Chaisson & Pearson (1997):
This species is distinguished from H. scitula by its coarser textured test and the delicate keel on the final chamber. Well-developed specimens are found in upper Miocene Sample 154-925B-22H-5, 65-67 cm, below its published FO (Kennett and Srinivasan, 1983). In Sample 154-925B-18H-5, 65-67 cm, specimens with an imperforate band entirely around the periphery of the test are observed, resembling H. margaritae primitiva. In Sample 154-925B-17H-5, 65-67 cm, H. cibaoensis specimens have fully keeled
chambers. |
Bermudez,P.J. (1949): Tertiary smaller foraminifers of the Dominican Republic . Spec. Publ.Cushman Lab. Foraminiferal Res., Vol. 25 p. 1-322
Kennett,J. and Srinivasan,M.S. (1983): Neogene Planktonic Foraminifera - A Phylogenetic Atlas.
Chaisson,W.P. and Pearson,P.N. (1997): Planktonic foraminifer biostratigraphy at Site 925: middle Miocene–Pleistocene. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 154 Eds: Shackleton, N.J.Curry, W.B.Richter, C.Bralower, T.J.
Chaisson,W.P. and d'Hondt,S.L. (2000): Neogene planktonic foraminifer biostratigraphy at Site 999, Western Caribbean Sea. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 165 Eds: Leckie, R.M.Sigurdsson, H.Acton, G.D.Draper, G. p. 19-56
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