Ice-binding mechanism of winter flounder antifreeze proteins

We have studied the winter flounder antifreeze protein (AFP) and two of its mutants using molecular dynamics simulation techniques. The simulations were performed under four conditions: in the gas phase, solvated by water, adsorbed on the ice (2021) crystal plane in the gas phase and in aqueous solution. This study provided details of the ice-binding pattern of the winter flounder AFP. Simulation results indicated that the Asp, Asn, and Thr residues in the AFP are important in ice binding and that Asn and Thr as a group bind cooperatively to the ice surface. These ice-binding residues can be collected into four distinct ice-binding regions: Asp-1/Thr-2/Asp-5, Thr-13/Asn-16, Thr-24/Asn-27, and Thr-35/Arg-37. These four regions are 11 residues apart and the repeat distance between them matches the ice lattice constant along the (1102) direction. This match is crucial to ensure that all four groups can interact with the ice surface simultaneously, thereby, enhancing ice binding. These Asx (x = p or n)/Thr regions each form 5-6 hydrogen bonds with the ice surface: Asn forms about three hydrogen bonds with ice molecules located in the step region while Thr forms one to two hydrogen bonds with the ice molecules in the ridge of the (2021) crystal plane. Both the distance between Thr and Asn and the ordering of the two residues are crucial for effective ice binding. The proper sequence is necessary to generate a binding surface that is compatible with the ice surface topology, thus providing a perfect "host/guest" interaction that simultaneously satisfies both hydrogen bonding and van der Waals interactions. The results also show the relation among binding energy, the number of hydrogen bonds, and the activity. The activity is correlated to the binding energy, and in the case of the mutants we have studied the number of hydrogen bonds. The greater the number of the hydrogen bonds the greater the antifreeze activity. The roles van der Waals interactions and the hydrophobic effect play in ice binding are also highlighted. For the latter it is demonstrated that the surface of ice has a clathratelike structure which favors the partitioning of hydrophobic groups to the surface of ice. It is suggested that mutations that involve the deletion of hydrophobic residues (e.g., the Leu residues) will provide insight into the role the hydrophobic effect plays in partitioning these peptides to the surface of ice.     

Adsorption of alpha-helical antifreeze peptides on specific ice crystal surface planes.

The noncolligative peptide and glycopeptide antifreezes found in some cold-water fish act by binding to the ice surface and preventing crystal growth, not by altering the equilibrium freezing point of the water. A simple crystal growth and etching technique allows determination of the crystallographic planes where the binding occurs. In the case of elongated molecules, such as the alpha-helical peptides in this report, it also allows a deduction of the molecular alignment on the ice surface. The structurally similar antifreeze peptides from winter flounder (Pseudopleuronectes americanus) and Alaskan plaice (Pleuronectes quadritaberulatus) adsorb onto the (2021) pyramidal planes of ice, whereas the sculpin (Myoxocephalus scorpius) peptide adsorbs on (2110), the secondary prism planes. All three are probably aligned along (0112). These antifreeze peptides have 11-amino acid sequence repeats ending with a polar residue, and each repeat constitutes a distance of 16.5 A along the helix, which nearly matches the 16.7 A repeat spacing along (0112) in ice. This structural match is undoubtedly important, but the mechanism of binding is not yet clear. The suggested mechanism of growth inhibition operates through the influence of local surface curvature upon melting point and results in complete inhibition of the crystal growth even though individual antifreeze molecules bind at only one interface orientation.     

A model for binding of an antifreeze polypeptide to ice.

A model is proposed, based on recent peptide analog and ice crystal etching studies, whereby an alanine-rich, alpha-helical antifreeze polypeptide (AFP) from the winter flounder inhibits the growth of ice crystals by hydrogen bonding of Thr, Asn, and Asp side chains in a specific pattern to the [2021] hexagonal bipyramidal planes of ice. It is further suggested that this mode of binding is unidirectional, maximizing opportunities for packing of AFPs on the ice surface, and that ice crystal growth inhibition occurs by a two-step mechanism involving hydrogen bonding and hydrophobic interpeptide interactions.     

