehler activity was observed in purified heterocysts of Anabaena, where light accelerated O₂ consumption by 3‐fold. Our results suggest that a major role for PSI in N₂‐fixing cyanobacteria is to effectively act as a photon‐catalyzed oxidase, consuming O₂ through pseudocyclic electron transport while simultaneously supplying ATP in both heterocystous and nonheterocystous taxa.     

ACCLIMATION OF SYNECHOCOCCUS STRAIN WH7803 TO AMBIENT CO2 CONCENTRATION AND TO ELEVATED LIGHT INTENSITY1

A CO₂ concentrating mechanism has been identified in the phycoerythrin-possessing Synechococcus sp. WH7803 and has been observed to be severely inhibited by short exposure to elevated light intensities. A light treatment of 300–2000 μmol quanta·m^?2·s^?1 resulted in a considerable decay in the variable fluorescence of PSII with time, suggesting decreased efficiency of energy transfer from the phycobilisomes, direct damage to the reaction center II, or both. Measurements of the activity of PSII and changes in fluorescence emission spectra during a light treatment of 1000 μmol quanta·m^?2·s^?1 indicated considerable reduction in the energy flow from the phycocyanin to the phycobilisome terminal acceptor and chlorophyll a. Consequently, whereas the maximal photosynthetic rate, at saturating light and Co₂ concentration, was hardly affected by a light treatment of 1000 μmol quanta·m^?2·s^?1 for 2 h, the light intensity required to reach that maximum increased with the duration of the light treatment.