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Praealveolina

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Journal Article
Published: 01 January 2002
Micropaleontology (2002) 48 (1): 53–66.
... the stratigraphical range of each species. The species Praealveolina iberica, P. pennensis and P. debilis successively replace each other from Early to Mid Cenomanian; they have been correlated with Mantelliceras mantelli and Acanthoceras rotomagense ammonite zones, and with Rotalipora brotzeni and the lower part...
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—Type Magwa Formation, Mishrif Limestone Member, Umm Gudair no. 1 well; alv...
Published: 01 November 1973
Fig. 6 —Type Magwa Formation, Mishrif Limestone Member, Umm Gudair no. 1 well; alveolinid, dicyclinid, algal, clayey limestone with no planktonic Foraminifera (Mi/B2). 1, Near-equatorial section of Praealveolina sp. in skeletal, micritic, clayey limestone groundmass (core sample from 4,638
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Benthonic foraminifera of the Early Cenomanian  <span class="search-highlight">Praealveolina</span> iberica  inte...
Published: 01 October 2013
Figure 12: Benthonic foraminifera of the Early Cenomanian Praealveolina iberica interval zone (as = axial section; sas = subaxial section; es = equatorial section; ses = subequatorial section; os = oblique section; ts = transversal section; ls = longitudinal section). (1 and 2) Praealveolina
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Benthonic foraminifera of Early Cenomanian  <span class="search-highlight">Praealveolina</span> iberica  interval...
Published: 01 April 2012
Figure 6d: Benthonic foraminifera of Early Cenomanian Praealveolina iberica interval zone: (1 and 2) Cuneolina pavonia , [os] through a young megalospheric form, (3) Nezzazatinella picardi [sas] (Zbeideh), (4 and 8) Nezzazata simplex , [ses] (Admir), (25) [sas] (Zbeideh). (5) Nezzezata
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(a) Foraminiferal bioclastic wackestone, <span class="search-highlight">Praealveolina</span> in micrite matrix; H...
Published: 01 October 2009
Figure 7: (a) Foraminiferal bioclastic wackestone, Praealveolina in micrite matrix; Halal Formation, Gabal Yelleg, P.L. (b) Durania assemblage (Y8), closed fabric of Durania individuals mutually supported, elevator morphotypes and autochthonous fabric of the Durania arnaudi shells; Wata Formation
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—<span class="search-highlight">Praealveolina</span> limestone from upper Sarvak Formation of Khuzestan. Cenomani...
Published: 01 December 1965
Fig. 40. —Praealveolina limestone from upper Sarvak Formation of Khuzestan. Cenomanian. ×25.
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Benthonic foraminifera of Late Cenomanian  Pseudedomia drorimensis  range z...
Published: 01 April 2012
], (8) [as] (Admir). (9, 10, 15, 18, 21 and 25) Praealveolina tenuis , (9, 21 and 25) [sas], (9) (Admir), (21 and 25) (Zbeideh), (10 and 18) [as] (Zbeideh). (11) Praealveolina simplex , [sas] (Zbeideh). (12 and 20) Hemicyclammina sp., (12) [as], (20) [ses] (Admir). (13 and 22) Praealveolina
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1973
AAPG Bulletin (1973) 57 (11): 2263–2279.
...Fig. 6 —Type Magwa Formation, Mishrif Limestone Member, Umm Gudair no. 1 well; alveolinid, dicyclinid, algal, clayey limestone with no planktonic Foraminifera (Mi/B2). 1, Near-equatorial section of Praealveolina sp. in skeletal, micritic, clayey limestone groundmass (core sample from 4,638...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2011
GeoArabia (2011) 16 (3): 17–26.
... simplex Reichel, appear together with orbitolines, Orbitolina (Mesorbitolina) aperta (Erman) and O. ( Conicorbitolina) conica (D’Archiac); (2) in the Khadrafi and Sarfait members there are no orbitolines and only Praealveolina cretacea Reichel is cited. The ages suggested by these authors...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2012
GeoArabia (2012) 17 (2): 155–184.
...Figure 6d: Benthonic foraminifera of Early Cenomanian Praealveolina iberica interval zone: (1 and 2) Cuneolina pavonia , [os] through a young megalospheric form, (3) Nezzazatinella picardi [sas] (Zbeideh), (4 and 8) Nezzazata simplex , [ses] (Admir), (25) [sas] (Zbeideh). (5) Nezzezata...
