Marine sediments cover two-thirds of our planet and harbor huge numbers of living prokaryotes. Long-term survival of indigenous microorganisms within the deep subsurface is still enigmatic, as sources of organic carbon are vanishingly small. To better understand controlling factors of microbial life, we have analyzed viral abundance within a comprehensive set of globally distributed subsurface sediments. Phages were detected by electron microscopy in deep (320 m below seafloor), ancient (∼14 Ma old) and the most oligotrophic subsurface sediments of the world’s oceans (South Pacific Gyre (SPG)). The numbers of viruses (104–109 cm−3, counted by epifluorescence microscopy) generally decreased with sediment depth, but always exceeded the total cell counts. The enormous numbers of viruses indicate their impact as a controlling factor for prokaryotic mortality in the marine deep biosphere. The virus-to-cell ratios increased in deeper and more oligotrophic layers, exhibiting values of up to 225 in the deep subsurface of the SPG. High numbers of phages might be due to absorption onto the sediment matrix and a diminished degradation by exoenzymes. However, even in the oldest sediments, microbial communities are capable of maintaining viral populations, indicating an ongoing viral production and thus, viruses provide an independent indicator for microbial life in the marine deep biosphere.
The world’s oceans harbor huge numbers of viruses. Viral lysis of cells is a driving force for shaping microbial community structures (Weinbauer and Rassoulzadegan, 2004). Furthermore, viruses cause a short-cut (viral shunt) in the carbon and nutrient cycling within the pelagic food web (Wilhelm and Suttle, 1999; Suttle, 2005). A high viral turnover and the associated release of organic carbon was previously shown for surficial deep-sea sediments (Danovaro et al., 2008). For the marine deep biosphere, there are no comparable data available and the viral impact on microbial communities and the related carbon cycling in the marine deep biosphere is poorly constrained. The organisms within deep-sea sediments have to cope with severe substrate and nutrient limitation (Jørgensen and D'Hondt, 2006) due to an increasing recalcitrance of organic matter with depth (Wellsbury et al., 1997). Even though prokaryotes are prone to starvation (Jørgensen and D'Hondt, 2006), the majority of the cells were shown to be alive and metabolically active (Schippers et al., 2005; Morono et al., 2011). The available energy per cell was estimated to be close to the minimum requirement for cell maintenance. As a result, the carbon turnover of prokaryotic communities has been estimated between 10 and 1000 years (Hoehler and Jorgensen, 2013). Cell activity might only represent the restoration of structural cell damage, for example, amino-acid racemization and depurination. If cells proliferate, growth, however, cannot exceed the rate of prokaryotic mortality, as the community size is decreasing with depth (Hoehler and Jorgensen, 2013). Cells are capable to deal with this energy-limited life style (Roy et al., 2012) but controlling factors for cell death in marine subsurface environments remain largely unidentified. The presence of inducible temperate phages in bacteria isolated from the deep subsurface (Engelhardt et al., 2011; Engelhardt et al., 2013) predict viral predation to control prokaryotic mortality.
Now we have analyzed the so far most comprehensive set of marine sediment samples for virus counts, covering a broad range of characteristics regarding total organic carbon (TOC) content, sedimentation rate, age and microbial activity (see Materials and methods section for detailed site description and Map Supplementary Figure S1). These comprise a highly active North Sea tidal-flat (Site Janssand) (Beck et al., 2009), continental margin sites exhibiting high sedimentation rates, open ocean sites with lower sedimentation rates and the South Pacific Gyre (SPG), the most oligotrophic oceanic province. The latter was integrated in this study, as mid-ocean gyres represent 42% of the world’s oceans (Kallmeyer et al., 2012) and their sediments harbor far lower cell numbers (106–103 cells per cm−3) than continental margins (109–105 cells per cm−3) (Parkes et al., 2000). We aimed for providing an independent indicator for microbial life in the marine subsurface as the presence of phages suggests active phage–host relationships.
Materials and methods
Most sediment samples were collected during ODP/IODP cruises onboard the JOIDES Resolution and were stored at −80 °C before analysis (Supplementary Figure S1). Additional samples were obtained from the IODP core repository to complement the available sediment samples from ODP Leg 201. German tidal-flats were sampled by vibro coring and samples were prepared for cell and virus counting immediately after sediment recovery.
