Fusulinids with ?Biomoldic Void

PMH-1, Javorniški Rovt, the western Southern Karavanks.

Trogkofel Formation (upper part)/Goggau Limestone?

Back-reef or back-bank lagoon with well-lit, well-agitated shallow water indicated by dasyclads and Osagid grains.

Bioclastic rudstone with peloidal-bioclastic packstone matrix (biopelmicrudite), containing fusulinids, dasyclad and dissolution void (?biomoldic pore space) with isopachous cement rim and geopetal infilling of calcisiltite and mosaic sparite