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Demir Altiner

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Articles

Coupled carbonate-shale thallium isotopes reveal the evolution of deep-marine anoxia during the end-Permian mass extinction

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By Chirag Manchanda, Ying Han, Thilo Hagendorff, Bob Yirka, Menghan Li, Andrew Siciliano Verified, Chadlin M. Ostrander, Sune G. Nielsen, Tapan Mukerji, Stephen E. Grasby, Demir Altiner, Daniel J. Lehrmann, David Bond, Meiyi Yu, Diego Fernandez Verified, Christopher Anderson, Jonathan Payne, Yanan Shen, Susannah C. Herz
| Science Magazine Verified
Reference #1 Abstract INTRODUCTION RESULTS DISCUSSION MATERIALS AND METHODS Acknowledgments Supplementary Materials REFERENCES eLetters (0) Information & Authors Metrics & Citations View Options References Figures Tables Media Share This article has 0 eLetter . Abstract Ocean anoxia played a key role in the end-Permian mass extinction, the most severe biotic crisis in Earth’s history, yet reconstructions of oxygenation through this event have lacked a focus on deep-water oxygen loss.
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Testing of Permian – Lower Triassic stratigraphic data in a half-graben/tilt-block system: evidence for the initial rifting phase in Antalya Nappes1

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By Demir Altiner
| nrcresearchpress.com
bMiddle East Technical University, Department of Geological Engineering, 06800 Ankara, Turkey. Received June 28, 2018. Accepted November 5, 2018. Ahr WM. 1973. The carbonate ramp: an alternative to the shelf model. Gulf Coast Association of Geological Societies Transactions 23: 221-225 Google Scholar. Altiner, D. 1981. Recherches stratigraphiques et micropaléontologiques dans le Taurus oriental au NW de Pınarbaşı. Unpublished Ph.D. thesis, University of Geneva, 450 p. Google Scholar Altiner, D. 1984.
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