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Pakistan Journal of Biological Sciences

Year: 2004 | Volume: 7 | Issue: 11 | Page No.: 1870-1875
DOI: 10.3923/pjbs.2004.1870.1875
Ecological Studies of the River Padma at Mawa Ghat, Munshiganj II. Primary Productivity, Phytoplankton Standing Crops and Diversity
Ashfaque Ahmed and Md. Almujaddade Alfasane

Abstract: Net primary productivity of the Padma river, studied during February to December 2002, ranged between 0.13 and 0.54 mg O2 L-1 h-1 and community respiration rate was 0.15 to 1.04 mg O2L-1 h-1. In some occasions, community respiration exceeds the net primary productivity. Phytoplankton community was represented by 29 genera belonging to 6 families. Greatest crops of phytoplankton occurred in February where 26 genera of 5 families were recorded among which Chlorophyceae was abundant (38.46%) in terms of number of genera. Melosira sp., Synedra sp. and Fragilaria sp. (897.9x103, 129.1x103 and 117.1x103 ind. L-1, respectively) of Bacillariophyceae and Actinastrum sp., Schroederia sp. (378.7x103 and 204.1x103 ind. L-1, respectively) of Chlorophyceae were the most abundant genera. In June only 2 genera of 2 families were recorded. Although the common river alga, Melosira sp. was found most common in February and April, it was totally absent in June. Two pollution indicator algae viz., Arthrospira sp. and Oscillatoria sp. were found during the sampling period. Four different most commonly used diversity indices were calculated which were interrelated. The values of Shannon and Wiener Index of Diversity were 0.81 (minimum) in June and 5.1 in February (maximum). Species diversity (Shannon and Wiener index) increased with higher net production.

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Ashfaque Ahmed and Md. Almujaddade Alfasane, 2004. Ecological Studies of the River Padma at Mawa Ghat, Munshiganj II. Primary Productivity, Phytoplankton Standing Crops and Diversity. Pakistan Journal of Biological Sciences, 7: 1870-1875.

Keywords: pollution indicator, indices of diversity, community respiration and productivity

INTRODUCTION

The results of observations taken on the physiochemical aspects on the river Padma at Mawa ghat, Munshiganj, during February 2002 to December 2002 were discussed in the earlier paper[1], but yielded no information about the seasonal growth of the algae and the population fluctuations in relation to habitat factors and the primary productivity. Phytoplankton primary productivity in association with limno-chemical qualities could be fruitfully utilized as indices of trophic status of water bodies[2,3]. Many workers have discussed the principles, mechanisms, techniques of measurements and limiting factors involved in the primary productions[4-7].

Reinhard[8] has discussed the influence of physical, chemical and biotic factors in the adaptation and distribution of plankton of Upper Mississippi. Effects of water quality on the diatom flora of Lesotho were described by Schoeman[9]. Phytoplankton in two English rivers was illustrated by Swale[10]. Crayton and Sommerfield[11] have investigated phytoplankton distribution and abundance in eleven tributaries of the Colorado River within the Grand Canyon. In the aquatic environment, the phytoplankton community is recognised as one of the most sensitive indicators of change and perturbations[12] and the present study will thus provide important baseline data in assessing the impact of any future exploitation.

MATERIALS AND METHODS

Primary production was estimated at the surface (depth: 0.1 m) by in situ incubation of water samples for 1.5 h in 100 mL light and dark bottles[13-15]. Dissolved oxygen was determined by the methods described in APHA[15] and the values were converted into carbon, using a factor of 0.375[16]. Gross and net primary production and respiration values and percentage of net production and respiration were calculated.

For the collection of phytoplankton sample plastic bottles of 100 mL capacity were used. Water samples were collected from 4 sites from each of the 3 zones. These samples were collected with a closing bottle from a depth of 0.5 m and the samples were preserved with Lugol’s iodine[17]. Then the bottles were closed and brought to the laboratory for phytoplankton counting. The genera of planktonic organisms were identified with the help of standard Bangladeshi and other literatures15,18-23].

Many indices are available for measuring diversity[24,25]. Some depend on the observation that the number of species (S) found in any one sample tends to be proportional to the logarithm of the number of specimens (N) counted (DL~ S/logH), some are based on probability theory and others are arbitrary. All are functions of the number of species present, their relative abundances, or both. For the present analysis four indices that are frequently used are chosen[26].

