Microforaminiferal linings as a proxy for paleodelta nd paleosalinity analysis: Danube delta example

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dc.contributor.authorMudie, Petra J.
dc.contributor.authorYanko-Hombach, Valentyna V.
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктовна
dc.contributor.authorЯнко-Хомбах, Валентина Венедиктівна
dc.contributor.authorМуди, Петра Дж.
dc.contributor.authorМуді, Петра Дж.
dc.date.accessioned2017-12-05T12:25:07Z
dc.date.available2017-12-05T12:25:07Z
dc.date.issued2017
dc.description.abstractMicroforaminiferal linings are the acid-resistant, chitin-like linings of small (<150 μm) foraminiferal tests that are recovered in organic residues after palynological processing of sediments or acid treatment of rock samples. These palynomorphs are considered reliable indicators of brackish and marine paleoenvironments, and they are a proxy for foraminiferal production when carbonate preservation is reduced (Mathison and Chmura, 1995). Presence or absence of microforaminiferal (abbrev. microforam) linings is an important criterion used in palynofacies models to distinguish the transition from coastal lakes across delta front, prodelta, and shelf sub-environments.uk
dc.identifier.citationProceedings joint plenary conference and fild trip of IGCP 610 "From the Caspian to Mediterranean: environmental change and human response during the quaternary", (2013-2017) and INQUA IFG POCAS "Ponto-Caspianstratigraphy and geochronology (2017-2020) : international geoscience programme, 1-9 October 2017, Palermo , Italy / Univ. of Palermo ; ed. in chief. A. S. Gilbert ; assoc. ed. V. Yanko-Hombach . – Palermo : Palermo univ. press, 2017 .uk
dc.identifier.urihttps://dspace.onu.edu.ua/handle/123456789/11734
dc.language.isoenuk
dc.subjectDanube deltauk
dc.subjectmicroforaminiferal liningsuk
dc.titleMicroforaminiferal linings as a proxy for paleodelta nd paleosalinity analysis: Danube delta exampleuk
dc.typeArticleuk
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