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Species Globorotalia broedermanni Cushman & Bermudez 1949 |
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Alternative name: |
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Diagnosis / Definition: |
Bolli (1957):
Shape of test biconvex, low trochospiral, moderately compressed; equatorial periphery nearly circular; axial periphery rounded to subangular. Wall calcareous, perforate, surface covered with short spines. Chambers subangular, inflated; about 12-15, arranged in 2 1/2 -3 whorls, the 5-6 chambers of the last whorl increasing slowly in size. Sutures on spiral side curved, slightly depressed between last chambers of final whorl; on umbilical side radial, slightly depressed. Umbilicus narrow, open. Aperture a low arch; interiomarginal, extraumbilical umbilical. Coiling over 90 percent dextral. Largest diameter of hypotype 0.33 mm. |
Discussion / Comments: |
Bolli (1957):
The origin of Globorotalia broedermanni Cushman and Bermudez cannot be traced in the Trinidad sections. The species appears at the base of the Globorotalia rex zone apparently fully developed and with a strong preference for dextral coiling (indicating an advanced evolutionary stage). A marked faunistic change between the Globorotalia rex zone and the older Globorotalia velascoensis zone indicates a hiatus in the studied sections. It is in this missing interval that possible ancestral forms of Globorotalia broedermanni have to be sought. |
Systematics: |
20 Genus Globorotalia
Species Globorotalia compressa
Species Globorotalia velascoensis
24 Genus Porticulasphaera
Species Globigerapsis index
Species Globorotalia aspensis
Species Globorotalia broedermanni
Species Porticulasphaera mexicana
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Synonym list: |
Bolli (1957):
Bolli (1957):
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Was used in synonym list of: |
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References: |
Cushman,J.A. and Bermudez,P.J. (1949): Some Cuban species of Globorotalia . Contributions from the Cushman Foundation for Foraminiferal Research Vol. 25 p. 26-44
Bolli,H.M. (1957): The genera Globigerina and Globorotalia in the Paleocene-Lower Eocene Lizard Springs Formation of Trinidad, B.W.I . Bulletin of the U.S. National Museum Vol. 215 p. 61-82
Bolli,H.M. (1957): Planktonic Foraminifera from the Eocene Navet and San Fernando formations of Trinidad, B.W.I. . Bull. U.S. natl. Mus. Vol. 215 p. 155-172
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