2021
DOI: 10.1111/1755-6724.14763
|View full text |Cite
|
Sign up to set email alerts
|

Abstract: The Sarvak Formation is a carbonate sequence of Late Albian-Early Turonian age in Zagros Basin in Iran. In this investigation, the Sarvak Formation at the Pyun Anticline section (Izeh Zone) has been studied. It consists of 797 m thick limestone which overlies the Kazhdumi Formation conformably and underlies the Gurpi Formation unconformably at the Pyun Anticline. A very rich fossil association (85 genera and 132 species) characterizes the Pyun section. Based on the stratigraphic distribution of diagnosed foram… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

6
13
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
5

Relationship

1
4

Authors

Journals

citations
Cited by 10 publications
(19 citation statements)
references
References 68 publications
6
13
0
Order By: Relevance
“…However, the number of whorls and the structure of chambers, chamberlets, septula and preseptal passage are recognized for observed alveolinids in the Sarvak Formation. Moreover, the structural elements of investigated alveolinids compared with several previous works that consisted of the various sections (sagittal, axial and tangential type; e.g., Calonge et al, 2002; Caus et al, 2009; Dousti Mohajer, Afghah, Dehghanian, & Sheikh Zakariaii, 2021, Dousti Mohajer, Afghah, Dehghanian, & Abyat, 2021; Ghanem & Kuss, 2013; Ghanem et al, 2012). The structural form of chamber and chamberlets coincided with the previous works that were recorded as common alveolinids in the Middle East (e.g., Afghah & Fadaei, 2015; Afghah, Yousefzadeh, & Shirdel, 2014; Dousti Mohajer, Afghah, Dehghanian, & Abyat, 2021; Dousti Mohajer, Afghah, Dehghanian, & Sheikh Zakariaii, 2021; Dousti Mohajer et al, 2022; Ghanem et al, 2012; Ghanem & Kuss, 2013).…”
Section: Alveolinid Identificationmentioning
confidence: 99%
See 4 more Smart Citations
“…However, the number of whorls and the structure of chambers, chamberlets, septula and preseptal passage are recognized for observed alveolinids in the Sarvak Formation. Moreover, the structural elements of investigated alveolinids compared with several previous works that consisted of the various sections (sagittal, axial and tangential type; e.g., Calonge et al, 2002; Caus et al, 2009; Dousti Mohajer, Afghah, Dehghanian, & Sheikh Zakariaii, 2021, Dousti Mohajer, Afghah, Dehghanian, & Abyat, 2021; Ghanem & Kuss, 2013; Ghanem et al, 2012). The structural form of chamber and chamberlets coincided with the previous works that were recorded as common alveolinids in the Middle East (e.g., Afghah & Fadaei, 2015; Afghah, Yousefzadeh, & Shirdel, 2014; Dousti Mohajer, Afghah, Dehghanian, & Abyat, 2021; Dousti Mohajer, Afghah, Dehghanian, & Sheikh Zakariaii, 2021; Dousti Mohajer et al, 2022; Ghanem et al, 2012; Ghanem & Kuss, 2013).…”
Section: Alveolinid Identificationmentioning
confidence: 99%
“…Also, in other identification of foraminifers, the embryonic zones are so significant for the determination of the species, but several previous works are represented without embryonic zones of the distinct species that are mentionable to Orbitolinidae with semi‐preserved samples (e.g., Baud, Cherchi, & Schroeder, 1994). Therefore, the adductions on alveolinid identification (Dousti Mohajer, Afghah, Dehghanian, & Sheikh Zakariaii, 2021; Dousti Mohajer, Afghah, Dehghanian, & Abyat, 2021) are completely unacceptable. Moreover, the essence of biostratigraphy is established by corrected identification.…”
Section: Alveolinid Identificationmentioning
confidence: 99%
See 3 more Smart Citations