Introduction

Contemporary microbial ecology studies use one or several ‘omics’ approaches to gain a deeper insight into the structure and function of microbial communities. Among these approaches, metaproteomics provides the direct link between genetic potential and actual functionality of the community. In recent years, a number of authors reviewed the steadily increasing number of metaproteomic studies and the ongoing technical progress, and almost all concluded that there is a need for quantitative input of metaproteomic studies (Keller and Hettich, 2009; Wilmes and Bond, 2009; Verberkmoes et al., 2009a; Schneider and Riedel, 2010). The rationale behind this is the often found redundancy of functionalities in complex communities, requiring quantitative data to decide which species is mainly responsible for some metabolic functions. Quantitation can be achieved by employing label-free approaches (Old et al., 2005; Neilson et al., 2011), chemical labeling such as isobaric tags (iTRAQ, TMT) (Thompson et al., 2003; Ong and Mann, 2005) or dynamic incorporation of stable isotopes into proteins based on metabolic activity (Ong et al., 2003; Beynon and Pratt, 2005; Jehmlich et al., 2008b). The incorporation of heavy isotopes, for example, 13C, in proteins can be detected on peptide level using a protein-stable isotope probing (protein-SIP) approach (Jehmlich et al., 2008b) and poses an additional way to unravel functionalities in relation to some specific processes such as hydrocarbon metabolism or degradation of organic xenobiotics. Diverse quantification methods were previously performed for pure cultures, but only label-free and metabolic labeling approaches were adopted for metaproteomic studies, and thus we will focus on them in the following sections.

Label-free approaches

Label-free quantitation has been frequently used to study natural communities and reliable results depend on standardized and reproducible liquid chromatography (LC) conditions (Neilson et al., 2011). Quantitation was performed using either signal intensity (area under the curve, AUC) or the number of fragmentation spectra (spectral counts, SC) (for review, see Neilson et al. (2011)). The AUC method is based on the detection of peptide ion abundances at specific retention times within given detection limits (Podwojski et al., 2010). In the SC quantitation, the numbers of identified fragment ion spectra per protein are counted, and calculation is based on the assumption that the number of fragment spectra for a peptide correlates with its abundance (Liu et al., 2004). This approach may lead to an overestimation of proteins of high molecular weight and peptide intensities. However, SC is recently becoming a common method for quantitative metaproteomic studies, as it is easy to implement for one-dimensional and two-dimensional proteomic data sets: Delmotte et al. (2009) used SC to roughly estimate protein abundances of 2257 proteins from phyllosphere microbiota, and Morris et al. (2010) evaluated the abundance of 2273 membrane proteins from microbial and viral communities of South Atlantic surface waters. The quantitation allowed them to clearly allocate molecular functions to specific phylotypes, which would not have been possible based on solely metagenome data. An improved SC approach is the normalized spectral abundance factor (NSAF), which considers the length of the quantified protein (Zybailov et al., 2007). The NSAF was used to analyze an acidophilic biofilm describing specific protein functions and ecological behaviors (Denef et al., 2010; Mueller et al., 2010; Jiao et al., 2011). Jiao et al. (2011) revealed that the abundance of 20 proteins account for more then the half of the 1351 identified proteins. The relative abundance of 6296 proteins from 28 biofilm samples were analyzed by hierarchical clustering and nonmetric multi dimensional scaling (Mueller et al., 2010). The NSAF of proteins within large multivariate data sets were compared and changes in the proteome of high and low abundant bacteria were discussed regarding the inhabiting biogeochemical zones. Microbial populations within distinct layers of a lake were investigated by Lauro et al. (2011) to compare 1824 proteins regarding their spatial distribution, and Schneider et al. (2012) studied the functionalities and microbial dynamics of litter degradation. Again, quantitation was the key for understanding the contribution of community members to the observed systemic activity. Recently, NSAF values were used to compare the effectiveness of different methods for the extraction of soil proteins (Keiblinger et al., 2012). Signal intensity measurements or AUC have been rarely used in metaproteomic studies, as they require highly reproducible chromatographic runs and are not very amenable to highly fractionated samples before LC-MS/MS (Neilson et al., 2011). A metaproteomic study described the biostimulation of an uranium-reducing aquifer community (Callister et al., 2010). They detected the shift of protein abundances by the AUC method in microbial consortia originating from different groundwater wells temporarily stimulated with a supply of acetate and were capable to allocate them to selected species. The effect of biostimulation of naphthalene-degrading enrichment cultures was described by Guazzaroni et al. (2013). Protein abundances of the cultures with or without a prior biostimulation showed a broad metabolic activity of the first one and specialized naphthalene degradation potential for the latter.

