Abstract

The functioning of microbial ecosystems has important consequences from global climate to human health, but quantitative mechanistic understanding remains elusive. The components of microbial ecosystems can now be observed at high resolution, but interactions still have to be inferred e.g., a time-series may show a bloom of bacteria X followed by virus Y suggesting they interact. Existing inference approaches are mostly empirical, like correlation networks, which are not mechanistically constrained and do not provide quantitative mass fluxes, and thus have limited utility. We developed an inference method, where a mechanistic model with hundreds of species and thousands of parameters is calibrated to time series data. The large scale, nonlinearity and feedbacks pose a challenging optimization problem, which is overcome using a novel procedure that mimics natural speciation or diversification e.g., stepwise increase of bacteria species. The method allows for curation using species-level information from e.g., physiological experiments or genome sequences. The product is a mass-balancing, mechanistically-constrained, quantitative representation of the ecosystem. We apply the method to characterize phytoplankton—heterotrophic bacteria interactions via dissolved organic matter in a marine system. The resulting model predicts quantitative fluxes for each interaction and time point (e.g., 0.16 µmolC/L/d of chrysolaminarin to Polaribacter on April 16, 2009). At the system level, the flux network shows a strong correlation between the abundance of bacteria species and their carbon flux during blooms, with copiotrophs being relatively more important than oligotrophs. However, oligotrophs, like SAR11, are unexpectedly high carbon processors for weeks into blooms, due to their higher biomass. The fraction of exudates (vs. grazing/death products) in the DOM pool decreases during blooms, and they are preferentially consumed by oligotrophs. In addition, functional similarity of phytoplankton i.e., what they produce, decouples their association with heterotrophs. The methodology is applicable to other microbial ecosystems, like human microbiome or wastewater treatment plants.

Highlights

  • Microbes are members and affect the functioning of many ecosystems, from the human gut to the global ocean, with important implications for health and climate

  • Also, our results suggest that phytoplankton are functionally similar in terms of what organic carbon species they produce, and that this decouples them from bacteria

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Summary

Introduction

Microbes are members and affect the functioning of many ecosystems, from the human gut to the global ocean, with important implications for health and climate. Past approaches to infer interactions from microbial time series data have been mostly empirical, including principal component analysis (PCA), non-metric multidimensional scaling (NMDS), empirical dynamic modeling (EDM) and various regression and correlation analyses [1,2,3, 8,9,10,11]. Past examples include phage—cyanobacteria genotypes [2], DOM species—bacteria genotypes [1], ciliate morphotypes—phytoplankton genera [12], and lake bacteria phytoplankton—environmental factor [10] interactions These empirical methods can point to possible interactions, but results can be difficult to interpret mechanistically (e.g., virus-virus interaction) and are not quantitative (e.g., do not provide carbon flux between species). These shortcomings limit the utility of empirical methods to develop a quantitative mechanistic understanding of microbial ecosystems

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