Conductive Particles Enable Syntrophic Acetate Oxidation between Geobacter and Methanosarcina from Coastal Sediments.

Coastal sediments are rich in conductive particles, possibly affecting microbial processes for which acetate is a central intermediate. In the methanogenic zone, acetate is consumed by methanogens and/or syntrophic acetate-oxidizing (SAO) consortia. SAO consortia live under extreme thermodynamic pressure, and their survival depends on successful partnership. Here, we demonstrate that conductive particles enable the partnership between SAO bacteria (i.e., Geobacter spp.) and methanogens (Methanosarcina spp.) from the coastal sediments of the Bothnian Bay of the Baltic Sea. Baltic methanogenic sediments were rich in conductive minerals, had an apparent isotopic fractionation characteristic of CO2-reductive methanogenesis, and were inhabited by Geobacter and Methanosarcina As long as conductive particles were delivered, Geobacter and Methanosarcina persisted, whereas exclusion of conductive particles led to the extinction of Geobacter Baltic Geobacter did not establish a direct electric contact with Methanosarcina, necessitating conductive particles as electrical conduits. Within SAO consortia, Geobacter was an efficient [13C]acetate utilizer, accounting for 82% of the assimilation and 27% of the breakdown of acetate. Geobacter benefits from the association with the methanogen, because in the absence of an electron acceptor it can use Methanosarcina as a terminal electron sink. Consequently, inhibition of methanogenesis constrained the SAO activity of Geobacter as well. A potential benefit for Methanosarcina partnering with Geobacter is that together they competitively exclude acetoclastic methanogens like Methanothrix from an environment rich in conductive particles. Conductive particle-mediated SAO could explain the abundance of acetate oxidizers like Geobacter in the methanogenic zone of sediments where no electron acceptors other than CO2 are available.IMPORTANCE Acetate-oxidizing bacteria are known to thrive in mutualistic consortia in which H2 or formate is shuttled to a methane-producing Archaea partner. Here, we discovered that such bacteria could instead transfer electrons via conductive minerals. Mineral SAO (syntrophic acetate oxidation) could be a vital pathway for CO2-reductive methanogenesis in the environment, especially in sediments rich in conductive minerals. Mineral-facilitated SAO is therefore of potential importance for both iron and methane cycles in sediments and soils. Additionally, our observations imply that agricultural runoff or amendments with conductive chars could trigger a significant increase in methane emissions.

Correlation between microbial community and granule conductivity in anaerobic bioreactors for brewery wastewater treatment.

Prior investigation of an upflow anaerobic sludge blanket (UASB) reactor treating brewery wastes suggested that direct interspecies electron transfer (DIET) significantly contributed to interspecies electron transfer to methanogens. To investigate DIET in granules further, the electrical conductivity and bacterial community composition of granules in fourteen samples from four different UASB reactors treating brewery wastes were investigated. All of the UASB granules were electrically conductive whereas control granules from ANAMMOX (ANaerobic AMMonium OXidation) reactors and microbial granules from an aerobic bioreactor designed for phosphate removal were not. There was a moderate correlation (r=0.67) between the abundance of Geobacter species in the UASB granules and granule conductivity, suggesting that Geobacter contributed to granule conductivity. These results, coupled with previous studies, which have demonstrated that Geobacter species can donate electrons to methanogens that are typically predominant in anaerobic digesters, suggest that DIET may be a widespread phenomenon in UASB reactors treating brewery wastes.

Plugging in or going wireless: strategies for interspecies electron transfer.

Interspecies exchange of electrons enables a diversity of microbial communities to gain energy from reactions that no one microbe can catalyze. The first recognized strategies for interspecies electron transfer were those that relied on chemical intermediates that are recycled through oxidized and reduced forms. Well-studied examples are interspecies H2 transfer and the cycling of sulfur intermediates in anaerobic photosynthetic communities. Direct interspecies electron transfer (DIET) in which two species establish electrical contact is an alternative. Electrical contacts documented to date include electrically conductive pili, as well as conductive iron minerals and conductive carbon moieties such as activated carbon and biochar. Interspecies electron transfer is central to the functioning of methane-producing microbial communities. The importance of interspecies H2 transfer in many methanogenic communities is clear, but under some circumstances DIET predominates. It is expected that further mechanistic studies and broadening investigations to a wider range of environments will help elucidate the factors that favor specific forms of interspecies electron exchange under different environmental conditions.

