Find research datasets worth reusing

Fig. 8 Broeckinella hensoni n in Broeckinella Hensoni N. Sp., A New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran And A Revision Of The Genus Broeckinella Henson, 1948

Fig. 8 Broeckinella hensoni n. sp., upper Maastrichtian Tarbur Formation of the Naghan (a, d–e) and Mandegan (b–c, f) sections, Zagros Zone, SW Iran. a Oblique equatorial section. Note porcelaneous test of Cuvillerinella sp. below. b Detail showing fine subepidermal network (sn, below), followed by zone with radial partitions (rp) only and finally the undivided central chamber part with foramina (f) piercing the septa (s). c Oblique section cutting the initial planispiral part. d–e Oblique equatorial sections showing zones of different internal structure (see Text-Figure 3). f Detail from c showing initial planispirally coiled part with numerous chambers. Note also the fine subepidermal network and main partitions (right side). Thin-sections: 2NG 166 (a), Rt 67-1 (b), RT 72 (c, f), 2NG 118 (d), 2NG 172 (e). Scale bars 1.0 mm for a, c–e, 0.2 mm for b and f.

Fig. 4 in Broeckinella Hensoni N. Sp., A New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran And A Revision Of The Genus Broeckinella Henson, 1948

Fig. 4 Internal structure of Broeckinella arabica Henson. a Drawing of a slightly oblique equatorial section (slightly modified from Henson, 1947, fig. 13c; see also Cherchi and Schroeder 1978, fig. 1C). 1 = subepidermal layer (network; exoskeleton), 2 = zone with transverse partitions only, 3 = undivided chamber interior (lacking endoskeleton); septa with foramina. b Tangential equatorial section of Broeckinella arabica showing the three zones of Henson (1948). Thin-section Rt 85, Mandegan section. c Tangential equatorial section showing main partitions aligned between successive chambers (detail from Fig. 6d). Thin-section NG 42-1, Naghan section.

Fig. 5 Broeckinella hensoni n in Broeckinella Hensoni N. Sp., A New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran And A Revision Of The Genus Broeckinella Henson, 1948

Fig. 5 Broeckinella hensoni n. sp. (a) and Broeckinella arabica Henson (b–d) from the upper Maastrichtian of the Tarbur Formation, Naghan section. a Foraminiferal wackestone with Broeckinella hensoni n. sp., thin-section 2NG 197. b Foraminiferal wackestone with Broeckinella arabica Henson, 2NG 128-1. c–d Details from b, showing a microspheric specimen. Scale bars in c and d = 1 mm.

Fig. 3 in Broeckinella Hensoni N. Sp., A New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran And A Revision Of The Genus Broeckinella Henson, 1948

Fig. 3 Naghan section, along the road from Naghan to Izeh with the type-level of Broeckinella hensoni n. sp. marked by an asterisk (left side).

Fig. 1 in Broeckinella Hensoni N. Sp., A New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran And A Revision Of The Genus Broeckinella Henson, 1948

Fig. 1 Peneroplis aragonensis (Peybernès) nov. comb. a Equatorial section. b Broken axial section (both from Peybernès, 1984, pl. 1, fig. 1 and 7, Late Albian of Spanish Pyrenees). c Detail from d showing fine surface ornamentation (striae). d Slightly oblique equatorial section. e Subaxial section showing fine striae of surface ornamentation (c-e from the Late Albian Barcenaciones Formation, Cantabria, N-Spain, leg M. Najarro).

Fig. 3 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 3 Upper Cretaceous (middle Campanian) microfacies of sample GKL 39. Pa = Paracoskinolina klokovaensis n. sp., Pal = Paleodictyoconus senonicus Moullade & Viallard, Di = Dicyclina schlumbergeri Munier-Chalmas.

Fig. 6 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 6 Comparison of Paracoskinolina species with one horizontal partition in the marginal zone: a P. klokovaensis sp. nov., b P. reicheli Guillaume, 1956. c P. arcuata (Arnaud-Vanneau 1976). D = test diameter, H = test height, n = number of chambers per last 0.5 mm axial length, h = chamber height (all data except D/H in mm). * measured from original illustrations. Stratigraphy of the two Lower Cretaceous species according to Clavel et al. (2014).

