ANKARA CİVARINDA BULUNAN BİRKAÇ PERMİEN KALKER ALGIN ETÜDÜ

1953 yılı yazında Ankara bölgesi Hasanoğlan civarı jeolojik çalışmalarımız neticesi (U. Bilgütay, M.T.A. Rapor No. 2617, 1957) belirtilmiş olup, paleontolojik etüdlerimiz bilhassa Hasanoğlan-Karacadere Permien kalkerleri üzerine teksif edilmiştir. Bu kalkerler içerisinde gayet bol Fusulinidae cinsleri ile kalker alg fosilleri tesbit etmiştik. Etüd sahamız dahilinde fosilli Permien yalnız Hasanoğlan köyünün kuzeydoğusuna isabet eden Karacadere mevkiinde görülmektedir. Fakat Fusulinidae'li kalkerler NNE da İdris dağı eteklerinde ve SSW da Odabaşı köyü Beypınarı mevkiinde de tarafımızdan görülmüştür (Şekil 1). Bu yazımızda Karacadere Fusulinidae'li kalkerlerinin ihtiva ettiği esmer alg (Rhodophyceae) lerden bir cins ile, yeşil alg (Cfılorophyceae) lerden iki, ve mavi alg (Cyanophyceae) lerden bir cinsten ibaret olan kalker alg fosillerinden bahsedilecektir. Alglerle beraber bulunan Foraminiferaların kısmı âzamisini aşağıda görüleceği gibi büyük Fusulinidae'li teşkil etmektedir. Bu Foraminiferaların etüdü S. Erk tarafından yapılmış olup, Üst Karbonifer-Permien olarak yaşlandırılmıştır. 

SOME PERMIAN CALCAREOUS ALGAE FROM THE VICINITY OF ANKARA

During the summer of 1953 a geological field study was made in the Ankara region in the vicinity of Hasanoğlan village (U. Bilgütay, M.T.A. Report No. 2617, 1957). The author has particularly concentrated her paleontological study on the Permian limestones of the HasanoğlanKaracadere area where she was able to identify in these limestones some rather abundant Fusulinidae species as well as calcareous algal fossils. In the area studied fossiliferous Permian formations were observed only in Karacadere locality NE of Hasanoğlan village. However, limestones containing Fusulinidae were seen by the author to the NNE on the slopes of the İdris Dağı and to the SSW near Odabaşı village in the locality named Beypınarı (Fig. 1). This paper describes the calcareous algal fossils consisting of one species of brown algae (Rhodophyceae), two of green algae (Chlorophyceae) and one species of blue algae (Cyanophyceae), all collected from the Karacadere locality in the Fusulinidae - bearing limestones. As will be seen below, the majority of the Foraminifera found together with the algae are represented by large Fusulinidae. These Foraminifera were studied by S. Erk, who attributed them -to the Upper Carboniferous-Permian age.

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