INTRODUCTION
Bacteria are ubiquitous living organisms with various cell shapes and sizes surrounding us in all environments (
1,
2). Soil is the most complex habitat harboring the largest diversity and density of bacteria known to date (cell densities ranging from 10
7 to 10
10 cells/g of soil) (
3–5). Soil bacteria are part of a community where they are in constant interaction with their own and other species (
6–8). Bacteria produce and release a plethora of metabolites into their environment. In this way, they not only chemically modify their niche but also affect the behavior and the secondary metabolite production of nearby bacteria (
9–11). Soil bacteria are known to produce a wide range of soluble and volatile secondary metabolites with different physicochemical and biological properties (
7,
12–14). In contrast to soluble compounds, volatile organic compounds (VOCs) are rather small molecules (<300 Da) that can diffuse easily through air- and water-filled soil pores (
15–17). These physicochemical properties make VOCs ideal metabolites for long-distance communication and interactions between soil microorganisms (
18–21).
In aquatic environments, bacteria are naturally found at lower cell densities compared to soil (10
3 to 10
6 cells/mL) (
22–24). Recent studies have shown that a significant component of aquatic microbial diversity consists of bacteria with small cell sizes of about ~0.1 μm (
25–27). However, little is known about bacteria with such cell sizes in soil environments, for instance in water-filled soil pores. There are indications that ultra-small bacteria might exist in rice paddy soils as described by Jansen (
28) as “dwarf cells” and in other soil environments (
29).
One can assume that a small cell size can be an advantage in challenging environments like soil. However, the distribution of microorganisms in soil is influenced by its water and moisture content, and a low soil moisture content leads to lower connectivity between soil pores, and thus to a lower number of accessible microhabitats.
Small bacterial cell size is often linked to a small genome size caused by genome streamlining (
30). Recent metagenomic studies suggest that genome streamlining is ubiquitous in bacteria (
31,
32). In some cases, the primary metabolism of one organism can be directly built on the primary metabolism of another organism, known as syntrophic relationships (
33,
34). The Black Queen Hypothesis states that genome-streamlined organisms have an evolutionary advantage because of the loss of genes whose function can be replaced by bacteria in the surrounding environment, effectively conserving energy (
35). Since bacteria with fewer genes have less adaptive capacity compared to bacteria with more genes, many of them are expected to depend on specific environmental conditions or on the presence of other specific organisms (
36) to produce metabolites that support their persistence.
Here, we aimed to explore if bacteria that can pass through 0.1-m filters are present in soil, and if such bacteria are cultivable. We further investigated their interaction with phylogenetically different bacteria commonly occurring in soil. The major research questions were if, and how interspecific interactions between bacteria that pass a 0.1-μm filter and other common soil bacteria that cannot pass 0.1-μm filters affected their fitness, behavior, gene expression, and the production of secondary metabolites.
DISCUSSION
Here, we report the first-time isolation of
H. gracilis from a terrestrial soil sample. This bacterium passed a 0.1-μm filter, which suggests a very small cell size, theoretically justifying referring to these bacteria as ultrasmall bacteria (
26). However, against our expectation, the microscopic analysis revealed that this bacterium is not ultrasmall in cell size but possesses a very thin diameter and showed the typical spiraled morphology known for these species (
38–41). These observations are in line with previous research by Wang et al. (
42) showing that
H. gracilis can pass through filters of various pore sizes ranging from 0.45 μm to 0.1 μm, most probably thanks to their cell shape and cell morphology.
