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Brazilian Journal of Biology

Print version ISSN 1519-6984

Braz. J. Biol. vol.65 no.2 São Carlos May 2005

http://dx.doi.org/10.1590/S1519-69842005000200016 

The nutritional status of zooplankton in a tropical reservoir: effects of food quality and community structure

 

O status nutritivo do zooplâncton em um reservatório tropical: efeitos da qualidade e da estrutura da comunidade

 

 

Pinto-Coelho, R. M.I; Giani, A.II; Morais-Jr., C. A.I; Carvalho-Jr., E. R.I; Bezerra-Neto, J. F.III

ILaboratório de Gestão de Reservatórios Tropicais, Departamento de Biologia Geral, Instituto de Ciências Biológicas, Universidade Federal de Minas Gerais, Belo Horizonte, Minas Gerais, Brazil
IILaboratório de Ficologia, Departamento de Botânica, Instituto de Ciências Biológicas, Universidade Federal de Minas Gerais, Belo Horizonte, Minas Gerais, Brazil
IIIPrograma de Pós-graduação em Ecologia, Conservação e Manejo da Vida Silvestre, Instituto de Ciências Biológicas, Universidade Federal de Minas Gerais, Belo Horizonte, Minas Gerais, Brazil

Correspondence to

 

 


ABSTRACT

The temporal variability of energetic reserves of zooplankton in the eutrophic Pampulha reservoir was investigated during two successive annual cycles. The effects of dominance of large filter-feeding cladocerans (Daphnia) and the occurrence of massive blooms of the cyanobacteria Microcystis on the energetic reserves of zooplankton were tested. This study showed that phytoplankton composition has a greater effect on energetic reserves of zooplankton. Some associations between lipid levels and the specific composition of zooplankton were also found. This study also demonstrated that the elementary composition of phosphorus in zooplankton can be used as an estimator of the nutritional status of zooplankton.

Key words: phosphorus, lipid, tropical zooplankton, nutritional status, reservoir.


RESUMO

A variabilidade temporal de reservas energéticas do zooplâncton no reservatório eutrófico da Pampulha foi investigada durante dois ciclos anuais sucessivos. Foram testados os efeitos da presença dos grandes cladóceros (Daphnia) e a ocorrência de florações maciças da cianobactéria Microcystis sobre as reservas energéticas do zooplâncton. Este estudo mostrou evidências de que a composição do fitoplâncton apresentou efeito intenso sobre as reservas energéticas do zooplâncton. Foram também encontradas associações entre o nível de lipídeos e a composição específica do zooplâncton. Demonstrou-se ainda que a composição elementar do fósforo no zooplâncton pode ser usada como indicador do status nutricional do zooplâncton.

Palavras-chave: fósforo, lipídeo, zooplâncton tropical, status nutricional, reservatório.


 

 

INTRODUCTION

Two of the most striking differences between tropical and temperate freshwater zooplankton are the smaller size of zooplankton and the relative scarcity of large filter-feeding Daphnia speciesin the tropics (Fernando et al., 1987). The most common hypotheses explaining these differences include the higher fish predation rates in the tropics (Northcote et al., 1990; Starling & Rocha, 1990), the lower food quality or the toxicity of cyanobacteria commonly dominant in tropical waters (Porter & Orcutt, 1980; Lampert, 1981), and the energetic constraints of living in warmer waters (Geller, 1986). Some factors associated with biogeography have also been mentioned (Matsumura-Tundisi, 1984).

The higher metabolic rates of zooplankton from the warmer tropical regions limit their energetic storage patterns. The allocation of energetic reserves can be assessed by measuring the total lipids since these compounds make up the bulk of energy reserves of zooplankton (Goulden & Henry, 1984). The most important groups of crustacean zooplankton are known to accumulate significant amounts of lipids, mostly in the form of tryacylglicerols (Farkas, 1970). Nonetheless, the lipid content of zooplankton can suffer extensive temporal variations (Vanderploeg et al., 1992). Indeed, some recent investigations have demonstrated that tropical freshwater zooplankton usually has lower lipid levels. Additionally, conspicuous diel variations in these energetic reserves have also been observed (Pinto-Coelho et al., 1997a, b; Santeiro & Pinto-Coelho, 2000).