Tidal-flat sediments (Site Janssand) are constantly supplied with fresh organic material. Highly active microbial communities extend down to several meters below seafloor (mbsf) (Beck et al., 2009, 2011). Three meter long cores were recovered, which is equivalent to ∼5000 years. Sediments from the continental slope of the Bering Sea (Site U1344, water depth 3172 meter), obtained during IODP Exp. 323, are located in the ‘Green Belt’ area. A relatively high deposition of organic matter is originating from the high primary production of 170 g C m−2 y−1 in the photic zone (Sambrotto et al., 2008) and a high sedimentation rate of 29–89 cm ky−1 (Wehrmann et al., 2011). Deep subsurface sediments from the Peru margin (sites 1227 and 1230) and the eastern equatorial Pacific (sites 1225 and 1226), recovered during ODP Leg 201, harbor a relatively high number of cells with low metabolic activity (D'Hondt et al., 2004). Water depths ranged between 151 and 5086 m. Sediments of the SPG were sampled during IODP Exp. 329. This mid-ocean gyre is characterized by extremely low primary production (ChlA content ∼0.01 mg m−3) leading to a low sedimentation rate and a TOC content of <0.2–0.003 wt% in sediments below the center of the gyre (D'Hondt et al., 2009). The basement ages are between ∼13.5 and 100 Ma (D’Hondt et al., 2011).
Cell counts for sediments from Peru margin and slope sites (ODP Leg 201, Site 1227–1231) and the equatorial Pacific (Site 1225, 1226) provided for this study, were described previously (D'Hondt et al., 2004). Preparations for cell counts for Bering Sea (Site U1344) and tidal-flat sediments (Site Janssand) were done accordingly, by applying SybrGreen I for cell staining (Noble and Fuhrman, 1998; Lunau et al., 2005). Enumeration of cells for sediments obtained during IODP Exp. 329 (Site U1365-1369, U1371) were done onboard the JOIDES Resolution (D’Hondt et al., 2011). Owing to the low cell abundances in sediments from IODP Exp. 329, a cell extraction protocol had to be used (Kallmeyer et al., 2008). Extraction efficiency was tested against non-extracted samples and was found to be 60–80%.
Extraction of viruses
Sediment samples for the extraction and enumeration of viruses were kept frozen at −80 °C after sediment recovery until further analysis. The preparation for virus counting was done immediately after thawing individual samples to minimize the loss of viruses that might occur in unfrozen and unfixed samples. The extraction of viruses was performed accordingly to the protocol by Danovaro et al. (2001), but was adapted to minimize the filter background that interfered with the virus counting. Briefly, individual subsamples of 1 cm3 were added to a 0.02-μm pre-filtered mixture of 3.5 ml ddH2O and 1 ml sodium-pyrophosphate (55 mM). Slurries were mixed at 2000 r.p.m. by vortexing until the sediment was completely suspended, but at least for 15 min. Samples were sonicated for 3 min with interruption of 30 s each minute and vortexed at 2000 r.p.m. during interruptions. After centrifugation at 1000–2000 × g for 2–10 min, supernatants were removed and 4 ml of Tris-EDTA buffer (10 mM Tris, 1 mM EDTA, pH 7.8, 0.02-μm filtered) was added to the remaining sediment. Slurries were shaken for 10 min after resuspension of sediment pellets followed by centrifugation as indicated above. Supernatants of both extraction steps were pooled and filtered through 0.45 μm polycarbonate filters.
For SPG sites U1368 and U1369, a carbonate dissolution was performed prior to virus extraction to further reduce unspecific background signals for these sediments. In addition, sediment samples of SPG sites U1366 and U1367 were used for control counts to verify that the treatment with acetate buffer does not cause a significant loss of viruses during the extraction. Therefore, instead of ddH2O, 3.5 ml 0.02-μm pre-filtered sodium-acetate buffer (0.47 M, pH 4.7) was added to 1 cm3 of sediment samples. The sediment was homogenized by shaking at 2000 r.p.m. Subsequently, the buffered slurries were gently shaken for 15–30 min. Further extraction procedure followed the protocol described above.
