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307 results for “benthic foraminifera”
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).
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).
Fig. 1 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 1 Location of the studied sections on the Romanian (A) and Serbian (B) territory showing the occurrence intervals (red lines) of Moulladella jourdanensis (Foury & Moullade) n. gen., nov. comb. A1 – location of the two studied sections in Romania; 1, Reşiţa-Moldova Nouă zone; 2, Dâmbovicioara zone, A2 – Succession of the Lower Cretaceous deposits from the Reşiţa- Moldova Nouă zone (modified from Bucur, 1997): 1, conglomerates and sandstones; 2, alternating sandstones and shales; 3, bedded bioclastic limestones; 4, massive bioclastic limestones; 5, chert-bearing limestones; 6, marly-limestones and marls; 7, micritic limestones; 8, micritic limestones with chert intercalations. A3 – Succession of the Lower Cretaceous deposits from Dâmbovicioara zone (modified from Bucur et al., 2011): 1, alternating marls and limestones; 2, marls with patch-reef limestone intercalations; 3, marly-limestones and marls; 4, glauconite-bearing limestones; 5, bedded limestones; CNM = Cetatea Neamţului Member. B1 – Location of the studied section in Serbia. JRA = Jerma River Area. B2 – Succession of the Lower Cretaceous deposits from the Jerma River Canyon (modified from Bucur et al., 1995): 1, conglomerates, sandstones and shales; 2, bedded limestones.
Fig. 6 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 6 Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. (a) Axial section of a megalospheric specimen. (b, f) Subaxial sections. (c–d, g, l) Oblique sections. (e, k, m–n, p) Slightly oblique transverse sections. (h, o) Tangential sections. (i–j) Tangential-oblique sections. Central zone highlighted in grey. b, beam; d,?deuteroconch; f, foramen; is, initial spire; p, proloculus; s, septum. Thin-sections: 14098-4 (a, c), 12568-4 (b), 12562-2 (d), 9-Mandrisag (e), 272-Ciclova (f), 4222- Ilidia (g), M10-Crivina (h), 14729 (i, l), 14734 (j–k), Lo 11 (m–n), 14733 (o). Location and age: (a-d) Dâmbovicioara area, Southern Carpathian, Romania (Early Valanginian); (e-h) Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania (Early Barremian); (i-l, o) Jerma River Canyon, Eastern Serbia (Early Valanginian); (m-n) Losenstein, Northern Calcareous Alps, Austria (Early Barremian, cobbles in Albian-Cenomanian conglomerates).
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.
Fig. 15 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 15 All scales represent 100 μm.1. Neoeponides schreibersi (d'Orbigny). Sample F4, Rupelian. 2.?Gyroidina constans (Reiser). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample F14, Rupelian. 3. Cibicidoides ungerianus filicosta (Hagn). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample F14, Rupelian. 4. Cibicidoides acutus (Samoylova). Sample F10, Rupelian. 5. Cibicides amphysiliensis (Andreae). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, FB18, Chattian. 6. Cibicidoides oligocenicus (Samoylova). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample F14, Rupelian. 7. Epistominella molassica (Hagn). Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample F14, Rupelian. 8. Fontbotia wuellerstorfi (Schwager). Same specimen, a. umbilical view, b. spiral view, same scale, sample F11,
Fig. 13 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 13 All scales represent 100 μm.1. Uvigerina moravia Boersma. Same specimen, a. apertural view, b. lateral view, same scale, sample F4, Rupelian. 2-5. Uvigerina popescui Rögl. 2a-b. same specimen, a. lateral view, b. lateral view, same scale, sample F6, Rupelian; 3a-b. same specimen, a. apertural view, b. apertural view, same scale, sample F6, Rupelian; 4a-b. same specimen, a. apertural view, b. lateral view, same scale, sample FB20, Chattian; 5a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F5, Rupelian. 6. Uvigerina vicksburgensis Cushman & Ellisor. Same specimen, a. apertural view, b. lateral view, same scale, sample F14, Rupelian. 