In the recent years, the identification and quantification of proteins in the gut microbiota became a hot topic in microbial ecology. The human gut microbiota was investigated starting by a 2-DE study (Klaassens et al., 2007), where a time-resolved analysis of protein spot changes was applied. Further on, gut microbiota studies were performed using 1-DE or label-free proteomic approaches. At first, Verberkmoes et al. (2009b) published an analysis employing relative protein abundances (normalized spectral) for a comparison of two fecal samples and two distinct sequence databases. Cantarel et al. (2011) used the same samples to test several computational strategies to improve protein identification. A new iterative workflow for protein identification leads to an increase of Clusters of Orthologous Groups (COG) categories (Rooijers et al., 2011). Special emphasis has been placed on the role of the gut microbiota for metabolic syndromes, inflammation and obesity. Therefore, feces of obese and lean adolescents were comparatively investigated with the results that a core proteome of 505 proteins with equal abundance was identified (counted by AUC) (Ferrer et al., 2013). Differences in the gene and protein composition between healthy and Crohn’s disease twin pairs were studied by metagenomic and metaproteomic analysis (Erickson et al., 2012). Besides protein identification and quantitation, clear differences between noninflammation and inflammation in the ileum were observed. Furthermore, the alteration of the microbiota during an antibiotic treatment was studied in a multi-omics approach (Peréz-Cobas et al., 2012). Besides metagenomics, metatranscriptomics and metametabolomics, a comprehensive analysis of the metaproteome was performed. Microbial populations showed oscillatory changes during the therapy, indicating an alteration of the gut microbiota and the strong interaction with the host. Feces analyses revealed only limited insight to the interface between host and microbiota. Thus, two studies focussed on the mucosa-associated microbiota in human and rats (Li et al., 2011; Haange et al., 2012). Representative, Haange et al. (2012) showed phylogenetic and functional differences along the intestinal tract (mucosa and gut content) of rats. The above-mentioned studies showed that metaproteomics goes clearly beyond mere identification because it allows functional classification and abundance correlation with consortia members.

Metabolic labeling

Besides label-free quantitation, protein abundances and expression patterns can be calculated by labeling strategies. Chemical labeling uses tags that are added after the cultivation; metabolic labeling uses the metabolic activity of the organisms to incorporate stable isotopes. In contrast to chemical labeling approaches, metabolic labeling techniques lead to the incorporation of the quantitation markers within the culture and thereby avoid artefacts from processing or chemical reactions. The most common approach for eukaryotes is stable isotope labeling with amino acids in cell culture (SILAC). There, isotope-labeled arginine and/or lysine are supplied and hence incorporated into the proteins during cultivation. After trypsin cleavage, they constitute the C-terminal amino acid and lead to at least one labeled amino acid per peptide. Combination of peptides and concomitant MS measurement allow the relative quantification of an unlabeled to a labeled sample in one measurement, hence avoiding any variability based on slight day-to-day differences in LC-MS/MS analysis. Despite being usually applied to organisms auxotrophic for arginine/lysine, the technique has also been used successfully for nematodes (Larance et al., 2011) and bacteria such as Staphylococcus aureus (Schmidt et al., 2010), which, although not being auxotrophic, were opportunistic enough to prefer the supplemented amino acids for peptide biosynthesis. Instead of amino acids, isotopically labeled substrates or nutrients can be applied that lead to a defined relative isotope abundance (RIA) in the biomass. Peptides derived from these experiments can then be mixed with a control and quantified on the basis of peak intensities of labeled and non-labeled peptide signals. This method has been described using 15N (Snijders et al., 2005; Pan et al., 2011) and also 36S (Jehmlich et al., 2012). The incorporation of stable isotopes into proteins by metabolic labeling can be used to quantify protein abundances and to observe changes in the microbial community structure. For static comparisons, 15N was used as an isotopic metabolic label to detect proteome changes of an acidophilic biofilm (Belnap et al., 2010, 2011; Mueller et al., 2011). The community of interest was grown in the presence of 15N-labeled medium to enable a >95% 15N labeling of the proteins. It was first used to prove that laboratory cultures are comparable to natural samples and further to show a differentiation of the metaproteome after cultivation of the biofilm in a pH range of 0.85–1.45 (Belnap et al., 2010, 2011). The spatial and temporal succession of the biofilm was studied using the 15N-labeling approach (Mueller et al., 2011). Beside the sole description of community structure, the analysis of functionalities allocated to the various members of the community is of particular interest. This requires more detailed information about isotope label distribution than accessible by mere quantitative metaproteomics. Protein-SIP is a method likely able to provide this additional information.

