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Quelques Espéces de Vaccinites et de Pironaea de L'anatolie Orientale

Necdet Karacabey
- 01 Mar 1970 - 
- Vol. 74, Iss: 74
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This article is published in Bulletin of the mineral research and exploration.The article was published on 1970-03-01 and is currently open access. It has received 6 citations till now.

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Biogeographic distribution of rudists and benthic foraminifera: An approach to Campanian-Maastrichtian palaeobiogeography of Turkey

TL;DR: In this article, the authors observed mixed siliciciclastic-carbonate sequences on three main platforms known as Rhodope-Pontide (RPP), Anatolide-Tauride (ATP), and Arabian (AP).
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Effects of ethyl pyruvate administration on female rats' pyramidal cells of cornu ammonis after brain ischemia: a stereological and histopathological study

TL;DR: The lithological and faunal succession cropping out close to the famous palaeontological locality of Bacevica (Eastern Serbia) is described along a very discontinuous and ill-exposed section and it is suggested that the wide variability of the ligamental ridge shape alone does not warrant the institution of so many species of the genus in question.
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Berriasian rudist faunas and micropalaeontology of Stramberk type carbonate exotics from the Lycian nappes, Bodrum Peninsula, southwest Turkey

TL;DR: The first record of this taxon on the southern Tethyan margin has been reported from the peri-Adriatic regions but is identified for the first time in Turkey as mentioned in this paper.
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Planktonic foraminifera and calcareous nannofossils record in the upper Campanian-Maastrichtian pelagic deposits of the Malatya Basin in the Hekimhan area (NW Malatya, eastern Anatolia)

TL;DR: In this paper, the uppermost Cretaceous (upper Campanian-Maastrichtian) pelagic successions from the Malatya Basin were studied by 688 samples, which were collected from five stratigraphic sections in the Hekimhan area.
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On the Senonianrudist-bearing sediments in Yugoslavia

Mileya Sladic-Trifunovic
- 01 Jan 1998 - 
TL;DR: In this paper, three regions with Senonian rudist-bearing sediments are distinguished in Yugoslavia (Serbia and Montenegro): eastern Serbia (rudist and other deposits from the Yugoslavian Carpatho-Balkanides), western and south-western Serbia (Rudist, and other sediment from the Inner Dinarids), and northern and southwestern Serbia, and Montenegria (Ruder and other sediments from the Yugoslavia's Outer Dinarid).