Contribution of hydrophobic residues to ice binding by fish type III antifreeze protein

Type III antifreeze protein (AFP) is a 7-kDa globular protein with a flat ice-binding face centered on Ala 16. Neighboring hydrophilic residues Gln 9, Asn 14, Thr 15, Thr 18 and Gln 44 have been implicated by site-directed mutagenesis in binding to ice. These residues have the potential to form hydrogen bonds with ice, but the tight packing of side chains on the ice-binding face limits the number and strength of possible hydrogen bond interactions. Recent work with alpha-helical AFPs has emphasized the hydrophobicity of their ice-binding sites and suggests that hydrophobic interactions are important for antifreeze activity. To investigate the contribution of hydrophobic interactions between type III AFP and ice, Leu, Ile and Val residues on the rim of the ice-binding face were changed to alanine. Mutant AFPs with single alanine substitutions, L19A, V20A, and V41A, showed a 20% loss in activity. Doubly substituted mutants, L19A/V41A and L10A/I13A, had less than 50% of the activity of the wild type. Thus, side chain substitutions that leave a cavity or undercut the contact surface are almost as deleterious to antifreeze activity as those that lengthen the side chain. These mutations emphasize the importance of maintaining a specific surface contour on the ice-binding face for docking to ice.     

Analysis of shorthorn sculpin antifreeze protein stereospecific binding to (2-1 0) faces of ice.

In this paper we report the results of our studies on the stereospecific binding of shorthorn sculpin antifreeze protein (AFP) to (2 -1 0) secondary prism faces of ice. Using ice crystal growth and etching techniques together with molecular modeling, molecular dynamics, and energy minimization, we explain the nature of preferential binding of shorthorn sculpin AFP along the [1 2 2] direction on (2- 1 0) planes. In agreement with ice etching studies, the mechanism of preferential binding suggested by molecular modeling explains why the binding of shorthorn sculpin AFP occurs along [1 2 2] and not along its mirror symmetry-related direction [-1 -2 2] on (2 -1 0). This binding mechanism is based on the protein-crystal surface enantioselective recognition that utilizes both alpha-helical protein backbone matching to the (2 -1 0) surface topography and matching of side chains of polar/charged residues with specific water molecule positions in the ice surface. The mechanisms of winter flounder and shorthorn sculpin antifreeze binding to ice are compared.     

Rational design of alpha-helical antifreeze peptides.

The alanine-rich alpha-helical antifreeze protein from the winter flounder Pseudopleuronectes americanus adsorbs to specific planes of ice guided by an ice lattice match to threonine residues regularly spaced 16.6 A apart. We report here that by redesigning the winter flounder antifreeze peptide to incorporate a 27.1-A spacing between putative 'ice-binding' threonines, the deduced binding alignment of the helical molecule on the ice lattice is changed from the Miller indices directional vector [1102 ] to [2203 ]. Subsequent ice-binding characteristics are altered, including changes in adsorption specificity, decreases in thermal hysteresis activity and the formation of rotated hexagonal bipyramid ice crystal morphology.     

Structure of a peptide antifreeze and mechanism of adsorption to ice

Sequence studies of an alpha-helical peptide antifreeze isolated from winter flounder have revealed the presence of clusters of polar amino acids separated by long sequences of alanine. Most of the polar residues are threonine and aspartate and are separated by 4.5 A, a repeat distance that also separates the oxygens in the ice lattice along the a-axis of an ice crystal. Such a lattice match suggests that the peptide binds to ice by means of hydrogen binding.     