Phosphorus is frequently a limiting resource in freshwater systems (Schindler, 1977), particularly for freshwater zooplankton (Hessen, 1992; Brett et al., 2000). Some empiric relationships between total phosphorus availability and zooplankton biomass have been found (Hanson & Peters, 1984). Furthermore, some cladocerans, specially the daphnids, are known to accumulate higher amounts of phosphorus (Hessen, 1990). In the last two decades, experimental and empirical evidence supporting the theory of elemental homeostasis (C, N, and P) in zooplankton have been published (Sterner et al., 1992). This theory is mostly based on the fact that the variation of elemental composition (C, N, and P) found in zooplankton biomass is lower than the variation observed in phytoplankton or seston particles (Hochstädter, 2000). This pattern indicates the possible existence of homeostasis in the elemental composition of zooplankton. Despite all the accumulated evidence, one possible drawback of a stoichiometric approach is that it ignores the biochemical characteristics of both substrate and consumers (Tang & Dam, 1996), which renders the role of element composition as an indicator of nutritional status of zooplankton still unclear. Therefore, the search must go on for possible relationships between elemental composition of potential limiting elements and nutritional status of zooplankton.

The present study focused on a small tropical reservoir, the Pampulha reservoir in Brazil, that for the past decade has suffered increasing trophy. The main objective was to evaluate the modifications in community structure of zooplankton that was observed during two successive seasons. These modifications were induced by increase in trophy grade of the system and predation by planktivores. The study period initially covered a season during which zooplankton was dominated by large-bodied Daphnia pulses. In the second phase, the system was dominated by small cyclopoids as a response to increased predation pressure by fish. In both periods, extensive blooms of the cyanobacteria Microcystis were recorded. These circumstances allowed testing two hypotheses that could explain why tropical zooplankton tends to have a lower nutritional status. First, the possible effect of cyanobacteria on food quality and energy reserves of zooplankton was investigated. Furthermore, we looked for some empirical relationship between the dominance of Daphnia in the zooplankton and the lipid level of total zooplankton. The suitability of elementary composition of phosphorus for estimating the nutritional status of zooplankton was also investigated.

 

MATERIAL AND METHODS

Study area

Pampulha reservoir, with a 11 x 106 m3 volume and surface area of 2.1 km2, is located in the northern part of Belo Horizonte, the capital of Minas Gerais State. The reservoir was built in 1938 for supplying water, but in the early eighties the use of the reservoir for drinking water was interrupted due to the incidence of cyanobacteria blooms in the lake. Since then, the reservoir has exhibited several signs of eutrophication, including outbreaks of the macrophyte Eichhornia crassipes (1992-1995) and successive blooms of Microcystis aeruginosa (1980, 1988-1990, 1995-1997). In recent years, a sharp increase in the population of an exotic fish, the African cichlid tilapia (Oreochromis niloticus), also occurred in the reservoir (1997-1998).

Sampling and laboratory procedures

Algae, zooplankton, and samples for chemical analysis were collected at a central station (z = 8 m) in the reservoir in a location used for regular monitoring for more than 15 years. Samplings were done monthly between 1993 and 1995, and every two weeks from 1996 to 1998. Phytoplankton and samples for chemical analysis were collected with a Van Dorn bottle at the following depths: 0 m, 0.5 m, 1.0 m, 2.0 m, 4.0, 6.0 m, and 0.5 m from the bottom. Zooplankton was collected using a 5.1 L Schindler-Patalas trap equipped with a 90 µm mesh net. Different depths covering the water column were considered: 0, 2, 4, and 6 m, but in this paper only zooplankton data from 2.0 m were used. Water transparency and conductivity were measured in situ by means of a Secchi disk 35 cm in diameter and a Yellow Springs device, respectively.

Water samples for chemical analysis were deep frozen (—25ºC). The determination of inorganic nitrogen (ammonium) was done according to Mackereth et al. (1978). Total phosphorus was determined according to Murphy & Riley (1962). Chlorophyll-a was determined using the conventional technique proposed by Lorenzen (1967); POC was estimated using a procedure described in Torres et al. (1998).

