Phycologia (2007) Volume 46 (5), 503–512 Published 4 September 2007 Characterising nutrient-induced fluorescence transients (NIFTs) in nitrogen-stressed Chlorella emersonii (Chlorophyta) KIRSTEN SHELLY1*, TARA HIGGINS1,2, JOHN BEARDALL1, BAYDEN WOOD3, DON MCNAUGHTON3 AND PHILIP HERAUD1 1 School of Biological Sciences and Centre for Biospectroscopy, Monash University, Clayton, Victoria, Australia 2 Department of Microbiology, National University of Ireland, Galway, Ireland 3 School of Chemistry and Centre for Biospectroscopy, Monash University, Clayton, Victoria, Australia K. SHELLY, T. HIGGINS, J. BEARDALL, B. WOOD, D. MCNAUGHTON AND P. HERAUD. 2007. Characterising nutrientinduced fluorescence transients (NIFTs) in nitrogen-stressed Chlorella emersonii (Chlorophyta). Phycologia 46: 503–512. DOI: 10.2216/06-55.1 Although determining the nutrient status of algae is highly desirable for water quality management, conventional methods for assessing nutrient limitation are confounded by a range of theoretical and practical limitations. The current paper examines the effectiveness of a novel rapid fluorometric technique, based on observations of nutrient-induced transients in chl a fluorescence (NIFTs), in providing accurate measurements of algal nutrient limitation. The progress of N-starvation in batch cultures of the freshwater chlorophyte Chlorella emersonii was followed and the NIFT responses of cells to N-starvation and additions of both NH4+ and NO32 were characterised using a number of techniques including NIFTs, conventional pigment analysis using UV/Visible spectrophotometry and Fourier transform infrared (FT-IR) and Raman spectroscopy. Results showed that the addition of NH4+ and NO32 elicited distinct changes in in vivo chl a fluorescence in N-limited Chlorella cells. The nature of the fluorescence change was dependent on the form of nitrogen supplied, with NH4+ additions producing a more complex effect on fluorescence than NO32 additions. Interestingly, the greatest fluorescence response following NH4+ injection occurred prior to cells becoming extremely N-starved. Despite Chlorella exhibiting many of the characteristic features of N-deficient cells such as lowered capacity for photosynthetic electron transport (rETRmax), reduced Chl a : b–carotene ratios and increased levels of carbohydrate accumulation relative to protein, values for the maximum effective quantum yield of Photosystem II (WPSIIe-max) remained high over the course of N-starvation. KEY WORDS: Chlorella emersonii, Nitrogen limitation, Nutrient-induced fluorescence transient (NIFT), Chlorophyll fluorescence INTRODUCTION Nutrient availability in both marine and freshwater systems frequently limits aquatic primary productivity, the most common of limiting nutrients being nitrogen and phosphorus (Schindler 1977; Wynne & Berman 1980; Lean & Pick 1981). The ability to rapidly identify nutrient limitation, and which nutrient in particular is limiting, would be of great importance, both in understanding aquatic ecology and for guiding water quality policies and management practices. Historically, a number of techniques have been used to determine the physiological health of algae, notably nutrient-enrichment bioassays, and external and cellular nutrient ratio analyses (as discussed by Hecky & Kilham 1988; Beardall et al. 2001b). However, most of these techniques are not only complicated and time consuming, they are also subject to potential artifacts, frequently indicating potential limitation (Liebig limitation) in the absence of other limiting factors rather than the in situ nutrient status (Elser et al. 1990). As a result, the interpretation and management of nutrient limitation in aquatic systems using conventional techniques is oftentimes difficult (Beardall et al. 2001b). * Corresponding author (Kirsten.shelly@sci.monash.edu.au). Nutrient limitation often is diagnosed in field populations of algae by chlorophyll a (Chl a) fluorescence (Kolber et al. 1994). In particular, the chlorophyll fluorescence parameter WPSIIe-max (the maximum quantum yield of PS II; 5 Fv/Fm) has been used as an index of microalgal physiological status. Recent studies spanning marine and freshwater organisms, involving both field assemblages and laboratory cultures of algae, have indicated that changes in steady state chlorophyll fluorescence and WPSIIe-max following nutrient addition could potentially serve as a diagnostic tool for assessing nutrient limitation in microalgae. Turpin & Weger (1988) originally reported that, if phosphorus or nitrogen is added to phytoplankton cultures limited in that particular nutrient, a rapid but transient change (within minutes) in fluorescence is seen. This change in chlorophyll fluorescence has been termed a nutrient-induced fluorescence transient, or NIFT (Wood & Oliver 1995). These fluorescence transients have been reported for the resupply of carbon (Miller et al. 1991), nitrogen (Holmes et al. 1989; Wood & Oliver 1995; Young & Beardall 2003b) and phosphorus (Wood & Oliver 1995; Gauthier & Turpin 1997; Roberts 1998; Beardall et al. 2001b) to suitably deficient cells. There is also some evidence that this phenomenon occurs with silicate (Lippemeier et al. 2001). The fluorescence response generally is not observed if a nonlimiting nutrient or distilled water is 503 504 Phycologia, Vol. 46 (5), 2007 added to the cells (Beardall et al. 2001a, b; Holland et al. 2004). Although the precise physiology behind NIFTs is still poorly understood, it is believed that the transient change in fluorescence is attributable to a reallocation of energy from photosynthesis to nutrient uptake. Chlorophyll a and b-carotene content, as well as the macromolecular composition of algae, also change with changing cell nutrient status. Raman spectroscopy and Fourier transform infrared (FT-IR) methodologies are novel ways in which to determine both pigments, such as chlorophyll a and b-carotene, and macromolecular content of cells, respectively. FT-IR spectroscopy previously has been used to carry out rapid, simple, concurrent and noninvasive analysis of cellular components. Giordano et al. (2001), for example, showed that FT-IR spectroscopy is a reliable way to precisely determine the relative concentration of silica, protein, carbohydrates and lipids in the diatom Chaetoceros muelleri. Given its ability to minimise disturbance of the intracellular environment due to reduced manipulation of the sample, FT-IR spectroscopy appears to be a powerful analytical tool. Previous methods for measuring cellular composition such as wet chemistry for internal pools of