In this study, 21 planktonic
Foraminifera species determined in the Middle Miocene sequence at the Karaisalı
region of Adana. The following biozones in Langhian-Serravalian ages are
distinguished: ? Globorotalia fohsi lobata zone, Globorotalia fohsi fohsi zone,
Globorotalia fohsi peripheroronda zone. In addition to above mentioned
planktonic Foraminifera, 13 Nannoplankton species are determined in the same
samples. The result of this study has been compared with other studies which
have been done in Trinidad, New Zeland, Libya, SW Africa and Nord Carrebean Sea
and similar results are obtained. The fossil association and property of the
sediments are also indicated that the environment is pelagic.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Ağustos 1985 |
Yayımlandığı Sayı | Yıl 1985 Cilt: 103-104 Sayı: 103-104 |
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