Abstract

ABSTRACTExperimental acidification of a tropical stream was conducted to measure the effects of declining pH on aquatic macroinvertebrates. The mechanisms by which anthropogenic acidification occur in a freshwater stream system are relatively well understood, while little is known about the natural phenomena of acidification or the corresponding effects on macroinvertebrate assemblages. Previous studies have attempted to model stream acidification using strong acids; however, this is one of the first studies which models stream acidification using the addition of gaseous CO2. This method is a more natural means of modeling stream acidification conditions arising from increased levels of dissolved CO2. We hypothesized that if experimental acidification was expressed most strongly at the injection site and produced a pH gradient downstream, macroinvertebrates should respond to the gradient and employ an escape mechanism to avoid the adverse conditions. Three macroinvertebrate sampling strategies were used: drift nets, leaf pack samples and benthic Surber samples. Samples were evaluated in the lab for macroinvertebrate abundance and taxonomic richness per m3 for drift net samples and benthic samples, and per g leaf material in the leaf pack samples. A maximum decline of 2 units in pH along a gradient was observed associated with the injection of CO2. Results obtained from drift net and benthic sample analysis were inconclusive, possibly because of low stream flow, although analysis of the leaf pack samples indicates lower macroinvertebrate composition at areas of lower pH. The leaf pack samples also show significant macroinvertebrate sensitivity to the most severe pH decline at the injection site.

Highlights

  • Stream acidification has been shown to have negative effects on freshwater ecosystems (Malmqvist & Rundle 2002; Dangles et al 2004; Camargo & Alonso 2006)

  • This study further demonstrated that acidic conditions could be created in a stream with the addition of CO2, and that the injection would create severe enough conditions to induce a macroinvertebrate response

  • We observed a clear effect on the macroinvertebrate composition and structure in the leaf pack samples as a product of the acidification

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Summary

Introduction

Stream acidification has been shown to have negative effects on freshwater ecosystems (Malmqvist & Rundle 2002; Dangles et al 2004; Camargo & Alonso 2006). Freshwater may be acidified either through the impact of dilution of acid neutralizing capacity, atmospheric deposition (i.e. sulfur and nitrogen deposition), oxidation–reduction (redox) reactions, organic acid inputs, or elevated concentrations of dissolved carbon dioxide (CO2). Small et al (2012) observed that an increase in labile carbon storage in the forest soil associated with the most severe drought during ENSO-1998 produced a pH decline of »3 units in. Small et al (2012) suggested that the pulse of CO2-saturated runoff when the rains returned contributed to higher levels of dissolved CO2, lowering the pH of shallow streams. Similar findings have been observed by Johnson et al (2008) in groundwater springs, where high soil CO2 concentrations contribute to a pH of 4.65, compared with first- and second-order streams with lower CO2 concentrations and a neutral pH

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