Baltic Sea hypoxia
Baltic Sea hypoxia refers to low levels of oxygen in bottom waters, also known as hypoxia, occurring regularly in the Baltic Sea. As of 2009 the total area of bottom covered with hypoxic waters with oxygen concentrations less than 2 mg/l in the Baltic Sea has averaged 49,000 km2 over the last 40 years. The ultimate cause of hypoxia is excess nutrient loading from human activities causing algal blooms. The blooms sink to the bottom and use oxygen to decompose at a rate faster than it can be added back into the system through the physical processes of mixing. The lack of oxygen (anoxia) kills bottom-living organisms and creates dead zones.
Causes
The rapid increase in hypoxia in coastal areas around the world is due to the excessive inputs of plant nutrients, such as nitrogen and phosphorus by human activities. The sources of these nutrients include agriculture, sewage, and atmospheric deposition of nitrogen containing compounds from the burning of fossil fuels. The nutrients stimulate the growth of algae causing problems with eutrophication. The algae sink to the bottom and use the oxygen when they decompose. If mixing of the bottom waters is slow, such that oxygen stocks are not renewed, hypoxia can occur.
Description
As of 2009 the total area of bottom covered with hypoxic waters with oxygen concentrations less than 2 mg/l in the Baltic Sea has averaged 49,000 km2 over the last 40 years.[1] In the Baltic Sea, the input of salt water from the North Sea through the Danish Straits is important in determining the area of hypoxia each year. Denser, saltier water comes into the Baltic Sea and flows along the bottom. Although large salt water inputs help to renew the bottom waters and increase oxygen concentrations, the new oxygen added with the salt water inflow is rapidly used to decompose organic matter that is in the sediments. The denser salt water also reduces mixing of oxygen poor bottom waters with more brackish, lighter surface waters. Thus, large areas of hypoxia occur when more salt water comes into the Baltic Sea.
Geological perspective
Geological archives in sediments, primarily the appearance of laminated sediments that occur only when hypoxic conditions are present, are used to determine the historical time frame of oxygen conditions.[2] Hypoxic conditions were common during the development of the early Baltic Sea called the Littorina Sea starting around 8,000 calendar years Before Present. Hypoxia disappeared for a period of nearly 3,000 years, appearing a second time just before the Medieval Warm Period around 400 AD until 1200 AD, i.e. lasted for 800 years. The Baltic Sea became hypoxic again around 1900 AD and has remained hypoxic for the last 100 years. The causes of the various periods of hypoxia are being scientifically debated, but it is believed to result from both climate and human impacts, which started several thousand years ago.
Impacts
The deficiency of oxygen in bottom waters changes the types of organisms that live on the bottom. The species change from long-living, deep-burrowing, slow-growing animals to species that live on the sediment surface. They are small and fast-growing, and can tolerate low concentrations of oxygen.[3] When oxygen concentrations are low enough only bacteria and fungi can survive. These areas are called dead zones. In the Baltic Sea, low oxygen concentrations also reduce the ability of cod to spawn in bottom waters. Cod spawning requires both high salinity and high oxygen concentrations for cod fry to develop, conditions that are rare in the Baltic Sea today.
The lack of oxygen also increases the release of phosphorus from bottom sediments. Excess phosphorus in surface waters and the lack of nitrogen stimulates the growth of cyanobacteria. When the cyanobacteria die and sink to the bottom they consume oxygen leading to further hypoxia and more phosphorus is released from bottom sediments. This process creates a vicious circle of eutrophication that helps to sustain itself.
Solutions
The countries surrounding the Baltic Sea have established the HELCOM Baltic Marine Environment Protection Commission to protect and improve the environmental health of the Baltic Sea. In 2007, the Member States accepted the Baltic Sea Action Plan to reduce nutrients. Because the public and media have been frustrated by the lack of progress in improving the environmental status of the Baltic Sea, there have been calls for large-scale engineering solutions to add oxygen back into bottom waters and bring life back to the dead zones. An international committee evaluated different ideas[4] and came to the conclusion that large-scale engineering approaches are not able to add oxygen to the extremely large dead zones in the Baltic Sea without completely changing the Baltic Sea ecosystem. The best long-term solution is to implement policies and measures to reduce the load of nutrients to the Baltic Sea.
References
- ↑ Conley, D.J., S. Björck, E. Bonsdorff, J. Carstensen, G. Destouni, B.G. Gustafsson, S. Hietanen, M. Kortekaas, H. Kuosa, H. E.M. Meier, B. Müller-Karulis, K. Nordberg, A. Norkko, G. Nürnberg, H. Pitkänen, N.N. Rabalais, R. Rosenberg, O.P. Savchuk, C.P. Slomp, M. Voss, F. Wulff, L. Zillén. 2009. Critical Review: Hypoxia-related processes in the Baltic Sea. Environ. Sci. Tech. 43: 3412-3420. http://pubs.acs.org/doi/pdf/10.1021/es802762a
- ↑ Zillén, L., D.J. Conley, T. Andrén, E. Andrén, and S. Björck. 2008. Past occurrences of hypoxia in the Baltic Sea and the role of climate variability, environmental change and human impact. Earth Sci. Rev. 91: 77-92.
- ↑ Vaquer-Sunyer, R. and C.M. Duarte. 2008. Thresholds of hypoxia for marine biodiversity. Proceed. Natl. Acad. Sci. USA 105: 15452-15457.
- ↑ Conley, D.J., E. Bonsdorff, J. Carstensen, G. Destouni, B.G. Gustafsson, L.-A. Hansson, N.N. Rabalais, M. Voss, L. Zillén. 2009. Viewpoint: Tackling hypoxia in the Baltic Sea: Is engineering a solution? Environ. Sci. Tech. 43: 3407-3411.