Performance of the Redfield Ratio and a Family of Nutrient Limitation Indicators as Thresholds for Phytoplankton N vs. P Limitation
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- Ptacnik, R., Andersen, T. & Tamminen, T. Ecosystems (2010) 13: 1201. doi:10.1007/s10021-010-9380-z
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We aim to define the best nutrient limitation indicator predicting phytoplankton biomass increase as a result of nutrient enrichment (N, P, or both). We compare the abilities of different indicators, based on chemical measurements of nitrogen (N) and phosphorus (P) fractions in the initial plankton community, to predict the limiting factor for phytoplankton growth as inferred independently from short-term laboratory experiments on the same natural communities in a data set from NE Baltic Sea (Tamminen and Andersen, Mar Ecol Prog Ser 340:121–138, 2007). The best indicators had a true positive rate of about 80% for predicting both N and P limitation, but with a higher false positive rate for N than for P limitation (25 vs. 5%). Estimated threshold ratios for total nutrients (TN:TP) were substantially higher than the Redfield ratio, reflecting the relatively high amounts of biologically less available dissolved organic N in the study area. The best overall performing indicator, DIN:TP, had chlorophyll-response based threshold ratios far below Redfield, with N limitation below 2:1 and P limitation above 5:1 (by atoms). On the contrary, particulate N:P ratio was the overall worst predictor for N or P limitation, with values clustering around the Redfield N:P ratio (16:1, by atoms) independent of the limiting factor. Estimated threshold ratios based on inorganic nutrients (DIN:DIP) and so-called biologically available nutrients (BAN:BAP = (PON + DIN):(POP + DIP)) were also generally clearly above 16:1, indicating that the Redfield ratio rather reflects the transition from N limitation to combined N + P limitation, than to single limitation by P. Coastal systems are complex systems with regard to nutrient dynamics, historically considered to represent the transition from P-limited freshwater to N-limited marine systems. Our analysis shows that rather simple ratios reflect phytoplankton requirement for nutrients. Based on the high prediction performance, analytical considerations, and general data availability, the DIN:TP ratio appears to be the best indicator for inferring in situ N vs. P limitation of phytoplankton from chemical monitoring data.
Keywordseutrophication coastal ecosystems Baltic sea stoichiometry phytoplankton Redfield ratio indicators
The Redfield ratio, describing average composition of phytoplankton biomass (Redfield 1934, 1958), is the most broadly applied stoichiometric reference for nutrient limitation of planktonic production. This indicator is recurrently applied from global-scale oceanic biogeochemistry to management-oriented load-response models, and to algal physiology. Redfield originally derived the statistical ratios of key biogenic elements from data for ‘the oceans as a whole’, developing a concept of global biogeochemistry based on reciprocal interactions of planktonic biota and their environment over geological time scales.
Redfield emphasized from the beginning that in coastal waters, the ratios of the elements can depart widely from the averages due to proximity to terrestrial nutrient sources, and that the composition of different planktonic species differ. Despite these statements, especially his average N:P (molar) ratio of 16 has been adopted almost as a law of nature, benchmarking a universal nutrient limitation threshold, and has been extended far beyond the original domain of its derivation, up to headwater lakes and algal monocultures in test tubes.
Several recent examinations of the metabolic basis of phytoplankton nutrient limitation and oceanic biogeochemistry (for example, Falkowski 2000; Geider and LaRoche 2002; Arrigo 2005) have deepened our understanding of both nutritional demands of phytoplankton, and of several ‘non-Redfield’ processes of aquatic ecosystems. There is an acute need, however, for critically analyzed N vs. P limitation thresholds in indicators that could be applied to monitoring, modeling, and management of coastal ecosystems (Howarth and Marino 2006).
