Ostracods and bivalves from an Upper Pleistocene (Tyrrhenian) marine terrace near Altinova (İzmit Province, Turkey)

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dc.contributor.authorSchneider, Simon
dc.contributor.authorWitt, Wolfgang
dc.contributor.authorYigitbaş, Erdinç
dc.date.accessioned2025-01-27T19:06:14Z
dc.date.available2025-01-27T19:06:14Z
dc.date.issued2005
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractOstracods and bivalves from two samples collected near Altinova (İzmit Province, Turkey) are studied. The sample sediment consists of coarse to fine grained sands and comes from the oldest part of the Marmara Formation, a succession of Late Pleistocene marine terraces. The composition of the ostracod fauna corroborates the Tyrrhenian radiometric age of the succession. The ostracod associations are composed predominantly of heavily calcified and ornamented genera, which indicate a nearshore, inner neritic depositional environment. The bivalve assemblages, containing byssate and cementing epifaunal and infaunal taxa, suggest a combination of rocky coastal environment and shallow marine clastic deposits. Faunal composition and shell dimensions of the bivalves are indicative of reduced salinity.
dc.identifier.endpage114
dc.identifier.issn1612-412X
dc.identifier.scopus2-s2.0-33645233277
dc.identifier.scopusqualityN/A
dc.identifier.startpage87
dc.identifier.urihttps://hdl.handle.net/20.500.12428/14197
dc.identifier.volume45
dc.indekslendigikaynakScopus
dc.language.isoen
dc.relation.ispartofZitteliana Reihe A: Mitteilungen der Bayerischen Staatssammlung fur Palaontologie und Geologie
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_Scopus_20250125
dc.subjectBivalves; Ostracods; Pleistocene; Turkey; Tyrrhenian
dc.titleOstracods and bivalves from an Upper Pleistocene (Tyrrhenian) marine terrace near Altinova (İzmit Province, Turkey)
dc.typeArticle

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