Benthic decomposition of Ulva lactuca: A controlled laboratory experiment |
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Authors: | Bente Aa. Lomstein Lise Bonne Guldberg Anne-Turi Amtoft Neubauer Jesper Hansen Andrew Donnelly Rodney A. Herbert Pierluigi Viaroli Gianmarco Giordani Roberta Azzoni Rutger de Wit Kai Finster |
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Affiliation: | 1. Department of Biological Sciences, Section for Microbiology, University of Aarhus, Building 1540, Ny Munkegade, DK-8000 Aarhus C, Denmark;2. Department of Environmental and Applied Biology, School of Life Sciences, University of Dundee, Dundee DD1 4HN, UK;3. Department of Environmental Sciences, Università di Parma, Area Parco della Scienze 33/A, 43100 Parma, Italy;4. UMR 5119 CNRS-Université Montpellier II, Université Montpellier II, Case 093, Place Eugène Bataillon, F-34095 Montpellier Cedex 05, France |
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Abstract: | The degradation of an Ulva lactuca mat (0.2 kg dw m−2) was studied in a controlled flow-through mesocosm for 31 d. Sediment chambers without U. lactuca served as controls. Fluxes of ∑CO2, O2, inorganic nitrogen, and urea were determined during the incubation period in addition to sulfate reduction rates, POC and PON content, enumeration of specific bacterial populations and evaluation of the physiological state of the added U. lactuca thalli. After U. lactuca addition to the chambers, there was an immediate increase in the efflux of ∑CO2 from 11 to 27 mmol-C m−2 d−1 and a concomitant increase in O2 uptake from 11 to 23 mmol m−2 d−1. These effluxes remained elevated throughout the incubation period. In contrast, the NH4+ efflux increased from 0.1 to 1.8 mmol NH4+ m−2 d−1 during the first 3 d of incubation, followed by 6 d with a constant efflux rate, after which time it decreased gradually to 0.3 mmol NH4+ m−2 d−1 by the end of the experiment. In total, NH4+accounted for 83% of the total nitrogen efflux after addition of U. lactuca. During the 31 d incubation period there was a continuous colonization of the thalli by bacteria. Sulfate reducers associated with the thalli accounted for 3% of the carbon oxidation on day 31. The molar C:N ratio in mineralization products (the ratio between the efflux of ∑CO2 and NH4+ + NO2− + NO3−) increased from 15 mol mol−1 at day 11 after U. lactuca addition to >80 mol mol−1 by the end of the incubation. Since the C:N ratio in the mineralization products was much higher than the original thallus material (8.9 mol mol−1) it is probable that a preferential incorporation of NH4+ into the increasing bacterial biomass occurred. The nitrogen for bacterial growth was most likely obtained from degradation of U. lactuca thalli as there was no stimulation of urea-N turnover in the sediment during incubation. The net increase in bacteria cell number in the 18-mm thick thallus layer was estimated to be 7.6 × 109 to 2.4 × 1010 bacterial cells cm−3. In contrast, the bacterial cell number remained constant in the −Ulva incubations. |
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Keywords: | Macroalgae Ulva lactuca Decomposition process Benthic mineralization Nitrogen flux |
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