Interaction among the twelve-residue segment of antifreeze protein type I,or its mutants,water and a hexagonal ice crystal

We have carried out a molecular dynamics analysis on a mixture of supercooled water, a hexagonal ice crystal and segments of winter flounder antifreeze protein. The segment consists of nine alanine residues, two threonine residues and one asparagine residue. Mutant segments, in which the threonine residues are replaced with valine residues, or serine residues, are also used. It is found that the threonine residue near the asparagine residue of the original segment is located in the vicinity of the prism face of the ice crystal. This is due to the hydrogen bond between the hydrophilic sites of these residues and water molecules, and the hydrogen bond between these water molecules and the water molecules on the ice surface. The valine and serine residues in the mutant segments do not approach the prism face of the ice crystal compared with the threonine residue near the asparagine residue. The motion of five segments, closely located side by side, is not remarkable. This is because of the gathering of water molecules caused by hydrophobic hydration, not only around alanine residues but also around the methyl sites of threonine residues.     

Adsorption to ice of fish antifreeze glycopeptides 7 and 8.

Experimental results show that fish antifreeze glycopeptides (AFGPs) 8 and 7 (with 4 and 5 repeats respectively of the Ala-Ala-Thr backbone sequence) bond onto ice prism planes aligned along a-axes, and inhibit crystal growth on prism planes and on surfaces close to that orientation. The 9.31-A repeat spacing of the AFGP in the polyproline II helix configuration, deduced from NMR studies, matches twice the repeat spacing of ice in the deduced alignment direction, 9.038 A, within 3%. A specific binding model is proposed for the AFGP and for the alpha-helical antifreeze peptide of winter flounder. For AFGP 7-8, two hydroxyl groups of each disaccharide (one disaccharide is attached to each threonine) reside within the ice surface, so that they are shared between the ice crystal and the disaccharide. This provides 24 hydrogen bonds between AFGP 8 and the ice and 30 for AFGP 7, explaining why the chemical adsorption is virtually irreversible and the crystal growth can be stopped virtually completely. The same scheme of sharing polar groups with the ice works well with the alpha-helical antifreeze of winter flounder, for which an amide as well as several hydroxyls are shared. The sharing of polar groups with the ice crystal, rather than hydrogen-bonding to the ice surface, may be a general requirement for adsoprtion-inhibition of freezing.     

Identification of the ice-binding face of antifreeze protein from Tenebrio molitor

The beetle Tenebrio molitor produces several isoforms of a highly disulfide-bonded beta-helical antifreeze protein with one surface comprised of an array of Thr residues that putatively interacts with ice. In order to use mutagenesis to identify the ice-binding face, we have selected an isoform that folds well and is tolerant of amino acid substitution, and have developed a heating test to monitor refolding. Three different types of steric mutations made to the putative ice-binding face reduced thermal hysteresis activity substantially while a steric mutation on an orthogonal surface had little effect. NMR spectra indicated that all mutations affected protein folding to a similar degree and demonstrated that most of the protein folded well. The large reductions in activity associated with steric mutations in the Thr array strongly suggest that this face of the protein is responsible for ice binding.     

Hydrogen bonding on the ice-binding face of a beta-helical antifreeze protein indicated by amide proton NMR chemical shifts

The dependence of amide proton chemical shifts on temperature is used as an indication of the hydrogen bonding properties in a protein. The amide proton temperature coefficients of the beta-helical antifreeze protein from Tenebrio molitor are examined to determine their hydrogen bonding state in solution. The temperature-dependent chemical shift behavior of the amides in T. molitor antifreeze protein varies widely throughout the protein backbone; however, very subtle effects of hydrogen bonding can be distinguished using a plot of chemical shift deviation (CSD) versus the backbone amide chemical shift temperature gradient (Deltadelta/DeltaT). We show that differences between the two ranks of ice-binding threonine residues on the surface of the protein indicate that threonine residues in the left-hand rank participate in intrastrand hydrogen bonds that stabilize the flat surface required for optimal ice binding.     

