Ostracods of the Cenomanian-Turonian transition in the Ksour and Amour Mountains (Saharan Atlas, Algeria)systematic and palaeobiogeographic implications

Referencias bibliográficas

• Abed, S. (1982). Lithostratigraphie et sédimentologie du Jurassique moyen et supérieur du Djebel Amour (Atlas saharien). MSc Thesis, Université de Pau, 242 p.
• Accarie, H.; Robaszynski, F.; Amédro, F.; Caron, M. & Zagrarni, M.F. (2000). Stratigraphie événementielle au passage Cénomanien-Turonien dans le secteur occidental de la plate-forme de Tunisie centrale (Formation Bahloul, région de Kalaat Senan). Annales des Mines et de la Géologie Tunis, 40: 63-80.
• Aguado, R.; Reolid, M. & Molina, E. (2016). Response of calcareous nannoplankton to the Late Cretaceous Oceanic Anoxic Event 2 at Oued Bahloul (central Tunisia). Palaeogeography, Palaeoclimatology, Palaeoecology, 459: 289-305. https://doi.org/10.1016/j.palaeo.2016.07.016
• Aït Ouali, R. (1991). Le rifting des monts des Ksour au Lias: Organisation du bassin, diagenèse des assises carbonatées, place dans les ouvertures mésozoïques au Maghreb. PhD Thesis, Université Houari Boumédiene Alger, 302 p.
• Aït Ouali, R. & Delfaud, J. (1995). Les modalités d'ouverture du bassin des Ksour au Lias dans le cadre du «rifting» jurassique au Maghreb. Comptes Rendus Academie Sciences, Paris, 320: 773-778.
• Al-Abdul Razzaq, S.K. (1979). Glenocythere, a new ostracode genus from the Hamadi Formation (Cretaceous) of Kuwait. Journal of Paleontology, 53: 920-930.
• Aly, M.F. & Abdel-Gawad, G.I. (2001). Upper Cenomaniane Lower Turonian ammonites from north and central Sinai, Egypt. El-Minia Science Bulletin, 13: 17-60.
• Aly, M.F.; Smadi, A. & Abu Azzam, H. (2008). Late Cenomanian-Early Turonian ammonites of Jordan. Revue de Paléobiologie, 27: 43-71.
• Amédro, A.; Accarie, H. & Robaszynski, F. (2005). Position de la limite Cénomanien-Turonien dans la Formation Bahloul de Tunisie centrale: apports intégrés des ammonites et des isotopes du carbone (δ13C). Eclogae Geologicae Helvetiae, 98: 151-167. https://doi.org/10.1007/s00015-005-1158-5
• Andreu, B. (1989). Le Crétacé moyen de la transversale Agadir-Nador (Maroc): précisions stratigraphiques et sédimentologiques. Cretaceous Research, 10: 49-80. https://doi.org/10.1016/0195-6671(89)90029-3
• Andreu, B. (1991). Les ostracodes du Crétacé moyen (Barrémien à Turonien), le long d'une transversale Agadir-Nador (Maroc). PhD Thesis, Touluse 3, 756 p. https://doi.org/10.1016/0031-0182(92)90020-6
• Andreu, B. (2002). Cretaceous ostracode biochronology of Morocco. Eclogae Geologicae Helvetiae, 95: 133-152.
• Andreu, B. & Bilotte, M. (2006). Ostracodes du Cenomanien supérieur et du Turpnien de la zone sous-pyrénéenne orientale (Corbières méridionales, SE France). Systématique, biostratigrahie, paléoécologie et paléobiogéographie. Revue de Micropaléontologie, 49: 55-73. https://doi.org/10.1016/j.revmic.2005.12.001
• Andreu, B.; Lebedel, V.; Wallez, M.J.; Lézin, C. & Ettachfini, M. (2013). The upper Cenomanian lower Turonian carbonate platform of the Preafrican Trough, Morocco: Biostratigraphic, paleoecological and paleobiogeographical distribution of ostracods. Cretaceous Research, 45: 216-246. https://doi.org/10.1016/j.cretres.2013.04.005
• Andreu, B. & Tronchetti, G. (1996). Ostracodes et foraminifères du Crétacé supérieur du synclinal d'El Koubbat. Moyen Atlas. Maroc: biostratigraphie, paléoenvironnements, paléobiogéographie. Systématique des ostracodes. Geobios, 29: 45-71. https://doi.org/10.1016/S0016-6995(96)80071-4
• Aquit, M.; Kuhnt, W.; Holbourn, A.; Chellai, E.H.; Stattegger, K.; Kluth, O. & Jabour, H. (2013). Late Cretaceous palleoenvironmental evolution of the Tarfaya Atlantic coastal Basin, SW Morocco. Cretaceous Research, 45: 288-305. https://doi.org/10.1016/j.cretres.2013.05.004
• Athersuch, J. (1988). The Biostratigraphy of Cretaceous Ostracods from Oman. Developments in Palaeontology and Stratigraphy, 11: 1187-1206. https://doi.org/10.1016/S0920-5446(08)70249-8
• Ayoub-Hannaa, W.; Huntley, J.W. & Fürsich, F.T. (2013). Significance of Detrended Correspondence Analysis (DCA) in palaeoecology and biostratigraphy: A case study from the Upper Cretaceous of Egypt. Journal of African Earth Sciences, 80: 48-59. https://doi.org/10.1016/j.jafrearsci.2012.11.012
• Babinot, J.F. (1980). Les ostracodes du Crétacé supérieur de Provence: systématique, biostratigraphie, paléoécologie, paléogéographie. Travaux du Laboratoire de Géologie Historique et Paléontologie, 10: 1-624.
