Western English Channel Fixation
16th December 2008
A trio of scientists from PML and the National Oceanography
Centre have discovered that the biological fixation of nitrogen in
the marine environment may be far greater than was previously
thought, and thus could quash the current school of thought on the
role of shelf seas such as the English Channel and the North Sea in
global nitrogen cycling.
A specialised, but diverse, group of organisms (diazotrophs),
which include cyanobacteria and bacteria, are able to obtain their
nitrogen requirements from atmospheric N2 (known as
nitrogen fixation) and pass it onto other organisms. This process
is particularly significant,as these organisms usually exist in
nutrient poor areas of the ocean, where they help to maintain the
productivity of the system.
Indirect evidence had indicated that N2 fixation in
the marine environment may be far greater than was previously
thought and recent work has proved this theory to be correct, with
fixation rates now being reported at previously unprecedented
levels. A pilot study at PML, to investigate the potential for
nitrogen fixation in the western English Channel, demonstrated the
first reported evidence of nitrogen fixation in a temperate,
coastal marine environment. This was a significant find in itself,
however using molecular techniques we found that the samples
contained a number of previously unreported nitrogen fixing
organisms.
A more focused examination of coastal waters close to Plymouth
is planned, whereby an historical library of stored DNA samples
will be interrogated to examine the potential nitrogen fixing
activity on a seasonal basis and how this may vary between years.
This information will be compared with long-term data sets of
nutrient and primary production measurements in order to assess the
contribution that nitrogen fixation makes to biological production
in temperate waters.
If this process is found to be significant in these waters, then
this will challenge existing models, budgets and predictions
concerned with coastal and shelf sea carbon and nitrogen cycling.
This will be of concern to all scientists who investigate marine
biogeochemical cycling and agencies with responsibilities in these
areas.