Abstract
Marine heterotrophic bacteria play a crucial role in the cycling of energy and nutrients in the ocean. Copper (Cu) belongs to the repertoire of essential trace nutrients for bacterial growth, yet physiological responses of marine heterotrophic bacteria to Cu deficiency remain unexplored. Here, we examined these responses in oceanic and coastal isolates of heterotrophic bacteria from ecologically significant microbial clades (Flavobacteriia [Bacteroidetes], Roseobacter clade [Alphaproteobacteria] and Alteromonadales [Gammaproteobacteria]). Bacterial growth, Cu quotas (Cu:P), macronutrient content and stoichiometry (cellular C, N, P, S and C:N, S:P), as well as carbon metabolism (respiration, productivity, carbon demand, growth efficiency) were monitored across a gradient of Cu conditions, characteristic of coastal and open-ocean surface waters. Cu deficiency had most severe effects on a Flavobacteriia member Dokdonia sp. strain Dokd-P16 for which we observed significant reductions in growth, C metabolism and Cu quotas. Other strains did not significantly reduce their growth rate, but adjusted their Cu content and some C metabolic rates (Ruegeria pomeroyi DSS-3, Roseobacter clade) or were unaffected (Pseudoalteromonas sp. strains PAlt-P26 and PAlt-P2, Alteromonadales clade). These diverse bacterial responses were accompanied by constant cellular composition of major elements and stoichiometric ratios. Changes in bacterial Cu quotas occurred within a modest range (~5-fold range) relative to the 50-fold variation in total Cu in the media. We hypothesize that this may reflect a well-controlled Cu homeostasis in marine heterotrophic bacteria. In a preliminary assessment, we found that Cu quotas of our bacteria and those of eukaryotic phytoplankton are not statistically different. However, compared to eukaryotic phytoplankton, the variability of Cu quotas in marine heterotrophic bacteria is smaller, which could reflect differences in their Cu homeostasis. Using Cu quotas obtained in our study, we assessed the contribution of bacterial Cu to the biogenic Cu pool in an oceanic euphotic zone in the NE Pacific. These preliminary estimates suggest that up to 50 % of the biogenic Cu could be contained in the heterotrophic bacteria biomass. Our study sheds light on the interactions between Cu and marine heterotrophic bacteria, and expands the understanding of factors influencing microbial ecology and bacterial role in Cu cycle.
Highlights
Planktonic bacteria represent most of the living biomass in the world’s oceans (Whitman et al, 1998)
We found diverse responses of bacterial growth rates and Cu quotas to changing Cu availability (Figure 1)
Lack of response in stoichiometry when growth rates are above 0.6 μ/μmax has been previously reported for freshwater bacterial isolates, for macronutrients (C, N, P, Godwin and Cotner, 2018)
Summary
Planktonic bacteria represent most of the living biomass in the world’s oceans (Whitman et al, 1998). Heterotrophic members of the bacterioplankton community play a critical role as the recyclers of organic material, influence fluxes of energy and essential elements within oceanic ecosystems. Their activity is governed by the availability of organic substrates as well as inorganic nutrients. The latter group includes bioactive metals, such as iron (Fe), copper (Cu), manganese (Mn), zinc (Zn), and cobalt (Co), that facilitate a variety of biological pathways in a prokaryotic cell. There is a paucity of information on how the availability of other essential metals regulate fundamental processes of heterotrophic bacteria, nor is it clear how these metals shape bacterial ecophysiology in the sea
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