Features of protein-SIP to simultaneously detect metabolic activity and phylogeny

Protein-SIP is based on the metabolic incorporation of isotopically labeled substrates, where 13C, 15N or 36S can be used (Jehmlich et al., 2008a, 2008b, 2012). The metabolism of the labeled substrates leads to assimilation of heavy isotopes and subsequent incorporation into the various classes of biomolecules, including proteins and can be detected by mass spectrometry of peptides as reviewed in Seifert et al. (2012). The amount of atoms replaced by their heavy isotopes changes the natural isotope composition and is defined as the RIA. The RIA can be determined by LC-MS/MS analysis at the peptide level (Table 1). The calculation of the RIA is either done by analysis of the distribution of different isotope patterns of the peptides or based on features of the peptide mass such as the relation of the parent mass to the first two digits (Jehmlich et al., 2008b; Fetzer et al., 2010; Jehmlich et al., 2010; Taubert et al., 2011a). For the first approach, the amino-acid sequence of the peptide is needed to calculate the elemental composition and the theoretical mass, thus this approach requires suitable sequence information. The calculation of the RIA includes the whole isotope pattern, which allows a highly accurate calculation of the RIA; enabling differentiation of deviations down to 0.1% with only 10 peptides (Taubert et al., 2011a). The second approach, called half decimal place rule, is sequence independent and the RIA calculation is based on the first two digits of the peptide mass. The major disadvantage of this method is the requirement of at least 40 peptides with equal RIA to achieve accuracy below 10% deviation (Jehmlich et al., 2010). Besides the amount of heavy isotopes within the molecules, the ratio between labeled and unlabeled molecules also contains valuable information. The ‘labeling ratio’ (LR) is based on the intensity ratio of the respective peptide MS signals (Table 1). The assessment of the LR allows, for example, the quantitation of protein biosynthesis as shown in a time series study by Taubert et al. (2011b), where protein induction by substrate shift was analyzed. Another valuable feature of protein-SIP is the possibility to detect differences in substrate usage by analysis of the shapes of isotope patterns in peptides. Direct metabolisation of isotopically labeled substrates leads to an isotope pattern closely resembling a normal distribution (Table 1), whereas cross-feeding, that is, usage of labeled intermediates from degradation processes accumulating in culture, result in tailed distributions. Hence, the incorporation of isotopes into proteins of different groups of microorganisms can be used to track carbon fluxes within the studied consortia. The corresponding phylogenetic resolution depends on the available (meta-)genome sequences, the diversity of the phyla and the detection of valuable phylogenetic marker proteins such as chaperonin, ATPases and ribosomal proteins (Taubert et al., 2012).

Table 1 Numerical parameters (RIA, LR) and features (shape) of protein-SIP posing carbon and nitrogen fluxes in microbial communities.

