Solution-grown single crystals of Fe2OBO3 were characterized by specific heat, Mössbauer spectroscopy, and x-ray diffraction. A peak in the specific heat at 340 K indicates the onset of charge order. Evidence for a doubling of the unit cell at low temperature is presented. Combining structural refinement of diffraction data and Mössbauer spectra, domains with diagonal charge order are established. Bond-valence-sum analysis indicates integer valence states of the Fe ions in the charge ordered phase, suggesting Fe2OBO3 is the clearest example of ionic charge order so far.PACS numbers: 61.50. Ks, 71.30.+h, 71.28.+d, 61.10.Nz Many physical phenomena in transition metal oxides, including colossal magnetoresistance [1] and hightemperature superconductivity [2], are related to charge ordering (CO). Ideally, CO consists of charge carriers localizing on ions with different integer valences forming an ordered pattern [3]. However, the application of this "ionic CO" concept has been controversial [4,5], because observed valence separations are usually small, and there is no clear example of CO with integer valences.Mössbauer spectra on the mixed-valent warwickite Fe 2 OBO 3 suggested a large, though not quantified, Fe valence separation below the onset of a monoclinic distortion of the structure (Fig. 1) at 317 K [6]. It is natural then to suspect an ordered arrangement of Fe 2+ and Fe 3+ ions (ionic CO), and Fe 2 OBO 3 has been suggested as an example of electrostatically driven CO [6]. However, no experimental evidence of a CO superstructure was found on the available polycrystalline samples, and consequently the occurrence of CO in Fe 2 OBO 3 has been under debate [7].Here, we report the first observation of superstructure reflections in single-crystalline Fe 2 OBO 3 , using X-ray diffraction. Combining structural refinement, Mössbauer spectroscopy, and electronic structure calculations, we establish a diagonal CO configuration. Bond-valence-sum analysis indicates that the ordered iron valence states are very close to integer Fe 2+ and Fe 3+ . Thus, Fe 2 OBO 3 is an excellent example of ionic CO. We discuss implications of the large structural modulations on the relevance of the electron-lattice coupling in driving the CO.Needle-like single crystals of Fe 2 OBO 3 (Fig. 2 inset) with length up to 1.5 cm were grown from a flux with a procedure very similar to the growth of Fe 1.91 V 0.09 OBO 3 reported by Balaev et al. [8], except that we omitted V 2 O 3 from the flux to avoid V doping.57 Fe Mössbauer spectra, obtained on powdered crystals using a constantacceleration spectrometer [9], were similar to previous results [6,10] with isomer shifts at low T (Fig. 5b) indicating divalent and trivalent Fe with no electron hopping.