Abstract
A Cenomanian-Turonian interval in the Mozduran pass section, eastern part of Kopet-Dagh basin (NE of Iran), was measured and studied in order to interpret the biostratigraphy and paleoecology (based on distribution of planktonic foraminifera). This section consists of 52.5-m light and gray marl and coincides with the Aitamir and Abderaz formation boundary. Based on study of 47 samples, 11 planktonic foraminifera genera and 27 species were encountered, and the following zones have been defined: Rotalipora cushmani Total Range Zone and three zones of Helvetoglobotruncana helvetica, Dicarinella primitiva-Marginotruncana sigali, and Dicarinella concavata as condenced zones. This study shows that the sediment record is incomplete in the section. This unconformity is just after a drowning succession, places in the Late Cenomanian-Early Turonian Whiteinella archaeocretacea Zone, and interpreted as a drowning unconformity. A paleoenvironmental model has been formulated to explain the successive paleocommunity changes during this drowning of the platform. We attribute the drowning of some parts of the platform to the occurrence of the Cenomanian-Turonian oceanic anoxic event. The impingement of anoxic waters over the platform could produce the drastic reduction of the carbonate producing observed in the stratigraphic section and therefore a reduction in carbonate accumulation rates. Subsidence and the Late Cenomanian-Early Turonian sea level rise were then able to drown the platform.
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References
Abramovich S, Keller G, Stueben D, Berner Z (2003) Characterization of late Campanian and Maastrichtian planktic foraminiferal depth habitats and vital activities based on stable isotopes. Palaeogeogr Palaeoclimatol Palaeoecol 202:1–29
Afsharharb A (1969) A brief history of geological exploration and geology of the Sarakhas Area and the Khangiran Gas Field. Bull Iran Pet Inst 37:86
Afsharharb A (1994) Kopet-Dagh geology, Tehran, geological survey of Iran
Aguilera-Franco N, Allison P (2004) Events of the Cenomanian-Turonian Succession, Southern Mexico. J Iber Geol 31:25–50
Aguilera-Franco N, Scott R (2005) Timing and rates of the Cenomanian-Turonian drowning on the Guerrero-Morelos Platform, Southern Mexico. Stratigraphy 4(2):341–354
Alavi M, Vaziri H, Seyedemami K, Lasemi Y (1997) The Triassic and associated rocks of the Aghdarband areas in central and north eastern Iran as remnant of the southern Turanian active continental margin. Geol Soc Am Bull 109:1563–1575
Amorossi A (1995) Glaucony and sequence stratigraphy: a conceptual framework of distribution in siliciclastic sequences. J Sediment Res 65:419–425
Arthur MA, Dean WE, Schlanger SO (1985) Variations in the global carbon cycle during the Cretaceous related to climate, volcanism and changes in atmospheric CO2. AGU Geophys Monogr 32:504–529
Berberian M, King GCP (1981) Toward a paleogeographyand tectonic evolution of Iran. Can J Earth Sci 18:210–265
Bice KL, Birgel D, Meyers PA, Dahl KA, Hinrichs KU, Norris RD (2006) A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO2 concentrations. Paleoceanography 21. doi:10.1029/2005PA001203
Brass GW, Southam JR, Peterson WH (1982) Warm saline bottom water in the ancient ocean. Nature 296:620–623
Braun H (1962) Zur Entstehung der marin-sedimentaeren Eisenerze. Z. Erzbergb. Metalhiitten Wes 15:613–623
