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6 results for “Elazigina”

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Fig. 1 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 1. Paleogeographic distribution of Elazigina (open circles) and Laffitteina (red circles) in latest Maastrichtian (A) and Paleocene (B). Records for the Maastrichtian are from Rahaghi (1992); Inan (1988, 2005); Schlüter et al. (2008); Goldbeck and Langer (2009); Hottinger (2014 and the references herein); and this work. Records for the Paleocene are from Rahaghi (1992); Inan (2005); Hottinger (2014 and the references herein); Serra-Kiel et al. 2016); and Benedetti et al. (2018). Maps are from Scotese (2013, 2014).

opencc-by-4.0Aug 2018View details →
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Fig. 4 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 4. Rotaliid foraminifer Elazigina siderea sp. nov. (A, holotype) from the Maastrichtian of Rod Abad section, Iran; axial (A, B, D, I, K), subaxial (E–H, J, L, N, O), oblique (C), and transversal-basal (M) sections. A–D, G, J–O. APNU-Tf12 (type-level). F, H, N. APNU-Tf11. E. APNU-Tf4. Abbreviations: f, feathers; pi, piles; pl, umbilical plug; sc, spiral canal.

opencc-by-4.0Aug 2018View details →
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Fig. 6. A–F in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 6. A–F. Facies from the Tarbur Formation of Rod Abad section, Iran. A, C, D. Packstone with Pseudomphalocyclus blumenthali Meriç, 1980 (o) and Elazigina siderea sp. nov. (e). B, E. Packstone-wackestone with Fissoelphidium operculiferum Smout, 1955 (f), Elazigina siderea sp. nov. (e), and mollusc fragments. F. Packstone-grainstone with Loftusia (lo) and echinoderm fragments (ec). G, H. Orbitokathina sp. G. APNU-Tf14. H. APNU-Tf12. Scale bars A–F, 1 mm; G, H, 0.5 mm.

opencc-by-4.0Aug 2018View details →
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Fig. 3 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 3. Stratigraphic columns from Mandegan (A) and Rod-Abad (B) sections with position of the studied samples and distribution of Elazigina siderea sp. nov.

opencc-by-4.0Aug 2018View details →
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Fig. 5 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 5. Rotaliid foraminifer Elazigina siderea sp. nov. from the Tarbur Formation of Rod Abad (A, C, D, F–J) and Mandegan (B, E, K) sections, Iran; transversal (A, C, E, J), transversal-basal (B, O), transversal-oblique (D, F–I, L), and tangential (K, M, N, P) sections. C, J, L, M. APNU-Tf12 (typelevel). D, G–I, P. APNU-Tf11. A, N. APNU-Tf10. F. APNU-Tf14. O. APNU-Tf4. B, E. APNU-Rt53. K. APNU-Rt55. Abbreviations: f, feathers; fo, folia; is, intraseptal canals; pi, piles; pl, umbilical plug; pr, proloculus; up, umbilical plate; sc, spiral canal.

opencc-by-4.0Aug 2018View details →
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Fig. 2 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran

Fig. 2. Position (asterisked) of studied localities in the general map of Iran (A) and position of Rod-Abad section (B).

opencc-by-4.0Aug 2018View details →

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