Abstract
Corals studies in Libya are very limited, although they play an important role in the oil exploration as they form excellent reservoirs of coral reef buildups at some oil fields of Sirt Basin (e.g. Intisar “Idris” and Sahabi Fields). Both fields are produced from Paleocene coral reefs. Meanwhile, in Cyrenaica, corals are of less importance as they are not reported in subsurface tertiary rocks, which probably in the environmental settings of these sediments out of the core of reef as occurred in the surface. Meanwhile, corals are reported from older (Jurassic) subsurface successions as in Concession NC-152, but the cementation diagenesis leads to blocking and destroying the porosity. This study presents the first surface documentation work of eight scleractinian coral species from the exposed sediments in northern Libya, where sixtaxa is reported from Al Jabal al Akhdar region, these include a) an association of huge colonies of Caulastrea sp. and Stylophora sp., from the Middle Eocene Darnah Formation at West Darnah road cut section. Theco-existence of the fastCaulastrea sp. with the slow Stylophora sp. is due to the competition strategy; b) Antiguastrea sp. which is reported from the Oligocene Algal Limestone of Al Bayda Formation at Daryanah-Abyar Roadcut section; c) Cyphastrea sp. andAleveopora sp. from Oligo-Miocene Al Faidiyah Formation at Al Fatayah cement quarry and d) Tarbellastraea sp. From Middle Miocene Benghazi Formation at Benghazi Cement Quarry. In addition, two species Astraeaopora sp. and Actinacis paroraiare reported from the Upper Miocene sediments of formation “M” in As Sahabi area.
Highlights
This paper deals with corals built up in the Cyrenaica
The documented subsurface coral occurrences in Libya are very limited and are mainly obtained from the oil exploration activities, where coralreef forms an excellent reservoir as evidenced from some previous reports of oil fields in Sirt Basin (e.g. Intisar “Idris”) [2]
The older Jurassic branching cup corals with the interior skeleton are completely filled with calcite cement and lime-mud matrix resulted in blocking the porosity, which are occasionally reported from the base of core #7(16199’) in Well A1-NC152 by [4]
Summary
Belkasim Khameiss1*, William Hoyt2, Saad K. El Ebaidi3, Ahmed M. Muftah3, James Klaus4, Ann Budd5 1Department of Geological Sciences, Ball State University, Muncie, IN, USA 2Earth and Atmospheric Sciences, University of Northern Colorado, Greeley, CO, USA 3Department of Earth Sciences, Faculty of Science, University of Benghazi, Benghazi, Libya 4Department of Geological Science, University of Miami, Coral Gables, FL, USA 5Department of Geoscience, University of Iowa, Iowa City, IA, USA
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