Typical features of particulate phosphorus in the Seine estuary (France) |
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Authors: | Julien Némery Josette Garnier |
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Institution: | (1) UMR Sisyphe 7619, UMPC Paris 6, Boite 105, Tour 56, Etage 4, 4 place Jussieu, 75005 Paris, France;(2) Present address: LTHE (UMR CNRS 5564, UJF, INPG, IRD), BP 53, 38 041 Grenoble Cedex 09, France |
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Abstract: | During the 2001–2002 hydrological cycle, 8,000 tons P year−1 (44% as particulate phosphorus) originating from the Seine basin entered the Seine estuary. P content in suspended sediments
(SS) is 2.9 g P kg−1 (80% as inorganic form) at Poses (the upstream limit of the Seine estuary). During the transfer from Poses to Caudebec (the
limit of saline water intrusion), Particulate Inorganic Phosphorus (PIP) in SS decreases by 40% whereas Particulate Organic
Phosphorus (POP) remains stable. This decrease is explained as the result of (i) a dilution by SS poorer in P, originating
from storage zones (mudflats) within the estuary, and (ii) a loss of P by sedimentation, especially in the Rouen harbour where
15% to 20% of SS are yearly trapped and extracted. Downstream, in the turbidity maximum of the estuary, P content in SS is
twice as low as at Poses (1.5 g P kg−1, 70% as inorganic form). PIP content is fairly homogeneous both vertically and throughout an annual survey. On the other
hand, POP varies by season. Higher POP content is observed during vernal period with phytoplankton accumulation. In a salinity
gradient from 0 to 30 (PSS78), PIP content further decreases by 30%. POP does not vary much in this gradient, leading to the
assumption that PIP is submitted to desorption in response to the dilution by marine waters (poor in orthophosphates). Using
32P isotopic method, we establish a mathematical formulation of P exchangeable between the suspended solid and water phases
of the Seine estuary. Particulate P in the turbidity maximum zone is shown to represent a possible source of dissolved P,
available for algal growth in the Seine Bight. Instead of playing a role of nutrient retention, the turbidity maximum zone
of the Seine estuary could favour coastal eutrophication. |
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Keywords: | Seine estuary Turbidity maximum zone Phosphorus dynamics |
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