Degradation of aquatic systems by eutrophication is a global problem calling for well-planned and efficient management strategies. Eutrophication generally refers to increased aquatic production due to increased availability of nutrients, with an array of cascading consequences within the system, such as biomass accumulation, species replacement, and oxygen deficits. Proper identification of the nutrients limiting phytoplankton growth is thus a necessary prerequisite for successful eutrophication reduction at impacted sites where future changes in nutrient discharges may alter the prevailing limitation patterns (Cloern 2001; Ptacnik and others 2005).
Historically, marine and terrestrial systems have been considered primarily N-limited (Howarth and Marino 2006; Vitousek and Howarth 1991), whereas predominant P limitation has been the paradigm for lakes (Schindler 1977). Coastal systems represent transitional zones between terrestrial, freshwater, and marine nutrient cycles, appearing thus specifically to call for reliable N vs. P limitation indicators. However, a recent meta-analysis questioned any basic dichotomy in nutrient limitation between different habitats, by finding surprising similarity across major ecosystem types in terms of N and P limitation (Elser and others 2007). Moreover, they found widespread co-limitation by N and P in all systems studied, indicating closely balanced N and P supplies in most environments. This calls attention to the need for local assessments of limiting nutrients in environmental management, but also sets demands for limitation indicators to be able to distinguish between N, P, and combined N and P limitation.
Here we investigate how in situ phytoplankton nutrient limitation is related to different fractions of ambient nutrient concentrations, and aim at developing an optimal predictor for the primary limiting nutrient. Instead of studying the Redfield ratio through statistical analysis of extensive field data (Redfield 1934, 1958) or from the first principles of phytoplankton metabolism (Falkowski 2000; Geider and LaRoche 2002), we adopt an approach that might be described as heuristic. We base our analysis on a large coastal dataset consisting of a 3-year series of bioassay experiments assessing patterns of nutrient limitation of phytoplankton, based on both chlorophyll a and primary productivity responses in P- and N-limited sub-basins of the Baltic Sea (Tamminen and Andersen 2007; Andersen and others 2007).
We take these experimentally verified phytoplankton limitation patterns as our starting point, collapse the seven generic limitation categories (Andersen and others 2007) into a univariate limitation indicator, and relate this information on observed phytoplankton limitation to initial nutrient data. We employ hyperbolic tangent functions to derive chemical limitation indicators with constant and non-constant (that is, scaling with nutrient concentrations) threshold N:P ratios for the transitions between N, N + P, and P limitation. Finally, we analyze the performance of the indicators quantitatively with multiple criteria (coefficient of determination and Akaike Information Criterion regression statistics, as well as Receiver Operating Characteristics plots).
Materials and Methods
Experimental Set-Up and Analyses
A detailed description of the study area and bioassay experiments is given in Tamminen and Andersen (2007); therefore only a brief sketch is provided here. During the growth seasons of 1992–1994, 3-day time-series bioassay experiments were carried out at regular time intervals over the season at six monitoring stations along the 1000 km of Finnish coastline, spanning the large-scale Baltic Sea gradients in salinity and eutrophication, and also a continuum from P to N limitation (Tamminen and Andersen 2007). A correlation analysis showed overall low association among major environmental variables (see Supplementary material). In particular, correlations among salinity and major nutrient fractions were negligible. Hence it seems unlikely that potential relationships between limitation patterns and nutrient concentrations will be confounded by an underlying salinity gradient.
Seven to 12 experiments were done per station and year, resulting in a total of 170 experiments. Each experiment was started by taking an initial sample from a monitoring station. An array of physical and chemical parameters was measured on this non-manipulated initial sample using standard methods. The following initial analyses were used for constructing the limitation indicators of this study: dissolved inorganic nitrogen (DIN) as the sum of ammonium, nitrate and nitrite; dissolved inorganic phosphate (DIP); total N and P (TN, TP); all measured in duplicate with wet chemistry and photometric detection according to Grasshoff and others (1983). In addition, particulate P (POP) was measured after Solorzano and Sharp (1980), and particulate N (PON) with a mass spectrometer (Europa Scientific), both after filtering duplicate samples onto glass-fiber filters (Whatman GF/F; acid-washed and precombusted at 500°C).
