Microforaminiferal linings as a proxy for paleodelta nd paleosalinity analysis: Danube delta example
Вантажиться...
Дата
2017
Науковий керівник
Укладач
Редактор
Назва журналу
ISSN
E-ISSN
Назва тому
Видавець
Анотація
Microforaminiferal 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.
Опис
Ключові слова
Danube delta, microforaminiferal linings
Бібліографічний опис
Proceedings 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 .