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Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey

Year 2019, Volume: 34 Issue: 1, 91 - 102, 31.03.2019

Güldemin Darbaş Murat Gül

https://doi.org/10.21605/cukurovaummfd.601321

Abstract

The occurrence and development of reefal carbonates depend on biological activity and depositional conditions. Besides of fossil assemblages, it is also critical to determine depositional parameters of environment such as sea level change, substratum or clastic input.  This study is realised on an important reefal carbonate units as known the Kaplankaya and Karaisalı formations in the Değirmençay locality of Mersin Province, Mediterranean. In this study, the ostracod and foraminifer assemblages were determined in the samples collected from reefal carbonate units of the Early-Middle Miocene age.  The base of the investigated area consists of Upper Cretaceous ophiolite and Upper Cretaceous-Palaeocene ophiolitic mélange. These units are unconformably overlain by Miocene sediments. This study determine ostracod and foraminifera assemblages of the Early-Middle Miocene reefal carbonate system. While abundance ostracod species were observed at the reefal carbonate levels, also a few planktonic foraminifer species. As a result of paleontological studies, 12 genera and 15 species from Ostracoda, 3 genera and 3 species from planktonic foraminifera have been determined. The Ostracoda species (Aurila soummamensis, Hemicyprideis villandarutensis), and planktonic foraminifer species (Globigerinoides trilobus, Globoquadrina dehiscens and Orbulina universa) point out that these reefal carbonates deposited at the Early-Middle Miocene time interval.

Keywords

Ostracod Foraminifer Reef Early-Middle Miocene Adana basin Turkey

References

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  • 22. Özer, E., Koc, H., Özsayar, T., 2004. Stratigraphical Evidence for the Depression of the Northern Margin of the Menderes-Tauride Block (Turkey) During the Late Cretaceous. Journal of Asian Earth Science, 22, 401–412.
  • 23. Yetiş, C., Kelling, G., Gökçen, S.L., Baroz, F. 1995. A Revised Stratigraphic Framework for Later Senozoic Sequences in the Northeastern Mediterranean Region. Geologishe Rundschau, 84, 794–812.
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  • 25. Nazik, A., Gurbuz, K., 1992. Karaisalı-Çatalan-Eğner Yöresi (KB Adana) Alt-Orta Miyosen Yaşlı Denizaltı Yelpazelerinin Planktonik Foraminifer Biyostratigrafisi. T.J.K. Bult. 35(1), 67–80, (in Turkish).
  • 26. Gürbüz, K., Kelling, G., 1993. Provenance of Miocene Submarine Fans in the Northern Adana Basin: a Test of Discriminant Function Analysis, Geol. J. 28, 277–295.
  • 27. Yetiş C., 1988. Reorganization of the Tertiary Stratigraphy in the Adana Basin, Southern Turkey. Newsl. Stratigr, 20(1), 43-58.
  • 28. Ünlügenç, U.C., Demirkol, C., 1988. Kızıldağ Yayla (Adana) Dolayının Stratigrafisi, Jeoloji Mühendisliği Dergisi, Ankara, 2-33, 17-25.
  • 29. Gürbüz, K., 1999. Regional Implications of Structural and Eustatic Controls in the Evolution of Submarine Fans: An Example from the Miocene Adana Basin, southern Turkey. Geol. Mag, 136.
  • 30. Satur, N., Hurst, A., Cronin, B., Kelling, G., Gurbuz, K., 2000. Sand Body Geometry in a Sand-rich, Deep-water Clastic System, Miocene Cingoz Formation of Southern Turkey. Mar. Petrol. Geol, 17(2), 239–252.
  • 31. Nazik, A., Gürbüz, K., 1992. Karaisalı-Çatalan-Eğner Yöresinin (KB-Adana) Alt-Orta Miyosen İstifinin Planktonik Foraminifer Biyostratigrafisi. Türkiye Jeoloji Bülteni, 35(1), 67-80.
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  • 33. Nazik, A., 1994. The Holocene Ostracods of İskenderun Bay. MTA, 116, 5-20.
  • 34. Şafak, Ü., 1998. The Tertiary Ostracod Assemblages of Çamlıyayla (İçel) Region. Çamlıyayla (İçel) Yöresi Tersiyer Ostrakod Topluluğu, 20th Anniversary of Geological Engineering Education Symposium in Firat University, Proceedings,183-189, (in Turkish).
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  • 36. Şafak, Ü., Ünlügenç, U.C., 1993. The Ostracod Assemblages and Biostratigraphy of Oligocene-Middle Miocene Units of Outcropped Around Kozoluk, Solaklı and Kevizli (N Adana), Geosound, 21, 117-141, (in Turkish).
  • 37. Şafak, Ü., 1993. The Ostracod Biostratigraphy of Antakya, TJB, 36, 115-137, (in Turkish).
  • 38. Carbonel, P., 1985. Atlas Des Ostracodes de France. Bull. Centres Rech. Explor.-Prod. Elf-Aquitaine, Mem. 9, Pau, (Ed: Oertli, H.J.).
  • 39. Avşar, N., Nazik, A., Dinçer, F., Darbaş, G., 2006. Environmerntal Inerpretation of the Kuzgun Formation in the Adana Basin through Microfossils. Yerbilimleri, 27(1), 1-21.
  • 40. Gökçen, N., 1984. Neomonoceratina Helvetica Superzone and Carinocythereis Datumplane in Neogene Sequences of Turkey, Newsl. Statigr. 2 Tab, Berlin-Stuttgart, 13(2), 94-103.
  • 41. Tanar, Ü., 1989. The Stratigraphical and Micropaleontological (Ostracod and Foraminifer) Investigation of Tertiary Unit of Mut Basin. PHD Thesis, Çukurova University, 199, (in Turkish).
  • 42. Şafak, Ü., 1993. Karsantı Yöresinde (KKD Adana) Yüzeyleyen Tersiyer İstifinin Ostrakod Dağılımı ve Ortamsal Özellikleri, Türkiye Jeoloji Bülteni, 36, 1.
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Değirmençay Bölgesindeki Alt-Orta Miyosen Resifal Karbonatların Ostrakod ve Planktonik Foraminifer Topluluğu, KB Mersin/G Türkiye

