Ran Drori1, Yeliz Celik2, Peter L Davies3, Ido Braslavsky4. 1. Institute of Biochemistry, Food Science and Nutrition, The Robert H. Smith Faculty of Agriculture, Food and Environment, The Hebrew University of Jerusalem, Rehovot, Israel. 2. Department of Physics and Astronomy, Ohio University, Athens, OH, USA. 3. Department of Biomedical and Molecular Sciences, Queen's University, Kingston, Ontario, Canada. 4. Institute of Biochemistry, Food Science and Nutrition, The Robert H. Smith Faculty of Agriculture, Food and Environment, The Hebrew University of Jerusalem, Rehovot, Israel Department of Physics and Astronomy, Ohio University, Athens, OH, USA ido.braslavsky@mail.huji.ac.il.
Abstract
Ice-binding proteins that aid the survival of freeze-avoiding, cold-adapted organisms by inhibiting the growth of endogenous ice crystals are called antifreeze proteins (AFPs). The binding of AFPs to ice causes a separation between the melting point and the freezing point of the ice crystal (thermal hysteresis, TH). TH produced by hyperactive AFPs is an order of magnitude higher than that produced by a typical fish AFP. The basis for this difference in activity remains unclear. Here, we have compared the time dependence of TH activity for both hyperactive and moderately active AFPs using a custom-made nanolitre osmometer and a novel microfluidics system. We found that the TH activities of hyperactive AFPs were time-dependent, and that the TH activity of a moderate AFP was almost insensitive to time. Fluorescence microscopy measurement revealed that despite their higher TH activity, hyperactive AFPs from two insects (moth and beetle) took far longer to accumulate on the ice surface than did a moderately active fish AFP. An ice-binding protein from a bacterium that functions as an ice adhesin rather than as an antifreeze had intermediate TH properties. Nevertheless, the accumulation of this ice adhesion protein and the two hyperactive AFPs on the basal plane of ice is distinct and extensive, but not detectable for moderately active AFPs. Basal ice plane binding is the distinguishing feature of antifreeze hyperactivity, which is not strictly needed in fish that require only approximately 1°C of TH. Here, we found a correlation between the accumulation kinetics of the hyperactive AFP at the basal plane and the time sensitivity of the measured TH.
Ice-binding proteins that aid the survival of freeze-avoiding, cold-adapted organisms by inhibiting the growth of endogenous ice crystals are called antifreeze proteins (AFPs). The binding of AFPs to ice causes a separation between the melting point and the freezing point of the ice crystal (thermal hysteresis, TH). TH produced by hyperactive AFPs is an order of magnitude higher than that produced by a typical fish AFP. The basis for this difference in activity remains unclear. Here, we have compared the time dependence of TH activity for both hyperactive and moderately active AFPs using a custom-made nanolitre osmometer and a novel microfluidics system. We found that the TH activities of hyperactive AFPs were time-dependent, and that the TH activity of a moderate AFP was almost insensitive to time. Fluorescence microscopy measurement revealed that despite their higher TH activity, hyperactive AFPs from two insects (moth and beetle) took far longer to accumulate on the ice surface than did a moderately active fish AFP. An ice-binding protein from a bacterium that functions as an ice adhesin rather than as an antifreeze had intermediate TH properties. Nevertheless, the accumulation of this ice adhesion protein and the two hyperactive AFPs on the basal plane of ice is distinct and extensive, but not detectable for moderately active AFPs. Basal ice plane binding is the distinguishing feature of antifreeze hyperactivity, which is not strictly needed in fish that require only approximately 1°C of TH. Here, we found a correlation between the accumulation kinetics of the hyperactive AFP at the basal plane and the time sensitivity of the measured TH.
Ice-binding proteins protect cold-environment organisms by limiting the growth of ice
crystals within and/or outside their body fluids [1,2].
These proteins have been found in fish [3], plants [4], insects
[5], fungi [6] and bacteria [7], and comprise antifreeze proteins (AFPs), ice
recrystallization inhibition proteins and a newly discovered ice adhesion protein [8]. AFPs adsorb to the surfaces of ice
crystals and lower the temperature at which an ice crystal grows, thereby creating a gap
(thermal hysteresis or TH) between the melting point and the non-equilibrium freezing
point in which ice growth is arrested. Although ice adhesion proteins show activities
similar to those of AFPs, they serve as a means to adhere to ice and not necessarily to
block its growth [8]. The accepted
model explaining the inhibition of ice growth by AFPs is the
adsorption–inhibition model. This model describes ice growth as occurring in the
gaps between adsorbed AFPs [9]. This
process increases the curvature of the ice surface between bound AFP molecules, thereby
decreasing the radius of curvature from infinity to a finite magnitude. Such an increase
in the surface curvature leads to a depression in the freezing point due to the
Gibbs–Thomson effect, which states that the equilibrium melting point of a solid
is related to the curvature of the solid surface and the interfacial energy [10,11]. Although the adsorption–inhibition model
assumes irreversible binding of AFPs to ice, the irreversibility of this binding remains
the subject of an ongoing debate in the AFP community [12-14].Hyperactive AFPs found in insects and microorganisms (hypAFPs) are ten to a hundred
times more active than moderate AFPs derived from fish and plants at equimolar
concentration [15]. Moderate AFPs
adsorb to prism and/or pyramidal planes of an ice crystal, whereas hypAFPs adsorb to
these surfaces and the basal plane of an ice crystal [16,17]. The morphology of an ice crystal is influenced by the plane to which an AFP
adsorbs. Moderate AFPs usually induce the formation of hexagonal bipyramidal crystals
that form by growing, whereas hypAFPs usually produce crystals with hexagonal symmetry
with curved surfaces that form during melting [17,18].Although the dependence of TH activity on the AFP concentration has been extensively
studied, the time dependence of this process remains unclear. A handful of experimental
studies of the time-dependent TH activities of moderate AFPs have been reported [13,19-21], and a few recent studies of hypAFPs are available [12,22,23]; however, none of
these studies has examined carefully the time-dependent TH activity of hypAFPs, nor have
they elaborated on the mechanisms underlying AFP activity. Chapsky & Rubinsky
found that the TH activity of a solution of AFP I from the winter flounder,
Pseudopleuronectes americanus, could increase over time. The same
researchers found that TH increased by a factor of 5 over time and reached a plateau
60–180 min after exposure of an ice crystal to the AFP I solution, depending on
the concentration. They hypothesized that time-dependent TH resulted from the
accumulation of AFP molecules on the ice surfaces or the rearrangement of adsorbed AFP
molecules on the ice (or a combination of the two) [19]. Takamichi et al. observed the same
phenomenon in a solution prepared from an AFPIII derived from Notched-fin eelpout. They
found that the TH activity increased by a factor of 2.5 after allowing for an annealing
time of 3 h [21]. The authors
proposed a model for the observed TH effects that involved secondary binding of the AFP
molecules to the convex ice front over time. A model for the kinetics of AFP ice growth
inhibition was proposed by Kubota [13]. This model assumed the slow and reversible adsorption of AFPs to ice; thus,
a period of time was needed to reach adsorption equilibrium. A working assumption of
this model was that the AFPs reversibly adsorbed to ice. Wilson et al.