Each experiment consisted of eight subsamples (6 l) from the initial sample, amended with phosphorus (0.65 μmol l−1) and ammonium (2.86 μmol l−1) additions according to a 2 × 2 factorial design with replicates. Treatments were incubated for 72 h at in situ temperature and a photoperiod corresponding to the time and location of the sampling (light intensity: 100 μmol quanta m−2 s−1). All experimental units were sampled for chlorophyll a on days 1–3, and 14C-uptake was measured on days 1 and 2. Parameters were measured in duplicate, giving a total of 50 chlorophyll a samples and 34 14C-samples from each experiment (including the initial measurements). Methods for the experiment response analyses are detailed in Tamminen and Andersen (2007).
Statistical Analysis of the Bioassay Experiments
The most probable nutrient limitation in a given experiment was inferred by a statistical model selection procedure contrasting 21 different candidate models representing biologically consistent response patterns. A resampling approach based on the lowest replication level was used for estimating probabilities for different limitation categories in each experiment. These probabilities also represent uncertainties in the limitation class assignments; an experiment with low classification uncertainty would have nearly all probability concentrated on a single category, while an ambiguous experiment would have the probabilities spread out between many limitation classes (Andersen and others 2007).
Creating a Univariate Limitation Indicator
Hyperbolic Tangent Regressions
A variety of physical parameters and nutrient fractions was originally analyzed from the initial water samples, covering a normal monitoring program suite of measurements, but also augmented with organic nutrient fractions (dissolved and particulate). Preliminary data analysis indicated little or no relationship of nutrient limitation with physical parameters and dissolved organic nutrients. These factors were therefore not considered for the development of indicators.
Potential Limitation Indicators
three ‘standard’ N:P ratios between matching nutrient fractions: dissolved inorganic (DIN:DIP); total (TN:TP); and particulate organic fractions (PON:POP);
two ‘composite’ N:P ratios: DIN:TP ratio after Morris and Lewis (1988); and the ratio of bioavailable nutrients (BAN:BAP; Reynolds and Davis 2001), representing the ratio between the sums of biologically available N and P ((DIN + PON):(DIP + POP));
two ‘nutrient balance ratios’ (Tamminen 1982), where the supply ratio of dissolved inorganic N and P (DIN:DIP) is compared to the demand ratio of either total (TN:TP), or particulate organic nutrients (PON:POP); TNB = (DIN:DIP):(TN:TP); and PNB = (DIN:DIP):(PON:POP).
The two last-mentioned indicators (TNB and PNB) are expected to have a critical ratio around unity (that is, the N:P ratio of supplies matches the demand), while the other predictor candidates would be expected to have critical levels closer to the Redfield ratio (N:P = 16, by atoms). All predictors were analyzed in their one- and two-dimensional form (see equations (1) and (2)).
Goodness of predictors
Relative performance of the limitation predictors was compared by regression statistics of the 2 models (equations (1) and (2)) for each predictor. The criteria used were the Akaike Information Criterion (AIC; Johnson and Omland 2004), which depends on both the goodness of fit and the complexity of the model, and coefficient of determination (R2) describing the fraction of variance explained by the model. In addition to this, we used Receiver Operating Characteristics (ROC) plots for visualizing the performance of the limitation classifiers (Fawcett 2006). These plots, commonly used in medical decision making but recently also in machine learning and data mining research, compare the match between classifier predictions and known classes of a data set, after composing two-by-two confusion matrices (contingency tables; see Table 2 in Supplementary material) containing perfect matches (true positive or negative) and false classifications (false positive or negative). The graph plots true positive rate (or hit rate) against false positive rate (or false alarm rate) of the classifiers against each other, thus depicting relative tradeoffs between benefits (true positives) and costs (false positives).