Year 2019, Volume: 34 Issue: 1, 91 - 102, 31.03.2019

Güldemin Darbaş Murat Gül

https://doi.org/10.21605/cukurovaummfd.601321

Abstract

Resifal karbonatların oluşumu ve gelişimi büyük ölçüde biyolojik aktivite ve çökelme ortam koşullarına bağlıdır. Bu nedenle resifal karbonatların oluşum ve gelişimini anlayabilmek için fosil toplululuğunu ortaya koymak, çökelme ortam koşullarını yansıtan deniz seviyesi, deniz tabanı ve klastik girdisini bilmek kadar önemlidir. Bu çalışma Akdeniz’de önemli bir resifal karbonat sistemi olan Kaplankaya ve Karaisalı Formasyonları üzerinde yürütülmüştür. Çalışma bölgesi Mersin İli’nin kuzeybatısındaki Değirmençay ilçesinin çevresinde yer almaktadır. İnceleme alanının tabanı Üst Kretase ofiyolitleri ve Geç Kretase-Paleosen yaşlı ofiyolitik melanjden oluşmaktadır. Bu birimler uyumsuz olarak Miyosen çökelleri tarafından örtülür. Bu çalışmada, Erken-Orta Miyosen resifal karbonat sisteminin ostrakod ve foraminifer toplulukları belirlenmiştir. Bu çalışmaların sonucunda resif düzeylerinde tespit edilen ostrakod içeriğinin planktonik foraminifer içeriğine göre daha fazla olduğu gözlenmiştir. Paleontolojik çalışmalar sonucunda, ostrakodlardan 12 cins ve 15 tür, planktonik foraminiferlerden ise 3 cins ve 3 tür tespit edilmiştir. Ostrakodlardan Aurila soummamensis ve Hemicyprideis villandrautensis ve planktonik foraminiferlerden Globigerinoides trilobus, Globoquadrina dehiscens ve Orbulina universa gibi türler bu resifal karbonatların Erken-Orta Miyosen zaman aralığında çökeldiklerini göstermektedir. 