• Babinot, J.F. & Basha, S.A. (1985). Ostracods from the Early Cenomanian of Jordan. A preliminary report. Geobios, 18: 257-262. https://doi.org/10.1016/S0016-6995(85)80019-X
• Barroso-Barcenilla, F.; Pascual, A.; Peyrot, D. & Rodríguez-Lazaro, J. (2011). Integrated biostratigraphy and chemostratigraphy of the upper Cenomanian and lower Turonian succession in Puentedey, Iberian Trough, Spain. Proceedings of Geologists' Association, 122: 67-81. https://doi.org/10.1016/j.pgeola.2010.11.002
• Bassiouni, M.A.A. (2002). Mid-Cretaceous (Aptian-Early Turonian) ostracoda from Sinai. Neue Paläontologische Abhandlungen, 5: 1-123.
• Bassoullet, J.P. (1973). Contribution à l'étude stratigraphique du Mésozoïque de l'Atlas saharien occidental (Algérie). PhD Thesis, Univ. Pierre et Marie Curie Paris, 477 p.
• Bassoullet, J.P. & Damotte, R. (1969). Quelques ostracodes nouveaux du Cénomanien-Turonien de l'Atlas saharien occidental (Algérie). Revue de Micropaléontologie, 3: 130-144.
• Bauer, J.; Kuss, J. & Steuber, T. (2002). Platform environments, microfacies and systems tracts of the Upper Cenomanian - Lower Santonian of Sinai, Egypt. Facies, 47: 1-25. https://doi.org/10.1007/BF02667703
• Benadla, M. (2019). Le passage Cénomanien-Turonien dans l'Atlas Saharien algérien: Sédimentologie, Biostratigraphie et Géochimie. PhD Thesis, University of Tlemcen, 184 p.
• Benadla, M.; Reolid, M.; Marok, A. & El Kamali, N. (2018). The Cenomanian-Turonian transition in the carbonate platform facies of the Western Saharan Atlas (Rhoundjaïa Formation, Algeria). Journal of Iberian Geology, 44: 405-429. https://doi.org/10.1007/s41513-018-0070-6
• Bergue, C.T.; Fauth, G.; Coimbra, J.C.; Ahmad, F.Y.; Smadi, A. & Farouk, S. (2016). The late Albian-early Cenomanian ostracodes from Naur formation, Jordan. Revista Brasileira de Paleontologia, 19: 195-210. https://doi.org/10.4072/rbp.2016.2.04
• Bettahar, A. (2009). Les accidents majeurs de l'Atlas saharien central et les structures associées. PhD Thesis, University of Science and Technology Houari Boumediene, 210 p.
• Bettahar, A.; Ait Ouali, R. & Beche, A. (2007). Etude de la région de Djebel Er-Radjel à déformation polyphasée avec mise en évidence d'une inversion tectonique (Atlas saharien central, Algérie). Bulletin Service géologique National, 18: 43-56.
• Bismuth, H.; Donze, P.; Lefevre, J. & Saint-Marc, P. (1981). Nouvelles espèces d'ostracodes dans le Crétacé Moyen et supérieur du Djebel Semmama (Tunisie du Centre-Nord). Cahiers de Micropaléontologie, 3: 51-69. https://doi.org/10.1016/0195-6671(82)90018-0
• Bonnet, L.; Andreu, B.; Rey, J.; Cubaynes, R.; Ruget, C.; N'Zaba-Makaya, O. & Brunel, F. (1999). Fluctuations of environmental factors as seen by means of statistical analyses in micropaleontological assemblages from a Liassic Series. Micropaleontology, 45: 399-417. https://doi.org/10.2307/1486122
• Boukhary, M.; Eissa, R. & Kerdany, M. (1977). Some ostracod species from the Galala Formation, western coast of the Gulf of Suez, Egypt. Proceedings Egyptian Academy Sciences Cairo, 30: 155-161.
• Boukhary, M.; Morsi, A.M.; Eissa, R. & Kerdany, M. (2009). Late Cenomanian ostracode faunas from the area south of Ain Sukhna, werstern side of the Suez, Egypt. Geologica Croatica, 62: 19-30. https://doi.org/10.4154/GC.2009.02
• Bracene, R. (2001). Géodynamique du nord de l'Algérie: impact sur l'exploration pétrolière. PhD Thesis, University of Cergy Pontoise, 101 p.
• Bryant, R. & Belanger, C.L. (2023). Spatian heterogeneity in benthic foraminiferal assemblages tracks regional impacts of paleoenvironmental change across Cretaceous OAE2. Paleobiology, 1-23. https://doi.org/10.1017/pab.2022.47
• Busson, G.; Dhondt, A.; Amédro, F.; Néraudeau, D. & Cornée, A. (1999). La grande transgression du Cénomanien supérieur-Turonien inférieur sur la Hamada de Tinrhert (Sahara algérien): Datations biostratigraphiques, environnements de dépôt et comparaison d'un témoin épicratonique avec les séries contemporaines à matière organique du Maghreb. Cretaceous Research, 20: 29-46. https://doi.org/10.1006/cres.1998.0137
• Caron, M.; Dall' Agnolo, S.; Accarie, H.; Barrera, E.; Kauffman, E.G.; Amédro, F. & Robaszynski, F. (2006). High-resolution stratigraphy of the Cenomanian-Turonian boundary interval at Pueblo (USA) and Wadi Bahloul (Tunisia): stable isotope and bio-events correlation. Geobios, 39: 171-200. https://doi.org/10.1016/j.geobios.2004.11.004
• Coiffait, P.E.; Coiffait, B.; Jaeger, J.J. & Mahboubi, M. (1984). Un nouveau gisement à mammifères fossiles d'âge Eocène supérieur sur le versant sud des Nementchas (Algérie orientale): découverte des plus anciens rongeurs d'Afrique. Comptes Rendus Academie Sciences Paris, 299: 893-898.