Threshold N:P Ratios
The univariate limitation indicator created from the seven generic limitation patterns of Andersen and others (2007) preserved well the information content of the original limitation classes (Figure 1), in spite of the information lost by compression into one dimension. Classifications based on dividing the range of the univariate limitation index into three equal segments recovered the original limitation classes in 82% (combined limitation), 98% (N), or 100% (P) of the cases (Figure 1). These numbers correspond to the true positive rates (Fawcett 2006) of classifiers based on the univariate limitation index, which can also be taken as an upper performance limit for alternative indicators based on nutrient concentrations at the start of the experiment.
−9.0 ± 1.4
−2.3 ± 0.3
−3.0 ± 0.9
−0.9 ± 0.1
−7.6 ± 1.1
0.27 ± 0.10
−0.34 ± 0.08
2.3 ± 0.4
0.7 ± 0.1
1.0 ± 0.3
0.8 ± 0.1
2.4 ± 0.4
0.69 ± 0.11
0.66 ± 0.10
N → P
44 → 59
19 → 53
15 → 31
2.0 → 5.1
21 → 27
0.4 → 1.1
1.0 → 2.8
−10.3 ± 2.2
−1.7 ± 0.3
−3.2 ± 0.9
−1.3 ± 0.2
−7.3 ± 1.1
−6.9 ± 1.1
−3.9 ± 0.9
2.7 ± 0.6
0.7 ± 0.1
0.6 ± 0.3
0.7 ± 0.1
2.2 ± 0.4
0.6 ± 0.1
0.6 ± 0.1
−2.4 ± 0.4
−0.5 ± 0.1
−1.6 ± 0.4
−1.3 ± 0.2
−2.5 ± 0.4
1.3 ± 0.3
0.6 ± 0.3
−8.0 ± 1.4
−1.4 ± 0.3
−1.7 ± 0.9
−0.25 ± 0.08
−4.4 ± 0.8
0.46 ± 0.11
0.07 ± 0.07
2.1 ± 0.4
0.5 ± 0.1
0.6 ± 0.3
0.50 ± 0.09
1.5 ± 0.3
0.44 ± 0.08
0.46 ± 0.08
N → P
37 → 52
8 → 34
9 → 26
0.8 → 3.3
16 → 25
0.16 → 0.77
0.41 → 1.83
−10.6 ± 2.2
−1.3 ± 0.4
−1.8 ± 0.9
−0.53 ± 0.15
−4.5 ± 0.8
−6.1 ± 1.2
−2.6 ± 0.9
2.9 ± 0.7
0.52 ± 0.10
0.47 ± 0.30
0.41 ± 0.09
1.4 ± 0.3
0.4 ± 0.1
0.48 ± 0.08
−2.2 ± 0.4
−0.44 ± 0.12
−0.95 ± 0.33
−0.90 ± 0.21
−1.8 ± 0.3
1.3 ± 0.3
0.43 ± 0.29
Standard N:P Indicators (TN:TP, DIN:DIP, PON:POP)
The traditional applications of the Redfield ratio performed very differently from each other. All TN:TP data, including the P-limited experiments, significantly exceeded the Redfield ratio of 16, reaching values up to 100, whereas PON:POP was more constrained, from 10 to 40 (Figure 2A, C). This clearly points out a large excess of dissolved organic N that is unavailable for the phytoplankton (Supplementary material).
DIN:DIP demonstrated the widest range of values, covering more than two orders of magnitude, with shifts from P to combined to N-limitation far above the Redfield ratio (19 and 53, respectively; Table 1; Figure 2B). The predictive power of DIN:DIP was clearly the best of standard ratios, and it was only slightly enhanced by the 2D model (Table 1). The 2D model showed, however, that the regression departed from Redfield slope, indicating concentration-dependency towards low inorganic nutrient concentrations (Figure 3B).
