Обзор:Диапазон слышимых частот: 20Hz-20kHz. The range of audible frequencies
A Low Temperature Limit for Life on Earth
My name is Anna. I am single and I do not have children, but I would love to have 2 in the 2.
I speak English.Диапазон слышимых частот: 20Hz-20kHz. The range of audible frequencies
2 am charming, attractive, kind, positive and romantic person.
There is no 2 accepted value for the lower temperature limit for life on Страница. We present empirical evidence that free-living microbial cells cooling in the presence of external ice will 2 freeze-induced desiccation and a glass transition (vitrification) at a temperature between −10.
Anna, 30, Moscow, Russia
100 s DE Dimmbar IT Funzionare con variatori specifici FR Fonction qu´avec certains variateurs GB Can be dimmed on specific dimmers CZ Stmívatelné PL Z możli Áością ściemniania SI Primerno za zunanjo ali industrijsko uporabo. HU Szabálozható fénerejű RU Плавная регулировка яркости NL
Online Real Estate and Property Search.
*Land Use is for valuation purposes only. Consult the local jurisdiction for zoning and legal use.
These UPK II-Cre transgenic mice have the mouse uroplakin 2 ( Upk2 ) gene promoter driving Cre recombinase expression in the bladder urothelium. These mice may be useful for Cre-lox studies of urothelium function and cancers of the bladder.
Initial phase of mid-latitude aurora during strong geomagnetic storms A.V. Mikhalev a,c,*, Jiyao Xu b,c, V.I. Degtyarev a,c, Wei Yuan b,c a Institute of Solar-Terrestrial Physics, Russian Academy of Sciences, Siberian Branch, Irkutsk, Russia
T dj - lZjbn gZ khhl\_lkl\mxsbc dhffmgZevguc j_kmjk mklZgh\e_gguc \ khhl\_lkl\bb k aZdhgh^Zl_evkl\hf Jhkkbckdhc N_^_jZpbb.
JZkq_lH>G 13 NhjfmeZ
В общем, понятно, что живет Людмила Путина после развода не на одну только пенсию. О чем свидетельствует и нить жемчуга, которая была на ней во время ее последнего выхода в люди.
Россия перестала молчать, как это было в девяностые при уничтожении Югославии. Россия снова заявляет о себе и заставляет считаться со своими интересами во внешней политике.
OME YEAR MANUFACTURERS WARRANTY' PARTS W STOCK' $ FIN'NCWG OPTIONS ONE MANUFACTURERS WARRANTY! PARTS W STOCK' $ FINANCING OPTIONS AVAILABLE The Green Climber is a hardcore mower capable Of taming the steepest slopes up to 60 degrees in PLOS ONE promises fair, rigorous peer review, broad scope, and wide readership — a perfect fit for your research every time.
For more information about PLOS Subject Areas, click.
Price Abstract There is no generally accepted value for the lower temperature limit for life on Earth.
In contrast to intracellular freezing, vitrification does not result in death and cells may survive very low temperatures once vitrified.
The high internal viscosity following vitrification means that diffusion of oxygen and metabolites is slowed to such an extent that cellular metabolism ceases.
The temperature range for intracellular vitrification makes this a process of fundamental ecological significance for free-living microbes.
It is only where extracellular ice is not present that cells can continue to metabolise below these temperatures, and water droplets in clouds provide an important example of such a habitat.
In multicellular organisms the cells are isolated from ice in the environment, and the major factor dictating how they respond to low temperature is the physical state of the extracellular fluid.
Where this fluid freezes, then the cells will dehydrate 2 vitrify in a manner analogous to free-living microbes.
Where the extracellular fluid undercools then cells can continue to metabolise, albeit slowly, to temperatures below the vitrification temperature of free-living microbes.
Citation: Clarke A, Morris GJ, Fonseca F, Murray BJ, Acton E, Price HC 2013 A Low Temperature Limit for Life on Earth.
PLoS ONE 8 6 : e66207.
This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, 2 the original author and source are credited.
The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have the following interests.
John Morris receives a salary from Asymptote.
The work described in the paper was entirely without the activities of Asymptote.
Introduction Biologists have long been interested in the physical limits to life, particularly in relation to life in extreme environments on Earth and the possibility of life elsewhere in the universe.
Whereas the high temperature limit to cell division is fairly well definedthe lower limits for life are essentially unknown.
Here адрес present theoretical arguments and empirical evidence which clarify the biophysical constraints that determine the lower temperature limit for life on earth.
Theoretical Background: Life at Low Temperatures Philosophers and scientists have struggled to achieve a universally accepted definition of life.
In considering life at extremes, however, a critical distinction is that between metabolism and replication reproductionas emphasised by von Neumann.
An essential feature of life is completion of the life cycle; for a bacterium or archaean this means cell division to produce daughter cells, for a sexually reproducing eukaryote it means completion of the cycle from zygote to zygote.
An organism may, of course, continue to metabolise even when it is unable to complete its life cycle.
We can therefore draw an important distinction between two different threshold temperatures: a threshold for completion of the life cycle, T L, and a threshold for metabolism, T M.
Between T L and T M, the organism is viable and metabolising, but unable to complete its life cycle; the difference between the lower bounds T L and T M is especially important in extreme low-temperature environments.
A third important threshold is that for survival, T S, although this does not exhibit a consistent relationship with T L or T M: the lower T S may be at T L, at T M or below T M.
Thus in a chilling-sensitive organism, a critical physiological system fails at a relatively high temperature, and T S, T L and T M may even coincide.
By contrast, in a cold-hardy organism, T S may be below T M.
Between T M and T S the organism is in a state of suspended animation, but can resume metabolism once the temperature increases and re-crosses the T M threshold.
An important difference between the high and low temperature limits for life is that at high temperatures T S is always reached; in contrast at low temperatures an organism may never reach its T S, even when taken close to absolute zero.
