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Sevketiye Formation

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Stratigraphic columns of the <span class="search-highlight">Şevketiye</span> <span class="search-highlight">Formation</span> in the <span class="search-highlight">Şevketiye</span> and Çamyu...
Published: 01 July 2022
Figure 2. Stratigraphic columns of the Şevketiye Formation in the Şevketiye and Çamyurt sections and position of the samples ŞEV6, ŞEV 7, and ÇAM14-17 with Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp. SBZ = Shallow Benthic Zones by Serra-Kiel et al
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Field photographs of the upper part of the <span class="search-highlight">Şevketiye</span> <span class="search-highlight">Formation</span> near Çamyurt...
Published: 01 July 2022
Figure 3. Field photographs of the upper part of the Şevketiye Formation near Çamyurt and Şevketiye villages in the Biga Peninsula and locations of the samples with Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp. Characteristic LBFs at both localities
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Line drawings of the embryonic and peri-embryonic chambers/chamberlets of  ...
Published: 01 July 2022
Figure 7. Line drawings of the embryonic and peri-embryonic chambers/chamberlets of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp., from the Şevketiye Formation. ( 1, 2 , 5 , 7 ) Çamyurt Section, SBZ 19A, Priabonian; ( 3, 4 , 6 ) Şevketiye Section; SBZ
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Equatorial sections of  Bigaella orbitoidiformis  Özcan, Mitchell, Pignatti...
Published: 01 July 2022
Figure 9. Equatorial sections of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp., from the Şevketiye Formation showing the transition from cyclical chamberlets to annular chambers with complex internal structures. The stolons of annular chambers
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Equatorial sections of  Bigaella orbitoidiformis  Özcan, Mitchell, Pignatti...
Published: 01 July 2022
Figure 8. Equatorial sections of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp., from the Şevketiye Formation showing its embryonic-nepionic stages. Note the lobate outline of the third chamber, which is a very characteristic feature. ( 1–5 ) Şevketiye
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( 1 ) Paleogeographic location of the Biga Peninsula during late middle Eoc...
Published: 01 July 2022
Figure 1. ( 1 ) Paleogeographic location of the Biga Peninsula during late middle Eocene paleogeography (reconstruction kindly provided by Halliburton and created from various sources, notably Stampfli and Borel, 2004 ). The star denotes the location of Biga Peninsula where the Şevketiye
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( 1–5, 8–10 ) Equatorial ( 6, 7 ) axial, and ( 11 ) sub-axial sections of  ...
Published: 01 July 2022
Figure 6. ( 1–5, 8–10 ) Equatorial ( 6, 7 ) axial, and ( 11 ) sub-axial sections of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp., from the Şevketiye Formation. ( 1–6 ) Şevketiye Section; SBZ 17/18A, Bartonian or late Bartonian–early Priabonian. ( 7–11
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Line drawings of the embryonic and peri-embryonic chambers/chamberlets of  ...
Published: 20 January 2022
Figure 8. Line drawings of the embryonic and peri-embryonic chambers/chamberlets of Caudriella ospinae (Caudri) from the Keşan Formation, SBZ 20, late Priabonian and from the Şevketiye Formation, SBZ 17/18A. Numbers in the equatorial chamberlets denote the growth stages, accepting
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External views (A, E), axial and off-centered axial sections (B–D) and equa...
Published: 20 January 2022
Figure 6. External views (A, E), axial and off-centered axial sections (B–D) and equatorial sections (F–H) of Caudriella ospinae (Caudri) from the Şevketiye Formation, SBZ 17/18A, Bartonian or Bartonian-Priabonian transition and the Keşan Formation, SBZ 20, late Priabonian. A–C) ŞEV7-108. D
Journal Article
Published: 01 July 2022
Journal of Paleontology (2022) 96 (4): 737–752.
...Figure 2. Stratigraphic columns of the Şevketiye Formation in the Şevketiye and Çamyurt sections and position of the samples ŞEV6, ŞEV 7, and ÇAM14-17 with Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp. SBZ = Shallow Benthic Zones by Serra-Kiel et al...
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Line drawings of the embryonic and peri-embryonic chambers/chamberlets of  ...
Published: 01 July 2022
Figure 5. Line drawings of the embryonic and peri-embryonic chambers/chamberlets of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp. from the Şevketiye Formation. ( 1–3 ) Şevketiye Section, SBZ 17/18A, Bartonian or late Bartonian-early Priabonian. ( 4
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Caudriella ospinae  (Caudri) from the Keşan <span class="search-highlight">Formation</span> (A–I) and  Caudriella...
Published: 20 January 2022
Figure 9. Caudriella ospinae (Caudri) from the Keşan Formation (A–I) and Caudriella sp. from Jamaica (J). Sub-axial (A) and equatorial sections (B–I), and interpretation of chamber arrangement in the nepionic stage, SBZ 20, late Priabonian and from the Şevketiye Formation, SBZ 17/18A
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( 1, 2 ) External views, ( 3 ) sub-axial, ( 4 ) axial, and ( 5, 6 ) equator...
Published: 01 July 2022
Figure 4. ( 1, 2 ) External views, ( 3 ) sub-axial, ( 4 ) axial, and ( 5, 6 ) equatorial sections of Bigaella orbitoidiformis Özcan, Mitchell, Pignatti, Simmons, and Yücel, n. gen. n. sp., from the Şevketiye Formation. ( 1, 2 , 4 , 6 ) SBZ 17 or 18A, Bartonian or late Bartonian–early
Journal Article
Published: 20 January 2022
Journal of Foraminiferal Research (2022) 52 (1): 21–39.
...Figure 8. Line drawings of the embryonic and peri-embryonic chambers/chamberlets of Caudriella ospinae (Caudri) from the Keşan Formation, SBZ 20, late Priabonian and from the Şevketiye Formation, SBZ 17/18A. Numbers in the equatorial chamberlets denote the growth stages, accepting...
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Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2016
DOI: 10.5382/SP.19.05
EISBN: 9781629499789
... stages of each extensional phase promoted higher structural permeability, enabling the development of vein systems and low-sulfidation epithermal-style mineralization. Postemplacement crustal extension resulted in “domino-style” block rotations and half-graben formation throughout the Miocene...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP321.10
EISBN: 9781862395695
... Hinsbergen et al. 2005 ; Dilek & Altunkaynak 2007 ). Exhumation of middle to lower crustal rocks and the formation of extensional metamorphic domes occurred in the backarc region of this progressively southward migrated trench and the Tethyan slab throughout the Cenozoic. Fig. 1. Tectonic map...
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