[20] measured the accumulation of
antifreeze glycoproteins (AFGPs) on the surfaces of ice crystals using ellipsometry
techniques based on optical changes in the water–ice interface. They found that
the signal from the interface changed over time until it reached a plateau at
approximately 60 min. Their interpretation was that the change at the water–ice
interface was caused by the adsorption of AFGP molecules to the ice crystal planes
[20].Various computational studies have suggested that AFPs form an ice-binding structure by
constraining water molecules present at the ice-binding sites into a structural ordering
that resembles ice [24,25]. Garnham et al.
have found evidence for these protein-bound ice-like waters [26]. However, owing to the short lifetime of the ordered
water structures on the AFP surfaces [27], it is likely that at any given time only a small proportion of the AFP
molecules possess sufficient appropriately ordered water molecules to bind to ice.
Higher AFP concentrations and longer exposure times should both increase the number of
binding events between the AFP and ice.Sander & Tkachenko developed a ‘kinetic pinning’ mathematical model
that described the AFP molecules as obstacles that induced surface pinning on the
growing ice surface [28]. The model
described a reduction in the ice front propagation as a function of the AFP
concentration. In their model, the growth velocity drops to zero as a function of
concentration and once the growth stops the proteins continued to accumulate on the ice
crystal surface. Ebbinghaus et al. [29] examined the dynamics of water molecules around the
AFGP structure in solution using terahertz (THz) spectroscopy. They found that the AFGP
hydration shell increased in size as the temperature was decreased and that the
hydration shell has a depressed freezing point compared to bulk water. Ebbinghaus
et al. suggested a mechanism by which AFGPs altered the dynamics of
water molecules in the hydration shell in such a way that the solution freezing process
was inhibited [29], thereby rejecting
the adsorption–inhibition model. Recently, the same group measured the water
dynamics around a hyperactive AFP (Dendroides canadensis,
DcAFP) and identified direct short-range interactions between the
AFP and the ice surface, in addition to long-range ice–water interactions
mediated by the AFP [14]. Solid-state
NMR studies suggested that the ice-binding site of AFPIII became stripped of its
hydration shell upon freezing, which enabled direct protein–ice contact [30]. Zepada et al.
suggested that AFGPs interrupted the arrangement of the ice–water interface
through kinetic effects rather than through mediating binding between the ice surface
and water molecules. Their final conclusion was that AFGPs could not be accurately
described using the Gibbs–Thomson model [31]. Knight & DeVries suggested that AFGPs
adsorbed only to the non-basal planes of ice crystals, thereby influencing the crystal
shape and minimizing the surface area of the unprotected basal plane. They offered a
mechanism by which the rate of AFGP adsorption governed the depression of the
non-equilibrium freezing point, and they proposed that this process was governed by the
concentration of the proteins in the solution and not the time of exposure to AFPs
[32]. These findings describe the
kinetic effects of AFPs known at this time and illustrate the uncertainty and confusion
in the field with regard to the mechanism of action of AFPs. The kinetic effects of the
hyperactive AFPs as well as a unified understanding of the mechanisms at work in both
the moderate AFP and hypAFP systems have not yet been established.Standard methods for measuring TH activity (the difference between the melting point and
the depressed temperature at which the ice crystal starts to grow) include the use of a
nanolitre osmometer [22] in which a
single crystal is formed and the melting point is identified with the aid of video
microscopy and image analysis. The temperature of the system is then lowered at a fixed
rate until the ice crystal undergoes a sudden burst of growth, which marks the
non-equilibrium freezing point. The time separating the formation of a single crystal
and the growth burst is defined as the ‘exposure time’ of the crystal
(figure 1). During the exposure
time, AFPs can adsorb to the ice crystal surface.
Figure 1.
Stages of the measurement are indicated by text. Sample temperature in the
nanolitre osmometer is represented by the bold line. TH is indicated by the
double-headed vertical arrow. (Online version in colour.)