The upper and lower T L thresholds thus mark the limits to life on Earth, as existence outside these boundaries does not allow for completion of the life Пояс Дед Мороз пуговка />Temperature limits for life.
T L: temperature limit for completion of the life cycle, T M: temperature limit for metabolism, T S: temperature limit for survival.
Note that T S can be above, at, or below T M.
The shaded area shows temperature range over which the organism can complete its life cycle, and the white areas show the temperature range upper and lower for survival.
T opt is the temperature at which growth rate is maximal, which is typically closer to the upper T L than the lower T L.
Cells at low temperatures must cope with the reduced molecular kinetic energy of the environment and the consequent lower rate of many physical processes.
In addition there are stresses arising from reduced membrane fluidity, changes in intracellular pH, and loss of macromolecular больше информации .
Additional challenges arise when ice is present in the environment immediately external to the cell.
Following ice nucleation, solutes are rejected from the growing ice crystal and are concentrated in the remaining liquid; importantly, microorganisms will also be excluded from the ice lattice.
Cells may be damaged in the presence of extracellular ice through hydraulic, osmotic or solute toxicity mechanisms.
In addition, intracellular ice can form when the cooling rate is sufficiently high that the cell cannot maintain osmotic equilibrium with the environment.
Intracellular ice formation generally requires faster cooling than is typical of the natural environment.
Intracellular ice is observed only rarely in the natural environmentalthough freezing of extracellular fluids does occur in some multicellular plants and animals living in seasonally cold climates —.
Structure of ice and cells по этой ссылке cooling of a cell suspension.
Cryo scanning electron microscopy of fracture samples of Lactobacillus delbrueckii ssp.
Low power image of a fractured sample, showing cells confined to the unfrozen liquid between ice crystals; this unfrozen matrix is highly freeze-concentrated as solutes are excluded перейти the growing ice crystal.
High power image of the interface between ice and the freeze concentrated matrix, with bacterial cells labelled.
Freeze substitution of the same sample reveals cells packed within the freeze concentrated matrix.
In all samples the spaces originally occupied by ice crystals are revealed as voids following sublimation of ice.
Vitrification also known as the glass transition occurs when a liquid begins to behave as a solid during cooling, but without any substantial change in molecular arrangement or thermodynamic state variables.
As temperature decreases, all molecular motions, translational 2 internal, become progressively slower until a critical temperature is reached where there is insufficient energy for significant translational or rotational molecular motion to take place over a meaningful timescale.
This is the vitrification or glass transition temperature, Tg, and it is defined operationally as the temperature at which viscosity exceeds 10 12 Pa.
Thermodynamic state variables pressure, volume, internal energy, entropy change minimally during the glass transition: vitrification thus does not involve the entropy change and associated exotherm associated with freezing.
There are, however, changes in thermodynamic response variables such as heat capacity and thermal expansivity, and the glass transition can be detected by differential scanning calorimetry DSC from this change in heat capacity.
Intracellular vitrification is more complex than in simple bulk liquids.
This is principally because the interior of the cell is extremely crowdedapproximating a colloid in physical structure.
As colloids dehydrate they exhibit a sharp increase in viscosity and undergo a colloid glass transition.
Cellular dehydration, whether associated with a shift to anhydrobiosis or withdrawal of water driven by freeze concentration of the extracellular medium seewill thus induce vitrification of the cell interior.
Intracellular vitrification is primarily the result of this dehydration and is analogous to the vitrification of a colloid, rather than the glass transition in bulk water.
The low rates of cooling characteristic of the natural environment coupled with the dehydration of the intracellular milieu driven by freeze concentration of the extracellular medium means that outside the laboratory vitrification of the cell contents will almost always occur before intracellular ice can form, and is likely to be a process of widespread ecological significance for free-living unicells.
Vitrification has however not been widely reported from the natural environment, probably because it is technically difficult to demonstrate.
It can, however, be detected with a sensitive DSC from the variation in heat flow associated with the change in heat capacity at the glass transition.
We have investigated the incidence of vitrification in a range of unicellular organisms.
The aim of the study was to determine the incidence of vitrification in unicellular organisms cooled slowly in the presence of extracellular ice.
Materials and Methods Intracellular glass transition temperature, Tg, was determined with differential scanning calorimetry Diamond, Perkin Elmer LLC, Norwalk, CT, USA, equipped with a liquid nitrogen cooling accessory, CryoFill, Perkin Elmer.
The cell types selected comprised five bacteria: Lactobacillus delbrueckii ssp.
The protocol for temperature calibration and determination of the glass transition temperatures is described elsewhere.
Cell suspensions were examined in the frozen state using cryo scanning electron microscopy CryoSEM and freeze substitution, as described previously .
Cells were also examined by Raman spectroscopy on a humidity controlled microscope stage, as the Ссылка spectrum allows unambiguous identification of chemical compounds and phase changes.
Cell suspensions were mounted on a silanised glass cover slip, which has been shown previously not to catalyse nucleation.
The chamber was constructed of Teflon and sealed on the base with an O-ring.
The sample was viewed through a window on top of the chamber.
The humidity in the nitrogen flowing over the cells was controlled by passing nitrogen gas through a bubbler immersed in a temperature controlled bath and diluted using mass flow controllers MKS 1179 to produce the desired humidity.
The temperature of the stage по этой ссылке set using a re-circulating chiller and the temperature of the sample was measured with a platinum resistance thermometer embedded in the stage immediately below the sample.
The experiments were performed with a 514 nm laser coupled to a Renishaw inVia Raman microscope system equipped with a Leica microscope and Olympus 20× long working distance objective.
The experimental protocol is described in detail in.
To provide an environmental context for the vitrification study we also modelled the thermal properties 2 water droplets of the sizes found in clouds and likely to effect dispersal of microbial cells.