Enumeration of viruses
For enumeration of viruses, 10 μl to 6 ml of virus extracts were filtered onto 0.02 μm Anodisc filters (13 mm, Whatman, Maidstone, UK). Filters were washed with Tris-EDTA buffer (10 mM Tris, 1 mM EDTA, pH 7.8). Viruses were stained by applying SybrGold or SybrGreen I (Invitrogen, Carlsbad, CA, USA). Briefly, filters were mounted on a drop of 40 μl 2 × SybrGold solution for 30 min in the dark. Remaining staining solution was removed and filters were mounted to a microscopic slide by using 4 μl embedding solution (VectaShield (Vector Laboratories, Peterborough, UK): glycerol (1:1), 0.1% phenyldiaminoxalat). For SybrGreen I-staining, 3.5 μl of a mounting solution (Lunau et al., 2005) containing SybrGreen I (final concentration 1 × ) was mounted directly onto the filter. Between 50 and 400 viruses were counted in 10 to 300 randomly chosen fields per sample by using an Olympus BX51 microscope (Hamburg, Germany).
Calculation of viral community half-lives in SPG sediments
To calculate viral community half-lives, semi-logarithmic plots of virus counts against the age of SPG sediments were used. Sediment ages were determined by assuming a linear sedimentation rate, the sediment thickness and the basement age. For each site, a power-law function (a) was used to describe the decrease in virus counts with sediment age. First-order derivations (b) were used to calculate half-lives of viral communities (c) for sediments of an approximated age of 1 and 10 Ma and at the basement age of the respective site.
(b) f ′(x)=a*n*x(x–1)
(c) t1/2=−log(2)/f ′(x)
Transmission electron microscopy
Viruses from 4 to 6 ml of virus extracts from various sediment samples were attached to carbon-coated 200 mesh formvar copper grids (Plano, Wetzlar Germany) by centrifugation (swing-out rotor, SW-41, 90 000 × g, 90 min) Virus-like particles were examined with an EM 902 A Transmission electron microscope (Zeiss, Jena, Germany). A Proscan High Speed SSCCD camera system with iTEMfive software was used for image acquisition.
Results and discussion
Viruses outnumber prokaryotes in subsurface sediments
Viruses were present in all studied sediments and always outnumbered the total cell counts as examined by epifluorescence microscopy using SybrGreen I staining. Verification and the explicit identification of the particles as phages in sediments as deep as 320 mbsf and up to 14 Ma old was performed by transmission electron microscopy (Figure 1). The highest counts of cells and viruses were found in the tidal-flat sediment (Site Janssand, Figure 2), with cell numbers of >108 cm−3 and virus counts around 109 cm−3 for the upper 3 m, constituting a virus-to-cell ratio of about 10. In Peru margin and equatorial Pacific (ODP Leg 201, Sites 1225–1231) as well as in Bering Sea sediments (IODP Exp. 323, Site U1344), cell numbers decreased from 108 cells cm−3 in the upper sediment layers by three orders of magnitude over a depth interval of 320 mbsf. Viral counts in the upper sediment column were up to seven times higher, but decreased more slowly with depth, resulting in virus-to-cell ratios of up to 20 below 100 mbsf. Surface sediments of the central SPG (IODP Exp. 329, Sites U1366–1369) harbored only 106 cells cm−3, and the counts strongly decreased by three to four orders of magnitude within the first meters below seafloor. At the same time, the viral counts decreased from about 107 cm−3 at the sediment surface by two to three orders of magnitude only, resulting in increasing virus-to-cell ratios of up to 225.
Extraction efficiency of viruses in deep subsurface sediments
The number of washing steps is crucial for the extraction efficiency of viruses from marine sediments (Danovaro et al., 2001; Middelboe et al., 2003; Siem-Jørgensen et al., 2008). These studies consistently showed that the initial extraction recovers the majority of viruses. After one additional washing step, the extraction efficiency was about 60–80%. For our deep-subsurface sediments, each additional washing step increased the volume of the extract and the amount of co-extracted substances and small particles. Both resulted in a more intense background on the filters. In particular for deeper and older sediments, virus counts were close to the detection limit. A reduction of the filter background was essential to avoid viruses to be covered by particles. Accordingly, only a single washing step was conducted during the virus extraction which in turn might lead to an underestimation of virus counts. However, the virus-to-cell ratio and subsequent calculations are not effected as both, virus and cell extraction efficiencies are in the same range of 60–80%.
The additional reduction of background-staining by acidic dissolution of carbonates (Kallmeyer et al., 2008) turned out to improve virus counting in sediments with high carbonate content and low viral abundance. At control sites, a comparison of virus counts with and without carbonate dissolution showed no significant differences in the number of extracted viruses (1.56±0.71 × 105 and 1.06±0.48 × 105, t-test; P>0.05).
