Abstract

To determine the adapted microbial populations to variant dissolved organic carbon (DOC) sources in the marine environment and improve the understanding of the interaction between microorganisms and marine DOC pool, field-based incubation experiments were carried out using supplemental 13C-labeled typical substrates D-glucose and D-glucosamine (D-Glc and D-GlcN, respectively), which are two important components in marine DOC pool in the South China Sea. 13C- and 12C-DNA were then fractionated by ultracentrifugation and the microbial community was analyzed by terminal-restriction fragment length polymorphism and 454 pyrosequencing of 16S rRNA gene. 12C-DNA-based communities showed relatively high similarities with their corresponding in situ communities, and their bacterial diversities were generally higher than 13C-DNA-based counterparts. Distinct differences in community composition were found between 13C- and 12C-DNA-based communities and between two substrate-supplemented 13C-DNA-based communities; these differences distinctly varied with depth and site. In most cases, there were more genera with relative abundances of >0.1% in D-Glc-incorporating communities than in D-GlcN-incorporating communities. The Roseobacter clade was one of the prominent actively substrate-incorporating bacterial populations in all 13C-DNA-based communities. Vibrio was another prominent actively D-GlcN-incorporating bacterial population in most incubations. However notably, different OTUs dominated this clade or genus in different treatments at different depths. Altogether, these results suggested that there were taxa-specific differences in DOC assimilations and, moreover, their differences varied among the typical water masses, which could have been caused by the variant compositions of original bacterial communities from different hydrological environments. This implies that ecologically, the levels of labile or recalcitrance of DOC can be maintained only in a specific environmental context with specific bacterial community composition.

Highlights

  • Heterotrophic bacteria function as a driving force of ocean carbon cycling, by incorporating, respiring, and transforming various organic substrates supplied into the ocean

  • SAR11 can use dimethylsulfoniopropionate but prefers amino acids [6, 7]; aerobic anoxygenic phototrophic bacteria (AAPB) selectively take up Dissolved organic carbon (DOC) generated by phytoplankton [8]; and the Archaea, widely distributed in the deep sea, are proficient in typical deep sea DOC metabolism, such as D-amino acid [9]

  • Bacterial Community Composition Based on terminal-restriction fragment length polymorphism (T-RFLP) Fingerprinting

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Summary

Introduction

Heterotrophic bacteria function as a driving force of ocean carbon cycling, by incorporating, respiring, and transforming various organic substrates supplied into the ocean. SAR11 can use dimethylsulfoniopropionate but prefers amino acids [6, 7]; aerobic anoxygenic phototrophic bacteria (AAPB) selectively take up DOC generated by phytoplankton [8]; and the Archaea, widely distributed in the deep sea, are proficient in typical deep sea DOC metabolism, such as D-amino acid [9]. Such specificity in incorporation of DOC by prokaryotic populations suggests that socalled “labile” substrates are available to some microbes but might be recalcitrant or difficult to metabolize for others [10]. The identity of microbial populations adapted to different DOCs among different water messes will improve the understanding of the interaction between microorganisms and the marine DOC pool

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