Quantitative and qualitative analysis of type III antifreeze protein structure and function

Some cold water marine fishes avoid cellular damage because of freezing by expressing antifreeze proteins (AFPs) that bind to ice and inhibit its growth; one such protein is the globular type III AFP from eel pout. Despite several studies, the mechanism of ice binding remains unclear because of the difficulty in modeling the AFP-ice interaction. To further explore the mechanism, we have determined the x-ray crystallographic structure of 10 type III AFP mutants and combined that information with 7 previously determined structures to mainly analyze specific AFP-ice interactions such as hydrogen bonds. Quantitative assessment of binding was performed using a neural network with properties of the structure as input and predicted antifreeze activity as output. Using the cross-validation method, a correlation coefficient of 0.60 was obtained between measured and predicted activity, indicating successful learning and good predictive power. A large loss in the predictive power of the neural network occurred after properties related to the hydrophobic surface were left out, suggesting that van der Waal's interactions make a significant contribution to ice binding. By combining the analysis of the neural network with antifreeze activity and x-ray crystallographic structures of the mutants, we extend the existing ice-binding model to a two-step process: 1) probing of the surface for the correct ice-binding plane by hydrogen-bonding side chains and 2) attractive van der Waal's interactions between the other residues of the ice-binding surface and the ice, which increases the strength of the protein-ice interaction.     

Primary quinone (QA) binding site of bacterial photosynthetic reaction centers: mutations at residue M265 probed by FTIR spectroscopy

In the primary quinone (Q(A)) binding site of Rb. sphaeroides reaction centers (RCs), isoleucine M265 is in extensive van der Waals contact with the ubiquinone headgroup. Substitution of threonine or serine for this residue (mutants M265IT and M265IS), but not valine (mutant M265IV), lowers the redox midpoint potential of Q(A) by about 100 mV (Takahashi et al. (2001) Biochemistry 40, 1020-1028). The unexpectedly large effect of the polar substitutions is not due to reorientation of the methoxy groups as similar redox potential changes are seen for these mutants with either ubiquinone or anthraquinone as Q(A). Using FTIR spectroscopy to compare Q(A)(-)/Q(A) IR difference spectra for wild type and the M265 mutant RCs, we found changes in the polar mutants (M265IT and M265IS) in the quinone C[double bond]O and C[double bond]C stretching region (1600-1660 cm(-1)) and in the semiquinone anion band (1440-1490 cm(-1)), as well as in protein modes. Modeling the mutations into the X-ray structure of the wild-type RC indicates that the hydroxyl group of the mutant polar residues, Thr and Ser, is hydrogen bonded to the peptide C[double bond]O of Thr(M261). It is suggested that the mutational effect is exerted through the extended backbone region that includes Ala(M260), the hydrogen bonding partner to the C1 carbonyl of the quinone headgroup. The resulting structural perturbations are likely to include lengthening of the hydrogen bond between the quinone C1[double bond]O and the peptide NH of Ala(M260). Possible origins of the IR spectroscopic and redox potential effects are discussed.     

The role of Ca2+-coordinating residues of herring antifreeze protein in antifreeze activity

The type II antifreeze protein of Atlantic herring (Clupea harengus harengus) requires Ca(2+) as a cofactor to inhibit the growth of ice crystals. On the basis of homology modeling with Ca(2+)-dependent lectin domains, five residues of herring antifreeze protein (hAFP) are predicted to be involved in Ca(2+) binding: Q92, D94, E99, N113, and D114. The role of E99, however, is less certain. A previous study on a double mutant EPN of hAFP suggested that the Ca(2+)-binding site of hAFP was the ice-binding site. However, it is possible that Ca(2+) might function distantly to affect ice binding. Site-directed mutagenesis was performed on the Ca(2+)-coordinating residues of hAFP in order to define the location of the ice-binding site and to explore the role of these residues in antifreeze activity. Properties of the mutants were investigated in terms of their structural integrity and antifreeze activity. Equilibrium dialysis analysis demonstrated that E99 is a Ca(2+)-coordinating residue. Moreover, proteolysis protection assay revealed that removal of Ca(2+) affected the conformation of the Ca(2+)-binding loop rather than the core structure of hAFP. This finding rules out the possibility that Ca(2+) might act at a distance via a conformational change to affect the function of hAFP. Substitutions at positions 99 and 114 resulted in severely reduced thermal hysteresis activity. These data indicate that the ice-binding site of hAFP is located at the Ca(2+)-binding site and the loop region defined by residues 99 and 114 is important for antifreeze activity.     