Stages of the measurement are indicated by text. Sample temperature in the
nanolitre osmometer is represented by the bold line. TH is indicated by the
double-headed vertical arrow. (Online version in colour.)Our objectives in this work were to characterize the effects of the exposure time on the
TH properties of various AFPs and to identify the distinctions between the kinetic
mechanisms by which various AFPs function. We found that the TH activities of
Tenebrio molitor AFP (TmAFP) and spruce budworm AFP
(sbwAFP) could be increased by a factor of 40 by increasing the exposure time. We
examined the accumulation rates of both the moderate and hyperactive AFPs on the
different crystal planes, as well as the TH activity.The findings reported here suggest a new approach to measuring and enhancing TH
activity. Appropriate kinetic models of AFP adsorption to ice crystal planes can improve
our understanding of the mechanisms by which these proteins act and could lead to a
unified description of AFP activity.
Material and methods
Thermal hysteresis activity measurements
We used a custom-designed nanolitre osmometer system that includes a 3040 Newport
temperature controller (Irvine, CA, USA) and a previously described custom-made
cooling stage [22,33]. The temperature of the cooling
stage was controlled using a LabVIEW program developed in-house. An AVI file was
generated by a CCD camera connected to a video frame grabber (IMAQ-PCI 1407, National
Instruments, Austin, TX, USA) and was recorded to a PC. The images were collected at
a rate of 30 frames s−1. TH measurements were as follows (figure 1): sub-microlitre volumes of
AFP solutions were placed in immersion oil and were cooled to –30°C to
generate freezing. The temperature was increased slightly above the melting point.
The melting point (Tm) was determined as described
elsewhere [34]. The bulk ice was
then melted until a single crystal 10–15 μm in size remained. These
crystals were then incubated in the AFP solution for different lengths of time at a
fixed temperature of typically 0.05°C below the
Tm. The temperature was subsequently decreased at a fixed
rate (0.15°C per min by reducing the temperature by 0.01°C every 4 s)
until the crystal underwent sudden, uncontrolled growth (burst). The time between the
crystal formation (the end of melting) and the growth burst was defined as the
crystal ‘exposure time’. The output AVI files were analysed after the
experiments to accurately identify the melting point and the growth burst of the
crystal [22]. The exposure times
obtained from each experiment were binned to form clusters of similar exposure times.
Each cluster comprised at least three experimental results, and the average TH of
each cluster was plotted as a function of the exposure time (figures 3–6).
Figure 3.
Effect on TH of the exposure time between ice and TmAFP.
Solutions of different concentrations were tested for TH as a function of
TmAFP exposure time: 1 µM (black squares), 4
µM (red circles), 10 µM (blue triangles) and 40 µM
(green inverted triangles). (a) Plots of TH versus exposure
time on a log scale for the different TmAFP concentrations.
TH values were the average of 3–10 measurements for each data point,
with the variability indicated by the vertical error bars.
(b) The untagged TmAFP were tested for
time dependence at a concentration of 10 µM. TH values were the
average of 3–5 measurements for each data point, with the variability
indicated by the vertical error bars. (c) Re-plotted data
from (a) where the closest data points to the intersection
of a 0.15°C min−1 constant cooling rate (dashed
line) are highlighted in yellow. (d) The highlighted data
points from (b) are plotted to examine the dependence of TH
on the concentration of TmAFP. The curved lines in
(a,d) were fitted using Origin
software.
Figure 6.
Sensitivity of the TH activity to sbwAFP exposure time. TH activity of 4
µM (open circles) and 8 µM (filled squares) sbwAFP solutions
plotted against the log of the exposure time. TH values are the average of
at least three measurements with the variability indicated by the vertical
error bars.
Proteins
Several proteins were tested in this study. Three hyperactive GFP-tagged AFPs were
produced in Escherichia coli: TmAFP-GFP [35] was stored in a solution
containing 20 mM ammonium bicarbonate buffered at pH 8; MpAFP-GFP
from Marinomonas primoryensis [36] was stored in 20 mM CaCl2, 25 mM
Tris–HCl (pH 8); and isoform 501 of sbwAFP-GFP [17] was stored in 20 mM Tris–HCl (pH 8). The
GFP-tagged moderately active AFP derived from ocean pout, AFPIII-GFP [33] was stored in 100 mM ammonium
bicarbonate buffered at pH 8.
Microfluidic device fabrication and microfluidic experiments
Previously, we developed and used microfluidic devices to understand the effects of
free unbound AFPs on ice crystal growth and the binding mechanism of the AFPs to ice
[12]. With the assistance of
Gerber's lab in Bar Ilan University, we further improved the devices to allow
for the exchange of solutions in a rapid and controllable manner, using a two-layer
fabrication technique that includes one layer for liquid handling and one layer that
provided actuation of a set of valves. These devices were used to obtain ice crystals
in which only the crystal surfaces were bound by the AFPs. This binding mode was
achieved by growing the ice in a solution that did not contain AFPs prior to the
introduction of the AFPs. This device was fabricated using a standard protocol
provided in [37,38], and further described in the
electronic supplementary material. The microfluidic device consisted of two aligned
layers—a flow layer that included the fluid (figure 2, white), and a control layer (yellow) that
included the pneumatic valves. The completed device was placed on a cold stage
controlled using a temperature controller (Model 3150, Newport, Irvine, CA, USA) that
was governed by a LabVIEW program described in [12]. The cold stage was mounted on a fluorescence
microscope (Ti Eclipse, Nikon, Japan) outfitted with a sCMOS camera (Neo 5.5 sCMOS,
Andor, UK) used for visualization.
Figure 2.
Microfluidic chip design. The control layer (yellow) was used as pneumatic
valves and was fabricated on top of the flow layer (white), which was
designed to fit the viewing hole of the cooled stage (5 mm in diameter). The
crystals were formed in the small side compartments in the flow layer.
