Integrated biostratigraphy of two Upper Maastrichtian – Palaeocene successions in north-central Sinai, Egypt

Main Article Content

Mahmoud Faris
Sherif Farouk

Abstract

Integration of the calcareous nannofossil and planktonic foraminiferal biostratigraphies has been performed for theUpper Maastrichtian – Palaeocene successions at Gebel Umm Khushayb and west El-Hassana sections (north-centralSinai, Egypt). The studied successions include the uppermost part of the Sudr, Dakhla, and their lateral coeval Beida Formation. Biostratigraphic analysis has allowed recognition from Zone CF2 to Zone P4in terms of planktonic foraminifera and from Zone CC26c to Zone NP7/8 in terms of calcareous nannofossils. Maastrichtian/Palaeogene (K/Pg) boundary is characterized by an erosional surface that marks a hiatus between theSudr/Dakhla or Sudr/Beida formation boundaries, as confi rmed by the absence of the planktonic foraminiferal CF1to P1a zones and their equivalent nannofossil zones (top part of CC26c to lowest part of Zone NP3). Selandian (Da/Se) boundary lies in the upper part of the Dakhla Formation within the top of nannofossil Zone NP4,and within planktonic foraminiferal Zone P3b, similar to that of the Global Standard Stratotype-section and Point(GSSP) of the D/S boundary which has recently been chosen at the Zumaia section, northern Spain. was observed across the Selandian/Thanetian boundary as indicated by a lithological change and a very condensedZone NP6, corresponding to the Dakhla and Tarawan formation boundary in the west El-Hassana section.

 

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Original Scientific Papers
Author Biographies

Mahmoud Faris, Geology Department, Faculty of Science, Tanta University, Egypt,

Geology Department,

Sherif Farouk, Egyptian Petroleum Research Institute

Exploration Department

References

ALLAM, A. & KHALIL, H. (1988): Geology and stratigraphy of the Arif El-Naqa area, Sinai, Egypt.– Egypt. J. Geol., 32, 199–218.

ALVAREZ, L.W., ALVAREZ, W., ASARO, F. & MICHEL, H.V. (1980): Extraterrestrial cause for the Cretaceous-Tertiary extinc-tion: experimental results and theoretical interpretation.– Science, 208, 1095–1108.

ALVAREZ, L.W., ALVAREZ, W., ASARO, F. & MICHEL, H.V. (1984): The end of the Cretaceous: sharp boundary or gradual transition.– Science, 223, 1183–1186. doi:10.1126/science.223.4641.1183

AL-WOSABI, K. & ABU SHAMA, A.Z. (2007): Planktonic foraminif-eral and calcareous nannofossil biostratigraphy around the K/P boundary at section, west central Sinai, Egypt.– Egypt. J. Paleont., 7, 87–115.

ARENILLAS, I. (2011): Patterns of spatio-temporal distribution as cri-teria for the separation of planktic foraminiferal species across the Danian-Selandian transition in Spain.– Acta Palaeont. Polon., 57/2, 401–402. doi: http://dx.doi.org/10.4202/app.2010.0076

AUBRY, M.-P. (1994): The Thanetian Stage in NW Europe and its sig-nifi cance in terms of global events.– GFF, 116, 43–44.

AWAD, G.H. & GHOBRIAL, M.G. (1966): Zonal stratigraphy of the Kharga Oasis.– Geological Survey of Egypt, Cairo, Paper, 34, 77 p.

AYYAD, S.N., FARIS, M., EL NAHASS, H.A. & SAAD, K.A.A. (2003): Planktonic foraminiferal and calcareous nannofossil bio-stratigraphy from the Upper Cretaceous-Lower Eocene successions in northeast Sinai, Egypt.– In: 3rd International Conference on the Geology of Africa, Assiut University, 1, 649–683.

BACKMAN, J. (1986): Late Palaeocene to middle Eocene calcareous nannofossil biochronologyfrom the Shatsky Rise, Walvis Ridge and Italy.– Palaeog., Palaeocl., Palaeoec., 57, 43–59.

BASSIOUNI, M.A., FARIS, M. & SHARABY, S. (1991): Late Maas-trichtian and Palaeocene calcareous nannofossils from Ain Dabadib section, NW Kharga Oasis, Egypt.– Qatar Univ. Sci. J., 11, 357–375.

