INTRODUCTION
The soil microbiome carries out several important ecological functions, including carbon (C) and nitrogen (N) cycling and plant growth promotion (
1–3). Central to these functions are interactions between the species that comprise soil microbial communities (
4–6). While the combined genomic and metabolic potential of the individual species of the soil microbiome is vast, novel functions can emerge at the community level through metabolic interactions (
7). A better understanding of these interactions will lead to a more complete view of the constituent organism’s and community’s functional capacity and will greatly expand our knowledge of how interaction networks can be affected by nutrient or environmental shifts (
8,
9).
One of the most enigmatic microbial functions that depends on species interactions is the decomposition of soil organic matter. Identification of metabolic interactions involved in decomposition is particularly challenging due to the complexity of organic substrates in soil, the biodiversity of organisms involved, and difficulty in extracting samples at microbiological scales in soil (
10). As a result, few studies have interrogated the taxon-specific gene expression and community metabolism that occur during C decomposition in soil. Microbially driven breakdown of plant-derived matter, such as cellulose (
11,
12), is of great interest due to its ubiquity in soil environments. While the genomic potential for cellulase enzyme production has been detected in almost 40% of bacterial genomes in the Carbohydrate-Active Enzyme database, only a small number of organisms have been shown to digest cellulose independently in pure culture (
13). The challenges described above in soil have made interactions centered on breakdown of cellulose difficult to ascertain. Even less is known about the decomposition of additional abundant molecules such as chitin that contribute to both carbon and nitrogen cycling in soil (
14,
15). While chitinases, like cellulases, are widespread in bacteria (
16), their expression is not universal and is differentially controlled by different species or even within a population (
17). Previous studies using fluorescent reporter assays focused on both transcripts and proteins showed that only a subpopulation of cells in a pure culture of a chitin-degrading strain actually produce chitinases, with the remaining cells feeding off breakdown products (
18,
19). In addition, chitinases are often not cell associated, meaning breakdown products are available not only to the species expressing the chitinase but also to other species of local community as well. As such, there is a strong element of inter/intraspecies interactions centered on community metabolism of chitin and its decomposition products.
The molecular details of community interactions during chitin decomposition and the generation of breakdown products have been previously studied in some detail in non-soil environments, especially in aquatic systems (
16,
20). Chitin is the polymer of (1→4)-β-linked
N-acetyl-
d-glucosamine (NAG) monomers, and the decomposition of chitin into its NAG monomers is driven either by membrane-bound chitinases or through excreted non-cell-associated enzymes. Once converted into NAG oligomers, import and intracellular metabolism are possible and dimers are converted to monomers via β-
N-acetylglucosaminidases. Numerous species have been found that contain transporters for uptake of NAG molecules or metabolic genes that act on NAG without a corresponding set of chitin-degrading genes, suggesting that some bacteria rely on NAG produced through chitin breakdown carried out by other species in their neighborhood (
21). In supporting chitin degraders, it is possible that NAG consumers contribute to more effective chitin breakdown by removing downstream metabolites to increase enzyme efficiency (
22) or providing additional metabolic benefits such as vitamins to alleviate the energetic costs expended by chitinase producers (
23). As a result, growth promotion is driven by chitin degraders and secondary consumers through metabolic cross talk, where growth of constituents is maximized through cooperation.
Ecological theory suggests that the ability of a species to take advantage of exometabolites for growth is driven in part by the size of a species’ fundamental niche (C sources they can metabolize themselves) compared to the realized niche (C sources that can be metabolized by the complete community) (
24). A large fundamental niche indicates that species may be able to take advantage of the presence of many exometabolites independently of other species. Yet it is not clear who has an advantage during growth with chitin as the sole carbon source—chitin degraders or consumers—nor is it clear how this advantage may be related to a species’ fundamental niche size. Laboratory growth experiments have suggested that primary consumers of complex carbon sources do not have a growth advantage (
25), but whether this is a consistent rule and how this extends to field environments is not known.
Finally, the identity of chitin degraders or consumers may shift in response to community dynamics because species can express emergent properties with other species that they do not express during growth alone. For example, previous work from our group explored interactions centered on chitin breakdown by investigating a naturally evolved community of soil microbes developed using chitin as the major C and N source (
26). Analyses of this community, MSC-1 (model soil consortium-1), identified several species, primarily a species of
Rhodococcus, that occupied central positions in a 16S rRNA gene amplicon coabundance network, suggesting that they may be dominant chitin degraders and in turn provide assimilable substrates to other community members. Following isolation of specific constituents of MSC-1, subsequent coculture work revealed that several genera of this community (including
Ensifer,
Dyadobacter, and
Rhizobium grown with
Rhodococcus and
Streptomyces grown with
Ensifer) showed higher biomass when cocultured versus in monoculture. These initial studies suggest a network of interactions centered on chitin breakdown. However, there is a knowledge gap regarding the molecular details of how a community of chitin degraders and nondegraders organize themselves to break down chitin and share metabolic products.