Ongoing viral production in subsurface sediments
Our data prove that deep-biosphere microbial communities are capable of maintaining viral communities of a respective size. Cell and viral counts correlate over seven orders of magnitude (r2=0.941, n=89, Figure 3). At tidal flats (Beck et al., 2009) and the deep seafloor, intense microbial activity supports high viral production (Danovaro et al., 2008). Here, virus-to-cell ratios of about 10 throughout the upper few meters indicate a short-term balance of viral production and decay (Figure 2c) as frequently found in the water column (Weinbauer, 2004). Consistently higher virus-to-cell ratios at less active (Jørgensen and D'Hondt, 2006), deeper and old sediment layers, point toward a better preservation of phages or a diminished viral decay. This might be caused by absorption of phage particles to the sediment matrix (Dowd et al., 1998) and a reduced activity of exoenzymes (Fischer et al., 2004). Semi-logarithmic plots of the viral counts against the sediment age can be fitted by a power-law function for the SPG sediments (Supplementary Figure S2). Not considering any viral production, first-order derivation was used to approximate half-lives of viral communities. At a sediment age of 1 Ma apparent half-lives of viral communities are between 0.5 and 1.6 Ma, for 10 Ma old sediments between 6.8 and 17.5 Ma and at basement age (13.5–100 Ma) (D’Hondt et al., 2011) half-lives are between 13.9 and 97 Ma (Table 1). However, viral community half-lives are probably overestimated and compensated by viral production. In a recent study, Middelboe et al. (2011) addressed viral abundance and decay in sediments on the eastern margin of the Porcupine Seabight (IODP site U1317). The authors estimated half-lives of viral communities to be 41 000 years for the upper sediment column (4–20 mbsf) and 580 000 years for the sediments as deep as 100 mbsf. They suggest a very old viral background community to persist in these sediments. For the SPG, we estimated half-lives of viral communities to be at least 10-fold higher. As the persistence of virus particles for up to tens of millions of years is questionable, the extreme half-life times rather confirm a continuous viral production which apparently overlays viral decay.
Viral biomass and the viral impact on subsurface carbon budget
After the recent recalculation of the global abundance of microbial cells in subseafloor sediments by Kallmeyer et al. (2012), the actual size of the deep biosphere is currently under debate (Hinrichs and Inagaki, 2012; Jørgensen, 2012; Kallmeyer et al., 2012). Depending on the approach, for example, quantification by CARD-FISH, qPCR (Biddle et al., 2006; Schippers et al., 2005) or analysis of intact polar lipids (Lipp et al., 2008), varying sizes of the bacterial and archaeal communities were determined. The quantification of viruses provides a novel and independent contribution to this debate. The high number of viruses supports the finding that cells are present and active within the deep biosphere.
Particularly in the oldest and extremely oligotrophic sediments, all quantification methods are close to their detection limits. Any variations in cell- and virus numbers, sizes and hence their carbon content would affect the virus-to-cell ratios and their biomass, respectively. In addition, the carbon content per cell encounters uncertainties that potentially change the global contribution of marine subsurface prokaryotic biomass (Hinrichs and Inagaki, 2012). However, by applying the so far most recent conversion factors of 0.2 fg per marine phage particle (Suttle, 2005) and 14 fg per prokaryotic cell (Kallmeyer et al., 2012), the amount of viral carbon would exceed the cellular organic carbon at virus-to-cell ratios >70. Thus, for the extreme old and oligotrophic sediments of the SPG with a virus-to-cell ratio of up to 225, viral biomass would equal or probably even exceed the amount of prokaryotic biomass. Even with a lower virus-to-cell ratio of up to 20 (continental margin sites 1227, 1230, U1344) viral-bound organic carbon would still represent a proportion of up to 30% of the total biomass. Thus, phage particles might represent a considerable reservoir of buried biomass. If the microbial community is capable to utilize slowly decaying phage particles, for example, proteins, the pool of bioavailable carbon would substantially be changed.
We conclude that phages are highly abundant in the marine subsurface and consistently outnumber prokaryotic cells. Particularly, in older and more oligotrophic sediments, viral biomass might represent a notable amount of buried organic carbon. The relative increase of viruses with depth is likely due to viral production coupled to diminished decay rates. Active viral communities would have a strong impact on the bioavailable carbon within the marine deep subsurface.
