Biostratigraphic and isotopic data on the Coreklik Member of the Hekimhan Formation (Campanian-Maastrichtian) of SE Turkey and their palaeoenvironmental significance

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dc.contributor.authorYildiz, A
dc.contributor.authorOzdemir, Z
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued1999
dc.departmentNiğde ÖHÜ
dc.description.abstractThe Coreklik Member of the Hekimhan Formation crops out in the Hekimhan (Malatya) region of SE Turkey. It includes beds that are rich in planktic and benthic foraminifera, and in calcareous nannoplankton. Eighty-eight rock samples, considered to be representative of the stratigraphic section, were examined. Seventeen species of planktic foraminifera and the Globotruncana ventricosa, Globotruncanita calcarata (Campanian), Globotruncanella havanensis, Globotruncana aegyptiaca, and Gansserina gansseri (Maastrichtian) planktic foraminiferal zones were recognised. Thirty-two calcareous nannoplankton species and the Ceratolithoides aculeus (CC-20), Quadrum sissinghii (CC-21), Quadrum trifidum (CC-22) (Campanian), Tranolithus phacelosus (CC-23) (Late Campanian-Early Maastrichtian), Reinhardites levis (CC-24), Arkhangelskiella cymbiformis (CC-25), and Lithraphidites quadratus (Early-Late Maastrichtian) zones were identified. Analyses of the sediments, the distribution of planktic and benthic foraminifera and calcareous nannoplankton, the sea-surface palaeotemperature values and palaeosalinity levels respectively calculated from delta(18)O parts per thousand (PDB) and delta(13)C parts per thousand (PDB) isotope Values obtained from globotruncanid tests, and the abundance and diversity of temperature-sensitive calcareous nannoplankton groups allowed the following conclusions to be drawn. (1) Maximum phytoplankton abundances and highest sea level were reached during the Early Campanian; (2) both the numbers of phytoplankton and the sea level began to fall from the Late Campanian onwards, reaching their lowest levels during the Late Maastrichtian; and (3) sea-surface temperature values were stable through the Campanian-Early Maastrichtian but began to fall slowly and intermittently from the end of Early Maastrichtian, reaching minimum values during the Late Maastrichtian. (C) 1999 Academic Press.
dc.identifier.doi10.1006/cres.1998.0139
dc.identifier.endpage117
dc.identifier.issn0195-6671
dc.identifier.issue1
dc.identifier.scopus2-s2.0-0033083889
dc.identifier.scopusqualityQ1
dc.identifier.startpage107
dc.identifier.urihttps://dx.doi.org/10.1006/cres.1998.0139
dc.identifier.urihttps://hdl.handle.net/11480/5815
dc.identifier.volume20
dc.identifier.wosWOS:000079744700007
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthor[0-Belirlenecek]
dc.language.isoen
dc.publisherACADEMIC PRESS LTD
dc.relation.ispartofCRETACEOUS RESEARCH
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectplanktic foraminifera
dc.subjectcalcareous nannoplankton
dc.subjectCampanian
dc.subjectMaastrichtian
dc.subjectbiostratigraphy
dc.subjectpalaeosalinity
dc.subjectpalaeotemperature
dc.subjectTurkey
dc.titleBiostratigraphic and isotopic data on the Coreklik Member of the Hekimhan Formation (Campanian-Maastrichtian) of SE Turkey and their palaeoenvironmental significance
dc.typeArticle

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