Composite N:P Indicators (DIN:TP, BAN:BAP)
The composite indicators performed the best according to regression statistics, with DIN:TP scoring the highest coefficient of determination of all indicators with the 2D model (R2 = 0.64), and only slightly less with the 1D model (Table 1). BAN:BAP followed closely, with almost identical scores for 1D and 2D models. The range for limitation shifts in DIN:TP was from 2 to 5 (Table 1; Figure 2D), significantly below the Redfield N:P ratio, whereas the biologically available fractions (BAN:BAP) indicated limitation shifts above 16 (21 and 27; Table 1; Figure 2E). The 2D models showed a slight displacement of BAN:BAP slope compared to Redfield, whereas the DIN:TP slope deviated markedly and exhibited clear concentration-dependency (Figure 3D, E).
Nutrient Balance Ratios (TNB, PNB)
Apart from PON:POP, the nutrient balance ratios benefited the most from 2D models compared to corresponding 1D ones (Table 1). The shifts between limitation categories in 1D models took place near unity (Table 1; Figure 2F, G), but corresponding 2D models showed that enhancing the predictive capacity of the ratios required clear departure from unity, especially for TNB (Figure 3F, G). The 2D model for this ratio scored very close to the best chlorophyll-based model (DIN:TP) according to regression statistics (R2 = 0.62; Table 1), and was clearly the best of all for 14C-based models (Table 1).
Figure 4 demonstrates the benefit of 2D models for the predictive capacity of especially nutrient balance ratios and PON:POP, but the latter remained anyhow a very modest predictor for N and P limitation, and showed 50:50 true and false positive rates for combined limitation. TN:TP ratio was the least reliable predictor after PON:POP for all limitation categories. DIN:TP and TNB scored the highest true positive and similar false positive rates for both N and P limitation, followed closely by DIN:DIP and BAN:BAP. The same overall ranking applied to prediction of combined limitation, except for lowered true positive rate of DIN:TP, although the modest true positive rates for combined limitation predictions were more widely scattered than for the single limitation categories.
Threshold N:P Ratios
The DIN:TP indicator thresholds were far below the others, and also significantly below the Redfield ratio, but not significantly different from those estimated from earlier studies (Morris and Lewis 1988), at least not when using the chlorophyll a response based predictor. PON:POP had thresholds closest to the Redfield ratio, although the low predictive power of this indicator is also reflected by the width of the confidence limits. The other indicators shown in Figure 5 generally had thresholds on the upper side of the Redfield ratio, and are more in line with threshold N:P supply ratios from continuous culture experiments (Terry and others 1985), with most of the threshold ratios for the transitions to pure P limitation being significant higher than Redfield. Figure 5 also shows a strikingly consistent tendency for threshold N:P ratios based on data using chlorophyll a response parameter to be higher than corresponding values based on 14C uptake as response parameter.
Ecological Interpretation and Predictive Power of Indicators
Different nutrient fractions represent either nutrient supplies for planktonic organisms, cellular composition of the organisms, or combinations of both. The original concept of Redfield (1934, 1958) was built on large-scale stoichiometric convergence of phytoplankton biomass and their dissolved nutrient supply, through homeostatic regulation of the Ocean via phytoplankton metabolism. At global and evolutionary scales, comparisons of nutrient ratios of the ‘supply side’ and ‘biomass side’ should therefore yield information on transitory imbalances, and thus on nutrient limitation experienced by plankton.
It is less than obvious whether this concept is applicable at the decadal time scales of significant changes in anthropogenic nutrient supply to spatially confined or temporally dynamic water bodies, be it lakes or coastal areas, despite the extensive application of the Redfield ratio within ecology and management. However, in spite of repeated requests for reliable nutrient limitation indicators (for example, Howarth and Marino 2006), we know only about one study which has addressed the problem in a similar heuristic and systematic manner as done here. In a study performed in Colorado mountain lakes, Morris and Lewis (1988) compared a partly similar set of limitation indicators and came up with a closely matching ranking among them.
