Abstract

Defining the geographic origins of free‐living aquatic microorganisms can be problematic because many such organisms have ubiquitous distributions, and proving absence from a region is practically impossible. Geographic origins become important if microorganisms have invasive characteristics. The freshwater diatom Didymosphenia geminata is a potentially ubiquitous microorganism for which the recent global expansion of nuisance proliferations has been attributed to environmental change. The changes may include declines in dissolved reactive phosphorus (DRP) to low levels (e.g., <2 mg/m3) and increases in dissolved inorganic nitrogen (DIN) to >10 mg/m3 because both these nutrient conditions are associated with nuisance proliferations of D. geminata. Proliferations of D. geminata have been observed in South Island, New Zealand, since 2004. We aimed to address the ubiquity hypothesis for D. geminata in New Zealand using historical river water nutrient data and new molecular analyses. We used 15 years of data at 77 river sites to assess whether trends in DRP or DIN prior to the spread of D. geminata were consistent with a transition from a rare, undetected, species to a nuisance species. We used new sequences of chloroplast regions to examine the genetic similarity of D. geminata populations from New Zealand and six overseas locations. We found no evidence for declines in DRP concentrations since 1989 that could explain the spread of proliferations since 2004. At some affected sites, lowest DRP occurred before 2004. Trends in DIN also did not indicate enhanced suitability for D. geminata. Lack of diversity in the chloroplast intergenic regions of New Zealand populations and populations from western North America is consistent with recent dispersal to New Zealand. Our analyses did not support the proposal that D. geminata was historically present in New Zealand rivers. These results provide further evidence countering proposals of general ubiquity in freshwater diatoms and indicate that, as assumed in 2004, D. geminata is a recent arrival in New Zealand.

Highlights

  • Species introductions are a recognized component of human-­ mediated global change (Ricciardi, 2007; Vitousek, D’Antonio, Loope, Rejmanek, & Westbrooks, 1997)

  • Ability to determine whether a species is native or non-­native becomes important when other components of global change, such as shifts in nutrient pools associated with widespread agriculture and changes in river flows linked to both water diversions and climate change (Foley et al, 2005), create conditions that favor proliferations of particular microorganisms

  • Based on the proposal that very low dissolved reactive phosphorus (DRP) concentrations are a primary cause of D. geminata proliferations (Bothwell et al, 2014), Taylor and Bothwell (2014) hypothesized that the range expansion of D. geminata blooms since the 1980s was largely a result of environmental change, declining DRP in rivers, or oligotrophication (Eimers, Watmough, Paterson, Dillon, & Yao, 2009; Stockner, Rydin, & Hyenstrand, 2000)

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Summary

| INTRODUCTION

Species introductions are a recognized component of human-­ mediated global change (Ricciardi, 2007; Vitousek, D’Antonio, Loope, Rejmanek, & Westbrooks, 1997). Based on the proposal that very low DRP concentrations are a primary cause of D. geminata proliferations (Bothwell et al, 2014), Taylor and Bothwell (2014) hypothesized that the range expansion of D. geminata blooms since the 1980s was largely a result of environmental change, declining DRP in rivers, or oligotrophication (Eimers, Watmough, Paterson, Dillon, & Yao, 2009; Stockner, Rydin, & Hyenstrand, 2000) This view was consistent with observations from Vancouver Island, Canada, from where there are records of D. geminata in the 1880s but no reports of proliferations until the 1980s (Bothwell et al, 2009). We used the combined environmental and molecular information, along with existing circumstantial evidence (Kilroy & Unwin, 2011), to reassess the probability of presence of D. geminata in New Zealand prior to the first discovery of proliferations in 2004

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Result
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| DISCUSSION
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