The Microbiome of a Shell Mound: Ancient Anthropogenic Waste as a Source of Streptomyces Degrading Recalcitrant Polysaccharides

doi:10.21203/rs.3.rs-661003/v1

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The Microbiome of a Shell Mound: Ancient Anthropogenic Waste as a Source of Streptomyces Degrading Recalcitrant Polysaccharides

https://doi.org/10.21203/rs.3.rs-661003/v1

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published 01 Nov, 2021

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Metagenome amplicon DNA sequencing and traditional cell culture techniques are helping to uncover the diversity and the biotechnological potential of prokaryotes in different habitats around the world. It has also had a profound impact on microbial taxonomy in the last decades. Here we used metagenome 16S rDNA amplicon sequencing to reveal the microbiome composition of different layers of an anthropogenic soil collected at a shell mound Sambaqui archeological site. The Samabaqui soil microbiome is mainly composed by phyla Acidobacteria, Rokubacteria, Proteobacteria and Thaumarchaeota. Using culture-dependent analysis we isolated few Streptomyces strains from the Sambaqui soil. One of the isolates, named Streptomyces sp. S3, was able to grow in minimal medium containing recalcitrant polysaccharides including chitin, xylan, carboxymethylcellulose or microcrystalline cellulose as sole carbon sources. The activities of enzymes degrading these compounds were confirmed in cell free supernatants. The genome sequence revealed not only an arsenal of genes related to polysaccharides degradation but also biosynthetic gene clusters which may be involved in the production of biotechnologically interesting secondary metabolites.

General Microbiology

Biotechnology and Bioengineering

biodiversity

16S sequencing

Streptomyces

hydrolase

Microbiomes constitute an important source for the prospection of industrially relevant enzymes and bioactive metabolites such as antibiotics or chemotherapeutic drugs. For instance, most of the antibiotics used in the clinics nowadays are still the fruits of valuable prospection of Streptomyces strains from the environment, mostly from soil (Liu et al., 2013).

The recent advances in metagenomic 16S rDNA amplicon sequencing and whole metagenome DNA sequencing is helping to uncover the microbial diversity and their biotechnological potential at an unprecedent scale (Nayfach et al., 2020; Thompson et al., 2017). Global efforts such as the earth´s microbiome is providing valuable data on how microbial diversity is distributed around the globe and how microbial taxa correlate in similar environments in distant locations (Stevens et al., 2017). In addition to these high-tech platforms, microbial diversity can be accessed using traditional culture isolation techniques. Quite remarkably, traditional methods are still very effective in the discovery of novel bacterial strains with biotechnological potential (Wilson et al., 2014).

Brazil hosts a significant portion of the world´s biodiversity and the Brazilian territory constitute an untapped source for the prospection of novel microbes. Still, most of the Brazilian biomes are only marginally explored in terms of microbiome composition (Pylro and Roesch, 2017). Our research group is combining metagenomics and traditional cell culture techniques to uncover the microbiome in yet to be explored Brazilian environments such as the pristine Amazon forest air (Souza et al., 2019) and the mangrove soil (Huergo et al., 2018).

Mangroves are particularly interesting habitats for microbial prospection, given the unique chemical characteristics and diel tidal variations which affect salinity, oxygen, pH and nutrient availability (Alongi, 2014). Nevertheless, there are very few studies on Brazilian mangrove microbiome (Andreote et al., 2012; Ceccon et al., 2019; Huergo et al., 2018; M. and R., 2020; Mendes and Tsai, 2018).

The high primary productivity of mangrove estuaries provides plenty of availability of sea food. Not surprisingly, mangrove estuaries were colonized by ancient groups of fisher-hunters-collectors, vestiges of these ancestral human activities are preserved in several archaeological sites on the coast of Brazil which are named Sambaqui sites (Okumura & Eggers, 2005; Gernet et al., 2014). Sambaqui sites consist mostly of molluscs’ shells which are likely to be the waste products of meals eaten by groups of hunter-fishers-collectors that lived in the area between 2,000–10,000 years ago (Scheel-Ybert, 2001). The Sambaqui anthropogenic soil are typically arranged in layers with varying composition that are likely to reflect the occupation of these sites by different groups (Fig. 1), with the bottom layers representing the debris of the most ancient groups.

