OSPAR eutrophication assessment

Introduction

Coastal eutrophication is a growing marine environmental problem in Europe and the need for more effective monitoring and control measures is increasing. In 1997 the OSPAR Commission adopted the Common Procedure for the identification of the Eutrophication Status of the maritime area. OSPAR committed all members to reduce phosphorus and nitrogen inputs into the maritime areas and to combat eutrophication to achieve a healthy environment where eutrophication does not occur. The Common Procedure includes the main parameters involved in eutrophication processes which are differentiated in four categories of qualitative assessment criteria for application in the Comprehensive Procedure:

• Category I: Nutrient enrichment
• Category II: Direct effects of nutrient enrichment
• Category III: Indirect effects of nutrient enrichment
• Category IV: Other effects of nutrient enrichment

These assessment criteria can be different for the three maritime areas with regard to eutrophication (non-problem areas, potential problem areas and problem areas).

Ecological Quality Objectives (EcoQOs)

Ecological Quality Objectives are a tool to support the application of the ecosystem approach to the management of human activities affecting the marine environment and provide a means to define the desired quality of the marine environment. The specific EcoQOs correspond to a selection of assessment parameters and their assessment levels as applied under the Common Procedure. The specific EcoQOs for eutrophication agreed at the 5th North Sea Conference by Ministers and OSPAR 2002 are:

1. Winter DIN and/or DIP should remain below elevated levels, defined as concentration > 50% above salinity related and / or region-specific natural background concentrations.
2. Maximum and mean region-specific chlorophyll a concentrations during the growing season should remain below region-specific elevated levels, defined as concentrations > 50% above the spatial (offshore) and/or historical background concentration.
3. Region/area-specific phytoplankton eutrophication indicator species should remain below respective nuisance and/or toxic elevated levels (and increased duration).
4. Oxygen concentration, decreased as an indirect effect of nutrient enrichment, should remain above region-specific oxygen deficiency levels, ranging from 4-6 mg oxygen per liter.
5. There should be no kills in benthic animal species as a result of oxygen deficiency and/or nuisance/toxic phytoplankton indicator species for eutrophication.

Category I: Nutrient enrichment

Introduction

The major causes of nutrient enrichment in coastal areas are associated with the need to satisfy human nutrition and diet by the use of fertilizers. Nutrients such as nitrates and phosphates are the most common single factor causing eutrophication. These nutrients are necessary for the growth of plants and biomass production of phytoplankton (microalgae) and macroalgae.

Nitrogen

Nitrogen is used by living organisms to produce a number of complex organic molecules such as amino acids, proteins and nucleic acids. The store of nitrogen found in the atmosphere (where it exists mainly as a gas (N₂)) plays an important role for life. Other major sources include organic matter in soil and the oceans. Nitrogen is often the most limiting nutrient for plant growth. This occurs because most plants can only take up nitrogen in two solid forms: ammonium ion (NH₄⁺) and the nitrate ion (NO₃^-). Most plants obtain the nitrogen they need as inorganic nitrate from the soil solution. Ammonium is used less by plants because it is extremely toxic in large concentrations. The stimulation of plant growth by nitrates may result in eutrophication, especially due to algae.

Phosphorus

The primary biological importance of phosphates is as a component of nucleotides which serve as energy storage (ATP) within cells or when linked together form the nucleic acids DNA and RNA. Most of world's phosphorus is locked up in rocks and can only be released weathering. A lot of the phosphorus that runs off into the ocean also gets buried into the ocean floor because it precipitates into a solid form and settles to the bottom as sediment. Phosphorus is only available to organisms in small quantities. For this reason, phosphorus is a limiting factor for plant growth. Their presence in water is due to detergents, fertilizers and biological processes. An excess of phosphate (PO₄^-) will stimulate the growth of plants and algae and is an important nutrient in eutrophication processes.

Silica

Diatoms are the predominant siliceous organisms in the marine environment and are a major component of the phytoplankton community. Diatoms accumulate silica (SiO₂) as a structural element in their cell walls.

Measuring devices

Nutrient analysers

References

1. OSPAR Commission, Background Document: Ecological Quality Objectives for the Greater North Sea with Regard to Nutrients and Eutrophication Effects [1]