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The Irish Sea: nutrient status and phytoplankton
Gowen, R.J.; Stewart, B.M. (2005). The Irish Sea: nutrient status and phytoplankton. J. Sea Res. 54(1): 36-50. https://dx.doi.org/10.1016/j.seares.2005.02.003
In: Journal of Sea Research. Elsevier/Netherlands Institute for Sea Research: Amsterdam; Den Burg. ISSN 1385-1101; e-ISSN 1873-1414, meer
Ook verschenen in:
Mills, D.K.; Gowen, R.J. (Ed.) (2005). Contrasting approaches to understanding eutrophication effects on phytoplankton. Journal of Sea Research, 54(1). Elsevier: Amsterdam. 1-124 pp., meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoorden
    ANE, Irish Sea
    Aquatic communities > Plankton > Phytoplankton
    Chemical elements > Nonmetals > Phosphorus > Organic phosphorus > Dissolved organic matter > Dissolved organic phosphorus
    Enrichment
    Enrichment
    Eutrophication
    Nutrients (mineral)
    Ierse Zee [Marine Regions]
    Marien/Kust
Auteurs  Top 
  • Gowen, R.J.
  • Stewart, B.M.
Abstract
    Historical nutrient and phytoplankton data from the Irish Sea are reviewed in the light of recent studies. Mean late winter concentrations of dissolved inorganic nitrogen (DIN as NO3- + NO2-), dissolved inorganic phosphate (DIP as PO43-) and silica (Si as SiO2) in offshore near-surface waters are 8.3, 0.7 and 6.6 μM, respectively. Concentrations in inshore waters of the eastern Irish Sea can reach 57 μM DIN, 5 μM DIP and 17 μM Si. The northwards residual flow through the Irish Sea (≈ 5 km- 3 d 1) is estimated to deliver ≈ 82 × 10³ t DIN and 12 × 10³ t DIP during the winter period. The annual freshwater inputs of DIN (including ammonium) and DIP are 123 and 9 × 10³ t, respectively. Offshore waters of the western Irish Sea are enriched with DIN and DIP (≈ 3.0 and 0.4 μM, respectively) relative to Celtic Sea shelf break concentrations but salinity DIN relationships show that measured winter concentrations are lower than predicted. Denitrification is considered a key process limiting nitrogen enrichment of the Irish Sea. The onset and duration of the production season is controlled by the sub-surface light climate. Differences in depth and tidal mixing in the Irish Sea give rise to regional variation in the timing and length of the production season. Maximum spring bloom biomass in coastal and offshore waters of the western Irish Sea (23 and 16 mg chlorophyll m- 3, respectively) compares with values of up to 44 mg chlorophyll m- 3 in Liverpool Bay and elevated production and biomass in the latter is attributed to enrichment. There is no evidence that enrichment and changes in nutrient ratios have caused major shifts in phytoplankton composition in Liverpool Bay. Species of Phaeocystis are found throughout the region in most years and together with other microflagellates can dominate the spring bloom. Red tides of dinoflagellates are rare events in the Irish Sea but regular monitoring of phytoplankton in the vicinity of shellfish beds has revealed the presence of toxin-producing dinoflagellates in the Irish Sea.
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