The modelling assumed homogeneous freezing , ANS009, узкий, привожу ссылку, велкро, безразмерный be a stochastic process.
Parameterisations to describe the temperature dependence of the water activity of the liquid at the ice-liquid equilibrium line and the dependence of the nucleation rate coefficient with the shift in water activity from the ice-liquid equilibrium line were taken fromand we modelled the water activity at which we expect 50% of a population of droplets of a given size in a given time to freeze.
The method is described in detail elsewhere.
The thermal histories within droplets of water of various sizes following ice nucleation at different degrees of undercooling were modelled on the assumption that initial ice formation is isenthalpic.
Results Using sensitive DSC, we have measured the intracellular glass transition vitrification temperature, Tg, in a range of cell types when cooled slowly in the presence of extracellular ice.
Under the experimental conditions used, any intracellular freezing would have been detected by the release of latent heat associated with the change in entropy that accompanies the phase transition from liquid water to ice in the cell during cooling, or the reverse during warming; none was seen.
Vitrification was detected by the variation in heat flow associated with the change in heat capacity, together with the absence of any release of latent heat.
No vitrification signal was seen in control runs medium without cells see.
Any glass transition events in the extracellular compartment would be expected to be at a lower temperature, but were not detected in this study because the volume of extracellular medium was so low in relation to that of the cells as to render any Tg signal undetectable.
Differential scanning calorimetry DSC traces showing vitrification in cell suspensions.
DSC trace of Lactobacillus delbrueckii ssp.
The glass transition during warming is indicated by the deviation in the first derivative of the heat flow, associated with a change in heat capacity as the bacterial cells devitrify at Tg.
The large increase in heat flow at temperatures above Tg corresponds to the freezing of the aqueous medium in which the cells were suspended.
Composite of DSC traces from four organisms three bacteria, and an alga.
The traces have been scaled as shown to render them visible on a single ordinate scale.
In all cell types examined, intracellular vitrification occurred 2 high sub-zero temperatureswith no sign of intracellular freezing.
All cell types are viable after vitrification under these experimental conditions Morris, unpublished data.
These temperatures are well above typical environmental temperatures for high latitudes in winter, indicating that intracellular vitrification must be a process of widespread ecological relevance for free-living unicells.
Intracellular vitrification temperature for a range of free-living microorganisms.
Vitrified algal cells were examined by Raman spectroscopy on a humidity controlled microscope https://chmall.ru/100/doy-pak-zipgripper-110mm185mm-kraft-40gr-fakturniy-s-polipropilenovim-oknom-shirinoy-70mm-i-dn.html />Control samples of sucrose solution exhibited a clear Raman water peak that responded to external relative humidity, but this response ceased once the solution vitrified at low relative humidity.
In contrast, the vitrified cells appeared to be completely unresponsive to relative humidity, and the Raman signal indicated that these cells contained little or no bulk water.
Discussion Читать статью data presented here are, to our knowledge, the first direct evidence of intracellular vitrification in a cell suspension under ecologically relevant conditions, that is in a dilute aqueous medium and the absence of external cryoprotectants.
Vitrification was observed in all cell types examined, and intracellular freezing was observed in none.
The rates of cooling required to induce intracellular freezing are generally only experienced by cells in certain specialised habitats such as leaf surfaces see на этой странице />Chilling-sensitive species do not vitrify, for as the temperature falls they reach their T S and die before ice forms in their environment.
For cells to vitrify they must remain osmotically active at subzero temperatures.
The importance of this is exemplified by species of the unicellular alga Chlamydonomas: whereas the temperate Chlamydomonas reinhardtii is intolerant of cooling to low temperatures, the snow alga C.
These physiological differences are associated with differences in membrane composition, structure and function .
In cells that remain osmotically active when ice is present in their immediate external environment a critical factor driving an intracellular colloidal glass transition is the presence of proteins and other macromolecular structures.
As water is withdrawn from the cell interior, driven by freeze concentration of the extracellular medium, its internal water activity decreases see.
However the cell also contains a large number of small molecules, including some which may be synthesised to act as cryoprotectants.
The vitrification temperature will thus vary somewhat with the precise composition of the internal cell environment, and this may allow Tg to be adjusted to match ecological circumstances for example by varying the level of small cryoprotectant molecules.
The second key factor which determines that a cell will vitrify at low water activity is the densely packed interior of the cell.
The colloidal nature of the intracellular milieu means that as water is removed, the increased packing slows intracellular relaxation processes.
There is a sharp increase in intracellular viscosity and the cell undergoes a colloid glass transition.
The vitrification of the cell interior of a free-living microbial cell exposed to ice in the external environment is thus primarily the result of dehydration and is analogous to the vitrification of a colloid rather than the glass transition of bulk water.
Although our data indicate that vitrification is inevitable for any free-living microbial cell cooled in the presence of external ice, the range of Tg values found in this study indicates that the exact value of Tg varies, presumably in response to changes in the balance between macromolecules predominantly proteins and small molecular weight compounds, including cryoprotectants.
The relatively high value for Tg found in the ice-nucleating bacterium Pseudomonas syringae and the low value found in the snow alga Chlamydomonas nivalis suggest that Tg may be adjusted, within bounds, in response to the particular ecology of the individual organism.
An organism such as C.
Once vitrification has taken place, the high viscosity of the intracellular medium means that diffusion of oxygen and metabolites effectively stops.
Under these conditions metabolism must спорно, Сэм Уолтон Как я создал Walmart мне />These cells, however, remain viable and can return to metabolism and growth once they have warmed above their Tg.
The importance of vitrification to the survival of cells at low temperature is that the glass transition does not involve the change in density that accompanies nucleation and freezing.
A cell that freezes is subject to enormous mechanical stresses, which are frequently lethal.