Fig. 4 Acanthochaetetes fischeri n in Acanthochaetetes Fischeri N. Sp. (Coralline Demosponge) From The Upper Paleocene (Thanetian) Of Iraq (Kurdistan Region) And Iran (Sistan Suture Zone)

Fig. 4 Acanthochaetetes fischeri n. sp. from the upper Paleocene of northeastern Iraq. a Longitudinal (left) and cross (right) sections. Note the thick double walls (black arrows). Thin-section 18. b–c cross sections, where spines inside calicles (black arrows) and thick double walls (white arrows in c) can be seen. Thin-sections 24 and 17. d Oblique section, showing scarce tabulae (black arrows). Thin-section 17. e Cross section. Note the round/oval to elliptical shape of calicles, as well as two fissiparous division processes (black arrows). Thin-section 24. f Longitudinal section, where tabulae (black arrows) and subsequent fissiparous division processes (grey arrows) can be observed. Thin-section 17. g Cross-to-oblique section, showing massive thickenings (square; common for all Acanthochaetetidae; compare Reitner, 1991; Sánchez-Beristain et al., 2019, 2021). Thin-section 16. h Oblique section, with abundant lamellae (black arrows), common for all Acanthochaetetidae (compare Reitner, 1991). Thin-section 24. i Cross-oblique section, showing round to elliptical shape of calicles, as well as multiple lamellae (right side of the picture). See text and table 1 for further details. Thin-section 24.

Fig. 3. Acanthochaetetes fischeri n in Acanthochaetetes Fischeri N. Sp. (Coralline Demosponge) From The Upper Paleocene (Thanetian) Of Iraq (Kurdistan Region) And Iran (Sistan Suture Zone)

Fig. 3. Acanthochaetetes fischeri n. sp. from the upper Paleocene of eastern Iran (a–b) and northeastern Iraq (c–f). a Longitudinal section, showing notable walls (yellow arrows) and tabulae (black arrows), the latter occurring seldom. Thin-section 2pz 93. b Longitudinal section, with spines within calicles, diagnostic for the genus Acanthochaetetes Fischer (yellow arrows). Spines in only one calicle are shown. Note also the huge intertabular space (between red arrows), measuring> 2 mm as a rule. In addition, thick double walls, diagnostic for A. fischeri n. sp. can be seen (black arrows). A fissiparous division process (black square) is highlighted. Thin-section 2pz 95. c–e Oblique section, where the high density of calicles/mm2 (1.5 to 2.5) can be confirmed. This trait can also be seen in d and e especially in the marked areas (squares). Thin-sections 24, 15, and 14. f Cross section, showing the remarkably thick double walls (red arrows), which can attain up to 0.3 mm. See text and table 1 for further details. Thin-section 26. Abbreviations: mb= macroboring (e.g. Gastrochaenolites-type), tb = tubulae.

Fig. 2 in Acanthochaetetes Fischeri N. Sp. (Coralline Demosponge) From The Upper Paleocene (Thanetian) Of Iraq (Kurdistan Region) And Iran (Sistan Suture Zone)

Fig. 2 Type-locality of Acanthochaetetes fischeri n. sp. in northern Sulaymaniyah Governorate, Iraq. a Location of the Nawar section close to Darbandikhan Lake (from google Earth). b Geological map showing the distribution of the Kolosh Formation. c Location of the type-locality of Acanthochaetetes fischeri n. sp. in northeastern Iraq close to the border to Iran.

Fig. 2 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 2 Upper Cretaceous successions of Klokova Mountain, SW Greece (see Fleury, 1970, fig. 1, for details) with the distribution of some benthic foraminifers (A-B: Senalveolina aubouini Fleury, sample GKL 43; C-D Accordiella conica Farinacci, sample GKL 43x, without scale). Note: the lower/middle Campanian boundary is approximately placed at the LAD of K. tergestina (Frijia et al., 2015, fig. 15). For microfacies of sample GKL 39 see Figure 3.