macromolecules, or estimates of changes in elemental ratios (e.g. C : N and N : P), are not necessarily specific to the limiting nutrient, and often are prone to interference from debris in natural assemblages (Beardall et al. 2001a). Cell protein profiles run on gel electrophoresis separate out proteins, which can identify changes in levels of specific proteins, but the sample sizes needed are often large and the method is time consuming (Beardall et al. 2001a). FT-IR spectroscopy takes around 20 seconds to acquire a spectrum, and the sample size is small enough not to perturb the culture system (,4 ml culture is needed), whilst still allowing accurate assessment of the changes in macromolecular content of the cell. Raman spectroscopy can be used with live cells (Wood et al. 2005) and allows spectra to be taken on a single cell basis (Heraud et al. 2006; Heraud et al. 2006). This technique is an efficient and simple tool for making measurements of chlorophyll a and b-carotene, rather than simply measuring carotenoids in bulk samples using conventional spectroscopic methods. To date, the exploration of NIFTs as a reliable index of nutrient limitation has been restricted to a small number of algal species. Few investigations have characterized these NIFT responses thoroughly (but see the studies on the marine chlorophyte Dunaliella tertiolecta by Young & Beardall 2003a, b). Holland et al. (2004) also reported briefly on the occurrence of phosphate and ammoniuminduced NIFTs in Chlorella, as well as in the cyanobacterium Oscillatoria and mixed field assemblages. In order to further explore the possibility of using this technique as an indicator of nitrogen stress in algae, the current study followed the progress of N-starvation in batch cultures of the freshwater chlorophyte Chlorella emersonii and characterized in detail the NIFT response shown by this organism to the respective addition of both NH4+ and NO32, as well as investigating the changes in chlorophyll a : b-carotene ratios and macromolecular composition of the cells. MATERIAL AND METHODS Culture conditions Chlorella emersonii was cultured under axenic batch growth conditions at 18uC using 250 ml glass vessels, which were exposed continuously to photosynthetically active radiation (PAR) (120 mmol quanta m22 s21) provided by Sylvannia Gro-lux WS (Osram Sylvania Ltd., Danvers, MA, US) fluorescent tubes. The cultures were maintained in MS/2 medium (Morris & Syrett 1965), in which only the nitrogen input was adjusted. Cultures were initiated with starting KNO3 concentrations of 50 mM (‘low-N cultures’) or 100 mM (‘high-N cultures’) in order to allow some initial growth, and 3 replicate 250-ml cultures were set up for both KNO3 levels. All other nutrients were in large excess. The two differing N treatments were used to induce starvation at different rates in order to improve our ability to resolve when cells start to show the onset of the NIFT perturbation. Measurement of WPSIIe-max Subsamples were withdrawn regularly from cultures to take chlorophyll fluorescence measurements. These were carried out with a PhytoPAM (Walz, Effeltrich, Germany), which was modified such that the cuvette could be maintained at the growth temperature and stirred from above with a motorised stirring unit. Prior to acquisition of the PhytoPAM measurements, cells were dark adapted in the cuvette for 15 min. WPSIIe-max then was measured after the application of a saturating pulse and calculated according to Van Kooten & Snel (1990). Rapid light curve (RLC) measurements were carried out on the PhytoPAM modified as above. The actinic light was altered after each measurement from 1 to 295 mmol quanta m22 s21, with each light intensity being applied for 30 seconds. The maximum relative electron transport rate (rETRmax) was calculated by fitting the rETR and irradiance data to the equations of Eilers & Peeters (1988). CHLOROPHYLLS AND CAROTENOIDS: Appropriate, duplicate volumes of sample (between 5 and 20 ml, depending on the cell density of the culture) were filtered through a GF/C filter. Filters were wrapped in aluminium foil and frozen for later processing. Frozen filters were extracted in 10-ml centrifuge tubes using 5 ml of a 1 : 1 v/v mixture of dimethyl sulfoxide (DMSO) and 90% acetone (Burnison 1980). Tubes were well shaken to accelerate pigment extraction and placed in darkness in a refrigerator. Following overnight extraction, tubes were centrifuged and the supernatant collected. Sample absorbances were read on a Cary 50 spectrophotometer and chlorophyll and carotenoid concentrations were calculated according to Golterman & Clymo (1971). FT-IR AND RAMAN SPECTROSCOPY: FT-IR spectra of dried cell pastes were collected on a Bruker IFS55 EQUINOX FT-IR spectrometer equipped with a liquid nitrogen cooled HgCdTe and using a Golden Gate (TM Specac, Woodstock, GA, US) single bounce diamond attenuated total reflectance (ATR) accessory. Moist cell pastes (approx 5 3 109 cells/ml) were air-dried onto the diamond window of the Shelly et al.: Nitrogen limited NIFTs 505 FT-IR accessory before spectra were collected. Typically, 50 scans were taken with a resolution of 6 cm21. Raman spectra of single viable algal cells were recorded on a Renishaw system 2000 (equipped with a Peltier cooled CCD detector) using a 782 nm excitation line from a diode laser and a modified BH2-UMA Olympus optical microscope with a Zeiss 3 60 water immersion objective running under Renishaw-WiRETM 2 software. Ten microliters of packed cells were added to a 6 cm diameter aluminium sputter coated Petri dish that was further coated in 0.01% poly-l-lysine to affix the cells to the bottom of the Petri dish. Power at the sample was ,2–3 mW for a 1–2 mm laser spot size. Spectra were recorded between 1800–200 cm21 with a resolution of ,1–2 cm21. For each spectrum 1 scan was accumulated and the laser exposure for each scan was 10 seconds for a population of 30 individual cells under each condition. The spectra were then baseline corrected using the rubber band method of the OPUSTM spectroscopic software (Bruker, Germany), corrected using the multiplicative scattering correction within The UnscramblerTM (Camo, Norway) and averaged. Nutrient-induced fluorescence transients NIFTs (Beardall et al. 2001a) were investigated during the course of N-starvation following the method of Holland et al. (2004). A 3-ml sample was taken from each of the batch cultures and placed in a mirrored glass fluorometer cuvette with a magnetic stirrer. The sample was placed in a Hitachi 2000 spectrofluorometer (EX at 435 nm and EM at 680 nm) and steady state fluorescence (Ft) values were measured until stable. Once fluorescence had stabilised, a 30-ml sample of either NH4+ or NO32 solution was injected into the cuvette, to give a final concentration of 100 mM. The observed changes in Ft then were recorded and the characteristic features of fluorescence changes following the injection were quantified (see Fig. 1). Subsamples also were cross-checked and no changes in fluorescence, at any point during starvation, were evident upon additions of either P (10 mM PO432) or dH2O, indicating that nitrogen was the limiting nutrient. Unless otherwise stated, differences between parameter values were analysed statistically by students t test. RESULTS WPSIIe-max There was no significant change (,5%; P . 