Mio-Pliocene basin development in the eastern part of the Cappadocian Volcanic Province (Central Anatolia, Turkey) and its implications for regional tectonics

2004 ◽  
Vol 93 (2) ◽  
pp. 314-328 ◽  
Author(s):  
Faruk Ocakoglu
2014 ◽  
Vol 280 ◽  
pp. 14-29 ◽  
Author(s):  
Elif Varol ◽  
Abidin Temel ◽  
Tekin Yürür ◽  
Alain Gourgaud ◽  
Hervé Bellon

2019 ◽  
Vol 75 (2) ◽  
pp. 268-280 ◽  
Author(s):  
Ünal Akkemik ◽  
Nevriye Neslihan Acarca Bayam

Taxodioxylon Hartig, (emended by Gothan 1905) was widely described from the late Oligocene of the European part of Turkey (Thrace) and the early Miocene of greater Turkey, Anatolia.,C,. was also described from the early Miocene of central Anatolia. The purpose of this paper is to present a more detailed extended history of these two genera up to the late Miocene (Tortonian) with new descriptions from the Galatean Volcanic Province in central Turkey. The wood identification showed the presence of two fossil species;,D,et B,and,(G,.) G,. In conclusion, the swamp and lowland warm-temperate forest composition including,and,in the Galatean Volcanic Province, continued from the early Miocene (Burdigalian) to the late Miocene (Tortonian).


IAWA Journal ◽  
2017 ◽  
Vol 38 (4) ◽  
pp. 561-570 ◽  
Author(s):  
Ünal Akkemik ◽  
Nevriye Neslihan Acarca ◽  
Murat Hatipoglu

ABSTRACTSilicified wood preserved in the Güdül fossil forest site in the Galatian Volcanic Province (GVP) near Ankara in Central Anatolia is described. The material comprises six petrified wood samples that date from early to middle Miocene. The woods have very low rays (2–5 cells high), bordered tracheidal pitting (9–10 μm), pinoid cross-field pits and very thin, unpitted, smooth walls of axial parenchyma and rays. This combination of characters indicates affinity to the fossil-genus Glyptostroboxylon. The presence of this wood genus suggests that the local environment was either riparian or wetland forest.


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