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1

Sharbazheri, Khalid, Imad Ghafor, and Qahtan Muhammed. "Biostratigraphy of the Cretaceous/Tertiary boundary in the Sirwan Valley (Sulaimani Region, Kurdistan, NE Iraq)." Geologica Carpathica 60, no. 5 (2009): 381–96. http://dx.doi.org/10.2478/v10096-009-0028-x.

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Biostratigraphy of the Cretaceous/Tertiary boundary in the Sirwan Valley (Sulaimani Region, Kurdistan, NE Iraq)The Cretaceous/Tertiary (K/T) boundary sequence, which crops out in the studied area is located within the High Folded Zone, in the Sirwan Valley, northeastern Iraq. These units mainly consist of flysch and flysch-type successions of thick clastic beds of Tanjero/Kolosh Formations. A detailed lithostratigraphic study is achieved on the outcropping uppermost part of the Upper Cretaceous successions (upper part of Tanjero Formation) and the lowermost part of the Kolosh Formation. On the
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2

Rivandi, Batool, Mohammad Vahidinia, Mehdi Nadjafi, Asadollah Mahboubi, and Abbas Sadeghi. "Biostratigraphy and Sequence Stratigraphy of Paleogene Deposits in Central Kopet-Dagh Basin (NE of Iran)." Journal of Geological Research 2013 (September 15, 2013): 1–12. http://dx.doi.org/10.1155/2013/892198.

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In this paper, the biostratigraphy and sequence stratigraphy of marine Paleogene deposits from the Kopet-Dagh basin (NE of Iran) are described. Particularly the absence of Morozovella genus is discussed. In addition, the Paleocene/Eocene boundary has been studied in detail using the record of planktonic and larger benthic foraminifera. This boundary is located probably within a thin red horizon (~10–15 cm) representing a paleosoil. Close to this boundary is located the base of the calcareous test dissolution interval, with the dominance of agglutinated benthic foraminifera and with a sudden de
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3

Carrasco, Jose, Morteza Taherpour-Khalilabad, Jafar Taheri, Maryam Ahmadi-Kooshki, and Mahmoud Majidifard. "First record of Gitolampas subrotundus (Cotteau, 1856) (Echinoidea) from the Late Paleocene of Iran." Annales g?ologiques de la Peninsule balkanique 80, no. 2 (2019): 1–11. http://dx.doi.org/10.2298/gabp1902001c.

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In this paper we present the first record of well preserved specimens of Gitolampas subrotundus (Cotteau, 1856) from the Late Paleocene of Iran (Jorasan Razavi county, northeast Iran). the detailed biostratigraphic and calcareous nannofossils investigations were carried out on a stratigraphic section in Chehel Formation. this study extends the palaeogeographical distribution of Late Paleocene echinids along the northern tethyanmargins. the investigated fossiliferous section is compared with coeval strata from other european regions.
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4

Hairapetian, Vachik, Mansoureh Ghobadi Pour, Leonid E. Popov, Peep Männik, and C. Giles Miller. "Silurian stratigraphy of Central Iran – an update." Acta Geologica Polonica 67, no. 2 (2017): 201–33. http://dx.doi.org/10.1515/agp-2017-0014.

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AbstractThe Silurian biostratigraphy, lithostratigraphy, and facies of Central Iran including the Kashmar (Boghu Mountains), Tabas (Derenjal Mountains, Ozbak-Kuh), Anarak (Pol-e Khavand) and Kerman regions is reviewed and updated. The current state of knowledge of the Silurian in the Zagros Basin, Alborz, Kopet-Dagh and Talysh regions, as well as in a few areas scattered across the Sabzevar Zone, and the Sanandaj-Sirjan terranes is also reviewed. Silurian volcanism in various parts of Iran is briefly discussed. The end of the Ordovician coincided with a widespread regression across Iran synchr
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5

Hamedi, Mir Alireza, Anthony J. Wright, Richard J. Aldridge, et al. "Cambrian to Silurian of East-Central Iran: New biostratigraphic and biogeographic data." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1997, no. 7 (1997): 412–24. http://dx.doi.org/10.1127/njgpm/1997/1997/412.