0.05) in WPSIIe-max over the 10-day experiment (Fig. 2a). Little variation was observed between batch cultures of different starting N concentrations, with both ‘low-N’ and ‘high-N’ treatments dropping to a similar WPSIIe-max value within 10 days of starvation (WPSIIe-max 0.740 and 0.743, respectively). CHLOROPHYLL AND CAROTENOIDS: Cellular chlorophyll concentrations decreased dramatically as N-starvation progressed (Fig. 2b). Cultures initiated at both ‘low-N’ and ‘high-N’ levels showed a similar pattern, with Fig. 1. An example of the characteristic features of (a) a NO32– nutrient-induced fluorescence transients (NIFTs) and (b) a NH4+– NIFT in ‘low-N’ batch cultures of Chlorella emersonii. chlorophyll dropping over fivefold, from 397.0 and 428.2 pg/cell on day 1 to 79.9 and 75.9 pg/cell on day 10 in ‘low-N’ and ‘high-N’ cultures, respectively. Carotenoid : Chlorophyll ratios (Fig. 2b) increased substantially as the cells became more N-starved, from 1.19 and 0.71 on day 1, to 3.24 and 3.01 on day 10, in the ‘low-N’ and ‘highN’ cultures, respectively. Values for chlorophyll content and carotenoid : chl ratio were not significantly different (P . 0.05) between ‘low-N’ and ‘high-N’ cultures except on day 4, when the chlorophyll content was lower in the ‘lowN’ cells (P , 0.05). RLC MEASUREMENTS: Measurements of rETR as a function of photon flux (Fig. 2c) indicated that, as N-starvation advanced, light saturated rates (rETRmax) declined by 27% and 32% in the ‘low-N’ and ‘high-N’ cultures, respectively (P . 0.05). The ‘low-N’ batch cultures exhibited 10–16% lower rETRmax compared with cells grown initially at ‘highN’ (P . 0.05). NIFT CHARACTERISTIC RESPONSE: Fig. 1 shows the characteristic NIFT response following NO32 and NH4+ additions 506 Phycologia, Vol. 46 (5), 2007 Fig. 2. (a) Changes in photosynthetic parameters and pigments of Chlorella emersonii batch cultures following the transfer of cells to ‘low-N’ (black bars, filled symbols) and ‘high-N’ (open bars, open symbols) batch cultures. (a) PSIIe-max; (b) total chlorophyll (bars) and carotenoid : chlorophyll ratio (lines); (c) light saturated rates of relative electron transfer (rETRmax). All data shown are the mean of replicate cultures, n 5 3, with the exception of chlorophyll/carotenoid data where n 5 6. Error bars, where shown, give standard deviations. to batch cultures of Chlorella emersonni as N-starvation progressed, normalised to pre-injection steady-state fluorescence (Ft). It is apparent that NH4+ additions (Fig. 1b) had a more complex effect on chl a fluorescence than did NO32 (Fig. 1a). Following injection of NO32, there was a slow, steady decline in fluorescence after 30–300 seconds (DDrop), followed by a very slow, gradual increase in fluorescence emission over a longer time interval, to ,75% of initial, pre-injection fluorescence (Ft) after 400 seconds. In contrast, NH4+ injection caused an initial small but marked (,10%) rise in fluorescence output after 10– 50 seconds (DPeak), quickly followed by a rapid drop in fluorescence after 50–100 seconds (DDrop), with fluorescence reaching a minimum (90%) before returning to a new, lower steady state value (91–94% of Ft) after 130 seconds (Fig. 1b). Addition of a nonlimiting nutrient (e.g. PO432) or control (dH2O) to the ‘low-N’ or ‘high-N’ Chlorella cultures produced no measurable change in fluorescence output, nor did the addition of NH4+ or NO32 to Chlorella cells grown in nutrient replete medium (data not shown). TIMING OF THE ONSET OF NIFTS: In the low-N Chlorella cultures, the addition of NO32 on day 1 produced no noticeable change in fluorescence (Fig. 3b), although the addition of NH4+ elicited a characteristic NH4+ NIFT, which was small in magnitude (,5% DPeak, ,5% Ddrop; Fig. 3a). By day 4, a more developed NIFT was evident and at its most prominent for both NH4+ (32% change in Ft,) and NO32 (23% change in Ft,) additions in the ‘low-N’ cultures, before beginning to disappear at day 7. By day 10, a NO32 NIFT had almost completely disappeared in the ‘low-N’ cultures (5% change in Ft; Fig. 3b), although the NH4+ NIFT was still evident, although of a considerably smaller magnitude than on day 4 (9% change in Ft; Fig. 3a). The % D Drop and % D Peak following NH4+ addition are quantified in Figs 1a, 4b, respectively. Both ‘low-N’ and ‘high-N’ batch cultures showed a significant (P , 0.05) rise to maximum peak in fluorescence following NH4+ injection on day 4 (18 and 28%; Fig. 4a). The % DDrop following the injection of NH4+ also increased significantly (P , 0.05) on day 4, before rapidly dropping as N-starvation progressed further (Fig. 4b). There were no significant differences in this pattern between ‘low-N’ and ‘high-N’ batch cultures (P . 0.05). By day 10, the % DDrop in response to NH4+ injection had declined significantly (P , 0.05) in both the ‘low-N’ and ‘high-N’ cultures (Fig. 4a), while the % Dpeak remained high with a significant difference (P , 0.05) remaining on day 10 between ‘low-N’ and ‘high-N’ cultures in the ‘high-N’ samples (19%; Fig. 4b). NIFTs showed a less distinct pattern in the % Ddrop following NO32 injection (Fig. 4c), compared with NH4+ injection (Fig. 4b). Both ‘low-N’ and ‘high-N’ cultures showed a large increase in the % Ddrop on day 4 following NO32 addition (31 and 30%, respectively). However, by day 7, ‘low-N’ batch cultures showed a decline in % Ddrop in response to NO32 addition, whilst the % Ddrop in the ‘high-N’ batch cultures remained significantly higher (e.g. 19% on day 10) compared to ‘low-N’ cultures (10% on day 10; P , 0.05; Fig. 4c). There appeared to be little correlation between the onset of NIFTs and trends in WPSIIe-max for Chlorella which, as already stated, remained consistently high over the course of the experiment (Fig. 2a). Indeed, the cultures exhibited the most marked NIFT responses on day 4, when