Key Points AML cells have increased mitochondrial mass, low respiratory chain complex activities, and low spare reserve capacity compared with normal cells. AML cells have heightened sensitivity to inhibitors of the respiratory chain complexes and oxidative stressors.

When polypeptide chains fold into a protein, hydrophobic groups are compacted in the center with exclusion of water. We report the crystal structure of an alanine-rich antifreeze protein that retains ~400 waters in its core. The putative ice-binding residues of this dimeric, four-helix bundle protein point inwards and coordinate the interior waters into two intersecting polypentagonal networks. The bundle makes minimal protein contacts between helices, but is stabilized by anchoring to the semi-clathrate water monolayers through backbone carbonyl groups in the protein interior. The ordered waters extend outwards to the protein surface and likely are involved in ice binding. This protein fold supports both the anchored-clathrate water mechanism of antifreeze protein adsorption to ice and the water-expulsion mechanism of protein folding.

The glycine-rich antifreeze protein recently discovered in snow fleas exhibits strong freezing point depression activity without significantly changing the melting point of its solution (thermal hysteresis). BLAST searches did not detect any protein with significant similarity in current databases. Based on its circular dichroism spectrum, discontinuities in its tripeptide repeat pattern, and intramolecular disulfide bonding, a detailed theoretical model is proposed for the 6.5-kDa isoform. In the model, the 81-residue protein is organized into a bundle of six short polyproline type II helices connected (with one exception) by proline-containing turns. This structure forms two sheets of three parallel helices, oriented antiparallel to each other. The central helices are particularly rich in glycines that facilitate backbone carbonyl-amide hydrogen bonding to four neighboring helices. The modeled structure has similarities to polyglycine II proposed by Crick and Rich in 1955 and is a close match to the polyproline type II antiparallel sheet structure determined by Traub in 1969 for (Pro-Gly-Gly)(n). Whereas the latter two structures are formed by intermolecular interactions, the snow flea antifreeze is stabilized by intramolecular interactions between the helices facilitated by the regularly spaced turns and disulfide bonds. Like several other antifreeze proteins, this modeled protein is amphipathic with a putative hydrophobic ice-binding face.

The snow flea (Hypogastrum harveyi) is protected from freezing at sub-zero temperatures by a glycine-rich antifreeze protein (AFP) that binds to seed ice crystals and prevents them from growing larger. This AFP is hyperactive and comprises two isoforms [Graham, L. A., and Davies, P. L. (2005) Science 310, 461]. The larger isoform (15.7 kDa) exhibits several-fold higher activity than the smaller isoform (6.5 kDa), although it is considerably less abundant. To establish the molecular basis for this difference in activity, we determined the sequence of the large isoform. The primary sequences of these two isoforms are surprisingly divergent. However, both contain tripeptide repeats and turn motifs that enabled us to build a three-dimensional model of the large isoform based upon the six-polyproline helix structure of the small isoform. Our model contains 13 polyproline type II helices connected by proline-containing loops stacked into two flat sheets oriented antiparallel to one another. The structure is strictly amphipathic, with a hydrophilic surface on one side and a hydrophobic, putative ice-binding surface on the other. The putative ice-binding site is approximately twice as large in area as that of the small isoform, providing an explanation for the difference in activity that is consistent with other examples noted. By tagging the recombinant AFP with green fluorescent protein, we observed its binding to multiple planes of ice, especially the basal plane. This finding supports the correlation between AFP hyperactivity and basal plane binding first observed with spruce budworm AFP.

Inchworm larvae of the pale beauty geometer moth, Campaea perlata, exhibit strong (6.4 °C) freezing point depression activity, indicating the presence of hyperactive antifreeze proteins (AFPs). We have purified two novel Thr- and Ala-rich AFPs from the larvae as small (∼3.5 kDa) and large (∼8.3 kDa) variants and have cloned the cDNA sequences encoding both. They have no homology to known sequences in current BLAST databases. However, these proteins and the newly characterized AFP from the Rhagium inquisitor beetle both contain stretches rich in alternating Thr and Ala residues. On the basis of these repeats, as well as the discontinuities between them, a detailed structural model is proposed for the 8.3 kDa variant. This 88-residue protein is organized into an extended parallel-stranded β-helix with seven strands connected by classic β-turns. The alternating β-strands form two β-sheets with a thin core composed of interdigitating Ala and Ser residues, similar to the thin hydrophobic core proposed for some silks. The putative ice-binding face of the protein has a 4 × 5 regular array of Thr residues and is remarkably flat. In this regard, it resembles the nonhomologous Thr-rich AFPs from other moths and some beetles, which contain two longer rows of Thr in contrast to the five shorter rows in the inchworm protein. Like that of some other hyperactive AFPs, the spacing between these ice-binding Thr residues is a close match to the spacing of oxygen atoms on several planes of ice.