Antifreeze protein from freeze-tolerant grass has a beta-roll fold with an irregularly structured ice-binding site

The grass Lolium perenne produces an ice-binding protein (LpIBP) that helps this perennial tolerate freezing by inhibiting the recrystallization of ice. Ice-binding proteins (IBPs) are also produced by freeze-avoiding organisms to halt the growth of ice and are better known as antifreeze proteins (AFPs). To examine the structural basis for the different roles of these two IBP types, we have solved the first crystal structure of a plant IBP. The 118-residue LpIBP folds as a novel left-handed beta-roll with eight 14- or 15-residue coils and is stabilized by a small hydrophobic core and two internal Asn ladders. The ice-binding site (IBS) is formed by a flat beta-sheet on one surface of the beta-roll. We show that LpIBP binds to both the basal and primary-prism planes of ice, which is the hallmark of hyperactive AFPs. However, the antifreeze activity of LpIBP is less than 10% of that measured for those hyperactive AFPs with convergently evolved beta-solenoid structures. Whereas these hyperactive AFPs have two rows of aligned Thr residues on their IBS, the equivalent arrays in LpIBP are populated by a mixture of Thr, Ser and Val with several side-chain conformations. Substitution of Ser or Val for Thr on the IBS of a hyperactive AFP reduced its antifreeze activity. LpIBP may have evolved an IBS that has low antifreeze activity to avoid damage from rapid ice growth that occurs when temperatures exceed the capacity of AFPs to block ice growth while retaining the ability to inhibit ice recrystallization.     

Biochemistry of fish antifreeze proteins

Four distinct macromolecular antifreezes have been isolated and characterized from different marine fish. These include the glycoprotein antifreezes (Mr 2.5-33 K), which are made up of a repeating tripeptide (Ala-Ala-Thr)n with a disaccharide attached to the threonyl residues, and three antifreeze protein (AFP) types. Type I is an alanine-rich, amphiphilic, alpha-helix (Mr 3-5 K); type II is a larger protein (Mr 14 K) with a high content of reverse turns and five disulfide bridges; and type III is intermediate in size (Mr 6-7 K) with no distinguishing features of secondary structure or amino acid composition. Despite their marked structural differences, all four antifreeze types appear to function in the same way by binding to the prism faces of ice crystals and inhibiting growth along the a-axes. It is suggested that type I AFP binds preferentially to the prism faces as a result of interactions between the helix macrodipole and the dipoles on the water molecules in the ice lattice. Binding is stabilized by hydrogen bonding, and the amphiphilic character of the helix results in the hydrophobic phase of the helix being exposed to the solvent. When the solution temperature is lowered further, ice crystal growth occurs primarily on the uncoated, unordered basal plane resulting in bipyramidal-shaped crystals. The structural features of type I AFP that could contribute to this mechanism of action are reviewed. Current challenges lie in solving the other antifreeze structures and interpreting them in light of what appears to be a common mechanism of action.     