Given their unique characteristics the Sambaqui sites constitute unique niches which may host interesting uncharacterized microbes. Here we used 16S rRNA gene amplicon sequencing and culture techniques to provide the first microbiome description of an anthropogenic Sambaqui soil, namely the Sambaqui Bogaçu, located in Guaratuba, south of Brazil. One isolated bacterial strain from this site, named Streptomyces sp. S3, showed interesting biotechnological properties including the ability to degrade recalcitrant polysaccharides such as chitin, xylan, carboxymethyl cellulose and microcrystalline cellulose. Hence, Streptomyces sp. S3 has potential applications in biofuel production from lignocellulose waste products. A draft genome of Streptomyces sp. S3 was obtained showing an arsenal of putative polysaccharides hydrolytic enzymes. Furthermore, several biosynthetic gene clusters were identified in the Streptomyces sp. S3 genome revealing that this strain may have the ability to produce important biotechnological secondary metabolites.

2.1 Sampling and culturable bacteria analysis

The Sambaqui Boguaçu is located at the margin of the Boguaçú river in a place called Ilha do Casqueiro, Guaratuba Bay estuary, Paraná, Brazil (25 ° 55'11 "S / 48 ° 37'39" W). This Sambaqui is 7 m high and is likely to date between 10,000 and 2,000 years ago (Huergo et al., 2018) (Fig. 1). Samples were collected in a dry region of the site not subject to sea tide or river flooding. Samples were retrieved from three visually different stratification profiles of the Sambaqui layers, namely samples B, CM and S, from bottom to top, respectively (Fig. 1). About 2g of sediment were removed from ∼ 15 cm within the interior of Sambaqui profile using a sterile spoon. Samples were immediately stored in a sterile tube. Approximately one hour after sampling, 1g sample of the sediment was diluted with 9 ml of sterile saline (10^− 1 dilution), vortexed for 5 min and allowed to stand for 5 minutes for dense material to settle down. The supernatant was used to prepare a 10^− 2 dilution in saline, of which 100 µl were spread on LB agar containing cyclohexamide 50 µg.ml^− 1 to inhibit the growth of fungi. Plates were incubated aerobically at 30^oC for 5 days. The colonies developed were further replicated and stored in glycerol 50% at -20 ^oC at the culture collection of Setor Litoral, Federal University of Parana (UFPR), Matinhos – PR, Brazil.

Some isolates were subjected to partial 16S rRNA gene sequencing as described previously (Stets et al., 2013). Isolates were taxonomically identified by comparing the DNA sequences against the 16S ribosomal RNA gene sequences (Bacteria and Archaea) database at NCBI, using blastn (Altschul et al., 1990). All sequences were deposited in GenBank under the accession numbers MT019671, MT019672, MT019673 and MT019674.

2.2 Total DNA extraction and 16S rRNA gene amplicon Illumina sequencing

Total DNA extraction from the three Sambaqui soil layers were performed using Power Soil DNA Kit (MOBIO). The DNA recovered from the kit was precipitated with ethanol 80%, dried and all the genetic material was used as template for PCR amplification as described previously (Souza et al., 2019). Briefly, the V4 region of the 16S gene was PCR amplified in 10 µl reactions using: all dried template DNA; 1 µM primer 515F; 1 µM primer 806R (which includes the barcode for each sample); and 5 µl KlenTaq DV ReadyMix (Sigma-Aldrich). The PCR cycles were 94^oC 3 min, 18x (94^oC 45 s, 50^oC 30 s, 68^oC 1 min), 72^oC 10 min. Amplicons were sequenced in a MiSeq platform using MiSeq 500v2 Reagent Kit (Illumina) pair-end reads (2x of 250 bp).