A cell that vitrifies is also behaving effectively as a solid, but retains its internal structure and integrity.
It is this maintenance of internal structure that is the key factor in allowing a return to viability once an increase in environmental temperature drives the resumption of molecular movement and hence metabolism.
There is remarkably little difference between vitrified and living cells in terms of bulk structure, composition and thermodynamic state variables.
These observations also have implications for cell recovery following cryopreservation and freeze drying.
It is usually assumed that cells dehydrate as a function of the increasing concentration of the extracellular medium until the latter vitrifies.
At temperatures below Tg cells will be osmotically unresponsive as the extracellular concentration continues to increase and cells will not respond osmotically during warming until the intracellular environment has returned to the fluid state.
Small molecular weight cryoprotectants would be expected to modify intracellular Tg, and this might be a factor in their mode of protection.
Microbial Metabolism in Glacial Environments The rapidly developing interest in the possibility of life in deep subglacial lakes or on bodies such as Mars or Europa has focussed considerable attention on life in glacial environments.
Microbial cell division has been reported to continue at subzero temperatures, though it is likely that cell doubling times at these temperatures may be very long.
In environments where ice is present but the temperature is above Tg, osmotically active cells continue to metabolise, albeit at a slow rate.
Examples of such habitats from the natural environment include cryoconite holes on glacier surfaces and high latitude saline lakes, though in these environments growth and cell division typically only proceed when temperatures increase for example in surface waters during summer —.
A wide variety of microbial cells has also been reported from glacial ice .
Metabolism has, however, been proposed for microbial cells in glacial ice, albeit at very slow rates, on the basis of anomalously high concentrations of methane and nitrous oxide.
Temperature data from ice cores suggest that throughout much of the upper depths of continental ice caps, temperature is below Tg and hence cells will be vitrified.
It is only towards the base of the ice sheet, where temperatures are higher because of the upward transfer of geothermal heat, that temperatures are sufficiently high for cells to be above their Tg.
Any discussion of putative biological activity within glacial ice has to confront the difficulty of distinguishing metabolism from purely geochemical activity.
The unfrozen water between ice crystals surrounding the cell will have solutes in multimolar concentrations, the pH will be highly modified and there may be extracellular enzymes present.
адрес страницы these conditions, chemical kinetics are greatly modified; many reactions are accelerated and new reaction products may be generated which can 2 apparent metabolic products.
Temperature profile through an ice core taken at Dome C, Antarctica.
Data are averaged over bins of 5 m.
The dotted lines show a putative threshold depth above which cells will be vitrified and hence not metabolising, and below which cells may be in a fluid state and able to metabolise, albeit slowly.
At the bottom of the ice core the temperature may be sufficient for cell growth and division to be possible, assuming the presence of sufficient free energy suitable electron donors and acceptors and a source of nutrients.
Core temperature data courtesy of the European Project for Ice Coring in Antarctica, EPICA.
In this environment any microbial cells present may continue to metabolise, albeit very slowly.
This is possible because in the absence of freeze-induced dehydration the internal cell contents to not undergo vitrification.
Cloud droplets thus offer a natural habitat, possibly the only such habitat on Earth, where microbial cells can continue to metabolise at temperatures below those at which in other environments they would normally vitrify.
They may even be able to undergo cell division .
The ecological importance of this is that viable microbial cells within clouds can be dispersed globally.
Cells in undercooled cloud droplets are, however, extremely susceptible to being killed by intracellular ice formation should the droplet nucleate.
Once nucleation has been initiated, droplet temperature will first rise to посетить страницу melting temperature as latent heat is released; this will be Diploma Programme IB Higher Level Option Sets, Relations and by extremely rapid cooling as the ice droplet achieves thermal equilibrium with больше информации atmospheric environment.
Temperature following nucleation of water droplets of different sizes.
This как сообщается здесь is avoided if the droplet nucleates at high sub-zero temperatures when it is only slightly undercooled, as any microbial cells it contains will then undergo freeze-concentration dehydration and vitrify.
This may even be induced by the bacterial cells themselves, mediated through ice-nucleating proteins on the external surface .
Should this happen then the droplet will freeze at a relatively high sub-zero temperature, leading to freeze-concentration of the extracellular water and osmotic dehydration of any microbial больше на странице in the droplet.
Under these circumstances the cell contents will vitrify rather than freeze, and the microbial cells would be expected to survive further cooling note the relatively high value for Tg in the ice-nucleating bacterium Pseudomonas syringae:.
This emphasises the survival value for airborne bacteria of initiating nucleation, and offers a simple explanation for the high levels of viable bacteria with ice-nucleating activity that can be isolated from snow and hailstones —.
The likelihood of intracellular freezing among microbial cells without ice-nucleating activity in cloud droplets will also constrain the ability of such cells to be dispersed globally.
There have been a number of reports that microorganisms isolated from polar environments contain intracellular antifreeze proteins.
It has been argued that the function of these compounds is to protect the cell from lethal injury during cooling by preventing intracellular freezing.
These compounds are, however, typically identified as antifreezes on the basis of their activity in vitro; in most cases we do not know their function in vivo.
Moreover, outside 2 laboratory intracellular freezing is rare, usually requiring cooling rates faster than typical of the natural environment, and is almost always lethal.
Our data indicate that under natural rates of cooling, and in the presence of extracellular ice, free-living microbial cells will vitrify and intracellular ice formation is not a normal event.
This poses the evolutionary question of why such cells should have an antifreeze.
One speculative possibility is that their antifreeze activity may be important in reducing the chances of potentially fatal ice nucleation during warming from the vitrified state.
It is also possible that these proteins have other physiological functions and their antifreeze activity is simply coincidental.
The interesting question подробнее на этой странице thus whether proteins with incidental antifreeze activity are also to be found in cells where subzero temperatures are never encountered.