The species diversity is simply the number of species found in a sample: Ds=S[27]

The species dominance is given as DD = p max[28]

where, pmax is the maximum proportion of any one species in a sample.

The dominance is the simplest of the indices that make use of species proportions to define diversity.

Two other indices making use of species proportions are considered: a modification of Simpson’s index and Shannon-Wiener index. These two indices depend on the whole spectrum of species proportions and are here referred to as “compound diversity”[26].

Simson’s index[29] can be written as

[30,31] in which form it measures the probability that two specimens, picked at random from a sample, belong to different species. This probability may be taken as a measure of diversity of an assemblage.

The Shannon Wiener diversity indices (H) were also calculated: H =-∑pi (log2pi)[32]

In the figure H is designated as DH.

RESULTS AND DISCUSSION

Primary production or the organic carbon fixed through photosynthetic activity by phytoplankton helps in understanding the productive function of aquatic system[33]. During the present investigation gross primary productivity (GPP or Pg), determined by oxygen method of the river Padma, varied from 0.4 to 1.57 mg O2 L–1 h–1 (Table 1). When the values were converted into carbon units (using a factor of 0.375)[16], it ranged between 0.15 and 0.59 mg C L–1 h–1. The highest value was noted in February and lowest in December. The variation in the primary production (gross production) in the Padma river could be attributed to the composition and density of phytoplankton and their photosynthetic efficiency which again are functions of the nutrients status and productive potential of the water body. Net primary production (NPP or Pt) values ranged from 0.05 to 0.20 mg C L–1 h–1. The gross primary production was higher than net production. The gross: net primary production ratio varied from 1.67 to 4.0. Community respiration (CR) values were 0.06 to 0.39 mg C L–1 h–1. The present study showed that CR surpassed NPP in some occasions which may be due to the dominance of zooplankton[34].

The estimates of production and respiration of ecosystem allow judgments as to the stage of ecosystem development and inference as to whether the ecosystem is importing energy[33]. The ratio Pg/Pt is ecologically significant, because values near unity indicate the process of community production and decomposition are nearly balanced (Table 1). Values less than unity generally indicate organic matter is being imported, while values greater than unity indicate a growth-type ecosystem[33]. The caveat in these conclusions is that one or two estimates of Pg/Pt ratio alone are unlikely to reveal much about ecosystem function since local conditions can temporarily alter the ratio on both sides of unity. For example, cloudy weather can depress the ratio below unity. Local upwelling of nutrient can lead to temporarily high values of Pg relative to Rt. etc. However, when Pg and Rt are measured frequently, trends in the value of the ratio provide insight into ecosystem function.

The total volume of plankton varies from season to season in all waters and the seasonal variations in quantity of phytoplankton of the river Padma were not found to be exception. The total algal flora and their density of the river Padma was shown in Table 2. Phytoplankton community was represented by 29 genera belonging to six classes viz., Cyanophyceae, Chlorophyceae, Bacillariophyceae, Cryptophyceae, Euglenophyceae and Dinophyceae. The greatest crops of phytoplankton occurred in winter (February) followed by summer (April) and lowest numbers during the rainy season (June). The diatoms dominated over the other classes of algae during February. Out of the 26 genera of 5 classes found during this period, the dominant phytoplankton recorded were Melosira sp., Synedra sp. and Fragilaria sp. (897.9x103, 129.1x103 and 117.1x103 ind. L–1, respectively) of Bacillariophyceae; Actinastrum sp. and Schroederia sp. (378.7x103 and 204.1x103 ind. L–1, respectively) of Chlorophyceae and Anabaena sp. (117.1x103 ind. L–1) of Cyanophyceae (Table 2). The most abundant species in terms of numbers was Melosira sp. which accounted for 31.57%.

Table 1: Seasonal variations in net-gross primary production ratio and respiration quantum

Table 2:Variations in total number of genus and total quantity of blue-greens, greens, diatoms, euglenoids, Cryptophyceae and Dinophyceae through out the sampling periods in the river Padma

It is evident from Table 3 that, when the groups were considered on the strength of the number of genera present in the phytoplankton, the Chlorophyceae come first represented by 10 genera and that are the most abundant in this time of the study period than in any other study time. Though the green algae exceeded in the number of genera, they did not do so in bulk as compared with diatoms. Algae belonging to the class Euglenophyceae were totally absent during this time.