• Damotte, R. & Freytet, P. (1974). Contribution à la connaissance du Cénomanien du Massif de Fontfroide (Aude, France): Etude des Ostracodes. Revista Española de Micropaleontología, 2: 201-207.
• Damotte, R. & Saint-Marc, P. (1972). Contribution a la connaissance des ostracodes Crétacé du Liban. Revista Española de Micropaleontología, 4: 273-296.
• Delfaud, J. (1975). Les grès des Ksour: un delta de plate-forme stable. XIème Congrès International de Sédimontologie, Nice, 159-162.
• Delfaud, J. (1986). Organisation scalaire des événements sédimentaires majeurs autour de la Mésogée durant le Jurassique et le Crétacé. Conséquences pour les associations biologiques. Bulletin des centres de recherches exploration-Production Elf-Aquitaine, 10 (2): 509-535.
• Depêche, F. (1984). Les ostracodes d'une plate-forme continentale au Jurassique. Recherches sur le Bathonien du Bassin parisien. PhD Thesis, University Pierre et Marie Curie, Paris, 325 p.
• Elderbak, K.; Leckie, R.M. & Tibert, N.E. (2014). Paleoenvironmental and paleoceanographic changes across the Cenomanian-Turonian Boundary Event (Oceanic Anoxic Event 2) as indicated by foraminiferal assemblages from the eastern margin of the Cretaceous Western Interior Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 413: 29-48. https://doi.org/10.1016/j.palaeo.2014.07.002
• Elmi, S.; Alméras, Y.; Ameur, M.; Bassoullet, J.B.; Boutakiout, M.; Benhamou, M.; Marok, A.; Mekahli, L.; Mekkaoui, A. & Mouterde, R. (1998). Stratigraphic and palaeogeographic survey of the Lower and Middle Jurassic along a north-south transect in western Algeria. Mémoires Musée National Histoire Naturel Paris, 179: 145-211.
• El-Nady, H.; Abu-Zied, R. & Ayyad, S. (2008). Cenomanian Maastrichtian ostracods from Gabal Arif El-Naga anticline, Eastern Sinai, Egypt. Revue de Paléobiologie, 27: 533-573.
• El-Sabbagh, A.; Tantawy, A.A.; Keller, G.; Khozyem, H.; Spangenberg, J.; Adatte, T. & Gertsch, B. (2011). Stratigraphy of the Cenomanian-Turonian Oceanic Anoxic Event OAE2 in shallow shelf sequences of NE Egypt. Cretaceous Research, 32: 705-722. https://doi.org/10.1016/j.cretres.2011.04.006
• Erba, E. (2004). Calcareous nannofossils and Mesozoic oceanic anoxic events. Marine Micropaleontology, 52: 85-106. https://doi.org/10.1016/j.marmicro.2004.04.007
• Erba, E.; Bottini, C. & Faucher, G. (2013). Cretaceous large igneous provinces: the effects of submarine volcanism on calcareous nannoplankton. Mineralogical Magazine, 77: 1044.
• Erbacher, J. & Thurow, J. (1997). Influence of oceanic anoxic events on the evolution of mid Cretaceous radiolaria in the North Atlantic and western Tethys. Marine Micropaleontology, 30: 139-158. https://doi.org/10.1016/S0377-8398(96)00023-0
• Escarguel, G. (2001). BG-Index version 1.1β. Programme et notice d'utilisation. Laboratoire de Paléontologie, Université Claude Bernard.
• Ettachfini, M. (2006). La transgression au passage du Cénomanien au Turonien sur le domaine atlasique marocain. Stratigraphie intégrée et relation avec l'évenement océanique global. PhD Thesis, University Chouaïb Doukkali, 299 p.
• Ettachfini, M. & Andreu, B. (2004). Le Cénomanien et le Turonien de la Plate-forme Préafricaine du Maroc. Cretaceous Research, 25: 277-302. https://doi.org/10.1016/j.cretres.2004.01.001
• Ettachfini, M.; Souhel, A.; Andreu, B. & Caron, M. (2005). La limite Cénomanien -Tutronien dans le Haut Atlas central, Maroc. Geobios, 38: 57-68. https://doi.org/10.1016/j.geobios.2003.07.003 https://doi.org/10.1016/j.geobios.2003.07.003
• Farouk, S.; Jain, S.; Shabaan, M.; Ahmad, F.; Salhi, I.; Elamri, Z.; El-Kahtany, K.; Zaky, A.S. & Abu Sham, A. (2022). High resolution upper Cenomanian to Turonian paleoenvironmental changes: Inferences from calcareous nannofossils at the Oued Ettalla section (Central Tunisia). Marine Micropaleontology, 175: 102151. https://doi.org/10.1016/j.marmicro.2022.102151
• Friedrich, O.; Erbacher, J. & Mutterlose, J. (2006). Paleoenvironmental changes across the Cenomanian/Turonian Boundary Event (Oceanic Anoxic Event 2) as indicated by benthic foraminifera from the Demerara Rise (ODP Leg 207). Revue de Micropaléontologie, 49: 121-139. https://doi.org/10.1016/j.revmic.2006.04.003
• Galmier, D. (1972). Photogéologique de la région d'Aïn Séfra (Algérie). Bulletin Service Géologique Algérie, 42: 1-177.
