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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Asia
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Primary terms
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Asia
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Europe
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Invertebrata
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Protista
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Foraminifera
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Rotaliina
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Cassidulinacea
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Anomalinidae
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Cibicidoides
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Cibicidoides wuellerstorfi (1)
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Globigerinacea
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Globigerinidae
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Globigerina
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Globigerinoides
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Orbulina
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Orbulina universa (2)
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Globorotaliidae
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Globorotalia
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Globorotalia menardii (1)
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Neogloboquadrina
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Neogloboquadrina dutertrei (1)
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isotopes
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radioactive isotopes
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C-14 (2)
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stable isotopes
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C-13/C-12 (3)
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O-18/O-16 (4)
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metals
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alkaline earth metals
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barium
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Ba/Ca (1)
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calcium
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Ba/Ca (1)
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Mg/Ca (3)
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Sr/Ca (2)
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magnesium
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manganese (3)
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Ocean Drilling Program
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Leg 165
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ODP Site 1000 (1)
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Leg 175
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ODP Site 1087 (1)
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oxygen
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Pacific Ocean
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sediments
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sediments
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marine sediments (3)
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Trilobatus sacculifer
Trilobatus sacculifer internal structure. Every colored chamber represents...
Effect of gross morphology on modern planktonic foraminiferal test strength under compression
Developmental plasticity in deep time: a window to population ecological inference
Western to Central Equatorial Pacific Planktic Foraminiferal Fluxes: Implication for the Relationship Between Their Assemblage and Warm Pool Migration from 1999 to 2002
Example of the contents of the Henry Buckley Collection, NHMUK: ( a ) slide...
Schematic representation of the dissolution effect on a broken planktonic f...
Elemental ratios of translucent (open symbols) and opaque (filled symbols) ...
Edge views of the eight species used in this study: ( a ) Globigerinoides ...
Optical and scanning electron microscope (SEM) images of translucent and op...
Modeled effect of different photosymbiont-related variables on δ 13 C-size ...
Oxygen isotope stratigraphy, age-depth profiles, sedimentation rate curves,...
Effects of seafloor diagenesis on planktic foraminiferal radiocarbon ages
The unknown planktonic foraminiferal pioneer Henry A. Buckley and his collection at The Natural History Museum, London
TAXONOMY, BIOSTRATIGRAPHY, AND PHYLOGENY OF OLIGOCENE TO LOWER MIOCENE GLOBIGERINOIDES AND TRILOBATUS
ABSTRACT The taxonomy, phylogeny and biostratigraphy of late Oligocene and early Miocene Globigerinoides and Trilobatus is reviewed. Trilobatus and Globigerinoides are two long-ranging genera appearing in the late Oligocene and early Miocene, respectively. They diversified within the range interval of Paragloborotalia kugleri and are still present in modern oceans as some of the most abundant mixed-layer dwelling groups. The distinctive characteristic of the genera is the presence of one to several supplementary apertures on the spiral side. Globigerinoides species possess a ruber/sacculifer -type wall, Trilobatus possesses a sacculifer-type wall texture. The ruber -type wall texture probably appeared in the late Miocene with the appearance of G. ruber s.s. The following species of Globigerinoides are recognized as valid: G. altiaperturus Bolli, G. bollii Blow, G. italicus Mosna and Vercesi, G. joli Spezzaferri n. sp., G. neoparawoodi Spezzaferri n. sp., G. obliquas Bolli, and G. subquadratus Brönnimann. The following species of Trilobatus are recognized as valid: T. altospiralis Spezzaferri n. sp., T. immaturus (LeRoy), T. praeimmaturus (Brönnimann and Resig), T. primordius (Blow and Banner), T. quadrilobatus (d’Orbigny), T. subsacculifer (Cita, Premoli Silva, and Rossi) and T. trilobus (Reuss).