Clavatorella nicobarensis Srinivasan & Kennett 1974 from: Srinivasan, M.S.Kennett, J.P. (1974): A planktonic foraminifer (Clavatorella) from the Pliocene . Journal of Foraminiferal Research Vol. 4 p. 77-79 . |
Notice: This catalogue page may contain unedited data.
To find validated information on this taxon please visit the following project pages: |
Species Clavatorella nicobarensis Srinivasan & Kennett 1974 |
|
|
Diagnosis / Definition: |
Kennett & Srinivasan (1983):
Test small, outline deeply lobulate, coiled in low trochospire; spiral side evolute, umbilical side involute with moderately shallow umbilicus. The spire is mostly
level or depressed below spiral surface of final whorl of chambers, giving false impression of biumbilicate, planispiral test; large specimens consist of nearly two
whorls containing nine or more chambers with five (or rarely six) in final whorl; early chambers spherical to subspherical, with later chambers progressively more radially elongate; sutures essentially radial, slightly curved, and depressed; wall penetrated by closely spaced pores and surface roughened by cancellate ridges between pores and by irregular calcite growths on ridges;
aperture simple, extending from the umbilicus to the periphery along base of final chamber, showing individual variation in height, and bordered by distinct, uniform, perforate lip throughout length; aperture does not extend
across the periphery onto dorsal side. |
Discussion / Comments: |
Kennett & Srinivasan (1983):
Cl. bermudezi (Bolli) is most closely related to Cl. nicobarensis but differs in swollen extremities of later
chambers, which are much more separated at their attenuated proximal ends. Also the wall surface of Cl. bermudezi (Bolli) is distinctly pitted. The former species also has
similar depressed trochoid coiling and shallow umbilical depression and a comparably placed but more elevated aperture. It appears to be the direct ancestor of Cl. nicobarensis.
Protentella prolixa Lipps differs in being planispiral and in having an equatorial symmetrical aperture.
Van Eijden & Smit (1991):
Remarks. A species indistinguishable from C. nicobarensis occurs in the uppermost Oligocene at Sites 757 and 758, although its reported range is upper Miocene-Pliocene. |
Systematics: |
3 Classis Foraminifera
Genus Clavatorella
Species Clavatorella nicobarensis
32 Ordo Foraminiferida
Familia Globorotaliidae
Genus Clavatorella
Species Clavatorella nicobarensis
|
Synonym list: |
Srinivasan & Kennett (1974):
Van Eijden & Smit (1991):
|
References: |
Srinivasan,M.S. and Kennett,J.P. (1974): A planktonic foraminifer (Clavatorella) from the Pliocene . Journal of Foraminiferal Research Vol. 4 p. 77-79
Kennett,J. and Srinivasan,M.S. (1983): Neogene Planktonic Foraminifera - A Phylogenetic Atlas.
Van Eijden,A.J.M. and Smit,J. (1991): Eastern Indian Ocean Cretaceous and Paleogene quantitative biostratigraphy. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 121 Eds: Weissel, J.Peirce, J.Taylor, E.Alt, J. p. 77-123
|
This work is licensed under a Creative Commons Attribution 2.5 License.
|
|