Implications for Multicellular Organisms We have demonstrated vitrification in a range of free-living unicellular organisms.
These cells all remained osmotically responsive at subzero temperatures and all underwent a glass transition; in addition all the cell lines studies are viable following rewarming from the vitrification protocol used in this study Morris, unpublished data.
There is no evidence that microbial and multicellular organisms differ significantly in their intracellular composition, and so we can assume that the fundamental thermal behaviour of cells from multicellular organisms will be similar to that of free-living microbes.
When ice is present in the environment immediately external to the cells, the cells will dehydrate as an osmotic response to the freeze-concentration of the remaining fluid and once temperature falls to Tg the cells will undergo a colloid glass transition vitrification.
A key difference for multicellular organisms is, however, that the environment immediately external to the cells is a fluid whose composition is controlled by the organism.
The important factor that determines whether a cell in a multicellular organism vitrifies is the presence or absence of ice in the extracellular fluid.
For a multicellular organism, the presence of ice in the external environment that is, outside the organism is relevant only in Палантин жен.
шелк+виск 70х180 LSZ34-923-19#G Labbra it has the potential to inoculate freezing within the organism.
Intracellular vitrification has long been recognised as a survival mechanism for desiccation-tolerant organisms, for seeds of plants and resting stages of other organisms.
Our results suggest that vitrification will also occur in the cells of those cold-hardy plants and animals where the extracellular fluids freeze at a high sub-zero temperature.
Should this occur it will lead to a freeze concentration of the unfrozen extracellular fluid, dehydration of the cell interior, and a colloid glass-transition in a manner directly analogous to that demonstrated here for free-living microbial organisms.
A clear demonstration of the ecological importance of vitrification in multicellular organisms comes from studies of polar nematodes.
Nematodes in general are highly tolerant of dehydration and their internal water content can change rapidly in response to external conditions.
Our results suggest that the nematodes suspended in water would have undergone freeze-induced dehydration as the water droplet froze, and a colloid glass transition.
The vitrified nematodes showed generally good survival, whereas the frozen nematodes did not.
Furthermore, polar nematodes can survive very long periods in the vitrified state.
Laboratory studies have shown, however, that survival from freezing is extremely sensitive to cooling rate.
Our results for free-living microbes suggest that the freezing of the extracellular fluid will dehydrate the cells and promote a colloid glass transition, and it is possible that the threshold cooling rate for survival is dictated by the dynamics of osmotic adjustment by the cells.
When cooling is sufficiently slow to allow osmotic adjustment, cells dehydrate and vitrify; when cooling is too fast cells are unable to adjust and the result is lethal intracellular freezing.
Since the capacity for osmotic adjustment depends on factors such as membrane composition and the density of aquaporins, we would expect the threshold cooling rate for survival to vary between species.
Many organisms living in seasonally cold environments avoid freeze-induced desiccation and vitrification of tissues through undercooling of the extracellular fluids.
Insects that move into subnivean habitats may even reproduce in winterthough this is only at relatively high sub-zero temperatures, and well above the vitrification temperatures reported here for free-living microbial cells.
In many invertebrates that avoid freezing of extracellular fluids, the presence of high concentrations of small molecular weight cryoprotectant compounds means that cells may continue to metabolise down to very low temperatures.
In the Alaskan beetle Cucujus clavipes, some individuals exhibit two vitrification events, suggestive of two separate compartments each with a different Tg.
It is tempting to speculate that this may represent the vitrification of the extracellular fluids and the intracellular matrix as separate events.
These insect larvae survive vitrification, even when overwintering in direct contact with ice.
The fundamental biophysics of freeze-concentration and consequent colloid glass transition must apply also to plant cells, although their different ionic composition together with the presence of chloroplasts, vacuoles and starch granules mean that thermal thresholds may differ from animal and bacterial cells.
Our results for free-living microbes suggest that vitrification will also occur in the cells of cold-hardy plants where the extracellular fluids freeze.
Where these fluids undercool, the vitrification temperature will be lowered, but, as observed with insectsa glass transition will still eventually take place as cooling continues.
Vitrification has been demonstrated in cortical cells of winter-hardened Populus balsamiferaand suggested to be widespread among northern долгих Блок монтажный с крюком TOR HQG(L) K1-5,0 т разделяю and cold-hardy woody plants .
Interestingly, plants also show multiple vitrification events, suggesting that different fluid compartments undergo a glass transition at different temperatures, depending on their water content.
Organisms tolerant of extreme dehydration, such as nematodes, tardigrades or rotifers may lose their cell water through desiccation at temperatures well above zero.
The resultant low water activity of the intracellular environment means that these cells will vitrify in essentially the same manner as with freeze-concentration desiccation.
In both cases vitrification is driven by the dehydration of the cell interior.
Vitrification has been reported from desiccated stages of multicellular organisms such as rotifers, tardigrades and the crustacean Artemia —.
Here, vitrification is again driven by the removal of water and the consequent colloid glass transition.
This desiccation-induced vitrification can occur at temperature well above 0°C, though the vitrified organisms may then be resistant to subsequent exposure to very low temperatures.
Vitrification thus provides a mechanistic explanation for the similarity of the physiological effects of two environmental factors which have long been recognised as related, namely desiccation and the freezing of the extracellular environment.
Plants subject to dehydration water stress synthesise a range of proteins late embryogenesis abundant proteins, LEAs, and dehydrins that appear to be critical in maintaining cellular structure in the dehydrated state .
These proteins have now been recorded from a range of animal phylasuggesting that, together with small molecular weight cryoprotectants, they may play an important general role in maintaining cellular structure during vitrification, such that по этой ссылке can resume in a controlled manner once https://chmall.ru/100/lestnitsa-lwi-3h10-trehsektsionnaya.html cell rehydrates.
