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10 results for “Salpingoporella”
Fig. 10 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 10 Stratigraphic distribution of Late Cretaceous (here: TuronianMaastrichtian) Salpingoporella species (redrawn from Carras et al., 2006; added the data for S. nicolacarassi from Radoičić and Conrad, 2012).
Fig. 8 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 8 Some dasycladales associated with Salpingoporella pasmanica Radoičić. a-b Pseudocymopolia anadyomenea (Elliott), thin-sections BSPG IX 2016-8 (Rt 89), Rt 67-3. c Pseudocymopolia? sp., thin-section Rt 72. Scale bars 1.0 mm.
Fig. 6 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 6 Salpingoporella pasmanica Radoičić, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Longitudinal section. b-c Oblique sections. d-e, n Tangential sections (partly oblique). f-h, j, l, m Transverse sections (partly slightly oblique). Thin-sections: Rt 113 (a) SNSB-BSPG 2016 III-8 (b-l, n), SNSB-BSPG 2016 III-3 (m).
Fig. 5 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 5 Salpingoporella pasmanica Radoičić, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. a Longitudinal section. b-d, m Longitudinal-tangential sections. e-f Oblique sections. g-l, n, o Transverse sections, partly slightly oblique. Thin-sections: Rt 89-2B (a-d), Rt 79-2 (e-f), SNSB-BSPG 2016 III-6 (g-o).
Fig. 4 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 4 Microfacies of Late Maastrichtian Tarbur Formation. a Bioclastic wacke-/packstone with large benthic foraminifer Loftusia sp. and dasycladale Salpingoporella pasmanica Radoičić (transverse section, arrow and detailed view). Thinsection Rt 177-1. Scale bars: 1.0 mm and 0.3 mm (detail, right below). b Bioclastic wacke-/packstone with large benthic foraminifera (Dicyclina? sp.), and dasycladalean algae Salpingoporella pasmanica Radoičić (arrow) and Salpingoporella? sp. with tilted laterals.
Fig. 3 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 3 Vertical distribution (total range) of selected taxa of larger benthic foraminifera and dasycladalean algae in the Tarbur Formation of the Mandegan section.
Fig. 1 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 1 Lithostratigraphy of the Late Cretaceous of the Zagros Zone, Iran (excerpt from the Stratigraphic Chart of Iran).
Fig. 9 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 9 Some biostratigraphic importance larger benthic foraminifera from the Maastrichtian Tarbur Formation of the Mandegan section. a Omphalocyclus macroporus (Lamarck), thin-section RT 65. b-c Neobalkhania bignoti Cherchi, Radoičić & Schroeder, thin-sections Rt 79-2, SNSB-BSPG 2016 III-6 (Rt 79). d Orbitoides media d´Archiac, thinsection RT 30. e Gyroconulina columellifera Schroeder & Darmoian, thin-section Rt 113. f Loftusia sp., thin-section Rt 113. g Siderolites cf. calcitrapoides Lamarck, thin-section Rt 36. Scale bars = 1.0 mm, except b-c, e = 0.5 mm.
Fig. 7 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 7 Schematic distribution of larger benthic foraminifera in the Eocene Trentinara Formation of Italy (based on Vecchio and Hottinger, 2007, fig. 5), and the Maastrichtian Tarbur Formation (examples; without scale). 1 Rotaliids (e.g., Rotorbinella), 2 Siderolites, 3 Orbitoides, 4 Loftusia, 5-6 Orbitolinidae (5: Dictyoconella minima), 7 Gyroconulina, 8 Rhapydionidae, 9 Spirolina, 10 Pyrgo?, 11 Broeckina. 5-7: Agglutinated conical foraminifera, 8-11: Porcelaneous foraminifera. Note the basinal facies corresponds to the Gurpi Formation.
Fig. 2 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran
Fig. 2 Location map of the studied area and Mandegan section.
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