Applications of protein-SIP in microbial ecology

The suitability of protein-SIP to detect key metabolic players within a community was first shown using a defined nitrate-reducing artificial mixed culture of the toluene-degrading Aromatoleum aromaticum EbN1 and a gluconate-degrading enrichment culture not able to use toluene as substrate (Jehmlich et al., 2008b). The mixed culture was fed with 13C-labeled toluene and 12C-gluconate as carbon sources. Although all members of the consortium grew under these conditions, 13C-labeled proteins were exclusively assigned to strain EbN1, demonstrating the suitability of protein-SIP to detect and identify 13C-labeled proteins in a mixed culture. Protein-SIP was further established as a suitable method to trace the carbon flux between a heterotrophic and an autotrophic bacterial species by Kermer et al. (2012). In the course of the labeling experiments, the development of the RIA and the LR of peptides revealed that a carbon transfer occurred when CO2 formed by heterotrophic metabolism was used by the autotrophic species as a carbon source (Figure 1). The mass shifts of the peptides caused by the alternating incorporation of 13C are depicted as colored isotopologue patterns in Figure 1. Protein-SIP applications in more complex cultures and environmental samples were conducted first in a study on a MTBE-degrading culture (Bastida et al., 2010). The microbial community structure was analyzed after growth on 13C-MTBE revealing that proteins related to members of the Comamonadaceae family were not 13C-labeled, whereas proteins related to Methylibium petroleiphilum PM1 showed an average 13C RIA of 94.5 atom% 13C. In this study, the phylogenetic information retrieved from proteins correlated well with the structure of the microbial community established by 16S rRNA gene libraries. In further studies, a relationship between RNA-SIP and protein-SIP data was published by Jechalke et al. (2013). The active fraction of an aerobic benzene-degrading microbial community was identified as members of Beta- and Gammaproteobacteria with RIAs of about 90 atom% 13C. The detection of 13C-labeled proteins related to toluene dioxygenase and catechol 2,3-dioxygenase suggested benzene degradation by a dihydroxylation pathway with subsequent meta-cleavage of the catechol formed. Recently, protein-SIP was used to characterize the functionality of a sulfate-reducing community with m-xylene as the sole source of carbon and energy (Bozinovski et al., 2012). Out of the 331 identified proteins, 23% were not 13C-labeled, whereas 77% showed an incorporation of 19–22 atom% 13C. 13C-labeled proteins were involved in anaerobic m-xylene biodegradation, in sulfate reduction, in the Wood–Ljungdahl pathway and in general house-keeping processes. Thirty-eight percent of the labeled proteins were affiliated to Deltaproteobacteria, which suggests a key role of this group in the assimilation of m-xylene. Morris et al. (2012) studied the carbon flow in an anaerobic hydrocarbon degrading consortium. The methanogenic culture was incubated either with an oil-containing or an oil-free solid matrix and amended with either 13C-labeled n-fatty acid or n-alkane. Proteins were identified with an in silico-created metagenome consisting of public genomes of sulfate-reducing species, fatty acid-metabolizing species and methanogenic archaea. Beside yielding different 13C RIAs of the metabolic groups, depending on the used substrate and solid matrix, protein-SIP allowed a differentiation of direct and indirect carbon utilization based on peptides’ isotope patterns (Table 1). The authors posed that peptides belonging to Methanoculleus marisnigri, which metabolizes CO2 and other C1 substrates, showed patterns typical for consumption of degradation products of a labeled substrate, while peptides from Methanosaeta thermophila, an acetoclastic methanogen, showed distributions resembling a direct usage of the labeled substrates. The results indicated that methanogenesis in this consortium was driven by acetate metabolisation and only secondary by hydrogenotrophic CO2 reduction. The carbon flow in a sulfate-reducing, benzene-degrading community was recently studied (Taubert et al., 2012). The anaerobic aquifer community was set up either using 13C-labeled benzene and 12C carbonate or 12C benzene and 13C-labeled carbonate. Up to five samples were investigated over 300 days per experiment. According to the development of the RIA and the LR over time, three distinct groups of proteins could be defined, based on MS identifications from metagenomic sequences, thus underlining the importance of following a time course in protein-SIP experiments (Figure 2). Phylogenetic affiliation was performed by BLASTP-based annotation of the respective metagenome contigs. The metagenome was employed to identify proteins and the labeling experiment resulted in a reconstruction of the carbon flow in the microbial community. Species belonging to Clostridiales were defined as the primary benzene consumers and as heterotrophic CO2-fixing bacteria. 13C-labeled CO2 was also fixed by Deltaproteobacteria members and additionally they used 13C-labeled metabolites released by the Clostridiales. 13C-labeled secondary metabolites or dead biomass of both groups were probably used as the carbon sources of putative scavengers belonging to Bacteroidetes/Chlorobi organisms defined as the third metabolic group in the consortium (Figure 2b).

Figure 1
figure 1

Overview of a protein-SIP experiment studying the carbon flux between heterotrophic (Acidiphilum cryptum) and autotrophic (Acidithiobacillus ferrooxidans) organisms over four sampling points (t1–t4) (Kermer et al., 2012). Labeled galactose is metabolized by A. cryptum to labeled CO2. In early time points, only a low amount of labeled CO2 is present and is fixed by the autotrophic strain, leading to a low RIA. In later time points, the metabolic activity of A. cryptum resulted in a strong increase in 13CO2, leading to a higher RIA in A. ferrooxidans. The 13C-flux was reconstructed by the changes of the isotopologue patterns (color code, see sampling bar in the figure). Representative mass spectra showing the peptide ion mass distribution of peptide AGGLPAVIGELIR of dihydroxy-acid dehydratase (A. cryptum, gi148259108) and peptide AFDGSSIAGWK of glutamine synthetase, type I (A. ferrooxidans, gi198282766).