Going wireless: Fe(III) oxide reduction without pili by Geobacter sulfurreducens strain JS-1.

Previous studies have suggested that the conductive pili of Geobacter sulfurreducens are essential for extracellular electron transfer to Fe(III) oxides and for optimal long-range electron transport through current-producing biofilms. The KN400 strain of G. sulfurreducens reduces poorly crystalline Fe(III) oxide more rapidly than the more extensively studied DL-1 strain. Deletion of the gene encoding PilA, the structural pilin protein, in strain KN400 inhibited Fe(III) oxide reduction. However, low rates of Fe(III) reduction were detected after extended incubation (>30 days) in the presence of Fe(III) oxide. After seven consecutive transfers, the PilA-deficient strain adapted to reduce Fe(III) oxide as fast as the wild type. Microarray, whole-genome resequencing, proteomic, and gene deletion studies indicated that this adaptation was associated with the production of larger amounts of the c-type cytochrome PgcA, which was released into the culture medium. It is proposed that the extracellular cytochrome acts as an electron shuttle, promoting electron transfer from the outer cell surface to Fe(III) oxides. The adapted PilA-deficient strain competed well with the wild-type strain when both were grown together on Fe(III) oxide. However, when 50% of the culture medium was replaced with fresh medium every 3 days, the wild-type strain outcompeted the adapted strain. A possible explanation for this is that the necessity to produce additional PgcA, to replace the PgcA being continually removed, put the adapted strain at a competitive disadvantage, similar to the apparent selection against electron shuttle-producing Fe(III) reducers in many anaerobic soils and sediments. Despite increased extracellular cytochrome production, the adapted PilA-deficient strain produced low levels of current, consistent with the concept that long-range electron transport through G. sulfurreducens biofilms is more effective via pili.

Promoting interspecies electron transfer with biochar.

Biochar, a charcoal-like product of the incomplete combustion of organic materials, is an increasingly popular soil amendment designed to improve soil fertility. We investigated the possibility that biochar could promote direct interspecies electron transfer (DIET) in a manner similar to that previously reported for granular activated carbon (GAC). Although the biochars investigated were 1000 times less conductive than GAC, they stimulated DIET in co-cultures of Geobacter metallireducens with Geobacter sulfurreducens or Methanosarcina barkeri in which ethanol was the electron donor. Cells were attached to the biochar, yet not in close contact, suggesting that electrons were likely conducted through the biochar, rather than biological electrical connections. The finding that biochar can stimulate DIET may be an important consideration when amending soils with biochar and can help explain why biochar may enhance methane production from organic wastes under anaerobic conditions.

Direct interspecies electron transfer between Geobacter metallireducens and Methanosarcina barkeri.

Direct interspecies electron transfer (DIET) is potentially an effective form of syntrophy in methanogenic communities, but little is known about the diversity of methanogens capable of DIET. The ability of Methanosarcina barkeri to participate in DIET was evaluated in coculture with Geobacter metallireducens. Cocultures formed aggregates that shared electrons via DIET during the stoichiometric conversion of ethanol to methane. Cocultures could not be initiated with a pilin-deficient G. metallireducens strain, suggesting that long-range electron transfer along pili was important for DIET. Amendments of granular activated carbon permitted the pilin-deficient G. metallireducens isolates to share electrons with M. barkeri, demonstrating that this conductive material could substitute for pili in promoting DIET. When M. barkeri was grown in coculture with the H2-producing Pelobacter carbinolicus, incapable of DIET, M. barkeri utilized H2 as an electron donor but metabolized little of the acetate that P.carbinolicus produced. This suggested that H2, but not electrons derived from DIET, inhibited acetate metabolism. P. carbinolicus-M. barkeri cocultures did not aggregate, demonstrating that, unlike DIET, close physical contact was not necessary for interspecies H2 transfer. M. barkeri is the second methanogen found to accept electrons via DIET and the first methanogen known to be capable of using either H2 or electrons derived from DIET for CO2 reduction. Furthermore, M. barkeri is genetically tractable,making it a model organism for elucidating mechanisms by which methanogens make biological electrical connections with other cells.

Syntrophic growth with direct interspecies electron transfer as the primary mechanism for energy exchange.

