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572 results for “Late Eocene”
Fig. 17 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 17. Distribution of latest Bartonian, Priabonian and Oligocene heterosteginid populations (mean values at the 95.44% confidence level) on the P–X (proloculus diameter versus number of undivided post−embryonic chambers) bivariate plot (X is on logarithmic scale).
Fig. 9 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 9. Distribution of the Eocene heterosteginid populations (mean values at the 95.44% confidence level) on the S–X (density of chamberlets in chamber 14 versus number of undivided post−embryonic chambers) bivariate plot (both scales are logarithmic).
Fig. 8 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 8. Distribution of heterosteginid specimens from sample Keçili 11 on the P–X (proloculus diameter versus number of undivided post−embryonic chambers) bivariate plot (X is on logarithmic scale). Solid circles, Heterostegina armenica; open circles, H. reticulata.
Fig. 6 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 6. The evolution of Heterostegina reticulata in the Mossano section (drawn after Papazzoni and Sirotti 1993) as reflected in the mean values (±2 s.e.) of three different parameters.
Fig. 7 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 7. Distribution of heterosteginid specimens from sample Possagno 1 on the P–S (proloculus diameter versus density of chamberlets in chamber 14) bivariate plot. Solid circles, Heterostegina reticulata; open circles, H. gracilis.
Fig. 4 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 4. The type locality of Heterostegina reticulata near the chalet Oberbergli (Switzerland). The uppermost Hohgant Sandstone includes here the transitional bed called Discocyclina Limestone. Photo: R. Stockar in 2005.
Fig. 14. Latest Bartonian and early Priabonian Heterostegina from different Western Tethyan localities. A–F in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 14. Latest Bartonian and early Priabonian Heterostegina from different Western Tethyan localities. A–F. Heterostegina reticulata reticulata Rütimeyer, 1850, latest Bartonian, SBZ 18 C. A–E. Mossano 3 (N Italy), equatorial sections, MÁFI E. 9549, A−form (A), MÁFI E. 9550, A−form (B), MÁFI E. 9551, A−form (C), MÁFI E. 9552, B−form (D), MÁFI E. 9553, A−form (E). F. Vedi (Armenia), MÁFI E. 9554, A−form, equatorial section. G–R. Heterostegina reticulata mossanensis ssp. nov., earliest Priabonian, SBZ 19 A. G–J. Mossano 6, equatorial sections, holotype, MÁFI E. 9555, A−form (G), paratype, MÁFI E. 9556, A−form (H), paratype, MÁFI E. 9557, A−form (I), paratype, MÁFI E. 9558 (J), B−form. K–M. Úrhida 10 (Hungary), Ą
Fig. 5 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 5. Normal fault at the road from Mossano to Monte Stria just before the junction with the cross−road to Olivari. Marne di Priabona in the left, Calcari nummulitici in the right side. Photo: C.A. Papazzoni in 1989.
Fig. 2 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 2. The measurement system in the equatorial section of megalospheric Heterostegina (see also text). Pre−heterosteginid chambers (X) are marked by solid circles, secondary chamberlets in chamber 14 (S) by asterisks.
Fig. 3. Locality maps. A in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 3. Locality maps. A. Geographical position of the samples studied. B. Detailed location of the Mossano samples (Italy) drawn after Papazzoni and Sirotti (1993). C. Detailed location of samples from Verona, Castel San Felice (Italy). D. Detailed location of the Úrhida samples (Hungary). E. Detailed location of the Şarköy samples (Turkey).
Fig. 16 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 16. Distribution of the latest Bartonian, Priabonian and Oligocene heterosteginid populations (mean values at the 95.44% confidence level) on the S–X (density of chamberlets in chamber 14 versus number of undivided post−embryonic chambers) bivariate plot (both scales are logarithmic).
Fig. 1 in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 1. Terminology for external features of Heterostegina: Heterostegina gracilis (A) and Heterostegina armenica (B).
Fig. 8 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 8. Equatorial sections of megalospheric upper Oligocene and lowermost Miocene Spiroclypeus blanckenhorni Henson, 1937 from Turkey. A. Upper Chattian, SBZ 23, Kelereşdere (E Turkey), sample KEL 29, MÁFI O. 08.3. B. Lower Aquitanian, SBZ 24, Tuzlagözü (Central Turkey), sample TUZ 1, ITU O/TUZ.1−42.
Fig. 2 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 2. The measurement system in the equatorial section of megalospheric Spiroclypeus. Pre−heterosteginid chambers (X) are marked by solid circles, secondary chamberlets in chamber 14 (S) by asterisks.
Fig. 6 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 6. Distribution of spiroclypeid populations (mean values at the 95.44% confidence level) on the D–X (second whorl diameter versus operculinid reduction) bivariate plot (X is on logarithmic scale).
Fig. 1 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 1. Terminology for external and lateral features of Spiroclypeus: Spiroclypeus carpaticus (A) and Spiroclypeus sirottii (B).
Fig. 5 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 5. Distribution of spiroclypeid populations (mean values at the 95.44% confidence level) on the P–X (proloculus diameter versus operculinid reduction) bivariate plot (X is on logarithmic scale).
Fig. 4 in The late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys
Fig. 4. Distribution of spiroclypeid populations (mean values at the 95.44% confidence level) on the S–X (heterosteginid escalation versus operculinid reduction) bivariate plot (both scales are logarithmic).
Fig. 5. A in A new salamander from the late Paleocene-early Eocene of Ukraine
Fig. 5. A salamander Seminobatrachus boltischki gen. et sp. nov. from the lower unit of Boltyshka sapropelite strata (late Paleocene–early Eocene, Ukraine), close up of part and counterpart of skull, anterior part of vertebral column with traces of soft tissue, PIN 3991/6. A. PIN 3991/6a, part in dorsal aspect. B. PIN 3991/6b, counterpart in ventral aspect. Photographs as exposed (A1, B1) and interpretative drawings (A2, B2). Grey areas in interpretive drawings represent soft tissues.
Fig. 2. A in A new salamander from the late Paleocene-early Eocene of Ukraine
Fig. 2. A salamander Seminobatrachus boltischki gen. et sp. nov. from the lower unit of Boltyshka sapropelite strata (late Paleocene–early Eocene, Ukraine), articulated, incomplete vertebral column (trunk, sacral, and anterior caudal regions) and limbs, PIN 3991/1a, part in lateral aspect. A. Photograph as exposed. B, C. Digital reconstructions based on high−resolution computed tomography of entire specimen (B) and close up of pectoral region rotated 90° counterclockwise (C).
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