Fig. 1 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 1 Geographic sketch map showing the location of Klokova mountains on the opposite side of the Gulf of Corinth facing Patra. This is the type-locality of Paracoskinolina klokovaensis n. sp.

Fig. 1 a-b in Acanthochaetetes Fischeri N. Sp. (Coralline Demosponge) From The Upper Paleocene (Thanetian) Of Iraq (Kurdistan Region) And Iran (Sistan Suture Zone)

Fig. 1 a-b Acanthochetetes sp. from a lower Albian hardground (base of Meruelo Formation) of Cape Ajo, Cantabria, N Spain. A. = Acanthochaetetes, s = serpulid tube, s.p. = siliceous sponge, e.f. = encrusting foraminifera. Scale bars = 1.0 mm. c-d Bioclastic packstone (upper slope facies) with Acanthochaetetes fischeri n. sp. from the upper Paleocene of eastern Iran; thin-sections 2pz 95 and BN 89. Scale bars 1.0 mm(a-b), 0.9 mm (c) and 0.6 mm (d).

Fig. 4 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 4 Coskinolinidae (a, d, g, j) and Orbitolinidae (b-c, e-f, h-i, k-l) from the Campanian of Klokova Mountain SW Greece (a-f, h-l) and Brač Island, Croatia (g). Lepinoconus chiocchinii Cruz-Abad et al. a Oblique section. d Broken transverse section. g, j Subaxial sections. Paleodictyoconus senonicus Moullade & Viallard b, e Oblique transverse sections. c, f Subaxial sections. Calvezicionus lecalvezae Caus & Cornella. h, k Oblique sections. i Oblique section passing the biloculine, slightly inclined megalospheric embryo. Dictyoconella complanata Henson. l Oblique section in the plane of compression. Abbreviations: b = beam, de = deuteroconch, f = foramen, p = protoconch, pi = pillar, s = septum. Thin sections: GKL 43 (a, j, i, l), GKL 43x (d, k), GKL 39 (b-c, e, h), GKL 39x (f).

Fig. 7 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 7 Central Mediterranean area (modified from Google Earth) with occurrences of Campanian Orbitolinidae-Coskinolinidae. 1: Zambetakis-Lekkas and Alexopoulos (2007) 2: Fleury (1970, 1980, this work) 3: Mount Biokovo (Sokač et al., 2012) 4: Brač Island (Gušić and Jelaska, 1990; CvetkoTešović et al., 2001) 5-7: Moro et al. (2016) 8: Luperto-Sinni (1976) 9: Frijia et al. (2015) 10: CruzAbad et al. (2017).

Fig. 5 Paracoskinolina klokovaensis n in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 5 Paracoskinolina klokovaensis n. sp., from the late early-middle Campanian of Mount Klokova, SW Greece (a-f, h-j) and Brač Island, Croatia (g). a Axial section. b-c, f-g Subaxial sections. d Oblique transverse section. h Oblique section. i Tangential section. j Axial section, holotype specimen. Abbreviations: b = beam, f = foramen, ib = intercalary beam, pi = pillar, r = rafter. Thin sections: a GKL 39 (1754) (from Fleury, 1970, pl. 1, fig. 2), b-j GKL 39 (3357).

Fig. 6 in Parurgonina Valanginiana N. Sp. From The Valanginian Of Sw Iran (Zagros Zone): The First Cretaceous Record Of The Genus

Fig. 6. Parurgonina valanginiana sp. nov. from the Valanginian Fahliyan Formation of SW Iran. a-c, f subaxial sections; samples RAP 10825 (a), sample RAP 10869 (b-c, f) (b, c = Figs. 12c and 12b in Jamalian et al., 2011 illustrated as Valdanchella). d-e, g, j transverse sections, partly slightly oblique; samples RAP 10869 (d-e), RAP 10827 (g, j). h-i, k Oblique sections; samples RAP 10869 (h), RAP 10825 (i, k). Abbreviation: pi = pillar.