7. Uvigerina steyri Papp. Same specimen, a. apertural view, b. lateral view, same scale, sample FB21, Chattian. 8. Uvigerina gracilis Reuss. Same specimen, a. apertural view, b. lateral view, same scale, sample FB21, Chattian. 9. Angulogerina globosa (Stoltz). Same specimen, a. apertural view, b. lateral view, same scale, sample F5, Rupelian. 10,13. Angulogerina angulosa (Williamson). 10a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F14, Rupelian; 13a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F9, Rupelian.11. Uvigerina tenuistriata schlichti Schudack & Nuglisch. Sample F3, Rupelian. 12. Uvigerina gracilis var. oligocaenica (Andreae). Sample F34,
Fig. 11 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 11 All scales represent 100 μm. 1. Bolivina scalprata retiformis Cushman. Same specimen, a. apertural view, b. lateral view, same scale, sample F11, Rupelian. 2. Bolivina fastigia Cushman. Same specimen, a. apertural view, b. lateral view, same scale, sample F11, Rupelian. 3. Bolivina dilatata maxima Cicha & Zapletalová. Same specimen, a. apertural view, b. lateral view, same scale, sample FB14, Chattian. 4. Bolivina dilatata hyalina Hofmann. Same specimen, a. apertural view, b. lateral view, same scale, sample FB01, Chattian. 5-6. Bolivina dilatata dilatata Reuss. 5. sample F27, Rupelian; 6. sample F33, Rupelian/Chattian. 7. Bolivina antiqua d'Orbigny. Sample F23, Rupelian. 8. Bolivina tereta (Cushman). Sample F38, Chattian. 9. Bolivina semistriata semistriata Hantken. Same specimen, a. apertural view, b. lateral view, same scale, sample F15, Rupelian. 10. Bolivina molassica Hofmann. Same specimen, a. apertural view, b. lateral view, same scale, sample F23, Rupelian. 11. Bolivina semistriata nobilis Hantken. Same specimen, a. apertural view, b. lateral view, same scale, sample F4, Rupelian. 12. Bolivina pokornyi serrata Cicha & Zapletalová. Same specimen, a. apertural view, b. lateral view, same scale, sample F13, Rupelian. 13. Cassidulinoides bodeni Hagn. Same specimen, a. lateral view, b. apertural view, same scale, sample F20, Rupelian. 14. Globocassidulina subglobosa (Brady). Sample F12, Rupelian. 15. Loxostomoides zsigmondyi (Hantken). Sample F20, Rupelian. 16. Globocassidulina globosa (Hantken). Sample F23, Rupelian.
Fig. 5 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 5 All scales represent 100 μm. 1. Spirorutilus carinatus (d'Orbigny). Same specimen, a. apertural view, b. lateral view, same scale, sample F4, Rupelian. 2. Semivulvulina pectinata (Reuss). Same specimen, a. apertural view, b. lateral view, same scale, sample F15, Rupelian. 3,6. Vulvulina spinosa Cushman. 3a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F2, Rupelian; 6. sample F7, Rupelian. 4. Vulvulina haeringensis (Gümbel). Sample F7, Rupelian. 5. Semivulvulina sagittula (Defrance). Sample F3, Rupelian. 7-8. Karrerulina conversa (Grzybowski). 7. sample F7, Rupelian; 8. sample F25, Rupelian. 9. Popovia plana (Bykova). Same specimen, a. lateral view, b. peripherial view, c. lateral view, same scale, sample FB20, Chattian.
Fig. 5 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. 5 Suraqalatia brasieri Görmüş, Lawa & Al Nuaimy, upper Maastrichtian Tarbur Formation of Mandegan section. Detailed view showing wall structure and exoskeleton (subepideremal network). Abbreviations: b = beam, ep = epiderm, f = foramen, s = septum. Thin-section Rt 63.
Fig. 4 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. 4 Suraqalatia brasieri Görmüş, Lawa & Al Nuaimy, upper Maastrichtian Tarbur Formation of Mandegan (a, e) and Naghan sections (b–d, f); oblique, partly tangential sections. Abbreviations: D = Dicyclina, L = Loftusia, N = Neobalkhania, O = Omphalocyclus. Scale bars = 1 mm. Thin-sections: Rt 63 (a), 2NG 183 (b), Rt 36 (c), 2NG 146 (d), 2NG 169 (f).
Fig. 2 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. 2 Distribution (total vertical range) of Suraqalatia brasieri Görmüş, Lawa & Al Nuaimy and some other larger benthic foraminifera in the Tarbur Formation of the Mandegan section.
