01.03.2013 Aufrufe

The Oder Estuary - IOW

The Oder Estuary - IOW

The Oder Estuary - IOW

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development of algae in the Pomeranian Bay started earlier, already in March during the 1980’s.<br />

<strong>The</strong> concentrations during spring became more pronounced during the 90’s (Fig. 8.3).<br />

µg/l<br />

30<br />

20<br />

10<br />

0<br />

-10<br />

-20<br />

-30<br />

-40<br />

J F M A M J J A S O N D<br />

Kl. Haff<br />

Gr. Haff<br />

Bucht<br />

Figure 8.3: Differences in median chlorophyll-a concentrations (µg/l) between the 1990’s<br />

compared to the 1980’s in the Kleines Haff, the Wielki Zalew (Grosses Haff) and the<br />

Pomeranian Bay (Bucht). Data source: State Agency of Environment, Protection of<br />

Nature and Geology Mecklenburg-Vorpommern (LUNG) and West Pomeranian<br />

Voivodeship Inspectorate in Szczecin (WIOS).<br />

<strong>The</strong> spatial chlorophyll pattern in the lagoon is influenced by the <strong>Oder</strong> river during several months.<br />

It is well known that phytoplankton forms patches, which are driven by wind and currents, and<br />

show strong vertical concentration gradients. <strong>The</strong>se effects create an intensive patchiness, which<br />

cannot be represented by the existing few sampling locations.<br />

<strong>The</strong> nitrogen as well as the phosphorus concentrations in the lagoon are very high and nutrients are<br />

abundant most of the time. Like in other temperate zone estuaries (NIXON & PILSON 1983) nitrogen<br />

becomes a scarce resource during late summer. Phosphorus can play a role as a limiting element for<br />

algae biomass in spring, indicated by low PO4 values between April and June. <strong>The</strong> same is true for<br />

silicate. However, especially in the eastern part of the lagoon even intensive phytoplankton blooms<br />

during summer usually do not deplete nutrients. One reason is the constant nutrient supply by the<br />

<strong>Oder</strong> river and another reason is the mineralization of organic material, which is an important<br />

source for nutrients. Due to self-shading effects and high water turbidity as a result of sediment<br />

resuspension, light is the most important resource in the lagoon. In winter low temperatures play a<br />

role, too. With decreasing nutrient loads with the <strong>Oder</strong> river during the 1990’s, the importance of<br />

nutrients in the lagoon slightly increased.<br />

In the Pomeranian Bay nutrients, especially nitrogen plays a more important role as limiting<br />

resources for algae biomass.

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