FIG. 5. — A, B, Operculina complanata (Defrance, 1822); A, equatorial section, İl-6C/2; B, incomplete equatorial section, İl-6B/2; C, J, Nummulites fichteli Michelotti, 1841; C, external view, İl-6C/3; J, axial section, megalospheric form, İl-6A; D-G, Nephrolepidina praemarginata (Douvillé, 1908); D, axial section, İl-6A; E, external view, İl-6B/4; F, axial section, megalospheric form, İl-6C/1; G, axial section, İl-6B/2. H, I, Eulepidina sp., subaxial sections, İl-6A, İl-6B/5. Scale bars: A, 1 mm; B, D-G, L, 0.5 mm; C, I, J, 2 mm.Published as part of Gedik, Fatma & Karadenizli, Levent, 2021, Oligocene larger benthic foraminifera and sedimentation of the Burdur Basin, SW Anatolia, Turkey, pp. 377-389 in Geodiversitas 43 (13) on page 385, DOI...
The Baskil section, located to the west of Elazığ in eastern Turkey, represents deep-marine facies o...
The Middle Eocene sequence in the Darende-Balaban Basin (Eastern Turkey) characterized by shallow an...
Larger foraminifers were recovered from three levels within Hole 841B, located on the Tongan Platfor...
FIG. 4. — A-J, Nummulites fichteli Michelotti, 1841; A, equatorial section and external view, megalo...
FIG. 2. — Details of the measured sections. Columns at right show the dominance of the facies throug...
FIG. 6. — The chart of Oligocene-Lower Miocene larger foraminiferal biozones (Cahuzac & Poignant 199...
Gedik, Fatma, Karadenizli, Levent (2021): Oligocene larger benthic foraminifera and sedimentation of...
FIG. 3. — Stratigraphic and sedimentological cross sections and stratigraphic correlations of select...
A revision of (early) Burdigalian hyaline larger foraminifera based on the biometric study of miogyp...
Gedik, Fatma (2017): First record of the new Neoplanorbulinid species (Foraminifera) from the Early ...
The Aksu Basin, near Antalya, is an important area from many aspects of the geology as it hosts the ...
The Oligocene strata of the Qom Formation from the Tajar-Kuh section, Central Iran, are rich in vari...
A revision of (early) Burdigalian hyaline larger foraminif-era based on the biometric study of miogy...
Abstract: The Eocene marine sequence in the southern part of the Thrace Basin (NW Turkey) involves a...
DSDP Site 516 contains a complete middle Eocene to lower Miocene interval with a well-developed Olig...
The Baskil section, located to the west of Elazığ in eastern Turkey, represents deep-marine facies o...
The Middle Eocene sequence in the Darende-Balaban Basin (Eastern Turkey) characterized by shallow an...
Larger foraminifers were recovered from three levels within Hole 841B, located on the Tongan Platfor...
FIG. 4. — A-J, Nummulites fichteli Michelotti, 1841; A, equatorial section and external view, megalo...
FIG. 2. — Details of the measured sections. Columns at right show the dominance of the facies throug...
FIG. 6. — The chart of Oligocene-Lower Miocene larger foraminiferal biozones (Cahuzac & Poignant 199...
Gedik, Fatma, Karadenizli, Levent (2021): Oligocene larger benthic foraminifera and sedimentation of...
FIG. 3. — Stratigraphic and sedimentological cross sections and stratigraphic correlations of select...
A revision of (early) Burdigalian hyaline larger foraminifera based on the biometric study of miogyp...
Gedik, Fatma (2017): First record of the new Neoplanorbulinid species (Foraminifera) from the Early ...
The Aksu Basin, near Antalya, is an important area from many aspects of the geology as it hosts the ...
The Oligocene strata of the Qom Formation from the Tajar-Kuh section, Central Iran, are rich in vari...
A revision of (early) Burdigalian hyaline larger foraminif-era based on the biometric study of miogy...
Abstract: The Eocene marine sequence in the southern part of the Thrace Basin (NW Turkey) involves a...
DSDP Site 516 contains a complete middle Eocene to lower Miocene interval with a well-developed Olig...
The Baskil section, located to the west of Elazığ in eastern Turkey, represents deep-marine facies o...
The Middle Eocene sequence in the Darende-Balaban Basin (Eastern Turkey) characterized by shallow an...
Larger foraminifers were recovered from three levels within Hole 841B, located on the Tongan Platfor...