Paleontologic and stable isotopic characteristics of the upper cretaceous and middle eocene foraminifera in the southern part of the Malatya Basin, Eastern Anatolia

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dc.authorscopusid33567547000
dc.authorscopusid24464000400
dc.authorscopusid24331243400
dc.contributor.authorÇa?lar M.K.
dc.contributor.authorÖnal M.
dc.contributor.authorDarbaş G.
dc.date.accessioned2024-08-04T20:04:07Z
dc.date.available2024-08-04T20:04:07Z
dc.date.issued2012
dc.departmentİnönü Üniversitesien_US
dc.description12th International Multidisciplinary Scientific GeoConference and EXPO, SGEM 2012 -- 17 June 2012 through 23 June 2012 -- Varna -- 101586en_US
dc.description.abstractLate Cretaceous Inekpi{dotless}nari{dotless} Formation and Middle Eocene Suludere Formations occur in the southern part of the Malatya Basin. The sediments of the formations contain a rich association of planktic and benthic foraminifera. Fifty four samples were examined from the measured sections, and the foraminifera species were determined. In this study, the sea level oscillations and values of paleosalinity and palaeotemperature were calculated based on ?18O %o and ?13C %o isotope values obtained from the analysis of tests on the Heterohelix striata, Racemiguembelina fructicosa, Contusotruncana contusa, Bolivina incrassata, Subbotina eocaena, Globigerina venezuelena and Turborotalia cerroazulensis frontosa. The results of this research indicate that the sea level, water temperature, and salinity were rising and falling episodically during the Late Cretaceous and the Middle Eocene. While the sea level and water temperature were increasing, the paleosalinity values were decreasing. © SGEM2012 All Rights Reserved by the International Multidisciplinary Scientific GeoConference SGEM Published by STEF92 Technology Ltd.en_US
dc.identifier.endpage232en_US
dc.identifier.scopus2-s2.0-84890836369en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage221en_US
dc.identifier.urihttps://hdl.handle.net/11616/92365
dc.identifier.volume1en_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.relation.ispartof12th International Multidisciplinary Scientific GeoConference and EXPO - Modern Management of Mine Producing, Geology and Environmental Protection, SGEM 2012en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectForaminiferaen_US
dc.subjectLate cretaceousen_US
dc.subjectMalatya Basinen_US
dc.subjectMiddle Eoceneen_US
dc.subjectPalaeotemperatureen_US
dc.titlePaleontologic and stable isotopic characteristics of the upper cretaceous and middle eocene foraminifera in the southern part of the Malatya Basin, Eastern Anatoliaen_US
dc.typeConference Objecten_US

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