Phytoplankton samples fixed with lugol acetic were routinely enumerated using the Utermöhl (1958) technique. Species identification was carried out following the descriptions provided by Eterovick & Giani (1997). At least 400 individuals of the dominant species were counted in each sample. The biovolume was estimated using the equations from Root (1981).

Zooplankton was fixed using a buffered formalin solution saturated with sucrose. A minimum of 700 individuals were enumerated and measured in each sample. A M3C-Leica dissecting stereomicroscope was used. In the early period (1993-1996), all individuals were measured by means of a calibrated eyepiece. Biomass estimation was done using allometric equations relating length to dry weight as derived by McCauley et al. (1989) and Masundire (1994).

Another 250 ml zooplankton sample was taken for chemical and biochemical analysis. The sample was placed in a thermos box filled with ice, and within 30 minutes transported to the laboratory. There the organisms were filtered on 160 mm inox gauze that was carefully transferred to a 10 cm Nalgene petri dish, wrapped in aluminum foil, N2 saturated, and placed in a dissecator air-tightened with silica gel. The dissecator was stored in a conventional freezer (—25ºC). Next day, the frozen samples were placed in an Edwards L5KR lyophilizer for 24 hs. After freeze—drying, the zooplankton samples were stored again, using the same procedure until the date of chemical analysis.

P-content of zooplankton

A 3.00 mg (weighed using a high precision Mettler balance) aliquot of freeze-dried zooplankton was placed in 50 ml glass tube, following which 0.1 ml of distilled water was added to each tube. The sample was mechanically grounded. The homogenate was then transferred to 125 ml Pyrex flasks for chemical digestion with potassium persulfate. The samples were allowed to evaporate until about 0.5-1.0 ml remained. The extract was ressuspended to exactly 50 ml using distilled water, and the phosphorus content was colorimetrically determined using the molybdate-ascorbic acid solution prepared according to Murphy & Riley (1962). A Shimadzu UV-VIS spectrophometer equipped with 5.0 cm quartz cuvettes was used.

Analysis of lipids

Total lipids were measured using a colorimetric method (Zollner & Kisrch, 1962) modified by Meyer & Walther (1988). A 0.50 to 2.00 mg aliquot of freeze-dried zooplankton was mechanically grounded after adding 0.1 ml of distilled water. After chemical digestion (with NaOH, 80ºC, 2 hs), 1.0 ml of a solution of fosforic acid and vaniline was added for color development. After exactly 30 minutes, sample absorbance was measured on a Shimadzu UV-VIS spectrophotomer (l = 546 nm) using a 1.0 cm glass cuvette. The standard solution was made of cholesterol (SIGMA, 99.99%).

 

RESULTS

During the past decade, Pampulha reservoir has suffered a steady increase in eutrophication, as shown by the long-term evolution of water transparency, electric conductivity, total phosphorus, and ammonium (Fig. 1). The Secchi disk readings showed a clear decrease in the 1995-1998 period with annual means of 83, 78, 47, and 46 cm, respectively. Conductivity and nutrients showed a evident seasonal pattern with higher values during the dry season, especially during the months of August, September, and October. Despite this seasonal pattern, there were clear increases in the annual maxima of all these variables during the study period. The annual maxima conductivity for the 1994-1998 periods were, respectively, 322, 340, 370, 378, and 401 mS.cm—1. Similar patterns were also found for inorganic nitrogen (ammonium) and total phosphorus. The annual maxima of total phosphorus (bottom values — 6 m) for the 1993-1998 periods were, respectively, 47, 77, 158, 166, 205, and 269 µg P-PO4.L—1 (Fig. 1).

During 1996 and 1997, an intensive survey of phytoplankton and zooplankton (sampling every two weeks) was performed. The data from this period are represented in Fig. 2. In 1996, the phytoplankton community was dominated by small chlorococcales (Oocystis lacustris, Scenedesmus acus, and Tetraedron minimum). In 1997, with the disappearance of Daphnia from the lake, the small phytophlagellates like the cryptophyceae Cryptomonas erosa, C. brasiliensis, and Rhodomonas sp. were also initially abundant. With the onset of more stable climatic conditions during the dry season (higher daily radiation and less windy), the structure of phytoplankton changed with the appearance of several pulses of cyanobacteria that bloomed in the lake, mostly between May and early December (Fig. 2A). The following species were regularly found: Microcystis aeruginosa, M. viridis, and M. flos-aquae.