Direct interspecies electron transfer (DIET) through biological electrical connections is an alternative to interspecies H2 transfer as a mechanism for electron exchange in syntrophic cultures. However, it has not previously been determined whether electrons received via DIET yield energy to support cell growth. In order to investigate this, co-cultures of Geobacter metallireducens, which can transfer electrons to wild-type G. sulfurreducens via DIET, were established with a citrate synthase-deficient G. sulfurreducens strain that can receive electrons for respiration through DIET only. In a medium with ethanol as the electron donor and fumarate as the electron acceptor, co-cultures with the citrate synthase-deficient G. sulfurreducens strain metabolized ethanol as fast as co-cultures with wild-type, but the acetate that G. metallireducens generated from ethanol oxidation accumulated. The lack of acetate metabolism resulted in less fumarate reduction and lower cell abundance of G. sulfurreducens. RNAseq analysis of transcript abundance was consistent with a lack of acetate metabolism in G. sulfurreducens and revealed gene expression levels for the uptake hydrogenase, formate dehydrogenase, the pilus-associated c-type cytochrome OmcS and pili consistent with electron transfer via DIET. These results suggest that electrons transferred via DIET can serve as the sole energy source to support anaerobic respiration.

When is a microbial culture "pure"? Persistent cryptic contaminant escapes detection even with deep genome sequencing.

UNLABELLED: Geobacter sulfurreducens strain KN400 was recovered in previous studies in which a culture of the DL1 strain of G. sulfurreducens served as the inoculum in investigations of microbial current production at low anode potentials (-400 mV versus Ag/AgCl). Differences in the genome sequences of KN400 and DL1 were too great to have arisen from adaptive evolution during growth on the anode. Previous deep sequencing (80-fold coverage) of the DL1 culture failed to detect sequences specific to KN400, suggesting that KN400 was an external contaminant inadvertently introduced into the anode culturing system. In order to evaluate this further, a portion of the gene for OmcS, a c-type cytochrome that both KN400 and DL1 possess, was amplified from the DL1 culture. HiSeq-2000 Illumina sequencing of the PCR product detected the KN400 sequence, which differs from the DL1 sequence at 14 bp, at a frequency of ca. 1 in 10(5) copies of the DL1 sequence. A similar low frequency of KN400 was detected with quantitative PCR of a KN400-specific gene. KN400 persisted at this frequency after intensive restreaking of isolated colonies from the DL1 culture. However, a culture in which KN400 could no longer be detected was obtained by serial dilution to extinction in liquid medium. The KN400-free culture could not grow on an anode poised at -400 mV. Thus, KN400 cryptically persisted in the culture dominated by DL1 for more than a decade, undetected by even deep whole-genome sequencing, and was only fortuitously uncovered by the unnatural selection pressure of growth on a low-potential electrode. IMPORTANCE: Repeated streaking of isolated colonies on solidified medium remains a common strategy for obtaining pure cultures, especially of difficult-to-cultivate microorganisms such as strict anaerobes. The results presented here demonstrate that verifying the purity of cultures obtained in this manner may be difficult because extremely rare variants can persist, undetectable with even deep genomic DNA sequencing. The only way to ensure that a culture is pure is to cultivate it from an initial single cell, which may be technically difficult for many environmentally significant microbes.

Transcriptomic and genetic analysis of direct interspecies electron transfer.

The possibility that metatranscriptomic analysis could distinguish between direct interspecies electron transfer (DIET) and H2 interspecies transfer (HIT) in anaerobic communities was investigated by comparing gene transcript abundance in cocultures in which Geobacter sulfurreducens was the electron-accepting partner for either Geobacter metallireducens, which performs DIET, or Pelobacter carbinolicus, which relies on HIT. Transcript abundance for G. sulfurreducens uptake hydrogenase genes was 7-fold lower in cocultures with G. metallireducens than in cocultures with P. carbinolicus, consistent with DIET and HIT, respectively, in the two cocultures. Transcript abundance for the pilus-associated cytochrome OmcS, which is essential for DIET but not for HIT, was 240-fold higher in the cocultures with G. metallireducens than in cocultures with P. carbinolicus. The pilin gene pilA was moderately expressed despite a mutation that might be expected to repress pilA expression. Lower transcript abundance for G. sulfurreducens genes associated with acetate metabolism in the cocultures with P. carbinolicus was consistent with the repression of these genes by H2 during HIT. Genes for the biogenesis of pili and flagella and several c-type cytochrome genes were among the most highly expressed in G. metallireducens. Mutant strains that lacked the ability to produce pili, flagella, or the outer surface c-type cytochrome encoded by Gmet_2896 were not able to form cocultures with G. sulfurreducens. These results demonstrate that there are unique gene expression patterns that distinguish DIET from HIT and suggest that metatranscriptomics may be a promising route to investigate interspecies electron transfer pathways in more-complex environments.