• Gebhardt, H.; Friedrich, O.; Schenk, B.; Fox, L.; Hart, M. & Wagreich, M. (2010). Paleoceanographic changes at the northern Tethyan margin during the Cenomanian-Turonian Oceanic Anoxic Event (OAE-2). Marine Micropaleontology, 77: 25-45. https://doi.org/10.1016/j.marmicro.2010.07.002
• Gebhardt, H.; Kuhnt W. & Holbourn, A. (2004). Foraminiferal response to sea level change, organic flux and oxygen deficiency in the Cenomanian of the Tarfaya Basin, southern Morocco. Marine Micropaleontology, 53: 133-157. https://doi.org/10.1016/j.marmicro.2004.05.007
• Gertsch, B.; Keller, G.; Adatte, T.; Berner, Z.; Kassab, A.S.; Tantawy, A.A.A.; El-Sabbagh, A.M. & Stueben, D. (2010). Cenomanian-Turonian transition in a shallow water sequence of the Sinai, Egypt. International Journal of Earth Sciences, 99: 165-182. https://doi.org/10.1007/s00531-008-0374-4
• Glintzboeckel, C. & Magné, J. (1959). Répartition des microfaunes à plancton et à Ostracodes dans le Crétacé supérieur de la Tunisie et de l'Est algérien. Revue de Micropaléontologie, 5: 53-59.
• Grekoff, M. (1969). Sur la valeur stratigraphique et les relations paléogéographiques des quelques ostracodes du Crétacé, du Paléocène et de l'Eocène inférieur d'Algérie orientale. Proceedings of the 3rd African Micropaleontological Coloquium, Cairo, 227-248.
• Grosdidier, E. (1973). Association d'Ostracodes du Crétacé d'Iran. Revue Institute Français du Pétrole, 28 (2): 131-169.
• Grosheny, D.; Chikhi-Aouimeur, F.; Ferry, S.; Benkherouf-Kechid, F.; Jati, M.; Atrops, F. & Redjimi-Bourouiba, W. (2008). The Upper Cenomanian-Turonian (Upper Cretaceous) of the Saharan Atlas (Algeria). Bulletin Société Géologique France, 179: 593-603. https://doi.org/10.2113/gssgfbull.179.6.593
• Grosheny, D.; Ferry, S.; Jati, M.; Ouaja, M.; Bensalah, M.; Atrops, F.; Chikhi-Aouimeur, F.; Benkherouf-Kechid, F.; Negra, H. & Aït Salem, H. (2013). The Cenomanian-Turonian boundary on the Saharan Platform (Tunisia and Algeria). Cretaceous Research, 42: 66-84. https://doi.org/10.1016/j.cretres.2013.01.004
• Guillemot, J. & Estorges, P. (1981). Notice de la carte de Brézina au 1/200000. Direction de la Géologie, Direction des Mines et de la Géologie, Ministère de l'Industrie Lourde, Algérie, 45 p.
• Guiraud, R. (1990). Evolution post-triasique de l'avant-pays de la chaîne alpine en Algérie d'après l'étude du bassin du Hodna et des régions voisines. Geological Survey of Algeria, Office National de la Geologie, 259 p.
• Hallam, A. (1992). Phanerozoic sea level changes. Columbia Press, New York, 266 p.
• Hammer, Ø., Harper, D. A. T., & Ryan, P. D. (2001). PAST-palaeontological statistics, ver. 1.89. Palaeontologia Electronica, 4 (1): 1-9.
• Hardas, P. & Mutterlose, J. (2007). Calcareous nannofossil assemblages of Oceanic Anoxic Event 2 in the equatorial Atlantic: Evidence of a eutrophication event. Marine Micropaleontology, 66: 52-69. https://doi.org/10.1016/j.marmicro.2007.07.007
• Harket, M. & Delfaud, J. (2000). Genèse des séquences sédimentaires du Crétacé supérieur des Aurès (Algérie). Rôle de l'eustatisme, de la tectonique, de la subsidence : une mise au point. Comptes Rendus Academie Sciences de Paris, 330: 785-792. https://doi.org/10.1016/S1251-8050(00)00229-9
• Hataba, H. & Ammar, G. (1990). Comparative stratigraphic study on the Upper Cenomanian - Lower Senonian sediments between the Gulf of Suez and Western Desrt, Egypt. EGPC 10th Exploration-Production Conference, 1-16.
• Hewaidy, A.A. & Morsi, A.M. (2001). Lower Cretaceous (Aptian-Albian) Foraminifera and Ostracoda from northern Sinai, Egypt. Egyptian Journal of Paleontology, 1: 229-252.
• Horne, D.J.; Cohen, A. & Martens, K. (2002). Taxonomy, morphology and biology of Quaternary and living Ostracoda. In: Holmes, J.A., Chivas, A.R. (Eds.), The Ostracoda: Applications in Quaternary Research. AGU Geophysical Monograph Series, 131: 5-36. https://doi.org/10.1029/131GM02
• Horne, D.J.; Brandao, S.N. & Slipper, I.J. (2011). The Platycopid signal deciphered: responses of ostracod taxa to environmental change during the Cenomanian-Turonian boundary event (Late cretaceous) in SE England. Palaeogeography, Palaeoclimatology, Palaeoecology, 308: 304-312. https://doi.org/10.1016/j.palaeo.2011.05.034
• Huber, B.T.; Norris, R.D. & McLeod, K.G. (2002). Deep-sea paleotemperature record of extreme warmth during the Cretaceous. Geology, 30: 123-126. https://doi.org/10.1130/0091-7613(2002)030<0123:DSPROE>2.0.CO;2
• Ismail, A.A. (1999). Aptian-Turonian ostracods from Northern Sinai, Egypt. Egyptian Journal of Geology, 43: 293-315.
