The basic architecture (Bauplan) and microstructure of the skeleton of
Recent Gardineria are noticeably different from those of most other m
odern scleractinians. The wall of the Gardineria skeleton is entirely
epithecate (non-trabecular). while in the majority of modern Scleracti
nia the epitheca is either absent or added to the main wall which usua
lly is of trabecular nature. These different patterns of theca formati
on reflect significant anatomical differences in the peripheral parts
of the polyp. The Bauplan of Gardineria pattern, exceptional in the mo
dern scleractinian fauna, was widespread among early Mesozoic corals,
particularly among the Triassic protoheterastraeids. Similar skeletons
also occur in some late Palaeozoic rugosans (e.g., polycoeliids). Zar
dinophyllum zardini, an aberrant Triassic scleractinian coral, with a
supposed rugosan septal insertion, supports the hypothesis of the rugo
san origin of the Scleractinia.