Linking activity, composition and seasonal dynamics of atmospheric methane oxidizers in a meadow soil.

Microbial oxidation is the only biological sink for atmospheric methane. We assessed seasonal changes in atmospheric methane oxidation and the underlying methanotrophic communities in grassland near Giessen (Germany), along a soil moisture gradient. Soil samples were taken from the surface layer (0-10 cm) of three sites in August 2007, November 2007, February 2008 and May 2008. The sites showed seasonal differences in hydrological parameters. Net uptake rates varied seasonally between 0 and 70 µg CH(4) m(-2) h(-1). Greatest uptake rates coincided with lowest soil moisture in spring and summer. Over all sites and seasons, the methanotrophic communities were dominated by uncultivated methanotrophs. These formed a monophyletic cluster defined by the RA14, MHP and JR1 clades, referred to as upland soil cluster alphaproteobacteria (USCα)-like group. The copy numbers of pmoA genes ranged between 3.8 × 10(5)-1.9 × 10(6) copies g(-1) of soil. Temperature was positively correlated with CH(4) uptake rates (P<0.001), but had no effect on methanotrophic population dynamics. The soil moisture was negatively correlated with CH(4) uptake rates (P<0.001), but showed a positive correlation with changes in USCα-like diversity (P<0.001) and pmoA gene abundance (P<0.05). These were greatest at low net CH(4) uptake rates during winter times and coincided with an overall increase in bacterial 16S rRNA gene abundances (P<0.05). Taken together, soil moisture had a significant but opposed effect on CH(4) uptake rates and methanotrophic population dynamics, the latter being increasingly stimulated by soil moisture contents >50 vol% and primarily related to members of the MHP clade.

Bacterial and archaeal communities involved in the in situ degradation of (13) C-labelled straw in the rice rhizosphere.

Rice straw is a major substrate for the production of methane in flooded rice fields and results in increase of CH4 emission into the atmosphere. We investigated the bacteria and archaea involved in straw degradation by adding (13) C-labelled straw to the rhizosphere of planted rice microcosms in the greenhouse. The degradation of added straw resulted in the production of (13) C-labelled CH4 as end-product, which was detected in the pore water. The incorporation of (13) C into ribosomal RNA of Bacteria and Archaea present in the rhizospheric soil and on the roots was assessed by stable isotope probing (SIP) followed by terminal restriction fragment polymorphism (T-RFLP) fingerprinting and cloning/sequencing of RNA fractions with different buoyant densities. Members of the Clostridium cluster I, III and XIVa were actively involved in straw degradation both in rhizospheric soil and on roots. However, on roots, Proteobacteria, Bacilli, Actinobacteria, Bacteroidetes and Chlorobi were also involved in the straw degradation process. Mostly Methanosarcina and to a less degree also Methanobacteriaceae were the dominant Archaea that assimilated straw-derived carbon in the rhizospheric soil. Both Bacteria and Archaea together were most likely responsible for the conversion of rice straw to CH4 . In conclusion, this study tackled the important and interesting issue of linking active microorganisms responsible for the straw degradation process to CH4 emission into the atmosphere.

Effect of nitrogen fertilization on methane oxidation, abundance, community structure, and gene expression of methanotrophs in the rice rhizosphere.