Sample sequences were imported and demultiplexed in QIIME2 (Bolyen et al., 2019), then inputted into the plugin DADA2 (Callahan et al., 2016) on QIIME2 to filter low-quality data, denoising sequences, remove chimeras, join forward and reverse reads, and dereplicate sequences in amplicon sequence variants (ASV). After all steps, non-chimeric sequences were generated and reduction in sequence numbers per samples were observed as follow: sample B, from 45,305 to 30,874 (31,8%) and sample S, from 133,303 to 108,230 (18,8%). A naïve Bayesian classifier was used through q2-feature-classifier QIIME2 plugin to classify sequences against a pre-trained classifiers on SILVA v.128 16S rRNA 515F/806R gene-region database clustered at 99% identity (Pedregosa et al., 2011; Quast et al., 2013), available at https://docs.qiime2.org/2020.11/data-resources (MD5: 28105eb0f1256bf38b9bb310c701dc4e). The 16S rDNA amplicon sequences were deposited in NCBI study numbers PRJNA605351, SRS6116179 and SRS6116180.

2.3 Screening for Bacteria isolates that degrade recalcitrant polysaccharides

Isolates were tested for the ability to grow in solid agar M9 minimum medium (Green et al., 2012) containing ammonium chloride 20 mM as nitrogen source and 1% (w/v) of glucose, xylan, colloidal chitin, carboxymethyl cellulose or cellulose microcrystalline as carbon sources. Control agar plates without extra carbon source was also used to evaluate the ability of the isolates to use agar as carbon source. Isolates were streaked on M9 media plates and incubated for 5 days at 30^oC. The ability to use each carbon source was based on the visual inspection of the amount of biomass after 5 days at 30^oC. The ability to degrade xylan, colloidal chitin and carboxymethyl cellulose was confirmed by the formation of degradation halo after staining the plates with congo red 0.1% (w/v) and de-staining with NaCl 1 mol/l.

To confirm the ability of Streptomyces S3 to degrade recalcitrant polysaccharides, one isolated colony from LA medium was inoculated into 200 ml of M9 liquid medium containing xylan, carboxymethyl cellulose, microcrystalline cellulose or filter paper 1% (w/v) as sole carbon source. The flasks were incubated for 7 days in a rotary shaker at 30^oC and 120 rpm. Bacterial growth was accessed by visual inspection of bacterial biomass, by staining the cell-substrate matrix clumps for protein with Bradford reagent and/or by electronic microscopy analysis of the cell-substrate matrix clumps. To verify the presence of secreted hydrolytic enzymes, the supernatant was separated from the cells and insoluble substrates by centrifugation at 5,000 xg for 10 min. A fraction of 10 µl of the supernatant was spotted onto a plate containing solid agar M9 medium with 1% (w/v) xylan or carboxymethyl as substrate. After incubation at 30^oC for 30 min enzymatic activity was confirmed by the formation of degradation halo after staining the plates with congo red.

2.4 Scanning electron microscopy

The samples were fixed with 2% paraformaldehyde, dehydrated in ascending ethanol series, and the critical point was reached in a Bal-Tec CPD − 030 with carbon dioxide. The gold plating was obtained in a Balzers SCD-030. SEM analysis were performed in a scanning electron microscope JEOL-JSM 6360 L at the Electron Microscopy Center of UFPR, Curitiba, PR. Brazil.

2.5 Genome sequencing and analysis

Total DNA extraction from the isolate Streptomyces sp. S3 were obtained from cells cultured in LB agar medium and extracted using Power Soil DNA Kit (MOBIO). The whole-genome sequence was carried out using Nextera DNA Library Preparation Kit and paired-end sequencing in the Illumina MiSeq platform. Raw reads quality was checked by FastQC (Andrews, 2010). DNA sequence was de novo assembled using Spades (Bankevich et al., 2012). The draft genome was annotated using Prokka (Seemann, 2014) and RAST (Overbeek et al., 2014). The draft genome sequence assembly was deposited in NCBI Assembly database under the identifier ASM1304450v1. Genome blast phylogeny was directly retrieved from NCBI.