In April, diatoms, blue-greens, greens, Euglenophyceae, Cryptophyceae and Dinophyceae were all present but total numbers of individuals were less. Melosira sp. was also dominant followed by Peridinium sp. and Actinastrum sp. out of 15 genera belonging to these 6 classes. During June, river reached a higher level which is characterized by swift flow. As a result dilution of the phytoplankton was expected. The observations showed low values or the absence of phytoplankton. Only two genera of Cyanophyceae and Euglenophyceae, one genus from each class, were recorded. Although the Melosira sp. was the dominant species during the months of February and April, it was totally absent in June. Seasonal variation in phytoplankton populations as a result of changing environmental conditions has been well documented[35,36]. The dynamics of phytoplankton growth and community structure over a seasonal cycle in temperate latitudes is controlled by a highly complex relationship of environmental factors in which one factor after another gains momentarily greater significance[35].

Diversity indices are often used to monitor the impact of pollutants on aquatic biological communities. Their main advantage is in summarizing large amounts of data which can be easily used by a wide variety of people. Although some authors have expressed their reservations about the use of diversity indices[37-39], there is little doubt that they represent an important tool in water quality studies[40-42]. Various investigators have shown a negative correlation between species diversity and environmental stress[43-45]. Wilhm and Dorris[45] reported that the following values of species diversity are generally with the following description of the water quality: H<1-sever pollution; 1<H<3-moderate pollution; H>3-clean water. In the present investigation the Shannon-Wiener diversity values ranged from 0.81 to 5.1 (Fig. 1) which indicate the polluted condition of the river Padma except during February. In February the value was 5.1 and in April it was 2.27. During June it was only 0.81. The various indices are interrelated (Fig. 1). Among the four commonly used indices of diversity, species diversity and compound diversity (Ds-Dp, Ds-DH) and Dp-DH were highly significantly correlated (p=0.001).

Table 3:
List of phytoplankton and their density (ind L–1) in water of the river Padma river near Mawa Ghat. Values are in thousand (U = Upper reach, M = Middle reach, D = Down reach)

Fig. 1:
Relationship between various diversity indices. DP, Ds, DD, DH are defined in text. Ds-Dp, Dp-DH and Dp-DH are highly significantly correlated

Fig. 2:
Species diversity in relation to primary productivity in the river Padma. Species diversity was measured by Shannon-Wiener function. Note high productivity with increase diversity

Connell and Orias[46] stated in their productivity hypothesis that greater production resulted in greater diversity. The present study supported this idea (Fig. 2). The maximum diversity was found when the productivity (GPP) was the highest and diversity decreased in lower production rates. The stability of primary production is a major determinant of the species diversity of a community[47].

Many investigators have tried to relate the presence or absence of specific indicator species to varying degree of water quality[48]. Kolkwitz and Marsson[49] have included four algae namely Arthrospira, Oscillatoria, Spirulina and Aphanotheca as indicator types of heavy pollution. In the present study Arthrospira (58.2x103 ind. L–1), Oscillatoria (16.6x103 ind. L–1) were found although typical river plankton like Melosira[50] was found most abundant. Though the concept of indicator species also offers a fast and efficient means of judging the quality of waters, many biologists have serious doubts about the use of a single species and consequently preferred the concept of indicator communities or assemblages[51,52].

ACKNOWLEDGMENTS

We thank the Delta Study Centre, Dhaka University for financial support of this work and Mr. Zakir Hossain and Mr. Isnain for assistance in the sample collection. The authors are also grateful to the Dean. Faculty of Biological Science, University of Dhaka for his financial help to cover up the printing cost.

REFERENCES

  • Ahmed, A., 2004. Ecological studies of the river padma at mawa ghat, munshiganj I. Physico-chemical properties. Pak. J. Biol. Sci., 7: 1865-1869.
    CrossRef    Direct Link    


  • Goldman, C.R., 1960. Primary productivity and limiting factors in three lakes of the Alaskan Peninsula. Ecol. Monogr., 30: 207-270.


  • Oglesby, R.T., 1977. Relationship of fish yields to lake phytoplankton standing crop, production and morphometric-edaphic factors. J. Fish. Res. Board Can., 34: 2271-2279.