Nitrogen, one of the limiting factors for the yield of rice, can also have an important function in methane oxidation, thus affecting its global budget. Rice microcosms, planted in the greenhouse, were treated with the N-fertilizers urea (UPK) and ammonium sulfate (APK) or were only treated with phosphorous and potassium (PK). Methane oxidation rates in PK and UPK treatments were similar during most of the rice-growing season, revealing no effect of urea. However, ammonium sulfate strongly suppressed methanogenesis providing an unfavorable environment for methanotrophs in APK treatment. Roots and rhizospheric soil samples, collected from six different growth stages of the rice plant, were analyzed by terminal restriction fragment length polymorphism (T-RFLP) of the pmoA gene. Assignment of abundant T-RFs to cloned pmoA sequences indicated that the populations on roots were dominated by type-I methanotrophs, whereas the populations in rhizospheric soil were dominated by type-II methanotrophs irrespectively of growth stages and fertilizer treatments. Non-metric multidimensional scaling ordination analysis of T-RFLP profiles revealed that the methanotrophic community was significantly (P<0.001) affected by the different fertilizer treatments; however, the effect was stronger on the roots than in the rhizospheric soil. Contrary to pmoA gene-based analysis, pmoA transcript-based T-RFLP/cloning/sequencing analysis in rhizospheric soil showed type I as the predominant methanotrophs in both PK and UPK treatments. Collectively, our study showed that type-I methanotrophs were dominant and probably active in rhizospheric soil throughout the season irrespective of nitrogen fertilizer used, whereas type-II methanotrophs were relatively more dominant under unfavorable conditions, such as in APK treatment.

Extraction of mRNA from soil.

Here, we report an efficient method for extracting high-quality mRNA from soil. Key steps in the isolation of total RNA were low-pH extraction (pH 5.0) and Q-Sepharose chromatography. The removal efficiency of humic acids was 94 to 98% for all soils tested. To enrich mRNA, subtractive hybridization of rRNA was most efficient. Subtractive hybridization may be followed by exonuclease treatment if the focus is on the analysis of unprocessed mRNA. The total extraction method can be completed within 8 h, resulting in enriched mRNA ranging from 200 bp to 4 kb in size.

Phylogenetic diversity and metagenomics of candidate division OP3.

Except for environmental 16S rRNA gene sequences, no information is available for members of the candidate division OP3. These bacteria appear to thrive in anoxic environments, such as marine sediments, hypersaline deep sea, freshwater lakes, aquifers, flooded paddy soils and methanogenic bioreactors. The 16S rRNA phylogeny suggests that OP3 belongs to the Planctomycetes/Verrucomicrobia/Chlamydiae (PVC) superphylum. Metagenomic fosmid libraries were constructed from flooded paddy soil and screened for 16S rRNA gene-containing fragments affiliated with the PVC superphylum. The screening of 63 000 clones resulted in 23 assay-positive fosmids, of which three clones were affiliated with OP3. The 16S rRNA gene sequence divergence between the fragments OP3/1, OP3/2 and OP3/3 ranges from 18% to 25%, indicating that they belong to different OP3 subdivisions. The 23S rRNA phylogeny confirmed the membership of OP3 in the PVC superphylum. Sequencing the OP3 fragments resulted in a total of 105 kb of genomic information and 90 ORFs, of which 47 could be assigned a putative function and 11 were conserved hypothetical. Using BLASTP searches, a high proportion of ORFs had best matches to homologues from Deltaproteobacteria, rather than to those of members of the PVC superphylum. On the fragment OP3/3, a cluster of nine ORFs was predicted to encode the bacterial NADH dehydrogenase I. Given the high proportion of homologues present in deltaproteobacteria and anoxic conditions in the natural environment of OP3 bacteria, the detection of NADH dehydrogenase I may suggest an anaerobic respiration mode. Oligonucleotide frequencies calculated for OP3/1, OP3/2 and OP/3 show high intraphylum correlations. This novel sequence information could therefore be used to identify OP3-related fragments in large metagenomic data sets using marker gene-independent procedures in the future. In addition to the OP3 fragments, a single metagenomic fragment affiliated with the candidate division BRC1 was obtained and analysed.

Transcriptional activity of paddy soil bacterial communities.

