Abstract

The Great Brak Estuary is a temporarily open/closed system situated along the warm temperate coast of the Western Cape, South Africa. The estuary is subject to a variety of anthropogenic impacts (e.g. freshwater abstraction and sewage discharge) that increases its susceptibility to prolonged periods of mouth closure, eutrophication, and ultimately the formation of macroalgal blooms. The aim of this study was to determine the decomposition characteristics of the most dominant submerged macrophyte and macroalgal species in the Great Brak Estuary. Laboratory experiments were conducted to determine the effect of different temperature regimes on the rate of decomposition of 3 macrophyte species and the extent of inorganic nutrients released. The results demonstrated that anaerobic decomposition of Zostera capensis, Ruppia cirrhosa, and Cladophora glomerata resulted in high levels of inorganic nutrient release over the 28-day study period. Ammonium (NH4+) was the dominant form of dissolved inorganic nitrogen (DIN) released during the decomposition process for all three species. The low levels of total oxidised nitrogen (nitrate and nitrite) released during decomposition were attributed to the inhibition of nitrification by heterotrophic bacteria under anoxic conditions. The relative levels of dissolved inorganic phosphorus (DIP) released were lower than that observed for DIN, and peaked early on in the experimental period (ca. 7 days), thereafter stabilising or decreasing. The DIP levels were explained, in part, by the varying nutrient requirements and limitations of each species (e.g. nitrogen-limited). The release of inorganic nutrients was greatest at higher temperatures (i.e. 25°C and 30°C), due to the reduced bacterial activity experienced at lower temperatures (i.e. 15°C). Ultimately, estuarine health deteriorates during macroalgal blooms, and therefore it is important to implement mitigation measures, such as artificial mouth breaching and plant harvesting, in order to minimise or reverse the effects of eutrophication.Keywords: Great Brak Estuary, decomposition, temperature, inorganic nutrient release, Cladophora glomerata, Zostera capensis, Ruppia cirrhosa

Highlights

  • The rate and extent of anthropogenic pressures on estuaries have increased greatly over recent times due to the demands of an ever-increasing global population

  • The overall ammonium (NH4+), soluble reactive phosphorus (SRP) and total oxidised nitrogen (TOxN) concentrations for the control treatments were shown to be significantly lower (p < 0.001) at all temperatures throughout the study period compared to the Z. capensis, R. cirrhosa and C. glomerata treatments

  • The experiment demonstrated that anaerobic decomposition of Zostera capensis, Ruppia cirrhosa, and Cladophora glomerata resulted in high levels of inorganic nutrient release over the 28-day study period

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Summary

Introduction

The rate and extent of anthropogenic pressures on estuaries have increased greatly over recent times due to the demands of an ever-increasing global population. The incidence of fast-growing ephemeral macroalgae proliferations has increased globally due to eutrophication caused by excessive nutrient inputs (mainly nitrogen and phosphorus) into coastal ecosystems (Paalme et al, 2002; Lomstein et al, 2006; Berezina and Golubkov, 2008; Gubelit and Berezina, 2010). Under these conditions macroalgae, either attached or free-floating, accumulate in very high biomass The consequences of such macroalgal blooms are numerous, and include oxygen depletion (anoxia), altered biogeochemical cycling in the water column and sediments, changes to the composition of higher trophic levels, shading of slow-growing, submerged macrophytes (such as seagrasses), and an overall reduction in biodiversity and recreational value (Hanisak, 1993; Pedersen and Borum, 1996; Paalme et al, 2002; Lomstein et al, 2006; Gubelit and Berezina, 2010)

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