The identification of carbohydrate-active enzymes were performed by comparing the Proteome of Streptomyces sp. S3 against the latest (available on January 2020) CAZy database (Cantarel et al., 2009) using BlastP (Altschul et al., 1990). Proteins were considered as putative carbohydrate-active enzymes when the alignment score with a CAzy database entry had evalue ≤ 5^− 100 and the fraction of hit (CAZy) covered in the alignment was ≥ 0.4. Analysis of secondary metabolite biosynthesis gene clusters were performed using antiSMASH (Blin et al., 2019) and phylogenetic analysis were performed using autoMLST (Alanjary et al., 2019).

2.6 Cell culture collection deposit

The strain Streptomyces sp. S3 was deposited at CMRP WDCM1240 - Microbiological Collections of Paraná Network - Federal University of Parana at code number CMRP5229.

In this study we focused on an archaeological Sambaqui site located in the Boguaçú River which is part of the Guaratuba bay estuary (Fig. 1). The soil of the Sambaqui Boguaçú is arranged in three visually distinct layers, with varying composition, that are likely to reflect the time of occupation of this site by different groups (Fig. 1C). To assess the microbial diversity within the Sambaqui-Boguaçú samples of the three visually different layers were collected and subjected to microbial cultivation approach and to metagenome microbial biodiversity survey.

3.1 Prokaryotic biodiversity using 16S rDNA amplicon sequencing

Total DNA was extracted from each of the three Sambaqui layers (Fig. 1C). The medium layer, namely CM, did not yield enough DNA for this analysis and was not considered for further analysis. The extracted metagenomic DNA from the top layer, namely S, and the bottom layer, namely B, were used as template for PCR amplification of the V4 region of the 16S rRNA gene and subjected to next generation Illumina sequencing using primers and methodology described previously (Huergo et al., 2018).

The amplicon sequence variants (ASV) were taxonomically classified; 13.8% and 9.3% of the ASV were classified as Archaea in S and B samples, respectively. Strikingly, despite being visually different (Fig. 1C), the samples S and B had similar biodiversity profiles at Phylum level (Fig. 2). The most represented Phylum were Acidobacteria, Rokubacteria, Proteobacteria and the Archaea Thaumarchaeota (Fig. 2). The most represented identified family was the methylotrophic Methylomirabilaceae (∼10% of the reads in both samples) (Figure S1). This family was reported to be abundant in paddy fields, an anaerobic habitat typically rich in methane (Ghashghavi et al., 2019). The Sambaqui site explored in this study was built over a mangrove which is also considered a habitat with high methane production, this may explain the abundance of the methylotrophic Methylomirabilaceae in our samples. Most of the remaining sequences could not be classified at Family (Figure S1) or lower taxonomic levels. These data support that the Sambaqui site hosts unique poorly characterized microorganisms.

3.2 Bacteria isolation and selection for growth in recalcitrant polysaccharides

All the three different layers of Sambaqui samples were diluted in saline and the 10^− 2 dilution was plated in LB agar medium. The samples from the layers B and CM did not yield any CFU, while sample S produced 8 CFU, namely S1 to S8. The isolates S3 and S8 showed a similar colony morphology and produced of a dark pigment in LB agar plates or LB liquid medium (Figure S2). The isolates were evaluated for their ability to growth in M9 minimum medium containing glucose, agar, colloidal chitin, microcrystalline cellulose (MCC), carboxymethyl cellulose (CMC) or xylan as carbon sources. All the isolates were able to grow using glucose as carbon source while using ammonium as nitrogen source (Table 1). Interestingly, the isolates S3 and S8 showed little growth in M9-glucose agar plates without a nitrogen source (Table 1). Furthermore, the isolates S3 and S8 grew well in LB agar prepared using sea water indicating halophilic properties (not shown).

