Influence of shellfish farming activities on the biogeochemical composition of the water column in Thau lagoon

Citation
P. Souchu et al., Influence of shellfish farming activities on the biogeochemical composition of the water column in Thau lagoon, MAR ECOL-PR, 218, 2001, pp. 141-152
Citations number
53
Categorie Soggetti
Aquatic Sciences
Journal title
MARINE ECOLOGY-PROGRESS SERIES
ISSN journal
01718630 → ACNP
Volume
218
Year of publication
2001
Pages
141 - 152
Database
ISI
SICI code
0171-8630(2001)218:<141:IOSFAO>2.0.ZU;2-C
Abstract
Thau lagoon is a Mediterranean shellfish ecosystem with large biomasses of oysters growing in waters with high residence time due to low tidal ranges, The influence of filter feeders (oysters and their epibiota) on the spatia l distribution of particulate and dissolved compounds in the water column o f Thau lagoon was studied through its variation with time, In 1991/1992, da ily variations were investigated in pens, corridors and outside shellfish f arming zones for nutrients, chlorophyll a and primary production. Salinity, dissolved oxygen, nutrients, organic matter and chlorophyll a were also mo nitored in surface waters inside and outside shellfish farming zones each w eek from January 1993 to March 1994. The presence of shellfish farms led to a decrease by only a few percent of oxygen concentrations in their vicinit y, but the mean (+/- SE) deficits of chlorophyll a and POC concentrations w ere 44 +/- 4 % and 26 +/- 9 % respectively in the eastern zone (8 m). The s hift induced by filter feeders in phytoplankton composition favoured picoph ytoplankton with higher growth rates. But the summer increase in phytoplank ton growth rate was stronger than the positive feedback due to filter feede r filtration. Summer was determinant for the growth of oysters owing to enh anced regenerated primary production. During this period, filter feeders we re not food limited, while they tended to control phytoplankton biomasses a nd production the rest of the year. The nutrient excess in shellfish farmin g zones was highly significant, with increases of 73 +/- 16, 36 +/- 12 and 19 +/- 8 % for ammonia, phosphates and silicate respectively in the eastern zone. In the western zone, the nutrient excess was less strong by half for ammonia and phosphate, because the lower depth (4 m) allows light to reach the bottom and enables benthic macroflora to grow on nutrients of benthic origin. The decline of phytoplankton biomasses in shellfish farms induced a decrease in the nutrient demand, especially for ammonia. This situation wa s likely to favour nitrification, which led during autumn to higher nitrate concentrations within shellfish farming zones than outside. Therefore, fil ter feeders were able to alter the dominant biogeochemical process in the w ater column by stimulating nitrification.