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6

Hamrsmid, Bohumil, and Fred Rögl. "Biostratigraphy of the Baba Heydar section, Iran." Senckenbergiana lethaea 80, no. 1 (2000): 39–44. http://dx.doi.org/10.1007/bf03043662.

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7

Hamedani, Ali. "New biostratigraphic data from the Paleozoic (Devonian-Carboniferous) of Isfahan, Iran." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1996, no. 5 (1996): 309–23. http://dx.doi.org/10.1127/njgpm/1996/1996/309.

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8

Hanifzadah, Reza, Koorosh Rashidi, and Mahnaz Amir Shahkarami. "Barremian-Aptian Biostratigraphy in Yazd Block, Central Iran." Open Journal of Geology 05, no. 06 (2015): 405–21. http://dx.doi.org/10.4236/ojg.2015.56039.

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9

Afghah, Massih, and Arash Shaabanpour Haghighi. "Aptian biostratigraphy in South Zagros Basin, southwest Iran." Geoscience Frontiers 5, no. 2 (2014): 277–88. http://dx.doi.org/10.1016/j.gsf.2013.07.001.

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10

MOGHADDAM, I. M., and H. RASHNOW. "Formation at the Southtern Flank of Mish Anticline, Izeh Zone, SW Iran." Anuário do Instituto de Geociências - UFRJ 41, no. 2 (2018): 623–35. http://dx.doi.org/10.11137/2018_2_623_635.

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11

Wilmsen, Markus, Marisa Storm, Franz Theodor Fürsich, and Mahmoud Reza Majidifard. "Upper Albian and Cenomanian (Cretaceous) ammonites from the Debarsu Formation (Yazd Block, Central Iran)." Acta Geologica Polonica 63, no. 4 (2013): 489–513. http://dx.doi.org/10.2478/agp-2013-0021.

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ABSTRACT Wilmsen, M., Storm, M., Fürsich, F.T. and Majidifard, M.R. 2013. Upper Albian and Cenomanian (Cretaceous) ammonites from the Debarsu Formation (Yazd Block, Central Iran). Acta Geologica Polonica, 63 (4), 489-513. Warszawa. New ammonite faunas consisting of 13 taxa provide the first reliable biostratigraphic dating of the Debarsu Formation of the Yazd Block, west-central Iran, indicating several levels in the Upper Albian and Lower Cenomanian, while a foraminiferal assemblage places the top of the Formation in the Middle Turonian. Among the identified ammonite taxa, Acompsoceras renevi
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12

Kallanxhi, Mădălina-Elena, Mostafa Falahatgar, Mojtaba Javidan, Mehdi Sarfi, and Tahere Parvizi. "Calcareous nannofossils- and ammonites-based biostratigraphy of the Baghamshah Formation (Central Iran Basin, Iran)." Studia Universitatis Babes-Bolyai, Geologia 60, no. 1 (2016): 29–42. http://dx.doi.org/10.5038/1937-8602.60.1.1288.

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13

Niazi, Mohsen, Mohammad Vahidinia, Sreepat Jain, and Mohamad Hosein Mahmudy Gharaie. "The Campanian-Maastrichtian planktonic foraminifera of the Kopet-Dagh Basin (NE Iran): bioevents and biostratigraphy." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 294, no. 1 (2019): 103–29. http://dx.doi.org/10.1127/njgpa/2019/0849.

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The Campanian–Maastrichtian Abtalkh Formation of the Kopet-Dagh Basin (NE Iran) has been studied for biostratigraphic purposes. The present study integrates results from three sections within the basin: Maraveh-Tapeh (Western Kopet-Dagh), Abtalkh Village and Qareh Sou (Eastern Kopet-Dagh). The biostratigraphic distribution of 59 species of planktonic foraminifera has been used to characterize the following zones: Globotruncanita elevata PRZ, Contusotruncana plummerae IZ, Globotruncana falsostuarti IZ, Radotruncana calcarata TRZ, Globotruncanella havanensis IZ, Globotruncana aegyptiaca IZ, Gans
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14

Allameh, Mohsen, and Reihane Rezayi Yazdi Nejad. "Late Cretaceous Biostratigraphy Planktonic Foraminifera of the Farokhi Formation, Iran." Open Journal of Geology 07, no. 03 (2017): 320–34. http://dx.doi.org/10.4236/ojg.2017.73022.