Alternative roles for putative ice-binding residues in type I antifreeze protein

Two sets of variants of type I antifreeze protein have been synthesized to investigate the role of Leu and Asn in the activity of this 37-residue alpha-helix. Leu and Asn flank the central two of four regularly spaced ice-binding Thr in the i-1 and i + 3 positions, respectively. All three residues project from the same side of the helix to form the protein's putative ice-adsorption site and are considered in some models to act together as an "ice-binding motif". Replacement of Asn by residues with shorter side chains resulted in either a small loss (Ala) or gain (Thr) of antifreeze activity. However, substitution of Asn by its slightly larger homologue (Gln) abolished thermal hysteresis activity. The Gln-containing peptide was very soluble, largely monomeric, and fully helical. Of the three variants in which Leu was replaced by Ala, two of the three were more active than their Leu-containing counterparts, but all three variants began to precipitate as the peptide concentration increased. None of the seven variants tested showed dramatic differences in ice crystal morphology from that established by the wild type. These results are consistent with a primary role for Leu in preventing peptide aggregation at the antifreeze protein concentrations (10 mg/mL) normally present in fish serum. Similarly the role for Asn may have more to do with enhancing the solubility of these rather hydrophobic peptides than of making a stereospecific hydrogen-bonding match to the ice lattice as traditionally thought. Nevertheless, the dramatic loss of activity in the Asn-to-Gln replacement demonstrates the steric restriction on residues in or near the ice-binding site of the peptide.     

Multiple genes provide the basis for antifreeze protein diversity and dosage in the ocean pout, Macrozoarces americanus

The ocean pout (Macrozoarces americanus) produces a set of antifreeze proteins that depresses the freezing point of its blood by binding to, and inhibiting the growth of, ice crystals. The amino acid sequences of all the major components of the ocean pout antifreeze proteins, including the immunologically distinct QAE component, have been derived by Edman degradation. In addition, sequences of several minor components were deduced from DNA sequencing of cDNA and genomic clones. Fifty percent of the amino acids are perfectly conserved in all these proteins as well as in two homologous sequences from the distantly related wolffish. Several of the conserved residues are threonines and asparagines, amino acids that have been implicated in ice binding in the structurally unrelated antifreeze protein of the righteye flounders. Aside from minor differences in post-translational modifications, heterogeneity in antifreeze protein components stems from amino acid differences encoded by multiple genes. Based on genomic Southern blots and library cloning statistics there are 150 copies of the 0.7-kilobase-long antifreeze protein gene in the Newfoundland ocean pout, the majority of which are closely linked but irregularly spaced. A more southerly population of ocean pout from New Brunswick in which the circulating antifreeze protein levels are considerably lower has approximately one-quater as many antifreeze protein genes. Thus, there appears to be a correlation between gene dosage and antifreeze protein levels, and hence the ability to survive in ice-laden seawater. Southern blot comparison of the two populations indicates that the differences in gene dosage were not generated by a simple set of deletions/duplications. They are more likely to be the result of differential amplification.     

A Ser residue influences the structure and stability of a Pro-kinked transmembrane helix dimer

When localized adjacent to a Pro-kink, Thr and Ser residues can form hydrogen bonds between their polar hydroxyl group and a backbone carbonyl oxygen and thereby modulate the actual bending angle of a distorted transmembrane α-helix. We have used the homo-dimeric transmembrane cytochrome b(559)' to analyze the potential role of a highly conserved Ser residue for assembly and stabilization of transmembrane proteins. Mutation of the conserved Ser residue to Ala resulted in altered heme binding properties and in increased stability of the holo-protein, most likely by tolerating subtle structural rearrangements upon heme binding. The results suggest a crucial impact of an intrahelical Ser hydrogen bond in defining the structure of a Pro-kinked transmembrane helix dimer.     

Interaction between a twelve-residue segment of antifreeze protein type I,or its mutants,and water molecules

A molecular dynamics simulation has been carried out for water molecules with a rigid segment of antifreeze protein type I. The segment consists of nine alanine residues, two threonine residues and one asparagine residue. Mutant segments, in which the threonine residues are replaced with valine residues, or serine residues, are also used. It is predicted that the hydrogen site of asparagine residue, and that of threonine residue, play an important role in the hydrogen bond of water molecules in these sites. This hydrogen bond is not noticeable between water molecules and the valine residue, or serine residue. The existence of four hydrophilic sites enhances the mobility of water molecules close to the serine residue of the mutant segment. The difference in the zenith-angle fluctuations of the original segment and the valine-mutant segment is less noticeable in the case of 230 K. This is because the gathering of water molecules due to the hydrophobic hydration is predominant near the alanine residues of the segments at this temperature.