Buryakovsky LA, Chilinger GV, Aminzadeh F (2001) Petroleum geology of south Caspian basin. Gulf Professional Publishing, USA
Caron M (1985) Cretaceous planktonic foraminifera. In: Plankton stratigraphy. Cambridge Univ pp 17–86
Davoudzadeh M, Schmidt K (1984) Review of the Mesozoic paleogeography and paleotectonic evolution of Iran. N Jb Geol Paläont (Abh) 2:182–207
Fairbridge RW (1967) Phases of diagenesis and authigenesis. In: Diageesis in Sediment, Elsevier, Amsterdam pp. 19–89
Flügel E (2010) Microfacies of carbonate rocks; analysis, interpretation and application. Springer-Verlag, Berlin
Föllmi KB (1996) The phosphorus cycle, phosphogenesis and marine phosphate-rich deposits. Earth Sci Rev 40:55–124
Gale AS, Smith AB, Monks NEA, Young JA, Howard A, Wray DS, Huggett JM (2000) Marine biodiversity through the Late Cenomanian-Early Turonian: palaeoceanographic controls and sequence stratigraphic biases. J Geol Soc London 157:745–757
Gradstein FM, Agterberg FP, Ogg JG, Hardenbol J, Veen PV, Huang Z (1995) A Tr iassic, Jurassic and Cretaceous time scale. SEPM Spec Publ 54:95–126
Haq BU, Hardenbol J, Vail PR (1987) Chronology of fluctuating sea levels since the Triassic. Science 235:1156–1167
Hardenbol J, Thierry J, Farley MB, Jacquin T, Graciansky PC, Vail PR (1998) Mesozoic and Cenozoic sequence chronostratigraphic framework of Europe anbasins. SEPM Spec Publ 60:3–13
Hart MB (1999) The evolution and biodiversity of Cretaceous planktonic foraminiferida. Geobios 32:247–255
Heydari E (2008) Tectonics versus eustatic control on superse-quences of the Zagros Mountains of Iran. Tectonophysics 451:56–70
Hilbretch H, Hubberton HW, Oberhansli H (1992) Biogeography of planktonic foraminifera and regional carbon isotope variations: productivity and water masses in Late Cretaceous Europe. Palaeogeogr Palaeoclimatol Palaeoecol 93:407–421
Huck S (2011) understanding the driving factors on the Oceanic Anoxic Event 1a (early Aptian) The neritic perspective. Dissertations, university of Bochum
Jarvis I, Carson GA, Cooper MKE, Hart MB, Leary PN, Tocher BA, Horne D, Rosenfeld A (1988) Microfossil assemblages and the Cenomanian-Turonian (Late Cretaceous) oceanic anoxic event. Cretac Res 9:3–103
Jarvis I, Mabrouk A, Moody RTJ, Cabrera S (2002) Late Cretaceous (Campanian) carbon isotope events, sea-level change and correlation of the Tethyan and Boreal realms. Palaeogeogr Palaeoclimatol Palaeoecol 188:215–248
Jenkyns HC (1999) Mesozoic anoxic events and palaeoclimate. Zbl Geol Paläontol 1:943–949
Jenkyns HC (2003) Evidence for rapid climate change in the Mesozoic-Palaeogene greenhouse world. Philos Trans R Soc 361:1885–1916
Keller G (2002) Guembelitria dominated late Maastrichtian planktic foraminiferal assemblages mimic early Danian in the Eastern Desert of Egypt. Mar Micropaleontol 47:71–99
Keller G, Pardo A (2004) Paleoecology of the Cenomanian-Turonian Stratotype Section (GSSP) at Pueblo, Colorado. Mar Micropleontol 51:95–128
Keller G, Adatte T, Luciani V, Karoui N, Zaghbib-Turki D (2002) Paleoecology of the Cretaceous-Tertiary mass extinction in planktic foraminifera. Palaeogeogr Palaeoclimatol Palaeoecol 178:257–298
Keller G, Stueben D, Zsolt B, Adatte T (2004) Cenomanian-Turonian sea level and salinity variations at Pueblo, Colorado. Palaeogeogr Palaeoclimatol Palaeoecol 211:19–43
Larson RL (1991) Latest pulse of earth evidence for a mid Cretaceous superplume. Geology 19:547–550
