Revised Late Campanian-Danian age of the melange-related turbiditic sequence in the Mersin area (Central Taurides, S. Turkey)

A planktonic foraminiferal assemblage obtained from the Yavca stratigraphic section north of Mersin shows that the age of a melange-related turbiditic sequence extends to the Danian (Early Palaeocene). Previously, this turbiditic sequence, termed the Yavca Formation, was considered to be of Late Cretaceous or Campanian-Maastrichtian age. The formation is either depositionally overlain by the Fındıkpınarı ophiolite-related melange or tectonically by Mersin Ophiolite slices or Jurassic-Cretaceous platform carbonates. Clayey limestone and mudstone samples collected from the type area of the Yavca Formation yielded planktonic foraminiferal assemblages, which include Parasubbotina pseudobulloides (Plummer), P. varianta (Subbotina), Praemurica pseudoinconstans (Blow), P. inconstans (Subbotina), Globanomalina compressa (Plummer), G. ehrenbergi (Blow), Subbotina triloculinoides (Plummer), S. triangularis (White), Morozovella praeangulata (White), and Eoglobigerina spiralis (Bolli). These assemblages range from the late Danian P1c subzone to the basal P3a subzone. Basal red pelagic limestones are assigned here to the late Campanian-Maastrichtian, based on the presence of Radotruncana cf. R. calcarata (Cushman) and Contusotruncana cf. C. walfischensis (Todd). The age of the melange-related turbiditic sequence is revised to be late Campanian (Late Cretaceous) to Danian (Early Paleocene). This revised age provides a new insight into the evolution of the Central Taurides and helps refine palaeogeographical interpretation during this time. The timing of the ophiolite emplacement in the Central Taurides is interpreted as post-Danian to pre-Miocene (Late Palaeocene or Late Eocene).

Revised Late Campanian-Danian age of the melange-related turbiditic sequence in the Mersin area (Central Taurides, S. Turkey)

A planktonic foraminiferal assemblage obtained from the Yavca stratigraphic section north of Mersin shows that the age of a melange-related turbiditic sequence extends to the Danian (Early Palaeocene). Previously, this turbiditic sequence, termed the Yavca Formation, was considered to be of Late Cretaceous or Campanian-Maastrichtian age. The formation is either depositionally overlain by the Fındıkpınarı ophiolite-related melange or tectonically by Mersin Ophiolite slices or Jurassic-Cretaceous platform carbonates. Clayey limestone and mudstone samples collected from the type area of the Yavca Formation yielded planktonic foraminiferal assemblages, which include Parasubbotina pseudobulloides (Plummer), P. varianta (Subbotina), Praemurica pseudoinconstans (Blow), P. inconstans (Subbotina), Globanomalina compressa (Plummer), G. ehrenbergi (Blow), Subbotina triloculinoides (Plummer), S. triangularis (White), Morozovella praeangulata (White), and Eoglobigerina spiralis (Bolli). These assemblages range from the late Danian P1c subzone to the basal P3a subzone. Basal red pelagic limestones are assigned here to the late Campanian-Maastrichtian, based on the presence of Radotruncana cf. R. calcarata (Cushman) and Contusotruncana cf. C. walfischensis (Todd). The age of the melange-related turbiditic sequence is revised to be late Campanian (Late Cretaceous) to Danian (Early Paleocene). This revised age provides a new insight into the evolution of the Central Taurides and helps refine palaeogeographical interpretation during this time. The timing of the ophiolite emplacement in the Central Taurides is interpreted as post-Danian to pre-Miocene (Late Palaeocene or Late Eocene).