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15

Afghah, Massih, and Hamid R. Fadaei. "Biostratigraphy of Cenomanian succession in Zagros area (southwest of Iran)." Geosciences Journal 19, no. 2 (2014): 257–71. http://dx.doi.org/10.1007/s12303-014-0045-3.

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16

Brasier, Martin D., Mordeckai Magaritz, Richard Corfield, et al. "The carbon- and oxygen-isotope record of the Precambrian–Cambrian boundary interval in China and Iran and their correlation." Geological Magazine 127, no. 4 (1990): 319–32. http://dx.doi.org/10.1017/s0016756800014886.

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AbstractThe fossiliferous section at Meishucun of Yunnan, China, is a candidate stratotype section for the Precambrian–Cambrian boundary. Early diagenetic dolomites and phosphorites have been sampled across the boundary interval here, and in the correlated section at Maidiping in Sichuanand Valiabad in Iran, for comparison of their carbon and oxygen isotopes. This is the first such study that is calibrated by biostratigraphy in the interval from the earliest (pre-Tommotian) skeletal fossils to trilobites. Although negative oxygen isotopes indicate a diagenetic signal in the Zhongyicun Member a
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17

Turner, S., and G. C. Young. "Thelodont scales from the Middle-Late Devonian Aztec Siltstone, southern Victoria Land, Antarctica." Antarctic Science 4, no. 1 (1992): 89–105. http://dx.doi.org/10.1017/s0954102092000142.

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A new fossil agnathan, Turinia antarctica sp. nov., based on numerous isolated scales, comes from the lower fish-bearing beds of the Aztec Siltstone. Scales from moraine at Mount Suess, originally described as selachian or psammosteid heterostracan, are referred to the new species which shows close affinity with T. gondwana from Bolivia and T. cf. hutkensis from Iran. Reassessment of the biostratigraphy of Middle Devonian turiniid scales suggests that the lower part of the Aztec Siltstone may be of Eifelian age.
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18

Babazadeh, Seyed Ahmad, Francis Robaszynski, and Marie Denis Courme. "New biostratigraphic data from Cretaceous planktic foraminifera in Sahlabad province, eastern Iran." Geobios 40, no. 4 (2007): 445–54. http://dx.doi.org/10.1016/j.geobios.2006.08.002.

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19

SHIRAZI, Mahnaz Parvaneh Nejad, Pegah SHAMS, and Mohammad BAHRAMI. "Biostratigraphy and Paleoecology of Maastrichtian Sediments in the Zagros Basin, Iran." Acta Geologica Sinica - English Edition 87, no. 5 (2013): 1387–95. http://dx.doi.org/10.1111/1755-6724.12136.

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20

Holakouee, Zohreh, Iraj Maghfouri Moghaddam, Mehdi Yazdi, and Bizhan Yousefi yeganeh. "Biostratigraphy and Microfacies of Qom Formation in Urumieh – Dokhtar Zone, Iran." International Journal of Engineering and Technology 10, no. 4 (2018): 1052–66. http://dx.doi.org/10.21817/ijet/2018/v10i4/181004216.

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21

Al-jubori, Falah H. Khalaf, Akram K. Youkhana, Srood F. Naqshabandi, and Dyana A. Bayz. "BIOSTRATIGRAPHIC CORRELATION OF PALEOZOIC ROCKS IN NORTHERN AND WESTREN IRAQ." International Journal of Research -GRANTHAALAYAH 8, no. 3 (2020): 315–23. http://dx.doi.org/10.29121/granthaalayah.v8.i3.2020.163.