During AFP accumulation, these compartments were isolated from any flow
using the pneumatic valves.
Microfluidic chip design. The control layer (yellow) was used as pneumatic
valves and was fabricated on top of the flow layer (white), which was
designed to fit the viewing hole of the cooled stage (5 mm in diameter). The
crystals were formed in the small side compartments in the flow layer.
During AFP accumulation, these compartments were isolated from any flow
using the pneumatic valves.AFP-free buffer solution in the microfluidic channel spontaneously nucleated to form
a bulk ice crystal at approximately –20°C. The bulk ice crystal was
subsequently warmed to a temperature near the equilibrium melting temperature to form
a single crystal. A 980 nm, 500 mW, diode laser (Wuhan Laserlands Laser Equipment
Co., ltd, China) was used to heat and melt any unwanted ice to help obtain the single
crystal in the designated cell. After ice formation, AFP solution was injected to the
flow line using a glass syringe. By this method, no AFP was present in the core of
the ice and the AFP molecules adsorbed to the crystals only at the surface (see the
electronic supplementary material, figure S1).
Results
The thermal hysteresis activity of Tenebrio molitor antifreeze
protein increased by a factor of 10 over a prolonged exposure time
TmAFP is a 9 kDa protein with eight disulfide bonds [39]. We used GFP labelled
TmAFP. The positioning of the GFP tag in the fusion protein did
not interfere with the ability of the proteins during binding to ice and have
actually enhanced the TH activity as a result of the larger protein size (36 kDa)
[33,40] (figure
3a,b). The addition of 27 kDa to the AFP may, however,
have slowed down the diffusion rate and influenced the adsorption rate. We tested the
significance of the mass effects by comparing the dependence of TH on incubation time
for the TmAFP and TmAFP-GFP proteins under several
conditions. Indistinguishable kinetic behaviours were observed (figure 3a,b).Effect on TH of the exposure time between ice and TmAFP.
Solutions of different concentrations were tested for TH as a function of
TmAFP exposure time: 1 µM (black squares), 4
µM (red circles), 10 µM (blue triangles) and 40 µM
(green inverted triangles). (a) Plots of TH versus exposure
time on a log scale for the different TmAFP concentrations.
TH values were the average of 3–10 measurements for each data point,
with the variability indicated by the vertical error bars.
(b) The untagged TmAFP were tested for
time dependence at a concentration of 10 µM. TH values were the
average of 3–5 measurements for each data point, with the variability
indicated by the vertical error bars. (c) Re-plotted data
from (a) where the closest data points to the intersection
of a 0.15°C min−1 constant cooling rate (dashed
line) are highlighted in yellow. (d) The highlighted data
points from (b) are plotted to examine the dependence of TH
on the concentration of TmAFP. The curved lines in
(a,d) were fitted using Origin
software.The kinetics of the TH activity were measured using a custom-made nanolitre
osmometer. The procedure is illustrated schematically in figure 1 and described in Material and methods and in
[22]. Measurements of the TH
activity as a function of the exposure time revealed that the TH activity in the
TmAFP solution increased with the exposure time for all solution
concentrations measured (figure
3a). The TH activity increased by factors of between 10
(for the 1 µM solution) and 3 (for the 40 µM solution). A long exposure
time (12 h) at a very low TmAFP concentration (1 µM)
increased the TH activity to a level comparable to that obtained from incubating an
ice crystal in a 10 µM solution for a much shorter period of time (10
min).Interestingly, the TH value did not reach a plateau at long exposure times, where 13
h was the longest time the TH value was tested. The TH obtained from the
TmAFP solutions obviously depended on the concentration (figure 3a). A plot of
the TH values obtained from the four TmAFP concentrations as a
function of the exposure time followed an approximately hyperbolic relationship
(figure 3c). The
exposure time was calculated as the sum of the incubation time and the cooling time
until bursting. Higher TH values were obtained with extended crystal incubation times
(figure 1). In many experiments
published previously in the literature, a constant cooling rate without an incubation
time was used [9,15]. Thus, the exposure time was the
same as the cooling time. We note that such a cooling scheme intersects with
the four concentration curves shown in figure 3c for a cooling rate of 0.15°C
min−1. Thus, it was possible to directly plot the effects of the
TmAFP concentration on the TH under such cooling conditions, as
shown in figure 3d.
The hyperbolic relationship was similar to other plots of the TH versus the AFP
concentration [9,15]; however, the latter represent
only part of the TH concentration dependence, without the full impact of the time
dependence, as shown in figure
3c.
Each antifreeze protein displayed different kinetics
The kinetics of the TH effects were further examined by conducting exposure
time-dependent TH measurements using different AFPs. Takamichi et
al. showed that the TH activity of moderately active fish AFPIII from
notched-fin eelpout was influenced by the exposure time [21]. These authors additionally found that the
temperature at which the crystal was incubated prior to the TH measurement (during
ice crystal stasis) affected the TH measurements. A solution incubated under highly
supercooled conditions (at 0.25°C below the melting point) yielded a TH
activity that was a factor of 1.7 times the TH activity obtained by incubating the
crystal under less supercooled conditions (at 0.05°C below the melting point).
This experiment was repeated here using the AFPIII from ocean pout (at a
concentration of 40 µM, which corresponded to the maximum concentration of
TmAFP tested here) and under two supercooling conditions
(incubation at 0.02°C or 0.1°C below the melting point). The results
(figure 4) qualitatively agreed
with previous findings [21]. A
short exposure time (a few seconds) under highly supercooling conditions produced a
slightly lower TH activity than a longer exposure time. Under a small degree of
supercooling (incubation at 0.02°C below the melting point), the TH activity
was unaffected by the exposure time.
