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Fig. 10 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 10 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan (a) and Mandegan (all others) sections, Zagros Zone, SW Iran. a–c, h Oblique equatorial sections. d, f–g Equatorial sections. e Equatorial section of an uncoiling specimen. Thin-sections: NG 197-2 (a), Rt 72 (b), Rt 79 (c), Rt 113 (d, f–h), Rt 98 (e).

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Fig. 12 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 12 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a, g, i–j) and Naghan sections (all others), Zagros Zone, SW Iran. a–e, h–i Oblique sections; note the rounded outline of the network in a and b. f Tangential section; note the rounded subepidermal network (lower part). g Almost centered axial section, holotype specimen. j Juvenile specimen showing protoconch connected to the following chamber (?deuteroconch) by numerous openings. Abbreviations: b = beam, p = proloculus, d? = possible deuteroconch, f = foramen, r = rafter, s = septum. Thin-sections: Rt 87 (a), NG 198 (b), 2NG 120-1 (c), 2NG 144 (d), 2NG 113 (e), 2NG 200-1 (f), Rt 113 (SNSB-BSPG 2016 V 16) (g), 2NG 200-1 (h), Rt 113-1 (i), Rt 72 (j).

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Fig. 9 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 9 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a, e, g) and Naghan sections (all others), Zagros Zone, SW Iran. a–b Equatorial sections. c–d, g Oblique equatorial sections; note tendency to uncoil in the youngest chambers. e–f Oblique equatorial sections of uncoiling specimens. Abbreviations: p = proloculus, d = possible deuteroconch, f = foramen, s = septum. Thin-sections: Rt 113 (a, g), 2NG 191 (b), 2NG 186 (c), 2NG 49 (d), Rt 87-1 (e), NG 196 (f).

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Fig. 8 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 8 Schematic drawing showing differences in the wall structure of Persiella n. gen. and Pseudocyclammina Yokoyama (without scale).

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Fig. 7 Flabelloperforata tarburensis n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 7 Flabelloperforata tarburensis n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a Oblique section showing multiple foramina. b Detail from a showing pseudo-keriotheka-like wall structure. c Oblique section. d, e Details (d from c) showing multiple foramina. f Oblique section. Thin-sections: 2NG 8 (a–b), 2NG 86 (c–e), 2NGN (f). Scale bars: a–b = 0.2 mm, c, f = 1 mm, d–e = 0.3 mm.

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Fig. 6 Flabelloperforata tarburensis n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 6 Flabelloperforata tarburensis n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a–e, g–l: Oblique sections; holotype specimen in a; multiple foramina depicted in i and k with arrows. f Oblique equatorial section. T: Tarburina zagrosiana Schlagintweit, Rashidi & Barani. m Slightly oblique subaxial section. Arrow: multiple foramina. Thin-sections: NG 85-2 (a), 2NG 81-2 (b), 2NG 85-1 (c), 2NG 83 (d), 2NG 84-1 (e, h), NG 49 (f), 2NG 81-4 (g), NG 83-2 (i), NG 81 (j), NG 61 (k), 2NG 87-2 (l), 2NG 197 (m).

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Fig. 1 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 1 Lithostratigraphy of Upper Cretaceous strata of the Zagros Zone (redrawn from the Stratigraphic Chart of Iran, Geological Society of Iran, 1995).

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Fig. 5 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 5 Neobalkhania bignoti Cherchi, Radoičić & Schroeder from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a), and Naghan sections (all others). a Subaxial section of a large specimen (diameter ~7 mm). b Axial section of a megalospheric specimen. c Four specimens in (sub)axial sections, and Dicyclina sp. (D). d Tangential section showing subepidermal network with coarse primary partitions (right below) and finer secondary partitions (left below). e Oblique axial section of a megalospheric specimen. f Fragmentary equatorial section, P = Persiacyclammina maastrichtiana Schlagintweit & Rashidi. g Oblique section of a megalospheric specimen showing large embryo with opening to the second annular chamber. Scale bars: a–b, d, f–g = 0.3 mm; C, E = 0.6 mm. Thin-sections: Rt 113 (a), 2NG 109 (b), 2NG 128 (c), 2NG 201-1 (d), 2NG 120 (e), 2NG 81 (f–g).

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Fig. 3 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 3 Typical microfacies of samples with Flabelloperforata tarburensis n. gen., n. sp (F in a–b), and Persiella pseudolituus n. gen., n. sp. (Ps in c–d), from the upper Maastrichtian Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a–b Wackestones/packstones with benthic foraminifera, among many porcelaneous and agglutinating taxa such as Dicyclina sp. (Di), Tarburina zagrosiana Schlagintweit, Rashidi & Barani (T), Dictyoconus bakhtiari Schlagintweit, Rashidi & Babadipour (D) and remains of dasycladalean algae (d in b). c Wackestone with small and larger benthic foraminifera and oblique longitudinal section of the dasycladale Pseudocymopolia cf. anadyomenea (Elliott) (P). d Grainstone/packstone with Omphalocyclus macroporus Lamarck (O), Dictyoconella? minima Henson (Dic), and slightly oblique axial section of Persiella pseudolituus n. gen., n. sp. (Ps). Thin-sections: 2NG 81-4 (a), 2NG 120 (b), 2NG 166 (c), 2NG 177 (d).

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Fig. 2 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 2 Location of the Naghan and Mandegan sections, the type localities of Flabelloperforata tarburensis n. sp., and Persiella pseudolituus n. gen., n. sp. (taken from google maps)

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Fig. 13 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 13 Pseudcyclammina lituus Yokoyama (a–c) compared to Persiella pseudolituus n. gen., n. sp. (d–f). a, d Equatorial sections; b, e axial sections; c, f subaxial-tangential sections. From Hottinger (1967): a = pl. 10, fig. 11 (late Jurassic of Poland), b and c = pl. 10, fig. 12 and fig. 13 (topo-type from Tithonian-Berriasian Torinosu limestone, Japan).

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Fig. 11 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 11 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a-b, d, g-h, m Axial sections (partly slightly oblique); note initial streptospiral coiling in a. e–f Subaxial sections. i–j: Details from f and h showing pseudokeriotheka-like wall structure. k–l Oblique sections. Thinsections: 2NG 76 (a), 2NG 120-1 (b), 2NG 152 (c), 2NG 122 (d), 2NG 153 (e), 2NG 154 (f, i), 2NG 127 (g), 2 NG 186 (h, j), 2NG 152-1 (k–l), NG 3-1 (m).

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Fig. 4 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 4 Vertical distribution of Persiella pseudolituus n. gen., n. sp. and some other larger benthic foraminifera in the Tarbur Formation of the Mandegan section.

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