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Miogypsinoides

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( a ) A Mediterranean  <span class="search-highlight">Miogypsinoides</span>  ( Mdes bantamensis  Tan Sin Hok), ( ...
Published: 01 January 2013
Fig. 5. ( a ) A Mediterranean Miogypsinoides ( Mdes bantamensis Tan Sin Hok), ( b ) an American Miogypsinoides ( Mdes praegunteri BouDagher-Fadel & Price 2010 ), ( c ) the Mediterranean Miogypsina mediterranea Bronnimann, and ( d ) the South Africa Miogypsina mcmilliana new sp.
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-  <span class="search-highlight">Miogypsinoides</span>  ex. interc.  complanatus-formosensis  from the uppermost...
Published: 01 June 2019
Fig. 5 - Miogypsinoides ex. interc. complanatus-formosensis from the uppermost part of the Porto Badisco Calcarenite (thin section A.8430.2). Scale bar is 500 μm for both specimens.
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<span class="search-highlight">Miogypsinoides</span> formosensis  Yabe and Hanzawa 1928 . Equatorial sections of ...
Published: 01 January 2017
Fig. 11.— Miogypsinoides formosensis Yabe and Hanzawa 1928 . Equatorial sections of megalospheric forms and one microspheric form (F). (A: OM-20; B, D, E, G, I: OM-30; C: OM-29; F: OM-26; H: OM-37).
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( a ) A sketch showing the earliest chamber of a late  <span class="search-highlight">Miogypsinoides</span> , suc...
Published: 01 January 2013
Fig. 3. ( a ) A sketch showing the earliest chamber of a late Miogypsinoides , such as Miogypsinoides complanatus . There are 18 spirally coiled nepionic chambers (biometric index X). The angle of rotation between the apical line of symmetry and the central line crossing the protoconch (p
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( a ,  b ,  n )  <span class="search-highlight">Miogypsinoides</span> dehaarti  ( van der Vlerk 1924 ). ( a ,  b ...
Published: 01 January 2013
Fig. A3. ( a , b , n ) Miogypsinoides dehaarti ( van der Vlerk 1924 ). ( a , b ) Miocene (Burdigalian), Nias, Sumatra, 201, UCL MF175–6, ×50; ( n ) Early Miocene, Middle Burdigalian, Subis Formation, Borneo, UCL MF178, ×24. ( c , d ) Miogypsina kotoi Hanzawa 1931 . Early Miocene, Middle
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( a – c ) Packstone of  <span class="search-highlight">Miogypsinoides</span> cyprea  new species. Late Oligocene,...
Published: 01 January 2013
Fig. A5. ( a – c ) Packstone of Miogypsinoides cyprea new species. Late Oligocene, Chattian, Terra Limestone, Cyprus, UCL MF262–4, ×20. ( d , e ) Miogypsina antillea ( Cushman 1919 ). Late Burdigalian, Cyprus, Terra member, UCL MF265–8, ×27. ( f – h ) Miolepidocyclina burdigalensis
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Photomicrograph of  Miogypsina  sp. and  <span class="search-highlight">Miogypsinoides</span>  sp. in a skeletal ...
Published: 01 July 2005
Figure 47: Photomicrograph of Miogypsina sp. and Miogypsinoides sp. in a skeletal dolopackstone from the Musayr Formation (Tayran Group). This assemblage confirms a basal early Miocene age. Wadi Al Hamd, Midyan Basin (28°23′55.9″N, 34°54′04.2″E). Magnification x 60.
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—Structure map of <span class="search-highlight">Miogypsinoides</span> sand.
Published: 01 December 1962
FIG. 4. —Structure map of Miogypsinoides sand.
Series: GSA Memoirs
Published: 01 February 1957
DOI: 10.1130/MEM66-p1
..., Lepidocyclina (Eulepidina) rotaensis, Discocycline (Discocyclina) indopacifica, and Miogypsinoides saipanensis. The first two are the genotype and subgenotype of the new genus Kanakaia and new subgenus Acervulina (Ladoronia). The age of the formations of the Mariana Islands and the ecological...
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Range chart of Western Tethyan, Late Oligocene to Early Miocene, diagnostic...