Figure 4.
Sensitivity of TH to the AFPIII exposure time. The TH activity of a 40
µM AFPIII solution was examined as a function of ice crystal exposure
time. TH values are the average of at least three measurements taken at
0.02°C below Tm (open circles) and
0.1°C below Tm (filled squares), with the
variability indicated by the vertical error bars.
Sensitivity of TH to the AFPIII exposure time. The TH activity of a 40
µM AFPIII solution was examined as a function of ice crystal exposure
time. TH values are the average of at least three measurements taken at
0.02°C below Tm (open circles) and
0.1°C below Tm (filled squares), with the
variability indicated by the vertical error bars.The hyperactive AFP derived from the Antarctic bacterium Marinomonas
primoryensis (MpAFP) is a 38 kDa protein and is somewhat
larger than most AFPs (3–16 kDa). The adsorption kinetics of
MpAFP to ice were distinct from those of AFPIII, although they
were closer to the kinetics of AFPIII than to the kinetics of TmAFP.
The TH activity was found to depend on the exposure time only at low concentrations
(2.4 µM) of MpAFP-GFP (figure 5) [22]. At higher concentration (4.2 µM), the TH activity increased
significantly over very short exposure times and did not increase at all over time at
much higher concentrations (8–55 µM, data not shown). After a 4 min
exposure time, the TH activity reached a plateau. This plateau was not observed among
the TmAFP solutions, even after 13 h, but was obtained from the
AFPIII solutions after a few minutes. At low concentrations, the kinetics of
MpAFP were similar to those obtained from TmAFP
(figure 3). After an exposure
time of a few minutes, the TH activity remained unchanged. Unlike AFPIII, the degree
of the solution supercooling during the exposure and TH measurements did not affect
the TH activity of the MpAFP solutions.
Figure 5.
Sensitivity of TH activity to MpAFP exposure time. The TH
activity of a 2.4 µM MpAFP solution was plotted
against the log of the exposure time. TH values (black squares) are the
average of at least three measurements with the variability indicated by the
vertical error bars. (Adapted with permission from [22].)
Sensitivity of TH activity to MpAFP exposure time. The TH
activity of a 2.4 µM MpAFP solution was plotted
against the log of the exposure time. TH values (black squares) are the
average of at least three measurements with the variability indicated by the
vertical error bars. (Adapted with permission from [22].)A third hyperactive AFP, sbwAFP from the spruce budworm moth, Choristoneura
fumiferana, was tested. This protein is 12 kDa in mass and contains TXT
motifs (Thr-X-Thr, where X is any amino acid) on its ice-binding site, similar to
those found in TmAFP and its orthologue from DcAFP
[41,42]. As with TmAFP, The TH of sbwAFP
depended profoundly on the exposure time (figure 6). Very short exposure times to the sbwAFP solutions (several
seconds) did not produce TH activity. A longer exposure time of a few minutes in the
presence of higher protein concentrations (8 μM) yielded a TH of 1°C,
and the TH continued to increase to 2°C as the exposure time increased (figure 6). The lowest concentration
solution tested (4 μM) also showed a remarkable TH enhancement over time
(figure 6). These results
suggested that adsorption rate of sbwAFP was smaller than the adsorption rate of
TmAFP (i.e. more time was needed for sbwAFP to depress the
freezing point) and was extremely slow compared with adsorption rate of AFPIII. The
TH activity increased by a factor of 40 as the sbwAFP exposure time was increased
from 8 s to 850 min. This TH ratio increase value was the highest value yet measured
among the AFPs tested thus far (figure
6). We hypothesize that the AFPs accumulated on the ice surface over time,
and this accumulation increased the measured TH activity.Sensitivity of the TH activity to sbwAFP exposure time. TH activity of 4
µM (open circles) and 8 µM (filled squares) sbwAFP solutions
plotted against the log of the exposure time. TH values are the average of
at least three measurements with the variability indicated by the vertical
error bars.
Direct measurement of the antifreeze protein accumulation rates using
fluorescence intensity measurements
The accumulation of AFP molecules on the ice surfaces was measured by imaging the ice
crystals in the presence of AFP molecules fused to GFP markers, AFP-GFP. Microfluidic
techniques were used to prepare a large ice crystal in an AFP-free solution. An
AFP-GFP solution was then injected into the microfluidic channel, and the large
crystal was partially melted. Once melting had ceased, the AFP-GFP molecules adsorbed
to the ice crystal surface under constant temperature conditions (approx.
0.05°C below the melting point of the crystal). The outer layer of the crystal
then became covered with AFP-GFPs, and no AFP-GFPs were observed within the crystal.
Note that if the ice crystals had been initially nucleated in solutions containing
AFP-GFP, the crystals that formed would have included AFP-GFPs within the ice, and
not only on the crystal surfaces. This procedure was performed for both the
AFPIII-GFP and TmAFP-GFP. There is a difference between the two AFP
types: ice in TmAFP-GFP solution is shaped during melting, while the
crystals in AFPIII-GFP are shaped within the hysteresis gap while growing from an
initial ice seed in the presence of AFPIII-GFP. Consequently, the ice grown from an
AFP-free seed in the presence of AFPIII-GFP does not contain fluorescence within the
ice because AFPIII-GFP does not adhere to the basal plane and therefore will not get
incorporated into the ice during formation of the bipyramidal tips by growth along
the c-axis. For example, a bright core was observed in crystals
formed in the presence of AFPIII-GFP (electronic supplementary material, figure
S1a and fig. 3b in [33]). The formation of ice crystals from AFP-GFP-free
solutions prior to exposing the crystals to an AFP-GFP solution is a unique feature
of the experiments conducted here using a microfluidic apparatus. This procedure
resulted in crystals that were bound by AFP-GFP only on their surfaces (electronic
supplementary material, figure S1b).The fluorescence signal was measured and extracted using the Nis-Elements program
(Nikon, Japan). An in-house Matlab program was used to analyse the fluorescence
signals and extract a maximum from each line profile of the fluorescence intensity
perpendicular to the crystal plane that crossed the ice–solution interface.
