Upper Triassic terebratulid brachiopod Rhaetina shows differential preservation of shell structure under cathodoluminescent (CL) and scanning electron microscope (SEM), indicating intra- and interspecific differences in brachiopod growth patterns.In longitudinal sections, the CL lines appear firstly in inner, ontogenetically older parts of the shell and their outlines are parallel with the internal valve surface in posterior parts of the shell. In anterior parts of the shell, CL lines run diagonally towards the external valve surface and terminate in external growth lines. The shell structure of external growth lines indicates that major growth lines (associated with gradual reorientation of calcitic crystals due to reflection of the mantle edge) and disturbance lines (associated with abrupt mantle regression) are present at the terminations of CL lines. These data indicate that CL lines correspond to zones recording slowing/cessation of the growth rate. Under SEM, shell layers that are luminescent can be locally recognized as amalgamated or altered relicts of the secondary fibres. The origin of luminescence in these areas can be related to (1) the increased Mn-bearing diagenetic fluid flow favoured by higher porosity of altered secondary fibres, or can be caused by (2) temporal changes in the redox state controlling the solubility of Mn2+ and Fe2+ during the mantle anaerobiosis. Similarly, amalgamated/altered shell structure could either point to (1) the primary modification of shell secretory regime during the slowing/cessation in growth rate, or could be (2) the product of diagenetic processes responsible for post-depositional alteration of a shell structure, due to the primary shell heterogeneity/porosity in areas of growth discontinuities. Although presented data do not convincingly solve this uncertainty, the important point is that CL lines of studied brachiopods reflect changes in the growth rate and can be used in the investigation of growth dynamics in brachiopods, complementary to external growth lines and isotope or trace element analysis. In order to verify the modification of shell structure and understand the origin of associated luminescence during the change in growth rate unbiased by diagenetic overprint, it is necessary to examine modern brachiopods.The distribution pattern of CL lines that correlates with growth rate fluctuations potentially reflects a short-term environmental instability on the time scale of an individual life span. The data show correlation between CL line pattern and different bathymetric settings. Regular repetition of CL lines is preserved in Rhaetina gregaria, Rhaetina hybensis and Rhaetina pyriformis that occur in relatively uniform depositional settings below a normal storm wave base. In contrast, irregular pattern of CL lines is typical of R. gregaria from highly variable deposit associations derived from very shallow, subtidal settings above a normal storm wave base. In the case of R. gregaria, this difference reflects intraspecific variations in growth dynamics among bathymetric settings, indicating environmental control on their growth rates. Rhaetina gregaria is mostly the only one brachiopod species present in benthic assemblages from very shallow, marginal marine environments in the Western Tethys. The implication is that R. gregaria, in contrast to most other brachiopods, could live in physically stressed habitats characterized by higher environmental instability/unpredictability.