In this two-year period, the reservoir's zooplankton community changed noticeably, and in 1996 it was dominated by the cladoceran Daphnia laevis, of which in that year there were at least three populational pulses (Fig. 2B). In 1997, this cladoceran disappeared from the lake and the small cyclopoid Thermocyclops decipiens became dominant, with numerous peaks in May, July, September, October, and December. Secondary pulses of the cladoceran Diaphanosoma birgei and Moina micrura were also observed in 1997 (Fig. 2B).

We routinely measured the nutritional status of zooplankton community during 1996 and 1997 (Fig. 3). The nutritional condition of zooplankton was evaluated using two approaches: the content of total lipids of zooplankton, and the elementary content of phosphorus. The lipid content of total zooplankton ranged between 4.12% and 32.12% of dry weight, with an average of 8.55 ± 4.35% of dry weight for the 1996-1997 period (Fig. 3B: pooled 1996-1997 data). The elementary composition of phosphorus was also monitored biweekly (Fig. 3C). The P-content ranged between 0.39% and 2.35% P-DW, with an average of 1.28 ± 0.44% P-DW (C:P molar = 113.4) for the pooled data (1996-1997). Figure 3 also demonstrates that both variables tended to show lower values during the periods of cyanobacteria blooms in the reservoir (vertical dashed lines).

The study found a significant linear correlation between the elementary content of phosphorus and the total lipid level in zooplankton community biomass. The linear regression between these two variables was significant (F = 12.77, p < 0.001, df = 36). This suggests that the phosphorus content can also be regarded as a good estimator of zooplankton food reserves in Pampulha reservoir (Fig. 4).

 

 

We regrouped the measurements of lipids and P-content according to specific years and conditions in the lake, after which the effects of Daphnia dominance and cyanobacteria blooms on the nutritional status of zooplankton as expressed by lipids and P-content were examined (Table 1). The annual average of lipid content of total zooplankton was higher in the first year with averages of 9.11% and 7.96% DW for 1996 and 1997, respectively. The total phosphorus content was also higher in 1996, with an annual average of 1.41% and 1.13% DW for 1997. Since there was a strong dominance of daphnids in 1996, these findings suggest that these organisms possibly have some impact on the overall nutritional condition of the zooplankton community.

 

 

There was a non-significant decrease of lipids in periods when D. laevis was absent from the zooplankton. The total lipids were 7.83 ± SD 1.93% DW for periods without Daphnia and 8.02 ± 2.02% DW, when Daphnia was present in the samples (F = 0.084, p < 0.774, n = 38) (Fig. 5). The dominance of this cladoceran in the zooplankton showed a stronger effect on the zooplankton P-content. This variable reached an average of 1.43 ± 0.42%. P-DW in the presence of this cladoceran, decreasing to 1.13 ± 0.39% P-DW in the absence of daphnids from the reservoir (F = 5.043, p < 0.031, n = 39) (Fig. 5).

The cyanobaceria Microcystis had a significant influence on both the total lipid and P-content of zooplankton. Zooplankton nutritional status as expressed by these two variables suffered significant reductions during algal blooms. Total lipids, for example, decreased from 8.41 ± 1.89% DW to 6.75 ± 1.36% DW (F = 5.704, p < 0.023, n = 36) in the presence of high densities of Microcystis (> 5.0 x 106 mm3.mm—3) (Fig. 5). The P-content also suffered a significant reduction during blooms, going from 1.35 ± 0.42% P-DW to 1.08 ± 0.26% P-DW (F = 4.998, p < 0.032, n = 35) (Fig. 5).

