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764 results for “foraminifera”
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.
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 Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia)
Fig. 6 Dasycladalean algae from the limestone pebbles of Trbušnica. a, b Salpingoporella muehlbergii (Lorenz); longitudinal-oblique (a) and transverse-oblique (b) sections; thin section RR4518. c, e Salpingoporella sp. in transverse section (c) and oblique section (e); thin section RR4518. d Salpingoporella gr. pygmaea (Gümbel) in oblique section; thin section RR4518. f, h Suppiluliumaella gr. polyreme Elliott; transverse-slightly oblique sections; e, thin section RR4516; h, thin section RR4517. i?Triploporella sp.; longitudinal-oblique section, thin sectionRR4518. g, j, k?Suppiluliumaella sp. in oblique sections (g, j) and longitudinal-oblique (k) sections; g, thin section RR4519; j, k, thin section RR4521. Scale bar = 0.25 mm.
Fig. 1 in Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia)
Fig. 1 Geological map of the Trbušnica area (modified from Filipović et al., 1976). The star indicates the location of the samples; 1. Igneous rocks; 2. Metamorphic rocks; 3.Upper Cretaceous ("Senonian"); 4.Middle Miocene; 5.Pliocene; 6.Fault
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).
Fig. 11 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 11 Broeckina cf. dufrenoyi (d'Archiac), Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Fragmentary equatorial section showing septules. b–c Oblique sections showing septula. d Subaxial section. Thin-sections: SNSB-BSPG 2016 III-16 (a–b), SNSB-BSPG 2016 III-17 (c), Rt 113-2 (d).
Fig. 3 a-b in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 3 a-b: Satellite (A, from google maps) and field views (b) of the Gurpi (GF) and Tarbur formations (TF) in the Mandegan area. The distance from left to right in A is ~4.7 km. Figure c: Conform boundary of Gurpi and Tarbur formations at the Mandegan section.
Fig. 7 in Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran
Fig. 7 Accordiella? tarburensis n. sp., Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a–f Oblique transverse sections. g–i, k–l Oblique sections. j Broken axial section. Thin-sections: SNSB-BSPG 2016 III-8 (a–c), Rt 68 (d–e), Rt 82 (f), Rt 87 (g), Rt 71 (h), Rt 64 (i), Rt 61-1 (j), Rt 70 (k), Rt 73 (l). Abbreviations: f = foramen, pi = pillar.
Figure 3 in Tintinnina (Ciliophora) and Foraminifera in plankton of hypersaline Lagoon Bardawil (Egypt): spatial and temporal variability
Figure 3. Dependence of number of found tintinnid species on number of analyzed samples in Lagoon Bardawil (a) and the Mediterranean Sea (b).
Figure 2 in Tintinnina (Ciliophora) and Foraminifera in plankton of hypersaline Lagoon Bardawil (Egypt): spatial and temporal variability
Figure 2. Dependence of total tintinnid abundance on number of tintinnid species in Lagoon Bardawil during 2009 and 2010 (a- winter, b- all seasons).
Fig. 6 in The phanerozoic diversity of agglutinated foraminifera: Origination and extinction rates
Fig. 6. Ranked per−capita extinction (A) and origination (B) rates, showing events of highest amplitude.
Fig. 1 in The phanerozoic diversity of agglutinated foraminifera: Origination and extinction rates
Fig. 1. Number of agglutinated foraminiferal genera in each geological stage based on updated ranges of 764 genera (including genera reported only from a single stage).
Fig. 2 in The phanerozoic diversity of agglutinated foraminifera: Origination and extinction rates
Fig. 2. Phanerozoic mean standing diversity of agglutinated foraminifera and mean sea level. The mean sea level curve was generated using Time Scale Creator, version 4.0.2 [http://www.tscreator.com]
Fig. 5 in The phanerozoic diversity of agglutinated foraminifera: Origination and extinction rates
Fig. 5. Per−capita (A) and percent (B) origination rates of agglutinated foraminiferal genera over the Phanerozoic.
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International Brain Laboratory public data
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OpenNeuro
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