[1] The Supergroup is composed of the Abu Mahara Group (ca.
[2] The supergroup contains a record of Neoproterozoic history, such as evidence of two glaciations, a massive reorganization of the global carbon cycle, and the Ediacaran-Cambrian transition.
[3] The Huqf Supergroup is exposed in the Jabal Akhdar of the Al Hajar Mountains, and in the deformed and metamorphosed domal culmination of the Saih Hatat.
[4] Source rocks of the Neoproterozoic to Cambrian Huqf Supergroup are associated with most of the South Oman oils.
[5] Huqf Supergroup preserves a complete sequence of Cryogenian, Ediacaran, and early Cambrian strata, becoming the group a reference in Earth history.