WPSIIemax values were relatively high (0.76 and 0.77 for the lowand high-N cultures, respectively). FOURIER TRANSFORM INFRARED SPECTROSCOPY: FT-IR spectra were acquired for both ‘low-N’ and ‘high-N’ batch cultures. Amide I and II bands arising from protein and a broad band associated with the C-O stretches of carbohydrate were identified in the regions from 1630– 1677 cm21, 1520–1560 cm21 and 990–1100 cm21, respectively (Fig. 5A). Fig. 6a shows clearly that, as N-starvation progressed, both the carbohydrate : amide I and carbohydrate : amide II ratios increased substantially in both ‘highN’ and ‘low-N’ starved cultures, and were shown to be significantly different (P , 0.05, analysis of variance) from the replete (day 1) cells. Principal component analysis also was performed, which supported the discrete difference between day 1 and day 10 data for both ‘high’ and ‘low’ N Shelly et al.: Nitrogen limited NIFTs 507 Fig. 3. (a) Graph showing nutrient-induced fluorescence transients (NIFTs) following NH4+ injection (represented by the vertical line) on days 1 (closed circles), 4 (open circles), 7 (closed triangles) and 10 (open triangles). (b) Graph showing NIFTs following NO3 injection (represented by the vertical line) on days 1 (closed circles), 4 (open circles), 7 (closed triangles) and 10 (open triangles). All data is for the ‘low-N’ cultures and are normalised to steady state values prior to N-addition. Typical traces have been shown in this graph and displaced by 10% for clarity; any variation between traces can be seen in Fig. 4. The line on graph 4a indicates the percentage change in fluorescence. cells. A loading plot is used to assign coefficients to relevant PCs from an x, y-variable data set. Loadings express relations between variables (i.e. wavenumber values), and enable one to tell which variables are dominating or influencing the model and how they are associated with one another. Analysis of the PC1 loadings plot in this study confirmed that the separation along PC1 primarily was associated with changes in the intensity of carbohydrate bands (data not shown). RAMAN SPECTROSCOPY: Raman spectroscopy was performed on ‘low-N’ and ‘high-N’ cultures. Chl a levels (identified as the integrated area between 1314 to 1337 cm21, Fig. 5B) showed a decline in the ‘low-N’ cultures after a short period of starvation and b-carotene (identified as integrated band areas from 1132–1172 and 1491–1518 cm21, referred to as b-carotene bands 1 and 2, respectively; Fig. 5B; see Wood et al. 2005 for a full description of band assignments). A clear decline over time in the chl a : b-carotene ratio is evident in both N treatments (Fig. 6b). All changes in cells from day 1 (replete) to day 10 (‘high’ and ‘low’ N) were significantly different (P , 0.05, analysis of variance). Principal component analysis also was performed (data not shown), which supported the discrete differences between day 1 and day 10 data for both ‘high’ and ‘low’ N cells. Loadings plots, in this case such differences were principally influenced by the changes in the b-carotene bands 1 and 2 (data not shown). Fig. 4. (a) Percentage difference in DPeak following NH4+ injection into ‘low-N’ (dark bars) and ‘high-N’ (light bars) cultures of Chlorella emersonii cells. (b) Percentage difference in DDrop following NH4+ injection into ‘low-N’ (dark bars) and ‘high-N’ (light bars) cultures of C. emersonii cells. (c) Percentage difference in DDrop following KNO3 injection into (‘low-’ and ‘high-N’) cultures of C. emersonii cells. All data shown are the mean of replicate batch cultures, n 5 3. Error bars represent the standard deviations. 508 Phycologia, Vol. 46 (5), 2007 Fig. 5. Representative curves from Chlorella cells on days 1 (replete) and 10 (‘high-’ and ‘low-N’) from (A) Fourier transform infrared (FT-IR) data showing the amide I (1630–1677 cm21), II (1520–1560 cm21) and carbohydrate (990–1100 cm21) bands. (B) Raman spectroscopy data showing bands for b-carotene (1491–1548 cm21) and chl a (1314–1327 cm21). DISCUSSION Nitrogen limitation can affect a number of processes in phytoplankton including photosynthesis, photochemical energy conversion and protein synthesis (Berges et al. 1996; Jansen et al. 1996; Masi & Melis 1997). This study showed that cellular Chl a : b-carotene ratios, measured using both a conventional spectroscopic assay as well as Raman spectroscopy, declined in the freshwater chloro- phyte Chlorella emersonii as N-starvation progressed. Raman spectroscopy can be an informative tool for the study of many biological systems because of the large number of active vibrational modes and the relative lack of spectral interference from water. The strong enhancement of many b-carotene bands at 785 nm makes Raman an excellent diagnostic tool to gain quick and precise information regarding chl a and b-carotene content (Wood et al. 2005). It is far more specific than conventional Fig. 6. Integrated areas for Chlorella cells on days 1 (replete) and 10 (‘high-’ and ‘low-N’) showing (a) Fourier transform infrared (FT-IR) data for ratios of carbohydrates: amide I (dark bars) and amide II (light bars). (b) Raman data showing ratios of chl a : b-carotene (1314– 1327 cm21 and 1491–1548 cm21 respectively). All data for both FT-IR and Raman on day 10 (‘high-’ and ‘low-N’) were shown to be significantly different from day 1 (replete; P , 0.05, analysis of variance) marked with an asterisk (*). Shelly et al.: Nitrogen limited NIFTs spectroscopic methods (e.g. Golterman & Clymo 1971), which only measure carotenoids as a group of compounds, rather than specifically b-carotene, and is much faster than high performance liquid chromatography (HPLC), which, while giving information on specific pigments, can be time consuming. Raman spectroscopy also can be applied to single cells rather than the bulk populations required for conventional spectrophotometric and HPLC approaches. It is well established that N-deficiency in eukaryotic algae can lead to decreases in antenna size and a decrease in the chl a : carotenoid ratio (Turpin 1991).This decline in chl a, as well as in proteins (see discussion of FT-IR data below), appears to imply either that the photosynthetic complex of Chlorella was compromised, or simply that there were reduced levels of photosynthetic units per cell which remained fully functional and were capable of maintaining photosynthetic efficiency as nitrogen starvation progressed. Photosynthesis can be affected by nitrogen limitation directly through the reduction in energy-collecting efficiency brought about by the loss of chl a and the concomitant increase