Published: 01 January 2009
F igure 1. Range chart of Western Tethyan, Late Oligocene to Early Miocene, diagnostic larger foraminifera. Species succession in Miogypsina , Miogypsinoides , and Miolepidocyclina lineages is after Drooger (1993) . The species succession and stratigraphy of Nephrolepidina are from de
Journal Article
Journal: PALAIOS
Published: 01 January 2017
PALAIOS (2017) 32 (1): 61–82.
... and coralline algae. The presence of Miogypsinoides complanatus and Miogypsinoides formosensis indicates a late Chattian age (Shallow Benthic Zone 23). The depositional profile is consistent with a homoclinal ramp. The absence of a barrier margin and thus, of a lagoon, facilitated the transport and re-working...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1962
AAPG Bulletin (1962) 46 (12): 2121–2132.
...FIG. 4. —Structure map of Miogypsinoides sand. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1966
AAPG Bulletin (1966) 50 (10): 2319.
.... The effect of this fault system is further supported by isopachous maps of the Heterostegina “lime”— Camerina interval and the Camerina-Miogypsinoides Sand interval. Each displays a pronounced thickening of section on the downthrown sides of the faults relative to a corresponding section on the upthrown side...
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The phylogenetic evolution of the Mediterranean and Indo-Pacific  Neorotali...
Published: 01 January 2013
Fig. 6. The phylogenetic evolution of the Mediterranean and Indo-Pacific Neorotalia , Paleomiogypsina , Miogypsinella and Miogypsinoides spp.
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( a )  Neorotalia tethyana  new species. Rupelian, Cyprus, Geroskipou, UCL ...
Published: 01 January 2013
; ( f ) holotype UCL MF229, ×27; ( c – e , g , h ) paratypes UCL MF230–33: ( c ) A, ×40; ( d ) ×42; ( e ) ×43; ( g ) A, ×40; ( h ) ×36. ( i , j ) Miogypsinoides complanatus ( Schlumberger 1900 ). Early Miocene, Aquitanian, Terra Limestone, Cyprus, UCL MF234–5: ( i ) ×32; ( j ) ×40. ( k , l , q
Journal Article
Published: 01 January 2013
Journal of the Geological Society (2013) 170 (1): 185–208.
...Fig. 5. ( a ) A Mediterranean Miogypsinoides ( Mdes bantamensis Tan Sin Hok), ( b ) an American Miogypsinoides ( Mdes praegunteri BouDagher-Fadel & Price 2010 ), ( c ) the Mediterranean Miogypsina mediterranea Bronnimann, and ( d ) the South Africa Miogypsina mcmilliana new sp. ...
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Series: Special Publication
Publisher: SEPM (Society for Sedimentary Geology)
Published: 05 April 2023
DOI: 10.2110/sepmsp.114.13
EISBN: 978-1-56576-369-2
... ranges from Oligocene to Miocene, based on the occurrence of the larger benthic foraminifera Miogypsinoides sp. (late Oligocene, Te4) and Miogypsina sp. (early Miocene, Te5), as well as on the calcareous nannofossils Sphenolithus capricornutus and Sphenolithus conicus (Te4). The boundary between...
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Range chart of Indo–West Pacific, Late Oligocene to Middle Miocene, diagnos...
Published: 01 January 2009
F igure 2. Range chart of Indo–West Pacific, Late Oligocene to Middle Miocene, diagnostic larger foraminifera. Species successions in Miogypsina , Miogypsinoides , and Lepidosemicyclina lineages are after Raju (1974) and Drooger (1993) , with their revised stratigraphic ranges
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2008
GeoArabia (2008) 13 (2): 187–190.
...Nabil Y. Al-Banna Table 1: Kirkuk Group, Qarah Chauq Dagh Area, Iraq (after R.C. van Bellen, 1953 ) Back reef/Lagoonal Faunizones Fore reef/Shoal Faunizones Age Anah Formation Miogypsinoides Miogypsinoides/Lapidocyclina Azkand Formation Miogypsinoides Miogypsinoides...
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A ,  B ) Undetermined form, with characteristics intermediate between  Risa...
Published: 01 January 2017
Fig. 12.— A , B ) Undetermined form, with characteristics intermediate between Risananeiza and Miogypsinoides , OM-24. C – H ) Postmiogypsinella aff. intermedia Sirel and Gedik 2011 , note the occasional lateral chamberlets. (C: OM-29; D, E: OM-24; F–H: OM-35).