When first described, R. cratoensis was known from a single fossil adult which is a compression-impression fossil preserved in layers of soft sedimentary rock. Along with other well-preserved insect fossils, the R. cratoensis specimen was collected from layers of the Upper Aptian Crato Formation. The formation is composed of unweathered grey and oxidized yellow limestones, which preserved numerous insects, fish, birds and reptiles as a notable lagerstätten. The area is a preserved inland lake or one of a series of lakes, though the nature as a fresh or salt-water body is uncertain. The depth of the basin has been suggested as either shallow or fairly deep. The basin formed near the center of the supercontinent Gondwana during the early part of the diversification of flowering plants.