in carotenoid pigments which are photochemically inactive (Herzig & Falkowski 1989; Berges et al. 1996). Photochemical energy conversion is affected by a reduction in protein synthesis, which ultimately affects the protein content of the PSI and PSII reaction centres. Although prior research has found that PSII content is affected more by nitrogen limitation than is PSI, it must be acknowledged that this may vary between species (Behrenfeld et al. 1996; Berges et al. 1996). Given that the PSII proteins, such as D1, have a rapid turnover, a decline in nitrogen availability could (1) reduce the supply of amino acids for repair; and (2) through effects on electron transport, reduce the adenosine 59-triphosphate (ATP) available to drive (re)synthesis of this protein, in effect enhancing the decline in PSII photosynthesis. In the current study, however, Chlorella showed no marked change in WPSIIe-max over the course of starvation. This observation was surprising, because the photosynthetic capacity of algal cells (including WPSIIe-max) typically declines markedly during N-limitation (Falkowski et al. 1989; Geider et al. 1993; Shelly et al. 2002; Young & Beardall 2003a). The fact that little difference in WPSIIe-max was observed between both the ‘low-N’ and ‘high-N’ cultures also suggested that the degree of N-starvation had little impact on photosynthetic capacity in Chlorella, with likely implications for the NIFT observations in the two treatments. In N-stressed batch cultures of Dunaliella, for example, WPSIIe-max decreased from more than 0.6 to 0.2 over 4 days (Young & Beardall 2003b). Other studies, however, have reported a contrasting trend similar to that observed here for Chlorella, in which WPSIIe-max values have remained consistently high over the course of nutrient starvation (Cullen et al. 1992; MacIntyre et al. 1997; Parkhill et al. 2001). Equally high WPSIIe-max values also were observed during the current study in C. emersonii grown in N-limited semicontinuous cultures (Shelly et al., unpublished data). Viewed collectively, these findings appear to suggest that WPSIIe-max responses to nutrient stress in algae are species-specific and that WPSIIe-max is not a robust indicator of nutrient stress in all algae (or, at least, not in N-limited Chlorella; see Kruskopf & Flynn 2006 for 509 a critique). One hypothesis is that algal cells can use ATP produced from cyclic electron flow around PSI, in order to repair damage to PSII or to drive nutrient uptake through ATP-dependent pumps (Berges 1997). Whether this mechanism would be capable of maintaining the integrity of PSII and sustaining the high WPSIIe-max observed here for Nstarved Chlorella is not known. FT-IR spectroscopy provides information on vibrationally active functional groups associated with macromolecules in biological samples, reflecting both the molecular structure and environment of the sample. The FT-IR technique has been used to examine isolated macromolecules such as nucleic acids, proteins, lipids and polysaccharides, with some studies having extended this work to investigate whole organisms, such as marine microalgae (Giordano et al. 2001) and higher plants (Stuart 1997; Heraud et al. 2006). Previous studies (Parker 1971) on the macromolecular content of cells have allowed a summary of band assignments to be collated. These studies also have validated the bands with standards, allowing the characterisation of amide I and amide II (proteins) by two strong bands at ,1650 cm21 and ,1540 cm21, assigned to specific vibrations of the peptide moiety. Carbohydrates show characteristic C-O bonds at ,1033, 1080 and 1150 cm21, while the carbonyl group is observed at 1740 cm21 (Kansiz et al. 1999). FT-IR analysis in the current study clearly revealed dramatic spectral differences between N-replete (day 1) and N-limited (day 10) Chlorella cultures. As N- starvation was induced, there was a shift towards carbohydrate accumulation, relative to protein. It is well established that N-limited algal cells generally accumulate starch or lipid and use this as a source of carbon for amino acid synthesis (Turpin 1991). Documentation of protein loss in algal cells during Nlimitation is extensive (Richards & Thurston 1980; Kolber et al. 1988; La Roche et al. 1993; Quigg and Beardall 2003; Young and Beardall 2003b). Smith et al. (1989) showed that allocation of ATP to protein synthesis declined when Nlimitation was imposed on the ice alga Nitzschia seriata, although allocation towards lipids increased. With certain exceptions (MacIntyre et al. 1997), studies have shown large declines in the pools of Rubisco under nitrogen limitation (Beardall et al. 1991). Young & Beardall (2003a) suggested that, under some conditions, the Rubisco protein can act as a store of N, which then can be mobilised to enable maintenance of other N-requiring functions, such as photosynthetic electron transport, under stress conditions. Given that Chlorella exhibited little change in WPSIIe-max during the current experiment, we can only assume that the turnover rate of the D1 protein remained intact and that the shift in cellular energy allocation from protein towards carbohydrates synthesis had little effect on the photosynthetic apparatus of Chlorella. As starvation progressed, the addition of NH4+ and NO32 to the N-limited Chlorella cells elicited characteristic, transient changes in in vivo chl a fluorescence (NIFTs). The configuration of the NIFT response was shown to depend on the form in which the nitrogen was supplied: NH4+ elicited a small, sudden rise in fluorescence, which then dropped sharply, before recovering to a new, lower steady state; NO32 additions, in contrast, caused a much more gradual, steady decline in fluorescence. Interestingly, the 510 Phycologia, Vol. 46 (5), 2007 latter response differed from that found in Dunalliella tertiolecta by Young & Beardall (2003b), supporting predictions that the precise nature of the fluorescence change depends on the particular algal species (Wood & Oliver 1995; Holland et al. 2004). In contrast, the NH4+–induced responses observed here were very similar to those reported by Holland et al. (2004) for N-limited Chlorella and by Young & Beardall (2003b) for N-starved D. tertiolecta, comprising an initial rapid and distinct peak in fluorescence, followed by a trough and then a gradual recovery in fluorescence to a new, lower, steady state level. As in previous studies (Beardall et al. 2001a, b; Young & Beardall 2003b), fluorescence perturbations were not seen in N-replete Chlorella cultures following additions of NH4+ and NO32, or in