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307 results for “benthic foraminifera”
Fig. 11 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 11 Representative illustrations of Mayncina orbignyi: a Equatorial section, Arnaud-Vanneau & Prestat in Schroeder & Neumann (1985, pl. 2, fig. 7, France); b Axial section, Arnaud-Vanneau & Prestat in Schroeder & Neumann (1985, pl. 2, fig.8, France).
Fig. 9 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 9 Representative illustrations of Deuterospira pseudodaxia: a Equatorial section, Hamaoui (1979, fig. 2a, Israel); b Axial section, Hamaoui (1979, fig. 2b, Israel).
Fig. 7 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 7 Representative illustrations of Daxia cenomana: a Equatorial section, Arnaud-Vanneau & Prestat in Schroeder & Neumann (1985, pl. 1, fig. 2, France); b Axial section, Arnaud-Vanneau & Prestat in Schroeder & Neumann (1985, pl. 1, fig.7, France).
Fig. 3 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 3 Cenomanian paleogeography with regions indicating the location of most planispiral LBF in this study. There are a few additional records from, for example, Peru, Afghanistan and Tibet. (Base paleogeographic map courtesy of Halliburton).
Fig. 5 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 5 Representative illustrations of Biconcava bentori: a Equatorial section, Hamaoui & Saint Marc (1970, pl. 21, fig. 1, Israel); b Axial section, Hamaoui in Schroeder & Neumann (1985, pl. 13, fig. 3, Lebanon).
Fig. 1 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 1 Anonymised snapshot of a figure caption from a 2016 paper (by a major publisher) with four taxa spelled incorrectly.
Fig. 39 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 39 Representative illustrations of Spirocyclina atlasica: a Equatorial section, Saint Marc and Rahhali (1982, pl. 2, fig. 1, Morocco); b External View, Etachfini (2006, pl. 13, fig. 9, Morocco); c Subaxial section, Saint Marc and Rahhali (1982, pl. 2, fig. 8, Morocco); d Axial section, Charriere et al. (1998, fig. 7(1), Morocco).
Fig. 2 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 2 Some morphological descriptions and visualisations of wall and/or chamber components of planispiral or part-planispiral LBF taxa. (a after Hamaoui & Saint-Marc, 1970; b-f after Hottinger, 2006; G: after Vicedo et al., 2013; h after Consorti et al., 2015; j after Consorti et al., 2018). Other abbreviations shown in image j are bl=basal layer; cs=conical spaces; if=intercameral foramina and sc=socculi crest.
Fig. 27 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 27 Representative illustrations of Moncharmontia compressa: a Equatorial section, Tasli et al. (2006, fig. 7(J), Turkey); b Axial section, Tasli et al. (2006, fig. 7(K), Turkey).
Fig. 35 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 35 Representative illustrations of Hemicyclammina whitei: a Axial view, Whittaker et al. (1998, pl. 12, fig. 1a, Qatar - see also Simmons & Bidgood, 2022, fig. 1a); b Axial section, Whittaker et al. (1998, pl. 59, fig. 8, U.A.E. - see also Simmons & Bidgood, 2022, fig. 3c); c Equatorial section, Simmons & Bidgood (2022, fig. 3a, Abu Dhabi).
Fig. 37 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 37 Representative illustrations of Reissella ramonensis: a Exterior view, (Hamaoui 1963, pl. 1, fig. 3, holotype, Israel); b Exterior view (schematic), (Hamaoui 1963, pl. 1, fig. 11, Israel); c Enlarged cutaway exterior view showing internal features (Hamaoui 1963, text fig. 1, Israel).
Fig. 21 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 21 Representative illustrations of Charentia cuvillieri: a Equatorial section, Neumann (1965, holotype, pl. 2, fig. 1c, France); b Axial section, Schroeder & Neumann (1985, pl. 3, fig. 3, France).
