Publication:
Palynostratigraphy and Vegetation Characteristics of Neogene Continental Deposits Interbedded with the Cappadocia Ignimbrites (Central Anatolia, Turkey)

dc.authorscopusid22137192000
dc.authorscopusid6603548880
dc.contributor.authorYavuz-Işık, N.
dc.contributor.authorToprak, V.
dc.date.accessioned2020-06-21T14:46:34Z
dc.date.available2020-06-21T14:46:34Z
dc.date.issued2010
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Yavuz-Işık] Nurdan, Department of Civil Engineering, Ondokuz Mayis Üniversitesi, Samsun, Turkey; [Toprak] Vedat, Department of Geological Engineering, Middle East Technical University (METU), Ankara, Ankara, Turkeyen_US
dc.description.abstractA palynological analysis of the Late Miocene and Early Pliocene successions of the Cappadocian Volcanic Province (Central Anatolia, Turkey) has been carried out with the aim of reconstructing the palaeovegetation and palaeoclimatic conditions. The samples are collected from outcrop sections from three different localities (A: Akdaǧ, B: Bayramhaci{dotless}li{dotless} and G: Güzelöz). The pollen spectra reveals the existence of a steppe vegetation dominated by Amaranthaceae-Chenopodiaceae and Artemisia, typical of present day arid and semi-arid continental areas (i. e. Middle East), and Asteraceae Asteroideae in the A section (Late Miocene) developed in arid climatic conditions. The flora of the G (Early Pliocene) and lower part of the B (Late Miocene) sections reflects steppes on which Asteraceae Asteroideae was dominant. This flora also indicates arid conditions. The development of trees in the upper part of the B section was possibly related to local paleoenvironmental conditions rather than a climatic change. This study provides the first palynological data to reveal the presence of an Amaranthaceae-Chenopodiaceae and Artemisia steppe already during the Late Miocene in Turkey. © 2009 Springer-Verlag.en_US
dc.identifier.doi10.1007/s00531-009-0486-5
dc.identifier.endpage1897en_US
dc.identifier.issn1437-3254
dc.identifier.issn1437-3262
dc.identifier.issue8en_US
dc.identifier.scopus2-s2.0-78349304435
dc.identifier.scopusqualityQ2
dc.identifier.startpage1887en_US
dc.identifier.urihttps://doi.org/10.1007/s00531-009-0486-5
dc.identifier.volume99en_US
dc.identifier.wosWOS:000285070100013
dc.identifier.wosqualityQ3
dc.language.isoenen_US
dc.publisherSpringer Verlag service@springer.deen_US
dc.relation.ispartofInternational Journal of Earth Sciencesen_US
dc.relation.journalInternational Journal of Earth Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectCappadociaen_US
dc.subjectNeogeneen_US
dc.subjectPalaeoclimateen_US
dc.subjectPalaeovegetationen_US
dc.subjectPalynostratigraphyen_US
dc.titlePalynostratigraphy and Vegetation Characteristics of Neogene Continental Deposits Interbedded with the Cappadocia Ignimbrites (Central Anatolia, Turkey)en_US
dc.typeArticleen_US
dspace.entity.typePublication

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