N-limited cultures following the addition of a nonlimiting nutrient (e.g. PO432) or control i.e. water (data not shown). It is worth pointing out that we investigated the responses of NH4+ and NO32 addition to cells that previously had been grown on nitrate. Whether these responses differ for cells grown on ammonia remains to be seen. Results from the current study on N-limited Chlorella indicated that the timing of NIFTs (i.e. their onset and disappearance) varied according to both the starting nitrogen concentration in the medium and the form of nitrogen (NH4+ or NO32) supplied. For example, ‘high-N’ cultures resupplied with NO32 showed a greater % Ddrop for an extended period of time compared with ‘low-N’ cultures, presumably reflecting the delayed starvation of the former cultures, in which cells were slower to reach the critical stage at which they lost the ability to show a NIFT. In ‘low-N’ cultures (initially 50 mm KNO3), NH4+ –NIFTs were, however, present from day 1 through to day 10; this is a longer timeframe than that reported by Holland et al. (2004), who observed NH4+–NIFTs over a period of 4 days in N-starved Chlorella cultures. In contrast, NO32–NIFTs appeared to have a smaller window of occurrence, being first present on day 4 and having completely disappeared by day 10. Young & Beardall (2003b) similarly recorded the persistence of NH4+–induced fluorescence perturbations for several days after additions of NO32 had ceased to elicit a fluorescence response. Both ‘low-N’ and ‘high-N’ cultures showed maximum changes in fluorescence following either NH4+ or NO32 injections on day 4, indicating the greatest fluorescence transients occurred prior to cells becoming extremely Nstarved. Other studies likewise have shown that the NO32induced NIFT disappears under extreme nutrient limitation (Roberts 1998; Young 1999). One explanation is that, in order to respond to NO32, cells must possess an induced and optimised NO32 uptake and/or reduction capacity, mechanisms which are only active in cells currently or recently supplied with external NO32 (Young & Beardall 2003b). Furthermore, recovery of NO32-uptake in Nstarved D. tertiolecta was shown to require protein synthesis (Young 1999). After prolonged starvation, the loss of fluorescence perturbations seems to suggest that the NO32/NO22 flux into the chloroplast is inadequate to induce the effect of N-assimilation on photosynthetic suppression. The fluorescence transients exhibited following NH4+ or NO32 injection to N-limited Chlorella presumably are induced by the uptake and assimilation of the limiting nutrient, nitrogen. N-uptake and assimilation in algae is dependent on photosynthesis for energy and carbon skeletons, and involve metabolic processes in both chloroplasts and mitochondria (Turpin et al. 1997). NH4+ or NO32 assimilation and uptake can influence cellular charge equilibria and, therefore, vary the relative requirement for ATP by photosynthesis and nitrogen metabolism (Turpin & Weger 1988; Holmes et al. 1989). Weger & Turpin (1989) showed that the decrease in NH4+ assimilation, in the absence of mitochondrial electron transport chain activity during photosynthesis, is not due to a limitation in ATP supply but rather to a shortage of carbon skeletons for amino acid synthesis. Holmes et al. (1989) also found that resupply of NH4+ to N-limited Selenastrum minutum resulted in a drop in Rubisco levels and limitation of photosynthetic carbon fixation, which they postulated was due to increased requirements for carbon skeletons in the synthesis of amino acids. Studies on S. minutum, using the electron transport inhibitor, DCMU, resulted in an 82% decrease in the rate of NH4+ assimilation, although NO32 assimilation was unaffected (Weger & Turpin 1989). It appears that, once the nutrient pulse has been added to the limited cells, amino acid turnover is stimulated via a reallocation in the source of these carbon skeletons from the Calvin cycle to stored carbohydrates, such as starch (Turpin & Weger 1988; Wood & Oliver 1995). Ammonium addition to both high- and low-N batch cultures resulted in an increase in DPeak within about 10 seconds; this is approximately the same timeframe that Turpin & Weger (1988) found for a decline in O2 evolution in S. minutum, signalling a suppression of photosynthesis as energy was reallocated to N-uptake and assimilation. DDecline followed the DPeak at around 15 seconds, which also seems to correspond with the timeframe for completion of ammonium assimilation and the recovery of photosynthesis and O2 evolution (Turpin & Weger 1988). Additions of NO32 or NH4+ to nutrient-replete Chlorella cells elicited no changes in chl a fluorescence. It is likely that high glutamine/glutamate ratios in the chloroplasts of nutrient replete cells maintain a priority for photosynthesis over N assimilation (Flynn 1991), so that N additions do not lead to changes in the relative use of ATP and electrons and so do not cause perturbations in chl a fluorescence. Young & Beardall (2003b) found that the resupply of NH4+ and NO32 to N-stressed D. tertiolecta cells also produced changes in nonphotochemical quenching, probably due to state transitions resulting from the reallocation of light harvesting components between PSI and PSII (Muller et al. 2001). For instance, S. minutum has been shown to exhibit a reversible transition from state I to state II under N-limitation, diminishing PSII activity and elevating the energy accessible to PSI (Turpin 1991). This would subsequently increase the ATP/nicotinamide adenine dinucleotide phosphate (NADPH) production ratio, in line with the metabolic requirements of NH4+ assimilation. Assimilation of NO32 and NO22 has an ATP/NADPH production ratio similar to that of CO2 assimilation, and these ions were not found to induce state transitions in S. minutum (Turpin 1991). State transitions could be a method in which algae maintain equilibrium of ATP and NADPH Shelly et al.: Nitrogen limited NIFTs production with changing metabolic demands. Whether a state transition is responsible for the fluorescence changes observed in the present study is yet to be determined. Unlike traditional mechanisms for assessing nutrient limitation in algae, NIFTs constitute rapid changes in chlorophyll fluorescence over time scales of minutes, thereby potentially offering an immediate indication of the nutrient status of a particular algal population. Whilst some parameters were measured using pulse amplitude modulated (PAM) fluorometers, steady state fluorescence for NIFT experiments were measured using the more simplistic Hitachi