Keywords

Ostrakod Foraminifer Resif Erken-Orta Miyosen Adana baseni Türkiye

References

  • 1. Karabıyıkoğlu, M., Tuzcu, S., İner, A., Deynoux, M., Orcen, S., Hakyemez, A., 2005. Facies and Environmental Setting of the Miocene Coral Reefs in the Late-orogenic Fill of the Antalya Basin, Western Taurides, Turkey: Implications for Tectonic Control and Sea-level. Sedimentary Geology, 173(1–4), 345–371.
  • 2. Gül, M., Eren, M., 2003. The Sedimentary Characteristics of Dağpazarı Patch Reef (Middle Miocene, Mut-Içel/Turkey). Carbonates and Evaporites, 18(1), 51–62.
  • 3. Şafak, Ü., Kelling, G., Gökçen, N.S., Gürbüz, K., 2005. The Mid-cenozoic Succession and Evolution of the Mut Basin, Southern Turkey, and its Regional Significance. Sedimentary Geology, 173(1-4), 121–150.
  • 4. Janson, X., Buchem F.S.P., Dromart, G., Eichenseer, H.T., Dellamonica, X., Boichard, R., Bonaffe, F. And Eberli, G., 2010. Architecture and Facies Differentiation within a Middle Miocene Carbonate Platform, Ermenek, Mut Basin, Southern Turkey. Geological Society, London, Special Publications, 329, 265-290.
  • 5. Görür, N., 1979. Sedimentology of the Karaisalı Limestone (Miocene). Geological Bulletin of Turkey, (in Turkish with English abstract). 22–2, 227-232.
  • 6. Görür, N., 1980. Diagenetic Evolution of the Karaisalı Limestone (Miocene). In: Fifth Petroleum Congress of Turkey, Ankara, 123-128 (in Turkish with English abstract).
  • 7. Görür, N., 1994. Tectonic Control in the Development of a Lower Miocene Reef at a Complex Triple Junction: Depositional History of the Karaisali Formation of the Adana Basin, Turkey. Geol. Mediterr, 49–67.
  • 8. Gül, M., 2007. Effects of Antecedent Topography on Reefal Carbonate Deposition: Early-Middle Miocene of the Adana Basin, S. Turkey. Jornal of Asian Sciences, 31, 18-37.
  • 9. Cronin, B.T., Gurbuz, K., Hurst, A., Satur, N., 1999. Vertical and Lateral Organization of a Carbonate Deep-water Slope Marginal to a Submarine Fan System, Miocene, Southern Turkey. Sedimentology, 47, 801–824.
  • 10. İkram, M., Varol, B. 2011. Neogene Reefal Limestones and Their Significance in the Basin Architecture, Osmaniye-Bahçe and Neighbouring Sub-basins, SE Turkey Carbonates and Evaporites, 217-234.
  • 11. Büyükutku, A.G., 2009. Reservoir Properties of Karaisalı Formation in the Adana Basin, Southern Turkey. Journal of Petroleum Science and Engineering, 65, 33–44.
  • 12. Buchem, F.S.P.V., Gerdes, K.D., Esteban, M., 2012. Mesozoic and Cenozoic Carbonate Systems of the Mediterranean and the Middle East: Stratigraphic and Diagenetic Reference Models-an Introduction. Geological Society, London, Special Publications, 329, 1-7.
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  • 15. Tanar, Ü., 1985, The Mollusca Assemblages of Karaisalı, Kuzgun and Memişli Formations of Körlü (Tarsus-Adana) Region. Körlü (Tarsus-Adana) Bölgesi Karaisalı, Kuzgun, Memişli Formasyonlarının Molluska Faunası Jeoloji, Müh. Der., 24, 17-31, Ankara (in Turkish).
  • 16. Nazik, A., 1993. The Ostracod Biostratigraphy and environmental interpretation of Gözne (Mersin) Clastic Sequences. Doğa-Yerbilimleri, 2, 167-173, Ankara (in Turkish).
  • 17. Safak, U., Nazik, A., 1994. Eshab-ı Kehf (Tarsus-Mersin) Dolayı Neojen İstifinin Ortamsal Yorumu. Yerbilimleri Geosound, 15. Yıl Sempozyumu, 22, 291–300, (in Turkish).
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  • 19. Ünlügenç, U.C., Kelling, G., Demirkol, C., 1990. Aspects of Basin Evolution in the Neogene Adana Basin, SE Turkey. In: Savas_c, in, M.Y., Eronat, A.H., Eds.), Proc. Int. Earth Science Cong. On Aegean Region, İzmir, 1, 353–370.
  • 20. İşler, F., 1990. Geology of the Ophiolite in the Fındıkpınarı (Mersin). Cumhuriyet University, Journal of Engineering, Serie A, Geosound, 6-7, 1-2, 45-53 (in Turkish with English abstract).