Table 1

Growth of isolates in M9 solid minimum medium with different carbon sources.
Isolate	Carbon Source¹
Isolate	Glucose	Agar	Chitin	MCC	CMC	Xylan	Glucose without nitrogen
S1	+++	-	-	-	-	-	-
S2	+	-	-	-	-	-	-
S3	+++	+	++	+	++	+++	+
S4	+	-	-	-	-	-	-
S5	+++	-	-	-	-	-	-
S6	+++	-	-	-	-	-	-
S7	+	-	-	-	-	-	-
S8	+++	+	++	+	++	+++	+
¹all media contain agar 15g/L. + indicates the visual amount of biomass observed after growth (+ low, ++ medium, +++ high).

The isolates S3 and S8 were able to growth in M9 agar containing different recalcitrant carbohydrates as carbon source including agar, chitin, CMC, MCC and xylan (Table 1 and Figure S3). Given that S3 and S8 were able to grow using agar as sole carbon source, we consider that the growth detected in the presence of other polysaccharides could be sustained by agar degradation instead. However, the degradation of chitin, CMC and xylan could be confirmed by staining the agar plates with congo red which showed typical polysaccharide degradation halo (Figure S3C).

To provide a taxonomic classification for the isolates the 16S rRNA gene of the isolates S3, S5, S6, and S8 were PCR amplified and subjected to partial sequencing. All sequences showed 100% identity to various Streptomyces strains when searched against specialized 16S rRNA NCBI database. Multiple sequence alignment of the 16S rRNA gene revealed two groups of sequences, one includes the sequences of S3 and S8 which were identical in pair wise comparison. The sequences of isolates S5 and S6 were also identical in pair wise comparison. The two different groups of isolates (S3-S8 and S5-S6) showed 4 base differences within the 16S rDNA V4/V5, 98.5% identity (Figure S4). Despite belonging to Streptomyces genus these two groups of isolates have completely different capacity to use recalcitrant polysaccharides as carbon source in M9 media (Table 1).

The isolate Streptomyces sp. S3 was subjected to further characterization. This bacterium was able to growth aerobically in M9 liquid medium containing the soluble polysaccharides xylan and CMC as the only carbon source. Streptomyces sp. S3 formed cell pellets in these media (Fig. 3A and B). Scanning electron microscopy analysis of these pellets showed the formation of typical Streptomyces mycelium (Fig. 3). Interestingly, the morphology of the mycelium was different in medium containing xylan or CMC. When using CMC as carbon source, the mycelium was covered with an apparent extracellular matrix (Fig. 3). We suspect that this cell surface adhering material may be formed by an extracellular complex of CMC and enzymes involved in CMC degradation.

Qualitative analyses for presence of active extracellular enzymes degrading xylan and CMC were carried out by placing 10 µl of each cell culture supernatant over M9 solid medium containing either xylan or CMC. After 30 min incubation at 30^oC, the plates were stained with congo red to detect substrate degradation. As expected, degradation of xylan was readily detected using the supernatant of cells cultured in xylan (Figure S5A, spot 1). On the other hand, and quite surprisingly, only a faint CMC degradation halo was detected using the supernatant of cells cultured in CMC (Figure S5A, spot 3). The amount of protein in the culture supernatants were below the limit of detection and could not be determined. Hence, at this point, we cannot infer if the differences in xylan vs CMC degradation halo are caused by differences in total enzymes load and/or specific enzyme activities.

