Foraminifera, algae and carbonate microproblematica from the late Wuchiapingian/Dzhulfian (late Permian) of Peloponnesus (Greece)

Vachard, D; Zambetakis-Lekkas, A; Skourtsos, E; Martini, R; Zaninetti, L

dc.contributor.author	Vachard, D	en
dc.contributor.author	Zambetakis-Lekkas, A	en
dc.contributor.author	Skourtsos, E	en
dc.contributor.author	Martini, R	en
dc.contributor.author	Zaninetti, L	en
dc.date.accessioned	2014-03-01T01:53:07Z
dc.date.available	2014-03-01T01:53:07Z
dc.date.issued	2003	en
dc.identifier.issn	0035-6883	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/26859
dc.subject	late Permian	en
dc.subject	Wuchiapingian	en
dc.subject	Dzhulfian	en
dc.subject	foraminifera	en
dc.subject	algae	en
dc.subject	microproblematica	en
dc.subject	taxonomy	en
dc.subject	biostratigraphy	en
dc.subject	Greece	en
dc.subject.classification	Geology	en
dc.subject.classification	Paleontology	en
dc.subject.other	CONTINENTAL GREECE	en
dc.subject.other	AFFINITY	en
dc.subject.other	TUBIPHYTES	en
dc.subject.other	COLANIELLA	en
dc.subject.other	ACCRETION	en
dc.subject.other	POSITION	en
dc.subject.other	PANGAEA	en
dc.subject.other	RUSSIA	en
dc.subject.other	HYDRA	en
dc.subject.other	BLOCK	en
dc.title	Foraminifera, algae and carbonate microproblematica from the late Wuchiapingian/Dzhulfian (late Permian) of Peloponnesus (Greece)	en
heal.type	journalArticle	en
heal.language	English	en
heal.publicationDate	2003	en
heal.abstract	The origin of late Permian olistoliths found in the Glypia Cenozoic flysch must be seeked in regions located to the east of the Parnon Mountain and in units that were more internal to Pindos Unit, especially in the islets of Karavia in the Argolis Gulf, and the Episkopi Formation in Hydra Island, that display probably the largest outcrops of this age. The most interesting olistolith is a bioclastic grainstone. It yields about forty taxa of algae, microproblematica, smaller foraminifera and fusulinids, that are briefly described. Three markers generally not co-occurring are locally associated: Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. The age of the Paradunharula (Shindella) biozone is most probably late Wuchiapingian/Dzhulfian, although other datings have been proposed from late Capitanian to late Changhsingian. Due to this dating of the Shindella zone, the coexistence of the first Colaniella with the last Hemigordiopsis are not late Capitanian/Midian in age, but late Wuchiapingian. The similarities of the Greek microfauna with that of South China and southeastern Pamirs, are incompatible with a larger Paleotethys but support the paleogeographic reconstructions which indicate a close location of these geographic units (Pangea B).	en
heal.publisher	UNIV STUDI MILANO	en
heal.journalName	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA	en
dc.identifier.isi	ISI:000184208000014	en
dc.identifier.volume	109	en
dc.identifier.issue	2	en
dc.identifier.spage	339	en
dc.identifier.epage	358	en