Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
| Line 7: | Line 7: | ||
<font size="2"> | <font size="2"> | ||
The Miocene–Pliocene Manzanilla Formation of northern Trinidad marks the arrival of the east-west flowing Orinoco River. Foraminifera were examined quantitatively in samples obtained at ∼5 m intervals from the lowest member of the formation, the San José Calcareous Silt Member, where exposed at eastern Manzanilla Bay and Point Noir. Recovery of ''Globorotalia merotumida'' indicates an age within the ''Globorotalia acostaensis'' Zone through Globorotalia margaritae evoluta Subzone, (N16–N19). Values of the information function (H) and the percentage of the total assemblage as planktonic foraminifera (%P), both traditionally used as palaeodepth indicators, were uncorrelated. ...... <br/> | The Miocene–Pliocene Manzanilla Formation of northern Trinidad marks the arrival of the east-west flowing Orinoco River. Foraminifera were examined quantitatively in samples obtained at ∼5 m intervals from the lowest member of the formation, the San José Calcareous Silt Member, where exposed at eastern Manzanilla Bay and Point Noir. Recovery of ''Globorotalia merotumida'' indicates an age within the ''Globorotalia acostaensis'' Zone through Globorotalia margaritae evoluta Subzone, (N16–N19). Values of the information function (H) and the percentage of the total assemblage as planktonic foraminifera (%P), both traditionally used as palaeodepth indicators, were uncorrelated. ...... <br/> | ||
| − | Highlights | + | '''Highlights''' |
• The San José Calcareous Silt Member was deposited under considerable freshwater influence. | • The San José Calcareous Silt Member was deposited under considerable freshwater influence. | ||