Beck M, Koester J, Engelen B, Holstein JM, Gittel A, Koenneke M et al (2009). Deep pore water profiles reflect enhanced microbial activity towards tidal flat margins. Ocean Dyn 59: 371–383.
Beck M, Riedel T, Graue J, Koester J, Kowalski N, Wu CS et al (2011). Imprint of past and present environmental conditions on microbiology and biogeochemistry of coastal Quaternary sediments. Biogeosciences 8: 55–68.
Biddle JF, Lipp JS, Lever MA, Lloyd KG, Sorensen KB, Anderson R et al (2006). Heterotrophic Archaea dominate sedimentary subsurface ecosystems off Peru. Proc Natl Acad Sci US A 103: 3846–3851.
D’Hondt S, Inagaki F, Zarikian CA Expedition 329 Scientists (2011), Proc. IODP, 329: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.329.2011.
D'Hondt S, Jørgensen BB, Miller DJ, Batzke A, Blake R, Cragg BA et al (2004). Distributions of microbial activities in deep subseafloor sediments. Science 306: 2216–2221.
D'Hondt S, Spivack AJ, Pockalny R, Ferdelman TG, Fischer JP, Kallmeyer J et al (2009). Subseafloor sedimentary life in the South Pacific Gyre. Proc Natl Acad Sci USA 106: 11651–11656.
Danovaro R, Dell'anno A, Trucco A, Serresi M, Vanucci S . (2001). Determination of virus abundance in marine sediments. Appl Environ Microbiol 67: 1384–1387.
Danovaro R, Dell'Anno A, Corinaldesi C, Magagnini M, Noble R, Tamburini C et al (2008). Major viral impact on the functioning of benthic deep-sea ecosystems. Nature 454: 1084–U1027.
Dowd SE, Pillai SD, Wang SY, Corapcioglu MY . (1998). Delineating the specific influence of virus isoelectric point and size on virus adsorption and transport through sandy soils. Appl Environ Microbiol 64: 405–410.
Engelhardt T, Sahlberg M, Cypionka H, Engelen B . (2011). Induction of prophages from deep-subseafloor bacteria. Environ Microbiol Rep 3: 459–465.
Engelhardt T, Sahlberg M, Cypionka H, Engelen B . (2013). Biogeography of Rhizobium radiobacter and distribution of associated temperate phages in deep subseafloor sediments. ISME J 7: 199–209.
Fischer UR, Weisz W, Wieltschnig C, Kirschner AKT, Velimirov B . (2004). Benthic and pelagic viral decay experiments: a model-based analysis and its applicability. Appl Environ Microbiol 70: 6706–6713.
Hinrichs K-U, Inagaki F . (2012). Downsizing the deep biosphere. Science 338: 204–205.
Hoehler TM, Jorgensen BB . (2013). Microbial life under extreme energy limitation. Nat Rev Micro 11: 83–94.
Jørgensen BB, D'Hondt S . (2006). Ecology–A starving majority deep beneath the seafloor. Science 314: 932–934.
Jørgensen BB . (2012). Shrinking majority of the deep biosphere. Proc Natl Acad Sci 109: 15976–15977.
Kallmeyer J, Smith DC, Spivack AJ, D'Hondt S . (2008). New cell extraction procedure applied to deep subsurface sediments. Limnol Oceanogr Methods 6: 236–245.
Kallmeyer J, Pockalny R, Adhikari RR, Smith DC, D'Hondt S . (2012). Global distribution of microbial abundance and biomass in subseafloor sediment. Proc Natl Acad Sci 109: 16213–16216.
Lipp JS, Morono Y, Inagaki F, Hinrichs K-U . (2008). Significant contribution of Archaea to extant biomass in marine subsurface sediments. Nature 454: 991–994.
Lunau M, Lemke A, Walther K, Martens-Habbena W, Simon M . (2005). An improved method for counting bacteria from sediments and turbid environments by epifluorescence microscopy. Environ Microbiol 7: 961–968.
Middelboe M, Glud RN, Finster K . (2003). Distribution of viruses and bacteria in relation to diagenetic activity in an estuarine sediment. Limnol Oceanogr 48: 1447–1456.
Middelboe M, Glud RN, Filippini M . (2011). Viral abundance and activity in the deep sub-seafloor biosphere. Aq Microbial Ecol 63: 1–8.