• Ismail, A.A. (2001). Correlation of cenomanian-Turonian ostracods of Gebel Shabraweet with their counterpart in Egypt, Nort Africa and the Middle East. Neues Jahrbush Geologische Paläontologische Monatshefte, 9: 513-533. https://doi.org/10.1127/njgpm/2001/2001/513
• Ismail, A.A.; Hussein-Kamel, Y.F.; Boukhary, M. & Ghandour, A.A. (2009). Late Cenomanian-Early Turonian foraminifera from Eastern Desert, Egypt. Micropaleontology, 55: 396-412. https://doi.org/10.47894/mpal.55.4.05
• Jarvis, I.; Carson, G.A.; Cooper, M.K.E.; Hart, M.B.; Leary, P.N.; Tocher, B.A.; Horne, D. & Rosenfeld, A. (1988). Microfossil assemblages and the Cenomanian-Turonian (late Cretaceous) oceanic anoxic event. Cretaceous Research, 9: 3-103. https://doi.org/10.1016/0195-6671(88)90003-1
• Jati, M.; Grosheny, D.; Ferry, S.; Masrour, M.; Aoutem, M.; Içame, N.; Gauthier-Lafaye, F. & Desmares, D. (2010). The Cenomanian-Turonian boundary event onthe Moroccan Atlantic margin (Agadir basin): Stable isotope and sequence stratigraphy. Palaeogeography, Palaeoclimatology, Palaeoecology, 296: 151-164. https://doi.org/10.1016/j.palaeo.2010.07.002
• Jenkyns, H.C. (1980). Cretaceous anoxic events: from continents to oceans. Journal Geological Society London, 137: 171-188. https://doi.org/10.1144/gsjgs.137.2.0171
• Jenkyns, H.C. (1997). Mesozoic anoxic events and paleoclimate. Zentralblatt für Geologie und Paläontologie, 1: 943-949.
• Jolet, P.; Philip, J.; Cecca, F.; Thomel, G.; López, G.; Tronchetti, G. & Babinot, J.F. (2001). Integrated platform/basin biostratigraphy of the Upper Cenomanian-Lower Turonian in Provence (SE France). Geobios, 34: 225-238. https://doi.org/10.1016/S0016-6995(01)80063-2
• Kaiho, K. & Hasegawa, T. (1994). End-Cenomanian benthic foraminiferal extinctions and oceanic dysoxic events in the northwestern Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 111: 29-43. https://doi.org/10.1016/0031-0182(94)90346-8
• Kazi-Tani, N. (1986). Evolution géodynamique de la bordure nord-africaine: le domaine intraplaque nord-algérien. Approche mégaséquentielle. PhD Thesis, University of Pau, 871 p.
• Khalil, M.M. (2020). Biostratigraphy and paleobiogeographic implications of the Cenomanian-Early Turonian ostracods of Egypt. Annales de Paléontologie, 106: 102408. https://doi.org/10.1016/j.annpal.2020.102408
• Kostak, M.; Cech, S.; Ulicny, D.; Sklenar, J.; Ekrt, B. & Mazuch, M. (2018). Ammonites, inoceramids and stable carbon isotopes of the Cenomanian-Turonian OAE2 interval in central Europe: Pecinov quarry, Bohemian Cretaceous Basin (Czech Republic). Cretaceous Research, 87: 150-173. https://doi.org/10.1016/j.cretres.2017.04.013
• Kuroda, J.; Ogawa, N.O.; Tanimizu, M.; Coffin, M.T.; Tokuyama, H.; Kitazato, H. & Ohkouchi, N. (2007). Contemporaneous massive subaerial volcanism and late Cretaceous Oceanic Anoxic Event 2. Earth Planetary Science Letters, 256: 211-223. https://doi.org/10.1016/j.epsl.2007.01.027
• Kuypers, M.M.M.; Pancost, R.D.; Nijenhuis, I.A. & Sinninghe-Damste, J.S. (2002). Enhanced productivity led to increased organic carbon burial in the euxinic North Atlantic Basin during the late Cenomanian oceanic anoxic event. Paleoceanography, 17: 1051. https://doi.org/10.1029/2000PA000569
• Lézin, C.; Andreu, B.; Ettachfini, M.; Walleez, M.-J.; Lebedel, V. & Meister, C. (2012). The upper Cenomanian-lower Turonian of the Preafrican Trough, Morocco. Sedimentary Geology, 245-246: 1-16. https://doi.org/10.1016/j.sedgeo.2011.12.003
• Lüning, S.; Marzouk, A.M.; Morsi, A.M. & Kuss, J. (1998). Sequence stratigraphy of the Upper Cretaceous of central-east Sinai, Egypt. Cretaceous Research, 19: 153-196. https://doi.org/10.1006/cres.1997.0104
• Majoran, S. (1989). Mid-Cretaceous Ostracoda of northeastern Algeria. Fossils Strata, 27: 1-67.
• Marok, A.; Sebane, A. & Bensalah, M. (2009). Les événements anoxiques du Mésozoïque dans quelques bassins nord algériens: Résultats préliminaires. Conférences sur l'Exploration dans le Nord de l'Algérie: Perspectives et Défis, Alger, 27-28.
• Mebarki, K.; Sauvagnat, J.; Benyoucef, M.; Zaoui, D.; Benachour, H-B.; Mohammed, A.; Mahboubi, M. & Bensalah, M. (2016). Cenomanian-Turonian ostracodes fron the Western Saharan Atlas and the Guir Basin (SE Algeria): systematic, biostratigraphy and paleobiogeography. Revue de Paleobiologie, 35: 249-277.
• Mekahli, L. (1998). Evolution des Monts des Ksour (Algérie) de l'Héttangien au Bajocien. Biostratigraphie, sédimentologie, paléogéographie et stratigraphie séquentielle. Documents Laboratoire Géologie Lyon, 147: 319 p.
• Momani, M.M. (2021). Petrographical and Geochemical Analyses of the Cenomanian-Turonian Oil Shale Successions in Ajloun, Northern of Jordan. PhD Thesis, University of Yarmouk, 79 p.
