Palaeogene triserial planktonic foraminifera

Author:

Jenkins D. Graham,Whittaker John E.,Curry Dennis

Abstract

Abstract. Triserial planktonic foraminiferal species from the Palaeogene are classified into the Early Danian Guembelitria, with pore mounds on the test surface, and the Early Eocene-Late Oligocene Jenkinsina, which are also microperforate but lack pore mounds. The stratigraphic and palaeogeographic ranges are discussed, the holotype of G. cretacea Cushman (the type species of Guembelitria) is re-illustrated, and neotypes designated for G. danica (Hofker) and Jenkinsina triseriata (Terquem). Chiloguembelitria is shown to be a junior synonym of Guembelitria.

Publisher

Copernicus GmbH

Subject

Paleontology

Reference47 articles.

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3. J., Beckmann: Chiloguembelina Loeblich and Tappan and related foraminifera from the Lower Tertiary of Trinidad, B.W.I, Bulletin of the U.S. National Museum, 215, 83-95, 1957.

4. W. A., Berggren, D. V., Kent and J. J., Flynn: Jurassic to Palaeogene: Part 2Palaeogene geochronology and chronostratigraphyIn (Ed.), The Chronology of the Geological Record, 141–198Blackwell Scientific Publications, Oxford(Memoir of the Geological Society of London, 10)., 1985.

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