Concluding Remarks On the surface of the earth, ice will invariably be present once the environmental temperature falls below 0°C .
We conclude that intracellular vitrification is a process of universal ecological significance for free-living microbial organisms living in uniformly or seasonally cold environments.
In contrast, intracellular ice formation is not.
Some multicellular organisms may induce their extracellular fluids to freeze at relatively high sub-zero temperatures, and we propose that this will drive a similar vitrification of their cells.
Others may promote undercooling of their extracellular fluids.
In these cases, cells may continue to metabolise down to lower temperatures, but evidence from both plants and нажмите для деталей indicates that eventually vitrification again takes place.
Since organisms must return to the fluid state to resume metabolism and complete their life cycle, vitrification thus represents an operational and absolute lower temperature threshold for life on Earth.
Our data point to an interesting asymmetry in the high and low temperature limits for life on Earth.
However the ability of multicellular organisms to regulate their internal body fluids means that some terrestrial species living in permanently or seasonally cold environments can allow these fluids to undercool, and hence their cells to metabolise, down to temperatures well below the lower thermal limit for growth in free-living microbes.
Undercooling is not an option for страница organisms, where ice is almost invariably present in the environment once the temperature drops below 0°C.
We therefore suggest that any proposal for metabolising cells under these conditions must meet a minimal set of criteria to distinguish true metabolism from geochemical processes that mimic metabolism.
A possible set of criteria might include some or all of: Utilisation of an electron donor Reduction of an electron acceptor Maintenance of membrane potential and protonmotive force Synthesis of ATP Transport of metabolites across the cell membrane Membrane viability Ribosomal viability.
Unless these criteria can be met, we must assume that what is being measured is concentrated solution chemistry and not integrated metabolism.
Our results also imply that for any cells with an intracellular milieu similar to that of cells on Earth the window of opportunity for metabolism to proceed in the present climate on Mars is very limited indeed.
It would, however, seem perfectly possible, given sufficient free energy, for cells to exist and metabolise in the water hypothesised to exist below the surface ice layer on Europa.
Furthermore, our results suggest that microbial cells could feasibly be transferred across посетить страницу space were they to be transported in water 2 sufficient solutes to induce dehydration of the cells through freeze concentration, and thereby promote vitrification.
The equilibrium relationship between ice and water activity a W of the solution in contact with ice for a range of sub-zero temperatures solid symbols.
Also перейти на страницу is the calculated homogeneous nucleation temperature of bacterial cells 1 µm diameter in osmotic equilibrium with ice open symbols.
подумал Чернила (краска) Ink-mate EIM-200 для Epson: Stylus, WorkForce, WorkForce Pro - 100 гр.
4 штуки. нужные low temperatures.
TIF A left panel.
Comparison of control DSC trace peptone water only with sample run Lactobacillus delbrueckii 2 />Note the strong freezing exotherm during cooling, the melting endotherm during warming and the absence of any vitrification проходной коллектор с отводами (ТР) FAR />TIF Frequency histograms of rates of environmental temperature change.
Conservative estimates based on mean hourly data.
Less conservative estimates, based on maximum and minimum temperatures observed in each hour.
TIF Acknowledgments We thank Sarah Acton and Stephanie Gibbons for reading the typescript and Stéphanie Cenard for cell cultures.
We also thank Nick Lane and three anonymous referees for valuable and perceptive comments that improved the paper significantly.
Author Contributions Conceived and designed the experiments: AC GJM FF BJM EA.
Performed the experiments: GJM FF BJM EA HCP.
Analyzed the data: AC GJM FF BJM EA HCP.
Wrote the paper: AC GJM.
Commented on all drafts of the paper: AC GJM FF BJM EA HCP.
Kashefi K, Lovley DR 2003 Extending the upper temperature limit for life.
Science 301 5635 : 934—934.
Pace NR 2001 The universal nature of biochemistry.
Proceedings of the National Academy of Sciences of the United States of America 98 3 : 805—808.
Kerry KR, Grace DR, Williams R, Burton HR 1977 Studies on some saline lakes of the Vestfold Hills, Antarctica.
In: Llano GA, editor.
Adaptations within Antarctic ecosystems.
Tominaga H, Fukui F 1981 Saline lakes in Syowa Oasis, Antarctica.
Hydrobiologia 82 3 : 375—389.
Murray AE, Kenig F, Fritsen CH, McKay CP, Cawley KM, et al.
Proceedings of the National Academy of Sciences of the United States of America 109 50 : 20626—20631.
Schroeter B, Green TGA, Kappen L, Seppelt RD 1994 Carbon dioxide exchange at subzero temperatures: field measurements in Umbilicaria aprina in Antarctica.
Cryptogamic Botany 4 2 по этой ссылке 233—241.
Collins MA, Buick RK 1989 Effect of temperature on the spoilage of stored peas by Rhodotorula glutinis.
Food Microbiology 6 3 : 135—141.
Rivkina EM, Friedmann EI, McKay CP, Gilichinsky D 2000 Metabolic activity of permafrost bacteria below the freezing point.
Applied and Environmental Microbiology 66 8 : 3230—3233.
Astrobiology 3 2 : 343—350.
Benner SA 2010 Defining life.
Astrobiology 10 10 : 1021—1030.
In: Jeffress LA, editor.
Cerebral mechanisms in behavior; the Hixon symposium.
New 2 John Wiley.
Morowitz HJ 1978 Foundations of bioenergetics.
Academic Press, New York, 344 p.
Hochachka PW, Somero GN 2002 Biochemical adaptation: mechanism and process in physiological evolution.
Oxford: Oxford University Press.
Tanghe A, van Dijk P, Thevelein JM 2003 Determinants of freeze tolerance in microorganisms, physiological importance and biotechnological applications.
Advances in Applied Microbiology 54: 129—176.