This procedure was used to measure the fluorescence signal from the ice surface over
time in the microfluidic channel. The intensity was interpreted as indicating the
amount of bound AFP present on the ice surface and was used to monitor the binding of
both AFPIII-GFP and TmAFP-GFP. Figure 7 plots the accumulation of AFP-GFPs as
a function of time onto different planes of an ice crystal. The hyperactive AFP
(TmAFP, figure
7a,b) displayed continuous accumulation
of TmAFP-GFP molecules on the basal plane over an exposure time of 4
h. We did not observe further accumulation during an additional 1.5 h of exposure
time suggesting that any subsequent change in fluorescence was too small to detect
using our instrumentation. The accumulation on the basal plane revealed that the
adsorption rate (the time derivative of the fluorescence intensity) was high within
the first few minutes after ice growth had ceased. After approximately 1000 s, the
adsorption rate slowed and nulled after approximately 4 h. The accumulation kinetics
measurements over periods of at least 1 h were repeated six times. Accumulation
experiments over shorter periods of time were repeated a greater number of times
(more than 200 experiments). The accumulation experiments performed using AFPIII
(figure
7c,d) showed that the accumulation of
AFPIII-GFP at the prism plane reached saturation very rapidly (within 6 min) compared
to TmAFP-GFP (within 4 h). The solid line in figure 7d followed the equationwhere I is the fluorescence intensity,
Imax is the maximum fluorescence intensity parameter,
t is the time from the ice formation and
τ = 70 s is a time constant parameter that fit the
data. Our experiments revealed that 6 s ≥ τ ≥
90 s for AFPIII-GFP depending on the solution concentration. We found a linear
correlation between the inverted τ and the concentration. Assuming that
1/τ = KonC, where
Kon is the adsorption constant and C
is the AFP concentration in the solution, we found that
Kon = 0.008 ± 0.001
µM−1 s−1 (electronic supplementary
material, figure S2). Nevertheless, single exponent formula did not fit the data for
TmAFP-GFP for any parameter set. A model that included three
exponents to describe the process of TmAFP accumulation, however,
provided a good description of the datawhere N = 3 and
τ = (9,110 and
4050)s, respectively.
Figure 7.
Accumulation of TmAFP and AFPIII on different ice crystal
planes. (a,b) TmAFP and
(c,d) AFPIII.
(a,c) Ice crystals with
surface-adsorbed AFP-GFP. Crystal axes are indicated by white arrows, and
their dimensions are indicated by the scale bar. In the upper image
(a), the two concentric lemon-shaped crystals are the
seed for the observed basal plane. See the electronic supplementary
material, movie S5, for the development of the basal planes from these
seeds. The seed crystals are slightly tilted thus the projection of the
basal planes that emerge from them is seen in the optical observation
direction that is perpendicular to the microfluidic channel. Note that the
apparent lens shape of the basal plane (marked with dotted lines) is caused
by the round shape of the microfluidic channels (see the electronic
supplementary material, figure S3). The scale bar is the same for both
images. (b,d) Measurement of the
fluorescence intensity of surface-adsorbed AFP-GFPs over time on the basal
planes (black squares, TmAFP) and prism plane (black
squares, AFPIII). The red lines were plotted using the equations presented
in the results section for each AFP.
Accumulation of TmAFP and AFPIII on different ice crystal
planes. (a,b) TmAFP and
(c,d) AFPIII.
(a,c) Ice crystals with
surface-adsorbed AFP-GFP. Crystal axes are indicated by white arrows, and
their dimensions are indicated by the scale bar. In the upper image
(a), the two concentric lemon-shaped crystals are the
seed for the observed basal plane. See the electronic supplementary
material, movie S5, for the development of the basal planes from these
seeds. The seed crystals are slightly tilted thus the projection of the
basal planes that emerge from them is seen in the optical observation
direction that is perpendicular to the microfluidic channel. Note that the
apparent lens shape of the basal plane (marked with dotted lines) is caused
by the round shape of the microfluidic channels (see the electronic
supplementary material, figure S3). The scale bar is the same for both
images. (b,d) Measurement of the
fluorescence intensity of surface-adsorbed AFP-GFPs over time on the basal
planes (black squares, TmAFP) and prism plane (black
squares, AFPIII). The red lines were plotted using the equations presented
in the results section for each AFP.The lack of binding between the moderate AFPs and the basal plane has been discussed
previously [15] and has been shown
qualitatively using AFPIII-GFP [17]. Here, we have directly and quantitatively measured this effect,
verifying that this AFP does not bind to the basal plane (electronic supplementary
material, figure S4). In summary, the fluorescence experiments reported here suggest
that the adsorption and accumulation of AFP-GFPs onto ice surfaces is a two-step
process. The first step (initial adsorption) is rapid and causes ice growth to cease,
whereas the second step (accumulation) is slow. The adsorption of the hyperactive AFP
was much slower and mainly occurred at the basal plane, whereas the moderate AFP
reached a saturated adsorption state quickly, and no basal plane accumulation was
observed. Electronic supplementary material, movie S5, is the experimental record of
the formation of the crystal and the fluorescence signal over time that is shown in
figure
7a,b.