BERGGREN, W.A., AUBRY, M.-P., VAN FOSSEN, M., KENT, D.V., NORRIS, R.D. & QUILLEVERE, F. (2000): Integrated Palaeocene calcareous plankton magnetobiochronology and stable isotope stra-tigraphy: DSDP Site 384 (NW Atlantic Ocean).– Palaeog., Palaeo-cl., Palaeoec., 159, 1–51. doi:10.1016/S0031-0182(00)00031-6

BERGGREN, W.A., KENT, D.V., SWISHER, C.C.I. & AUBRY, M.-P. (1995): A revised Cenozoic geochronology and chronostratig-raphy.– In: HARDENBOL, J. (ed.): Geochronology, time scales and global stratigraphic correlation, Society of Economic Paleontolo-gists and Mineralogists, Special Publication, 54, 129–212.

BERGGREN, W.A. & NORRIS, R.D. (1997): Biostratigraphy, phylog-eny, and systematics of Palaeocene planktic foraminifera.– Micro-paleontolgy, 43 (Supplement 1), 1–116. doi:10.2307/1485988

BERGGREN, W.A. & PEARSON, P.N. (2005): A revised tropical to sub tropical Palaeogene planktonic foraminiferal zonation.– J. Fo-ram. Res., 35, 279–314. doi:10.2113/35.4.279

BERNAOLA, G., MARTIN-RUBIO, M. & BACETA, J.I. (2009): New high resolution calcareous nannofossil analysis across the Danian-Selandian transition at the Zumaia section: comparisons with South Tethys and Danish sections.– Geol. Acta, 7, 79–92.

BERNAOLA, G. & MONECHI, S. (2007): Calcareous nannofossil ex-tinction and survivorship across the Cretaceous−Palaeogene bound-ary at Walvis Ridge (ODP Hole 1262C, South Atlantic Ocean).– Palaeog., Palaeocl., Palaeoec., 255, 132–156.

BOLLE, M.-P. & ADATTE, T. (2001): Palaecoene-early Eocene climat-ic evolution in the Tethyan realm: clay mineral evidence.– Clay Min., 36, 249–261.

CLEMEN, W.A., ARCHIVALD, J.D. & HICKEY, L.J. (1981): Out with a whimper not a bang.– Paleobiology, 7, 293–298.

COURTILLOT, V., FERAUD, G., MALUSKI, H., VANDAMME, D., MOREAU, M.G. & BESSE, J. (1988): Deccan fl ood basalts and the Cretaceous/Tertiary boundary.– Nature, 333, 843–846. doi: 10.1038/333843a0

DINARES-TURELL, J., BACETA, J.I., BERNAOLA, G., ORUE-ETXEBARRIA, X. & PUJALTE, V. (2007): Closing the Mid-Pal-aeocene gap: Toward a complete astronomically tuned Palaeocene Epoch and Selandian and Thanetian GSSPs at Zumaia (Basque Ba-sin, W Pyrenees).– Earth Plan. Sci. Lett., 262, 450–467. doi:10.1016/ j.epsl.2007.08.008

EL-DEEB, W.Z., FARIS, M. & MANDOUR, M.M. (2000): Foraminif-eral and calcareous nannofossil biostratigraphy of the Palaeocene in North Central Sinai, Egypt.– Annals of the Geological Survey of Egypt, 23, 103–118.

EL-NADY, H. & SHAHIN, A. (2001): Planktonic foraminiferal biosta-tigraphy and palaeobathymetry of the Late Cretaceous-Early Ter-tia ry succession at northeast Sinai, Egypt.– Egypt. J. Paleont., 1, 193–227.

FARIS, M., ABD EL-HAMEED, A.T., MARZOUK, A. & GHANDOUR, I.M. (1999): Early Palaeogene calcareous nannofossil and plank-tonic foraminiferal biostratigraphy in Central Egypt.– N. Jahrb. Ge-ol. Paläont. Abhandl., 213/2, 261–288.

FARIS, M. & ABU SHAMA, A.M. (2007): Nannofossil biostratigraphy of the Palaeocene –Eocene succession in the Thamad area, East Central Sinai, Egypt.– Micropaleont., 1–2, 127–144. doi: 10.2113/gsmicropal.53.1-2.127

FARIS, M., AYYAD, S.N., EL NAHASS, H.A., & AL WOSABI, KH.A. (2005): Early Palaeogene stages and their boundaries in Sinai, Egypt.– In: The fourth International Conference on the Geology of Africa, Assiut University, Egypt, 2, 753–768.