Figure 2
figure 2

Data evaluation of a protein-SIP experiment to detect the carbon flux in an anaerobic benzene-degrading community (Taubert et al., 2012). (a) Protein grouping based on RIA vs LR to define metabolic groups of bacterial organisms obtained by 13C benzene metabolisation. Colored data points indicate different metabolic groups: group 1, Clostridiales (orange dots); group 2, Deltaproteobacteria (blue triangles); group 3, Bacteroidetes (green squares). Arrows indicate the chronological development between the RIA and LR. A low variability of the RIA and a strong increase in LR (as shown for group 1) indicates a direct metabolisation of the 13C-labeled substrate and a high growth rate. A stronger change of RIA over time indicates an indirect metabolisation (like shown for group 2 and 3). (b) Model of the carbon flux with the bacterial community based on data of the protein-SIP experiment using 13C-labeled benzene and 13C-labeled carbonate.

Overall, protein-SIP is capable of providing insights into microbial consortia beyond the mere identification and quantification of proteins. Protein-SIP can (i) accurately detect metabolic activity and thereby distinguish between key players and bystanders in a microbial community, (ii) differentiate between the type of substrate usage and (iii) deliver information on protein induction. Further applications of protein-SIP may allow the deciphering of the main pathways and key players involved in the biodegradation of newly appearing pollutants, in the global carbon and nitrogen cycling in aquatic and terrestrial ecosystems and in the interaction between human and their microbiota.

Future development: automatic calculation of isotope labeling

To increase the throughput of mass spectra analysis for protein-SIP, an automated calculation of RIA and LR is needed. Currently, one automated pipeline is available and its application has been shown for 15N-labeled proteins by transforming the whole in silico mass spectra from the sample-specific metagenome with increments of 1% in 15N RIA to identify species-specific migration patterns from established into regrowing communities of an acid-mine drainage biofilm (Pan et al., 2011). Because of the stepwise transformation of a huge data set, the process required a relatively high amount of processing time in respect to more complex samples. In addition, a higher resolution with RIAs of 0.1% would even need more computational effort using the described bioinformatic pipeline. One alternative that has to be developed could be an automated tool, which identifies 13C- or 15N-labeled masses in correlation to the unlabeled ones within a certain retention time window and determines peptide sequences, RIAs and LRs in one step.

Integration of protein-SIP in the toolbox of microbial ecology and conclusion

The toolbox of microbial ecology comprises techniques that either use DNA, RNA, proteins and metabolites extracted from the whole community, or analyze intact single cells. The combination of SIP with these techniques leads to a holistic view into the metabolic networks (Figure 3). Single-cell analysis with nano secondary ion mass spectrometry is the most sensitive method to detect stable isotope incorporation. However, the gain of information about the phylogeny and function of the single cells depends highly on the used probes, and high-throughput experiments are not applicable due to the required machine time (Musat et al., 2012). This problem might have been solved by the development of Chip-SIP (Mayali et al., 2012). Raman microspectroscopy has a high spatial resolution but requires a label of at least 10 atom% for spectral shifts for identification of isotope enrichment in labeling experiments (Huang et al., 2007).

Figure 3
figure 3

Integration of protein-SIP in the toolbox of microbial ecology and the combination of OMICS to reconstruct metabolic networks.

Within the SIP toolbox, protein-SIP is integrated as an interface between the nucleic acids-based techniques that provide the sequence database for MS analysis and the analysis of metabolites that indicate protein activities (Figure 3). In comparison to other SIP approaches three important features of protein-SIP are noteworthy: (i) minimal required incorporation of heavy isotope (about 0.1% of additional 13C incorporation) compared with DNA/RNA-SIP (50/10 atom% (Manefield et al., 2002; Radajewski et al., 2003)), (ii) dynamic range for quantification of isotope composition (two orders of magnitude) and (iii) high resolution of species and function (depending on the database) due to the fact that proteomic studies are not dependent on the amplification of target genes. The combination of multi-omics approaches to quantify metabolic groups and by using meta-metabolome-SIP would lead into a comprehensive tool to track the nutrient fluxes within microbial communities.