In silico analysis of 16 terrestrial metagenome data available on MG-RAST (
https://www.mg-rast.org/) showed that
H. gracilis was not present in terrestrial metagenome data (not shown), suggesting that
H. gracilis is not commonly present in terrestrial soils. The bacterial interaction assays revealed that
H. gracilis grows better when interacting with
Paenibacillus sp. AD87 or
S. plymuthica PRI-2C. The cell numbers of
H. gracilis were higher when exposed to cell-free supernatants of
Paenibacillus sp. AD87 and
S. plymuthica PRI-2C, suggesting that the metabolites released by the latter bacteria in cocultures with
H. gracilis are associated with improved growth of
H. gracilis. We hypothesized that
H. gracilis grows better in coculture, either because growth is stimulated by signals produced by the other organism, or because the environment that is created by the other organism allows
H. gracilis to make more efficient use of certain metabolic pathways. Indeed, the metabolic experiments with Biolog plates showed that during interspecific interactions of
H. gracilis with
Paenibacillus sp. AD87 or with
S. plymuthica PRI-2C, more carbohydrates could be utilized compared to the monocultures. This is an interesting observation, and it may indicate that interaction of bacteria can trigger the production of exoenzymes, enabling the degradation of carbohydrates, which the bacteria were not able to degrade in monoculture.
We speculated that since
H. gracilis grows better in interaction with other bacteria and is of relatively small cell size,
H. gracilis might have evolved according to a genome streamlining strategy, i.e., the adaptive loss of genes for which functions it relies on interaction with other bacteria in the immediate environment. The whole-genome sequencing of
H. gracilis revealed a genome size of 3.82 Mbp. This is a relatively small genome size for free-living soil bacteria that typically have estimated average genome sizes of ~4.7 Mbp (
36,
43–46). The
in silico antiSMASH (
37) comparison of genes that are part of secondary metabolite gene clusters showed that the
H. gracilis genome contained only three gene clusters encoding the production of secondary metabolites (bacteriocins, terpenes, and aryl polyenes). Terpenes and aryl polyenes are known as protective compounds against abiotic stressors, while bacteriocins have antimicrobial activities against closely related bacteria (
17,
47–51). We hypothesize that
H. gracilis genome streamlining has allowed it to be more competitive, by retaining only the most essential metabolic functions while having roughly about one quarter less DNA to replicate during each cell division. Gene loss and reduced genome size may cause dependency on other microbes in their surroundings, and this may explain a considerable part of the phenomenon that most of the detectable bacteria in the environment are not cultivable under laboratory conditions.
To investigate the mechanisms of interaction, we performed transcriptome analysis on the interaction pairs of
H. gracilis with
S. plymuthica PRI-2C and
Paenibacillus sp. AD87. Interestingly, a larger amount of significantly differentially expressed genes was induced by
H. gracilis in the other two competing bacteria compared to the transcriptomic changes in
H. gracilis. Several processes, enriched according to GO term enrichment analysis, could be part of a mechanism(s) mediating interactions between
H. gracilis and
S. plymuthica PRI-2C and
Paenibacillus sp. AD87, for example genes related to chemotaxis. Moreover, the GO terms for signal transduction, secondary metabolite production, and cell motility were enriched in the transcriptome of
H. gracilis during the cocultivation with
Paenibacillus sp. AD87, suggesting that chemotaxis and cell movement is an important feature during interspecific interactions between these two bacterial taxa (
52,
53). In addition, GO terms referring to iron-sulfur (Fe-S) complex assembly were enriched in the transcriptomes of
H. gracilis during the cocultivation with
S. plymuthica PRI-2C and
Paenibacillus sp. AD87. Fe-S clusters are important for sustaining fundamental life processes: they participate in electron transfer, substrate binding/activation, iron or sulfur storage, regulation of gene expression, and enzyme activity (
54,
55). This upregulation could indicate that, potentially, in coculture, normal-sized bacteria released metabolites that
H. gracilis used for synthesizing Fe-S complexes. It is also possible that iron-sulfur complex assembly is activated during competition with the interacting bacteria for sulfur or iron collection (scavenging) (
56–59).
