Akademik Veri Yönetim Sistemi
Forams 2018, Edinburgh, Birleşik Krallık, 17 - 22 Haziran 2018, ss.170
Eocene aged units locating on Mesozoic old basis in the east of Malatya with angular unconformity, again Neogene old units overlap unconformably. This study was done in Gedik formation consisted of carbonated mudstone, siltstone, sandstone, carbonated pebble stone, nummulites limestone with Suludere Formation formed by Eocene old flysh type sediments that expose in Orduzu and Pinarbasi, three stratigraphic sections were measured from these formations and 65 samples were collected. As a result of micropaleontologic studies done with studied sections, it was obtained that samples contain abundant planktonic, benthic foraminifers however slightly ratio of ostracod. With detailed biostratigraphic studies done with foraminifers, ostracod genus and species such as Bairdia sp., Cytherella triestina, Cytherella sp., Krithe rutoti, Trachyleberidea stricta, Xestoleberis subglobosa, Paracypris sp., Quadracythere vermiculata, Hermanites sp. in these formations given Ipresien-Bartonian (Early-Middle Eocene) age, were defined. Defined ostracod abundance reflects epineritic and infraneritic conditions in Ipresien-Bartonian.