Nutrient and iron limitation to Ulva blooms in a eutrophic coastal lagoon (Sacca di Goro,Italy) |
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Authors: | Pierluigi?Viaroli author-information" > author-information__contact u-icon-before" > mailto:pierluigi.viaroli@unipr.it" title=" pierluigi.viaroli@unipr.it" itemprop=" email" data-track=" click" data-track-action=" Email author" data-track-label=" " >Email author,Marco?Bartoli,Roberta?Azzoni,Gianmarco?Giordani,Claudio?Mucchino,Mariachiara?Naldi,Daniele?Nizzoli,Laura?Tajé |
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Affiliation: | (1) Dipartimento di Scienze Ambientali, Università di Parma, Parco Area delle Scienze 33A, I-43100 Parma, Italy;(2) Dipartimento di Chimica Generale e Inorganica Chimica Analitica, Chimica Fisica, Università di Parma, Parco Area delle Scienze 17A, I-43100 Parma, Italy |
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Abstract: | Growth patterns and bloom formation of the green seaweed Ulva rigida were analysed in the eutrophic Sacca di Goro lagoon (Po River Delta, Italy). Variations of standing biomasses and elemental composition of Ulva were analysed through an annual cycle with respect to nitrogen, phosphorus and iron. Growth rates, nutrient and iron uptake and nitrate storage by macroalgal thalli were also assessed with field experiments during the formation of a spring bloom. The control of Ulva growth and the bloom formation depended on multiple factors, especially on nitrogen availability and iron deficiency. In the nitrate rich waters of the Sacca di Goro lagoon, nitrate accumulation in Ulva thalli was inversely related with Fe uptake, indicating an influence of Fe limitation on N acquisition. Since length and magnitude of nitrate luxury uptake are inversely related to the size of the intracellular nitrate pools, in nitrate rich waters the fast growing Ulva may face risk of N-limitation not only when exposed to low N concentrations or at high biomass levels, but also when exposed to pulsed dissolved nitrate concentrations at low iron availability. The potential Fe limitation could be affected by processes controlled by geochemical reactions and by macroalgal growth and decomposition. Both Fe oxidation during the active macroalgal growth and the formation of insoluble FeS and FeS2 during bloom collapse can result in a drastic decrease of soluble iron. Thus, a potential limitation of Fe to macroalgae can occur, determining positive feedbacks and potentially controlling the extent of bloom development and persistence. |
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Keywords: | nitrogen phosphorus nitrate iron Ulva blooms |
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