• Monnet, C. (2009). The Cenomanian-Turonian boundary mass extinction (Late Cretaceous): New insights from ammonoid biodiversity patterns of Europe, Tunisia and the Western Interior (North America). Palaeogeography, Palaeoclimatology, Palaeoecology, 282: 88-104. https://doi.org/10.1016/j.palaeo.2009.08.014
• Monteiro, F.M.; Pancost, R.D.; Ridwell, A. & Donnadieu, Y. (2012). Nutrients as the dominant control on the spread of anoxia and euxinia across the Cenomanian-Turonian oceanic anoxic event (OAE2): model-data comparison. Paleoceanography, 27 (4): PA4209. https://doi.org/10.1029/2012PA002351
• Morsi, A.M. & Bauer, J. (2001). Cenomanian ostracods from Sinai Peninsula, Egypt. Revue de Paléobiologie, 20: 377-414.
• Morsi, A.M. & Wendler, J.E. (2010). Biostratigraphy, palaeoecology and palaeogeography of the Middle Cenomanian-Early Turonian Levant Platform in Central Jordan based on ostracods. Geological Society Special Publication, 341: 187-201. https://doi.org/10.1144/SP341.9
• Nagm, E. (2009). Integrated stratigraphy, palaeontology and facies analysis of the Cenomanian-Turonian (Upper Cretaceous) Galala and Maghra El Hadida Formations of the Western Wadi Araba, Eastern Desert, Egypt. PhD Thesis, University of Würzburg, 213 p. https://doi.org/10.1127/0078-0421/2010/0002
• Nagm, E.; Wilmsen, M.; Aly, M.F. & Hewaidy, A. (2010). Upper Cenomanian-Turonian (Upper Cretaceous) ammonoids from the western Wadi Araba, Eastern Desert, Egypt. Cretaceous Research, 31: 473-499. https://doi.org/10.1016/j.cretres.2010.05.008
• Nagm, E.; Farouk, S. & Ahmed, F. (2017). The Cenomanian-Turonian boundary in Jordan: Ammonite biostratigraphy and faunal turnover. Geobios, 50: 37-47. https://doi.org/10.1016/j.geobios.2016.11.002
• Nagm, E.; Jain, S.; Mahfouz, K.; El Sabbagh, A. & Abu Shama, A. (2021). Biotic response to the latest Cenomanian drowning and OAE2: A case study from the Eastern Desert of Egypt. Proceedings Geologists' Association, 132: 70-92. https://doi.org/10.1016/j.pgeola.2020.10.001
• Naili, H.; Belhadj, Z.; Robaszynski, F. & Caron, M. (1995). Présence de roches mère à faciès Bahloul vers la limite Cénomanien-Turonien dans la région de Tébessa (Algérie orientale). Notes du Service Géologique Tunisie, 61: 19-32.
• Negra, M.H.; Zagrarni, M.F.; Hanini, A. & Strasser, A. (2011). The filament event near the Cenomanian-Turonian boundary in Tunisia: filament origin and environmental signification. Bulletin de la Société Géologique de France, 182: 507-519. https://doi.org/10.2113/gssgfbull.182.6.507
• Neufville, E.M.H. (1973). Ostracoda from the Ezu-Akshale (Turonian, Cretaceous), Nkalagu, Nigeria. Bulletin of the Geological Institution of the University of Uppsala, 4: 44-51.
• Norris, R.D.; Bice, K.L.; Magno, E.A. & Wilson, P.A. (2002). Jiggling the tropical thermostat in the Cretaceous hothouse. Geology, 30: 299-302. https://doi.org/10.1130/0091-7613(2002)030<0299:JTTTIT>2.0.CO;2
• N'Zaba-Makaya, O.; Andreu, B.; Brunel, F.; Mouterde, R.; Rey, J. & Rocha, R.B. (2003). Biostratigraphie et paléoécologie des peuplements d'ostracodes dans le Domérien du Bassin Lusitanien, Portugal. Ciências da Terra, 15: 21-44.
• Piovesan, E.K.; Cabral, M.C.; Colin, J.-P.; Fauth, G. & Bergue, C.T. (2014). Ostracodes from the Upper Cretaceous deposits of the Potiguar Basin, Northeastern Brazil: taxonomy, paleoecology and paleobiogeography, part 1: Turonian. Carnets de Géologie, 14: 211-252. https://doi.org/10.4267/2042/54003
• Pogge von Strandmann, P.A.E.; Jenkyns, H.C. & Woodfine, R.G. (2013). Lithium isotope evidence for enhanced weathering during Oceanic Anoxic Event 2. Nature Geosciences, 6: 668-672. https://doi.org/10.1038/ngeo1875
• Posenato, R.; Frijia, G.; Morsilli, M.; Moro, A.; Del Viscio, G. & Mezfa, A. (2020). Paleoecology and proliferation of the bivalve Chondrodonta joannae (Choffat) in the upper Cenomanian (Upper Cretaceous) Adriatic Carbonate Platform of Istria (Croatia). Palaeogeography, Palaeoclimatology, Palaeoecology, 548: 109703. https://doi.org/10.1016/j.palaeo.2020.109703
• Prauss, M.L. (2012). The Cenomanian/Turonian Boundary Event (CTBE) at Tarfaya, Morocco, northwest Africa: Eccentricity controlled water column stratification as major factor for total organic carbon (TOC) accumulation: Evidence from marine palynology. Cretaceous Research, 37: 246-260. https://doi.org/10.1016/j.cretres.2012.04.007
• Reolid, M. (2020). Microfossil assemblages and geochemistry for interpreting the incidence of the Jenkyns Event (early Toarcian) in the south-eastern Iberian palaeomargin (External Subbetic, SE Spain). Journal of Micropalaeontology, 39: 233-258. https://doi.org/10.5194/jm-39-233-2020
• Reolid, M. & Ainsworth, N.R. (2022). Changes in benthic microfossil assemblages before, during and after the eary Toarcian biotic crisis in the Portland-Wight Basin (Kerr McGee 97/12-1 well, offshore southern England). Palaeogeography, Palaeoclimatology, Palaeoecology, 599: 111044. https://doi.org/10.1016/j.palaeo.2022.111044
• Reolid, M.; Rodríguez-Tovar, F.J.; Marok, A. & Sebane, A. (2012). The Toarcian Oceanic Anoxic Event in the Western Saharan Atlas, Algeria (North African Paleomargin): role of anoxia and productivity. Geological Society of America Bulletin, 124: 1646-1664. https://doi.org/10.1130/B30585.1
• Reolid, M.; Sánchez-Quiñónez, C.A.; Alegret, L. & Molina, E. (2015). Palaeoenvironmental turnover across the Cenomanian-Turonian transition in Oued Bahloul, Tunisia: foraminifera and geochemical proxies. Palaeogeography, Palaeoclimatology, Palaeoecology, 417: 491-510. https://doi.org/10.1016/j.palaeo.2014.10.011
• Reolid, M.; Sánchez-Quiñónez, C.A.; Alegret, L. & Molina, E. (2016). The biotic crisis across the Oceanic Anoxic Event 2: Palaeoenvironmental inferences based on foraminifera and geochemical proxies from the South Iberian Palaeomargin. Cretaceous Research, 60: 1-27. https://doi.org/10.1016/j.cretres.2015.10.011
• Rerbal, L. (2008). Le Crétacé supérieur du Djebel El Kohol (Atlas saharien, Algérie). MsC Thesis, University of Tlemcen, 59 p.