FARIS, M., EL-DEEB, W. & MANDOUR, M. (2000): Biostratigraphy of some Upper Cretaceous/Lower Eocene successions in North and Southwest Sinai, Egypt.– Annals of the Geological Survey of Egypt, 23, 135–161.

FARIS, M. & SALEM, R.F. (2007): Palaeocene-Early Eocene calcare-ous nannofossil biostratigraphy in West Central Sinai, Egypt.– In: Proceedings of the 8th Conference Geology of Sinai for Development, Ismailia, 1–14.

FARIS, M. & ZAHRAN, E. (2002): Calcareous nannofossil biostratig-raphy of the Late Palaeocene/Early Eocene of El-Bruk area, North Central Sinai.– Egypt. J. Paleont., 2, 359–369.

FAROUK, S. & FARIS, M. (2008): Campanian to Eocene planktic fo-raminiferal and calcareous nannofossil biostratigraphy in the syn-clinal areas around Gebel Libni, North Sinai, Egypt.– Earth Sci. Ser., 22, 187–201.

GARDAN, S. (2002): Late Maastrichtian to early Danian calcareous nannofossils at Elles, Northwest Tunisia: A tale of one million years across the K-T boundary.– Palaeog., Palaeocl., Palaeoec., 178, 211–231. doi:10.1016/S0031-0182(01)00397-2

GHORAB, M.A. (1961): Abnormal stratigraphic features in Ras Gharib oil fi eld.– In: 3rd Arab Petroleum Congress, Alexandria, Egypt, p. 10.

HALLAM, A. (1987): End-Cretaceous mass extinction event: argument for terrestrial causation.– Science, 238, 1237–1242.

KELLER, G. (2002): Guembelitria-dominated late Maastrichtian planktic foraminiferal assemblages mimic early Danian in central Egypt.– Marine Micropaleont., 47, 71–99. doi:10.1016/S0377-8398(02) 00116 -0

KELLER, G., ADATTE, T., TANTAWY, A.A., BERNER, Z., STINNES-BECK, W., STUEBEN, D. & LENAZA, H.A. (2007): High stress late Maastrichtian early Danian palaeoenvironment in the Neuque ́n Basin, Argentina.– Cretac., Res., 28, 939–960.

KENNETT, J.P. & STOTT, L.D. (1991): Abrupt deep-sea warming, pa-leoceanographic changes and benthic extinction at the end of the Palaeocene.– Nature, 353, 225–229.

KNOX, R.W. (1994): The age and regional context of the Thanetian stra-totype sections of the SE England.– GFF, 116, 55–56. doi:10.1038/ 353225a0

LAMOLDA, M.A. & GOROSTIDI, A. (1992): Nannofossil stratigraph-ic record in the Upper Maastrichtian–Lowermost Danian at Zuma-ya (Northern Spain).– In: Proceedings of the 3rd International Nan-noplankton Association Conference. Mem. Sci. Geol., 43, 149–161.

LEES, J.A. (2002): Calcareous nannofossils biogeography illustrates pa-laeoclimate change in the Late Cretaceous Indian Ocean.– Cretac. Res., 23, 537–634. doi:10.1006/cres.2003.1021

LI, L. & KELLER, G. (1998): Maastrichtian climate, productivity and faunal turnovers in planktic foraminifera in South Atlantic DSDP sites 525 and 21.– Marine Micropaleont., 33, 55–86.

LÜNING, S., MARZOUK, A.M. & KUSS, J. (1998): The Palaeocene of Central East Sinai, Egypt: ‘Sequence stratigraphy' in monotonous hemipelagites.– J. Foram. Res., 28/1, 19–39.

MARTINI, E. (1971): Standard Tertiary and Quaternary calcareous nan-noplankton zonation. – In: FARINACCI, A. (ed.): Proceedings of the Second Planktonic Conference, Edizioni Tecnoscienza, Rome, 2, 739–785.

MARZOUK, A.M. & LÜNING,S. (1998): Comparative biostratigraphy of calcareous nannofossils and planktonic foraminifera in the Pal-aeocene of Eastern Sinai, Egypt.– N. Jahrb. Geol. Paläontol., Ab-handl., 207/1, 77–105.