Fig. 4 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 4 All scales represent 100 μm. 1. Reophax scorpiurus Montfort. Sample F38, Chattian. 2. Reophax pilulifer Brady. Sample FB23, Chattian. 3. Subreophax scalaris (Grzybowski). Sample F25, Rupelian. 4. Ammobaculites agglutinans (d'Orbigny). Sample FB62, Chattian. 5-9. Haplophragmoides carinatus Cushman & Renz. 5. sample F14, Rupelian; 6a-b. same specimen, a. lateral view, b. peripherial view, same scale, sample FB61, Chattian; 7. sample F19, Rupelian; 8. sample F35, Rupelian/Chattian; 9. sample F2, Rupelian. 10-11. Haplophragmoides suborbicularis (Grzybowski). 10a-b. same specimen, a. lateral view, b. peripherial view, same scale, sample F1, Rupelian; 11. sample F26, Rupelian. 12. Sculptobaculites barri Beckmann. Sample F24, Rupelian. 13. Ammosphaeroidina pseudopauciloculata (Mjatliuk). Sample F28, Rupelian. 14. Recurvoides sp. Same specimen, a.
Fig. 3 All scales represent 100 in Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania)
Fig. 3 All scales represent 100 μm. 1. Bathysiphon taurinensis Sacco. Same specimen, a. apertural view, b. lateral view, same scale, sample F8, Rupelian. 2. Nothia sp. Same specimen, a. apertural view, b. lateral view, same scale, sample FB20, Chattian. 3. Nothia sp. Sample F19, Rupelian. 4-5. Nothia excelsa (Grzybowski). 4. sample F4, Rupelian; 5. sample F22, Rupelian. 6. Hyperammina rugosa Verdenius & Van Hinte. Same specimen, a. apertural view, b. lateral view, same scale, sample FB62, Chattian. 7. Hyperammina elongata Brady. Sample F7, Rupelian. 8. Hyperammina sp. Sample F14, Rupelian. 9. Glomospira charoides (Jones & Parker). Sample F32, Rupelian/Chattian. 10. "Glomospira" serpens (Grzybowski). Sample F20, Rupelian. 11. Ammodiscus pennyi Cushman & Jarvis. Sample F15, Rupelian. 12. Reophax duplex Grzybowski. Sample F22, Rupelian. 13. Hormosina trinitatensis Cushman & Renz. Sample F31, Rupelian/Chattian. 14. Reophax globosus Sliter. Sample FB62, Chattian. 15. Reophax subfusiformis Earland. Sample FB23, Chattian. 16. Reophax excentricus Cushman. Sample F1, Rupelian. 17. Pseudonodosinella elongata (Grzybowski). Sample F13, Rupelian.
Fig. 14 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 14 Spirolina? farsiana n. sp., Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Subaxial section. b–c, f Equatorial section, partly oblique. d–e, g Subaxial, slightly oblique sections. Thinsections: Rt 67-3 (a, e), Rt 70 (b, f), Rt 86 (c), SNSB-BSPG 2016 III-3 (d), Rt 84 (g).
Fig. 10 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 10 Fleuryana adriatica De Castro, Drobne & Gušić, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a, f Equatorial sections. b–c Oblique sections. d Broken oblique section. e Axial section. Thin-sections: Rt 87 (a), SNSB-BSPG 2016 III-7 (b–c), Rt 82 (d), Rt 68 (e), Rt 70 (f).
Fig. 1 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 1 Lithostratigraphy of the Late Cretaceous of the Zagros Zone, Iran (excerpt and redrawn from the Stratigraphic Chart of Iran published by the Geological Society of Iran in 1995).
Fig. 8 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 8 Stratigraphic distribution and general comparison of Accordiella conica Farinacci, Accordiella? tarburensis n. sp., and Pseudoaccordiella ayaki Gallardo-Garcia & Serra-Kiel, (from Serra-Kiel et al., 2016, fig. 30.3 and 30.7).
Fig. 13 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 13 Spirolina? farsiana n. sp., Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Oblique equatorial section of specimen with uncoiled adult part. b Slightly oblique equatorial section with few uncoiling chambers; holotype specimen. c Subaxial section: Note changing growth direction of enrolled part. d Detail of e showing foramina with lip-like projections. e, f "Axial" section of the uncoiled part. g–h Subaxial sections. Note teeth-like projections in g (arrow). i, fragmentary oblique section. Thin-sections: Rt 67-3 (a, e–d), Rt 67-2 (b, h), SNSB-BSPG 2016 III-1 (c, g, i), SNSB-BSPG 2016 III-8 (f).
Fig. 16 Lamellar perforate foraminifera Laffiteina monodi Marie. a in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 16 Lamellar perforate foraminifera Laffiteina monodi Marie. a Oblique section, thin-section Rt 100-2. b Subaxial section, thin-section Rt 90.
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