Discussion
This study examined the influence of the exposure time, at a temperature slightly below
the Tm, on the hysteresis activities of several AFPs. This
influence was then found to be correlated with the accumulation of the tagged AFPs on
the surfaces of the ice crystals. Our study of moderate and hyperactive AFPs revealed
very different TH dynamics. This study showed that the TH of hyperactive AFPs increased
with longer AFP exposure times. Although the TH activities of the TmAFP
and sbwAFP solutions were sensitive to the exposure time (the TH activity increased by a
factor of up to 40 as the exposure time was increased from a few seconds to several
hours), the TH activity of the AFPIII solution was relatively insensitive to the
exposure time (the TH activity varied by only a factor of 1.5 in an hour). The TH
activity of MpAFP, a bacterial hyperactive AFP, was only sensitive to
the exposure time at low concentrations (2.4 µM). Over short exposure times (a
few seconds), all hyperactive AFPs showed very low TH activity. The differences between
the kinetics suggested that TmAFP and sbwAFP bound to ice at a much
slower rate than MpAFP, which bound slower than the moderately active
AFP. The rapid adsorption of AFPIII to the ice crystal could explain the observed TH
activity. Evidence for rapid adsorption was obtained from fluorescence microscopy
measurements during ice formation in the presence of AFPIII-GFP. Significant amounts of
the measured fluorescence signal on fast growing ice was observed the instant the ice
growth halted. In AFPIII accumulation experiments, in which the fluorescence intensity
was measured after the crystal had melted to a smaller size and then shaped slowly to a
bipyramidal structure (electronic supplementary material, movie S6), we measured single
exponent intensity growth. The fast increase in the fluorescence signal from the surface
of the fast growing crystals might be due to high local AFP concentration that developed
during growth. Alternatively, this fast kinetics can attribute to modified ice surface
in comparison to the gentle growth within the TH gap. We note that in the presence of
the moderate AFP, the ice grew along the c-axis, and the ice surface
developed within the hysteresis gap. This behaviour contrasts with ice crystal shaping
in the presence of hypAFP that occurs during ice melting and not within the TH gap
[18]. The rapid adsorption of
AFPIII to the ice reduced the sensitivity of the TH to the cooling rate and could
explain the small variations in the TH measurements obtained in the presence of the
moderate AFPs, which contrasted with the large variations seen with hypAFPs, as reported
by Scotter et al. [15]. Note that for our experiments conducted in a microfluidic device, ice
crystals were formed in water without AFP, after which a solution containing AFP
molecules was added to the experimental chamber. Prior to designing this microfluidic
apparatus, it was not possible to form a single ice crystal without a core of
fluorescent protein in the ice (electronic supplementary material, figure
S1b). This unique feature both enhanced the ability to measure
fluorescence on the surfaces and indicated that the AFP trapped inside of an ice crystal
did not influence the TH.It was not surprising that the two insect AFPs displayed similar TH dynamics, because
these two proteins have the same function of protecting their hosts from freezing in
sub-zero temperatures. The proteins also have very similar ice-binding sites within the
protein structure that comprise tandemly arrayed TXT motifs. MpAFP, on
the other hand, includes the ice-binding domain of an ice adhesin is thought to be
involved in docking its host bacterium to an ice crystal [8]. Although it is indeed a hypAFP, it has not evolved to
be efficient at TH. Its TH activity curve as a function of AFP concentration differed
from that of typical AFPs [36].
MpAFP showed an almost sigmoidal increase in TH activity, but then
rapidly approached a plateau value slightly greater than 2°C. By contrast, the
insect AFPs approached TH values of 5–6°C at modest AFP concentrations
[15]. In nature, freeze-avoiding
insects, such as the Tenebrio molitor beetle and spruce budworm, can
endure much lower temperatures (–20°C) than are indicated by the TH
measured in the nanolitre osmometer [43]. This anomaly may be partially resolved by the fact that insects also
produce colligative cryoprotectant agents, such as glycerol, to assist with freezing
point lowering [43]. Another
contributing factor is the effect of the crystal size on TH activity, as discussed by
Zachariassen & Husby [44].
Crystals formed in the nanolitre osmometer (approx. 15 µm) are larger than those
that form inside an insect [44]. Our
findings may suggest yet another mechanism for resolving the differences between the
in vitro TH measurements and the survival temperatures of the
insects. Long exposure times to tiny ice crystals, as is allowed in the haemolymph of an
insect, can increase the apparent TH in the insect beyond the values that are typically
measured in the nanolitre osmometer.The binding kinetics of the AFPs to ice were characterized using fluorescence microscopy
techniques to measure the accumulation of the AFPs on the different ice crystal planes.
Takamichi et al. [21] measured the accumulation of AFPIII fused to GFP and suggested that AFPs may
progressively bind to ice over a few hours. Their measurement did not differentiate
between the accumulation kinetics at different crystal planes, and a hyperactive AFP was
not tested. Ellipsometry experiments performed by Wilson et al. [20] estimated the accumulation of AFGPs
on ice surfaces. They found that the AFGPs accumulated on the ice surfaces over time,
and a plateau in accumulation was observed after approximately 60 min at the prism
plane. They also reported that the AFGPs did not appear to desorb from the ice surfaces
[20]. Their results have met with
skepticism due to certain inaccuracies in the measurements that discredited surface
accumulation over time [45].Our direct measurements of the AFP accumulation rates revealed that the initial
adsorption of the AFPs to ice (over a few seconds) was very fast, and this process was
similar for the AFPIII and TmAFP. Subsequently, the hyperactive
TmAFP accumulated progressively on the basal plane over a few hours.