  • 21. Parlak, O., Delaloye, M., 1996. Geochemistry and Timing of Postmetamorphic Dyke Emplacement in the Mersin Ophiolite (southern Turkey): New Age Constraints from 40Ar/39Ar Geochronology. Terranova 8, 585–592.
  • 22. Özer, E., Koc, H., Özsayar, T., 2004. Stratigraphical Evidence for the Depression of the Northern Margin of the Menderes-Tauride Block (Turkey) During the Late Cretaceous. Journal of Asian Earth Science, 22, 401–412.
  • 23. Yetiş, C., Kelling, G., Gökçen, S.L., Baroz, F. 1995. A Revised Stratigraphic Framework for Later Senozoic Sequences in the Northeastern Mediterranean Region. Geologishe Rundschau, 84, 794–812.
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  • 25. Nazik, A., Gurbuz, K., 1992. Karaisalı-Çatalan-Eğner Yöresi (KB Adana) Alt-Orta Miyosen Yaşlı Denizaltı Yelpazelerinin Planktonik Foraminifer Biyostratigrafisi. T.J.K. Bult. 35(1), 67–80, (in Turkish).
  • 26. Gürbüz, K., Kelling, G., 1993. Provenance of Miocene Submarine Fans in the Northern Adana Basin: a Test of Discriminant Function Analysis, Geol. J. 28, 277–295.
  • 27. Yetiş C., 1988. Reorganization of the Tertiary Stratigraphy in the Adana Basin, Southern Turkey. Newsl. Stratigr, 20(1), 43-58.
  • 28. Ünlügenç, U.C., Demirkol, C., 1988. Kızıldağ Yayla (Adana) Dolayının Stratigrafisi, Jeoloji Mühendisliği Dergisi, Ankara, 2-33, 17-25.
  • 29. Gürbüz, K., 1999. Regional Implications of Structural and Eustatic Controls in the Evolution of Submarine Fans: An Example from the Miocene Adana Basin, southern Turkey. Geol. Mag, 136.
  • 30. Satur, N., Hurst, A., Cronin, B., Kelling, G., Gurbuz, K., 2000. Sand Body Geometry in a Sand-rich, Deep-water Clastic System, Miocene Cingoz Formation of Southern Turkey. Mar. Petrol. Geol, 17(2), 239–252.
  • 31. Nazik, A., Gürbüz, K., 1992. Karaisalı-Çatalan-Eğner Yöresinin (KB-Adana) Alt-Orta Miyosen İstifinin Planktonik Foraminifer Biyostratigrafisi. Türkiye Jeoloji Bülteni, 35(1), 67-80.
  • 32. Öğrünç, G., Gürbüz, K., Nazik, A., 2000. Adana Baseni Üst Miyosen-Pliyosen İstifinde Messiniyen Tuzluluk Krizi’ne ait Bulgular. Yerbilimleri, 22, 183-192.
  • 33. Nazik, A., 1994. The Holocene Ostracods of İskenderun Bay. MTA, 116, 5-20.
  • 34. Şafak, Ü., 1998. The Tertiary Ostracod Assemblages of Çamlıyayla (İçel) Region. Çamlıyayla (İçel) Yöresi Tersiyer Ostrakod Topluluğu, 20th Anniversary of Geological Engineering Education Symposium in Firat University, Proceedings,183-189, (in Turkish).
  • 35. Darbaş, G., Gül, M., 2006. The Paleontology of Coal Units in Alacık Formation (Kahramanmaraş Basin). KSU Journal of Science and Engineering, 9(2), 71-81, (in Turkish).
  • 36. Şafak, Ü., Ünlügenç, U.C., 1993. The Ostracod Assemblages and Biostratigraphy of Oligocene-Middle Miocene Units of Outcropped Around Kozoluk, Solaklı and Kevizli (N Adana), Geosound, 21, 117-141, (in Turkish).
  • 37. Şafak, Ü., 1993. The Ostracod Biostratigraphy of Antakya, TJB, 36, 115-137, (in Turkish).
  • 38. Carbonel, P., 1985. Atlas Des Ostracodes de France. Bull. Centres Rech. Explor.-Prod. Elf-Aquitaine, Mem. 9, Pau, (Ed: Oertli, H.J.).
  • 39. Avşar, N., Nazik, A., Dinçer, F., Darbaş, G., 2006. Environmerntal Inerpretation of the Kuzgun Formation in the Adana Basin through Microfossils. Yerbilimleri, 27(1), 1-21.
  • 40. Gökçen, N., 1984. Neomonoceratina Helvetica Superzone and Carinocythereis Datumplane in Neogene Sequences of Turkey, Newsl. Statigr. 2 Tab, Berlin-Stuttgart, 13(2), 94-103.
  • 41. Tanar, Ü., 1989. The Stratigraphical and Micropaleontological (Ostracod and Foraminifer) Investigation of Tertiary Unit of Mut Basin. PHD Thesis, Çukurova University, 199, (in Turkish).
  • 42. Şafak, Ü., 1993. Karsantı Yöresinde (KKD Adana) Yüzeyleyen Tersiyer İstifinin Ostrakod Dağılımı ve Ortamsal Özellikleri, Türkiye Jeoloji Bülteni, 36, 1.
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There are 53 citations in total.

