the first report of the koilosoma ichnofossil cenonian on golbaf section (southeast of kerman)

Cenonian detrital deposits in the south of golbaf, located in the southeast of kerman, are 147 meters thick and consist of siltstone, silty siltstone sandstone and shale. the studied section contains many ichnofossils, including koilosoma ichnofossils in red siltstone sandstones of the studied sequence, which have been seen in continental environments such as rivers to sea. it is the only ichnofossil work that can be attributed to the scoyenia ichnofassies. this low many ichnofossil has a hollow, irregular polygonal structure that resembles a honeycomb. has a nutritional behavior pattern that refers to the activity of frog babies.