Find research datasets worth reusing

Fig. 9 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 9 All scales represent 100 μm. 1. Saracenaria arcuata (d'Orbigny). Same specimen, a. lateral view, b. apertural view, same scale, sample F3, Rupelian. 2-3. Frondovaginulina tenuissima (Hantken). 2. sample F17, Rupelian; 3. sample F28, Rupelian. 4. Percultazonaria fragaria (Gümbel). Same specimen, a. apertural view, b. lateral view, same scale, sample FB20, Chattian. 5-6. Amphicoryna spinicosta (d'Orbigny). 5. sample F13, Rupelian; 6. same specimen, a. apertural view, b. lateral view, same scale, sample FB21, Chattian. 7. Amphicoryna armata (Neugeboren). Sample F21, Rupelian. 8. Amphicoryna crassa (Hantken). Sample F10, Rupelian. 9. Marginulina behmi (Reuss). Same specimen, a. apertural view, b. lateral view, c. peripherial view, same scale, sample FB21, Chattian. 10. Hemirobulina recta (Hantken). Sample F12, Rupelian. 11. Hemirobulina hantkeni (Bandy). Same specimen, a. apertural view, b. lateral view, same scale, sample FB21, Chattian.

Fig. 16 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 16 All scales represent 100 μm. 1. Planulina compressa (Hantken). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample FB20, Chattian. 2. Planulina costata (Hantken). Same specimen, a. umbilical view, b. spiral view, same scale, sample F12, Rupelian. 3. Asterigerinoides guerichi (Franke). Same specimen, a. umbilical view, b. spiral view, same scale, sample F18, Rupelian. 4. Nonion commune (d'Orbigny). Same specimen, a. lateral view, b. peripherial view, same scale, sample F4, Rupelian. 5. Pullenia salisburyii Stewart & Stewart. Same specimen, a. lateral view, b. peripherial view, same scale, sample F10, Rupelian. 6. Chilostomella cylindroides Reuss. Sample F34, Rupelian/Chattian. 7. Quadrimorphina petrolei (Andreae). Same specimen, a. umbilical view, b. spiral view, same scale, sample F18, Rupelian. 8-9. Alabamina tangentialis (Clodius). 8a-b. same specimen, a. umbilical view, b. spiral view, same scale, sample FB01, Chattian; 9a-b. same specimen, a. umbilical view, b. spiral view, same scale, sample FB21, Chattian. 10. Anomalinoides granosus (Hantken). Same specimen, a.

Fig. 7 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 7 All scales represent 100 μm. 1. Spiroloculina sp. Sample F9, Rupelian. 2. Spiroloculina canaliculata d'Orbigny. Sample F5, Rupelian. 3,5. Cycloforina ludwigi (Reuss). 3. sample F14, Rupelian; 5a-c. same specimen, a. lateral view, b. apertural view, c. lateral view, same scale, sample FB21, Chattian. 4. Quinqueloculina sp. Sample F17, Rupelian. 6. Sigmoilinita tenuis (Czjzek). Same specimen, a. apertural view, b. lateral view, same scale, sample F5, Rupelian. 7. Sigmoilinita tenuissima (Reuss). Same specimen, a. apertural view, b. lateral view, same scale, sample F5, Rupelian. 8- 9. Laevidentalina elegans (d'Orbigny). 8. sample F7, Rupelian; 9. sample F15, Rupelian. 10. Laevidentalina communis (d'Orbigny). Sample F18, Rupelian. 11. Nodosaria soluta (Reuss). Sample F3, Rupelian. 12. Neugeborina longiscata (d'Orbigny). Sample F12, Rupelian.

Fig. 8 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 8 All scales represent 100 μm. 1. Pyramidulina latejugata (Gümbel). Sample FB20, Chattian. 2. Dentalina contorta (Hantken). Sample F12, Rupelian. 3. Amphimorphina haueriana Neugeboren. Sample F4, Rupelian. 4. Dimorphina sp. Sample F12, Rupelian. 5. Lenticulina vortex (Fichtel & Moll). Sample F15, Rupelian. 6. Neolenticulina peregrina (Schwager). Sample FB21, Chattian.7. Lenticulina limbosa (Reuss). Same specimen, a. lateral view, b. peripherial view, c. lateral view, same scale, sample FB21, Chattian. 8. Lenticulina gibba (d'Orbigny). Sample F11, Rupelian. 9. Lenticulina arcuatostriata (Hantken). Same specimen, a. lateral view, b. peripherial view, same scale, sample FB20, Chattian. 10. Lenticulina inornata (d'Orbigny). Same specimen, a. lateral view, b. peripherial view, same scale, sample FB20, Chattian. 11. Lenticulina calcar (Linné). Sample F15, Rupelian. 12. Saracenaria senni Hedberg. Same specimen, a. lateral view, b. apertural view, same scale, sample F3, Rupelian. 13. Saracenaria propinqua (Hantken). Same specimen, a. lateral view, b. apertural view, same scale, sample F5, Rupelian.