Details

Primary Language English
Journal Section Articles
Authors

Güldemin Darbaş

Murat Gül

Publication Date March 31, 2019
Published in Issue Year 2019 Volume: 34 Issue: 1

Cite

APA Darbaş, G., & Gül, M. (2019). Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi, 34(1), 91-102. https://doi.org/10.21605/cukurovaummfd.601321
AMA Darbaş G, Gül M. Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey. cukurovaummfd. March 2019;34(1):91-102. doi:10.21605/cukurovaummfd.601321
Chicago Darbaş, Güldemin, and Murat Gül. “Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates Within the Değirmençay Area, NW Mersin/S Turkey”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 34, no. 1 (March 2019): 91-102. https://doi.org/10.21605/cukurovaummfd.601321.
EndNote Darbaş G, Gül M (March 1, 2019) Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 34 1 91–102.
IEEE G. Darbaş and M. Gül, “Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey”, cukurovaummfd, vol. 34, no. 1, pp. 91–102, 2019, doi: 10.21605/cukurovaummfd.601321.
ISNAD Darbaş, Güldemin - Gül, Murat. “Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates Within the Değirmençay Area, NW Mersin/S Turkey”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 34/1 (March 2019), 91-102. https://doi.org/10.21605/cukurovaummfd.601321.
JAMA Darbaş G, Gül M. Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey. cukurovaummfd. 2019;34:91–102.
MLA Darbaş, Güldemin and Murat Gül. “Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates Within the Değirmençay Area, NW Mersin/S Turkey”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi, vol. 34, no. 1, 2019, pp. 91-102, doi:10.21605/cukurovaummfd.601321.
Vancouver Darbaş G, Gül M. Ostracoda and Foraminifera Assemblages of the Lower-Middle Miocene Reefal Carbonates within the Değirmençay Area, NW Mersin/S Turkey. cukurovaummfd. 2019;34(1):91-102.