Polymorphism of water has been extensively studied, but controversy still exists over the phase transition between high-density amorphous (HDA) and low-density amorphous (LDA) ice. We report the phase behavior of HDA ice inside high-pressure cryocooled protein crystals. Using X-ray diffraction, we demonstrate that the intermediate states in the temperature range from 80 to 170 K can be reconstructed as a linear combination of HDA and LDA ice, suggesting a first-order transition. We found evidence for a liquid state of water during the ice transition based on the protein crystallographic data. These observations open the possibility that the HDA ice induced by high-pressure cryocooling is a genuine glassy form of high-density liquid.liquid-liquid hypothesis ͉ supercooled water ͉ water phases ͉ high-density liquid S upercooled water shows anomalous thermodynamic behavior (1-3). Theories that account for these anomalous properties include the stability limit (4), the singularity-free (5, 6), and the liquid-liquid (LL) critical point (7) hypotheses. The latter 2 hypotheses propose the existence of 2 distinct forms of supercooled water: high-density liquid (HDL) and low-density liquid (LDL) water (8). In the singularity-free hypothesis, HDL transforms continuously to LDL. In the LL critical point theory, HDL undergoes a first-order phase transition to LDL (8). However, experimental study of the HDL-LDL phase transition is challenging as supercooled water spontaneously converts to crystalline forms below the homogeneous nucleation temperature (Ϸ235 K at 0.1 MPa). The transition between 2 glassy forms of water, high-density amorphous (HDA) and low-density amorphous (LDA) ice, has been extensively studied (9-18), as an analogue of the HDL-LDL transition. Controversy still exists as to whether the HDA-LDA ice transition is truly a first-order phase transition (10-13) or if it occurs because of a relaxation process of an unstable amorphous structure (15-18). More importantly, the connection between the HDA-LDA ice transition and the HDL-LDL phase transition, implied by thermodynamic and structural studies on water (19-22), remains challenging to prove experimentally (8).We used X-ray diffraction to study the transition of HDA to LDA ice in protein crystals. HDA ice was induced inside protein crystals by a high-pressure cryocooling method (23) originally developed for macromolecular crystallography (23-26). The Bragg diffraction from protein crystals mainly provides information on protein structure. The simultaneously recorded water diffuse diffraction (WDD) profile reports on the phase of the water in the protein crystal, which accounts for typically 40-60% of its volume. Fig. 1 shows diffraction images and the WDD profiles from a high-pressure cryocooled crystal of the globular protein thaumatin. As the crystal temperature is increased from 80 to 170 K, the primary WDD peak, corresponding to the mean distance between neighboring water molecule oxygen atoms, shifts to lower momentum transfer (Q) region [Q ϭ 4 sin( )/ , wh...