The
deepest areas of the Baltic Sea have always had a low oxygen
content. The inflow of fresh water is actually limited by low
thresholds at the entrance to the Baltic Sea. At the same time,
there is a relatively fresh layer above the denser and saltier water
in the deep layer of the sea. This results in an effective
stratification of the water column, which prevents the mixing of
water masses necessary to transfer oxygen to the water at the
bottom.
During
the last century, the areas of oxygen depletion have increased
drastically from approximately 5,000 km2 in around
1900 to the present day, where they extend to 60,000 km2 --
or about one and a half times the total area of Denmark.
"We
analysed data for the water temperature, oxygen content and salinity
stretching back for 115 years. On the basis of this analysis, we can
determine that the many nutrients from the land are the main cause
of the widespread oxygen depletion," says Professor Jacob
Carstensen, Department of Bioscience, Aarhus University.
Seabed
without oxygen
Oxygen
depletion occurs when the oxygen uptake at the bottom exceeds the
amount of oxygen brought to the deeper water layers via currents and
mixing by the wind.
During
the last twenty years, climate change has also played a role in the
poor oxygen situation. Warmer conditions reduce the solubility of
oxygen from the atmosphere and increase oxygen consumption because
the biological respiration processes are boosted.
"The
water temperature has risen and will continue to rise in the years
ahead. It's therefore extra important that all the countries
surrounding the Baltic Sea are committed to the Baltic Sea action
plan they joined, and that they comply with the necessary efforts to
reduce the release of nutrients into the Baltic," emphasises
Professor Carstensen, who is also director of the Baltic Nest
Institute in Denmark.
Oxygen
depletion on the seabed has a negative impact on the entire
ecosystem. This is partly because the seabed turns into a 'desert'
inhabited only by bacteria that can survive without or with very low
amounts of oxygen. Some bacteria produce methane, which can bubble
up to the water and tear large areas of the toxic, hydrogen
sulphide-rich seabed with it. This involves sediment disturbances
that can kill fish high up in the water column.
Studies
show that it takes decades before benthic fauna once more return to
a dead seabed when the oxygen conditions improve.