Ecology of deepwater rice-fields in Bangladesh 5. Mineral composition of the rice plant and other aquatic macrophytes

The mineral composition of deepwater rice (cultivar Kartik Sail) was studied during 1986 in a field near Sonargaon, Bangladesh, which is flooded by water from R. Meghna. Samples were taken four times, once prior to flooding and three times during the flood season. On two of the latter days (10 August = end of first flood peak, 23 September = second flood peak) the study was extended to other components of the ecosystem (sediments + soil, water, other aquatic macrophytes). On 23 September, 32% of the mass of the plant was out of water, 65% in water and 3% in sediment/soil. There were marked differences between elements in their pattern of accumulation by deepwater rice through the season. In comparison with the final totals for each element, about 48% of N, but only 11% of P and 10% of Na had been accumulated by the time the floodwater had arrived. The aquatic roots doubled in mass between the times of the two flood peaks and it is suggested that much of the P taken up by the plant may reach the plant via its aquatic roots after having becoming mobilized and released to the water when sediments become anaerobic. In comparison with other parts of the plant, Na was always much higher in the stem and Zn in the basal roots.Other aquatic macrophytes (weeds) increased from 0.40% of the mass (dry weight) of deepwater rice on 10 August to 4.0% on 23 September. However their content of each element (% dry weight) was considerably higher than that in deepwater rice, so they may at times compete effectively with the rice for nutrients. During the flood period (to 23 September) weeds accumulated 16% of the N accumulated by rice during the same period.     

Ecology of deepwater rice-fields in Bangladesh 1. Physical and chemical environment

This introduces a series of five papers describing physical, chemical and biological features of Bangladesh deepwater rice-fields. Flooding occurs typically from late June to early November. There were two distinct flood peaks (late July, mid-September) at the two main research sites during each of the years 1981–86, with maximum depths reaching about 1.5–2.0 m. Temperature showed a narrow range, with values for the upper part of the water column during July–October seldom outside the range 29–35 °C. Data for PAR (Photosynthetically Active Radiation) obtained with two types of sensor (4 and cosine) are summarized, with examples of profiles and changes throughout the day. Water chemistries sampled from 13 different locations at various times during 1981–1983 are compared for: conductivity, pH, total alkalinity, O₂, major metals (Na, K, Mg, Ca, Mn, Fe), minor metals (Co, Ni, Cu, Zn, Cd, Pb), NH₄-N, NO₂-N, NO₃-N, filtrable reactive P, filtrable organic P, non-filtrable P, Cl, SO₄-S, reactive-Si.Overall the concentrations of aqueous N and P may be regarded as providing a mesotrophic environment for algae, but with relatively low N : P. Filtrable organic P was at least as important as filtrable reactive P, with mean values at the various locations from 0.020 to 0.036 mg l^–1 P for the former and 0.005 to 0.038 mg l^–1 for the latter. Measurements of N and P in the water column at any one time typically gave values (expressed per unit area) slightly lower than totals for these elements deposited in sediments throughout the whole season. At least until the end of September, the upper part of the water column was almost always oxic during the daytime and occasionally supersaturated with O₂ in the afternoon. However DWR fields in south Bangladesh (Phaltita) visited on a sunny day in late September had waters which were almost entirely anoxic even in the afternoon: channels were lacking here and rotting rice stems from an earlier crop were widespread.     

Ecology of deepwater rice-fields in Bangladesh 6. Influence of environmental factors on seasonal changes in the rice plant

Measurements of the biomass of deepwater rice plants at sites on the three major floodplains in Bangladesh (Ganges, Jamuna, Meghna) with and without fertilizer treatment were made from shortly before the arrival of flood water (June) until it was receding (mid-October). There was usually an approximately linear increase in biomass per unit area with time until September, but subsequently there were marked differences in response, ranging from a continued steady increase to a sharp drop. Difference in the flood pattern were an important factor influencing changes in biomass and productivity.Net productivity (biomass change) measured at different stages in growth ranged from - 73 to + 220 kg ha^-1 d^-1 in unfertilized fields and from - 141 to + 430 kg ha^-1 d^-1 in fertilized fields, with mean values of + 130 in unfertilized and + 160 kg ha^-1 d^-1 in fertilized fields. However,grain yield reflected the increased biomass in only one of four experiments.     