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The Paleozoic rocks outcropped in northern Iraq (Ora, Chia Zairi section) are biostratigraphically investigated for their microfossils content. Benthonic foraminifera and algal genera characterize the upper part of the section while palynomorphs (Miospores & Acritarchs) dominated the lower part the section which is consist of clastic sediments. The study also include the stratigraphic succession of the section and its correlation to the subsurface sections penetrated in oil and water wells drilled in the western desert of Iraq in order to determine the regional distribution of the economic
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22

Lawa, Fadhil. "BIOSTRATIGRAPHIC ANALYSIS OF THE OLIGOCENE-EARLY MIOCENE SUCCESSIONS FROM SULAIMANI AREA, KURDISTAN REGION, IRAQ." Iraqi Geological Journal 53, no. 2D (2020): 19–41. http://dx.doi.org/10.46717/igj.53.2d.2ms-2020-10-24.

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Three sections (Darzila, Hazar Kani and Basara) of the Oligocene –Early Miocene successions from Sulaimani area, Kurdistan region-NE Iraq, were measured and studied in order to interpret the biostratigraphic zonations at the Low and High Folded Thrust zones boundary, Low Folded Thrust zone, which are integrated with strontium stratigraphic dating. Accordingly, five biozones have been identified and they are:1- Nummulites vascus- Nummulites intermedius- Nummulites fichteli Assemblage Zone (Shallow Benthic Zone, SBZ 22A) represents the Rupelian age, 2- Lepidocyclina dilatata- Nummulites vascus -
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23

Honarmand, Atusa, Mohammad Vahidinia, Mohammad Hosein Mahmudy Gharaie, and Meysam Shafiee Ardestani. "Biostratigraphy of the Gurpi Formation (Zagros Basin, western Iran) based on planktonic foraminifera." Geologica Balcanica 49, no. 1 (2020): 53–66. http://dx.doi.org/10.52321/geolbalc.49.1.53.

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Micropalaeontological and biostratigraphic studies of the Gurpi Formation were carried out at the Kuhe-Surgah section (Zagros Basin, Iran). In this research, 62 species of planktonic foraminifera, belonging to 23 genera, were recognized and used to describe the following zones: 1) Contusotruncana plummerae Interval Zone; 2) Radotruncana calcarata Total Range Zone; 3) Globotruncanella havanensis Partial Range Zone; 4) Globotruncana aegyptiaca Interval Zone; 5) Gansserina gansseri Interval Zone; 6) Contusotruncana contusa Interval Zone; 7) Abathomphalus mayaroensis Interval Zone; 8) Pseudoguembe
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24

Hadi, Mehdi, Amir Salahi, Yaghub Nasiri, and Hossein Mosaddegh. "SOKOLOWIA HORIZON OF THE ZIARAT FORMATION (EASTERN ALBORZ, IRAN): BIOSTRATIGRAPHIC AND PALEOGEOGRAPHIC IMPLICATIONS." Acta Palaeontologica Romaniae, no. 15 (2) (July 14, 2019): 15–27. http://dx.doi.org/10.35463/j.apr.2019.02.02.

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The present study deals with molluscan accumulations of the Sokolowia horizon, which is a key-bed in the middle Eocene of the Kalateh section (Ziarat Formation, Eastern Alborz, Iran). The age of this “key horizon” is at-tributed to Bartonian based on presence of larger benthic foraminifera species such as Nummulites lyelli (D'Archiac & Haime), Orbitoclypeus zitteli (Checchia-Rispoli) and Asterocyclina stella stella (Gümbel) immediately below it. The paleogeographic distribution of Sokolowia occurrence from Tarim Basin in eastern Central Asia to the Transylvanian Basin in southeastern Europ
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25

Bordbar, Azadeh, Fatemeh Hadavi, Abbas Ghaderi, and Marziyeh Notghi Moghaddam. "Biostratigraphy of Baghamshah Formation based on calcareous nannofossils in the Southwest Tabas, Iran." Revista Brasileira de Paleontologia 24, no. 3 (2021): 165–78. http://dx.doi.org/10.4072/rbp.2021.3.01.

