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Volume 6, Spring 2008 - Saddleback College

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Fall 2007 Biology 3A Abstracts<br />

turned to a bluish clear color with blue color<br />

precipitate floating in the water.<br />

Conc of N (ppm)<br />

1.8<br />

1.6<br />

1.4<br />

1.2<br />

1<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0<br />

low<br />

high<br />

Figure 1. There was no difference in nitrate concentration<br />

between low tide (1.07 ± 0.3 ppm (± se) and high tide (1.5<br />

± 0.1 ppm (± se), (p = 0.1, one tailed t- test). Error bars<br />

show the standard error.<br />

1<br />

Conc of P (ppm)<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0<br />

low<br />

high<br />

Figure 2. Phosphate concentration was greater during<br />

high tide (0.77 ± 0.09 ppm (± se) than low tide ( 0.28 ±<br />

0.02 ppm (± se,) (p= 0.02, one-tailed t-test). Error bars<br />

indicate the standard error.<br />

Discussion<br />

For nitrate ion concentration was 1.07 ± 0.3<br />

ppm (± se) at low tide and 1.5 ± 0.1 ppm (± se) at<br />

high tide. Although hypothesis stated that nitrate ion<br />

concentration and the tide level were corresponding,<br />

the difference of nitrogen gas concentration at low<br />

tide and high tide were not significant. The<br />

concentration of nitrogen did not depend on the level<br />

of tide in this study. The result may suggest that<br />

dissolved nitrogen gas concentration varies<br />

depending on the season of the year or water<br />

conditions; for example salinity, temperature and<br />

tides.<br />

In this study, the phosphate concentration<br />

showed the relatively high value. For phosphate<br />

concentration, it was 0.3 ± 0.02 ppm (± se) at low<br />

tide and was 0.77 ± 0.09 ppm (± se) at high tide.<br />

Increased rate of phosphate supply led to the growth<br />

of two species of photosynthetic alga, O. agardhii<br />

and A. Formosa (Tilman et al, 1982). Tilman et al<br />

(1982) proved that nitrogen and phosphate limitation<br />

was the factor which led to a succession of algal<br />

growth.<br />

Horne et al, (1972) measured dissolved<br />

nutrients in the lake. In Oaks arm, nitrogen fixation<br />

was very low, but much higher in the two basins<br />

where high nitrogen fixation was occurring. This<br />

observation suggests that the possibility of a lasting<br />

nitrogen gas and phosphate gas limitation in Oaks<br />

arm following the peak of the bloom at the end of<br />

August. In contrast, organic dissolved nitrogen<br />

showed no significant variation. Horne et al (1972)<br />

provide a reasonable answer as to why low nitrogen<br />

concentration was found at certain times and only in<br />

non oligotrophic lakes. In oligotrophic lakes, these<br />

conditions of some combined inorganic nitrogen and<br />

sufficient dissolved organic nitrogen may never<br />

occur. In stratified non-oligotrophic lakes, the<br />

condition is normally only provided toward the end<br />

of a spring bloom and during autumn overturn. In<br />

non-stratified, non-oligotrophic lakes, the condition<br />

may occur at irregular intervals throughout the year<br />

were dependent on nitrogen turnover rates. Carbon,<br />

Nitrogen and Phosphorus are the chemical building<br />

blocks for living organism, therefore nitrogen<br />

fixation is a natural process that is needed in order for<br />

all organisms to survive, (Tzortziou, 2007 ) but the<br />

over use of nitrogen gas becomes a toxin that may<br />

also harm marine life. As water was collected and<br />

nitrogen gas and phosphorous gas levels were<br />

calculated with a DR/850 Calorimeter (Hach<br />

Company, CO. U.S.A) from Dana Point Harbor in<br />

Southern California at both low and high tide; Nitrate<br />

ions and Phosphorous gas levels did in fact increase<br />

as sea levels increased. This DR/850 Calorimeter<br />

devise has several settings and packets that contain<br />

compounds that create reactions obtaining accurate<br />

results. The mean of phosphate gas concentration was<br />

0.28 ± 0.02 ppm (± se) (N=3) at low tide and 0.77 ±<br />

0.09 ppm (± se) (N=3) at high tide. Nitrate ion<br />

concentrations were 1.07 ± 0.27 ppm (± se) at low<br />

tide and 1.5 ± 0.1 ppm (± se) at high tide; although<br />

there was no significant difference of nitrate ion<br />

levels between low and high tide. Nitrogen gas that<br />

ends up in the ocean waters by run offs of farmlands<br />

are contributing to the outbreak of Domoic acid (Pan<br />

et al, 1996) ; as the fish eat the polluted plankton, the<br />

toxins become more potent, then marine mammals<br />

consume this contaminated food source, affecting<br />

them tremendously. As a result their bodies can no<br />

longer digest the toxins and their brain’s<br />

hippocampus becomes paralyzed resulting in seizures<br />

19<br />

<strong>Saddleback</strong> Journal of Biology<br />

<strong>Spring</strong> <strong>2008</strong>

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