Nitrogenase activity of blue-green algae on seasonally flooded soils in Bangladesh

Blue-green algal communities formed an extensive cover on soils at five deepwater rice-growing locations in Bangladesh during the month before the arrival of floodwater. The principal taxa wereAnabaena, Cylindrospermum, Lyngbya, Microcoleus, Nostoc, Prophyrosiphon notarisii, Scytonema mirabile andTolypothrix byssoidea. One of two locations studied after the floodwaters had receded also had an extensive cover, mainlyScytonema mirabile. Nitrogenase activity assayed at mid-day was from one to three orders of magnitude higher per unit area of community than bare soil. Nostoc showed higher activity than Tolypothrix, whether expressed per unit area or biomass. Whole field estimates of N₂ fixed by blue-green algal communities during the pre-flood period ranged from 1.0 to 10.2 kg N ha^–1. Much of this is probably not recycled until floodwaters cover the fields. However N₂ fixed after floodwaters have receded is probably recycled rapidly due to ploughing.     

Ecology of deepwater rice-fields in Bangladesh 3. Associated algae and macrophytes

1. Aquatic macrophytes formed dense beds in fallow areas during the four and a half months of the flood season in all but one deepwater rice-growing location in Bangladesh; these included several types of life-form, but the fine-leaved species, Myriophyllum sp., Najas indica, Utricularia stellaris were often especially abundant. The same species grew inside deepwater rice fields, but at much lower densities. A similar contrast occurred for the algae, although deepwater rice often developed dense masses of epiphytes on aquatic roots, stems and leaf sheaths, when plants were growing in isolated, well-illuminated situations.
2. Two widespread algae, Aulosira fertilissima and Scytonema mirabile, were equally successful on soil in the period prior to the arrival of floodwaters and floating on the surface of the water during the flood season. Other species common during the flood season differed from those common on soil.
3. Most blue-green algae inside deepwater rice fields were heterocystous; the only species not so, but forming distinct colonies, was Aphanothece stagnina. However only non-heterocystous forms were found at one location in south Bangladesh (Phaltita) and a change from heterocystous to non-heterocystous forms was noted at the main research site (near Sonargaon) during late September in at least one year. The water column at the former was almost entirely anoxic, while the change at the latter occurred at a time when the water sometimes became anoxic during the night. It is suggested that differences in ability to tolerate anoxic periods may be a key factor in determining the success of the algal and vascular plant species in the different micro-habitats within these DWR-growing areas.
4. Although diatoms were quantitatively only a minor component of the algal biomass, they became more frequent later in the season when the water became microaerobic or anoxic for part of the day. Navicula confervacea was overall the most abundant species at the two main research locations.

     

Studies on mixed mass cultivation of Anabaena spp. (nitrogen-fixing blue-green algae, cyanobacteria) on a large scale

Studies on mixed mass cultivation of Anabaena spp. on a large scale (5170m²) were conducted continuously for 3 years. Under the continental monsoon climate in northern subtropics (30°N, 115°E), 7–11 g dry weight m⁻² day⁻¹ of microalgal biomass on average was harvested in simple plastic greenhouses in the effective growth days during the warmer seasons. The maximum productivity was 22 g m⁻² day⁻¹ in the middle of summer. Observations on the productive properties of strains of Anabaena spp. indicated that they were different from and could compensate for each other in their productivities and adaptations to the seasonal changes. With different lining materials (PVC sheets, concrete, sand and soil) in the culture ponds, no significant variation of productivity was found, but bubbling with biogas in the middle of the day and the application of some growth regulating substances (2,4-D, NaHSO₃ and extracts of oyster mushroom spawn) was able to improve the production. The cost of microalgal biomass in this way was around 0·75–1·0 US dollar(s) per kilogram.     

4. Geographic distribution of freshwater blue-green algae

The analysis of the currently available data for morphologically unambiguously defined freshwater blue-green algae indicates that besides (sub-)cosmopolitan species, taxa with a more restricted distribution also exist. Many of these have a holarctic or pantropic distribution. It is hypothesized that, besides the distribution of ecological niches, temperature is one of the main controlling factors restricting species to particular latitudinal zones. Furthermore, the presence of species with a regional distribution (endemics) can not be ruled out, indicating that other factors must be considered. The possible role of dispersal capacities and of dispersal rates in relation to the earth history and to the speciation of blue-green algae is discussed.     