The ability of Streptomyces sp. S3 to grow aerobically in M9 liquid medium carrying insoluble MCC or filter paper as sole carbon sources was also evaluated. Even though the cells did not appear as pellets as observed when growing with CMC or xylan, it was possible to confirm microbial biomass development adhered to the insoluble MCC by staining the remaining insoluble substrate for protein using the Bradford reagent (not shown). Furthermore, it was possible to detect active xylan and CMC degrading extracellular enzymes from the Streptomyces sp. S3 supernatant of cells cultured in MCC (Figure S5A, spot 3). The supernatant from MCC growing cells produced a more intense CMC degradation halo than those assayed with the supernatant of cells growing in CMC itself (Figure S5B, compare spots 3 and 4).

3.3 Genome analysis

A draft genome sequence of Streptomyces sp. S3 was obtained comprising 569 contigs (40558 N50), with a total of 10,992,946 bp with G + C content of 70.55%. Genome annotation revealed 9844 protein coding sequences. The Streptomyces sp. S3 genome was used to perform phylogenetic analysis against reference organisms using Automated Multi-Locus Species (auto MLST) (Alanjary et al., 2019). The phylogenetic tree revealed that Streptomyces antibioticus DSM40234 is the closet type strain to Streptomyces sp. S3 (Figure S6) with a MASH distance of 0.1064 and estimated average nucleotide identity of 0.8936 (Table S1). S. antibioticus was originally isolated from soil and is well known for its potential to produce several bioactive compounds, including several antibiotics. There are strains of S. antibioticus isolated form marine environment which may explain the halophilic properties of the Streptomyces S3 isolate (Sharma et al., 2019; Waksman and Woodruff, 1941; Wang et al., 2017; Xu et al., 2011). Automated genome blast-based phylogeny retrieved from NCBI indicated that soil environmental isolate Streptomyces sp. WM6386 (Blodgett et al., 2016) as the closest relative (Figure S7).

In order to identify biosynthetic gene clusters (BGC) the Streptomyces sp. S3 genome was subjected to antiSMASH analysis (Blin et al., 2019) which predicted 22 BGCs, totalling 464,995bp (4.2% of the genome), including: 4 terpene (76,408bp); 1 polyketide synthase (PKS; 32,694bp); 1 polyketide synthase (PKS)/nonribosomal peptide synthetase (NRPS) hybrid (68,067bp); 6 NRPS among other (220,742bp) (Table S2). Out of these, only 5 showed similarities ≥ 0.7 to known BGC including those involved in the biosynthesis of the terpenes albaflavenone, geosmin, ectoine and hopene. A BGC for melanin production was also found, suggesting that melanin be responsible for the black pigmentation of Streptomyces sp. S3 when cultured in LB medium (Figure S2). Indeed, two putative tyrosinases containing secretion N-terminal signal peptides were identified in the annotated genome (not shown). A BGC involved in ectoine production was identified (Table S2). Ectoine is produced by halophilic and halotolerant microorganisms to prevent osmotic stress in highly saline environments (Reshetnikov et al., 2011). The production of ectoine may explain the halotolerant behavior of Streptomyces sp. S3.

To assess the potential for carbohydrate degradation the predicted proteome of Stremptomyces S3 were compared with the enzymes deposited at the CAZy database using blastP. This analysis revealed a total of 459 enzymes comprising: 247 Glycosyl Hydrolase; 99 Glycosyl transferases; 25 Polysaccharide lyases; 31 Carbohydrate esterases; 5 Auxiliary activity; 121 Carbohydrate-binding modules (Table S3). 214 (46.6%) of these putative CAZy enzymes were annotated as hypothetical proteins by Prokka while some enzymes were annotated as putative Chitinases, xylanases and cellulases (Table S3). These data provide additional support that Stremptomyces S3 is well suited for recalcitrant polysaccharide degradation and a potential source of biotechnologically relevant enzymes.

