Biogenic crystals, i.e., crystals produced by living organisms, have attracted a great deal of attention in latter years because of their fascinating microstructures and superior properties. [1][2][3] The interrelation between the microstructure of materials and their properties is a key issue of materials science. Impressive examples of scientific achievements in this field include our ability to control the strength of metals and alloys by annealing-mediated grain size, [4] and bandgap engineering in semiconductor thin film structures by lattice mismatch-mediated interfacial strains. [5] At the same time, unique methods for controlling microstructure and, hence, crystal properties, exist in nature. In fact, organisms can control the polymorphism, [6][7][8] morphology, [9] orientation, and size of crystalline blocks [10] in biogenic crystals by means of organic molecules involved in the biomineralization process. These organic molecules can stabilize an amorphous precursor phase, [11][12][13][14] which might also play an important role in the control of the material properties of the end product. However, not much is yet known about the molecular mechanisms that control the interaction between the organic phase and the growing mineral. In this paper, we shed additional light on these interactions by tracking the microstructure modifications in biogenic calcite after heat treatments at elevated temperatures. Our findings allow us to better understand the microstructure of biocomposites on a nanometer scale, which we believe is of great importance to future design and fabrication of bio-inspired advanced materials. At the end of the 1980s, Berman et al. [15] showed that occluded organic molecules are located within biogenic calcite (CaCO 3 ) crystals and proposed that these intracrystalline molecules reveal chemical recognition to specific atomic planes. The researchers suggested that during biomineralization, the organic macromolecules adhere to specific planes and impede crystal growth in the perpendicular direction, which respectively lowers the size of coherently scattered crystal blocks. [15][16][17] This fact indicates that organisms can also control the preferred orientation (texture) of biogenic crystals. By measuring the "coherent lengths" for X-ray scattering along different directions in biogenic calcite crystals and then comparing these values with those in synthetic calcite, the researchers were able to determine the crystallographic planes on which the organic molecules presumably adhere. However, to date we have practically no information about the specific types of macromolecules, their conformation states, and how exactly they match the mineral structure. Very recently we showed that organisms could control not only the texture, but in some sense the atomic structure of biogenic crystals. Specifically, by using high-resolution X-ray powder diffraction at dedicated synchrotron beam lines, we found anisotropic lattice distortions in mollusk-made aragonite [18] and calcite, [19] as compared to their ...