You are not currently logged in.
Access JSTOR through your library or other institution:
If You Use a Screen ReaderThis content is available through Read Online (Free) program, which relies on page scans. Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Endemic Foraminifera of the Late Maastrichtian from the Northern Branch of the Neotethys, NE Turkey
Nurdan İnan and Selim İnan
Vol. 55, No. 5 (2009), pp. 514-522
Published by: The Micropaleontology Project., Inc.
Stable URL: http://www.jstor.org/stable/20627993
Page Count: 9
You can always find the topics here!Topics: Maastrichtian age, Geology, Turkeys, Diameters, Canals, Evolution, Hyalin, Taxa, Micropaleontology, Micrometers
Were these topics helpful?See something inaccurate? Let us know!
Select the topics that are inaccurate.
Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Preview not available
The study of benthic foraminifera from the upper Maastrichtian intraplatform open shelflimestones in northeastern (Eastern Pontides) and central (Anatolides parts of Turkey reveals the presence of some benthic foraminiferal taxa, which appear to characterize the northern branch of the Neo-Tethys. The limestones are mainly composed of two microfacies: skeletal wackestone and bioclastic wackestone. These facies include Sirelina orduensis (Meriç and İnan), Laffitteina turcica (İnan), Cideina soezerii (Sirel), Selimina spinalis (İnan), Sivasella goekceni (Meriç and İnan) and Postomphalocyclus merici (İnan). The geographic distribution of these species seems to be limited to the southern continental margin of the northern branch of the Neo-Tethys Ocean and the southern margin of the Rhodope-Pontide Fragment. These endemic taxa are associated with Orbitoides medius, Orbitoides apiculatus, Omphalocyclus macroporus, Pseudomphalocyclus blumenthali, Simplorbites papyraceus, Hellenocyclina beotica, Siderolites calcitrapoides, Loftusia minor, Smoutina cruysi, Sirtina orbitoidiformis, Laffitteina marsicana, Cuneolina ketini, Moncharmontia sp. and Dargenionella sp. which indicate a Late Maastrichtian age.
Micropaleontology © 2009 The Micropaleontology Project., Inc.