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Our new Biological Assessment is out - Klamath Basin Crisis

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<strong>Klamath</strong> Project Operations <strong>Biological</strong> <strong>Assessment</strong><br />

Endangered Suckers: Environmental Baseline for Suckers<br />

becomes the limiting nutrient. When light, nutrients, or other conditions for algae<br />

become unfavorable, the production of the algal bloom will cease or rapidly<br />

decline, resulting in an algal “crash.”<br />

The massive blooms of AFA and the subsequent rapid decline (crash) can cause<br />

extremes in water quality including elevated pH, low DO concentrations<br />

(hypoxia), and elevated levels of un-ionized ammonia, which can be toxic to f<strong>is</strong>h<br />

(Kann and Smith 1993; Kann and Smith 1999; Perkins et al. 2000 Water Quality;<br />

Walker 2001; Welch and Burke 2001; Wood et al. 2006; Kuwabara et al. 2007;<br />

Morace 2007). In the process of rapid growth, algal biomass can form extremely<br />

dense blooms, which can vary in magnitude depending on the availability of<br />

growth-promoting conditions (Kann and Smith 1993; Kann and Smith 1999;<br />

Perkins et al. 2000 Water Quality). During the same bloom conditions and<br />

following a bloom crash, particularly when coupled with high rates of nighttime<br />

respiration, DO can drop to levels that restrict f<strong>is</strong>h growth and that can be lethal<br />

(Kann and Smith 1993; Kann and Smith 1999; Perkins et al. 2000 Water Quality).<br />

In addition, when dense algae blooms die off, the microbiological decomposition<br />

of the algae and organic matter in the bed sediment can further deplete DO and<br />

produce increased concentrations of ammonia (Kann and Smith 1993; R<strong>is</strong>ley and<br />

Laenen 1999; Kann and Smith 1999; Perkins et al. 2000 Water Quality; Walker<br />

2001; Welch and Burke 2001; Wood et al. 2006; Kuwabara et al. 2007; Morace<br />

2007). The potential for low DO concentration increases later in the growing<br />

season (July-September) when the algae blooms have crashed and considerable<br />

organic matter has accumulated in the sediments. During th<strong>is</strong> same period,<br />

increased water temperature increases water column oxygen depletion rates as<br />

decomposition and respiration take place at a faster rate, and oxygen<br />

concentration in the water column tends to be lower because solubility of oxygen<br />

decreases as water temperature increases.<br />

Nutrient Input Algal GrowthWater Quality ChangesF<strong>is</strong>h Survival and<br />

Propagation<br />

Wetlands may affect water quality through production and release of<br />

decomposition products, particularly d<strong>is</strong>solved humic 1 substances that appear to<br />

inhibit AFA growth (Geiger et al. 2005). Figure 2-12 shows how humic<br />

substances from wetlands may inhibit AFA growth (Geiger et al. 2005). The<br />

absence or reduction of th<strong>is</strong> algae species just downstream, at or within marsh<br />

environments has been noted at Hanks Marsh (Forbes et al. 1998) and Upper<br />

<strong>Klamath</strong> National Wildlife Refuge (Sartor<strong>is</strong> and S<strong>is</strong>neros 1993, cited by Campbell<br />

1993a). Perdue et al. (1981) noted the absence of AFA in UKL at a location<br />

1 From humus, which are dark organic material in soils, produced by the decomposition of<br />

vegetable or animal matter and essential to the fertility of the earth.<br />

74

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