Here, we aimed to fill these knowledge gaps by constructing and examining a new model community assembled from MSC-1 isolates, model soil consortium-2 (MSC-2). To delineate how MSC-2 degrades chitin, we used a multiomics approach combining species abundance analyses and expressed functions (metatranscriptomics) and extracellular nutrient pools (metabolomics) applied to chitin growth assays of the MSC-2 consortium as a community as well as its constituents in monoculture. We set out to answer three questions. (i) Which species have a growth advantage in a community—chitin degraders or species with large fundamental niches that can take the most advantage of chitin breakdown products? (ii) To what degree do MSC-2 members organize themselves into a chitin-degrading community, with each member contributing certain aspects of the breakdown process (cleaving of chitin polymer bonds, breakdown of NAG trimers or dimers, and processing of NAG monomers into further C and N pathways)? Finally, with an eye on native soil ecology, (iii) to what extent is the chitin decomposition phenotype of a species defined by the composition of the community in which this species grows? Answering these questions will shed light on how diverse bacterial species contribute to community decomposition and to what degree the ability to degrade organic C and/or assimilate breakdown products translates into a growth advantage in a mixed community.
DISCUSSION
The native soil microbiome is a complex community consisting of thousands of species with potentially millions of interactions between them. Because no species exists in isolation, it is these interactions that lead to the emergent properties of the soil microbiome and its role in cycling C and N substrates. Here, we sought to better understand organismal phenotypes, the roles of individual species, and how this is affected by fellow community members. By focusing on a well-defined, simplified consortium (MSC-2) that was derived from a naturally evolved soil consortium (MSC-1) (
26), we were able to investigate species-specific contributions to community metabolism, using the decomposition of chitin as our study system.
One of our major findings is that within MSC-2, chitin degradation potential (as measured by the ability to grow with chitin as the sole C source in monoculture) is not the sole or even the major determinant of how abundant (as measured by metatranscriptomic analysis and evaluating how many reads align to a given species) a member will be in the community when grown on a complex carbon source like chitin. Analysis of the fundamental and realized niches of MSC-2 members as well as the growth advantages and disadvantages of member species in a community versus axenic growth showed that ranking the species from largest to smallest fundamental niche (
Fig. 2C) aligned very well with ranking by the abundances of each species (
Fig. 4 and see
Fig. S3 in the supplemental material). For some species, we noticed a lack of abundance in MSC-2, even though the ability of these species to grow on chitin had been shown. The trade-off between the ability to grow on chitin in monoculture and abundance in the MSC-2 community is especially striking for
Sinorhizobium. Although this species can grow on chitin and expresses chitin binding genes, its relative abundance in MSC-2 was low. This contrast between chitin growth ability and community abundance (during growth on chitin) may be because the fundamental niche of
Sinorhizobium is small compared to those of other species such as
Ensifer. As a result of
Ensifer’s larger niche, while it may not drive chitin degradation, it may be able to grow on breakdown products provided by initial chitin degraders such as
Sinorhizobium. In contrast,
Sinorhizobium, with its smaller fundamental niche, is not able to take great advantage of the range of chitin breakdown products and is limited to focusing on chitin itself, which is constantly falling in concentration as the experiment proceeds and is difficult to metabolize, all of which may lead to less growth of
Sinorhizobium.
The observation that microbes with large fundamental niches may survive off chitin breakdown products opens a new question: what do these secondary consumers provide to the community in exchange for receiving breakdown products? Several possibilities emerge. First, secondary consumers may survive off C and N sources that degraders are generating but cannot metabolize themselves as has been seen with phenylalanine and
Escherichia coli (
35,
36). Alternatively, consumption of metabolites by secondary consumers may relieve stoichiometric pressure on critical enzymatic reactions of degraders, allowing for more continued degradation of chitin (
22). This may especially be the case for
Streptomyces as high levels of NAG have been shown to repress chitin breakdown in this organism (
17). Another possibility is that secondary consumers may produce important vitamin cofactors such as cobalamin. While this vitamin is critical to the soil microbiome, only a small number of bacteria and archaea produce B
12 (
23), suggesting that these B
12 producers are important to community growth even if they do not provide C or N. Our experiments here included excess B
12, but this may be the case for other vitamins or secondary metabolites that are limiting. For example, the major chitin degraders
Neorhizobium and
Streptomyces have importers for both branched-chain amino acids and xylose molecules (
Fig. 3). Gaining these from nondegraders would be energetically favorable for these species. It is important to note that these fundamental niche conclusions are possible only after defining this soil-derived consortium and building metabolic models for each individual species. Such a detailed understanding of a soil microbial consortium will help to answer several questions beyond what we show here and will allow us to begin to bridge the gap between the molecular details possible with laboratory experiments and the more complex, but translational, results from direct field analysis.