  • Odum, H.T., 1960. The role of tidal marshes in estuarine production. nySt. Conserv., 60: 1-4.


  • Olah, J., 1971. Glass effect and the microbial plankton-seston relation in the water of Lake Balaton and Betro. Anal. Biol. Tihany, 38: 153-160.


  • Nasar, S.A.K. and J. Dutta Munshi, 1975. Studies on primary production in a freshwater pond. Jap. J. Ecol., 25: 21-23.


  • Gupta, B.P., 1982. Studies on primary production in Bhavanisagar reservoir (Tamil Nadu). J. Inland Fish. Soc. India, 14: 49-54.


  • Reinhard, E.G., 1931. Plankton ecology of upper mississippi: Part II. Influence of physical, chemical and biological factors. Ecol. Monogr., 4: 395-464.
    Direct Link    


  • Swale, E.M.F., 1969. Phytoplankton in two English River. J. Ecol., 57: 1-23.
    Direct Link    


  • Crayton, M.W. and M.R. Sommerfield, 1979. Composition and abundance of phytoplankton in tributaries of the Lower Colorado River, Grand Canyon region. Hydrobiologia, 66: 81-93.
    CrossRef    


  • Duthie, H.C. and M.L. Ostrofsky, 1975. Environmental impact of the Churchil Falls (Labrador) Hydroelectric project: A preliminary assessment. J. Fish. Res. Board Can., 32: 117-125.
    Direct Link    


  • Gaarder, T. and H.H. Gran, 1927. Investigations on the production of plankton in the Oslo Fjord. P.V.R Rappeun. Commn. Int. Explor. Sci. Mer. Mediterr., 42: 1-48.


  • Janus, L.L. and H.C. Duthie, 1979. Phytoplankton composition and periodicity in a Northeastern Quebec Lake. Hydrobiologia, 63: 129-134.
    CrossRef    


  • Huber-Pestalozzi, G., 1955. Das phytoplankton des suswasers systemdatik und Biologie, Euglenophyceen: A. Thienemann, Die Binnengewasser. Stuttgart, 16: 1-606.


  • Islam, A.K.M.N. and M. Khatun, 1966. Preliminary studies on the phytoplankton of polluted waters. Sci. Res., 4: 141-149.


  • Islam, A.K.M.N. and L. Nahar, 1967. Primary studies on the phytoplankton of polluted waters. II. Blue green algae. Sci. Res., 4: 141-149.


  • Islam, A.K.M.N. and Z.N.T. Begum, 1970. Studies on the phytoplanktons of Dacca district. Order: Chlorococcales. J. Asiatic Soc. Pak., 15: 227-271.


  • Sanders, H.L., 1968. Marine benthic diversity: A comparative study. Am. Naturalist, 102: 243-243.
    Direct Link    


  • Berger, W.H. and F.L. Parker, 1970. Diversity of planktonic foraminifera in deep-sea sediments. Science, 168: 1345-1347.
    CrossRef    Direct Link    


  • Fisher, A.G., 1960. Latitudinal variations in organic diversity. Evolution, 14: 64-64.


  • Simpson, E.H., 1949. Measurement of diversity. Nature, 163: 688-688.
    CrossRef    Direct Link    


  • Stehli, F.G. and C.E. Helsley, 1963. Paleontologic technique for defining ancient pole positions. Science, 142: 1057-1057.


  • Ruggiero, M.A. and H.C. Merchant, 1979. Water quality, substrate and distribution of macroinvertebrates in the Partuxent River, Maryland. Hydrobiologia, 64: 183-189.


  • Das, A.K., 2002. Phytoplankton primary production in some selected reservoirs of Andha Pradesh. Geobios, 29: 52-57.
    Direct Link    


  • Riley, G.A., 1946. Factors controlling phytoplankton populations on Geroges Bank. J. Mar. Res., 6: 54-73.


  • Carpenter, E.J., 1971. Annual phytoplankton cycle on the Cape Fear River Estauary, North Carolina. Chesapeake. Science, 12: 95-104.


  • Godfrey, P.J., 1978. Diversity as a measure of benthic macroinvertebrate community response to water pollution. Hydrobiologia, 57: 111-122.