The metabolic pathway analysis showed that the loss of genes in
H. gracilis does not appear to have resulted in functional loss of metabolic pathways. Loss of nonessential and possibly redundant genes in several metabolic pathways could explain why and how the genome of
H. gracilis has become so small. The missing genes are not essential to complete metabolic pathways and only appear to result in limited options in certain metabolic pathways. RAST analysis showed that all basal metabolic pathways remain feasible with the annotated enzymes and pathways of
H. gracilis. The only exception is EC term 5.2.1.1 (maleate isomerase). There are several ways to synthesize fumarate, e.g., in the glycolysis pathway (
41,
60,
61) and in the citric acid cycle (
41,
62). Based on the available data, it cannot be unambiguously determined which alternative pathway may preferably be used by
H. gracilis to synthesize fumarate.
The metabolomics analysis revealed the production of specific antimicrobial compounds such as pyrollnitrin (
S. plymuthica PRI-2C) and 2,5-bis(1-methylethyl)-pyrazine (
Paenibacillus sp. AD87) which are well known for their broad-spectrum antimicrobial activity (
63–67). However, the produced antimicrobial compounds didn’t show activity against
H. gracilis: in both interactions,
H. gracilis showed increased growth when growing in coculture with either
Paenibacillus sp. AD87 or
S. plymuthica PRI-2C.
The understanding of natural metabolites that mediate interactions between organisms in natural environments is the key to elucidate ecosystem functioning. The detection and identification of the compounds that mediate such interactions is still challenging. Techniques such as mass spectrometry imaging (MSI) provide new opportunities to study environmentally relevant metabolites in their spatial context (
68–70). In this study, the metabolomics was performed using three independent approaches namely, DART-MS analysis, GC/MS-Q-TOF analysis and LAESI-MSI from living bacterial colonies. LAESI-MSI analysis revealed that several mass features were detected in higher abundance during the cocultivation of
H. gracilis with
Paenibacillus sp. AD87, these mass features were
m/z 425.2886 and
m/z 558.2832. LAESI-MSI is not suitable for unambiguous compound annotation, but can still be used for putative compound annotation. To annotate the detected mass features to compounds with high certainty, LAESI-MSI should be coupled with ion mobility separation as previously suggested (
71–73). Yet, LAESI-MSI can help to spatially distinguish the produced secondary metabolites of living bacterial colonies with limited sample preparation and can give insight into the spatial distribution of metabolites.
Several studies indicate that the volatile blend composition of the volatiles greatly depends on biotic interactions and on growth conditions (
15,
19,
74–76). Here, a higher number of volatile compounds were detected in the bacterial cocultures, most likely due to the combination of emitted volatiles of the interacting bacteria. The high number of sulfur-containing compounds indicates that these compounds are commonly produced by bacteria and might play an important role in signaling during interspecific interactions (
77,
78). No novel volatile compounds were detected during the coculture of the three bacteria.
Overall, our study showed that H. gracilis can pass through a 0.1-μm filter and is present in terrestrial environments. The growth performance and physiological behavior of H. gracilis were dependent on the cocultivated bacterial partner and they might be metabolically depending on the cocultivated bacteria. At the same time, H. gracilis was able to change the physiology, release of volatile organic compounds, and secreted enzymes of the cocultivated bacteria without direct cell-cell contact.
Microbial interspecific interactions play an important role in the functioning of the terrestrial ecosystem. Soil microbial communities are very diverse and dynamic and involve frequent and sporadic interspecific interactions. Our study indicates that sulfur and Fe-S clusters could play an important role in microbial interspecific interactions in terrestrial environments and more studies are required to understand their role. The study of sporadic interspecific interactions and the inclusion of rare taxa in future analysis could help to better understand microbial communities and functions of those.
ACKNOWLEDGMENTS
This work was financially supported by the Netherlands Organization for Scientific Research (NWO) VIDI personal grant 864.11.015 granted to P.G.
The authors thank the students of the WUR bioinformatics course BIF-51806 (2018) for their input and primary data analysis and discussions on the data. Additionally, the authors thank the two anonymous reviewers for their critical comments and suggestions for improvement of the manuscript.
O.T. and P.G. designed the experiments. O.T., A.O., P.K., and W.I.J. performed the lab experiments. O.T. and P.K. and performed the data analysis and prepared the figures and tables. O.T., P.K., A.O., V.T., M.H.M., P.B., K.J.F.V., and P.G. wrote the manuscript. All authors read and critically revised the manuscript.
We declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.