Despite global efforts to uncover the microbial diversity and biotechnological potential there are still untapped sources to explore specially in environments where less sampling efforts were concentrated. In this study we provide the first microbiome analysis of the anthropogenic soil layers of an archeological Sambaqui site located in the South of Brazil. By using metagomic DNA extraction and 16S rDNA amplicon sequencing we identified Acidobacteria (∼19%), Rokubacteria (∼17%), Proteobacteria (∼16%) and Thaumarchaeota (∼9%) as the most representative phylum in different layers of the Sambaqui soil. Quite remarkably, most of the reads could not be classified at lower taxonomic level suggesting that this site contains unique previously undescribed microbes (Fig. 2 and Figure S1). We have analysed previously the microbiome of the pristine mangrove soil and mangrove soil affected by the eroding debris at this Sambaqui site. The microbiome composition in the mangrove soil at the flooding level was remarkably different with Proteobacteria (∼49%), Chloroflexi (∼12%), and Bacterioidetes (∼6%) being the dominant taxa (Huergo et al., 2018).

Using culture techniques, a low number of CFU was obtained from just one of the soil layers using the rich medium for cell culture (Figure S2). Such poor recovery is likely to reflect the fact that the Sambaqui soil is poor in organic matter despite abundant carbonaceous shell debris. Nevertheless, few Streptomyces could be isolated which may reflect the fact that Streptomyces can survive in dormant spores and/or because Streptomyces typically can use a range of substrates as carbon sources including recalcitrant polysaccharides. In fact, the isolated Streptomyces sp. S3 was able to use agar, chitin, CMC, MCC and xylan as carbon sources and showed residual growth even in the absence of a nitrogen source (Table 1). The presence of enzyme degrading recalcitrant polysaccharides was confirmed by assaying the enzymatic activity in cell culture supernatant (Figure S5) and corroborated by genome analysis of Streptomyces sp. S3 (Table S3). Interestingly, several studies on different Streptomyces support that some strains have the ability to degrade cellulosic biomass (Takasuka et al. 2013; Lim et al. 2015; Pinheiro et al. 2017). Studies are under way to identify the enzymes responsible for CMC and MCC degradation in Streptomyces sp. S3.

The genome analysis of Streptomyces sp. S3 indicated that S. antibioticus is the closest type strain (Figures S1 and S6). However, the low nucleotide identity ANI suggest that Streptomyces sp. S3 may constitute a novel species. The genome data also support that Streptomyces sp. S3 may produce secondary metabolites of biotechnological importance (Figure S2). This is expected since its closest relative S. antibioticus is a well-known antibiotic producer (Sharma et al., 2019).

Funding This work was supported by CNPq, Fundação Araucária, CAPES and CNPq-INCT of Biological Nitrogen Fixation.

Conflicts of interest/Competing interests Nothing to declare

Availability of data and material Materials and data are available upon request

Code availability Not applicable.

Authors' contributions. L.H, M.C, M.V.G, M.G collected and processed the samples; V.B and E.B processed the samples for Illumina sequencing; E.M.G. and T.T. performed the microscopy analysis; A.P. analyzed microbiome data; L.H, D.G, L.C and G.C analyzed the genome sequence. R.R, L.H, E S, L.C and F.P, project and lab management. L.H wrote the manuscript with inputs form all authors.

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The Microbiome of a Shell Mound: Ancient Anthropogenic Waste as a Source of Streptomyces Degrading Recalcitrant Polysaccharides

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Abstract

Figures

1. Introduction

2. Material And Methods

2.1 Sampling and culturable bacteria analysis

2.2 Total DNA extraction and 16S rRNA gene amplicon Illumina sequencing

2.3 Screening for Bacteria isolates that degrade recalcitrant polysaccharides

2.4 Scanning electron microscopy

2.5 Genome sequencing and analysis

2.6 Cell culture collection deposit

3. Results

3.1 Prokaryotic biodiversity using 16S rDNA amplicon sequencing

3.2 Bacteria isolation and selection for growth in recalcitrant polysaccharides

3.3 Genome analysis

4. Discussion

5. Declarations

6. References

Supplementary Files

Status:

Journal Publication

Version 1