MCLEAN, D.M. (1982): Deccan volcanism and the Cretaceous – Ter-tiary transition scenario: a unifying causal mechanism.– Syllogeus, 39, 143–144.

MCLEAN, D.M. (1985): Deccan Traps mantle degassing in the terminal Cre taceous marine extinctions.– Cretac. Res., 6, 235–259. doi: 10.1016/0195 -6671(85)90048-5

MONECHI, S., BLEIL, U. & BACKMAN, J. (1985): Magnetobiochro-nology of late Cretaceous-Palaeogene and late Cenozoic pelagic sedimentary sequences from the Northwest Pacifi c (Deep Sea Drill-ing Project Leg 86, Site577).– In: Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Offi ce, Washington, 787–797.

OBAIDALLA, N.A., EL-DAWY, M.H. & KASSAB, A.S. (2009): Bi-ostratigraphy and paleoenvironment of the Danian/Selandian (D/S) transition in the Southern Tethys: A case study from north Eastern Desert, Egypt.– J. Afr. Earth Sci., 53, 1–15. doi:10.1016/j.jafrear-sci.2008.07.004

OKADA, H. & BUKRY, D. (1980): Supplementary modifi cation and introduction of code numbers to the low latitude coccolith biostrati-graphic zonation (Bukry, 1973, 1975).– Marine Micropaleont., 5, 321–325. doi:10.1016/0377-8398(80)90016-X

OLSSON, R.K., HEMLEBEN, C., BERGGREN, W.A. & HUBER, B.T. (1999): Atlas of Palaeocene planktonic foraminifera.– Smithsonian Contributions to Paleobiology, 85, 1–252.

ORUE-ETXEBARRIA, X., APELLANIZ, E. & CABALLERO, F. (2007): Discrepancies in planktic foraminifera biostratigraphies across the Danian/Selandian transition at Zumaia: no poor preservation, but taxonomic different concepts.– In: Abstracts of the In-ternational Workshop of the Palaeocene Working Group (Zumaia, Basque Country), 25–27.

PERCH-NIELSEN, K. (1985a): Mesozoic calcareous nannofossils.– In: BOLLI, H. M., SAUNDERS, J. B. & PERCH-NIELSEN, K. (eds.): Plankton Stratigraphy, Cambridge University Press, 329–426.

PERCH-NIELSEN, K. (1985b): Cenozoic calcareous nannofossils.– In: BOLLI, H.M., SAUNDERS, J.B. & PERCH-NIELSEN, K. (eds.): Plankton Stratigraphy, Cambridge University Press, 427–554.

POSPICHAL, J.J. (1994): Calcareous nannofossils at the K–T boundary, El Kef: no evidence for stepwise, gradual, or sequential extinc-tions.– Geology, 22, 99–102. doi:10.1130/0091-7613(1994)022< 0099:CNATKT>2.3.CO;2

QUILLEVERE, F., AUBRY, M.-P., NORRIS, R.D. & BERGGREN, W.A. (2002): Palaeocene oceanography of the eastern subtropical Indian Ocean: an integrated magnetostratigraphic and stable isotope study of ODP Hole 761B (Wombat Plateau).– Palaeogeog., Palaeo-clim., Palaeoec., 184/4, 371–405.

ROMEIN, A.J.T. (1979): Lineages in early Palaeogene calcareous nan-noplankton.– Utrecht Micropalaeont. Bull., 22, 1–230.SAID, R. (1961): Tectonic framework of Egypt and its infl uence on dis-tribution of foraminifera.– AAPG Bulletin, 45, 198–218.

SAID, R. (1962): The geology of Egypt.– Elsevier Publishing Company, Amsterdam, 370 p.SAMIR, A. (2002): Biostratigraphy and paleoenvironment changes in the Upper Cretaceous-Early Palaeogene deposits of Gabal Samra section, southwestern Sinai, Egypt.– Egypt. J. Paleont., 2, 1–40.

SCHMITZ, B., MOLINA, E., VON SALIS, K. (1998): The Zumaya sec-tion in Spain: a possible global stratotype section for the Selandian and Thanetian Stages.– Newsletters on Stratigraphy, 36, 35–42.SISSINGH, W. (1977): Biostratigraphy of Cretaceous calcareous nan-noplancton.– Geologie en Mijnbouw, 56, 37–65.