The effect of Daphnia on filament length of blue-green algae

Water from a hypertrophic lake rich in filamentous blue-green algae was passed through a continuous-flow system of aquaria containing Daphnia magna, and a control system without Daphnia. Daphnia caused a significant decrease in the blue-green algal density, and a two-fold reduction in filament length. It is suggested that feeding activity of Daphnia may result in an increase in the availability of blue-green filaments to filter-feeding cladocerans.     

Bioactive compound production by thermophilic and thermotolerant cyanobacteria (blue-green algae)

A thermotolerant species of Phormidium produced extracellular anti-microbial material during batch culture. Although this material was inactive when screened against a number of other cyanobacteria, it inhibited the growth of a wide range of Gram-positive and Gram-negative heterotrophic bacteria, Candida albicans and Cladosporium resinae.The authors are with the Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, UK     

Regulation of blue-green algal buoyancy and bloom formation by light,inorganic nitrogen,C02, and trophic level interactions

In highly eutrophic ponds, buoyancy of the gas-vacuolate blue-green alga Anabaenopsis Elenkinii (Miller) was regulated by complex interactions between chemical and physical parameters, as well as by biological interactions between various trophic levels. Algal buoyancy and surface bloom formation were enhanced markedly by decreased light intensity, and to a lesser extent by decreased CO₂ availability and increased availability of inorganic nitrogen. In the absence of dense populations of large-bodied Cladocera, early season blooms of diatoms and green algae reduced light availability in the ponds thus creating conditions favorable for increased buoyancy and bloom formation by A. Elenkinii. The appearance of blue-green algal blooms could be prevented by a reduced density of planktivorous fish, which allowed development of dense cladoceran populations. The cladocerans limited the growth of precursory blooms of diatoms and green algae, and given the resulting clear-water conditions, buoyancy of A. Elenkinii was reduced, and blue-green algal blooms never appeared.     

Consequences of iron deficiency on photosynthetic and respiratory electron transport in blue-green algae

Growth of Aphanocapsa in low iron media resulted in a decrease of the endogenous iron pool. Below a critical concentration photosynthetic electron transfer was specifically depressed. This was caused by a strong inhibition of the synthesis of cytochromes b-559 of PSII, cytochromes b-563, f-557, and the Rieske Fe-S center of the cytochrome complex and especially the Fe-S centers of PSI. The influence of iron limitation on respiration and chlorphyll formation was negligible.Paper presented at the FESPP meeting (Strasbourg, 1984)     

Nitrogen fixation inpara-nodules of wheat roots by introduced free-living diazotrophs

Nitrogen-fixation (C₂H₂-reduction) was demonstrated in wheat root nodules (p-nodules) induced by 2,4-dichlorophenoxyacetate (2,4-D) and inoculated withA. brasilense. By lowering the O₂ tension it was possible to distinguish the nitrogenase activity of bacteria located within thep-nodule of the wheat root system from that in the rhizosphere. Using cytological evidence, nitrogenase activity was attributed mainly to be coming from the bacteria within thep-nodule. It was also shown that the host plant was able to supply the necessary substrate required for the bacterial N₂-fixation (C₂H₂-reduction) within thep-nodules.     

Nitrogen fixation by hydrogen-utilizing bacteria

Seventeen strains of nitrogen-fixing bacteria, isolated from different habitats on hydrogen and carbon dioxide as well as on other substrates, morphologically resembled each other. All strains, including Mycobacterium flavum 301, grew autotrophically with hydrogen. The isolate strain 6 was sensitive to oxygen when dependent on N₂ as nitrogen source, a consequence of the sensitivity of its nitrogenase towards oxygen. At the same time, strain 6 was sensitive to hydrogen when growing autotrophically on N₂ as nitrogen source, but hydrogen did not affect acetylene reduction by these cells.Abbreviations MPN Most probable number - BS medium basal salts medium     

Nitrogen fixation by blue-green algal communities in the intertidal zone of the lagoon of Aldabra Atoll

