Abstract

Coastal ecosystems are subject to human impacts both through adjacent lands and by run-off from the broader catchment area. Nutrient inputs, like phosphorus, were often lowered decades ago, but many aquatic ecosystems have not recovered accordingly. Therefore, restoration and future protection measures need to be founded upon insights on the nutrient demands of phytoplankton in order to limit their growth and negative impacts upon coastal water bodies. This study investigated phosphatase activity, phosphate uptake, and growth of phytoplankton in a model lagoon system at the southern Baltic Sea coast. This lagoon system is perennially dominated by Cyanobium, a clade of picocyanobacteria which lack nitrogen fixation but which are common in brackish waters. Dissolved phosphate and total nutrient ratios from long-term monitoring point to an overall P-limitation of the system. Apparent phosphatase activities confirmed P-starvation. However, experimental phosphate-fertilisations repeated over an annual cycle increased chlorophyll concentration only when either dissolved nitrogen, or N-fixing cyanobacteria were present. In contrast to chlorophyll, particulate matter increased within a week most of the time at the observed stations, even in unfertilised samples. The difference between chlorophyll and particulate responses could be explained by chlorosis after phosphorus fertilisation, as nitrogen was co-limiting. Similar findings have been described for other water bodies. This study indicates that nitrogen is co-limiting in the lagoon system, and that phosphorus input has not yet declined sufficiently.

Highlights

  • Induced eutrophication is one of the most challenging problems in aquatic ecosystems worldwide, as it changed the amounts, and the timing of nutrient flows to water bodies

  • Average dissolved inorganic P (DIP) was low at both stations and close to the determination limit (

  • Phytoplankton can regulate cellular P uptake systems, based on antecedent DIP pulses rather than previously stored P (Aubriot et al, 2011). These results combined with our findings indicate that plankton showed a slower response to applied DIP pulses during summer, because DIP was already supplied through high apparent alkaline phosphatase activity (APA)-release rates, even though DIP was below detection

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Summary

Introduction

Induced eutrophication is one of the most challenging problems in aquatic ecosystems worldwide, as it changed the amounts, and the timing of nutrient flows to water bodies. In case of the Baltic Sea, coastal lagoon systems cover 5% of the entire coastal zone, but account for 10% of the P burial and half of the denitrification of all coastal ecosystems in this region (Asmala et al, 2017). These characteristics point at the potential of coastal water bodies to protect larger water bodies. Coastal water bodies, like lagoons stand in the focus of restoration measures This filter effect makes coastal water bodies themselves prone to eutrophication, as they receive and store nutrient loads from a catchment area. Increased primary production and biomass can lead to increased turbidity, changed food webs, and sometimes harmful algal blooms (see de Jonge et al, 2002; Smith and Schindler, 2009 and sources cited therein)

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