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Series: AAPG Memoir
Published: 01 January 1993
DOI: 10.1306/M56578C21
EISBN: 9781629810973
...) to middle Cenomanian (Praealveolina cretacea) Tectonic-sedimentary setting: Platform developed in the conjunction of the Iberian aulacogen with the eastern Tethyan margin of the Iberian plate Basin type: Pericontinental to peri-epicontinental Paleoclimate: Not well known, probably warm and humid...
Journal Article
Published: 01 January 1966
Micropaleontology (1966) 12 (1): 65–70.
...K. H. A. Gohrbandt Abstract Thomasinella punica, Buccicrenata libyca n.sp., and Praealveolina cretacea tenuis from the lower Cenomanian (Cretaceous) Ain Tobi formation of the Kussabat area, northwest Libya, are described. Data on the stratigraphy of the section exposed along the Homs-Kussabat road...
Journal Article
Published: 01 January 1964
Bulletin de la Société Géologique de France (1964) S7-VI (2): 273–277.
... of the Pyrenees. The limestone is locally underlain by a thin bed of quartz conglomerate, quartzite, and shale of unknown age. The basal part of the limestone, generally sandy or conglomeratic and with local beds of dolomite, is dated as Cenomanian (basal upper Cretaceous) by the foraminifer Praealveolina...
Image
—Type Magwa Formation, Mishrif Limestone Member, Umm Gudair no. 1 well; alv...
Published: 01 November 1973
Fig. 7 —Type Magwa Formation, Mishrif Limestone Member, Umm Gudair no. 1 well; alveolinid, dicyclinid, algal, clayey limestone with no planktonic foraminifers (Mi/B2). 1, Axial section in Praealveolina sp. in skeletal, micritic, clayey, limestone groundmass (core sample 4,682–4,686 ft
Journal Article
Published: 01 December 2006
Micropaleontology (2006) 52 (5): 471–476.
... Praealveolina cretacea lower interval The Cisalveolina sp. upper interval yields the following assemblage: Cisalveolina sp., Biplanata peneropliformis Hamaoui and Saint-Marc 1970 , Carinoconus iraqiensis n. sp., Chrysalidina gradata d’Orbigny 1839 , Coxites zubairensis Smout 1956 , Cycledomia...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1972
AAPG Bulletin (1972) 56 (8): 1464–1493.
... a rich foraminiferal assemblage was recorded by Owen and Nasr (1958) including Multispirina iranensis Reichel, Cisalveolina fallax Reichel, C. lehneri Reichel, Pseudochrysalidina conica (Henson), Taberina bingistani (Henson), Dicyclina qatarica Henson, and Praealveolina cretacea (d’Archiac...
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Journal Article
Published: 01 February 2006
Petroleum Geoscience (2006) 12 (1): 59–68.
... with a Praealveolina biozone. The top boundary in both areas has been chosen based on the overall facies evolution, showing a turnaround to a long-term increase in accommodation (this study and Van Buchem et al . 2002 a ). A remarkable difference between sequence II in the studied area and Oman is that the latter...
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Journal Article
Published: 01 January 2011
Journal of Foraminiferal Research (2011) 41 (1): 41–52.
... Range. Praeaveolina zones from Calonge and others 2002 . Sellialveolines in the upper interval occur in thin-bedded limestones intercalated with massive and dolomitic limestones of the Villa de Vés Formation. They are associated with Praealveolina debilis Reichel, Orbitolina ( C...
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Journal Article
Published: 20 October 2021
Bulletin de la Société Géologique de France (2021) 192 (1): 49.
... gr. T Arabica , Praeglobotruncana delrioensis , Rotalipora cushmani , Praealveolina cushmani , Praealveolina cretacea , Orbitolina conica , Orbitolina paeneconica , Orbitolina concava , Latest Albian/Santonian Flysch à silex Fm. ( Boissonnas et al. , 1974 ; Le Pochat et al. , 1976...
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Journal Article
Journal: Geology
Published: 01 September 2008
Geology (2008) 36 (9): 715–718.
...-strategists among the late Cenomanian larger foraminifers. The shells of adult individuals of Cisalveolina and Praealveolina can commonly reach diameters of 5 mm and 15 mm, respectively. Large size is generally the result of a long life cycle, a trait that is most advantageous in stable, nutrient-poor...
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