• Robaszynski, F. (1989). L'événement à l'échelle globale pendant la partie moyenne du Crétacé. Geobios Mémoire Spécial, 11: 311-319. https://doi.org/10.1016/S0016-6995(89)80067-1
• Robaszynski, F. & Caron, M. (1995). Foraminifères planctoniquesdu Crétacé: Commentaire de la zonation Europe-Méditerranée. Bulletin de la Société Géologique France, 166: 681-692.
• Robaszynski, F.; Zagrararni, M.F.; Caron, M. & Amedro, F. (2010). The global bio-event at the Cenomanian-Turonien transition in the reduced Bahloul Formation of Bou Ghanem (central Tunisia). Cretaceous Research, 31: 1-15. https://doi.org/10.1016/j.cretres.2009.07.002
• Ruault-Djerrab, M.; Ferré, B.; Kechid-Benkherouf, F. & Djerrab, A. (2012). Etude micropaléontologique du Cénomano-Turonien dans la région de Tébessa (NE Algérie): implications paléoenvironnementales et recherche de l'empreinte de l'OAE2. Revue Paléobiologie, 31: 127-144.
• Ruault-Djerrab, M.; Kechid-Benkherouf, F. & Djerrab, A. (2014). Données paléoenvironnementales sur le Vraconnien/Cénomanien de la région de Tébessa (Atlas Saharien, nord-est Algérie). Caractérisation de l'OAE2. Annales de Paléontologie, 100: 343-359. https://doi.org/10.1016/j.annpal.2014.03.002
• Salmouna, D.J.; Chaabani, F.; Dhahri, F.; Mzoughi, M.; Salmouna, A. & Zijlstra, H.B. (2014). Lithostratigraphic analysis of the Turonien-Coniacian Bireno and Douleb carbonate Members in Jebels Berda and Chemsi, Gafsa basin, central-southern Atlas of Tunisia. Journal of African Earth Sciences, 100: 733-754. https://doi.org/10.1016/j.jafrearsci.2014.07.025
• Schlanger, S.O.; Arthur, M.A.; Jenkyns, H.C. & Scholle, P.A. (1987). The Cenomanian- Turonian oceanic anoxic event, I. Stratigraphy and distribution of organic-rich beds and the marine δ13C excursion. Geologival Society Special Publication, 26: 371-399. https://doi.org/10.1144/GSL.SP.1987.026.01.24
• Schulze, F.; Marzouk, A.M.; Bassiouni, M.A.A. & Kuss, J. (2004). The late Albian-Turonian carbonate platform succession of west-central Jordan: stratigraphy and crisis. Cretaceous Research, 25: 709-737. https://doi.org/10.1016/j.cretres.2004.06.008
• Shahin, A. (1991). Cenomanian-Turonian ostracods from Gebel Nezzazat, southwestern Sinai, Egypt, with observations on δ13C values and the Cenomanian/Turonian boundary. Journal of Micropalaeontology, 10: 133-155. https://doi.org/10.1144/jm.10.2.133
• Shahin, A. & Elbaz, S. (2013a). Cenomanian-Early Turonian of the shallow marine carbonate platform sequence at west central Sinai: Biostratigraphy, paleobathymetry and paleobiogeography. Revue de Micropaléontologie, 56: 103-126. https://doi.org/10.1016/j.revmic.2013.04.004
• Shahin, A. & Elbaz, S.M. (2013b). Cenomanian-Early Turonian Ostracoda of the shallow marine carbonate platform sequence at west central Sinai: Biostratigraphy, paleobathymetry and paleobiogeography. Revue de Micropaléontologie 56: 103-126. https://doi.org/10.1016/j.revmic.2013.04.004
• Shahin, A. & Elbaz, S. (2021). Early-Middle Cenomanian foraminifera and ostracods from BB-80-1 well, Gulf of Suez, Egypt: Biostratigraphy, palaeoecology, and palaeobiogeographic significance. Geological Journal, 56: 3745-3770. https://doi.org/10.1002/gj.4131
• Shahin, A.; Kora, M. & Semiet, A. (1994). Cenomanian ostracods from West Central Sinai, Egypt. Mansoura University Science Bulletin, 21: 33-102.