 

DISCUSSION

The modifications observed in zooplankton structure between 1996 and 1997 are possibly associated with increasing trophy fishing and fish predation. In 1996, during June, July, and September, respectively, at least three events of massive fish mortality occurred in the reservoir; in at least one of them, extensive death of zooplankton was also observed (Pinto-Coelho et al., 2003). These events are possibly associated with rapid climatic changes, the so-called cold fronts, characterized by abrupt changes in the air temperatures caused by the entrance of cold, oceanic air fronts from the subtropical areas of the Atlantic Ocean. These can last from 1 to 5 days, and often induce rapid circulation in water columns in shallow water bodies such as Pampulha reservoir. In highly eutrophic systems, column circulation often causes a sharp decrease or even total disappearance of dissolved oxygen from surface waters for short periods, usually during the night. In 1996, fish mortality in Pampulha occurred in periods of high cyanobacteria densities. Thus, the possible effects of cyanotoxins in these fish deaths cannot be ruled out. These species of cyanobacteria are known to produce toxins, known as microcystines (Ferrão-Filho et al., 2000). Stressful conditions may have contributed to maintain the fish populations at lower levels in 1996. In the following year, despite the occurrence of algal blooms, no major event of fish mortality was observed in the lake. The juvenile fish recruitment possibly allowed rapid recovery of fish standing stocks, which maintained high predation rates upon zooplankton during 1997 and the following years. Increased vertebrate predation possibly induced changes in the structure of this community, such as the disappearance of large Daphnia laevis from the lake.

Plankton community monitoring in Pampulha reservoir in the three subsequent years (1998-2000) demonstrated that the zooplankton community continued to be dominated by Thermocyclops, and that daphnids were absent throughout these years (Pinto-Coelho et al., 2001). An inventory of fish fauna (Godinho et al., 1992) showing 944 specimens in different regions of the reservoir demonstrated that tilapia (Oreochromis niloticus) were already the dominant organisms, with 82.4% of the total catch. Other species such as the piscivorous traíra (Hoplias lacerdae, H. malabaricus) and a small piranha, Serrasalmus were also common. However, after 1997 the population of this exotic African fish became largely dominant in the reservoir. In 1999, another inventory of the fish fauna was made. About 1200 specimens were collected, weighed, and identified. The local fish fauna was poor in species and strongly dominated by only one species of an African tilapia, Oreochromis niloticus, a common inhabitant of most Brazilian reservoirs (Álvares et al., 2000). The increase of the tilapia population in the reservoir may explain the disappearance of Daphnia and the increase of small cyclopoids in the lake.

The changes in the zooplankton community had no significant effect on the patterns of lipid accumulation. However, they were associated with the zooplankton P-content. Despite large variations in the total zooplankton biomass, no significant difference was found in the profile of lipid reserves in periods with and without Daphnia. In contrast, the amount of total lipids of zooplankton as well as the elementary composition of phosphorus experienced significant reductions during periods of cyanobacteria blooms.

Cyanobacteria are known as organisms of poor food quality with respect to zooplankton (Reinikainen et al., 1995) but tropical zooplankton, particularly daphnids, are often forced to ingest these items in their normal diet (Eskinazi-Sant'Anna et al., 2002). Several studies have shown a reduction in the growth and reproduction of Daphnia either due to the higher rate of food rejection in the presence of filamentous cyanobacteria or to its poor nutritional quality, or to the presence of cyanotoxins (Lampert, 1981; Gliwicz & Lampert, 1990). But it is known that zooplankton species differ considerably in their responses to toxic cyanobacteria (DeMott et al., 1991). Differences were also found between clones of the same species (Hietala et al., 1997), suggesting a genotype-dependent response. Furthermore, it is also possible that during cyanobacteria blooms, more resistant zooplankton species are selected.

Stoichiometry, a familiar approach in studies about zooplankton production, typically places food resources into three major elemental categories: carbon, nitrogen, and phosphorus (Tang & Dam, 1996). Several studies have concluded that freshwater zooplankton is usually P-limited (e.g. Hessen, 1992). For purposes of comparison, we did an approximate estimation of molar C:P ratios for the Pampulha zooplankton using a constant proportion of 49% (Berberovic, 1990) of carbon and varying P-values, as presented in Fig. 3. The annual averages were 112.6 and 153.3 for 1996 and 1997, respectively. The P-content of zooplankton found in this study and the estimated molar C:P ratios above confirmed that this community had lower phosphorus levels than most temperate zooplankton (Hessen, 1990; Hessen & Lyche, 1991). In the lake Constance (Germany), for example, the molar C:P ratios for zooplankton range usually between 45 and 65 (Hochstädter, 2000). Even considering the fact that these C:P ratios were not estimated at the species level, the higher values found in the present study can be seen as evidence of the limiting role of phosphorus for zooplankton in Pampulha reservoir.