The following section discusses these results provides an interpretation to place the
results into context.Several models have been proposed to describe the kinetics of AFP adsorption to ice
[13,28]. For example, Kubota's work described the
slow adsorption and desorption of AFPs, yielding a function that correlated the surface
coverage with time as , where σ is the surface coverage,
σmax is the maximum possible coverage,
t is the time from the ice formation and τ
is the time constant for the accumulation. This equation is a modified version of the
original model that takes into account the incubation time. Indeed, our measurements of
the AFPIII-GFP fluorescence intensity over time were consistent with this model, as
shown in figure 7d.
Knight & DeVries suggested that the inhibition of ice growth by those AFPs that
could not bind to the basal plane (moderate AFPs) was not time-dependent and was instead
a function of the AFP concentration and the degree of supercooling [32]. Thus, considering that AFPIII could
not bind to the basal plane, the accumulation on the prism plane did not contribute to
the TH activity. Indeed, AFPIII adsorbed to the prism plane rapidly
(Kon = 0.008 ± 0.001
µM−1 s−1), and the TH was found to be
insensitive (relative to the behaviour of hypAFP) to the exposure time. The modest time
dependence occurred on a timescale that exceeded the accumulation kinetics of the
fluorescence signal. The measured Kon value presented here
is the first experimental report of the adsorption constant of AFP molecules to ice.On the other hand, the hyperactive TmAFP accumulated on the basal plane
in a slow and progressive manner. Our measurements of the accumulation of
TmAFP did not reveal any particular timescale
(τ). A multi-exponential function with at least three time
constants was needed to describe the fluorescence data. Processes that must be modelled
across many timescales or through the use of a stretched exponential are common in
annealing processes, for example, in glass ageing [46]. The Weibull distribution [47] describes systems in which the durability of a
bacteria population changes over time, and the time to decimation is not constant. In
our system, multiple timescales could indicate that the adsorption of
TmAFP-GFP to ice was influenced by both the number of binding sites
and by another process, such as the suitability of the available binding sites to
interactions with AFP. The secondary binding process proposed by Takamichi et
al. [21] provides a
possible example of such a process. Garnham et al. [26] suggested that the pattern of bound
water may also contribute to these dynamics. Several subpopulations of the AFP-bound
water molecules may potentially fit different residual binding sites on the ice. The
basal plane binding could explain the enhanced TH activity of the TmAFP
and sbwAFP over long periods of time, as was observed in our TH measurements.
Accordingly, the ability of the hypAFPs to bind to the basal plane and to inhibit ice
growth on this plane contributed most significantly to the time-dependent TH
activity.The interpretations of our results may be summarized in terms of two kinetic processes
that contribute to TH. First, the AFPs blocked ice crystal growth in a
concentration-dependent manner, as described by Sander et al. [28] and Knight & DeVries [32]. According to their theory, the
velocity of an advancing ice front reduces to zero at certain AFP concentrations,
depending on the degree of supercooling. Once the AFPs are adsorbed onto an ice crystal
surface and the ice growth has been arrested, the second kinetic process of protein
accumulation governs the TH. Sander suggested this possibility in previous publications
[28]. We found that the
hyperactive and moderate AFPs differed in their abilities to further inhibit crystal
growth. HypAFPs accumulated over time, particularly on the basal plane, and protected
the crystal from prematurely ending its TH. Moderate AFPs cannot bind to the basal plane
and, for this reason, do not display kinetics that depend significantly on the
incubation time. As mentioned above, Takamichi et al. [21] explained their measurements of TH
enhancement over time by hypothesizing a ‘secondary binding’ conformation
of AFPs. This explanation would suggest, however, that the moderate AFPs that bound in
such configurations onto the prism plane only did not directly affect the TH activity.
Alternatively, the TH enhancement over time by the moderate AFPs may be explained by a
slow decrease in the basal plane surface area as was mentioned by Knight &
DeVries [32]. One supporting piece of
evidence for this claim is that when a crystal was incubated at a higher degree of
supercooling, the extent to which the incubation time enhanced the TH increased. Thus, a
bipyramidal crystal that is incubated at a high degree of supercooling, gradually grows
in the c-direction and consequently decreases the basal plane surface
area which leads to higher TH activities.Our experiments using fluorescence microscopy techniques in conjunction with
microfluidic devices demonstrated the binding of AFPs to ice crystals during the active
exchange of solutions around a crystal. This study revealed the complex dynamics of
protein attachment to the ice crystals and the time-dependent effects of protein
attachment on the TH activity. The sensitivity of TH to the exposure time highlights the
necessity of reporting the exposure time parameter along with any reported AFP TH
activity. This is especially important for the TH activities of proteins that are highly
sensitive to the exposure time, such as sbwAFP and TmAFP. The
relationship between the number of AFP molecules accumulated onto an ice surface and the
measured TH will be investigated further in future studies.
Authors: Peter L Davies; Jason Baardsnes; Michael J Kuiper; Virginia K Walker Journal: Philos Trans R Soc Lond B Biol Sci Date: 2002-07-29 Impact factor: 6.237
Authors: Andrew J Scotter; Christopher B Marshall; Laurie A Graham; Jack A Gilbert; Christopher P Garnham; Peter L Davies Journal: Cryobiology Date: 2006-08-02 Impact factor: 2.487
Authors: Luuk L C Olijve; Konrad Meister; Arthur L DeVries; John G Duman; Shuaiqi Guo; Huib J Bakker; Ilja K Voets Journal: Proc Natl Acad Sci U S A Date: 2016-03-02 Impact factor: 11.205
Authors: Kai Liu; Chunlei Wang; Ji Ma; Guosheng Shi; Xi Yao; Haiping Fang; Yanlin Song; Jianjun Wang Journal: Proc Natl Acad Sci U S A Date: 2016-12-07 Impact factor: 11.205