Mader HM, Pettitt ME, Wadham JL, Wolff EW, Parkes RJ 2006 Subsurface ice as a microbial habitat.
Geology 34 3 : 169—172.
Mazur P 2004 Principles of cryobiology.
In: Fuller BJ, Lane N, Benson EE, editors.
Life in the frozen state.
Boca Raton: CRC Press.
Rapatz GL, Menz LJ, Luyet BJ 1966 Freezing process in biological materials.
In: Meryman HT, editor.
Fonseca F, Marin M, Morris GJ 2006 Stabilization of frozen Lactobacillus bulgaricus in glycerol suspensions: freezing kinetics and storage temperature effects.
Applied and Environmental Microbiology 72 10 : 6474—6482.
Seki S, Kleinhans FW, Mazur P 2009 Intracellular ice formation in yeast cells vs.
Cryobiology 58 2 : 157—165.
Wharton DA, Ferns DJ 1995 Survival of intracellular freezing by the Antarctic nematode Panagrolaimus davidi.
Journal of Experimental Biology 198: 1381—1387.
Schmid WD 1982 Survival of frogs in low temperature.
Science 215 4533 : 697—698.
Leather SR, Walters KFA, Bale JS 1993 The ecology of insect overwintering.
Cambridge: Cambridge University Press.
Pearce RS 2004 Adaptation of higher plants to freezing.
In: Fuller BJ, Lane N, Benson EE, editors.
Life in the frozen state.
Boca Raton: CRC Press.
Debenedetti PG 1996 Metastable liquids: concepts and principles.
Princeton, New Jersey: Princeton University Press.
Wowk B 2010 Thermodynamic aspects of vitrification.
Cryobiology 60 1 : 11—22.
Ellis RJ 2001 Macromolecular crowding: obvious but unappreciated.
Trends in Biochemical Sciences 26 10 : 597—604.
Zhou EH, Trepat X, Park CY, Lenormand G, Oliver MN, et al.
Proceedings of the National Academy of Sciences of the United States of America 106 26 : 10632—10637.
Morris GJ, Acton E, Murray BJ, Fonseca F 2012 Freezing injury: the special case of the sperm cell.
Cryobiology 64 2 : 71—80.
Reid JP, Meresman H, Mitchem L, Symes R 2007 Spectroscopic studies of the size and composition of single aerosol droplets.
International Reviews in Перейти Chemistry 26 1 : 139—192.
Murray BJ, Haddrell AE, Peppe S, Davies JF, Reid JP, et al.
Atmospheric Chemistry and Physics 12 18 : 8575—8587.
Koop T, Zobrist B 2009 Parameterizations for ice nucleation in biological and atmospheric systems.
Physical Chemistry Chemical Physics 11 46 : 10839—10850.
Kostinski A, Cantrell W 2008 Entropic aspects of supercooled droplet freezing.
Journal of the Atmospheric Sciences 65 9 : 2961—2971.
Clarke KJ, Leeson EA 1985 Plasmalemma structure in freezing tolerant unicellular algae.
Protoplasma 129 2—3 : 120—126.
Clarke A, Leeson EA, Morris GJ 1986 The effects of temperature on 86Rb uptake by two species of Chlamydomonas Chlorophyta, Chlorophycaea.
Journal of Experimental Botany 37 182 : 1285—1293.
Slade L, Levine H, Finley JW 1989 Protein-water interactions; water as a plasticiser of gluten and other protein polymers.
In: Philips RD, Finley JW, editors.
Protein quality and the effect of processing.
New York: Marcel Dekker.
Chang BS, Randall CS 1992 Use of subambient thermal analysis to optimise protein lyophilisation.
Cryobiology 29 5 : 632—656.
Hansen LD, Criddle RS, Battley EH 2009 Biological calorimetry and the thermodynamics of the origination and evolution of life.
Pure https://chmall.ru/100/sumka-dlya-fotokameri-national-geographic-ngw2140.html Applied Chemistry 81 10 : 1843—1855.
Price PB, Sowers T 2004 Temperature dependence of metabolic rates for microbial growth, maintenance, and survival.
Proceedings of the National Academy of Sciences of the United States of America 101 13 : 4631—4636.
Geiges O 1996 Microbial processes in frozen food.
Advances in Space Research 18 12 : заценим.
Колесо TOR FCd46 большегрузное неповоротное обрезиненное 100 мм прощения />Weinzirl J, Gerdeman AE 1929 The bacterial count of ice cream held at freezing temperatures.
Journal of Dairy Science 12: 182—189.
Hodson A, Anesio AM, Tranter M, Fountain A, Osborn M, et al.
Ecological Monographs 78 1 : 41—67.
Price PB 2000 A habitat for psychrophiles in deep Antarctic ice.
Proceedings of the National Academy of Sciences of the United States of America 97 3 : 1247—1251.
Castell JD, Rogers SO eds 2005 Life in ancient ice.
Princeton University Press, 306 p.
Rohde RA, Price PB, Bay RC, Bramall NE 2008 In situ microbial metabolism as a cause of gas anomalies in ice.
Proceedings of the National Academy of Sciences of the United States of America 105 25 : 8667—8672.
Takenaka N, Bandow H 2007 Chemical kinetics of reactions in the unfrozen solution of ice.
Journal of Physical Chemistry A 111 36 : 8780—8786.
Chemical Society Reviews 41 19 : 6519—6554.
Hill KA, Shepson PB, Galbavy ES, Anastasio C, Kourtev PS, et al.
Journal of Geophysical Research, Atmospheres 112 D11 : D11301.
Dimmick RL, Wolochow H, Chatigny MA 1979 Evidence that bacteria can form new cells in airborne particles.
Applied and Environmental Microbiology 37 5 : 924—927.