Fig. 3 in Parurgonina Valanginiana N. Sp. From The Valanginian Of Sw Iran (Zagros Zone): The First Cretaceous Record Of The Genus

Fig. 3. Selected dasycladalean algae (a–j, l, m, q) and benthic foraminifera (k, n-p, r) from the Berriasian–Valanginian Fahliyan Formation of SW Iran. a. Salpingoporella annulata Carozzi, sample RAP 1819. b. Aloisalthella sulcata (Alth) (right) and Campbelliella striata (Carozzi) (middle), sample RAP 10804. c. Humiella cf. catenaeformis (Radoičić), sample RAP 10798. d, l. Salpingoporella granieri Dieni & Radoičić, samples RAP 10835 (D) and RAP 10825 (L). e, h, m. Clypeina sp. or Salpingoporella sp., or Iranella inopinata sensu Hosseini et al. (2013), sample RAP 1028. f. Actinoporella cf. podolica (Alth), sample RAP 10860. g. Clypeina aff. dragastani Dieni & Radoičić, sample RAP 10820. i, q. Salpingoporella piriniae Carras and Radoičić, sample RAP 10828. j. Actinoporella? sp. aff. jaffrezoi Granier, sample RAP 10851. k. Coscinoconus alpinus Leupold, sample RAP 10824. n. Coscinoconus cf. sagittarius (Arnaud-Vanneau et al.), sample RAP 10850. o. Coscinoconus cherchiae (Arnaud-Vanneau et al.), sample RAP 10866. p. Choffatella decipiens Schlumberger, sample RAP 10881. r. Pseudocyclammina lituus (Yokoyama), sample RAP 10819. Scale bars = 0.20 mm.

Fig 5 in Parurgonina Valanginiana N. Sp. From The Valanginian Of Sw Iran (Zagros Zone): The First Cretaceous Record Of The Genus

Fig 5. Parurgonina valanginiana sp. nov. from the Valanginian Fahliyan Formation of SW Iran (a–h, j–k, m–n) and the Upper Jurassic of Algeria (i, l; from Schroeder et al., 1975, pl. 2, figs. 3-4). a–d. (Sub)axial sections of juvenile specimens showing embryo and 'praevalvulind' early stage sensu Septfontaine (2020); samples RAP 10825 (a–c), RAP 10869 (d). e. Slightly oblique axial section dissection the apical embryo; holotype specimen, sample RAP 10825. f. Subaxial section showing well developed thickened pillars in the central test part; sample RAP 10825 (= Fig. 12a in Jamalian et al., 2011 illustrated as Valdanchella). g. Tangential section showing the undivided marginal chamber area in the part following the 'praevalvulinid' stage; sample RAP 10825. h. Tangential oblique section; sample RAP 10825. i. Slightly oblique transverse section showing lunular pillars (from Schroeder et al., 1975, pl. 2, fig. 4, copyright by Swiss Geological Society). j. Oblique section; sample RAP 10825. k. Oblique section showing lunular pillars; sample RAP 10825. l. Slightly oblique transverse section (from Schroeder et al., 1975, pl. 2, fig. 3). m. Oblique transverse section; sample RAP 18025. n. Subaxial section; sample RAP 18025

Fig. 1.A in Parurgonina Valanginiana N. Sp. From The Valanginian Of Sw Iran (Zagros Zone): The First Cretaceous Record Of The Genus

Fig. 1.A. Simplified geological map of Iran (modified after Schlagintweit and Yazdi-Moghadam, 2021) showing the main tectonic subdivisions. B. Road map and position of the studied section. C. Tectono-stratigraphic units of the Zagros belt (modified after Yazdi-Moghadam and Schlagintweit, 2021) with position of the Kuh-e Siah section. Abbreviations: BF Balarud Fault, CEIM Central East Iran Microplate, HZF High Zagros Fault, KZF Kazerun Fault, MFF Mountain Front Fault, MZRF Main Zagros Revers Fault, MZT Main Zagros Thrust, SSZ Sanandaj-Sirjan Zone, UDMA Uromia Dokhtar Magmatic Arc, ZFTB Zagros Fold Thrust Belt.