Bulk mRNA was used to explore the transcriptional activity of bacterial communities in oxic versus anoxic paddy soil. Two microbial cDNA libraries were constructed from composite samples using semi-randomly primed RT-PCR. cDNAs averaged 500-600 bp in length and were treated as expressed sequence tags (ESTs). Clustering analysis of 805 random cDNAs resulted in 179 and 155 different ESTs for the oxic and anoxic zones respectively. Using an E-value threshold of e(-10), a total of 218 different ESTs could be assigned by blastx, while 116 ESTs were predicted novel. Both the proportion and significance of the EST assignments increased with cDNA length. Taxonomic assignment was more powerful in discriminating between the aerobic and anaerobic bacterial communities than functional inference, as most ESTs in both oxygen zones were putative indicators of similar housekeeping functions, in particular ABC-type transporters. A few ESTs were putative indicators for community function in a biogeochemical context, such as beta-oxidation of long-chain fatty acids specifically in the oxic zone. Expressed sequence tags assigned to Alpha- and Betaproteobacteria were predominantly found in the oxic zone, while those affiliated with Deltaproteobacteria were more frequently detected in the anoxic zone. At the genus level, multiple assignments to Bradyrhizobium and Geobacter were unique to the oxic and anoxic zones respectively. The phylum-level affiliations of 93 16S rRNA sequences corresponded well with two taxonomically distinct EST patterns. Expressed sequence tags affiliated with Acidobacteria and Chloroflexi were frequently detected in both oxygen zones. In summary, the soil metatranscriptome is accessible for global analysis and such studies have great potential in elucidating the taxonomic and functional status of soil bacterial communities, but study significance depends on the number and length of cDNAs being randomly analysed.

Activity and composition of methanotrophic bacterial communities in planted rice soil studied by flux measurements, analyses of pmoA gene and stable isotope probing of phospholipid fatty acids.

Methanotrophs in the rhizosphere of rice field ecosystems attenuate the emissions of CH(4) into the atmosphere and thus play an important role for the global cycle of this greenhouse gas. Therefore, we measured the activity and composition of the methanotrophic community in the rhizosphere of rice microcosms. Methane oxidation was determined by measuring the CH(4) flux in the presence and absence of difluoromethane as a specific inhibitor for methane oxidation. Methane oxidation started on day 24 and reached the maximum on day 32 after transplantation. The total methanotrophic community was analysed by terminal restriction fragment length polymorphism (T-RFLP) and cloning/sequencing of the pmoA gene, which encodes a subunit of particulate methane monooxygenase. The metabolically active methanotrophic community was analysed by stable isotope probing of microbial phospholipid fatty acids (PLFA-SIP) using (13)C-labelled CH(4) directly added to the rhizospheric region. Rhizospheric soil and root samples were collected after exposure to (13)CH(4) for 8 and 18 days. Both T-RFLP/cloning and PLFA-SIP approaches showed that type I and type II methanotrophic populations changed over time with respect to activity and population size in the rhizospheric soil and on the rice roots. However, type I methanotrophs were more active than type II methanotrophs at both time points indicating they were of particular importance in the rhizosphere. PLFA-SIP showed that the active methanotrophic populations exhibit a pronounced spatial and temporal variation in rice microcosms.

Phylogenetic identity, growth-response time and rRNA operon copy number of soil bacteria indicate different stages of community succession.

Bacterial community succession corresponds to changes in the phylogenetic identity, growth-response time and rRNA operon (rrn) copy number of culturable populations. To test this hypothesis, we compared the bacterial fractions culturable from the oxic zone of flooded, unplanted paddy soil microcosms after 1-day (early succession) and 70-day (late succession) incubation periods. The proportion of bacteria that was cultivable on solid media corresponded for early and late succession to 37-40% and 31-35% of total DAPI cell counts, which were 7.40 (+/-0.36) x 10(8) and 5.54 (+/-0.28) x 10(8) cells per gram of dry soil, respectively. In colony-forming curve analysis, late successional bacteria showed a significant delay in their growth response compared with those from early succession. A total of 59 early successional isolates grouped into 16 species-level clusters (SLC) plus three Bacilli-like SLC, while 66 late successional isolates formed 25 SLC plus five Bacilli-like SLC. Except Bacilli-like spp., isolates from early succession always belonged to different SLC than those from late succession. Betaproteobacteria and Gammaproteobacteria were typical of the early stage, while Alphaproteobacteria and Actinobacteria prevailed in late succession. Considering all SLC except those assigned to Bacilli, growth-response time and rrn copy number were significantly correlated with successional stage. Isolates of most early successional SLC (14 of 16) formed visible colonies within 1 (11 SLC) or 2 days (three SLC) and contained >or= 4 rrn copies. In contrast, isolates of late successional SLC (23 of 25) formed visible colonies within 2 days (four SLC) or, in most cases, only within 3-15 days (19 SLC) and contained