Journals / Bulletin of the mineral research and exploration / 2020 / Cilt: 0 - Sayı: 163

First Turolian findings in the Neogene sequence of Denizli Basin (SW Anatolia) and its regional palaeobiogeographic significance

Denizli Havzası (GB Anadolu) Neojen istifinde ilk Turoliyen bulgusu ve bölgesel paleobiyocoğrafik önemi

Pages
1–12
Publication Date
2022-10-12
DOI
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

These first Turolianrecords from the basin fill succession bear importance on reconstruction for the palaeobiogeographicdiversity of relevant taxons as well as admit of interbasinal stratigraphic correlation for the WesternAnatolian terrestrial Neogene basins.

📌 3 Key Takeaways

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Objective & Hypothesis:The large fossil vertebrates obtained from the alluvial flood-plain deposits of the Kolankaya formationare determined as Skoufotragus laticeps (Andree, 1926) and Hipparion brachypus (Hensel, 1862),as representative elements of palaeomammal faunas spanning from the eastern Mediterranean toIranian domains during the late Miocene (early-middle Turolian, MN11-12).
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Key Findings & Data:The large fossil vertebrates obtained from the alluvial flood-plain deposits of the Kolankaya formationare determined as Skoufotragus laticeps (Andree, 1926) and Hipparion brachypus (Hensel, 1862),as representative elements of palaeomammal faunas spanning from the eastern Mediterranean toIranian domains during the late Miocene (early-middle Turolian, MN11-12).
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Conclusion & Impact:These first Turolianrecords from the basin fill succession bear importance on reconstruction for the palaeobiogeographicdiversity of relevant taxons as well as admit of interbasinal stratigraphic correlation for the WesternAnatolian terrestrial Neogene basins.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

The large fossil vertebrates obtained from the alluvial flood-plain deposits of the Kolankaya formationare determined as Skoufotragus laticeps (Andree, 1926) and Hipparion brachypus (Hensel, 1862),as representative elements of palaeomammal faunas spanning from the eastern Mediterranean toIranian domains during the late Miocene (early-middle Turolian, MN11-12). These first Turolianrecords from the basin fill succession bear importance on reconstruction for the palaeobiogeographicdiversity of relevant taxons as well as admit of interbasinal stratigraphic correlation for the WesternAnatolian terrestrial Neogene basins.

Özet

Denizli Havzası Neojen istifine ait Kolankaya formasyonu alüvyon yelpazesi taşkın düzlüğü birimleri (Güzelpınar Üyesi) içerisinde bulunan omurgalı fosiller, geç Miyosen (erken-orta Turoliyen, MN11-12) süresince Doğu Akdeniz’den İran’a kadar yayılan coğrafyanın memeli paleofaunasının karakteristik elemanı olan Skoufotragus laticeps (Andree, 1926) ve Hipparion brachypus (Hensel, 1862) olarak tanımlanmıştır. Havza istifinde bilinen bu ilk Turoliyen bulgusu, ilgili taksonların paleobiyocoğrafik yayılımlarının kurgulanmasında önemli olduğu gibi Batı Anadolu karasal Neojen havzaları arasında stratigrafik korelasyona da olanak vermektedir.

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Cite This Article

ALÇİÇEK, M. C., DOĞAN, A., MAYDA, S. (2022). First Turolian findings in the Neogene sequence of Denizli Basin (SW Anatolia) and its regional palaeobiogeographic significance. Bulletin of the mineral research and exploration, Cilt: 0 - Sayı: 163, 1–12. https://ajindex.com/articles/469395

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References (7)

  1. Akgün, F., Kaya, T., Forsten, A., Atalay, Z. 2000. Biostratigraphic data (Mammalia and palynology) for the late Miocene Incesu Formation in Düzyayla (Hafik-Sivas). Turkish Journal of Earth Sciences 9, 57-67.
  2. Alçiçek, H. 2010. Stratigraphic correlation of the Neogene basins in Southwestern Anatolia: regional palaeogeographical, palaeoclimatic and tectonic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 291, 297-318.
  3. Alçiçek, H., Alçiçek, M.C. 2014. Palustrine carbonates and pedogenic calcretes in the Çal basin of SW Anatolia: Implication on the Plio-Pleistocene regional climatic pattern in the Eastern Mediterranean. Catena 112, 48-55.
  4. Alçiçek, H., Varol, B., Özkul, M. 2007. Sedimentary facies, depositional environments and palaeogeographic evolution of the Neogene Denizli Basin of SW Anatolia, Turkey. Sedimentary Geology 202, 596- 637. Alçiçek, H., Wesselingh, F.P., Alçiçek, M.C. 2015. Palaeoenvironmental evolution of the late Pliocene-early Pleistocene fluvio-deltaic sequence of the Denizli Basin (SW Turkey). Palaeogeograpy, Palaeoclimatology, Palaeoecology 437, 98-116.
  5. Alçiçek, M.C. 2007. Tectonic development of an orogentop rift recorded by its terrestrial sedimentation pattern: the Neogene Eşen Basin of Southwestern Anatolia, Turkey. Sedimentary Geology 200, 117- 140. Alçiçek, M.C., Kazancı, N., Özkul, M. 2005. Multiple rifting pulses and sedimentation pattern in the Çameli Basin, Southwestern Anatolia, Turkey. Sedimentary Geology 173, 409-431.
  6. Alçiçek, M.C., Ten Veen, J.H., Özkul, M. 2006. Neotectonic development of the Çameli Basin, Southwestern Anatolia, Turkey. In: A. H. F. Robertson, D. Mountrakis (Eds.), Tectonic Development of the Eastern Mediterranean Region. Geological Society London Special Publication 260, 591- 611. Alçiçek, M.C., Mayda, S., Alçiçek., H. 2012. Faunal and palaeoenvironmental changes in the Çal Basin, SW Anatolia: Implications for regional stratigraphic correlation of late Cenozoic basins. Comptes Rendus Geoscience 344, 89-98.
  7. Alçiçek, M. C., Brogi, A., Capezzuoli, E., Liotta, D., Meccheri, M. 2013. Superimposed basin formation during Neogene- Quaternary extension in SWAnatolia (Turkey): insights from the kinematics of the Dinar fault zone. Tectonophysics 608, 713- 727. Alçiçek, M.C., Mayda, S., Ten Veen, J.H., Boulton, S.J., Alçiçek, H., Tesakov, A., Saraç, G., Hakyemez, Y., Göktaş, F., Murray, A., Wesselingh, F.P., JimenezMoreno, G., Büyükmeriç, Y., Bouchal, J.M., Demirel, F.A., Kaya, T.T., Halaçlar, K., Bilgi