Sedi̇mantoloji̇k Ve Mi̇kropaleontoloji̇k Veri̇lerle Güzelhi̇sar Çayi Kiyi Ovasinin Holosen Paleocoğrafyasi

Abstract

Human have been affected by their geographical surroundings and influenced their surroundings with the transition to settled life. The Güzelhisar river coastal plain is one of the places that have good examples of the natural environment change-human interaction from the Middle Holocene. The plain and the shoreline progressed from the interior to the present during the Holocene. This change has affected the archeological settlements such as Myrina, Tisna and Çaltılıdere in the vicinity of the plain. In order to determine the paleogeography of the plain and its effect on these settlements in the surrounding area, 35 core drillings was carried out and grain size, element, microfossil analyzes of drilling samples were made. Microfossil analyzes were used to identify coastal marshes, lagoons and marine environments. As a result of the studies made, the alluvium layers of the ovary were classified by separating 6 alluvial deposits according to the environments they reflect. According to this classification and dates, the development of the Güzelhisar coastal plain and deltas during the last 6500-7000 years (along with Holocene transgression-from the Middle Holocene) has been determined according to the changing coastal lines. Geoarchaeological interpretations of the archaeological embellishments such as Myrina, Tisna and Çaltılıdere affected by the changing natural landscape have been made. Geoarchaeological interpretations of archeological settlements such as Myrina, Tisna and Çaltılıdere affected by the changing natural landscape were made. It was reaffirmed by microfossil analysis that the settlement of Myrina's ancient city had begun 3000 thousand years ago with the existence of a narrow shallow and narrow throat that the other hill (kalabasar hill) is an island 4000 years ago today. Beside this, it was determined that Sarıkaya Depression was connected to the depression of Güzelhisar in Çaltılıdere Bay with a shallow marine channel 6000-6500 years ago. This channel, formed by Holocene transgression, was filled up and became into a land in a short time. The Çaltildere settlement in this area should also be established with the Middle Bronze Age. It is understood that the city of Tisna, on the other hand, is located on a ridge 1-2 km away from the shore even during the most intrusive period of the sea by the Holocene transgression. In the depression of Güzelhisar Creek, in the natural sediments of the coastline during the period when the sea was most intruded archaeological deposits belonging to an ancient settlement where was closer was determined.

Boynak Bi̇ri̇ki̇nti̇ Koni̇si̇ni̇n Geli̇şi̇mi̇ (Söke/Aydin): Sedi̇mantoloji̇k Ve Paleontoloji̇k Sonuçlar

“…Sedimantolojik ve paleontolojik analizlerden elde edilen sonuçlara göre sedimanlar; flüvyalkolüvyal, geçiş ve denizel olmak üzere üç ana birime ayrılmıştır (Şekil 5; Şekil 6; Şekil 7; Şekil 10). Ayrılan bu birimler Batı Anadolu Holosen stratigrafisi ile ilgili yapılmış çalışmalar ile de uyumludur (Kayan, 1991;Kayan, 1997;Kayan, 1999;Kayan, 2003;Karadaş, 2014;Kayan ve Öner, 2015;Vardar ve Öner, 2017;Vardar vd., 2017;Vardar, 2018;İlhan ve Öner, 2018 (İlhan, 2017'den düzenlenmiştir).…”

“…2010;Yıldız ve Öner, 2015; Öner ve Akbulut, 2015; Kayan ve Öner, 2015; Vardar vd., 2017; Öner ve Vardar, 2018a; Öner ve Vardar, 2018b;Vardar, 2018). Farklı süreçler altında şekillenen koninin Holosen'deki gelişimini değerlendirebilmek sedimantolojik analizlerin yanı sıra sedimanın içerisindeki kalıntıların da değerlendirilmesini gerekli kılmıştır.…”

Gedi̇z Deltasi Paleocoğrafyasinda Panaztepe Ni̇n Li̇manini Bulma Umudu

“…2003;Meriç vd. 2004;İnan 2009, Vardar ve Öner 2017, Vardar 2018. Daha önceki araştırmalarda Gediz deltası sedimanlarındaki mikrofosilleri ışığında değerlendirilmiştir (Özkan 1995;Öner ve Kayan 2005).…”

“…Sığ deniz ortamını yansıtan bu sedimanlar Homa lagünü yönünde nispeten daha derin denizel ortamı yansıtmaktadır. Mikrofosiller Batı Anadolu deltalarımızın dolgularındaki bu gibi ortamların belirlenmesinde iyi bir biyolojik göstergedir (Kayan ve Öner 2015;Vardar ve Öner 2017;Öner ve Vardar 2017;Vardar 2018). Bu yaklaşımla denizel ortama ait devam etmekte olan mikrofosil analizleri tamamlandığında ortam koşulları daha ayrıntılı olarak ele alınabilecektir.…”

Ekşi̇ Höyük Çevresi̇nde (Çal/Deni̇zli̇) Paleocoğrafya Ve Jeoarkeoloji̇ Araştirmalari

“…;Kayan ve Öner, 2013;Karadaş, 2014;Akbulut ve Öner, 2015;Kayan ve Öner, 2015; Vardar vd., 2017;Öner ve Vardar, 2018;Vardar, 2018a;Vardar, 2018b;.…”