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      • Geopersia
      • Volume 4, Issue 2
      • مشاهده مورد
      •   صفحهٔ اصلی
      • نشریات انگلیسی
      • Geopersia
      • Volume 4, Issue 2
      • مشاهده مورد
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      The first report of cryptospore assemblages of Late Ordovician in Iran, Ghelli Formation, Eastern Alborz

      (ندگان)پدیدآور
      Mahmoudi, MaryamSabouri, JafarAlimohammadian, HabibMajidifard, Mahmoud Reza
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      نوع مدرک
      Text
      Research Paper
      زبان مدرک
      English
      نمایش کامل رکورد
      چکیده
      For the first time, an assemblage of cryptospores, which includes 10 species belonging to nine genera, from the Upper Ordovicianstrata, is being reported, in Iran. These cryptospore assemblages were recovered from the upper part of Ghelli Formation., from theeastern Alborz Mountain range. These peri-Gondwanan cryptospores have been classified based on their morphology (monad, truedyad, pseudodyad, true attached, and loose tetrads). The results of the present study support previous findings that there are nosignificant differences between similar-aged cryptospore assemblages of the peri-Gondwanan, Baltic provinces and other parts of theworld. Based on the presence of the chitinozoan index of the northern Gondwana (Spinachitina oulebsiri), the index acritarchs, and thepresent cryptospores, a late Hirnantian (Late Ordovician) age is proposed to the top of the Ghelli Formation. The cryptospores seem tobe transported from an adjacent land area and the lack of land-derived elements in the up-section may indicate an increased distanceoffshore.
      کلید واژگان
      Cryptospore
      Late Ordovician
      Ghelli Formation
      Eastern Alborz
      Iran

      شماره نشریه
      2
      تاریخ نشر
      2014-10-01
      1393-07-09
      ناشر
      Tehran, University of Tehran Press
      سازمان پدید آورنده
      Geoscience Research Center, Geological survey of Iran, Tehran, Iran
      Ferdowsi University of Mashhad International Campus
      Enviromental and Paleomagnetic Laboratory, Geological survey of Iran, Tehran
      Geoscience Research Center, Geological survey of Iran, Tehran, Iran

      شاپا
      2228-7817
      2228-7825
      URI
      https://dx.doi.org/10.22059/jgeope.2014.52714
      https://geopersia.ut.ac.ir/article_52714.html
      https://iranjournals.nlai.ir/handle/123456789/369693

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