One possible drawback of the stoichiometric approach is that it ignores biochemical constraints on both substrate and consumers. As Tang & Dam (1996) admit, there is a need for more empirical research in order to confirm the robustness of predictions arrived at through stoichiometric models. The present study found a significant relationship between total lipids of zooplankton and the elemental content of phosphorus in the biomass. Lipids and carbohydrate are the main energetic compounds of these animals (Farkas, 1970). The relationship between a limiting nutrient (P) and one of main energetic compounds of zooplankton suggests the key role exerted by phosphorus in the energetic metabolism of zooplankton. The stoichiometry theory predicts that the element in excess will be differentially regenerated in order to maintain rigid elemental ratios in the biomass.

The correspondence between P-content and total lipids is not always consistent. The dominance of daphnids had no significant effect on lipid reserves, but these organisms were clearly associated with higher phosphorus levels in the total zooplankton biomass. Hessen (1990) has already found that this genus has the highest phosphorus amounts in freshwater zooplankton. Furthermore, the highest values for total lipids of tropical zooplankton were found in a community dominated by Diaphanosoma and not Daphnia (Pinto-Coelho et al., 1997b). Therefore, the structure of a zooplankton community may have a strong influence on the relationship between energetic reserves and elemental composition, making predictions arrived at through a stoichiometric approach much more difficult. Additionally, recent experimental evidence shows that the P-content of zooplankton is linked with excretory metabolism, which is affected by short-term variations and food supply (Macedo & Pinto-Coelho, 2000).

This study confirms our previous findings suggesting that tropical zooplankton normally tend to have a lower profile of energetic reserves as measured by total lipids. The amount of total lipids in different tropical reservoirs is usually lower than 15% (Pinto-Coelho et al., 1997a). In most cases, a conspicuous diel cycle with higher values was found during the night (Pinto-Coelho et al., 1997a; Santeiro & Pinto-Coelho, 2000). These patterns are possibly a result of the higher energetic demand of organisms living in temperatures that are always higher than 18ºC. In optimal conditions of food supply, total lipids of tropical zooplankton can reach values as high as 25% DW, as was observed for short periods in a zooplankton community dominated by Diaphanosoma birgei in fertilized plankton ponds of hatchery stations (Pinto-Coelho et al., 1997b). Similar values were also obtained in laboratory cultures of Daphnia laevis or Moina micrura that fed at 20ºC on the green algae Ankistrodesmus gracilis (Macedo, 1999). These optimal conditions of food supply, however, are rarely found in the open waters of tropical lakes and reservoirs.

 

CONCLUSIONS

This study provided data on the effect of food quality in the energetic reserves and P-content of zooplankton in a tropical reservoir. The food quality effect on energetic reserves is present even considering extensive modifications in zooplankton structure. However, unlike total lipids, the P-content of zooplankton was also affected by the changes in the taxonomic structure of zooplankton, suggesting that community structure may have an important role in the internal cycling of a limiting element (phosphorus) in Pampulha reservoir. The study also showed a significant linear relation between the total lipid and the elemental composition of phosphorus in zooplankton.

Acknowledgements — We wish to thank the city of Belo Horizonte for supporting this research (grant 3998, FUNDEP/SMMA/PBH); the Fundação de Amparo à Pesquisa do Estado de Minas Gerais (FAPEMIG)g for a grant to Elildo R. Carvalho Jr., and the National Research Council (CNPq) for a research grant to Ricardo M. Pinto-Coelho. We also thank an anonymous referee for comments and suggestions on an earlier version of the manuscript.

 

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Correspondence to
Ricardo Motta Pinto-Coelho
Laboratório de Gestão de Reservatórios Tropicais
Departamento de Biologia Geral, ICB, UFMG, C.P. 486
CEP 31270-901, Belo Horizonte, Minas Gerais, Brazil
e-mail: rmpc@icb.ufmg.br

Received October 7, 2002 — Accepted February 3, 2004 — Distributed May 31, 2005