• Slami, R.; Ferré, B. & Benkherouf-Kechid, F. (2022). Cenomanian ostracods (Crustacea) of Djebel Sabaoune (Batna, Algeria): Specific assemblage and significance. Journal of African Earth Sciences, 193: 104604. https://doi.org/10.1016/j.jafrearsci.2022.104604
• Takahashi, A. (2005). Responses of inoceramid bivalves to environmental disturbances across the Cenomanian/Turonian boundary in the Yezo forearc basin, Hokkaido, Japan. Cretaceous Research, 26: 567-580. https://doi.org/10.1016/j.cretres.2005.02.006
• Tchenar, S.; Ferré, B.; Adaci, M.; Zaoui, D.; Benyoucef, M.; Bensalah, M. & Kentri, T. (2020). Incidences de l'Évènement Anoxique Océanique II sur l'évolution des ostracodes des dépôts cénomano-turoniens du bassin du Tinrhert (SE Algérie). Carnets de Géologie, 20 (08): 145. https://doi.org/10.4267/2042/70792
• Touir, J.; Mechi, C. & Ali, H.H. (2017). Changes in carbonate sedimentation and faunal assemblages in the Tunisian carbonate platform around the Cenomanian-Turonian boundary. Journal of African Earth Sciences, 129: 527-541. https://doi.org/10.1016/j.jafrearsci.2017.01.025
• Turgeon, S.C. & Creaser, R.A. (2008). Cretaceous oceanic anoxic event 2 triggered by a massive magmatic episode. Nature, 454: 323-326. https://doi.org/10.1038/nature07076 PMid:18633415
• Vivière, J.L. (1985). Les ostracodes du Crétacé supérieur (Vraconien à Campanien basal) de la région de Tébessa (Algérie du Nord-Est. Stratigraphie, Paléoécologie, Systématique). Mémoire Science de la Terre, University Marie Curie, Paris 85, 261.
• Viviers, M.C.; Koutsoukos, E.A.M.; Da Silva-Telles, A.C. & Bengtson, P. (2000). Stratigraphy and biogeographic affinities of the late Aptian-Campanian ostracods of the Potiguar and Sergipe basins in northeastern Brazil. Cretaceous Research, 21: 407-455. https://doi.org/10.1006/cres.2000.0205
• Voigt, S.; Erbacher, J.; Mutterlose, J.; Weiss, W.; Westerhold, T.; Wiese, F.; Wilmsen, M. & Wonik, T. (2008). The Cenomanian-Turonian of the Wunstorf section (North Germany): global stratigraphic reference section and new orbital time scale for Oceanic Anoxic Event 2. Newsletters on Stratigraphy, 43: 65-89. https://doi.org/10.1127/0078-0421/2008/0043-0065
• Wan, X., Wignall, P.B. & Zhao, W. (2003). The Cenomanian-Turonian extinction and oceanic anoxic event: evidence from southern Tibet. Palaeogeography, Palaeoclimatology, Palaeoecology, 199: 283-298. https://doi.org/10.1016/S0031-0182(03)00543-1
• Wang, J.P.; Bulot, L.G.; Taylor, K.G. & Redfern, J. (2021). Controls and timing of Cenomanian-Turonian organic enrichment and relationship to the OAE2 event in Morocco, North Africa. Marine and Petroleum Geology, 128, art. 105013. https://doi.org/10.1016/j.marpetgeo.2021.105013
• Wendler, J.E.; Lehmann, J. & Kuss, J. (2010). Orbital time scale, intra-platform basin correlation, carbon isotope stratigraphy and sea-level history of the Cenomanian-Turonian Eastern Levant platform, Jordan. Geological Society Special Publication, 341: 171-186. https://doi.org/10.1144/SP341.8
• Whatley, R.C. (1991). The platycopid signal: a means of detecting kenoxic events using Ostracoda. Journal of Micropalaeontology, 10: 181-183. https://doi.org/10.1144/jm.10.2.181 https://doi.org/10.1144/jm.10.2.181
• Whatley, R.C. (1995). Ostracoda and oceanic palaeoxygen levels. Mitteilungen aus dem Hamburgischen Zoologischen Museum und Institut, 92: 337-353.
• Wilmsen, M. & Nagm, E. (2013). Sequence stratigraphy of the lower Upper Cretaceous (Upper Cenomanian-Turonian) of the Eastern Desert, Egypt. Newsletters on Stratigraphy, 46: 23-46. https://doi.org/10.1127/0078-0421/2013/0030
• Yelles-Chaouche, A.K.; Aït Ouali, R.; Bracene, R.; Derder, M.E.M. & Djellit, H. (2001). Chronologie de l'ouverture du bassin des Ksour (Atlas Saharien, Algérie) au début du Mésozoïque. Bulletin Société Géologique France, 3: 285-293. https://doi.org/10.2113/172.3.285
• Zaghbib-Turki, D. & Soua., M. (2013). High resolution biostratigraphy of the Cenomanian-Turonian interval (OAE2) based on planktonic foraminiferal bioevents in North-Central Tunisia. Journal of African Earth Sciences, 78: 97-108. https://doi.org/10.1016/j.jafrearsci.2012.09.014
• Zagrarni, M.F.; Negra, M.H. & Amine Hanini, A. (2008). Cenomanian-Turonian facies and sequence stratigraphy, Bahloul Formation, Tunisia. Sedimentary Geology, 204: 18-35. https://doi.org/10.1016/j.sedgeo.2007.12.007
• Zakhera, M.S. & Kassab, A.S. (2002). Integrated macrobiostratigraphy of the Cenomanian-Turonian transition, Wadi El-Siq, west central Sinai, Egypt. Egyptian Journal of Paleontology, 2: 219-233.
• Zazoun, R.S.; Marok, A.; Samar, L.; Benadla, M. & Mezlah, H. (2015). La fracturation et les bandes de déformation dans la région d'El Kohol (Atlas Saharien Central, Algérie): analyse fractale, lois d'échelles et modèle de réseaux de fractures discrètes. Estudios Geologicos, 71: 1-23. https://doi.org/10.3989/egeol.42011.359