Summary All eight types of blue-green algal community sampled from the intertidal sediments of the lagoon of Aldabra showed detectable rates of acetylene reduction, and six of them showed at least some examples of rates considered by previous authors to be rapid. When the reduction rates are related to the chlorophyll a contents of the communities, the maximum rates recorded come in the following order: Hyella balani, Scytonema sp., Hyella balani-Schizothrix sp., Calothrix crustacea, Rivularia sp., Microcoleus chthonoplastes, Hyella balani-purple sulphur bacteria, Pleurocapsa-Chroococcus. With the exception of the mixed Hyella balani-purple sulphur bacterial community, the rate of acetylene reduction was in all experiments greater in the light than in the dark, the difference being significant (P<0.05) in the majority of cases. The rates were similar in all experiments whether incubation was carried out with sea or brackish water. It seems probable that nitrogen fixation by blue-green algal communities makes an important addition to the lagoon ecosystem, and that not only heterocystous, but also some non-heterocystous, species are involved. Among the latter, the data for Hyella balani and Microcoleus chthonoplastes are especially convincing.     

Nitrogen fixation in breeding lines of Phaseolus vulgaris L.

Nitrogen fixation in nine common bean (Phaseolus vulgaris L.) lines was estimated using the ¹⁵N isotope dilution method at two locations in two seasons. In the first season at one location no N₂ fixation was detected while in the second season up to 51 kg N ha^–1 were estimated. There were significant differences between lines and correlations between trials were significant for the amounts of N₂ fixed, but not for total shoot nitrogen. The plants that fixed the most nitrogen nodulated rapidly after germination. Differences in maximum nodule mass, but not specific nodule activity, were detected also.     

Nitrogen Fixation During Blooms of Nodularia in Coastal Waters and Backwaters of the Arkona Sea (Baltic Sea) in 1974

Nitrogen fixation was investigated by means of the acetylene reduction method during the development of a water bloom of Nodularia in coastal waters of the Baltic Sea west of the island of Hiddensee and in backwaters showing different degrees of eutrophication. Depending on plankton density, the values found varied greatly. The maximum of nitrogen fixation values found in extremely dense water blooms under special conditions (Baltic Sea, 2250 μg N₂/l · h; Kleiner Jasmunder Bodden, 374 μg N₂/l · h) are up to 10³ times higher than from other parts of the Baltic Sea or from inland waters. The average nitrogenase activity determined for coastal water populations of the Baltic Sea is 2.15 pg N₂/heterocyst · h and that of the inmost backwaters 0.77 pg N₂/heterocyst · h. The relationship between N₂-fixation and nutrient content in water is discussed.     

Bloom formation of Gloeotrichia echinulata and Aphanizomenon flos-aquae in a shallow,eutrophic, Danish lake

Over a period of four years, the seasonal periodicity of dominant phytoplankton species in a shallow, eutrophic Danish lake changed markedly. Cyanophytes prevailed during the summer period of all four years. In the first three years, species of Microcystis, Anabaena and Aphanothece dominated, whereas in the fourth year of investigation, these algae were replaced by Gloeotrichia echinulata (J. E. Smith) Richter and Aphanizomenon flos-aquae (L.) Ralfs. The most striking environmental differences in the fourth year as compared with the previous three years, were an increase in tranparency, from about 0.5 meter in 1989–1991 to more than 2 metres preceding the summer maximum in 1992, and a simultaneous occurrence of low oxygen concentrations. A collapse of the fish population was followed by an increased proportion of large Cladocerans in the zooplankton. Improved light conditions at the bottom and grazing pressure from large Cladocerans favoured growth of the large colony forming blue-green algae, Gloeotrichia echinulata and Aphanizomenon flos-aquae. These species germinate from resting spores in the sediment and are able to sustain some growth there before migration to the lake water. The transfer of algal biomass from the bottom sediment to the water phase was accompanied by a marked increase in concentrations of particulate phosphorus and nitrogen in the entire lake.     

Nitrogen fixation by white clover in pastures grazed by dairy cows: Temporal variation and effects of nitrogen fertilization

