Fig. 3. Pseudo-nitzschia seriata TEM micrograph of the poroid structure arranged
within the striae consisting of two outer rows of larger poroids and one or two inner
rows of smaller poroids.
induce DA production in P. australis
[7], and the most potent DA-inducing
N form has been shown to be urea. It is
very likely that urea and/or nitrate affected the DA production in P. seriata.
Studies on P. australis show that urea
is highly potent and induces the production of DA at least 4-fold compared
to nitrate and ammonium treatments.
Ammonium doubled the production of
DA compared to the control (normal sea
levels of nutrients)[7].
Our observations support the hypothesis that high N levels induce DA
production in PN. An increase in landbased runoff of N (especially in the form
of urea) may increase the frequency
and toxicity of toxic blooms. Therefore
strict limits of fertilizer usage and spills
may be important to avoid washout and
runoff of N, potentially causing algal
blooms, damaging the environment and
mussel harvesting industries.
Acknowledgements
We are grateful to Helene Munk Sørensen (Ministry of Environment and Food)
for her thorough support and steadfast
belief in the use of monitoring data.
Fig. 4. TEM micrograph of a mixed water sample from the bloom, resembling a culture
sample.
tons. The silo contained 9500 tons at
the time of the breakdown and thereby
passed its maximum capacity by 500
tons [3]. The adjacent areas and especially the waters immediately outside
the harbour were heavily affected by
the extensive amounts of nitrogen. The
discharge consisted of N32 and N16
fertilizer liquids, which is predominantly urea. Organic nitrogen in the form of
urea is (as inorganic nitrogen) 100 %
bioavailable [4]. The organic molecule
in urea is easily separated from the rest
by the enzyme urease, splitting ammonium from bicarbonate [5] [6]. Monitoring data showed peaks in nitrate levels
immediately after the outlet, revealing
more than double the average amount
of available nitrate for the area. Phosphorus levels were not increased.
In Denmark, the major part of nitrogen runoff from land happens from
October till January. During this period
14
algal growth is limited by light rather than nutrients. From February and
further into the summer period, algal
growth is controlled mostly by nutrients. The usual pattern is depletion of
phosphorous followed by nitrogen depletion.
In spring 2016 in Little Belt (between Jutland and Funen) the discharge
of 4000 tons of readily available nitrogen must inarguably have affected the
ecosystem in the area. The general concentrations of planktonic algae were
unusually high in the following month
(data not shown here). Available nitrogen was possibly crucial for P. seriata to
overtake the diatom community for a
period of time and additionally producing the high amounts of DA vectoring up
the food web.
Nitrogen repletion has been shown
to induce toxin production in other PN
species. Different forms of nitrogen can
References
1. Lundholm N et al 2005. I M S Newsletter
29: 8-10
2. Lundholm N & S Harðardóttir 2017. HAN
56: 4-5
3. Kudsk CE et al 2017. Technical Report.
Technological Institute.
4. Markager S 2016. Technical Report. Aarhus University and Fredericia Municipality.
5. Tinoco Jr I et al 2002. Physical Chemistry.
Principles and Applications in Biological
Sciences. 4th Edition. Pearson Prentice
Hall, Pearson Education International.
6. Bradley PBM. et al 2010. Estuarine,
Coastal and Shelf Science 88: 429- 441.
7. Howard MDA et al 2007. Harmful Algae
6: 206217.
Authors
Anna Olesen & Nina Lundholm, Natural
History Museum of Denmark, University of
Copenhagen, Denmark
Sara Hardardottir, The Geological Survey of
Denmark and Greenland, Denmark
Maren Moltke Lyngsgaard, Orbicon, Denmark
Per Andersen, Niras, Denmark
Corresponding author:
wlx447@alumni.ku.dk
HARMFUL ALGAE NEWS NO. 60 / 2018
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