  • Eberhardt, L.L., 1969. Some aspects of species diversity models. Ecology, 50: 503-505.


  • Hulbert, S.H., 1971. The concept of species diversity: A critique and alternate parameters. Ecology, 52: 577-586.


  • Devaux, J., 1975. Succession ecologique, diversite specigique et production primarie dans un lac oligotrophe d`Auvergne (France). Verh. Int. Verein. Limnol., 19: 1165-1171.


  • Wilhm, J., 1968. Biomass units versus numbers of individuals in species diversity indices. Ecology, 49: 153-156.


  • Slobodchikoff, C.N. and J.E. Parrott, 1977. Seasonal diversity in aquatic insect communities in an all-year stream system. Hydrobiologia, 52: 143-151.


  • Itow, S., 1963. Grassland vegetation in the uplands of Western Honshu, Japan: II Sussession and grazing indicators. Jap. J. Bot., 18: 133-167.


  • Gordon, A.G. and E. Gorham, 1963. Ecological effects of air pollution from an iron-sintering plant at Wawa, Ontario. Can. J. Bot., 41: 1063-1078.


  • Wilhm, J.L. and T.C. Dorris, 1968. Biological parameters for water quality criteria. Bioscience, 18: 477-481.
    Direct Link    


  • Connell, J.H. and E. Orias, 1964. The ecological regulation of species diversity. Am. Nat., 98: 399-414.
    Direct Link    


  • Gaufin, A.R. and C.M. Tarzwell, 1956. Aquatic macroinvertebrates as indicators of organic pollution in Lytle Creek. Sewage Ind. Wastes, 28: 906-924.


  • Kolkwitz, R. and M. Marsson, 1908. Okologie der Pflanzlichen saprobien (Ecology of plant saprobes)- Ber. Berichte der Deutschen Botanischen Gesellschaft, 26: 1-505.


  • Cairns, J.C., G.R. Lanza and B.C. Parker, 1972. Pollution related structural and functional changes in aquatic communities with emphasis on freshwater algae and protozoa. Proc. Acad. Nat. Sci. Philadelphia, 124: 79-127.
    Direct Link    


  • Schoeman, F.R., 1973. A Systematical and Ecological Study of the Diatom Flora of Lesotho with Special Reference to Water Quality. V. and R. Printer, Pretoria, South Africa, pp: 355


  • Vollenweider, R.A., 1969. A Manual of Methods for Measuring Primary Production in Aquatic Environments. Blackwell Scientific Publications, Oxford and Edinburg


  • American Public Health Association, 1976. Standard Methods for the Examination of Water and Waste Water. 14th Edn., APHA, New York


  • Lind, O.T., 1974. Hand Book of Common Methods in Limnology. C.V. Mosby Company, St. Louis


  • Smith, G.M., 1950. The Fresh Water Algae of the United States. 2nd Edn., McGraw Hill Book Co., New York, pp: 719


  • Ward, H.B. and G.C. Whipple, 1959. Fresh Water Biology. 2nd Edn., John Wiley and Sons, New York, USA


  • Hutchinson, G.E., 1967. A Treatise on Limnology. Wiely, New York, pp: 360


  • Beerbower, J.R. and D. Jordan, 1969. Application of information theory to paleontologic problems: Taxonomic diversity. J. Paleontol., 43: 1184-1198.
    Direct Link    


  • Stehli, F.G., 1965. Paleontologic technique for denning ancient ocean currents. Science, 148: 943-946.


  • Odum, E.P., 1971. Fundamental of Ecology. 3rd Edn., W.B. Saunders Co., Philadelphia and Toppan Co. Ltd., Tokyo, Japan, pp: 574


  • Krebs, C.J., 1978. Ecology, The Experimental Analysis of Distribution and Abundance. Harper and Row Publishers, New York, London, pp: 470


  • Reynolds, C.S., 1988. Potamoplankton: Paradigms, Paradoxes and Prognoses. In: Algae and the Aquatic Environment, Round, F.E. (Ed.). Biopress Ltd., Bristol, pp: 285-311


  • Roback, S.S., 1974. Insects (Arthopoda: Insecta). In: Pollution Ecology of Freshwater Invertebrates, Hart, C.W. and S.L.H. Fuller (Eds.). Academic Press, New York, pp: 313-376

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