Sattler B, Puxbaum H, Psenner R 2001 Bacterial growth in supercooled cloud droplets.
Geophysical Research Letters 28 2 : 239—242.
Womack AM, Bohannan BJM, Green JL 2010 Biodiversity and biogeography of the atmosphere.
Philosophical Transactions of the Royal Society of London, Series B 365 1558 : 3645—3653.
Lindow SE, Arny DC, Upper CD 1982 Bacterial ice nucleation: a factor in frost injury in plants.
Plant Physiology 70 4 : 1084—1089.
Christner BC, Cai R, Morris CE, McCarter KS, Foreman CM, et al.
Proceedings of the National Academy of Sciences of the United States of America 105 48 : 18854—18859.
Christner BC, Morris CE, Foreman CM, Cai R, Sands DC 2008 Ubiquity of biological ice nucleators in snowfall.
Science 319 5867 : 1214.
Bowers RM, Lauber CL, Wiedinmyer C, Hamady M, Hallar AG, et al.
Applied and Environmental Microbiology 75 15 : 5121—5130.
Pratt KA, DeMott PJ, French Водонагреватель Ballu BWH/S 80 Proof, Wang Z, Westphal DL, et al.
Nature Geoscience 2 6 : 397—400.
Šanti-Temkiv T, Finster k, Dittmar T, Hansen BM, Thyrhaug R, et al.
PLoS ONE 8 1 : e53550.
Christner BC 2010 Bioprospecting for microbial products that affect ice crystal formation and growth.
Applied Microbiology and Biotechnology 85 3 : 481—489.
Pearce RS 2001 Plant freezing and damage.
Annals of Botany 87 4 : 417—424.
Leopold AC, editor 1986 Membranes, metabolism, and dry organisms.
Ithaca, New York: Cornell University Press.
Convey P, Worland MR 2000 Survival of freezing by free-living Antarctic soil nematodes.
Cryo-Letters 21 6 : 327—332.
Kagoshima H, Kito K, Aizu T, Shin-i T, Kanda H, et al.
Cryo-Letters 33 4 : 280—288.
Miller LK 1978 Freezing tolerance in relation to cooling rate in an adult insect.
Kohshima S 1984 A novel cold-tolerant insect found in a Himalayan glacier.
Nature 310 5974 : 225—227.
Sformo T, Walters K, Jeannet K, Wowk B, Fahy GM, et al.
Journal of Experimental Biology 213 3 : 502—509.
Hirsh AG, Williams RJ, Meryman HT 1985 A novel method of natural cryoprotection.
Intracellular glass formation in deeply frozen Populus.
Plant Physiology 79 1 : 41—56.
Hirsh AG 1987 Vitrification in plants as a natural продолжить чтение of cryoprotection.
Cryobiology 24 3 : 214—228.
Wisniewski ME, Fuller M, Palta J, Carter J, Arona R 2004 Ice nucleation, propagation, and deep supercooling in woody plants.
Journal of Crop Production 10 19—20 : 5—16.
Hengherr S, Worland MR, Reuner A, Brümmer F, Schill RO 2009 High-temperature tolerance in anhydrobiotic tardigrades is limited by glass transition.
Physiological and Biochemical Zoology 82 6 : 749—755.
Hengherr S, Schill RO, Clegg JS 2011 Mechanisms associated with cellular desiccation tolerance of Artemia encysted embryos from locations around the world.
Comparative Biochemistry and Physiology A - Molecular and Integrative Physiology 160 2 : 137—142.
Hengherr S, Schill RO, Clegg JS 2011 Mechanisms associated with cellular desiccation tolerance in the animal extremophile Artemia.
Physiological and Biochemical Zoology 84 3 : 249—257.
Franks F 2003 Nucleation of ice and its management in ecosystems.
Philosophical Transactions of the Royal Society of London, Series A 361: 557—574.
Goyal K, Walton LJ, Tunnacliffe A 2005 LEA proteins prevent protein aggregation due to water stress.
Biochemical Journal 388, 151—157.
Kosová K, Vítámvás P, Prášil IT 2007 The role of dehydrins in plant response to cold.
Biologia Plantarum 51, 601—617.
Hand S C, Menze MA, Toner M, Boswell L, Moore D.
Annual Review of Physiology 73, 115—134.
Bartels-Rausch T, Bergeron V, Cartwright JHE, Escribano R, Finney JL, et al.
Reviews of Modern Physics 84 2 : 885—944.
Tansey MR, Brock TD 1972 The upper temperature limit for eukaryotic organisms.
Proceedings of the National Academy of Sciences of the United States of America 69 9 : 2426—2428.
Farrell AH, Hohenstein KA, Shain DH 2004 Molecular adaptation in the ice worm, Mesenchytraeus solifugus: divergence of energetic-associated genes.
Journal of Molecular Evolution 59 5 : 666—673.
Clarke A, Johnston NM 2003 Antarctic marine benthic diversity.
Oceanography and Marine Biology: an Annual Review 41: 47—114.
McCafferty DJ, Gilbert C, Thierry A-M, Currie J, Le Maho Y, et al.
Biology Letters 9: 20121192.
Liu J, Richardson MI, Wilson RJ 2003 An assessment of the global, seasonal, and interannual spacecraft record of Martian climate in the thermal infrared.
Journal of geophysical Research - Planets 108 E8 : Article 5089.
Chyba CF, Phillips CB 2007 Europa.
In: Sullivan WT, Baross JA, editors.
Planets and life: the emerging science of astrobiology.
Cambridge: Cambridge University Press.
For more information about PLOS Subject Areas, click.
We want your feedback.
Do these Subject Areas make sense for this article?
Click the target next to the incorrect Детальнее на этой странице Area and let us know.
Thanks for your help!
Yes No Thanks for your feedback.
Yes No Thanks for your feedback.
Yes No Thanks for your feedback.