Fig. 29 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 29 Representative illustrations of Buccicrenata ex gr. subgoodlandensis: a Uncoiled equatorial section, Loeblich & Tappan (1985, pl. 2, fig. 7, Texas); b Close up of section through wall and septum, Loeblich & Tappan (1985, pl. 2, fig. 10, Texas); c Equatorial section, Loeblich & Tappan (1985, pl. 2, fig. 5, Texas); d External view, Loeblich & Tappan (1985, pl. 2, fig. 9, Texas).
Fig. 33 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 33 Representative illustrations of Pseudocyclammina sarvakensis: a Equatorial section, Schlagintweit & Yazdi-Moghadam (2023, fig. 4b, Iran, holotype); b Subaxial section, Ibid. (2023, fig. 4d, Iran); c Oblique tangential section, Ibid. (2023, fig. 4f, Iran). Not scale bar change for figs. b & c.
Fig. 23 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 23 Representative illustrations of Fleuryana gediki: a Equatorial section, Solak et al. (2020, fig. 15(R), Turkey); b Axial section, Solak et al. (2020, fig. 15(S), Turkey).
Fig. 31 in "Larger" Benthic Foraminifera Of The Cenomanian. A Review Of The Identity And The Stratigraphic And Palaeogeographic Distribution Of Non-Fusiform Planispiral (Or Near-Planispiral) Forms
Fig. 31 Representative illustrations of Pseudocyclammina rugosa: a Equatorial section, Maync (1952, pl. 12, fig. 9, France); b Equatorial section of uncoiled specimen, Maync (1959b, pl. 1, fig. 14, France); c Axial section, Maync (1952, pl. 12, fig. 8, France).
Fig. 1 in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 1. Measured column of the Qorban member in the study locality. A. Position of the Qorban section in the general map of Iran. B. Satellite image with the position of the section base (star). C. Qorban Member stratigraphy with indication of the four Mardinella-rich levels studied in this work. Abbreviations: Fm., Formation; Maas., Maastrichtian; SBZ, Shallow Benthic Zones; U.C., Upper Cretaceous.
Fig. 3 in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 3. Megalospheric forms of soritid foraminifer Mardinella daviesi (Henson, 1950) from the Thanetian, Paleocene of Iran. A. Gmm13980F41b, centred section of a gamont (A2) individual. C, E, G. Gmm13980F39a, Gmm13980F39c, Gmm13980F41c, respectively, juvenile schizonts (A1) in equatorial (C, G) and axial (E) views. B, H. Gmm13980F40e, Gmm13980F41d, respectively, equatorial section of an adult schizont. D. Gmm13980F39b, subaxial sections of two adult schizonts. F. Gmm13980F39d, equatorial section of an adult schizont; note the crosswise oblique disposition of pillars. Scale bar 1 mm.
Fig. 2. Microspheric B in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 2. Microspheric B forms (agamonts) of soritid foraminifer Mardinella daviesi (Henson, 1950) from the Thanetian, Paleocene of Iran. A. Gmm13980F40a, subaxial oblique section; note the brood chambers in the adult reproductive stage of growth (arrows). B. Gmm13980F40b, axial section showing empty brood chambers (two-headed arrow) on both sides of the specimen. C. Gmm13980F40c, subequatorial section. D. Gmm13980F40d, oblique section with some brood chambers (two-headed arrow). E. Gmm13980F41a, fragment of shell with five brood chambers; note the irregularly disposed beams. Scale bar 1 mm.
Fig. 6 in Seasonal response of benthic foraminifera to anthropogenic pressure in two stations of the Gulf of Trieste (northern Adriatic Sea, Italy): the marine protected area of Miramare versus the Servola water sewage outfall
Fig. 6: Rank-frequency diagram for the Ser(a) and Res(b) stations using the cumulative abundance (as relative frequency) for y-axe and the decreasing rank order for x-axe of each species for each sample. Both axes are on logarithmic scale.
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