Spectrophotometer, paving the way for field experiments to be carried out on simple, affordable fluorometers. Previous studies assessing the applicability of the technique for investigating in situ algal nutrient limitation have reported encouraging results for nitrate-induced NIFTs in the green algae Dunaliella tertiolecta (Young & Beardall 2003b) and for ammonium and phosphate-induced NIFTs in Chlorella emersonii and the cyanobacterium Oscillatoria sp. (Holland et al. 2004), as well as in natural, mixed field assemblages (Wood & Oliver 1995; Holland et al. 2004). The current characterisation of the distinct fluorescence responses of Nstarved Chlorella emersonii to NH4+ and NO32 additions provides further evidence of the potential of NIFTs both for identifying N-limitation generally and for assessing the relative importance to algal nutrient of different nitrogen sources. The apparent insensitivity of the onset and magnitude of fluorescence changes to the initial N concentrations (50 and 100 mM NO3 in the ‘low-N’ and ‘high-N’ cultures, respectively) may be a caveat to the precision and application of the technique as a diagnostic tool for the degree of nutrient limitation. The observed high WPSIIe-max values, however, indicate that Chlorella emersonii cells may behave atypically under N-limiting conditions by apparently maintaining a high photosynthetic efficiency. Thus, the interaction between N-assimilation and photosynthetic suppression believed responsible for causing the fluorescence transients may likewise be atypical in Chlorella. Additional work is needed in order to better elucidate the physiology behind the NIFT and to assess the variability, or otherwise, of nutrient-induced fluorescence perturbations in different algal species under varying levels of nutrient deficiency. ACKNOWLEDGEMENTS This work was supported by the Australian Research Council. Tara Higgins was a visitor to Monash University on an Endeavour Fellowship awarded by the Australian Department for Education, Science and Training (DEST). REFERENCES BEARDALL J., ROBERTS S. & MILLHOUSE J. 1991. Effect of nitrogen limitation on uptake of inorganic carbon and specific activity of ribulose-1,5-bisphosphate carboxylase/oxygenase in green microalgae. Canadian Journal of Botany 69: 1146–1150. 511 BEARDALL J., BERMAN T., HERAUD P., OMO KADIRI M., LIGHT B.R., PATTERSON G., ROBERTS S., SULZBERGER B., SAHAN E., UEHLINGER U. & WOOD B. 2001a. A comparison of methods for detection of phosphate limitation in microalgae. Aquatic Sciences 63: 107–121. BEARDALL J., YOUNG E. & ROBERTS S. 2001b. Approaches for determining phytoplankton nutrient limitation. Aquatic Sciences 63: 44–69. BEHRENFELD M.J., BALE A.J., KOLBER Z.S., AIKEN J. & FALKOWSKI P.G. 1996. Confirmation of iron limitation of phytoplankton photosynthesis in the equatorial Pacific Ocean. Nature 383: 508–511. BERGES J.A. 1997. Algal nitrate reductases. European Journal of Phycology 32: 3–8. BERGES J.A., CHARLESBOIS D.O., MAUZERALL D.C. & FALKOWSKI P.G. 1996. Differential effects of nitrogen limitation of photosynthetic efficiency of photosytems I and II in microalgae. Plant Phycology 110: 689–696. BIRCH P.B., GORDON D.M. & MCCOMB A.J. 1981. Nitrogen and phosphorus nutrition of Cladophora in the Peel-Harvey Estuarine System, Western Australia. Botanica Marina 2: 381–387. BURNISON B.K. 1980. Modified dimethyl sulfoxide (DMSO) extraction for chlorophyll analysis of phytoplankton. Canadian Journal of Fisheries and Aquatic Sciences 37: 729–733. CULLEN J.J., YANG X. & MACINTYRE H.L. 1992. Nutrient limitation of marine photosynthesis. In: Primary Productivity and Biogeochemical Cycles in the Sea (Ed. P.G. Falkowski & A.D. Woodhead), Plenum Press, New York, pp. 31–45. EILERS P.H.C. & PEETERS J.C.H. 1988. A model for the relationship between light intensity and the rate of photosynthesis in phytoplankton. Ecological Modeling 42: 199–215. ELSER J.J., MARZOLF E.R. & GOLDMANM C.R. 1990. Phosphorus and nitrogen limitation of phytoplankton growth in the freshwaters of North America: a review and critique of experimental enrichments. Canadian Journal of Fisheries and Aquatic Sciences 47: 1468–1477. FALKOWSKI P.G., SUKENIK A. & HERZIG R. 1989. Nitrogen limitation in Isochrysis galbana (Haptophyceae). II. Relative abundance of chloroplast proteins. Journal of Phycology 25: 471–478. FLYNN K.J. 1991. Algal carbon-nitrogen metabolism: a biochemical basis for modelling the interactions between nitrate and ammonium uptake. Journal of Plankton Research 13: 373–387. GAUTHIER D.A. & TURPIN D.H. 1997. Interactions between inorganic phosphate (Pi) assimilation, photosynthesis and respiration in the Pi-limited green alga Selenastrum minutum. Plant, Cell and Environment 20: 12–24. GEIDER R.J., LA ROCHE J., GREENE R.M. & OLAIZOLA M. 1993. Response of the photosynthetic apparatus of Phaeodactylum tricornutum (Bacillariophyceae) to nitrate, phosphate or iron starvation. Journal of Phycology 29: 755–766. GIORDANO M., KANSIZ M., HERAUD P., BEARDALL J., WOOD B. & MCNAUGHTON D. 2001. Fourier transform infrared spectroscopy as a novel tool to investigate changes in intracellular macromolecular pools in the marine microalga Chaetoceros muellerii (Bacillariophyceae). Journal of Phycology 37: 271–279. GOLTERMAN H.L. & CLYMO R.S. 1971. Methods for chemical analysis of fresh waters Blackwell Scientific, Oxford, 166 pp. HECKY R.E. & KILHAM P. 1988. Nutrient limitations of phytoplankton in freshwater and marine environments: a review of recent evidence on the effects of enrichment. Limnology and Oceanography 33: 796–822. HERAUD P.R., BEARDALL J., MCNAUGHTON D. & WOOD B.R. 2006. The effect of preprocessing on the classification of in vivo Raman spectra acquired from nutrient replete or nitrogen starved microalgal cells. Journal of Chemometrics 20: 1–5. HERAUD P.R., BEARDALL J. & MCNAUGHTON D. In vivo prediction of nutrient status of individual algal cells using Raman microspectroscopy. FEMS Microbiology Letters. HERAUD P.R., CAINE S., SANSON G., GLEADOW R., MCNAUGHTON D. & WOOD B.R. 2006. Comparison between synchrotron infrared micro-spectroscopic mapping and focal plane array imaging of leaf tissue. New Phytologist 3: 216–225. 512 Phycologia, Vol. 46 (5), 2007 HERZIG R. & FALKOWSKI P.G. 1989. Nitrogen limitation in Isochrysis galbana. 