THE ROLE OF THE BLUE MUSSEL MYTILUS-EDULIS IN THE CYCLING OF NUTRIENTS IN THE OOSTERSCHELDE ESTUARY (THE NETHERLANDS)

Authors
Citation
Tc. Prins et Ac. Smaal, THE ROLE OF THE BLUE MUSSEL MYTILUS-EDULIS IN THE CYCLING OF NUTRIENTS IN THE OOSTERSCHELDE ESTUARY (THE NETHERLANDS), Hydrobiologia, 283, 1994, pp. 413-429
Citations number
79
Categorie Soggetti
Marine & Freshwater Biology
Journal title
ISSN journal
00188158
Volume
283
Year of publication
1994
Pages
413 - 429
Database
ISI
SICI code
0018-8158(1994)283:<413:TROTBM>2.0.ZU;2-H
Abstract
The fluxes of particulate and dissolved material between bivalve beds and the water column in the Oosterschelde estuary have been measured i n situ with a Benthic Ecosystem Tunnel. On mussel beds uptake of POC, PON and POP was observed. POC and PON fluxes showed a significant posi tive correlation, and the average C:N ratio of the fluxes was 9.4. The re was a high release of phosphate, nitrate, ammonium and silicate fro m the mussel bed into the water column. The effluxes of dissolved inor ganic nitrogen and phosphate showed a significant correlation, with an average N:P ratio of 16.5. A comparison of the in situ measurements w ith individual nutrient excretion rates showed that excretion by the m ussels contributed 31-85% to the total phosphate flux from the mussel bed. Ammonium excretion by the mussels accounted for 17-94% of the amm onium flux from the mussel bed. The mussels did not excrete silicate o r nitrate. Mineralization of biodeposition on the mussel bed was proba bly the main source of the regenerated nutrients. From the in situ obs ervations net budgets of N, P and Si for the mussel bed were calculate d. A comparison between the uptake of particulate organic N and the re lease of dissolved inorganic N (ammonium + nitrate) showed that little N is retained by the mussel bed, and suggested that denitrification i s a minor process in the mussel bed sediment. On average, only 2/3 of the particulate organic P, taken up by the mussel bed, was recycled as phosphate. A net Si uptake was observed during phytoplankton blooms, and a net release dominated during autumn. It is concluded that mussel beds increase the mineralization rate of phytoplankton and affect nut rient ratios in the water column. A comparison of N regeneration by mu ssels in the central part of the Oosterschelde estuary with model esti mates of total N remineralization showed that mussels play a major rol e in the recycling of nitrogen.