Fig. 6 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 6 All scales represent 100 μm. 1. Reticulophragmium amplectens (Grzybowski). Sample F7, Rupelian. 2. Reticulophragmium rotundidorsatum (Hantken). Sample F28, Rupelian. 3. Reticulophragmium acutidorsatum (Hantken). Sample F2, Rupelian. 4. Karreriella chilostoma (Reuss). Sample F18, Rupelian. 5. Valvulina sp. Same specimen, a. umbilical view, b. spiral view, same scale, sample F2, Rupelian. 6. Karreriella hantkeniana Cushman. Sample F4, Rupelian. 7. Karreriella gaudryinoides (Fornasini). Sample F15, Rupelian. 8-10. Valvulina flexilis Cushman & Renz. 8. sample F8, Rupelian; 9-10. sample F31, Rupelian/Chattian.

Fig. 1 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)

Fig. 1 Simplified geological map of the studied area and location of sampled outcrops (modified after Beldean & Filipescu, 2011; detailed map redrawn after GiuȘcă & Rădulescu, 1967).

opencc-by-4.0Jul 2018View details →

Fig. 7 in Suraqalatia Brasieri Görmuş, Lawa & Nuaimy, 2017 (Larger Benthic Foraminifera; Suraqalatiidae N. Fam.) From The Late Maastrichtian Of The Tarbur Formation (Zagros Fold-Thrust-Belt) And Remarks On Dicyclina Munier-Chalmas, 1887

Fig. 7 Dicyclina schlumbergeri Munier-Chalmas, Late Maastrichtian Tarbur Formation of the Naghan section. a–b Oblique equatorial sections showing embryonic chamber, kidney-shaped in outline. Note the presence of primary partitions only (arrows). c Oblique section of a juvenile specimen. d, f Partial, slightly oblique axial sections. e Fragmentary equatorial section. Scale bars = 1 mm. Thin-sections: 2NG 191 (a), NG 83 (b), NG 13-1 (c), NG 34 (d), NG 49 (e), 2NG 34 big (f).

opencc-by-4.0Jul 2018View details →

Fig. 3 in Suraqalatia Brasieri Görmuş, Lawa & Nuaimy, 2017 (Larger Benthic Foraminifera; Suraqalatiidae N. Fam.) From The Late Maastrichtian Of The Tarbur Formation (Zagros Fold-Thrust-Belt) And Remarks On Dicyclina Munier-Chalmas, 1887

Fig. 3 Suraqalatia brasieri Görmüş, Lawa & Al Nuaimy, upper Maastrichtian Tarbur Formation of Mandegan (a, c) and Naghan sections (b, d, f); oblique, partly tangential sections. e development of annular chambers (in grey) in some orbitolinids (modified from Douglass, 1960, fig. 21) and two sections (X–X' and Y–Y') comparable to those illustrated in a–d, and f. Abbreviations: b = beam, ch = chamber, ib = intercalary beam, s = septum, sn = subepidermal network. Thin-sections: Rt 63 (a), 2NG 183 (b), Rt 36 (c), 2NG 146 (d), 2NG 169 (f).

Fig. 7 Microfacies and selected alveolinids from the Chenesht section. a–c Alveolina-Opertorbitolites packstone with Coskinolina sistanensis n in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 7 Microfacies and selected alveolinids from the Chenesht section. a–c Alveolina-Opertorbitolites packstone with Coskinolina sistanensis n. sp. (C), Alveolina elliptica (Sowerby) (arrows in b), Alveolina frumentiformis Schwager (arrow in c). d Alveolina elliptica nuttali Davies. e Alveolina oblonga d'Orbigny. Samples CH 2 (a), CH 6 (b, e), CH 12 (c), CH 5 (d). Scale bars 1 mm.

Fig. 6 a Coskinolina sistanensis n in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 6 a Coskinolina sistanensis n. sp., compared to the type-species Coskinolina liburnica Stache in b–c, d Coskinolina roberti Schlumberger, e Coskinolina perpera Hottinger & Drobne, f Coskinolina douvillei (Davies).

Fig. 5 Coskinolina sistanensis n in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 5 Coskinolina sistanensis n. sp., Illerdian-Cuisian of Iran: a oblique section of a low-conical specimen (?microspheric form). b, oblique section showing embryo. c–d, g–h, subaxial sections. e, tangential-oblique section. f, i, slightly oblique axial sections; embryo shown in (i). j axial section of a small megalospheric specimen showing embryo. k–l slightly oblique transverse sections. Thin-sections: CH 2 (a, c–h), CH 7 (b), CH 12 (i, k–l), CH 4 (j). Abbreviations: deu = deuteroconch, fo = foramen, m.a. = marginal aperture, pi = pillar, pr = proloculus.