Effects of rate of nitrogen (N) fertilizer and stocking rate on production and N₂ fixation by white clover (Trifolium repens L.) grown with perennial ryegrass (Lolium perenne L.) were determined over 5 years in farmlets near Hamilton, New Zealand. Three farmlets carried 3.3 dairy cows ha^–1 and received urea at 0, 200 or 400 kg N ha^–1 yr^–1 in 8–10 split applications. A fourth farmlet received 400 kg N ha^–1 yr^–1 and had 4.4 cows ha^–1.There was large variation in annual clover production and total N₂ fixation, which in the 0 N treatment ranged from 9 to 20% clover content in pasture and from 79 to 212 kg N fixed ha^–1 yr^–1. Despite this variation, total pasture production in the 0 N treatment remained at 75–85% of that in the 400 N treatments in all years, due in part to the moderating effect of carry-over of fixed N between years.Fertilizer N application decreased the average proportion of clover N derived from N₂ fixation (P_N; estimated by ¹⁵N dilution) from 77% in the 0 N treatment to 43–48% in the 400 N treatments. The corresponding average total N₂ fixation decreased from 154 kg N ha^–1 yr^–1 to 39–53 kg N ha^–1 yr^–1. This includes N₂ fixation in clover tissue below grazing height estimated at 70% of N₂ fixation in above grazing height tissue, based on associated measurements, and confirmed by field N balance calculations. Effects of N fertilizer on clover growth and N₂ fixation were greatest in spring and summer. In autumn, the 200 N treatment grew more clover than the 0 N treatment and N₂ fixation was the same. This was attributed to more severe grazing during summer in the 0 N treatment, resulting in higher surface soil temperatures and a deleterious effect on clover stolons.In the 400 N treatments, a 33% increase in cow stocking rate tended to decrease P_N from 48 to 43% due to more N cycling in excreta, but resulted in up to 2-fold more clover dry matter and N₂ fixation because lower pasture mass reduced grass competition, particularly during spring.     

Nitrogen fixation in subarctic streams influenced by beaver (Castor canadensis)

Nitrogen fixation was measured in four subarctic streams substantially modified by beaver (Castor canadensis) in Quebec. Acetylene-ethylene (C₂H₂ C₂H₄) reduction techniques were used during the 1982 ice-free period (May–October) to estimate nitrogen fixation by microorganisms colonizing wood and sediment. Mean seasonal fixation rates were low and patchy, ranging from zero to 2.3 × 10^–3 µmol C₂H₄ · cm^–2 · h^–1 for wood, and from zero to 7.0 × 10^–3 µmol C₂H₄ · g AFDM^–1 · h^–1 for sediment; 77% of all wood and 63% of all sediment measurements showed no C₂H₂ reduction. Nonparametric statistical tests were unable to show a significant difference (p > 0.05) in C₂H₂ reduction rates between or within sites for wood species or by sediment depth.Nitrogen contributed by microorganisms colonizing wood in riffles of beaver influenced watersheds was small (e.g., 0.207 g N · m^–2 · y^–1) but greater than that for wood in beaver ponds (e.g., 0.008 g N · m^–2 · y^–1) or for streams without beaver (e.g., 0.003 g N · m^–2 · y^–1). Although mass specific nitrogen fixation rates did not change significantly as beaver transform riffles into ponds, the nitrogen fixed by organisms colonizing sediment in pond areas (e.g., 5.1 g N · m^–2 · y^–1) was greater than that in riffles (e.g., 0.42 g N · m^–2 · y^–1). The annual nitrogen contribution is proportional to the amount of sediment available for microbial colonization. We estimate that total nitrogen accumulation in sediment, per unit area, is enhanced 9 to 44 fold by beaver damming a section of stream.     

Nitrogen fixation by Nodularia spumigena Mertens (Cyanobacteriaceae). 2: Laboratory studies

The effects of changes in diurnal light patterns, salinity, and phosphorus on nitrogen fixation (as measured by acetylene reduction) by Nodularia spumigena Mertens were examined. As well, the effects of added inorganic nitrogen on growth, nitrogen fixation and heterocyt frequencies, and changes in nitrogen fixation and heterocyst frequencies during the growth cycle of Nodularia in cultures were determined.The diurnal pattern of nitrogenase activity in Nodularia was primarily light-induced, though dark activity did occur. Nitrogenase activity following a period of darkness exceeded the normal light rate (> 90 compared to 50 nmol · C₂H₂ reduced · ml^–1 · h^–1). Nitrogen fixation was reduced by high and very low salinities (5 to 10 was the optimum range), and added phosphorus stimulated nitrogenase in P-starved cells. Added nitrogen (ammonium or nitrate) had no effect on the growth of Nodularia, but in short term studies, ammonium completely inhibited nitrogenase activity. Heterocyst frequencies were greatest in the log phase of growth (to 40 per mm). During stationary phase, nitrogenase activity was negligable.