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Apertural features and surface texture of upper Paleogene biserial planktonic foraminifers: links between Chiloguembelina and Streptochilus.

January 1, 1985

Several upper Paleogene species of Chiloguembelina have an internal apertural plate that is very similar to the internal plate typical of the Neogene genus Streptochilus. The type species of Chiloguembelina, C. midwayensis midwayensis (Cushman), however, lacks any internal apertural structure or modifications. Therefore, the following 'Chiloguembelina', which have an internal plate, are assigned to Streptochilus: S. cubensis (Palmer), S. martini (Pijpers) and S. sp.aff. S. martini. -Authors

Publication Year 1985
Title Apertural features and surface texture of upper Paleogene biserial planktonic foraminifers: links between Chiloguembelina and Streptochilus.
DOI 10.2113/gsjfr.15.1.1
Authors R.Z. Poore, L.B. Gosnell
Publication Type Article
Publication Subtype Journal Article
Series Title Journal of Foraminiferal Research
Index ID 70013135
Record Source USGS Publications Warehouse
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