Denizli Yöresindeki Bartoniyen–Priyaboniyen (Orta–Geç Eosen) Mikrofosilleri içeren Başçeşme Formasyonu’nun Stratigrafik ve Ortamsal Önemi, Batı Anadolu

Bu çal›flma, Çardak–Tokça havzas›n›n (Bat› Anadolu) Baflçeflme formasyonunundan elde edilen Bartoniyen–Priyaboniyen (Orta–Geç Eosen) yafll›, fauna ve floran›n stratigrafik ve paleoortamsal önemini aç›klar. Çal›fl›lan istif, stratigrafik kesiklik olmaks›z›n, s›¤ deniz, k›y› ortam›nda çökelmifl Baflçeflme formasyonundan bir yüzlektir. Baflçeflme formasyonunun palinolojik toplulu¤unda 40 cins ve 58 tür tan›mlanm›flt›r. ‹yi korunmufl çeflitli palinomorf ve foraminifer topluluklar›, Baflçeflme formasyonun yafl›n› Orta–Geç Eosen olarak vermektedir. Bat› Anadolu’da, mangrove elementleri olan Nypa ve Pelliciera ilk kez bu çal›flmada kaydedilmifltir. Mangrov gerisindeki ortamda Mauritia ve Acrostichum polenleri mevcuttur. Alçak alan-Irmak kenar› elemanlar›, Myricaceae, Betulaceae, Engelhardia, Fagaceae, Myrtaceae, Anacardiaceae ve Taxodiaceae, da¤ elemanlar› ise Pinus, Abies, Picea, Cathaya, Quercus ve Castanea ile karakterize edilir. Tatl›su elamanlar› Sparganiaceae, Pediastrum sp. ve Aglaoreidia cyclops ile temsil edilir. Elde edilen palinolojik veriler, Baflçeflme formasyonun alt kesimlerinden al›nan örneklerin mangrov gerisi ortam› belirtti¤ini göstermektedir. ‹stifin üst kesimlerinde kötü korunmufl dinoflagellatler›n varl›¤› tortullaflman›n mangrove ortam›nda gerçekleflti¤ini göstermektedir. Mercan, bivalvia ve gastropodlu iyi korunmufl foraminifer verileri, tortulaflman›n s›¤ denizel ortamda son buldu¤unu göstermektedir. Bu makalede, ‘coexistence approach’ yöntemine dayal›, Baflçeflme formasyonunun karasal iklimsel koflullar› da tart›fl›lm›flt›r. 

Stratigraphic and Palaeoenvironmental Significance of Bartonian–Priabonian (Middle–Late Eocene) Microfossils from the Baflçeflme Formation, Denizli Province, Western Anatolia

This study explains the stratigraphical and palaeoenvironmental significance of Bartonian-Priabonian (Middle-Late Eocene) fossils, the fauna and flora obtained from the Başçeşme formation of the Çardak-Tokça basin (western Anatolia). The studied sequence is an outcrop from the Başçeşme formation, deposited in a shallow-marine to coastal environment without stratigraphic breaks. Forty genera and 58 species have been recognized in the palynological assemblage of the Başçeşme formation. A well-preserved diverse palynomorph and foraminiferal assemblages yield the Middle-Late Eocene age for the Başçeşme formation. In western Anatolia, mangrove elements Nypa and Pelliciera have been first recorded in this study. The pollen of Mauritia and Acrostichum occur in the back-mangrove environment. Lowland-Riparian and montane elements are characterized by dominance of Myricaceae, Betulaceae, Engelhardia, Fagaceae, Myrtaceae, Anacardiaceae and Taxodiaceae, Pinus, Abies, Picea, Cathaya, Quercus and Castanea, respectively. Fresh-water elements are represented by Sparganiaceae, Pediastrum sp. and Aglaoreidia cyclops. The palynological data for samples taken from the lower part of the section of the Başçeşme formation indicate a back-mangrove environment. The presence of poorly preserved dinoflagellate cysts suggest that sedimentation occurred in a mangrove environment in the upper part of the section. The well-preserved foraminiferal data, along with corals, bivalves and gastropods, indicate that sedimentation ceased in the shallow-marine environment. In this paper, terrestrial climatic conditions of the Başçeşme formation are also discussed on the basis of the coexistence approach.

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