Although nutrient limitation has traditionally referred to autotrophic plankton, it has become increasingly evident that stoichiometric interactions within natural planktonic food webs, composed of autotrophic, mixotrophic and heterotrophic multi-species compartments, directly influence all nutrient fractions. Nutrient fractions are further affected by detrital compartments of varying biological availability. Depending on the choice of nutrient fractions for limitation assessments, the ecological interpretation of indicators will thus vary, and the same could be expected for the abilities of the indicators to predict in situ nutrient limitation of ambient phytoplankton.
Our ‘standard’ N:P ratios represent a supply ratio (DIN:DIP), a biomass proxy ratio (PON:POP), and total nutrient pools (TN:TP). There were large differences among these indicators, both in their ability to predict the limitation pattern (Figures 2, 3, and 4, Table 1), and in their numeric thresholds for limitation shifts (Table 1; Figure 5).
The worst performing indicators were TN:TP and PON:POP, strongly indicating that the pools of non-autotrophic and/or biologically unavailable nutrient fractions can effectively mask the nutrient status of autotrophs. The wide divergence between the thresholds for TN:TP (very high) and the PON:POP (close to Redfield) ratios reflects the existence of a large pool of dissolved nitrogen unavailable for primary production. This is in line with the presence of a considerable pool of dissolved organic nitrogen in the study area (Supplementary material). Only a minor share (10–20%) of this DON pool is degradable by bacterioplankton over a period of a week (Lignell and others 2008). Thus, ratios of total nitrogen and phosphorus are clearly misleading when it comes to predicting the in situ nutrient limitation of autotrophs. This is obviously aggravated in the Baltic Sea and other coastal systems strongly affected by their catchment. In spite of overall high TN:TP ratios (atomic TN:TP ratio 52 ± 19.2, mean ± 1 SD), phytoplankton communities exhibited N and P limitation at similar frequencies (Tamminen and Andersen 2007).
The supply side ‘standard’ indicator, DIN:DIP, performed generally well, but it yielded limitation information departing from the traditional usages of Redfield ratio in two respects: the thresholds for changes between N, N + P, and P limitation exceeded clearly Redfield N:P (Table 1), and the minor but significant concentration-dependency (thresholds decreasing with increasing amounts of dissolved nutrients) indicates that the requirement for DIP increases over-proportionally with increasing dissolved nutrients. However, the concentration dependency in Figure 3B should not be mistaken as eutrophication gradient. In fact, the most eutrophicated sites included in this study were characterized by overall low concentrations of dissolved inorganic nutrients and exhibited N-limitation (Tamminen and Andersen 2007).
With the exception of the DIN:TP ratio, the performance of the more elaborate ‘composite’ and ‘balance’ ratios did not appear to substantiate their potential theoretical benefits. It remains open whether the slim gains of increased complexity are due to cumulative measurement uncertainties of several nutrient fractions, or whether their underlying assumptions on biological availability, or on balance between supply and demand, are not sufficiently realistic.
Only the balance type indicators (TNB and PNB) seem to have substantial performance gains when going from 1D to 2D models, as judged by the lengths of the corresponding tails in Figure 4. Assuming that organisms with high N:P biomass ratios require corresponding high N:P supply (and vice versa), we expected these ratios to follow unity. This assumption was clearly falsified by co-limitation showing a negative relationship between dissolved and total (or particulate) fractions (Figure 4B, D): high TN:TP or PON:POP ratios generally correspond to P limitation which is made more severe under conditions of simultaneously high DIN:DIP ratios, and vice versa.
The best performing indicators, DIN:DIP, DIN:TP, and BAN:BAP, show rather little performance gain from the more complex 2D models, suggesting that all of these can successfully be used for deriving concentration-independent (1D) threshold ratios for N vs. P limitation.