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The Tabas Block is part of the Central Iran microcontinent, located between the Lut Block in the East and the Yazd Block in the West. The Baghamshah Formation is the second lithostratigraphic unit from the sedimentary cycle of the Magu Group and the Baghamshah Subgroup in the Jurassic of Tabas Block. This formation is conformably underlaid with the grey pisoidal limestones of the Parvadeh Formation and overlaid with the Pectinid limestones of the Kamar-e-Mehdi Formation (Esfandiar Subgroup). In this research, the biostratigraphy of the Baghamshah Formation in the Rizu and Kamar-e-Mehdi section
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26

Abawi, Tarik S., and Rezan A. Maroof. "Planktonic foraminifera and biostratigraphy of the Oligocene Ibrahim Formation, Sinjar area, northwestern Iraq." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1988, no. 7 (1988): 391–402. http://dx.doi.org/10.1127/njgpm/1988/1988/391.

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27

Abawi, Tarik S., and Rezan A. Maroof. "Planktonic foraminiferal biostratigraphy of the Serikagni Formation (Oligocene/Miocene), Sinjar area, NW Iraq." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1992, no. 12 (1993): 709–20. http://dx.doi.org/10.1127/njgpm/1992/1993/709.

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28

Fazli, Leila, and Saeedeh Senemari. "Calcareous nannofossil biostratigraphy of the Eocene of the Zagros Basin in Iran." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 287, no. 2 (2018): 143–51. http://dx.doi.org/10.1127/njgpa/2018/0709.

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29

Mahanipour, A., M. Eftekhari, and M. Dastanpour. "Barremian-Aptian Calcareous Nannofossil Biostratigraphy in Zagros Basin (west Iran), Tethyan Realm." Stratigraphy and Geological Correlation 26, no. 7 (2018): 783–97. http://dx.doi.org/10.1134/s0869593818070031.

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30

Najafpour, Amineh, Azam Mahanipour, and Mohammad Dastanpour. "Calcareous nannofossil biostratigraphy of Late Campanian–Early Maastrichtian sediments in southwest Iran." Arabian Journal of Geosciences 8, no. 8 (2014): 6037–46. http://dx.doi.org/10.1007/s12517-014-1644-z.

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31

Vaziri, Mohammadreza, and Azam Mahanipour. "Biostratigraphy and paleoecology of Qum Formation (Oligo-Miocene) of Kashan area, Iran." Anuário do Instituto de Geociências 29, no. 1 (2006): 366. http://dx.doi.org/10.11137/2006_1_366-366.

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32

Taherpour-Khalil-Abad, Morteza, Jafar Taheri, Mahmoud Rezamajidifard, Zinat Hassanzadeh, and Ivana Carevic. "Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canerot, 1979 from the late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions." Annales g?ologiques de la Peninsule balkanique 80, no. 2 (2019): 39–51. http://dx.doi.org/10.2298/gabp1902039t.

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during micropaleontological investigations on the lower cretaceous successions of the tirgan Formation in Kopet-dagh sedimentary basin, some new achievements are yielded. in this regards, the first occurrence of Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar in close association with Torremiroella hispanica Brun & canerot is reported for the first time from the upper Barremian of Kopet-dagh sedimentary basin (ne iran). the biostratigraphic investigations were carried out on a 197.5 m thick gelian stratigraphic succession cropping out along the tirgan Formation located 35 km sou
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33

Gliwa, Jana, Abbas Ghaderi, Lucyna Leda, et al. "Aras Valley (northwest Iran): high-resolution stratigraphy of a continuous central Tethyan Permian–Triassic boundary section." Fossil Record 23, no. 1 (2020): 33–69. http://dx.doi.org/10.5194/fr-23-33-2020.

