Neogene Stratigraphy of the Bozbelen area (Çayırhan, Nallıhan) and a New Vertebrate Fossil Locality
Neogene Stratigraphy and a New Vertebrate Fossil Locality
DOI:
https://doi.org/10.5281/zenodo.13631322Keywords:
Bozbelen (Çayırhan), Vertebrate fossils, late Miocene - early Pliocene, Geoheritage,Abstract
Within the scope of the research, we present the vertebrate fossil findings for the first time around Çayırhan (W Ankara). Fossils are only in a single locality namely Bozbelen area and its vicinity within the lacustrine sediments mostly at clayey, marly levels. The paper aims to introduce the fossil findings of this locality, which is important in terms of geoheritage and Miocene-Pliocene geological history of Türkiye, and to revise stratigraphy of the study area that is located in the Beypazarı Neogene Basin. The Miocene basin comprises various lithological units. Stratigraphy based on field observations and satellite views are from bottom to top as follows: Paleogene-aged Karabayır formation (red coloured clastics), Miocene-aged Akpınar formation (=Çayırhan formation) (rhythmic greenish tuffite, claytone, sandstone), Kırmızıtepe formation (red-coloured sandstones, conglomerates), Miocene-Pliocene aged Bozbelen formation (marls, siltstones, mudstones), Aşağıbozbelen formation (sandstones, siltstones), Yukarıbozbelen formation (sandstones, conglomerates) and Quaternary alluvium and slope deposits. The formations have lateral and vertical facies that change each other. Various teeths and broken bones of Hipparion sp., Gazellesp. and Ictitherium sp. are within the sediments of the Bozbelen formation. The age of the unit is late Miocene-early Pliocene. Reworked fossils into the lake muds and lithological features of the studied formation show a very shallow lake coast side paleoenvironment. Trace fossils and silica fillings in the muds originating from the volcanic activity are also noteworthy.
References
Stchepinsky, V., 1942. Beypazarı-Nallıhan-Bolu-Gerede bölgesi jeolojisi hakkında rapor. M.T.A. Raporu, No: 1363.
Rondot, J. 1956. l : 100 000 lik 39/2 (güney kısmı) ve 39/4 paftalarının jeolojisi, Seben-Nallıhan-Beypazarı. M.T.A. Rap., no. 2517 (yayınlanmamış), Ankara.
Kalafatcıoğlu, A., Uysallı, H., 1964. Beypazarı-Nallıhan-Seben civarının jeolojisi. Maden Tetkik Arama Enstitüsü Dergisi 62(1), 1-11.
Siyako,F., 1983. Beypazarı (Ankara) kömürlü Neojen havzasının ve çevresinin jeoloji raporu. M.T.A. Raporu, No:7431, Ankara.
Görmüş, M., Kadıoğlu, Y.K., Demircan, H., Yağmurlu, F., 2018. Haymana, Orhaniye ve Nallıhan (Ankara) Çevrelerindeki Üst Kretase ve Paleojen Çökellerinin İri Bentiklerindeki Mikrobiyoerozyonal Yapılar, 115R058 nolu Tübitak-Çaydağ projesi
Önal, M, Helvacı, C., İnci, U., Yağmurlu, F., Meriç, E., Tansel, İ., 1988. Çayırhan (KB) Ankara kuzeyindeki Soğukçam kireçtaşı, Nardin formasyonu ve Kızılçay gurubunun stratigrafisi, yaşı, fasiyes ve depolama ortamları. TPJD Bülteni 1/2, 132-163.
Ardahanlıoğlu, A. Davutoğlan - Çayırhan (Nallıhan / Ankara) bölgesinin jeolojisi. Ankara Üniversitesi, Fen Bilimleri Enstitüsü, Yüksek Lisans Tezi, 71s.
Ardahanlıoğlu, A., Seyitoğlu, G., Esat, K. 2020. The internal structure of Beypazarı Blind Thrust Zone around Çayırhan. Bull. Min. Res. Exp., 163: 77-97
Saraç, G., 2001. Türkiye Omurgalı Fosil Yatakları. Maden Tetkik ve Arama Genel Müdürlüğü. MTA Raporları, 169s.
Erten, H., Görmüş, M. 2011. Türkiye Neojen küçük memelileri. SDUGEO (Online), 2 (2), 8-14
İnci, U., 1991, Miocene alluvial fan-alkaline playa lignite - trona bearing deposits from an inverted basin in Anatolia: Sedimentology and tectonic controls on deposition. Sedimantary Geology, 71, 73-97.
Inci, U., Helvacı, C., Yağmurlu, F., 1988. Stratigraphy of Beypazarı Neogene basin, Central Anatolia, Turkey. Newsl. Stratigr. 18(3), 165-182.
Kavuşan G., 1991, Beypazarı-Çayırhan linyitlerindeki C,H, O,N, S dağılımları ve infrared spektrofotometrik araştırılması,tektonik ile değişimleri, A.Ü. Araştırma Fonu Proje Raporu, 61 s. Ankara.
Yağmurlu,F., Helvacı, C., 1994. Sedimentological characteristics and facies of evaporite-bearing Kirmir Formation (Neogene), Beypazarı Basin, Central Anatolia, Turkey. Sedimentology 41, 1-14.
Yağmurlu,F., Helvacı, C., Inci, U., 1988. Depositional setting and geometric structure of Beypazarı lignite deposits, Central Anatolia. International Journal of Coal Geology 10, 337-360.
Yağmurlu,F., Helvacı, C., Inci, U., 1990. Tectonic characteristics and structural of the Beypazarı and Nallıhan Neogene basin, Central Anatolia. METU Journal of Pure and Applied Sciences 21 (1-3), 127-143
Karadenizli, L., 1995. Beypazarı havzası (Ankara batısı) Üst Miyosen – Pliyosen jipsli serilerinin sedimantolojisi. Türkiye Jeoloji Bülteni 38(1), 63-74.
Helvacı, C., 2010. Geology of the Beypazarı trona field, Ankara, Turkey. Mid-congress Field Exursions Guidebook, TectonicCrossroads: Evolving Orogens of Eurasia-Africa-Arabia, 4--8 October 2010 Ankara, Turkey, 33 p.
Koral, H., Behzad, B., İşbil, D., Karaağaç, S., 2019. Çayırhan (Ankara) Neojen Havzasının Stratigrafisi ve Neotektonik Özellikleri. İstanbul Yerbilimleri Dergisi, 14s.
Görmüş, M. 1995. Kızılören (Batı Konya) Dolayının Jeolojisi. Süleyman Üniversitesi, Mühendislik Fakültesi Dergisi Jeoloji Seksiyonu, 8, 127-142
Demirci, C., 2000. Structural analysis in Beypazarı-Ayaş-Kazan-Peçenek area NW of Ankara (Turkey) / Beypazarı-Ayaş-Kazan-Peçenek bölgesinde yapısal analiz, Ankara kuzeybatısı (Türkiye). Middle East Technical University, PhD thesis, 278s.
https://en.wikipedia.org/wiki/Hipparion
https://en.wikipedia.org/wiki/Gazelle
https://en.wikipedia.org/wiki/Ictitherium
Vislobokova, I.A., 2023. Ovis gracilis sp. nov. (Artiodactyla, Bovidae) from the Lower Pleistocene of the Taurida Cave in the Crimea and History of the Genus Ovis. ISSN 0031-0301, Paleontological Journal, 2023, Vol. 57, No. 5, pp. 573–585. © Pleiades Publishing, Ltd., Russian Text © The Author(s), 2023, published in Paleontologicheskii Zhurnal, 2023, No. 5, pp. 94–106.
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