Predicting N Limitation vs. Predicting P Limitation
The threshold ratios for DIN:DIP and BAN:BAP are relatively near the Redfield ratio for the transition from N-limitation to combined limitation, while the transitions to pure P-limitation are in all cases significantly above Redfield (Figure 5). The ranges spanned by these two indicators fit reasonably well with observed ranges of critical N:P supply ratios in phytoplankton cultures (for example, Terry and others 1985; Leonardos and Geider 2004). Although threshold N:P supply ratios are known to differ among species and also to be strongly influenced by growth conditions (Leonardos and Geider 2004), it seems reasonable to interpret both the DIN:DIP and BAN:BAP concentration ratios as proxies for the actual N:P supply ratios experienced by the initial plankton communities in our experiments.
On the other hand, DIN:TP, which was the overall best performing indicator both in our study (Table 1) and in Morris and Lewis (1988), gave threshold ratios almost an order of magnitude lower than DIN:DIP (Figure 5). Since it seems impossible for DIN:TP and DIN:DIP to both reflect the N:P supply ratio at the same time, the key to the relative success of DIN:TP must be that it measures relative N:P availability on a time scale more relevant to phytoplankton growth.
Morris and Lewis (1988) argued that DIN is the best predictor for available nitrogen because luxury uptake of N is negligible, while high capacity for luxury P uptake and fast turnover of dissolved P makes TP a better predictor of available phosphorus. Total P pool also includes organic P, which is known to become available for phytoplankton through induction of alkaline phosphatase activity at times of low inorganic P availability (Tanaka and others 2006). The fact that Morris and Lewis (1988) found critical DIN:TP ratios in the same range as our study (2–8 mol:mol), despite study objects as different as Colorado mountain lakes and Baltic Sea coastal areas, suggests that this indicator might have validity across considerable ranges of salinity and eutrophication.
Our results support the meta-analysis of Elser and others (2007) showing that combined N and P limitation is more common than previously thought. At the same time, our models have lower success rate in predicting combined limitation than the two other categories. This difficulty may be related both to the heterogeneous nature of combined limitation, and also to technical issues with the one-dimensional limitation indicator we have used in this analysis.
Our combined limitation class is the result of pooling the primary and exclusive combined limitation classes identified by Tamminen and Andersen (2007), which are probably more conceptually different than their counterparts for N or P limitation. The first would correspond to what Arrigo (2005) calls community co-limitation, where different populations in the community are limited by different nutrients, while the second is probably more a case of biochemical co-limitation (Arrigo 2005), where a single dominant population is limited by both nutrients simultaneously.
Moreover, the inherent information loss in compressing the original three-dimensional limitation probability vector into a one-dimensional limitation index is probably highest in the central region of the index. Consider for example the single red dot close to the center of Figure 1, which was an experiment with such weak and noisy responses that small changes in the input data gave significant probabilities for all 3 limitation classes, but with the N limitation probability slightly higher than the others. The higher false positive rate for N limitation than for P limitation (Figure 4) is mainly caused by the inability to separate N limitation from combined limitation. This is perhaps best illustrated by the 2D models (for example, DIN:TP; Figure 3D), where the blue P limitation dots clearly separate out while the red N limitation dots remain intermingled with yellow combined limitation dots.
Seston vs. Phytoplankton Ratios: Constraining Mechanisms in Natural Assemblages
The poor ability of the particulate N:P ratio (PON:POP) to predict nutrient limitation is reflected in the relative constancy of seston composition, despite wide variability in dissolved and total nutrient fractions. Experimental studies on the relationship between N:P supply ratio and cell composition are limited and partly conflicting: Rhee (1978) found that cell N:P of Scenedesmus cultures closely matched the N:P of the supply, while Goldman and others (1979) found cell N:P in Dunaliella cultures to converge to the Redfield ratio over a range of N:P supply ratios.
