RESUMEN
Terrestrial ecosystems are becoming increasingly nitrogen-saturated due to anthropogenic activities, such as agricultural loading with artificial fertilizer. Thus, more and more reactive nitrogen is entering streams and rivers, primarily as nitrate, where it is eventually transported towards the coastal zone. The assimilation of nitrate by coastal phytoplankton and its conversion into organic matter is an important feature of the aquatic nitrogen cycle. Dissolved reactive nitrogen is converted into a particulate form, which eventually undergoes nitrogen removal via microbial denitrification. High and unbalanced nitrate loads to the coastal zone may alter planktonic nitrate assimilation efficiency, due to the narrow stochiometric requirements for nutrients typically shown by these organisms. This implies a cascade of changes for the cycling of other elements, such as carbon, with unknown consequences at the ecosystem level. Here, we report that the nitrate removal efficiency (NRE) of a natural phytoplankton community decreased under high, unbalanced nitrate loads, due to the enhanced recycling of organic nitrogen and subsequent production and microbial transformation of excess ammonium. NRE was inversely correlated with the amount of nitrate present, and mechanistically controlled by dissolved organic nitrogen (DON), and organic carbon (Corg) availability. These findings have important implications for the management of nutrient runoff to coastal zones.
Asunto(s)
Ecosistema , Eutrofización , Nitratos/metabolismo , Agua de Mar/química , Agua de Mar/microbiología , Microbiología del Agua , Compuestos de Amonio/metabolismo , Archaea/metabolismo , Carbono/metabolismo , Modelos Lineales , Nitrógeno/metabolismo , Ciclo del Nitrógeno , Isótopos de Nitrógeno/química , Oxidación-Reducción , Fitoplancton/metabolismo , Ríos/químicaRESUMEN
As the atmospheric CO(2) concentration rises, more CO(2) will dissolve in the oceans, leading to a reduction in pH. Effects of ocean acidification on bacterial communities have mainly been studied in biologically complex systems, in which indirect effects, mediated through food web interactions, come into play. These approaches come close to nature but suffer from low replication and neglect seasonality. To comprehensively investigate direct pH effects, we conducted highly-replicated laboratory acidification experiments with the natural bacterial community from Helgoland Roads (North Sea). Seasonal variability was accounted for by repeating the experiment four times (spring, summer, autumn, winter). Three dilution approaches were used to select for different ecological strategies, i.e. fast-growing or low-nutrient adapted bacteria. The pH levels investigated were in situ seawater pH (8.15-8.22), pH 7.82 and pH 7.67, representing the present-day situation and two acidification scenarios projected for the North Sea for the year 2100. In all seasons, both automated ribosomal intergenic spacer analysis and 16S ribosomal amplicon pyrosequencing revealed pH-dependent community shifts for two of the dilution approaches. Bacteria susceptible to changes in pH were different members of Gammaproteobacteria, Flavobacteriaceae, Rhodobacteraceae, Campylobacteraceae and further less abundant groups. Their specific response to reduced pH was often context-dependent. Bacterial abundance was not influenced by pH. Our findings suggest that already moderate changes in pH have the potential to cause compositional shifts, depending on the community assembly and environmental factors. By identifying pH-susceptible groups, this study provides insights for more directed, in-depth community analyses in large-scale and long-term experiments.
Asunto(s)
Agua de Mar/microbiología , Microbiología del Agua , Ecosistema , Flavobacteriaceae/genética , Flavobacteriaceae/fisiología , Gammaproteobacteria/genética , Gammaproteobacteria/fisiología , Concentración de Iones de Hidrógeno , Mar del Norte , ARN Ribosómico 16S/genética , Rhodobacteraceae/genética , Rhodobacteraceae/fisiología , Estaciones del AñoRESUMEN
We present a new procedure for effectively detaching particle-associated bacteria by 10% (v/v) methanol and sonication which is particularly suitable for samples with a high particle load and sediments. We also optimized the sample preparation by applying the highly dsDNA-specific fluorescent stain SybrGreen I together with an optically brilliant mounting medium (polyvinylalcohol 4-88, 'moviol') in one step. The new protocol allows a much faster, easy and less toxic handling of samples as compared to other methods. Cells are stained directly on a black Nuclepore filter and show an intensive fluorescence signal with low background. The detachment procedure was optimized with respect to the temperature of the 10% methanol solution (35 degrees C), ultrasonication and centrifugation. The application of the new method in comparison with detachment procedures with pyrophosphate and Tween-80 with various types of marine samples including sediments always yielded higher numbers and/or higher fractions of particle-associated cells. Staining and mounting the samples with the moviol-SybrGreen I solution allowed an accurate and highly reproduceable enumeration of bacteria also in samples with high concentrations of SPM. Fixation of bacteria by glutardialdehyde resulted in a brighter fluorescence as compared to fixation by formalin. Because of the high specificity to dsDNA and bright fluorescence of SybrGreen I, the fast and easy handling and the possibility to store stained samples for at least several months at -20 degrees C without any loss in fluorescence intensity, the newly developed method is also an attractive alternative to DAPI staining of aquatic bacteria.