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Untitled - WWF - Pakistan

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Detailed Ecological Assessment Report 2008 – Keenjhar Lake<br />

documented from an ecological point of view. The knowledge of temperate lakes<br />

and their phytoplankton is much greater that that of tropical and sub-tropical lakes.<br />

Tropical lakes appear to have different plankton community structure from<br />

temperate lakes and are mostly populated by submerged and emergent<br />

macrophytes.<br />

Nitrogen was reported as the main limiting factor for production in tropical waters<br />

(Payne, 1986). But the shallow lakes of Salado River Basin are rich in both nitrates<br />

and phosphates (Quiros, 1989) and limitation by nutrient is not evident contrary to<br />

most tropical aquatic eco-systems where nutrients are rapidly mineralized (Fisher,<br />

1978; Junk & Furch, 1991); sediments of these lakes store high amount of organic<br />

matter, mainly derived from macrophytes. Macrophytes appeared as the main<br />

factor influencing structure and abundance of phytoplankton (Izaguirre & Vincour,<br />

1994)/. Lakes with a greater biomass of higher plants showed lower phytoplankton<br />

densities. The influence of macrophyhtes on phytoplankton communities has been<br />

discussed by several authors and attributed to different factors, shading allelopathy<br />

and competition for nutrients (Welch and Cooke, 1987: Engel, 1998 and Mitchell,<br />

1989)<br />

In temperate region the blue green algae often dominates summer phytoplankton<br />

of both shallow and deep lakes (Sommer et al, 1986). In other Danish lakes poor<br />

light conditions and continuous circulation lead to the dominance of blue green<br />

algae (Chorus & Shlag, 1993). Nutrient limitation did not fulfill any obvious role, the<br />

annual pattern of phytoplankton dynamics appeared to have been dominated by<br />

hydrological and climatological features (Barone & Flores, 1984). More over the<br />

coupling of hydrological and algal seasonability is well seen in other man made<br />

lakes (Talling, 1986) and the hydrodynamic control of phytoplankton growth has<br />

been discussed by Harris (1986)<br />

In tropical and sub-tropical lakes, seasonal cycle of phytoplankton seems to be<br />

strongly related to the water level fluctuations and the climatological features and it<br />

seems reasonable to agree with the results of Harris (1986) & Barone & Flores<br />

(1994), that abiotic factors such as flooding, dewatering, light, and mixing mainly<br />

affect the phytoplankton dynamics and also by inhabiting or delaying the<br />

development if biotic relationships (i.e. fry predation efficiency) which commonly<br />

takes place in aquatic environment.<br />

The construction of dams creates large bodies of standing waters which may be<br />

the subject to chemical and biological changes symptomatic of eutrophication.<br />

Among the most dramatic consequences of eutrophication results in the formation<br />

of water blooms of blue green algae (Goldman & Horne, 1983). Blue green algae<br />

can release allelopathic substances which are toxic to humans (Lawton & Codd,<br />

1991) and to other organisms (Feuillade, 1992). The occurrence of blue green<br />

algae’s in Indian lakes and reservoirs has been well studies by Gopal et al., (1998)<br />

and Houk, (1989).<br />

Baker Lake is a shallow, eutrophic lake that also serves as a reservoir. The<br />

knowledge gained through this piece of work will provide a clear picture of the<br />

phytoplankton composition of the lake. Changes in water levels played an<br />

important role in the structure of phytoplankton communities. The distinct increase<br />

of secchi disc depth in lake is the main factor responsible for change in cynaphyta<br />

compositions. The improved light condition at bottom made it possible for<br />

Gloeotrchia and Amphanizomenon to establish lake population in the sediment.<br />

The migration of Amphanizomenon and Gloeotrichia transfers particularly<br />

phosphorus and nitrogen from sediment to the lake (Osgood 1988 and Barbieror &<br />

Welch, 1992). Istvanovics et al., (1993) and Pettersson et al., (1993) clearly confirm<br />

the phenomena.<br />

<strong>WWF</strong> <strong>Pakistan</strong> – Indus for All Programme Page 19 of 165

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