Our investigations of MSC-2 provide a deeper understanding of how species that cannot grow on complex organic carbon axenically may alter their phenotypes and contribute to decomposition in the context of other community members. For example, under the growth conditions of this experiment
Streptomyces was not able to grow in monoculture on chitin as the sole C source. This result was consistent for each of the three
Streptomyces strains that we isolated (
Fig. 1B). This lack of growth in monoculture combined with the observed high abundance of
Streptomyces within MSC-2 and our metatranscriptomic analysis suggests that
Streptomyces contributes directly toward chitin decomposition in MSC-2, but the energy limitations presented by monoculture growth on chitin prohibit enzyme production. Moving a species from an environment with labile C sources (our initial growth on R2A medium) to an environment with chitin as the only C substrate may not allow
Streptomyces, when grown in monoculture, to generate chitin-degrading enzymes.
Streptomyces may then be “stuck” with abundant chitin but not enough nutrients to allow for the initial synthesis of chitinases. We designed the experiment to account for this possibility by including a 3-day period of growth in chitin and NAG to allow for species to acclimate from richer medium (R2A) to chitin-only minimal medium. While this may have been useful for some organisms, it may have had the opposite effect on
Streptomyces as chitinase production in
Streptomyces species has been shown to be repressed by the presence of NAG (
17). However, in contrast to monoculture, in the context of the complete MSC-2 community, other species can initially degrade chitin, provide breakdown products, allow
Streptomyces to grow and make its own chitin-degrading enzymes, and contribute to chitin degradation later in the experimental timeline.
These conclusions emphasize the differences between inherent phenotypes of microorganisms in isolation (e.g., no growth of
Streptomyces on chitin in monoculture) versus the phenotypes expressed when grown as a community (e.g., growth of
Streptomyces on chitin in a community). There is an extension of this observation that is more closely related to soil ecology: that phenotypes of a species are dependent on the nature of the surrounding community. As communities are constantly shifting in soil as a function of environmental changes, testing this hypothesis further is critical for a deeper understanding of the community interactions that are at the foundation of soil microbial ecology. Emergent properties are often thought of as functions emerging from the community as a whole (
37). However, species within a community also show phenotypic properties that emerge only when they are grown with certain other species. In fact, emergent properties of individual species are likely what leads directly to emergent properties of the community as a whole. These results also emphasize the importance of examining species in both the context of other microorganisms and axenically (where possible) to fully understand their contributions to community metabolism and growth. Incorporation of species’ actions during monoculture versus community growth is also critical for applying what is learned with model communities back to the field, where no species exist in isolation and community growth is the rule. While our development of MSC-2 will help bridge the gap between laboratory and field, it should be noted that this is a community of relatively few isolates that are combined from individual strains, so the discoveries learned here may not represent the phenotypes expressed in the field. However, two aspects of our studies suggest that MSC-2 is a valuable tool for understanding soil microbial ecology. First, while MSC-2 is comprised of isolates, these isolates were drawn from a naturally evolved community derived from the complete soil microbiome (MSC-1) (
26). Members of MSC-1 (and therefore MSC-2) were chosen not by us by rather by existing interactions of soil microbiology that drove community assembly. Therefore, constituents of MSC-2 are likely to participate in interactions that are, in part, representative of processes of the native soil microbiome. Second, our use of MEMPIS in these studies allows us to apply the same methods and the same omics measurements between the lab (MSC-2) and the field (native soil microbiome). This will allow us to map processes happening in both systems and highlight where MSC-2 can be used to better understand and interpret native soil microbiome processes and where it cannot.
In summary, we describe a model chitin-degrading consortium and use multiomics analysis as well as axenic versus coculture studies to delineate the role of individual species within this consortium. Chitin-degrading members likely supported non-chitin degraders through sharing of chitin breakdown products. Because of this sharing, the main driver of a species growth and success was not the ability to carry out specific metabolic processes related to abundant C sources (chitin breakdown), but rather which species could take the most advantage of shared breakdown products. Also related to community growth, we show that the phenotype of a species, regarding its role as a primary decomposer or not, is driven by the surrounding community. The data and conclusions gathered here will be instrumental in guiding future experiments focused on combining individual constituents of MSC-2 in pairwise combinations and performing experiments in which members of MSC-2 are left out. These conclusions will also be critical to our understanding of how native soil microbiomes process soil organic C, especially substrates such as chitin that drive interactions and metabolite sharing, and how these processes may shift as community membership changes as a function of both biotic and abiotic pressures. Application of these conclusions to the native soil microbiome will greatly expand our ability to identify what the keystone species are, which may have the greatest advantage for growth, and how these communities are organized to promote C cycling in natural settings.