1. Photosynthetic energy conversion and growth efficiencies. Journal of Phycology 25: 462–471. HOLLAND D., ROBERTS S. & BEARDALL J. 2004. Assessment of the nutrient status of phytoplankton: a comparison between conventional bioassays and nutrient-induced fluorescence transients (NIFTs). Ecological Indicators 4: 149–159. HOLMES J.J., WEGER H.G. & TURPIN D.H. 1989. Chlorophyll a fluorescence predicts total photosynthetic electron flow to CO2 or NO32/NO22 under transient conditions. Plant Physiology 91: 331–337. JANSEN M.A.K., GREENBERG B.M., EDELMAN M., MATTO A.K. & GABA V. 1996. Accelerated degradation of the D2 protein of Photosystem II under ultraviolet radiation. Photochemistry and Photobiology 63: 814–817. KANSIZ M., HERAUD P., WOOD B., BURDEN F., BEARDALL J. & MCNAUGHTON D. 1999. Fourier transform infrared microspectroscopy and chemometrics as a tool for the discrimination of cyanobacterial strains. Photochemistry 52: 407–417. KOLBER Z., ZEHR J. & FALKOWSKI P.G. 1988. Effects of growth irradiance and nitrogen limitation on photosynthetic energy conversion in photosystem 2. Plant Physiology 88: 923–929. KOLBER Z.S., BARBER R.T., COALE K.H., FITZWATER S.E., GREENE R.M., JOHNSON K.S., LINDLEY S. & FALKOWSKI P.G. 1994. Iron limitation of phytoplankton photosynthesis in the equatorial Pacific Ocean. Nature 371: 145–149. KRUSKOPF M. & FLYNN K.J. 2006. Chlorophyll content and fluorescence responses cannot be used to gauge reliably phytoplankton biomass, nutrient status or growth rate. New Phytologist 169: 525–536. LA ROCHE J., GEIDER R.J., GRAZIANO L.M., MURRAY H. & LEWIS K. 1993. Induction of specific protein in eukaryotic algae grown under iron–phosphorus or nitrogen deficient conditions. Journal of Phycology 29: 767–777. LEAN D.R.S. & PICK F.R. 1981. Photosynthetic response of lake plankton to nutrient enrichment: a test for nutrient limitation. Limnology and Oceanography 26: 1001–1019. LIPPEMEIER S.R.H., VANSELOW K.H., HARTIG P. & COLJIN F. 2001. In-line recording of PAM fluorescence of phytoplankton cultures as a new tool for studying effects of fluctuating nutrient supply of photosynthesis. European Journal of Phycology 36: 89–100. MACINTYRE H.L., SHARKEY T.D. & GEIDER R.J. 1997. Activation and deactivation of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco) in three marine microalgae. Photosynthesis Research 51: 93–106. MASI A. & MELIS A. 1997. Morphological and molecular changes in the unicellular green alga Dunaliella salina grown under supplemental UV-B radiation: cell characteristics and Photosystem II damage and repair properties. Biochimica Biophysica Acta 1321: 183–193. MILLER A.G., ESPIE G.S. & CANVIN D.T. 1991. The effects of inorganic carbon and oxygen on fluorescence in the cyanobacterium Synechococcus UTEX 625. Canadian Journal of Botany 69: 1151–1160. MORRIS I. & SYRETT P.J. 1965. The effect of nitrogen starvation on the activity of nitrate reductase and other enzymes in Chlorella. Journal of General Microbiology 38: 21–28. MULLER P., LI X.P. & NIYOGI K.K. 2001. Nonphotochemical quenching. A response to excess light energy. Plant Physiology 125: 1558–1566. PARKER F.S. 1971. Application of infrared spectroscopy in biochemistry, biology and medicine. Plenum, New York, 601 pp. PARKHILL J., MAILLET G. & CULLEN J. 2001. Fluorescence-based maximal quantum yield for PSII as a diagnostic of nutrient stress. Journal of Phycology 37: 517–529. QUIGG A. & BEARDALL J. 2003. Protein turnover in relation to maintenance metabolism at low photon flux in two marine microalgae. Plant, Cell and Environment 26: 693–703. RICHARDS L. & THURSTON C.F. 1980. Protein turnover in Chlorella fusca var. vacuolata: measurement of the overall rate of intracellular protein degradation using isotope exchange with water. Journal of General Microbiology 121: 49–61. ROBERTS S.C. 1998. Physiological effects of phosphorus limitation on photosynthesis in two green algae. PhD Thesis, Monash University, Clayton, Victoria, Australia. 116 pp. SCHINDLER D.W. 1977. Evolution of phosphorus limitation in lakes. Science 195: 260–262. SHELLY K., HERAUD P. & BEARDALL J. 2002. Nitrogen limitation in Dunaliella tertiolecta Butcher (Chlorophyceae) leads to increased susceptibility to damage by ultraviolet-B radiation but also increased repair capacity. Journal of Phycology 38: 1–8. SMITH R.E.H., CLEMENT P. & HEAD E. 1989. Biosynthesis and photosynthate allocation patterns of arctic ice algae. Limnology and Oceanography 34: 59l–605. STUART B. 1997. Biological applications of infrared spectroscopy. Wiley, Chichester, 212 pp. TURPIN D.H. 1991. Effects of inorganic N availability on algal photosynthesis and carbon metabolism. Journal of Phycology 27: 14–20. TURPIN D.H. & WEGER H.G. 1988. Steady-state chlorophyll a fluorescence transients during ammonium assimilation by the N-limited green alga Selenastrum minuturn. Plant Physiology 88: 97–101. TURPIN D.H., WEGER H.G. & HUPPE H.C. 1997. Interactions between photosynthesis, respiration and nitrogen metabolism. In: Plant Metabolism (Ed. by D.T. Dennis, D.B. Layzett, D.D. Lefeovre & D.H. Turpin), pp. 509–524. Addison Wesley Longman, Harlow. VAN KOOTEN O. & SNEL J.F.H. 1990. The use of chlorophyll fluorescence nomenclature in plant stress physiology. Photosynthesis Research 25: 147–150. WEGER H.G. & TURPIN D.H. 1989. Mitochondrial respiration can support NO32 and NO22 reduction during photosynthesis. Interactions between photosynthesis, respiration and N assimilation in the N-limited green alga Selenastrum minutum. Plant Physiology 89: 409–415. WOOD B.R., HERAUD P., STOJKOVIC S., MORRISON D., BEARDALL J. & MCNAUGHTON D. 2005. A portable Raman acoustic levitation spectroscopic system for the identification and environmental monitoring of algal cells. Analytical Chemistry 77: 4955–4961. WOOD M.D. & OLIVER R.L. 1995. Fluorescence transients in response to nutrient enrichment of nitrogen- and phosphoruslimited Microcystis aeruginosa cultures and natural phytoplankton populations: a measure of nutrient limitation. Australian Journal of Plant Physiology 22: 331–340. WYNNE D. & BERMAN T. 1980. Hot water extractable phosphorus — an indicator of nutritional status of Peridinium cinctum (Dinophyceae) from Lake Kinneret (Israel)? Journal of Phycology 16: 40–46. YOUNG E.B. 1999. Interactions between photosynthetic carbon and nitrogen acquisition in the marine microalga Dunaliella tertiolecta Butcher. Ph.D. Thesis, Monash University, Clayton, Victoria, Australia. 228 pp. YOUNG E.B. & BEARDALL J. 2003a. Photosynthetic function in Dunaliella tertiolecta (Chlorophyta) during a nitrogen starvation and recovery cycle. Journal of Phycology 39: 897–905. YOUNG E.B. & BEARDALL J. 2003b. Rapid ammonium- and nitrate-induced perturbations to chl a fluorescence in nitrogenstressed Dunaliella tertiolecta (Chlorophyta). Journal of Phycology 39: 332–342. Received 14 July 2006; accepted 30 April 2007 Associate editor: Charles Amsler