High alkaline phosphatase activity in phosphate replete waters: The case of two macrotidal estuaries
|Author(s)||Labry Claire1, Delmas Daniel1, Youenou Agnes1, Quere Julien1, Leynaert Aude2, Fraisse Stephane3, Raimonet Melanie2, Ragueneau Olivier2|
|Affiliation(s)||1 : Ifremer Dyneco Pelagos, Plouzane, France.
2 : Inst Univ Europeen Mer, UMR 6539, Lab Sci Environm Marin, Plouzane, France.
3 : Univ Rennes 1, UMR CNRS ECOBIO 6553, Campus Beaulieu, Rennes, France.
|Source||Limnology And Oceanography (0024-3590) (Wiley-blackwell), 2016-07 , Vol. 61 , N. 4 , P. 1513-1529|
|WOS© Times Cited||20|
|Abstract||The occurrence of alkaline phosphatase activity (APA) that hydrolyses organic phosphorus into phosphate (PO4) is commonly related to PO4 deficiency of oceanic, coastal and fresh waters. APA is almost never investigated in PO4-rich estuaries, since very low activities are expected to occur. As a consequence, microbial mineralization of organic phosphorus into PO4 has often been ignored in estuaries. In this study, we examined the importance of potential APA and the associated microbial dynamics in two estuaries, the Aulne and the Elorn (Northwestern France), presenting two different levels of PO4 concentrations. Unexpected high potential APA was observed in both estuaries. Values ranged from 50 to 506 nmol L−1 h−1, which range is usually found in very phosphorus-limited environments. High potential APA values were observed in the oligohaline zone (salinity 5–15) in spring and summer, corresponding to a PO4 peak and a maximum bacterial production of particle-attached bacteria. In all cases, high potential APA was associated with high suspended particulate matter and total particulate phosphorus. The low contribution of the 0.2–1 μm fraction to total APA, the strong correlation between particulate APA and bacterial biomass, and the close relationship between the production of particle-attached bacteria and APA, suggested that high potential APA is mainly due to particle-attached bacteria. These results suggest that the microbial mineralization of organic phosphorus may contribute to an estuarine PO4 production in spring and summer besides physicochemical processes.|