Morono Y, Terada T, Nishizawa M, Ito M, Hillion F, Takahata N et al (2011). Carbon and nitrogen assimilation in deep subseafloor microbial cells. Proc Natl Acad Sci US A 108: 18295–18300.
Noble RT, Fuhrman JA . (1998). Use of SYBR Green I for rapid epifluorescence coun of marine viruses and bacteria. Aq Microbial Ecol 14: 113–118.
Parkes RJ, Cragg BA, Wellsbury P . (2000). Recent studies on bacterial populations and processes in subseafloor sediments: a review. Hydrogeol J 8: 11–28.
Roy H, Kallmeyer J, Adhikari RR, Pockalny R, Jorgensen BB, D'Hondt S . (2012). Aerobic microbial respiration in 86-million-year-old deep-sea red clay. Science 336: 922–925.
Sambrotto RN, Mordy C, Zeeman SI, Stabeno PJ, Macklin SA . (2008). Physical forcing and nutrient conditions associated with patterns of Chl a and phytoplankton productivity in the southeastern Bering Sea during summer. Deep-Sea Res Part Ii-Topical Stud Oceanogr 55: 1745–1760.
Schippers A, Neretin LN, Kallmeyer J, Ferdelman TG, Cragg BA, Parkes RJ et al (2005). Prokaryotic cells of the deep sub-seafloor biosphere identified as living bacteria. Nature 433: 861–864.
Siem-Jørgensen M, Glud RN, Middelboe M . (2008). Viral dynamics in a coastal sediment: seasonal pattern, controlling factors and relations to the pelagic-benthic coupling. Marine Biol Res 4: 165–U120.
Suttle CA . (2005). Viruses in the sea. Nature 437: 356–361.
Wehrmann LM, Risgaard-Petersen N, Schrum HN, Walsh EA, Huh Y, Ikehara M et al (2011). Coupled organic and inorganic carbon cycling in the deep subseafloor sediment of the northeastern Bering Sea Slope (IODP Exp. 323). Chem Geol 284: 251–261.
Weinbauer MG . (2004). Ecology of prokaryotic viruses. FEMS Microbiol Rev 28: 127–181.
Weinbauer MG, Rassoulzadegan F . (2004). Are viruses driving microbial diversification and diversity? Environ Microbiol 6: 1–11.
Wellsbury P, Goodman K, Barth T, Cragg BA, Barnes SP, Parkes RJ . (1997). Deep marine biosphere fuelled by increasing organic matter availability during burial and heating. Nature 388: 573–576.
Wilhelm SW, Suttle CA . (1999). Viruses and nutrient cycles in the sea—viruses play critical roles in the structure and function of aquatic food webs. Bioscience 49: 781–788.
We thank the participants of ODP Leg 201, IODP Exp. 323 and Exp 329 for their contribution to obtain sample material and Erhard Rhiel for helping with the transmission electron microscope preparation. Steven D’Hondt is acknowledged for valuable comments on the manuscript. We thank Karsten Lettmann for suggestions of data analysis. This work was funded by IODP and the German Research Foundation (DFG).
The authors declare no conflict of interest.
TE and BE developed the ideas and planed the project. TE performed the sample preparation, virus and cell counting and data processing. JK provided additional cell counts. All authors (TE, BE, JK and HC) contributed to data interpretation and writing of the manuscript.
Supplementary Information accompanies this paper on The ISME Journal website
Rights and permissions
About this article
Cite this article
Engelhardt, T., Kallmeyer, J., Cypionka, H. et al. High virus-to-cell ratios indicate ongoing production of viruses in deep subsurface sediments. ISME J 8, 1503–1509 (2014). https://doi.org/10.1038/ismej.2013.245
- viral ecology
- South Pacific Gyre
- microbial abundance
This article is cited by
Ecogenomics reveals viral communities across the Challenger Deep oceanic trench
Communications Biology (2022)
An Appraisal of Bacteriophage Isolation Techniques from Environment
Microbial Ecology (2022)
Bacteriophage therapy in aquaculture: current status and future challenges
Folia Microbiologica (2022)
Hybrid genome de novo assembly with methylome analysis of the anaerobic thermophilic subsurface bacterium Thermanaerosceptrum fracticalcis strain DRI-13T
BMC Genomics (2021)
Ammonia-oxidizing archaea have similar power requirements in diverse marine oxic sediments
The ISME Journal (2021)