Larson RL, Erba E (1999) Onset of the mid-Cretaceous greenhouse in the Barremian-Aptian: igneous events and the biological, sedimentary, and geochemical responses. Paleoceanography 14:663–678
Lecki RM, Yuretich RF, West OOL, Finkelstein D, Schmidt M (1998) Paleoceanography of the southwestern Western Interior Sea during the time of the Cenomanian-Turonian boundary (Late Cretaceous). Concepts Sedimentol Paleontol 6:101–126
Leckie RM (1985) Foraminifera of the Cenomaian-Turonian boundary interval, Greenhorn Formation, Rock Canyon Anti-cline, Pueblo, Colorado. Mar Micropaleontol 4:139–149
Lenton TM, Watson AJ (2000) What regulates the oxygen content of the atmosphere? Glob Biogeochem Cycles 14:249–268
Marino M, Santantonio M (2010) Understanding the geological record of carbonate platform drowning across rifted Tethyan margins: Examples from the Lower Jurassic of the Apennines and Sicily (Italy). Sediment Geol 225:116–137
Masse JP, Fenerci-Masse M (2013) Drowning events, development and demise of carbonate platforms, andcontrolling factors: The Late Barremian-Early Aptian record of Southeast France. Sediment Geol 298:28–52
Moussavi-Harami R, Brenner RL (1992) Geohistory analysis and petroleum reservoir characteristics of Lower Cretaceous (Neocomian) sandstone, eastern portion of Kopet-Dagh basin, northeast Iran. AAPG Bull 76:1200–1208
Premoli-Silva I, Verga D (2004) Practical Manual of Cretaceous planktonic Foraminifera. Universities of Perugia and, Milano
Price GD, Hart MB (2002) Isotopic evidence for early to mid-Cretaceous ocean temperature variability. Mar Micropaleontol 46:45–58
Schlager W (1981) The paradox of drowned reefs and carbonate platforms. Geol Soc Am Bull 92:197–211
Schlager W (1989) Drowning unconformities on carbonate platforms. Soc. Econ. Paleontol. Mineral Spec Publ 44:15–25
Schlanger SO, Arthur MA, Jenkyns HC, Scholle PA (1987) The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ13C excursion. Geol Soc London Spec Publ 26:371–399
Shafiee-Ardestani M, Vahidinia M, Youssef-Ali M (2011) Biostratigraphy and foraminiferal bioevent of the Abderaz Formation (middle Turonian-lower Companian) in the Kopeh-Dagh basin, northeastern Iran. Egypt J Paleontol 11:1–16
Shafiee-Ardestani M, Vahidinia M, Sadeghi A (2013) Paleoceanography and Paleobiogeography Patterns of the Turonian-Campanian Foraminifers from the Abderaz Formation, North Eastern Iran. Open J Geol 3:19–27
Vahidinia M, Ariai A, Sobhani E (1999) A new approach to Abderaz Formation in the east of Kopet-Dagh basin. Sci J Islam Azad Univ 31:2325–2385
Vogt PR (1989) Volcanogenic upwelling of anoxic, nutrient-rich water: A possible factor in carbonate-bank/reef demise and benthic faunal extinctions. Geol Soc Am Bull 101:1225–1245
Wilson J (1975) Carbonate facies in geologic history. Springer, New York
Wissler L, Funk H, Weissert H (2003) Response of Early Cretaceous carbonate platforms to changes in atmospheric carbon dioxide levels. Palaeogeogr Palaeoclimatol Palaeoecol 200:187–205
Wonders AA (1980) Middle and late Cretaceous planktonic Foraminifera of the western Mediterranean area. Utrecht Micropaleontol Bull 24:1–158
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Kalanat, B., Vahidinia, M., Vaziri-Moghaddam, H. et al. A Cenomanian-Turonian drowning unconformity on the eastern part of Kopet-Dagh basin, NE Iran. Arab J Geosci 8, 8373–8384 (2015). https://doi.org/10.1007/s12517-015-1779-6
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DOI: https://doi.org/10.1007/s12517-015-1779-6