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  • Başalan, A., İnan, N., Koç, H., Taslı, K. & İnan, S. 2007. Geology of the southern part of Çamlıyayla (NE Mersin) and contributions on description of the Güzeller Formation. Yerbilimleri-Geosound 50-51, 115-137 (in Turkish).
  • Berggren, W.A., Aubry, M.P., Fossen, M., Kent, D.V., Norris, R.D. & Qullévéré, F. 2000. Integrated Paleocene calcareous plankton magnetobiocronology and stable isotope stratigrapy: DSDP Site 384 (NW Atlantic Ocean). Paleogeography, Paleoclimatology, Paleoecology 159, 1-51.
  • Collins, A.S. & Robertson, A.H.F. 1997. Lycian melange, southwestern Turkey: An emplaced Late Cretaceous accretionary complex. Geology 25, 255-258.
  • Demirtaşlı, E., Turhan, N., Bilgin, A.Z. & Selim, M. 1984. Geology of the Bolkar Mountains. In: Tekeli, O., Göncüoğlu, M.C. (eds), Geology of the Taurus Belt. Maden Tetkik ve Arama Enstitüsü, Ankara, Turkey, 125-141.
  • Gradstein, F.M. & Ogg, J.G. 2004. Geologic Time Scale 2004 - why, how and where next! Lethaia 37, 175-181.
  • İlker, S. 1975. Geology and petroleum possibilities of northwest of the Adana Basin. Türkiye Petrolleri Anonim Ortaklığı, Report No. 973, Ankara (in Turkish, unpublished).
  • Koç, H., Özer, E. & Özsayar, T. 1997. Geology of Aydıncık (İçel) area. Yerbilimleri Geosound 30, 417-427 (in Turkish).
  • Koç, H. & Taslı, K. 2010. Litho-biostratigraphy and event analysis of the Cenomanian-Maastrichtian sediments in the Central Taurides (S Turkey). TÜBİTAK Project No. 109Y161, Report, 94 p. (in Turkish, unpublished).
  • Olsson, R.K., Hemleben, C., Berggren, W.A. & Huber, B.T. (eds) 19 Atlas of Paleocene Planktonic Foraminifera. Smithsonian Contributions to Paleobiology, Washington D.C. 85, 1-252. Özer, E., Taslı, K. & Koç, H. 2002. The stratigraphy and tectonic evolution of the Late Cretaceous foreland basin in the İçel region (Central Taurides, Turkey). 1st International Symposium of the Faculty of Mines (ITU) on Earth Science and Engineering, 16-18 May, İstanbul, p. 87.
  • Özgül, N. 1976. Torosların bazı temel jeoloji özellikleri (some major geological features of Taurus). Bulletin of the Geological Society of Turkey 19, 65-78 (in Turkish).
  • Parlak, O. & Robertson, A.H.F. 2004. The ophiolite-related Mersin Melange, southern Turkey: its role in the tectonic–sedimentary setting of Tethys in the Eastern Mediterranean region. Geological Magazine 141, 257-286.
  • Patterson, R.T., Fowler, A.D.  &  Huber, B.T. 2004. Evidence of hierarchical organisation in the planktic foraminiferal evolutionary record. Journal of Foraminiferal Research 34, 85
  • Ricou, L.E. 1980. The structural behavior of Taurus between Hellenides and Zagrids. Bulletin of the Geological Society of Turkey 23, 101-118.
  • Robaszynski, F. & Caron, M. 1995. Foraminifères planktoniques du Crétacé: commentaire de la zonation Europe-Méditerranée. Bulletin Société Géologique de France 166, 681-692.
  • Robertson, A.H.F. & Dixon, J.E. 1984. Introduction: aspects of geological evolution of the Eastern Mediterranean. In: Dixon, J.E. and Robertson, A.H.F. (eds), The Geological Evolution of the Eastern Mediterranean. Geological Society, London, Special Publications 17, 1-74.
  • Robertson, A.H.F., Parlak, O. & Ustaömer, T. 2009. Melange genesis and ophiolite emplacement related to subduction of the northern magrin of the Tauride Anatolide continent, central and western Turkey. Geological Society, London, Special Publications 311, 9-66.
  • Şengör, A.M.C. & Yılmaz, Y. 1981. Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics 75, 181-241.
  • Taslı, K. & Eren, M. 1999. Stratigraphic and sedimentologic approach to the Aptian-Campanian erosional unconformity in the Aydıncık (İçel) area, Central Taurides, S Turkey. YerbilimleriGeosound 34, 229-245.
  • Taslı, K., Özer, E. & Koç, H. 2006. Benthic foraminiferal assemblages of the Cretaceous platform carbonate succession in the Yavca area (Bolkar Mountains, S Turkey): biostratigraphy and paleoenvironments. Geobios 39, 521-533.
  • Tekeli, O., Aksay, A., Ürgün, B.M. & Işık, A. 1984. Geology of the Aladağ Mountains. In: Tekeli, O. & Göncüoğlu, M.C. (eds), Geology of the Taurus Belt. Maden Tektik ve Arama Enstitüsü, Ankara, Turkey, 143-158.
  • Toumarkine, M. & Luterbacher, H. 1985. Paleocene and Eocene planktic foraminifera. In: Bolli, H.M., Saunders, J.B. & PerchNielsen K. (eds), Plankton Stratigraphy, Cambridge University Press, 87-154.
  • Yaman, S. 1991. The Geology and Metogenesis of the Mersin Ophiolites. Ahmet Acar Geology Symposium, 255-267.
  • Yılmaz, Y. 1993. New evidence and model on the evolution of the southeast Anatolian orogen. Geological Society of America Bulletin 105, 251-271.
Turkish Journal of Earth Sciences-Cover
  • ISSN: 1300-0985
  • Yayın Aralığı: Yılda 6 Sayı
  • Yayıncı: TÜBİTAK
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