Characteristic mollusc, larger foraminifera findings and environmental interpretations of the Middle Eocene Kocacay formation deposits around Ayvalica (Bayat, Corum)

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Gursoy M., GÖRMÜŞ M.

BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION, vol.162, pp.235-267, 2020 (ESCI) identifier identifier

  • Publication Type: Article / Article
  • Volume: 162
  • Publication Date: 2020
  • Doi Number: 10.19111/bulletinofmre.685461
  • Journal Name: BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION
  • Journal Indexes: Emerging Sources Citation Index (ESCI), Scopus, Directory of Open Access Journals, TR DİZİN (ULAKBİM)
  • Page Numbers: pp.235-267
  • Keywords: Cankiri-Corum Basin, Middle Eocene, Kocacay formation, Ostrea, Velates, Nummulites, CANKIRI BASIN, TECTONIC EVOLUTION, BIOSTRATIGRAPHY, CLASSIFICATION, NW, STRATIGRAPHY, NOMENCLATOR, NUMMULITES, NORTHERN, UNITS
  • Ankara University Affiliated: Yes

Abstract

Although the Cankiri-Corum Basin was studied for various purposes such as geological, stratigraphical, tectonic, coal and oil exploration, studies on fossils are limited. Especially there have not been detailed studies on molluscs and larger foraminifera The research area is located at the vicinity of Ayvalica (north of Cankiri-Corum basin). The Middle Eocene Kocacay formation, which outcrops in the Cankiri-Corum Basin, is widespread around Bayat Corum in the north of the basin, Sulakyurt Kirikkale in the west, Cicekdagi Kirsehir in the south and Sungurlu comm in the middle of the basin. The formation is composed of conglomerate, carbonated sandstone, limestone and sandy marls and also includes rich larger foraminifera and molluscs. This study mainly focuses on taxonomy and environmental interpretations of Ostrea roncaensis (Partsch in coll. Bayan, 1870) de Gregorio, 1884, Velates perversus (Gmelin, 1791) species from Mollusca and Nummulites beaumonti d'Archiac and Haime, 1853, N. aturicus Joly and Leymerie,1848, N. perforatus (de Montfort, 1808) and Assilina exponens (Sowerby, 1840) species from larger Foraminifera. In addition, considering faunal features from bottom to top Ostrea roncaensis, Velates perversus, Nummulites aturicus and Assilina exponens Abundance Biozones were identified. The age range of the Kocacay Formation is determined as Lutetian-Bartonian. Lithological and faunal contents indicate that sediments of the Kocacay formation were deposited within lagoon to nummulitic sets in a shallow marine environment.