Fig. 1 in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 1 Geographic map and location of the Chenesht section (Geological map of Birjand region, 1/100000 from Eftekhar-Nezhad, 1986).

Fig. 4 Coskinolina sistanensis n in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 4 Coskinolina sistanensis n. sp., Illerdian-Cuisian of Iran: a, d–e, g (sub)axial sections showing small initial spire. Holotype specimen in a. b, h oblique sections of megalospheric form. c, f tangential-oblique sections. i–k transverse slightly-oblique sections. l tangential section showing undivided marginal zone and pseudokeriotheka (right side). Thinsections: CH 4 (a–c, e), CH 12 (d, f, j–l), CH 2 (g–h), CH 7 (i). Abbreviations: fo = foramen, ma = marginal aperture, pr = proloculus, pi = pillar.

Fig. 2 in Coskinolina Sistanensis N. Sp., A New Larger Benthic Foraminifera From The Early Eocene Of Eastern Iran

Fig. 2 Field view of the Chenesht section with schematic distribution of main groups of larger benthic foraminifera.

opencc-by-4.0Jul 2018View details →

Fig. 6 in Suraqalatia Brasieri Görmuş, Lawa & Nuaimy, 2017 (Larger Benthic Foraminifera; Suraqalatiidae N. Fam.) From The Late Maastrichtian Of The Tarbur Formation (Zagros Fold-Thrust-Belt) And Remarks On Dicyclina Munier-Chalmas, 1887

Fig. 6 Dicyclina sampoi Cherchi & Schroeder, from the Cenomanian of the Sarvak Formation, Zagros Zone, SW Iran, slightly oblique axial section (from Omidvar et al., 2014, fig. 3.10 as Dicyclina schlumbergeri). Megalospheric specimen showing embryonic apparatus and bilateral symmetric pores (foramina) enabling the communication with the first cyclic postembryonic chamber. These are located between the supra- (upper; in yellow) and subembryonic zones (below; in red) (arrows). Both zones are subdivided by primary (b = beams) and secondary partitions (ib = intercalary beams).

Fig. 6 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran

Fig. 6 Accordiella? tarburensis n. sp., Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a–d, f, h–m Axial and subaxial sections. e, g Oblique sections. Thin-sections: Rt 87 (a, g), Rt 67-3 (b), Rt 61-1 (c), SNSB-BSPG 2016 III-4 (d), Rt 89-3 (e), Rt 113-2 (f), Rt 67 (h), Rt 70 (i), Rt 105 (j), Ng 189 (k), Rt 82 (l), Rt 73 (m).

Fig. 5 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran

Fig. 5 Microfacies of some charactersistic samples. a Packstone with benthic foraminifera Gyroconulina columellifera Schroeder & Darmoian (G), Omphalocyclus macroporus (Lamarck) (O), Laffiteina sp. (L), Minouxia/Tetraminouxia (M), Accordiella? tarburensis n. sp. (Z), Sirtina (S). Thin-section Rt 105. b Wackestone with Loftusia sp. (L), and Broeckina cf. dufrenoyi (d'Archiac) (B), thin-section Rt 113.

Fig. 9 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran

Fig. 9 Broeckinella arabica Henson (a–e) and Dicyclina cf. schlumbergeri Munier-Chalmas (f), Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a–d Oblique equatorial sections, partly fragmentary, in some parts crossing the subepidermal network of beams and rafters (e.g., left side of d). e Oblique section of Broeckinella arabica, comparable to the section erroneously illustrated as "Dicyclina schlumbergeri" by Khosrow Tehrani et al., 2008 in pl. 1, fig. 6. f Dicyclina cf. schlumbergeri Munier-Chalmas, subaxial section. Thin-sections: Rt 104 (a), Rt 64 (b), Rt 78 (c), Rt 85 (d), Rt 68 (e), SNSB-BSPG 2016 III-4 (f). Scale bars 0.5 mm.

Fig. 4 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran

Fig. 4 Vertical distribution of the described taxa and some index forms of larger benthic foraminifera in the Tarbur Formation of the Mandegan section.

Fig. 12 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran

Fig. 12 Cuvillierinella? sp., Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Oblique section close to axial plane. b–c Subaxial sections. sl = septulum. Thin-sections: Rt 100 (a), SNSB-BSPG 2016 III-10 (b), SNSB-BSPG 2016 III-18 (c).