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Nitrogen isotope variations and environmental perturbations during Cenomanian-Turonian transition in the NE Tethyan realm, Koppeh-Dagh basin | ||
Geopersia | ||
مقاله 1، دوره 7، شماره 1 - شماره پیاپی 22287825، فروردین 2017، صفحه 1-9 اصل مقاله (592.54 K) | ||
نوع مقاله: Research Paper | ||
شناسه دیجیتال (DOI): 10.22059/geope.2016.59787 | ||
نویسندگان | ||
Behnaz Kalanat1؛ Mohammad Hosein Gharaie* 1؛ Mohamad Vahidinia1؛ Hossein Vaziri-Moghaddam2؛ Akihiro Kano3 | ||
1Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, Mashhad, Iran | ||
2Department of Geology, Faculty of Science, University of Isfahan, Isfahan, Iran | ||
3Department of Environmental Changes, Faculty of Social and Cultural Studies, Kyushu University, Fukuoka, Japan | ||
چکیده | ||
The Cenomanian-Turonian Gharesu section in the east of Kopet-Dagh basin have been investigated to determine the relationship between palaeoenvironmental perturbations and nitrogen cycling across OAE2. This succession is composed of 43 m shale and marl interbedded with glauconitic sandstone and lies between Aitamir-Abderaz formations boundary. The nitrogen Isotope values fluctuate between 0‰ to +3‰ and TOC/TN ratios range from 3.5 to 20.5 in this section. The TOC/TN exhibits high ratios in the organic-rich sediments which were deposited in a low-oxygen environment because nitrogen-rich organic matter was preferably degraded in this condition. The δ15N values are also low in the organic-rich sediments which indicate a nitrogen fixation process as a consequence of greenhouse climate, enhanced productivity and expanded oxygen minimum zone during OAE2. | ||
کلیدواژهها | ||
Kopet-Dagh basin؛ environmental perturbations؛ nitrogen isotope؛ OAE2؛ TOC/TN ratio | ||
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