SPEIJER, R.P. (2003): Danian–Selandian sea-level change and biotic excursion on the southern Tethyan margin (Egypt).– In: WING, S. L., GINGERICH, P.D., SCHMITZ, B. & THOMAS, E. (eds.): Causes and Consequences of Globally Warm Climates in the Ear-ly Palaeogene, Geological Society of America, Special Paper, 369, 275–290.

SPRONG, J., SPEIJER, R.P. & STEURBAUT, E. (2009): Biostratigra-phy of the Danian/Selandian transition in the southern Tethys: Spe-cial reference to the lowest occurrence of planktic foraminifera Ig-orina albeari.– Geol. Acta, 7/1–2, 63–77.

STAMPFLI, G., FAVRE, P., PILLEVUIT, A. & VANNAY, J. (1995): The Neotethys-East Mediterranean Basin connection.– In: 2nd Interna-tional Symposium The geology of the Eastern Mediterranean re-gion, Abstract book, p. 17.

STEURBAUT, E., DUPUIS, C., ARENILLAS, I., MOLINA, E. & MAT-MATI, M.F. (2000): The Kalaat Senan section in Central Tunisia: a potential reference section for the Danian/Selandian boundary.– In: SCMITZ, B., SUNDQUIST, B. & ANREASSON, F.P. (eds.): Early Palaeogene Warm Climates and Biosphere Dynamics, GFF, 122/1, 158.160. doi:10.1080/11035890001221158

STEURBAUT, E. & SZTRAKOS, K. (2008): Danian/Selandian bound-ary criteria and North Sea Basin. Tethys correlations based on cal-careous nannofossil and foraminiferal trends in SW France. Marine Micropaleont., 67, 1–29.

STROUGO, A. (1986): The Velascoensis event: A signifi cant episode of tectonic activity in the Egyptian Palaeogene.– N. Jahrb. Geol. Pa-läont., Abhand., 173, 253–269.

TANTAWY, A.A. & KELLER, G. (2004): Biotic effects of volcanism on calcareous nannofossils and planktic foraminifera: Ninetyeast Ridge, Indian Ocean.– Egypt. J. Paleont., 3, 1–23.

TANTAWY, A.A., KELLER, G., ADATTE, T., STINNESBECK, W., KA SSAB, A. & SCHULTE, P. (2001): Maastrichtian to Palaeocene depositional environment of the Dakhla Formation, Western Desert, Egypt: Sedimentology, mineralogy, and integrated micro- and mac-rofossil biostratigraphies.– Cretac. Res., 22, 795–827. doi:10.1006/cres.2001.0291

TANTAWY, A.A., ZAKHERA, M. & KASSAB, A. (2003): Biostratig-raphy and paleoecology of the Upper Cretaceous-Palaeocene Se-quence, northern scarpe of Farafra Oasis, Western Desert.– In: Ab-stracts of the 3rd Annual Meeting of Paleontological Society of Egyptian, p. 6–7.

THIERSTEIN, H.R. (1981): Late Cretaceous nannoplankton and the change at the Cretaceous–Tertiary boundary.– In: WARME, J.E, DOUGLAS, R.G. & WINTERER, E.L. (eds.): The Deep Sea Drill-ing Project: a Decade of Progress, SEPM Special Publication, 32, 355–394.

VAN ITTERBEECK, SPRONG, J., DUPUIS, C., SPEIJER, R.P. & STEURBAUT, E. (2007): Danian/Selandian boundary stratigraphy and ostracod records from Sidi Nasseur, Tunisia.– Marine Micro-paleont., 62, 211–234.

VAROL, O. (1989): Palaeocene calcareous nannofossil biostratigra-phy.– In: CRUX, J.A. & VAN HECK, S.E. (eds.): Nannofossils and their Applications, British Micropalaeontological Society, 12, 267–310.

WORSLEY, T. & MARTINI, E. (1970): Late Maastrichtian nannoplank-ton provinces.– Nature, 225, 1242–1243.YOUSSEF, A.M. (2009): High resolution calcareous nannofossil bios-tratigraphy and paleoecology across the Latest Danian event (LDE) in central Eastern Desert, Egypt.– Marine Micropaleont., 72, 111–128. doi:10.1016/j.marmicro.2009.03.007