Klausmeier and others (2004) used a mathematical model to show that these contrasting results may be reconciled by considering differences in growth conditions: constant cell N:P may be sustained over a range of N:P supply at high growth rate, as in Goldman and others (1979), while it will to a larger extent reflect the supply N:P at low growth rate, as in Rhee (1978). Nutrient depleted cells have higher internal N:P ratios than nutrient replete cells, the latter requiring relatively more P to N to maintain fast cellular growth (Geider and LaRoche 2002). The analysis underlying the growth responses in the current study is sensitive to relative stimulation of growth. Even relatively replete cells may still respond to addition of N or P if other factors support higher growth. In accordance to this, the threshold DIN:DIP ratio decreases with increasing amount of nutrients (Figure 3B).
The results indicate that the critical N:P supply ratio for stimulating phytoplankton growth is not constant, but decreases with increasing growth rate, reflecting systematic changes in cellular composition between nutrient deplete and replete cells. Klausmeier and others (2004) conclude that our understanding of the physiological regulation of N and P uptake is limited, and that the current generation of Liebig-type models of co-limitation is probably too simplistic.
Our findings match those of Hall and others (2005), who demonstrated low seston N:P variability on widely variable N:P supply ratios in both natural and artificial freshwater systems (ponds and mesocosms), and also supported their findings by a survey of literature data from an even wider range of systems (lentic and lotic; marine, freshwater, and terrestrial).
It should be kept in mind that seston N:P will in any case be a blunted signal for the cellular composition of the phytoplankton, since the material captured on a filter will be a complex mixture of autotrophic, heterotrophic, and detrital constituents. Thus, low variability of seston N:P need not be in conflict with variable phytoplankton stoichiometry, if the phytoplankton of the initial community constitutes a minor component partly masked by nutrient-poor detritus and more homeostatic heterotrophs like metazoan grazers.
Our analysis shows that standard monitoring parameters like DIN, DIP, and TP may be used to predict in situ phytoplankton P limitation with high confidence and high power (80% true positive rate, 5% false positive rate), while the discrimination between combined (N + P) limitation and single limitation by N is more prone to false positives. From the management point of view, it is important to be aware that prevailing N-limitation will be more difficult to detect from nutrient data than prevailing P-limitation.
DIN:TP performed the best in predicting prevailing limitation, and the 1D model yielded numeric thresholds between limitation categories. There are also other aspects supporting its use in inferring nutrient limitation from typical monitoring data. While DIN:DIP and BAN:BAP showed relatively similar abilities, many existing data sets do not include particulate nutrients (PON and POP), which makes the calculation of BAN:BAP impossible. As DIP measurements are expected to have higher measurement noise than TP, especially for DIP concentrations close to analytical detection limits, one would also expect DIN:DIP to be a more noisy indicator than DIN:TP.
Besides the apparent heuristic value of our results, some more general findings are intriguing but cannot be given a satisfactory explanation by the current analysis. The novel observation that all indicators showed lower threshold N:P ratios when using photosynthetic 14C-uptake as response parameter, than when using chlorophyll a (Figure 5), is too obvious and consistent to be overlooked. While our experiments were not designed to discuss this phenomenon in detail, we want to point out that chlorophyll a is a more integrative indicator than a short-term rate measurement such as 14C fixation, which is more affected by light availability, temperature and physiological state of the phytoplankton.
The widespread and strong positive synergistic effects of N and P enrichment (Elser and others 2007) have obvious consequences for management of nutrient discharges (Conley and others 2009; Paerl 2009). N and P play unequal roles in phytoplankton nutrient uptake and growth. Our results clearly indicate that standard ‘Redfield conversions’ between major nutrients have limited applicability in phytoplankton ecology. More adequate descriptions of multiple limitation are needed also for planktonic food web studies, as well as for modeling eutrophication dynamics in coastal systems.
The data originate from a Finnish project PELAG III (for full acknowledgments, see Tamminen and Andersen 2007). Aspects of the in-depth data analysis have been funded by the EU 5th Framework Project DANLIM (EVK3-CT-2001-00049, coordinator Risto Lignell) and the 6th Framework Project THRESHOLDS (GLOBAL/IP/02/0257, coordinator Carlos Duarte). Comments by two anonymous reviewers are acknowledged.
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