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Abstract. The Permian–Triassic boundary section in the Aras Valley in NW Iran is investigated with respect to carbonate microfacies, biostratigraphy (particularly conodonts, nautiloids, and ammonoids), chemostratigraphy (carbon isotopes), and environmental setting. Correlation of the data allows the establishment of a high-resolution stratigraphy based on conodonts (with four Wuchiapingian, 10 Changhsingian, and three Griesbachian zones), ammonoids (with nine Changhsingian zones), and carbon isotopes; it forms the base for the reconstruction of the environmental changes before and after the en
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34

Cheng-Yuan, Wang, Scott M. Ritter, and David L. Clark. "The Sweetognathus complex in the Permian of China: implications for evolution and homeomorphy." Journal of Paleontology 61, no. 5 (1987): 1047–57. http://dx.doi.org/10.1017/s0022336000029395.

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The well-exposed and fossiliferous Permian carbonates in China have yielded Early and Late Permian species of the Sweetognathus complex that permit worldwide stratigraphic evaluation of members of the group. The sporadic appearance of species of Sweetognathus and related genera throughout the Permian in western North America and Iran, in particular, may represent iterative evolution and homeomorphy. The pectiniform element morphologies of the several species are interpreted as most important for evolutionary studies and document a partial Permian biostratigraphy in China that aids in the inter
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35

Ghazi, A. M., E. A. Pessagno, A. A. Hassanipak, S. M. Kariminia, R. A. Duncan, and H. A. Babaie. "Biostratigraphic zonation and 40Ar–39Ar ages for the Neotethyan Khoy ophiolite of NW Iran." Palaeogeography, Palaeoclimatology, Palaeoecology 193, no. 2 (2003): 311–23. http://dx.doi.org/10.1016/s0031-0182(03)00234-7.

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36

Shepherd, Hannah M. E., George D. Stanley, and Fatemeh Amirhassankhani. "Norian to Rhaetian scleractinian corals in the Ferdows Patch Reef (Nayband Formation, east central Iran)." Journal of Paleontology 86, no. 5 (2012): 801–12. http://dx.doi.org/10.1666/12-001.1.

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The Nayband Formation is one of the best known sedimentary units in central Iran. The type section consists of a thick succession of shale, siltstone, reef limestone and sandstone that is subdivided into five distinct members: Gelkan, Bidestan, Hoz-e-Sheykh, Howz-e- Khan and Qadir. Abundant and well-preserved framework-building scleractinian corals are included among the macrofossils of the Nayband Formation; these corals characterize the formation and are the subject of this study. The Hassan-Abad section, located in northeast Iran in Lute Block (northwest of Ferdows city), was chosen for det
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37

Asgharian Rostami, Masoud, Mohammad Vahidinia, Ebrahim Ghasemi-Nejad, and Abbas Sadeghi. "Biostratigraphy and Mass Extinction Pattern across the Cretaceous/Paleogene Boundary, Northern Alborz, Iran." Open Journal of Geology 03, no. 01 (2013): 33–38. http://dx.doi.org/10.4236/ojg.2013.31005.

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Khavari Khorassani, Manooseh P., Fatemeh Hadavi, Ebrahim Ghasemi-Nejad, and Reza Mousavi-Harami. "Biostratigraphy and Paleoecological Study of Pabdeh Formation in Interior Fars, Zagros Basin, Iran." Open Journal of Geology 04, no. 11 (2014): 571–81. http://dx.doi.org/10.4236/ojg.2014.411042.

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39

Ghavidel-syooki, Mohammed, and Theresa Winchester-Seeto. "Biostratigraphy and palaeogeography of Late Ordovician chitinozoans from the northeastern Alborz Range, Iran." Review of Palaeobotany and Palynology 118, no. 1-4 (2002): 77–99. http://dx.doi.org/10.1016/s0034-6667(01)00108-7.

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40

Nadaf, Reza, Mohammad Vahidinia, Mehdi Nadjafi, and Mohamad Hosein Mahmudy-Gharaie. "Biostratigraphy of Eocene settings in the Binalood zone (northeastern Iran) based on foraminifera." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 288, no. 3 (2018): 283–98. http://dx.doi.org/10.1127/njgpa/2018/0742.

