Abstract

Cobalamin (vitamin B12) is an essential enzyme cofactor for most branches of life. Despite the potential importance of this cofactor for soil microbial communities, the producers and consumers of cobalamin in terrestrial environments are still unknown. Here we provide the first metagenome-based assessment of soil cobalamin-producing bacteria and archaea, quantifying and classifying genes encoding proteins for cobalamin biosynthesis, transport, remodeling, and dependency in 155 soil metagenomes with profile hidden Markov models. We also measured several forms of cobalamin (CN-, Me-, OH-, Ado-B12) and the cobalamin lower ligand (5,6-dimethylbenzimidazole; DMB) in 40 diverse soil samples. Metagenomic analysis revealed that less than 10% of soil bacteria and archaea encode the genetic potential for de novo synthesis of this important enzyme cofactor. Predominant soil cobalamin producers were associated with the Proteobacteria, Actinobacteria, Firmicutes, Nitrospirae, and Thaumarchaeota. In contrast, a much larger proportion of abundant soil genera lacked cobalamin synthesis genes and instead were associated with gene sequences encoding cobalamin transport and cobalamin-dependent enzymes. The enrichment of DMB and corresponding DMB synthesis genes, relative to corrin ring synthesis genes, suggests an important role for cobalamin remodelers in terrestrial habitats. Together, our results indicate that microbial cobalamin production and repair serve as keystone functions that are significantly correlated with microbial community size, diversity, and biogeochemistry of terrestrial ecosystems.

Highlights

  • Supplementary information The online version of this article contains supplementary material, which is available to authorized users.Cobalamin, once referred to as “nature’s most beautiful cofactor” [1], plays an important role as a coenzyme involved in the synthesis of nucleotides and amino acids, in addition to carbon processing and gene regulation within all domains of life [2, 3]

  • Sequences affiliated with the Proteobacteria phylum dominated the genetic potential to produce cobalamin, contributing 45.9% of cobalamin biosynthesis genes across all soil metagenomes, followed by Actinobacteria (24.9%), Firmicutes (6.2%), Acidobacteria (5.1%), and Thaumarchaeota (2.9%) (Fig. 2a)

  • Soil type influenced the composition of potential cobalaminproducing taxa, and cobalamin biosynthesis gene relative abundance from each major potential cobalamin-producing phylum (Proteobacteria, Actinobacteria, Firmicutes, Acidobacteria, and Thaumarchaeota) varied significantly among different soil types (ANOVA; p < 0.01; Fig. S1)

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Summary

Introduction

Despite widespread metabolic dependency on cobalamin, only a relatively small subset of bacteria and archaea are capable of its production [4,5,6]. Cobalamin is present across natural systems in several chemical forms that differ in their upper ligand, including the enzymatically active forms of adenosylcobalamin (Ado-B12), methylcobalamin (Me-B12), hydroxocobalamin (OH-B12), and the inactivated form cyanocobalamin (CN-B12), of which the upper ligands are interchangeable through both enzymatic and abiotic processes [4, 7]. Cobalamin biosynthesis requires more than 30 enzymatic steps, via aerobic or anaerobic pathways [8,9,10] (Fig. 1), and represents a high genomic and metabolic burden for microbial producers. Previous research on cobalamin production and its environmental significance has focused on marine systems

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