Intact preservation of environmental samples by freezing under an alternating magnetic field

An oscillating magnetic field suppresses ice-crystal growth during rapid freezing of muscle tissue of mice

Regenerative medicine would benefit from a safe and efficient cryopreservation method to prevent the structural disruption caused by ice-crystal formation in cells and tissue. Various attempts have been made to overcome this problem, one of which is the use of an oscillating magnetic field (OMF). However, the underlying mechanism is unclear. In this study, to evaluate the effect of an OMF on ice-crystal formation in the leg muscles of mice, we used to use the frozen-section method with a slower freezing rate than is, usual which resulted in ice crystals forming in the tissue. We assessed the mean size and number per unit area of intracellular ice holes in sections of muscle tissue, with and without OMF. Ice-crystal growth was reduced in frozen tissue subjected to OMF. Furthermore, we evaluated the structure and function of proteins in frozen tissue subjected to OMF by immunostaining using an anti-dystrophin antibody and by enzymatic histochemistry for NADH-TR and myosin ATPase. The results imply that the ability of OMF to suppress ice-crystal growth might be related to their stabilization of bound water in biomolecules during freezing.

Storage of soil microbiome for application in sustainable agriculture: prospects and challenges

Soil microbiome is a dynamic micro-ecosystem driving and fine-tuning several biological processes in the global macro-ecosystems. Its tremendous potential towards mediating sustainability in the ecosystem necessitates the urgent need to store it optimally and efficiently as "next-generation biologicals" for future applications via soil transplantation. The challenge, therefore, is to devise a strategy for the storage of soil microbiome such that its "functionality" is preserved for later application. This review discusses the current endeavours made towards storage of the soil microbiome. The methods for assessing the integrity of soil microbiome by targeting the structural diversity and functional potential of the preserved microbiomes have also been discussed. Further, the success stories related to the storage of fecal microbiome for application in transplants have also been highlighted. This is done primarily with the objective of learning lessons, and parallel application of the knowledge gained, in bringing about improvement in the research domain of soil microbiome storage. Subsequently, the limitations of current techniques of preservation have also been delineated. Further, the open questions in the area have been critically discussed. In conclusion, possible alternatives for storage, comprehensive analyses of the composition of the stored microbiome and their potential have been presented.

Temperature limits to deep subseafloor life in the Nankai Trough subduction zone

Microorganisms in marine subsurface sediments substantially contribute to global biomass. Sediments warmer than 40°C account for roughly half the marine sediment volume, but the processes mediated by microbial populations in these hard-to-access environments are poorly understood. We investigated microbial life in up to 1.2-kilometer-deep and up to 120°C hot sediments in the Nankai Trough subduction zone. Above 45°C, concentrations of vegetative cells drop two orders of magnitude and endospores become more than 6000 times more abundant than vegetative cells. Methane is biologically produced and oxidized until sediments reach 80° to 85°C. In 100° to 120°C sediments, isotopic evidence and increased cell concentrations demonstrate the activity of acetate-degrading hyperthermophiles. Above 45°C, populated zones alternate with zones up to 192 meters thick where microbes were undetectable.

A Recent Overview of Microbes and Microbiome Preservation

Microbes are mediators in almost all ecosystem processes and act as a pivotal game changer in various ecological activities, globally. Therefore, understanding of microbial community structure and related functions in different environmental and micro-environmental niches is not only critical, but also a matter of greatest importance. Due to our inability to cultivate and preserve all sorts of microorganisms, we are losing some ecologically and industrially relevant components of microbial community, due to extinction caused by environmental and climatic variations with time. Intact sample and microbiome preservation are crucial for future cultivation as well as to study the effects of ecological and climatic variations on community functionality and shift with time, using OMICS. Although, methods for pure culture preservation are almost optimized, the techniques of microbiome preservation still remain as an unsolved challenge for microbiologists due to technical and physiological constraints. Present article discusses, recent approaches of microbial preservation with special reference to intact sample, mixed culture and microbiome preservation. It also incorporates recent practices used to achieve the highest viability and metabolic activities in long-term preserved microbiome.

Methyl-compound use and slow growth characterize microbial life in 2-km-deep subseafloor coal and shale beds

The past decade of scientific ocean drilling has revealed seemingly ubiquitous, slow-growing microbial life within a range of deep biosphere habitats. Integrated Ocean Drilling Program Expedition 337 expanded these studies by successfully coring Miocene-aged coal beds 2 km below the seafloor hypothesized to be "hot spots" for microbial life. To characterize the activity of coal-associated microorganisms from this site, a series of stable isotope probing (SIP) experiments were conducted using intact pieces of coal and overlying shale incubated at in situ temperatures (45 °C). The 30-month SIP incubations were amended with deuterated water as a passive tracer for growth and different combinations of ¹³C- or ¹⁵N-labeled methanol, methylamine, and ammonium added at low (micromolar) concentrations to investigate methylotrophy in the deep subseafloor biosphere. Although the cell densities were low (50-2,000 cells per cubic centimeter), bulk geochemical measurements and single-cell-targeted nanometer-scale secondary ion mass spectrometry demonstrated active metabolism of methylated substrates by the thermally adapted microbial assemblage, with differing substrate utilization profiles between coal and shale incubations. The conversion of labeled methylamine and methanol was predominantly through heterotrophic processes, with only minor stimulation of methanogenesis. These findings were consistent with in situ and incubation 16S rRNA gene surveys. Microbial growth estimates in the incubations ranged from several months to over 100 y, representing some of the slowest direct measurements of environmental microbial biosynthesis rates. Collectively, these data highlight a small, but viable, deep coal bed biosphere characterized by extremely slow-growing heterotrophs that can utilize a diverse range of carbon and nitrogen substrates.

Coupling Mechanism of Electromagnetic Field and Thermal Stress on Drosophila melanogaster

Temperature is an important factor in research on the biological effects of extremely low-frequency electromagnetic field (ELF-EMF), but interactions between ELF-EMF and temperature remain unknown. The effects of ELF-EMF (50 Hz, 3 mT) on the lifespan, locomotion, heat shock response (HSR), and oxidative stress (OS) of Canton-Special (CS) and mutant w1118 flies were investigated at 25°C and 35°C (thermal stress). Results showed that thermal stress accelerated the death rates of CS and w1118 flies, shortened their lifespan, and influenced their locomotion rhythm and activity. The upregulated expression levels of heat shock protein (HSP) 22, HSP26, and HSP70 indicated that HSR was enhanced. Thermal stress-induced OS response increased malondialdehyde content, enhanced superoxide dismutase activity, and decreased reactive oxygen species level. The effects of thermal stress on the death rates, lifespan, locomotion, and HSP gene expression of flies, especially w1118 line, were also enhanced by ELF-EMF. In conclusion, thermal stress weakened the physiological function and promoted the HSR and OS of flies. ELF-EMF aggravated damages and enhanced thermal stress-induced HSP and OS response. Therefore, thermal stress and ELF-EMF elicited a synergistic effect.