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41

Daneshian, Jahanbakhsh, and Leila Ramezani Dana. "Foraminiferal biostratigraphy of the Miocene Qom Formation, northwest of the Qom, Central Iran." Frontiers of Earth Science 12, no. 1 (2017): 237–51. http://dx.doi.org/10.1007/s11707-017-0669-5.

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42

Bagi, Hoseinali, and Kemal Tasli. "Paleoenvironmental analysis and biostratigraphy of the Upper Jurassic Esfandiar Formation (East–Central Iran)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 243, no. 1 (2007): 101–11. http://dx.doi.org/10.1127/0077-7749/2007/0243-0101.

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43

Bernor, Raymond L. "Mammalian biostratigraphy, geochronology, and zoogeographic relationships of the Late Miocene Maragheh fauna, Iran." Journal of Vertebrate Paleontology 6, no. 1 (1986): 76–95. http://dx.doi.org/10.1080/02724634.1986.10011600.

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44

Valizadeh Kakhki, Bahareh, Seyed Mahmood Hosseini-Nezhad, and Mohammad Vahidinia. "Conodont biostratigraphy of late Devonian deposits in the Shirband section (Damghan, NE Iran)." Arabian Journal of Geosciences 8, no. 9 (2014): 7229–43. http://dx.doi.org/10.1007/s12517-014-1683-5.

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45

Esmaeilbeig, Mohammad Reza. "Biostratigraphy of the Gurpi Formation (Santonian–Maastrictian) by using Globotruncanidae, Zagros Mountains, Iran." Carbonates and Evaporites 33, no. 1 (2017): 133–42. http://dx.doi.org/10.1007/s13146-017-0342-9.

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46

Habibi, Tahereh, Carlo Corradini, and Mehdi Yazdi. "Conodont biostratigraphy of the Upper Devonian–Lower Carboniferous Shahmirzad section, central Alborz, Iran." Geobios 41, no. 6 (2008): 763–77. http://dx.doi.org/10.1016/j.geobios.2008.04.002.

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47

Babazadeh, S. A., and M. Soltani Najafabadi. "Biostratigraphy of Eocene Sedimentary Rocks Based on Alveolina in East Lut Block, Iran." Kharazmi Journal of Earth Sciences 1, no. 1 (2015): 1–20. http://dx.doi.org/10.29252/gnf.1.1.1.

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Hadi, Mehdi, Mohamad Vahidinia, and Nasrollah Abbassi. "Ilerdian–cuisian Alveolinids from the Western Alborz and Eastern Iran Zones: Systematic and Biostratigraphic Implications." Journal of Foraminiferal Research 49, no. 2 (2019): 141–62. http://dx.doi.org/10.2113/gsjfr.49.2.141.

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Abstract:
Abstract The alveolinid taxa, found in three stratigraphic sections of Eocene shallow-marine successions in the western Alborz (Baghdareh and Gheynarjeh sections) and eastern Iran (Chenesht section) regions, have been studied to determine their systematics and biostratigraphy for the first time. The rich alveolinid assemblages in these regions are correlated with coeval faunas (in shallow benthic zones) of the Tethyan province. The 29 species of alveolinids identified include: Glomalveolina lepidula, Alveolina ellipsoidalis, A. moussoulensis, A. subpyrenaica, A. aff. sakaraensis, A. tumida, A.
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Zandkarimi, Keyvan, Daniel Vachard, Pedro Cózar, Bahram Najafian, Bahauddin Hamdi, and Hossein Mosaddegh. "New data on the Late Viséan–Late Serpukhovian foraminifers of northern Alborz, Iran (biostratigraphic implications)." Revue de Micropaléontologie 60, no. 2 (2017): 257–78. http://dx.doi.org/10.1016/j.revmic.2016.11.003.

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Daneshian, Jahanbakhsh, and Leila Ramezani Dana. "Early Miocene benthic foraminifera and biostratigraphy of the Qom Formation, Deh Namak, Central Iran." Journal of Asian Earth Sciences 29, no. 5-6 (2007): 844–58. http://dx.doi.org/10.1016/j.jseaes.2006.06.003.

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