2017
DOI: 10.1007/s12517-016-2787-x
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Salpingoporella (dasycladalean algae) species from the Lower Cretaceous carbonate facies of Kopet Dagh basin (NE Iran)

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Cited by 4 publications
(4 citation statements)
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“…The last occurrence datum (LOD) of Acicularia sp., Bakalovella elitzae Bakalova, 1971, Clypeina gigantean Sokač, 1996 and Terquimella sp. have also been recorded in this boundary that confirms the end of the Barremian (Dragastan, 1999;Granier, 2001;Mancinelli and Chiocchini, 2006;Taherpour Khalil Abad, 2017). The Lower/Upper Aptian boundary is marcked by the FOD of Mesorbitolina parva Douglass, 1960 and LOD of Praeorbitolina cormyi Schroeder, 1964and Palorbitolina lenticularis Blumenbach, 1805(Schroeder et al, 2010 and recorded in the basal layers of the unit 5.…”
Section: Biostratigraphy Of Section No1mentioning
confidence: 61%
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“…The last occurrence datum (LOD) of Acicularia sp., Bakalovella elitzae Bakalova, 1971, Clypeina gigantean Sokač, 1996 and Terquimella sp. have also been recorded in this boundary that confirms the end of the Barremian (Dragastan, 1999;Granier, 2001;Mancinelli and Chiocchini, 2006;Taherpour Khalil Abad, 2017). The Lower/Upper Aptian boundary is marcked by the FOD of Mesorbitolina parva Douglass, 1960 and LOD of Praeorbitolina cormyi Schroeder, 1964and Palorbitolina lenticularis Blumenbach, 1805(Schroeder et al, 2010 and recorded in the basal layers of the unit 5.…”
Section: Biostratigraphy Of Section No1mentioning
confidence: 61%
“…while there are many sections with rich fossil algae have reported from CEIM (Bucur et al, 2003;Bucur and Săsăran, 2005b;Bucur et al, 2012;Bucur et al, 2013;Hanifzadah et al, 2015;Taherpour Khalil Abad, 2017;Bucur et al, 2018).…”
Section: Microfacies Analyzes and Sedimentary Modelmentioning
confidence: 99%
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“…it was formed on hercynian metamorphosed basement at the Sw margin of the turan platform and is composed of about 10 km of mostly conformably Mesozoic and tertiary sediments (mostly carbonates) (taherpour-Khalil-aBad et al 2013). these sediments were deposited in a marginal sea of the northern tethys ocean, one of the so-called peritethyan basins that became closed with the suturing of northeast iran to the eurasian turan platform resulting from the convergence between the arabian and eurasian plates (taherpour- Khalil-aBad et al, 2013, 2017.…”
Section: Geological Settingmentioning
confidence: 99%